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Curtin University, Perth, WA
Editors: Ladislav Mucina and Glen Daniel
VEGETATION MAPPING IN
THE NORTHERN KIMBERLEY,
WESTERN AUSTRALIA
2013
Vegetation Mapping in the
Northern Kimberley,
Western Australia
Editors
Ladislav Mucina and Glen Daniel
Curtin University, Perth
2013
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Published in July 2013 by:
Curtin University
Kent Street
Bentley 6102
Australia
ISBN 13: 978-0-646-90719-2
ISBN 10: 0646907190
Printed by: Advance Press
This a scientific peer-reviewed document.
Suggested citation formats:
The Book:
Mucina, L. & Daniel, G. (eds) 2013. Vegetation Mapping
in the Northern Kimberley, Western Australia. Curtin
University, Perth, WA. ISBN 13: 978-0-646-90719-2,
ISBN 10: 0646907190
A chapter:
Mucina, L., Daniel, G., Stephenson, G., Boonzaaier, I., van
Niekerk, A., Barrett, M., Barrett, R., Tichý, L. & Valachovič,
M. 2013. Floristic-ecological mapping in the Northern
Kimberley: Field survey methods and mapping protocols.
In: Mucina, L. & Daniel, G. (eds), Vegetation mapping in the
Northern Kimberley, Western Australia. pp. 26-87.
Curtin University, Perth, WA. ISBN 13: 978-0-646-90719-2,
ISBN 10:0646907190
Photographic credits:
All photographs in this book have been made by the members of the field
teams associated with the project Northern Kimberley Vegetation Mapping,
except those where authorship have been specified explicitly and the photo
on page 2 (upper) by F.G.T. Radlo, Stellenbosch, South Africa, fig. no. 2 on
page 7 and fig. no. 4 on page 27 (images from Digital Globe, google earth).
Glen Daniel
Glen Daniel is a Senior Fire Operations Ocer with the
Western Australian Department of Parks and Wildlife
(DPaW). His qualifications are in Environmental Science,
with an emphasis on land management. He has previously
worked in vegetation and wetland management.
His primary focus is currently the development of fire
planning instruments for Western Australia’s varied natural
and cultural environments. Other interests include studies
of fire behaviour and post fire recovery of natural systems.
Glen undertook his work on the Northern Kimberley
Vegetation Mapping Project as a two year secondment
to Curtin University.
Contact address:
Fire Management Services Branch
Department of Parks and Wildlife (DPaW)
Locked Bag 104
Bentley Delivery Centre 6983
Perth, Australia
W/Professor Ladislav Mucina
Laco Mucina is a Winthrop Professor of Vegetation
Science and Biogeography, Iluka Chair, at the School of
Plant Biology, The University of Western Australia, Perth,
Australia. He has worked in a number of universities on four
continents (Europe, Asia, Africa and Australia), published
more than 300 scientific papers (23 books), served as editor
of several international scientific journals, and supervised
more than 30 PhD and MSc student projects. His global
scientific interests span descriptive vegetation science
(especially vegetation surveys, classification and mapping),
biosystematics, molecular phylogeny, evolutionary
biology, biogeography, palaeoecology, biodiversity science,
environmental management, plant community restoration,
and conservation biology.
Contact address:
School of Plant Biology
The University of Western Australia
35 Stirling Highway
Crawley 6009
Perth, Australia
Email: Laco.Mucina@uwa.edu.au
26
Ladislav Mucina1, Glen Daniel2, Garth Stephenson3,
Ilze Boonzaaier3, Adriaan van Niekerk3, Matthew Barrett4,
Russell Barrett4, Lubomír Tichý5 and Milan Valachovič6
1 Department of Environment & Agriculture, Curtin University, GPO Box U1987,
Perth 6845, Australia; School of Plant Biology M084, The University of Western
Australia, 35 Stirling Highway, Crawley 6009, Australia;
Email: Laco.Mucina@uwa.edu.au
2 Fire Management Services Branch, Department of Parks and Wildlife (DPaW),
Perth, Locked Bag 104, Bentley Delivery Centre, WA 6983, Bentley, Australia.
3 Centre for Geographical Analysis, Department of Geography & Environmental
Studies, Stellenbosch University, Private Bag X1, Matieland 7602, Stellenbosch,
South Africa.
4 Botanic Gardens & Parks Authority, Kings Park & Botanic Garden, Fraser Avenue,
WA 6005, West Perth, Australia; School of Plant Biology, M084. The University of
Western Australia, WA 6009, Crawley, Perth, Australia.
5 Department of Botany & Zoology, Masaryk University, Kotlářská 2, CZ-61137
Brno, Czech Republic.
6 Department of Geobotany, Institute of Botany, Slovak Academy of Sciences,
Dúbravská cesta 9, SK-84523 Bratislava, Slovakia.
ABSTRACT
This chapter describes the procedures and outcomes of
the floristic-ecological mapping of the Mitchell Plateau and
Pantijan areas of the Northern Kimberley region, Western
Australia. A protocol is presented comprising a seven step
process of: setting mapping goals, collecting and collating
data, identifying the major ecological drivers of vegetation
patterns, setting classification and mapping rules, modelling
procedures, verification and presentation. The mapping
protocol provides a definitive approach to vegetation mapping
at intermediate scales (1:50,000 to 1:250,000) where the
availability of ground data is constrained by limited access to
the mapping area. This is the first time that formal vegetation
data-analytical tools have been used to classify the
vegetation of Western Australia’s savanna biome. The study
is also unique in linking the resultant vegetation classification
system to formal mapping modelling, to produce a map of
the potential natural vegetation of part of the State. The
field-survey, data analytical tools and methods of vegetation
26
Mucina, L., Daniel, G., Stephenson, G., Boonzaaier, I., van Niekerk, A., Barrett, M.,
Barrett, R., Tichý, L. & Valachovič, M. 2013. Floristic-Ecological Mapping in the
Northern Kimberley: Field Survey Methods and Mapping Protocols. In: Mucina, L.
& Daniel, G. (eds), Vegetation Mapping in the Northern Kimberley, Western Australia.
pp. 26-87. Curtin University, Perth, WA.
Chapter 2
Floristic-Ecological Mapping
in the Northern Kimberley:
Field Survey Methods and
Mapping Protocols
modelling proved very successful and both maps are useful
depictions of the patterning of vegetation at the targeted
scale. The validity of these maps is evident from both formal
verification and interpretation (the message conveyed by
the maps about ecological drivers and previous
flora-assembly processes).
INTRODUCTION
1.1 Motivation
Vegetation mapping utilises technical protocols and tools
to translate vegetation-ecological theory into a model
known as a ‘vegetation map’. This is a very complex process,
but there are some basic steps that may be followed to
construct an ecologically informative and scientifically
sound map. The first step is to gather the pertinent data
sets. These are then used to classify the vegetation, with the
aim of simplifying the vegetation complexity and defining
operational units called plant communities or vegetation
mapping units. The third step is to identify the major
ecological drivers, or environmental fabric, underpinning the
vegetation complexity. This allows the classification to be
linked to the environmental fabric. Finally the vegetation-
environment relationship is translated into a spatial model
or vegetation map.
The basic steps described above are common to all
vegetation-mapping protocols (see for instance Keith
2002, Brocklehurst et al. 2004, Sivertsen 2009 and
Neldner et al. 2012 for some representative examples from
Australia). Each dierent mapping area, however, will have
idiosyncratic features that must be considered. Examples
of such features are the availability of geographic data
sets, their quality and spatial resolution, accessibility of the
mapping area and taxonomic challenges.
The Northern Kimberley is a challenging region in which to
undertake vegetation mapping. It does, however, provide a
good opportunity to develop and test vegetation-mapping
strategies for areas where data availability is less than
optimal. With this goal in mind, two areas within the
Northern Kimberley were chosen as locations to construct
vegetation maps that will inform future biodiversity and
social benchmarking research. This was also used as an
opportunity to develop mapping protocols for future large-
scale floristic-ecological mapping of the remainder of the
Kimberley and the State of Western Australia.
1.2 Operational Targets
The broad goals described in the preceding paragraph were
refined to the following operational targets:
(1) Test the applicability of the basic vegetation-mapping
protocols under development (Mucina in prep.) for
WA and further develop them for areas with limited
accessibility and scarce ground data (sampling plots)
coverage;
(2) Formulate floristic-sociological vegetation
classification systems (based on floristic co-occurrence
data) for the Mitchell Plateau and Pantijan areas, using
contemporary field-survey procedures and numerical-
analytical tools;
(3) Construct ecologically informative vegetation maps of
the Mitchell Plateau and Pantijan areas, at a mapping
scale of 1:50,000, that inform biodiversity and social
benchmarking; and
(4) Draw lessons from this classification and mapping
exercise to facilitate Kimberley-wide and state-wide
vegetation mapping programmes.
1.3 Challenges
The Kimberley is situated in the northernmost part of
Western Australia. The region features extensive tracts
of wilderness, where human activity is limited and
infrastructure sparse. There are few roads and access is
further limited by the topographically highly articulated
landscape and extreme climatic conditions during the wet
cyclone season.
A vegetation survey in such a remote and poorly accessible
area faces a number of formidable challenges, such as:
• Highcostofeldsurveyworkduetothelargedistances
travelled, need for specialised 4WD vehicles, dependence
on significant logistical support and low quality of the
road network oen resulting in damage to vehicles.
• Highlevelofrisktoparticipantsduetohealthhazardsand
a lack of medical emergency infrastructure.
27
CHAPTER 2 FIELD SURVEY AND PROTOCOLS
28
APPROACH
The approach used in the current study follows the
vegetation-environmental paradigm. That is, it relies on
the high predictive value of the link between the current
vegetation patterns and the environmental matrix. It
designates the environmental matrix as the current
ecological driver of the biotic patterns at the regional,
landscape and habitat scales. This approach rests on seven
basic postulates of vegetation mapping as defined by
Mucina et al. (2006):
Postulate 1: Vegetation is a real, tangible object expressed
in the form of recognizable patches. In other words:
vegetation is a real phenomenon and can be studied.
Postulate 2: The dierences between the vegetation
patches in terms of structure, texture (floristic composition)
as well as in terms of environmental composition of the
habitats supporting the vegetation, make the classification
of vegetation (or conceptualisation of theoretical constructs
called ‘vegetation types’) possible. In other words: we can
classify vegetation patches into vegetation types.
Postulate 3: The great complexity of vegetation, both of a
discrete and continuous nature, makes the classification
of vegetation (or the reduction of information content to a
simplified system) necessary. In other words: classification
is one (and a very eective) way of simplifying the
complexity of vegetation.
Postulate 4: The levels of dierence between vegetation
types make building a hierarchical system (comprising
a series of nested vegetation types and their groups)
possible. The hierarchical system is another tool for further
simplification of vegetation complexity. In other words:
the hierarchical system is another eective way to view
important emergent properties of the major patterns of
vegetation.
Postulate 5: The structure and dynamics of vegetation is
a result of properties of its constituent plant populations
and their response to the nature and dynamics of the
environment which can aid classification and mapping
(‘vegetation-environment axiom’). In other words:
environmental conditions determine (together with the
properties of vegetation itself) the complexity of vegetation.
Postulate 6: Vegetation is composed of populations of
plant species (representing taxa). Each taxon oen shows
an individual response to ecological factors and hence
serves as an important ecological indicator. Major eorts to
devise an alternative classification of functional types have
yet to yield a viable system for widespread application. In
other words: we use floristic composition as the primary
entity for the conceptualisation of mapping units.
• Lowqualityofspatialdata,particularlythosethatare
based on field observations. For example, geological
mapping may be of poor quality and the precision of
bioclimatic modelling may be low due to the paucity of
climatic stations collecting baseline data.
• Qualityofecologicalandvegetationelddata
compromised due to a lack of suitable spatial data and
challenges imposed by climatic seasonality. For example,
field sampling is usually limited to the phenologically
suboptimal dry season.
• Impededprogressoftaxonomicknowledgeoftheora
and a lack of taxonomic expertise due to the diculty of
obtaining comparative floristic material.
• Restrictionsonaccesstosomeareasforculturalreasons.
In addition to the above, budgetary limitations and time
constraints are omnipresent challenges to any field
survey work.
Expectations defined by the Challenges
The challenges described above are likely to have a
deleterious eect on the process of developing a vegetation
map for a remote area. Vegetation mappers in such areas
should, therefore, enter into the process with the following
expectations:
(1) The costs of the field survey work will be high hence the
quantity and quality of data may be low. Alternative
ways of collecting ground data should be sought in
order to meet the minimum requirements.
(2) The volume of ground data will be small and the
spatial dispersion of the data points will be suboptimal
(spatially biased).
(3) Plant specimen identification will be dicult as many
of the specimens are likely to be collected out of their
optimal phenological phase. It may be necessary to
engage external contractors with particular expertise
in the local flora. Short-lived plants and grasses should
be excluded from sampling due to the high risk of
field sampling bias, especially amongst inadequately
trained or less experienced field sta. Such workers
may overlook species that are in poor phenological
condition. Collections of ephemeral taxa in poor
condition would also necessitate forensic identification
hence incurring disproportionate eort and cost.
(4) Qualitative ecological data will be used in the analyses
to a greater extent than would be the case in regions
where high-quality GIS and remote-sensed data are
available. This will not necessarily impede the analyses.
(5) Attention must be paid to the selection of a modelling
(mapping) approach that is suitable for sparse data
and low quality GIS coverage.
29CHAPTER 2 FIELD SURVEY AND PROTOCOLS
4) the repeatability of the mapping process, i.e. whether
it is a one-o mapping exercise or part of a monitoring
program; and
5) whether there are any constraints that might
prevent project goals from being achieved e.g.
access limitations, disturbance regimes or technical
constraints.
Decisions and Outcomes
1) The Mitchell Plateau mapping area was selected
because it is relatively accessible, has previously been
mapped, has high landscape and geological diversity,
and therefore presumably also has high biotic
variability, and is culturally important to Traditional
Owners. The Pantijan mapping area was selected
because it receives less rainfall than the Mitchell
Plateau, has high landscape and geological diversity,
and therefore presumably also high biotic variability,
and is culturally important to Traditional Owners.
2) Both maps have a floristic-ecological theme. They
depict major biodiversity (vegetation) patterns
that reflect the current ecological fabric and past
evolutionary history (biogeographic eects) of the
mapping area.
3) The acceptable mapping scale is between 1:50,000
and 1:250,000. The precision of most of the available
spatial data for these areas is within this range.
4) Neither map will serve a targeted monitoring
programme. As such, it is reasonable to incorporate
mapping tools that are not fully automated.
5) The following additional constraints were considered:
a. There is a strong influence of fire in the mapping
areas that aects the utility of some remotely-
sensed data sets, such as NDVI.
b. The mapping areas are characterised by strong
climatic seasonality that restricts the identification
of some elements of the flora and the use of some
remotely-sensed datasets.
c. There is very high grazing pressure on nutrient-
rich soils derived from igneous rocks. The grazing
pressure in environments characterised by low
nutrient availability, such as on sandstone and
laterite is low.
d. Access to the mapping areas is restricted by a lack
of roads and highly articulated topography. There
is particularly poor access to sandstone-dominated
landscapes.
e. Permission for access to the mapping areas was
granted by the relevant Traditional Owners; these
processes were facilitated by the Kimberley Land
Council.
Postulate 7: Vegetation patches occur in space hence
they can be mapped in spatial models. In other words:
complexity of vegetation can be shown on a map.
The concepts of zonality and azonality (Walter 1964,
1973) also underlie the approach to mapping adopted
in the current project. For details on these and related
concepts, consult Box 2.1.
The theme of this mapping exercise is colloquially known
as a floristic-ecological map. The reason for this is that
the map is based on the relationship between the present
plant species (flora) and the environment.
The maps produced during the current project feature
potential natural vegetation (see Tüxen 1956 for basic
concepts and Mucina 2010 for a recent review). This
reflects the use of the current flora/ecology relationship to
predict the distribution of vegetation patterns in areas not
sampled. Some of the units will, however, be delineated by
the mapping of actual patches. This applies especially to
azonal and relict vegetation such as Kimberley monsoonal
rainforests (see Chapters 3 and 4 for details).
VEGETATION SURVEY AND MAPPING PROTOCOL
Seven basic steps summarise the entire survey and
mapping exercise, from the definition of goals to the final
presentation. These steps may also be seen as the basis of
the state vegetation mapping protocols. The steps are:
Step 1: Primary decisions: setting goals and parameters.
Step 2: Collecting and collating mapping data sets.
Step 3: Identifying major drivers of vegetation patterns.
Step 4: Setting mapping rules and modelling.
Step 5: Making post-modelling adjustments.
Step 6: Verification.
Step 7: Presentation.
Each of these steps is explained in detail below.
3.1. Step 1: Primary Decisions: Setting Goals
and Basic Parameters
The first step in the mapping process is of utmost
importance. It aims to increase the specificity of the
client’s description of the desired product by identifying
the theme/topic, mapping scale, mapping frequency and
any constraints on the process. In particular, the following
must be decided:
1) the exact delimitation of the mapping area(s);
2) the theme or topic of the map, i.e. whether real
vegetation or modelled vegetation will be mapped;
3) the mapping scale, although this may be revised in
Step 2 as the quality of the available data sets may
influence the mapping targets;
30
seven bands per Landsat scene. The stacked images were
radiometrically corrected to reflectance using ATCOR2
(Richter 2004) in PCI Geomatica (www.pcigeomatics.
com/). This improved the compatibility between scenes.
ATCOR3, the version of ATCOR that includes topographical
corrections, was not used, since a digital elevation model
with suitable quality was not available for the study area.
The Landsat scenes were visually inspected to determine
their suitability for further analyses. Images showing
cloud cover or large recent fire scars were discarded.
The following images were selected for use in the
modelling process:
Panjitan: L5109071_20100331 (dated 31 March 2010).
Mitchell Plateau: L510970_20100603 (dated 3 June 2010).
The scenes were clipped to the extent of the pre-defined
Mitchell Plateau and Pantijan mapping areas.
Image Transformations
An image transformation is any operation that
re-expresses the information content of an image
for the purpose of deriving usable data not apparent
from the individual bands (Mather 2011). Two image
transformations were applied to the clipped Landsat
scenes, Principal Components Analysis (PCA) and the
Normalised Dierence Wetness Index (NDWI).
There is oen a high degree of correlation between the
individual bands of a multispectral image. PCA (for general
algorithms and explanation in ecological context see Orlóci
1978, Legendre & Legendre 1998) reduces the redundancy
of the data by identifying the optimal linear combinations
of the original channels and altering the dimensional
axes in such a manner that correlation is minimized. The
outcome of PCA is a series of coecients, or eigenvectors,
that align the principal axis along the strongest degree
of correlation in dimensional space. This concentrates
the maximum amount of information possible into one
band, called the first principal component (PC1). The
second largest axis, mutually perpendicular to (and hence
independent from) the first axis in dimensional space is
called the second principal component (PC2). This contains
the maximum amount of information from that which
remains aer the creation of PC1. This process is repeated
to form the same number of principal components as the
original number of bands (or otherwise specified), resulting
in a set of layers of decreasing variability (Liang 2004,
Campbell 2006, Mather 2011).
In the Kimberley mapping, a six-band PCA was undertaken
on bands 1–5 and 7 of the Landsat images. Band 6 is a
thermal band and was excluded from all analyses due to its
lower resolution.
3.2 Step 2: Collecting and Collating Mapping
Data Sets
The availability of spatial data has a major impact on
the quality of vegetation mapping. Published literature
and non-published scientific reports are both important
sources of data. Spatial data sets may also be derived
from a variety of sources, but should be carefully validated
before use.
Decisions and Outcomes
1) We obtained all accessible published and unpublished
(grey) literature that is pertinent to vegetation survey
and mapping in the Kimberley. The literature studies
reinforced our primary assessment that geology is
one of the major drivers of vegetation patterns in the
region. The best available geological mapping of the
Mitchell Plateau and Pantijan mapping areas is the
Australian 1:250,000 Geological Map Series. These
were available as a hard-copy map or as a scanned,
geo-referenced raster image. We digitised the relevant
map sheets (see also Chapter 1) to obtain a dataset
that could be manipulated with GIS. The Mitchell
Plateau mapping area coincided with the Montague
Sound and Drysdale-Londonderry geology map sheets
while the Pantijan mapping area incorporated the
Charnley and Prince Regent-Camden Sound map
sheets.
2) We obtained numerous spatial datasets as GIS layers
or rasters. A full list of these is provided in Appendix
1.1. The 35 low-resolution climatic variables derived
from the BioClim mean monthly climate estimates (for
details see Nix 1986) were of particular importance.
These were used in modelling the map units while the
19 basic WorldClim variables (Hijmans et al. 2005)
were used in the numerical (ordination) analyses.
Landsat Imagery Selection and Preprocessing
Landsat satellite imagery was recognised as a dataset
that is crucial to mapping in the Kimberley. This imagery
is freely available from the Earth Resources Observation
and Science Centre of the United States Geological Survey
(http://glovis.usgs.gov/). The Landsat scenes used in the
current project covered the period from 1999 to 2010;
these were derived from Landsat 5 and Landsat 7. Both of
these platforms possess very similar multispectral sensors
(Turner et al. 2003). Preference was given to the Landsat
5 imagery because the correction of a fault inherent in
the Landsat 7 imagery aects the quality of the images
supplied by that platform.
The Landsat imagery was supplied in a Standard Terrain
Correction Level 1T format that included systematic
radiometric and geometric corrections. A separate image
for each sensor spectral band was supplied. These band
images were then stacked, resulting in one image with
31CHAPTER 2 FIELD SURVEY AND PROTOCOLS
devised for the areas by Beard (1978, 1979, 1988) and
Hnatiuk & Kenneally (1981). The methods used to produce
the Mitchell Plateau map are summarised in Box 2.2.
A similar approach was adopted to produce the preliminary
vegetation map of the Pantijan area.
The vegetation classification system of Hnatiuk &
Kenneally (1981) recognises 26 habitat/vegetation types.
The classification and mapping by Beard (1978, 1979) is
simpler in both of the mapping areas as it clearly reflects
the driving influence of geology. The later Beard map
(1988) of the Mitchell Plateau also reflects the importance
of geology as a driver of vegetation patterns.
The preliminary map of the Mitchell Plateau was used to
identify suitable locations to situate sample plots during
the survey. This selection was designed to incorporate
the full range of vegetation variability depicted on the
preliminary map while allowing for considerations
of access. We refrained from pre-selecting sampling
locations in the Pantijan mapping area because of a lack of
information about the nature of that area.
Validating Previous Maps
The two classification systems previously developed for
the mapping areas (Beard 1978, 1979, 1988, Hnatiuk &
Kenneally 1981) were tested in the field to determine if
they adequately represented the vegetation. We assigned
vegetation patches studied in the field to communities
using the characteristics of the plant communities
described in the source publications. The results of this
process were compared to the findings of an expert
classification undertaken in the field. In some cases,
these comparisons assisted in selection of sampling plots
(see below for more detail). We have established that the
vegetation classification system of Hnatiuk & Kenneally
(1981) for the Mitchell Plateau was very logical.
Establishing Survey Plots
It was necessary to modify the pre-selected set of plots
in the Mitchell Plateau mapping area (Fig. 2.1). When the
pre-selection process was undertaken, it was thought that
a helicopter would be used to access some of the more
remote sampling locations. However, since an aircra was
not available at the time of the survey, such sites could
not be reached. This particularly aected sampling of the
dissected sandstone landscapes where the nature of the
terrain makes overland travel very dicult. As a result
of this constraint, plot sampling was limited to areas in
the proximity of roads. The extent of the road network in
the Mitchell Plateau mapping area allowed a reasonably
representative set of sampling plots to be established. The
vegetation of the lateritic plateau and associated low-lying
basalt landscapes was sampled more intensively, however,
than that of the sandstone landscapes (Fig. 2.3).
Spectral indices were not used in mapping as it was
thought that the individual spectral bands and six principal
components would encompass all of the spectral variation
within the Landsat images. The only exception was an
attempt to use the Normalized Dierence Wetness Index
(NDWI) to create a dataset informative of the distribution
of water in the landscape. It was hoped this would assist
with the identification of azonal riparian vegetation. The
NDWI was therefore calculated for both areas according to
the following formula by Gao (1996): NDWI = [(Band 4) -
(Band 5)] / [(Band 4) + (Band 5)].
3.3 Step 3: Identifying Major Drivers of
Vegetation Patterns
A vegetation map is a model of vegetation that expresses a
theory about the pattern of vegetation and the logic of its
distribution in space and time. A scientifically plausible and
informative map relies on the mapper’s ability to recognise
the processes that play a role in shaping the vegetation.
These may be acting in the present at an ecological scale or
may be an historical artefact considered at an evolutionary
scale. Identifying the drivers of vegetation patterning is
crucial to modelling the vegetation patterns themselves.
In the preliminary steps of the Kimberley mapping project
we learnt about the drivers of vegetation patterns from the
observations of previous workers in the area. In particular,
the work of Beard (1978, 1979, 1988) and Hnatiuk &
Kenneally (1981) provided valuable information about the
processes that shape the vegetation of the Mitchell Plateau
and Pantijan areas. We supplemented this information,
however, by collecting field data from the mapping areas.
We analysed these data sets and drew conclusions about
the role of environmental factors that might have driven
the current as well as relict vegetation patterns observed in
the mapping areas.
3.3.1. Field Sampling
Two vegetation surveys were conducted during the
Kimberley mapping project. The Mitchell Plateau mapping
area was sampled between 20 July 2011 and 26 July 2011
and the Pantijan mapping area was sampled between 1
August 2011 and 6 August 2011. These surveys collected
vegetation-plot material for modelling and identified the
major ecological drivers of vegetation patterns in the
Mitchell Plateau and Pantijan areas. The Mitchell Plateau
survey also tested the validity of the previous vegetation
classification systems applied to that area (Beard 1979,
1988, Hnatiuk & Kenneally 1981).
Survey Preparation
The first task in preparing for the survey campaign was
to prepare preliminary vegetation maps for the Mitchell
Plateau (Fig. 2.1) and the Pantijan area (Fig. 2.2). These
were based on the vegetation classification systems
32
FIG. 2.3
Survey sites
showing the
actual positions
of plots sampled
in the Mitchell
Plateau
mapping
area in 2011.
Validation sites,
represented by
yellow circles,
indicate the
position of
independent
verification
points collected
during the 2012
field campaign.
FIG. 2.4
Survey sites
showing the
actual positions
of the plots
sampled in the
newly delimited
Pantijan mapping
area in 2011.
33CHAPTER 2 FIELD SURVEY AND PROTOCOLS
3) The classification of tree and shrub savanna plant
communities using only the tree component has
been shown to be highly informative (Nežerková-
Hejcmanová et al. 2005 and ample literature cited
therein). Arndt & Norman (1959) also found little
interdependence between tree and ground flora.
On the basis of the information given above, we concluded
that the woody component carried sucient ecological
information to allow an eective classification of the
vegetation. Indeed, as the herbaceous layer is prone
to bias, woody vegetation is the preferred source of
classification variables.
3.3.2 Collation of the Field Data
Plant Identifications
The survey team included few individuals with sucient
taxonomic-floristic knowledge to undertake accurate field
identification of specimens. As such, almost all woody
plant species were collected, marked and preserved by
pressing. Very few plants were identified with confidence
in the field and hence not collected. Where appropriate,
photographs were also taken of the plant from which a
specimen was collected. Information about the habit, bark,
leaves, fruit and flowers was thus recorded and proved very
useful during the identification process.
Most of the collected plant material was identified using
the facilities of the State Herbarium (PERTH) located at
the Western Australian Biodiversity Conservation Centre
(DPaW), Kensington. The identifications were aided by:
• Flora of the Kimberley Region (Wheeler 1992);
• Field Guide to Eucalyptus (Brooker & Kleinig 1994);
• EUCLID (Centre for Plant Biodiversity Research 2006) was
used for Eucalyptus;
• WATTLE (Maslin 2001) was used for Acacia;
• Plants of the Kimberley Rangelands by Petheram et al. (2003);
• WAorachecklistbyPaczkowska&Chapman(2000);
• FloraBaseidenticationtools(www.orabase.dec.wa.gov.au;
and
• thelatestrevisionsofsomegeneraencounteredinthe
collected material.
Despite the sub-optimal phenological states and poor
condition of many of the specimens, more than 90% were
identified unequivocally to species (and in many cases
subspecies) level.
Collation of the Environmental and Geographical Data
There was some inconsistency in the way that
environmental and geographical data were collected
during sampling. This resulted from the large number of
participants in the survey and the limited opportunity
to provide training in survey techniques. The lack of
completeness and consistency in the environmental and
geographical datasets limited their usefulness as a source
of data for modelling. In particular:
1) The variables describing the topographic position
and landform (see Tables 3 and 4 in Appendix 2.1
The sandstone vegetation in the Pantijan mapping area
was sampled more intensively than in the Mitchell Plateau
area. This was possible because the access route, the
Munja Track, passed through extensive areas of sandstone.
Overall, however, the track network in the Pantijan mapping
area was very limited and a lack of access constrained the
placement of sampling plots. In fact, a significant proportion
of the sampling plots in the Pantijan area were placed
outside the originally defined mapping area (Fig. 2.4). This
should not be seen as detrimental to the mapping exercise,
however, as the strong link between major vegetation
patterns and geology in the Kimberley (Gardner 1942, Miles
& Burbridge 1975, Kabay & Burbridge 1977, George 1978,
Beard 1978, 1979, Fox et al. 2001, Kenneally et al. 2008)
allows extrapolation (modelling) over large distances.
Field Sampling Protocols were designed prior to the
commencement of the survey campaign. These are
presented in Appendix 2.1, along with justification of the
survey design. Sampling commenced much later than
expected, however, aer unusually high rainfall in the
2010/2011 wet season caused extensive damage to the
road network. This prevented access to the mapping areas
until late in the dry season and meant that herbs and
grasses were in very poor condition at the time of sampling.
It was necessary, therefore, to alter the protocols to allow
for the prevailing conditions.
Sampling was limited to woody vegetation (trees, shrubs,
lianas) and perennial herbs. We recorded the total cover
(in %) of the tussock (e.g. Themeda, Heteropogon,
Cymbopogon etc.) and hemisphaeric grasses (Triodia) as
separate variables. Grasses and short-lived herbs were
excluded from sampling for the following reasons:
1) Part of the grassy component of the vegetation is
short-lived and can only be found while in an optimal
phenological state (flowering and seeding) during, and
shortly aer, the wet season. At the time of sampling,
these grasses had deteriorated significantly and were
found in the post-reproductive stage of development.
The progressed phenology made field identification
extremely dicult and would have impeded the
laboratory identification of plant material.
2) The grassy understorey in savanna vegetation is highly
dynamic and is characterised by rapidly changing
dominance relationships in response to fire and
precipitation. Hüttich (2011) and Hüttich et al. (2011)
showed that woody vegetation in savannas provides
more stable variables for use in vegetation modelling/
mapping than herbaceous vegetation. Also, that woody
vegetation is less likely to present errors of omission
and commission compared with herbaceous vegetation.
Woody vegetation is essentially less sensitive to inter-
annual variability than herbaceous life forms (Archibald
& Scholes 2007).
34
FIG. 2.5
Example of the OptimClass analyses for vegetation classifications of the Mitchell Plateau plot data (for 3-layer data
matrix only) using various combinations of the Unweighted Pair Group Method Using Arithmetic Averages. X axis
denotes the number of cluster solutions tested and the Y axis represents the OptimClass value.
FIG. 2.6
Example of the OptimClass analyses for the vegetation classifications of the Pantijan plot data (for 3-layer data matrix
only) using various combinations of the Unweighted Pair-Group Method Using Arithmetic Averages. The X axis denotes
the number of cluster solutions tested and the Y axis represents the OptimClass value.
35CHAPTER 2 FIELD SURVEY AND PROTOCOLS
FIG. 2.7
A dendrogram of the UPGMA based on Similarity Ratio (= quantitative form of Jaccard’s Similarity Index)
and logarithmic transformation of the percentage data of the Mitchell Plateau sample plots. Capital letters
code the plant community as recognised in the final classification system for the region (see Table 2.4).
FIG. 2.8
A dendrogram of the UPGMA based on Similarity Ratio (= quantitative form of Jaccard’s Similarity Index) and
logarithmic transformation of the percentage data of the Pantijan sample plots. Capital letters code the plant
community as recognised in the final classification system for the region (see Table 2.6). The plots engulfed in a red
rectangle are representatives of Community J that were misclassified as Community C (see text for more detail).
36
data set. The diagnostic value of each species can be
ascertained using various statistical criteria; Fisher’s exact
test is used in OptimClass (see Tichý & Chytrý 2006).
If a classification produces well-defined, interpretable
clusters, then these clusters should have a high number of
diagnostic species.
We performed an OptimClass search on a selection of
the most widely-used techniques in community ecology,
including Unweighted Pair-Group Method using Arithmetic
Averages (UPGMA), Beta Flexible Clustering, Ward’s Method
in combination with a Bray-Curtis Index, Similarity Ratio,
Chord Distance and none or logarithmic and/or power
transformation. The cluster analyses used to calculate the
OptimClass were performed using the soware package
PC-ORD 5.20 (McCune & Meord 2011). The full list of the
tested combinations is shown in Table 2.2.
We tested all three data matrix options (all layers, 3-layers,
1-layer) on the Mitchell Plateau and Pantijan vegetation
data matrices. Examples of selected OptimClass analyses
are presented in Figs 2.5 and 2.6. The information provided
by OptimClass influenced us to treat our data as follows:
1) We selected the 3-layer data matrix for the
classification. The inclusion of more detailed vertical
layering, such as two to three sub-layers in the
tree layer and two sub-layers in the shrub layer
(see Appendix 2.1), is valuable in the description of
vegetation structure. It may, however, introduce ‘noise’
to the analysis by introducing variables with little
ecological information value. This may result in an
overzealous fragmentation of the floristic information.
Flattening the data by collapsing all structural layers
into one, however, provides information only on species
(not species per layer) presence and abundance.
Valuable, ecologically relevant information about
vegetation structure may be lost. The use of a three
layer data matrix is a suitable compromise between
these extremes.
2) We performed a log-transformation on the data
prior to clustering. This was necessary because the
vegetation projected cover measurements collected
in the field were highly biased towards low cover
values. In most plots, more than ½ of the species were
scored as 1% cover. On the other hand, in most of
our sampled plots there were one or two pronounced
dominants (scoring high cover percentage estimates).
The log-transformation balances the % (scale 0–100)
data by recalculating them into smaller span, hence
underweighting the dominants slightly and giving
more weight to the low-score species. The use of the
log-transformation is hence useful when there is high
variation among attributes (estimated cover values of
the recorded species) within the sampled data set (see
for example McCune et al. 2002, McCune & Meord
2011 for more details).
for definitions) were not used in the analyses. Field
descriptions of these variables appeared biased
toward particular categories, suggesting survey team
members had diculty categorising them in the field.
2) It was necessary to supplement the field-collected
descriptions of geology prior to analyses. We used
a simplified system of rock types (see Table 5 in
Appendix 2.1), with surveyors designating the
sampling site as being on sandstone, laterite, basalt
or dolerite. It was apparent from an examination of the
field datasheets, however, that this information was
only recorded accurately where outcrop was visible
at the sampling location. There was considerable
ambiguity in situations where deep soils covered the
parent rock. In order to correct this, the description of
geology collected in field was cross-referenced against
the descriptions of habitat and soil texture, geological
maps and satellite imagery and amended where
required. Since vegetation on dolerite not sampled
during the 2011 field trip, one plot from dolerite was
sampled during the 2012 verification exercise and was
added to the modelling data set (see below).
Preparation of the Final Data Matrices
The vegetation data from each plot were entered into an
MS Excel spreadsheet and all taxonomy was checked for
currency. A MS Excel macro (developed by W/Prof. Phil
Withers, UWA, Perth) was then used to combine the plot
vegetation data into a single comprehensive vegetation
data matrix. The environmental and geographical data were
also entered in an MS Excel spreadsheet and the variables to
be used in numerical analyses (see below) were coded (for
details of the variable and the coding see Table 2.1).
The collated and corrected versions of the original plot
data are provided as Electronic Appendices on the CD
accompanying this report. The relevant files are Kimberley
Vegetation Plot Data and Kimberley Header Data. The
vegetation data matrices used in the classification are also
provided on the accompanying CD. The relevant files are
VegClassMitchell and VegClassPantijan.
3.3.3 Classification of the Field Plot Data
OptimClass: Search for the Optimal Classification Tools
There are many classification analytic options available
that represent dierent combinations of clustering
techniques, resemblance, and data transformation (see for
instance Legendre & Legendre 1998, Podani 2000, 2001,
McCune et al. 2002). We undertook an OptimClass analysis
to determine the most suitable approach to classification
based on the available data. OptimClass (Tichý et al. 2010)
is a test of the classification quality using the total count
of diagnostic species as the major criterion. Diagnostic
species can be defined as a species that would characterise
a cluster (community or group of communities) in the
37CHAPTER 2 FIELD SURVEY AND PROTOCOLS
4) The choice of Similarity Ratio (quantitative form of the
well-known Jaccard’s Similarity Index; see for instance
Tamás et al. 2001) was motivated by its simplicity
and emphasis on species co-occurrence patterns.
Wishart’s similarity ratio has been widely used in/for
resemblance in numerical syntaxonomy (see Mucina
& van der Maarel 1989) and remains currently useful
since it has produced very informative (i.e. having
high interpretative value) results in combination
with common cluster techniques, particularly those
preserving the resemblance space (Hajdu 1981,
Hubálek 1982). Also, the OptimClass analyses
suggested such combinations to be highly informative.
Clustering, Definition of Clusters and Tabular Sorting
The log-transformed three-layer vegetation data matrices
for the Mitchell Plateau and Pantijan mapping areas were
clustered with UPGMA using the Similarity Ratio as the
resemblance. The final clustering analyses were run in
the SYNTAX 2000 package (Podani 2001) because of the
favourable quality of the graphical outputs in this program.
The dendrograms showing the results of the clustering
analyses are shown in Figs 2.7 and 2.8.
3) We selected UPGMA as the clustering tool. The analysis
of the OptimClass results revealed that UPGMA, Beta
Flexible Clustering (beta: -0.25) and Ward’s Method
were nearly equally powerful in revealing classification
structure in the analysed data sets. We chose UPGMA
because of its simple philosophy and wide use but
this choice was also governed by consideration
of the nature of the resemblance space distortion
imposed by some techniques. As succinctly captured
by the classic textbook by Sneath & Sokal (1973, p.
214–245), the dimensions of the resemblance space
become distorted as new resemblances are computed
between the growing clusters during the agglomeration
(amalgamation) process. Some of the clustering
techniques preserve the original resemblance space,
while other techniques either dilate or contract the
space (Lance & Williams 1967). In order to preserve the
original resemblances, we chose UPGMA because this
technique is known for its space-preservation property.
TABLE 2.1
List of environmental variables used in the CCA analyses as well as CART modelling.
Name Code Scale States Unit Source Note
Geology Geol Nominal/categorical San (sandstone)
Lat (laterite)
Bas (basalt)
Dol (dolerite)
1/0
1/0
1/0
1/0
field data
field data
field data
field data only in Pantijan data set
Altitude Alt Ratio n/a meter GPS device
Slope Slope Ratio n/a degree field estimates
Aspect Asp Ratio/Circular n/a degree compas measurement
Disturbance Dist Nominal/categorical No-Dist
Graz
Fire
1/0
1/0
1/0
no obvious disturbance
grazing disturbance
light fire disturbance
Annual Mean Temperature BC01 Ratio n/a ° C BioClim (modelled)
Mean Diurnal Range BC02 Ratio n/a ° C BioClim (modelled) mean of monthly (max temp - min temp)
Isothermality BC03 Ratio n/a %BioClim (modelled) (BIO 2/BIO7) *100
Temperature Seasonality BC04 Ratio n/a BioClim (modelled) (standard deviation * 100)
Max Temperature of Warmest Month BC05 Ratio n/a ° C BioClim (modelled)
Min Temperature of Warmest Month BC06 Ratio n/a ° C BioClim (modelled)
Temperature Annual Range BC07 Ratio n/a ° C BioClim (modelled) BIO5 - BIO6
Mean Temperature of Wettest Quarter BC08 Ratio n/a ° C BioClim (modelled)
Mean Temperature of Driest Quarter BC09 Ratio n/a ° C BioClim (modelled)
Mean Temperature of Warmest Quarter BC10 Ratio n/a ° C BioClim (modelled)
Mean Temperature of Coldest Quarter BC11 Ratio n/a ° C BioClim (modelled)
Annual Precipitation BC12 Ratio n/a mm BioClim (modelled)
Precipitation of Wettest Month BC13 Ratio n/a mm BioClim (modelled)
Precipitation of Driest Month BC14 Ratio n/a mm BioClim (modelled)
Precipitation Seasonality BC15 Ratio n/a mm BioClim (modelled) coecient of variation (CV)
Precipitation of Wettest Quarter BC16 Ratio n/a mm BioClim (modelled)
Precipitation of Driest Quarter BC17 Ratio n/a mm BioClim (modelled)
Precipitation of Warmest Quarter BC18 Ratio n/a mm BioClim (modelled)
Precipitation of Coldest Quarter BC19 Ratio n/a mm BioClim (modelled)
38
TABLE 2.2
List of OptimClass options.
Clustering Resemblance Transformation
Average linkage (UPGMA) Bray-Curtis none
Average linkage (UPGMA) Bray-Curtis log (2)
Average linkage (UPGMA) Bray-Curtis power 0.333
Average linkage (UPGMA) Bray-Curtis power 0
Average linkage (UPGMA) Jaccard none
Average linkage (UPGMA) Jaccard log (2)
Average linkage (UPGMA) Jaccard power 0.333
Average linkage (UPGMA) Jaccard power 0
Beta flexible (β= -0.25) Bray-Curtis none
Beta flexible (β= -0.25) Bray-Curtis log (2)
Beta flexible (β= -0.25) Bray-Curtis power 0.333
Beta flexible (β= -0.25) Bray-Curtis power 0
Beta flexible (β= -0.25) Jaccard none
Beta flexible (β= -0.25) Jaccard log (2)
Beta flexible (β= -0.25) Jaccard power 0.333
Beta flexible (β= -0.25) Jaccard power 0
Beta flexible (β= -0.1) Bray-Curtis none
Beta flexible (β= -0.1) Bray-Curtis log (2)
Beta flexible (β= -0.1) Bray-Curtis power 0.333
Beta flexible (β= -0.1) Bray-Curtis power 0
Beta flexible (β= -0.1) Jaccard none
Beta flexible (β= -0.1) Jaccard log (2)
Beta flexible (β= -0.1) Jaccard power 0.333
Beta flexible (β= -0.1) Jaccard power 0
Beta flexible (β= -0.4) Bray-Curtis none
Beta flexible (β= -0.4) Bray-Curtis log (2)
Beta flexible (β= -0.4) Bray-Curtis power 0.333
Beta flexible (β= -0.4) Bray-Curtis power 0
Beta flexible (β= -0.4) Jaccard none
Beta flexible (β= -0.4) Jaccard log (2)
Beta flexible (β= -0.4) Jaccard power 0.333
Beta flexible (β= -0.4) Jaccard power 0
Ward's method (= ISS) Chord (= normalised ED) none
Ward's method (= ISS) Chord (= normalised ED) log (2)
Ward's method (= ISS) Chord (= normalised ED) power 0.333
Ward's method (= ISS) Chord (= normalised ED) power 0
Ward's method (= ISS) Euclid none
Ward's method (= ISS) Euclid log (2)
Ward's method (= ISS) Euclid power 0.333
Ward's method (= ISS) Euclid power 0
Furthest neighbour (CLC) Bray-Curtis none
Furthest neighbour (CLC) Bray-Curtis log (2)
Furthest neighbour (CLC) Bray-Curtis power 0.333
Furthest neighbour (CLC) Bray-Curtis power 0
Furthest neighbour (CLC) Jaccard none
Furthest neighbour (CLC) Jaccard log (2)
Furthest neighbour (CLC) Jaccard power 0.333
Furthest neighbour (CLC) Jaccard power 0
39CHAPTER 2 FIELD SURVEY AND PROTOCOLS
to be straightforward except for the classification of Plots
A108, A115 and B151. These were all sampled on basalt
and are indicated by the red square in the dendrogram (Fig.
2.5). The clustering process classified these three plots as
Community C (Terminalia canescens Comm.), despite the
occurrence of basalt indicators such as Eucalyptus tectifica,
Corymbia greeniana, C. disjuncta, Hakea arborescens and
Grevillea mimosoides. This anomaly may be ascribed to
the dominance of Terminalia canescens in the three plots,
one of a few tree species showing apparent indierence to
substrate. The three anomalous plots were reclassified as
Community J (Eucalyptus tectifica−Corymbia greeniana
Comm.). The final non-hierarchical classification vegetation
system of the Pantijan data is presented in Table 2.6.
3.3.4 Ordination of the Field Plot Data
Data Collation and Analytical Parameters
The Mitchell Plateau and Pantijan plot data were subjected
to separate ordination analyses with the aim of revealing
and quantifying the major ecological drivers of vegetation
patterns. We used Canonical Correlation Analysis (CCA:
ter Braak 1986) and the soware package CANOCO 4.5
(ter Braak & Šmilauer 2002) to achieve this. The choice
of CCA as the ordination model was motivated by a high
probability that species would show a unimodal rather than
a linear response along putative environmental gradients.
We used a simple CCA analysis with no transformation of
the percentage cover data prior to analysis, with scaling
focused on interspecies distances, biplot scaling applied
and no forward selection of environmental variables. Visual
representations of the ordination results were prepared
using the CanoDraw option of the CANOCO 4.5 soware
package. These show ordination planes of Axes 1 and 2.
The CCA analysis uses two data matrices. The first matrix
is the vegetation data matrix featuring the occurrence
patterns of species in plots with percentage cover estimates
used as the original input values. The second matrix is
the environmental data matrix. This contains selected
environmental variables (scored in all studied plots)
expected to control the vegetation patterning. Both matrices
have the same number of plots, although the number of
variables (species variables and environmental variables)
may dier.
The CCA analysis of the Mitchell Plateau data set involved
355 species variables shared between 67 plots. The CCA
analysis of the Pantijan data set involved 300 species
variables shared by another set of 67 plots. A species
variable represents a taxon recorded in a particular vertical
vegetation layer; this implies that each taxon can occur in
the matrix up to three times if it occurs in each of the three
predefined vertical vegetation layers considered (E3, E2, E1;
see Appendix 2.1 or Mucina et al. 2000 for the definition of
this layering system).
Aer clustering, the data were ordered. The procedure below
describes the ordering of the data matrix of the Mitchell
Plateau. An analogous procedure was applied to achieve the
ordering of the Pantijan matrix.
1) The plots of the original data matrix were ordered using
the new order of plots as suggested by the dendrogram
(Fig. 2.7) from le to right.
2) The ordered table was sequentially subdivided from the
top down using the amalgamation pattern depicted by
the dendrogram. The four outlying clusters (O1–O4)
were recognised first, followed by clusters A and B (Fig.
2.7). The A and B clusters were subdivided into A1, A2,
B1 and B2.
3) The species limited to particular clusters were identified,
along with species groups shared by combinations of
clusters.
4) A preliminary interpretation of the clusters was
undertaken to assess the plausibility of the ecological
message conveyed by the recognised cluster versus
species group combinations.
5) The clusters A1, A2, B1 and B2 were further sequentially
subdivided by recognising the major gaps between
the sub-clusters. Steps 3 and 4 were repeated on the
subdivided clusters.
6) The process of subdividing clusters and repeating steps
3 and 4 continued until we reached the approximate
optimum number of clusters as suggested by the
UPGMA/SR/log algorithm. The resultant clusters were
recognised as ecologically interpretable and floristically
well defined, each having their own diagnostic species
group.
Definition of the Final Vegetation Classification System for
the Mitchell Plateau
OptimClass identified 22 clusters as the optimal solution
when applying the UPGMA/SR/log algorithm to the Mitchell
Plateau data. We iteratively applied the six-step sorting
algorithm described above to order the Mitchell Plateau
vegetation table and achieve this optimal result (Table
2.3). Plot A28 had been misclassified in the resultant
dendrogram as it had very low similarity to its allocated
Cluster (C+D) and should have been placed in Cluster E.
This misclassification was ascribed to the influence of
Terminalia canescens in plot A28. This is a dominant species
of Clusters C and D and appeared dominant in plot A28 only
because the plot was extremely species-poor. The final non-
hierarchical classification vegetation system of the Mitchell
Plateau data is shown in Table 2.4.
Definition of the Final Vegetation Classification System
for Pantijan
We used the same analytical classification combination
(UPGMA/SR/log) and six-step algorithm to structure the
Pantijan vegetation table as used for the Mitchell Plateau
data (Table 2.5). The definition of communities appeared
40
TABLE 2.3
Phytosociological data of the Mitchell Plateau that served as the basis of the
vegetation classification system for the region (see Table 2.4 on page 44).
Running number LH12345678910 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29
Field Code
A01
B69
A72
E63
A74
B50
A77
A73
B14
B61
E45
E08
B70
B71
A20
B99
A32
B60
A76
E44
B67
B13
B57
E19
B16
A28
A52
E58
B36
Community A A A A A A A A B B B B B B C C C C D D D D D D D E E E E
Corymbia nesophila E3 10 30 520 15 40 ...........2....5......
Corymbia nesophila E2 .1.10 3..1.........2...........
Corymbia nesophila E1 .1.10 .2.......................
Livistona eastonii E3 52515 1 . 10 5 . . 10 15 .............2.5.
Livistona eastonii E2 10 5 2 10 1.310 5 5 20 1.....2.....1.110 5 1
Livistona eastonii E1 2 . 1 3 3 . 5 1 . 1 1 1 . . . . . . . . . 1 . 1 . . . . 1
Gossypium rotundifolium E2 H......1......................
Gossypium rotundifolium E1 H1.1.....11...................
Merremia quinata E1 H......1..1..1................
Eucalyptus miniata E3 . . . 5 . . 1 . . 30 40 30 10 25 5 2 1 . . ...35.....
Eucalyptus miniata E2 . . . 3 . . . . 5 5 . 10 10 111.1...........
Eucalyptus miniata E1 5....23..1.2..1..........1...
Acacia oligoneura E2 ........1.1..................
Acacia oligoneura E1 ...........................2.
Eucalyptus tetrodonta E3 20 510 5 . . . . . 5 5 3 . . 20 20 10 325 30 510 530 25 5 5 . .
Eucalyptus tetrodonta E2 . . 1 10 . . . . 2 1 2 2 . . . 5 . 1 . 20 5 4 5 . 10 ....
Eucalyptus tetrodonta E1 . . . 3 . . . . 1 1 1 . . . . . 1 2 . 3 1 . 1 . . . . . .
Petalostigma pubescens E2 ....12........3.1....523.....
Petalostigma pubescens E1 .1..............1....1.......
Tricoryne sp. Kimberley (K.F.
Kenneally 4857) E1 H..1.1...........1............
Hibbertia hooglandii E1 1.............20 50 10 25 .1....1....
Bossiaea bossiaeoides E2 ..............510 2............
Bossiaea bossiaeoides E1 ...............21............
Acacia areolata E2 ..............2.5.1..........
Acacia areolata E1 ................1............
Stenocarpus acacioides E2 ...............11............
Stenocarpus acacioides E1 ................2............
Bossiaea sp. West Kimberley
(R.L. Barrett & M.D. Barrett RLB
4045)
E2 ..................15 20 1........
Bossiaea sp. West Kimberley
(R.L. Barrett & M.D. Barrett RLB
4045)
E1 ..................1..........
Corymbia latifolia E3 .........................320 20 5
Corymbia latifolia E2 ..................1.2.......1
Corymbia latifolia E1 .....1....................111
Eucalyptus apodophylla E3 .............................
Eucalyptus alba var.
australasica E3 .............................
Eucalyptus alba var.
australasica E1 .............................
Eriocaulon tortuosum E1 H . . . . .........................
Melaleuca leucadendra E1 .............................
Melaleuca nervosa subsp.
nervosa E2 .............................
Melaleuca nervosa subsp.
nervosa E1 .............................
Acacia retinervis E2 ...............4...12........
Acacia retinervis E1 .............................
Gonocarpus leptothecus E1 ...............1...1.........
Terminalia carpentariae E3 .............................
Terminalia carpentariae E2 .............................
Acacia gonocarpa E2 .............................
Corymbia torta E3 .............................
Corymbia torta E2 .............................
Corymbia torta E1 .............................
Acacia sp. Kununurra (Lullfitz
6195) E2 .............................
Acacia delibrata E3 .............................
Acacia delibrata E2 .............................
Tephrosia rosea E2 .............................
Tephrosia rosea E1 .............................
41CHAPTER 2 FIELD SURVEY AND PROTOCOLS
Each column in the main body of the table represents a relevé (plot) and has the field code of the plot at the point of sampling.
The codes in Column L indicate the vertical layers (E3: tree layer, E2: shrub layer, E1: ground layer). The code “H” in Column H indicates
which of the taxa are herbs (all others are either trees, shrubs, saplings or woody seedlings). The species/taxa (per layer) are grouped
in such a manner as to delimit a community or groups of communities. Only diagnostic species are shown (the species with low or
no diagnostic value were omitted). Codes for the Communities match those in Table 2.4. The colour coding of the background of the
Community Codes matches the colour coding of major mapping units in the maps (Green: Sandy Woodlands; Yellow: Clayey Woodlands;
Grey: Sandy Shrublands). See the text for detail of table sorting.
30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 58 59 60 61 62 63 64 65 66 67
E27
A02
Z11
A56
A55
B86
B97
B33
A62
E41
B18
E12
A06
E47
E07
E40
A79
A04
A54
A30
A22
B35
B31
A03
B15
B30
E42
A29
B17
E06
A05
A75
B65
B68
E10
B64
E43
B66
E F F G H H H H I I J J K L M M M N O O O O O P P P P R R R S T T T U V V V
......................................
......................................
..............1.......................
.5..........1..........31.............
. . 1 . . . . . . . 1 5 . . 2 5 . 20 .1....1.............
.1.........1..21.......1....11........
......................................
.................1....................
.......................1..............
......................................
......................................
......................................
......................................
......................................
......1...............................
......3........10 ......................
........1.............................
......221.............................
......1...............................
......................................
......1...............................
......................................
......1...............................
......................................
......................................
......................................
......................................
..............................70 .......
..............................1.......
20 5....................................
5....1................................
15 ....1................................
.10 20 ...................................
..5...................................
..1...................................
. . 10 ...................................
..1...................................
.1....................................
.31...................................
2 . . . 10 875......................1.......
....111...............................
....111...............................
....10 .................................
....1..1...1..........................
........10 1.........................1..
......3.510 ..................7.........
......1..10 ............................
.......2.1..................1.........
.........5............................
.........5...... ......................
.......1.1............................
........21............................
........1.............................
42
TABLE 2.3 Continued
Running number LH12345678910 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29
Field Code
A01
B69
A72
E63
A74
B50
A77
A73
B14
B61
E45
E08
B70
B71
A20
B99
A32
B60
A76
E44
B67
B13
B57
E19
B16
A28
A52
E58
B36
Community A A A A A A A A B B B B B B C C C C D D D D D D D E E E E
Pandanus spiralis E2 .............................
Pandanus spiralis E1 .............................
Antidesma ghaesembilla E2 .......1...............1.....
Antidesma ghaesembilla E1 .............................
Corymbia bella E2 .............................
Acacia stigmatophylla E2 .............................
Xanthostemon eucalyptoides E3 . ............................
Corymbia bella E3 .............5...............
Melaleuca viridiflora E3 .............................
Melaleuca viridiflora E2 ....1........................
Melaleuca viridiflora E1 ....2........................
Erythrophleum chlorostachys E3 3. ..1..1.....................
Erythrophleum chlorostachys E2 1 . . 20 1 1 . 5 . . . . 2 . 1 . . . . . . . . 2 10 ....
Erythrophleum chlorostachys E1 ...1.................1...3...
Sauropus torridus E1 H . . . . . 1 1 . 1 . 2 1 1 . . . . 1 . . . . . . 1 . . . .
Eucalyptus bigalerita E3 .............................
Eucalyptus bigalerita E2 .............................
Eucalyptus bigalerita E1 .............................
Lophostemon grandiflorus
subsp. riparius E2 .............................
Eucalyptus tectifica E3 .........2..............5....
Eucalyptus tectifica E2 ...1.....1...................
Eucalyptus tectifica E1 .............................
Corymbia disjuncta E3 .................3.......3...
Corymbia disjuncta E2 ........................21...
Corymbia disjuncta E1 .............................
Corymbia greeniana E3 ........................1....
Corymbia greeniana E2 ............21...............
Corymbia greeniana E1 .............1...............
Dendrolobium cheelii E1 .............................
Gossypium pilosum E1 ......................1......
Terminalia fitzgeraldii E3 .............................
Terminalia fitzgeraldii E2 .............................
Terminalia fitzgeraldii E1 .............................
Calytrix exstipulata E2 ...........................1.
Calytrix exstipulata E1 .............................
Calytrix achaeta E2 ..............15....5......1.
Calytrix achaeta E1 ...............11..........2.
Acacia kelleri E2 .............................
Grevillea agrifolia subsp.
microcarpa E2 .............................
Calytrix brownii E2 .............................
Calytrix brownii E1 .............................
Acacia arida E2 .............................
Terminalia canescens E3 .............................
Terminalia canescens E2 .2....1.....2.....110 3 . . 2 1 1 1 . 1
Terminalia canescens E1 ....................5........
Buchanania obovata E3 .........................1...
Buchanania obovata E2 . . . 1 . 1 . . . . . . . . 3 . 1 . . 2 2 . . 1 1 1 . . .
Buchanania obovata E1 ......1.......1.1....1.1.....
Grewia retusifolia E2 .............1.........21....
Grewia retusifolia E1 ....11.......2...1......1....
Hakea arborescens E3 .............................
Hakea arborescens E2 .......................1.2...
Hakea arborescens E1 .......................1.....
Grevillea mimosoides E2 ...1.............1.....2.1...
Grevillea mimosoides E1 ........1....................
Planchonia careya E3 .......................3.....
Planchonia careya E2 . . . 1 . . . 1 . . . . 1 . 1 1 . 1 . . . . . 1 . . . . .
Planchonia careya E1 .1.1..1.1.......1............
Gardenia resinosa subsp.
kimberleyensis E3 .............................
Gardenia resinosa subsp.
kimberleyensis E2 ...............1....1........
Gardenia resinosa subsp.
kimberleyensis E1 ................1............
Psydrax pendulina E2 1...... ...........1..........
Psydrax pendulina E1 .11.....1.....2.......1......
Phyllanthus aridus E1 ..1..1...........1...1......1
Dolichandrone heterophylla E2 ..1..........................
Dolichandrone heterophylla E1 ..1....1.........1......1....
Ficus aculeata E2 .......1...............2.1...
Ficus aculeata E1 ......1......................
Passiflora foetida var. hispida E3 .............5...............
Passiflora foetida var. hispida E2 .............2.........1.....
Passiflora foetida var. hispida E1 .............2.........221...
Vachellia valida E1 .............................
Vachellia valida E2 ........................23...
43CHAPTER 2 FIELD SURVEY AND PROTOCOLS
30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 58 59 60 61 62 63 64 65 66 67
E27
A02
Z11
A56
A55
B86
B97
B33
A62
E41
B18
E12
A06
E47
E07
E40
A79
A04
A54
A30
A22
B35
B31
A03
B15
B30
E42
A29
B17
E06
A05
A75
B65
B68
E10
B64
E43
B66
E F F G H H H H I I J J K L M M M N O O O O O P P P P R R R S T T T U V V V
..........10 510 2........................
............11........................
..........15.10 1 1 . 1 . . . 1 . . . 1 . 1 1 1 . . . . . . . .
...........2..1.......................
..........11.1........................
............15 .........................
............5.........................
.............20 ........................
.............50 ........................
..........2.110 ........................
.............1........................
..............25 20 5....1........3.......
....2.........515 5....1................
...............13.....................
................1.....................
...............10 .20 ....................
...............1.1....................
.................1....................
. . ...............10 ....................
................5.520 10 40 2...............
. . . . . . . . . . 1 . . . 2 1 1 . 3 . . . 2 1 1 5 20 2..........
........................1.............
...................1......553.........
..........2...12.1.1...10 215 1...........
...1..........1..1.......5..2.........
....................10 5................
...1............5.1.2211.10 5..5........
..........................1...........
.................1.... . . 2 5 5 . 1 2 . . . . . . . .
......................131.............
...........................10 .5........
...........1.4...2.........3520 ........
...........1................215 ........
....1..1.......................551....
.................................1....
......................2........2.1....
.................................1....
..................................45 ...
....5.............................15 ...
....................................54
...................................2.1
...................................520 .
..................1.....1.............
...10 151.1.1...5......22.1.............
....13..1.....4................1......
..............................5.......
1..2....1......1...111................
1..1......................1...........
.............1.21..1.......3..........
..........12..11....2..1. 2 3 2 1 2 . . . . . . . .
........................1.............
..............1.1.....5...1...........
................1.....112.............
..............1...11.11......1........
..............1......11......1........
...................1.......1..........
..........11.....1......1...12........
1.1...........1..1....................
......................2...............
1...............3.....2.2.............
......1.........1.....................
......................................
......................................
......................................
......................................
...1...........11...11..1....1........
...1......1...1.1....1................
........................1.............
......................................
......................................
...1................12...1.11.........
................1....2....2...........
................1....21..13...........
44
TABLE 2.4
Vegetation system for the Mitchell Plateau as interpreted on the basis of numerical
classification.
A: Corymbia nesophila−Livistona eastonii Comm.
B: Eucalyptus miniata−Livistona eastonii Comm.
C: Eucalyptus tetrodonta−Hibbertia hooglandii Comm.
D: Eucalyptus tetrodonta−Bossiaea sp. West Kimberley Comm.
E: Corymbia latifolia Comm.
F: Eucalyptus apodophylla−Eucalyptus alba var. australasica Comm.
G: Terminalia canescens Comm. (NOT MODELLED)
H: Acacia retinervis−Gonocarpus leptothecus Comm.
I: Acacia gonocarpa−Corymbia torta Comm.
J: Pandanus spiralis−Melaleuca nervosa Comm. (NOT MODELLED)
K: Pandanus spiralis−Acacia stigmatophylla Comm. (NOT MODELLED)
L: Melaleuca viridiflora−Antidesma ghaesembilla Comm. (NOT MODELLED)
M: Erythrophleum chlorostachys−Livistona eastonii Comm.
N: Eucalyptus bigalerita Comm.
O: Eucalyptus tectifica−Corymbia greeniana Comm.
P: Eucalyptus tectifica−Corymbia disjuncta Comm.
R: Terminalia fitzgeraldii Comm.
S: Bossiaea sp. West Kimberley−Corymbia polycarpa Comm.
T: Calytrix exstipulata−Calytrix achaeta Comm.
U: Acacia kelleri−Grevillea agrifolia Comm.
V: Acacia arida−Calytrix brownii Comm.
45CHAPTER 2 FIELD SURVEY AND PROTOCOLS
46
TABLE 2.5
Phytosociological data of the Pantijan area that served as the basis of the vegetation classification system for the
region (see Table 2.6 on page 50). For other legends and explanations of the codes, see the header of Table 2.3.
Running number LH12345678910 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29
Field Code
A37
A114
A81
A109
A86
B89
C88
B90
C85
C255
A101
B158
C25
B159
A108
A115
B151
B152
B38
C258
A102
C84
A110
A111
B160
C259
B165
C82
C93
Community A A B B B B B B B B C C C C J J J C D D E E E E E E E E E
Melaleuca leucadendra E3 10 70 ...........................
Pandanus cf. darwinensis E2 10 20 ...........................
Pandanus cf. darwinensis E1 .1...........................
Timonius timon E3 5............................
Timonius timon E2 10 ............................
Acacia plectocarpa subsp.
plectocarpa E3 .............................
Acacia plectocarpa subsp.
plectocarpa E2 11...........................
Corymbia torta E3 . . 2 3 10 5 5 20 15 10 .3.................
Corymbia torta E2 . . . . 1 1 . . 1 . 1 1 3 1 . . . . . 1 . . . . 1 . . . 1
Corymbia torta E1 ..111.....1...........1......
Owenia vernicosa E3 . . . 1 2 2 10 . . 10 .................5.
Owenia vernicosa E2 ...1.1...1.........1......1..
Owenia vernicosa E1 ...11....1..................1
Planchonella arnhemica E3 ......32.....................
Planchonella arnhemica E2 ..11.1.....................1.
Tephrosia rosea E1 ......1.1.1......1...........
Terminalia canescens E3 ........5......2...5.......55
Terminalia canescens E2 . . 2 1 . 1 1 1 10 . 5535510 5 2 10 4 . . . . . . 1 . 1
Terminalia canescens E1 . . 1 1 . . 1 1 . . 1 . 1 2 2 . . . . . . . . . . . . 1 .
Acacia gonocarpa E2 . . 2 . . . . 1 . . . 2 15 .....10 ..........
Acacia gonocarpa E1 ..1...............1..........
Canarium australianum var.
glabrum E3 .........10 ...................
Acacia platycarpa E3 .........5...................
Acacia platycarpa E2 .........3..................1
Acacia platycarpa E1 ...1.....1...................
Calytrix exstipulata E2 ..........52.................
Calytrix exstipulata E1 ..........1..................
Acacia dunnii E2 ..........5..................
Terminalia carpentariae E3 .......2.5........10 10 .........
Terminalia carpentariae E2 ...21........................
Vitex glabrata E2 .............1....10 ..........
Eucalyptus brachyandra E3 ...................10 .........
Eucalyptus miniata E3 .....25......1......10 20 20 25 55519 5
Eucalyptus miniata E2 ....................1........
Eucalyptus miniata E1 ....................11...2...
Petalostigma pubescens E3 .........................10 ...
Petalostigma pubescens E2 ....22............10 . 531112252
Petalostigma pubescens E1 ....................1.11.2...
Bossiaea bossiaeoides E2 ..........2.........52......3
Bossiaea bossiaeoides E1 ....................13.1.....
Acacia nuperrima E2 ....................2....3...
Acacia nuperrima E1 ....................32.1.....
Corymbia polycarpa E3 .......................2.....
Corymbia polycarpa E2 .......................11....
Corymbia dichromophloia or
Corymbia polycarpa E3 ...........................10 .
Callitris columellaris E3 .............2...............
Callitris columellaris E1 ...1.........................
Eucalyptus tetrodonta E3 .............1...............
Eucalyptus tetrodonta E2 .............1...............
Eucalyptus tetrodonta E1 .............................
Buchanania obovata E3 .....................5.......
Buchanania obovata E2 . . 251 . 1 . 112112 . . . . . . 551251121
Buchanania obovata E1 . . . 2 1 . 1 1 1 . . . . . . . . . 1 . 2 . 2 2 . . . 1 1
Acacia dissimilis E2 .......................1.....
Acacia dissimilis E1 .............................
Acacia arida E2 ........2....................
Acacia arida E1 .............................
Acacia delibrata E3 .............................
Acacia delibrata E2 .........3..............1..1.
Acacia delibrata E1 .............................
Celtis philippensis E2 .............................
Capparis jacobsii E1 .............................
Bombax ceiba E2 .............................
47CHAPTER 2 FIELD SURVEY AND PROTOCOLS
30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 58 59 60 61 62 63 64 65 66 67
C34
B150
B162
B96
A116
A100
A113
C83
A87
C257
A82
C24
A104
A91
A105
B154
A103
B78
C251
B164
C253
C254
A106
C252
B39
B155
C94
C250
A92
B153
A107
B156
B157
C80
A112
B161
B163
B95
E E E E F G G G H H I I I J J J J J J J J J J J J J J J J J K K K K L L L M
......................................
......................................
......................................
......................................
......................................
......................................
......................................
2..2.................................1
1.......1.............................
......................................
......................................
1..1..................................
......................................
......................................
......................................
......................................
.......5...................5..........
...1...1.............10 ..1..1..........
. . .....1.............2................
......................................
......................................
......................................
......................................
........1.............................
......................................
.......1..............................
......................................
......................................
5.....................................
1.1...................................
......................................
......................................
10 252..................................
1.....................................
1..2..................................
......................................
.10 21....1.............................
......................................
...10 ................................2.
. . . 1 ................................1.
......................................
......................................
.15 5.................................5.
......................................
......................................
....30 .................................
....1.................................
..5.2.................................
....5.................................
....5................... ..............
...................................1..
221.22..1..........................11.
......................................
....1.................................
..2.1.................................
.....325 20 ..............................
.....1................................
........5.............................
........55............................
........11............................
........1.............................
........2.............................
........1.............................
48
TABLE 2.5 Continued
Running number LH12345678910 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29
Field Code
A37
A114
A81
A109
A86
B89
C88
B90
C85
C255
A101
B158
C25
B159
A108
A115
B151
B152
B38
C258
A102
C84
A110
A111
B160
C259
B165
C82
C93
Community A A B B B B B B B B C C C C J J J C D D E E E E E E E E E
Brachychiton viridiflorus E2 ...........1.......2....1....
Ficus virens E2 .............................
Flagellaria indica E2 H...................1.........
Flagellaria indica E1 H............................1
Exocarpos latifolius E2 .............1...............
Hypoestes floribunda var. a.
suaveolens E2 .............................
Hypoestes floribunda var. a.
suaveolens E1 .............................
Plectranthus congestus E2 .............................
Ficus brachypoda E3 .............................
Ficus brachypoda E2 .............................
Eucalyptus bigalerita E3 .............................
Eucalyptus bigalerita E2 ................1............
Eucalyptus bigalerita E1 .............................
Eucalyptus tectifica E3 .........................32..
Eucalyptus tectifica E2 ..............12..........1..
Eucalyptus tectifica E1 ...............5.............
Corymbia greeniana E3 ................1............
Corymbia greeniana E2 ................1............
Corymbia greeniana E1 ................1............
Corymbia disjuncta E3 ...............1.............
Corymbia disjuncta E2 ..............32.............
Corymbia disjuncta E1 .............................
Grevillea mimosoides E2 ................1. ...1....1..
Grevillea mimosoides E1 .............................
Hakea arborescens E3 .............................
Hakea arborescens E2 ..............23.............
Hakea arborescens E1 ..............12.............
Cullen badocanum E2 .. ...........................
Cullen badocanum E1 .. ...........................
Decaschistia occidentalis E2 .............................
Decaschistia occidentalis E1 .........................1...
Dendrolobium cheelii E1 .............................
Corymbia cf. latifolia E2 .............................
Corymbia cf. latifolia E1 .............................
Terminalia fitzgeraldii E3 .............................
Terminalia fitzgeraldii E2 ............... ..............
Terminalia fitzgeraldii E1 .............................
Corymbia bella E3 .............................
Vachellia suberosa E2 .............................
Vachellia suberosa E1 .............................
Banksia dentata E3 .............................
Banksia dentata E2 .............................
Banksia dentata E1 .............................
Grevillea pteridifolia E3 .............................
Grevillea pteridifolia E2 .............................
Grevillea pteridifolia E1 .............................
Eucalyptus alba var.
australasica E3 .............................
Eucalyptus alba var.
australasica E2 .............................
Eucalyptus alba var.
australasica E1 .............................
Melaleuca viridiflora E3 .............................
Melaleuca viridiflora E2 .............................
Eucalyptus houseana E3 .............................
Eucalyptus houseana E1 .............................
Pandanus spiralis E2 1....................1.......
Pandanus spiralis E1 .............................
Osbeckia australiana E2 .............................
Osbeckia australiana E1 .............................
Antidesma ghaesembilla E3 .............................
Alphitonia excelsa E3 .............................
Alphitonia excelsa E2 .............................
Myrtaceae E2 .............................
Cajanus hirtopilosus E2 . . . . . . .......................
Cajanus hirtopilosus E1 .............................
Carallia brachiata E2 .............................
Corymbia ptychocarpa subsp.
ptychocarpa or Corymbia
polycarpa
E2 .............................
Lygodium microphyllum E2 H.............................
Lygodium microphyllum E1 H.............................
Terminalia hadleyana or
Terminalia ferdinandiana E3 .............................
49CHAPTER 2 FIELD SURVEY AND PROTOCOLS
30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 58 59 60 61 62 63 64 65 66 67
C34
B150
B162
B96
A116
A100
A113
C83
A87
C257
A82
C24
A104
A91
A105
B154
A103
B78
C251
B164
C253
C254
A106
C252
B39
B155
C94
C250
A92
B153
A107
B156
B157
C80
A112
B161
B163
B95
E E E E F G G G H H I I I J J J J J J J J J J J J J J J J J K K K K L L L M
........1.............................
........1.............................
........2.............................
......................................
........1.............................
........1.............................
........5.............................
.........70 ............................
.........15 ............................
.........5............................
..........50 20 5.........................
..........2.1.........................
..........1...........................
.............2310 5 2 10 10 20 15 515 5 5 10 10 1.........
. . . . . . . . . . 1 3 . 7 5 2 1 2 5 1 1 1 1 1 . 1 . . 1 3 1 . 2 . . . . .
...............1515.3153..1...........
..............1...5210 5......1.........
.............1551.11.1.11..11.........
. . ............11.....1.1.1............
.................1......10 2............
................11....1..1...1......2.
...............111....1...............
................211...1....1..........
................211...1.....21........
............................1.........
...............1...1111.2.3.1.........
..............11....1..1....1.........
.............1..1.......1.5.1.........
................1..... ......11........
............................1.........
....................1..1..............
..............1.......35.2............
....................5.................
....................1.................
..........1......................5....
..........1...........53......5555....
.......................1......1.......
...................2..........55......
...................2..........2.1.....
..............................1.1.....
...................................22.
.5................................60 2 1 .
..................................5...
.1................................1.1.
..................................255.
..................................1...
...................................10 . .
..................................1...
..................................2...
..................................1.10 .
...................................2..
.5........1.........................10 15
...................................1..
..................................15215
.....................................2
....................................1.
.....................................1
.....................................20
.....................................20
.....................................4
.....................................10
.....................................5
.....................................5
.....................................3
.....................................5
.....................................10
.....................................1
.....................................10
50
TABLE 2.6
Vegetation system for Pantijan as interpreted on the basis of numerical classification
and table sorting analyses.
A: Melaleuca leucandendra Comm. (NOT MODELLED)
B: Corymbia torta−Terminalia canescens Comm.
C: Terminalia canescens Comm.
D: Terminalia carpentariae Comm.
E: Eucalyptus miniata−Petalostigma pubescens Comm.
F: Callitris columellaris Comm. (NOT MODELLED)
G: Acacia arida Comm.
H: Acacia delibrata−Ficus brachypoda Comm.
I: Eucalyptus bigalerita Comm.
J: Eucalyptus tectifica−Corymbia greeniana Comm.
K: Terminalia fitzgeraldii−Corymbia bella Comm.
L: Banksia dentata−Grevillea pteridifolia Comm.
M: Alphitonia excelsa Comm. (NOT MODELLED)
51CHAPTER 2 FIELD SURVEY AND PROTOCOLS
52
FIG. 2.9
Ordination plot (Axes 1 and 2) of the canonical correspondence analysis for Mitchell Plateau sample plots. The red
circles indicate the position of the plots and the blue arrows indicate the axes defined by the environmental data. The
nominal variables (all except the climatic data, aspect and slope) are also shown as vectors (arrows) to allow quicker
orientation. Actually the nominal variables that show a large spread of positions of the particular states (position is
defined by the tip of the arrow) are supposed to have a stronger influence on the vegetation patterning than those
located close to each other.
53CHAPTER 2 FIELD SURVEY AND PROTOCOLS
FIG. 2.10
Ordination plot (Axes 1
and 2) of the canonical
correspondence analysis
for Pantijan sample plots.
For other explanations see
caption of Fig. 2.9.
Disturbance is less informative. Most of the plots scored the
state Non-Dist indicating that no disturbance was detected
in the plot. The states Fire and Graz were shown to play a
role only in the basalt-dominated landscapes. Slope and
Aspect do not play a major role in structuring the data.
Direct Gradient Analysis of the Pantijan Data: Interpretation
The results of the CCA ordination of the Pantijan data are
shown as a biplot in Fig. 2.10. The combination of the CCA
Axes 1 and 2 explains 7.6% and 17.1% of the variance of
species data and species-environment relations respectively.
The same environmental factors were used in the canonical
correspondence analyses of the Pantijan data as in the
Mitchell Plateau data set. The nominal variable Geology
consists of states San, Bas and Dol.
Three plots (39, 64 and 65) were identified as clear floristic
outliers. Plot 39 is classified as Plectranthus congestus-
dominated sandstone woodland (Community H), while
the other two plots are representatives of Community L
(seasonally wet sandstone woodlands). Plot 34 is also a
slight outlier as it represents ecologically odd, fire-protected
Callitris columellaris woodland on dolerite. The BioClim
variables again show a contracting grouping pattern, with
one group characterising high-altitude, high precipitation
sandstone landscapes and the other being characteristic
of low-altitude, warmer basalt-dominated landscapes.
Geology again plays an important role as a driver and data-
structuring variable (see the broad span of the states of the
variables on the CCA ordination plane defined by Axes 1 and
2 in Fig. 2.10).
The environmental data sets used in the CCA analyses for
the Mitchell Plateau and Pantijan are shown in Appendices
2.2 and 2.3 respectively. A list of the environmental
parameters, including the measurement scale and the unit
of the measurement, is given in Table 2.1.
Direct Gradient Analysis of the Mitchell Plateau Data:
Interpretation
The results of the CCA ordination of the Mitchell Plateau
data are given in Fig. 2.9 as a biplot showing the position
of all 67 plots and the visualised importance of the studied
environmental factors. The combination of the CCA Axes
1 and 2 explains 5.9% and 16% of the variance of species
data and species-environment relations respectively.
Two of the environmental factors are nominal variables:
Geology, containing states San, Lat, Bas and Disturbance,
containing states Graz, Fire, No-Dist. The remaining
variables are in ratio scale. The climatic (BioClim) variables
show an interesting polarised pattern. Two distinct groups
of variables emerge with one indicating high precipitation
for the vegetation on the elevated laterite plateau. The
ratio variable ‘Alt’ also groups with this ‘high-precipitation’
group of variables. The other group of BioClim variables is
informative of higher temperature being characteristic of
parts of the low-altitude basalt woodlands and outlying
sandstone shrublands (Plots 53, 63–66; Fig. 2.9). Geology
appears to play an important role in structuring the data.
All three character states (connected by the pink triangle
in Fig. 2.9) are remote and show distance from the centre
of the coordinate system, indicating their exclusive role in
separate parts of the ordination space. The nominal variable
54
regarding predictor variable or target class modification
to be implemented at any stage of the process. For these
reasons, CART analysis was selected as the most suitable
classification methodology for this project.
In practicality, a CART analysis models a target
variable according to a set of predictor variables. In this
project, this meant establishing which environmental
variables (predictors) were of highest importance when
determining splitting threshold values for vegetation
type (target) classification, and how these ‘splitters’
should be structured in a logical sequence. An alternative
interpretation would be that the CART analysis determined
the optimal set of rules for vegetation classification.
CART 6.0 (Steinberg & Golovnya 2006), the soware used
in this project, is based on the original CART algorithm
developed by Breiman et al. (1984). In order to determine
an optimal decision tree, the soware runs thousands
of random splitting iterations resulting in hundreds of
dierent trees of varying classification accuracy. The final
return is a profile of the ‘best’ trees, determined by the
number of nodes (tree size) against the calculated relative
cost of that tree (total classification error divided by the
number of nodes). Relative cost is scaled between 0 and 1,
where a value of 0 would indicate no error and a value of 1
would represent the performance of random guessing. Fig.
2.11 gives an example of such a profile, where each square
represents one tree, plotted according to relative cost and
tree size. The 10-node tree highlighted by the horizontal
line is considered the optimal tree, as the relative cost is
lowest of all of the trees displayed.
However, since the resulting trees determined through CART
analysis are not defined according to a stopping criterion,
the tree with the lowest relative cost will not always model
every class of the target variable. In such cases, the optimal
tree can be ‘grown’ (increasing the number of branches) in
the hope that the CART algorithm will find a splitter for a
3.4 Step 4: Setting Mapping Rules and Modelling
3.4.1 Classification and Regression Trees
Over the past decade-and-a-half, the use of classification
trees has become steadily more prevalent for autonomously
creating rulesets (Lawrence & Wright 2001). Classification
trees, also known as ‘decision trees’ (or DTs), are constructed
by recursive division of training data into increasingly
homogeneous subsets. A branch or split in the classification
tree is a threshold value for the image feature that produces
the most deviance in the data set. Subsequent subsets are
subject to further division, perhaps using a dierent feature
showing high heterogeneity, until either a pre-set variance or
classification tree level is reached. The result is a hierarchical
ruleset used for digital image classification (Hansen et al.
1996, Lawrence & Wright 2001).
Classification and Regression Trees (CART; see Breiman
et al. 1984, Fielding 2007 for detailed descriptions of
the technique and Bayes & Mackey 1991, Michaelsen
et al. 1994, Cains 2001, Miller & Franklin 2002 for selected
vegetation-related reviews and applications) is a robust
decision-tree tool for data mining, predictive modelling and
data processing. It can be used to generate accurate and
reliable predictive models for a wide range of applications
using both discrete and continuous data sets. CART diers
from other decision-tree methodologies in several aspects.
Firstly, the iterative data splitting (recursive division)
is binary rather than multi-way and this avoids data
fragmentation and a consequent accompanying decrease
in pattern detection. Secondly, the size of a decision tree
developed by CART is not determined by a stopping rule,
e.g. a given degree of homogeneity on the terminal nodes.
Rather, the tree is over-developed, so as not to miss any
structure in the data, and then pruned as necessary.
Thirdly, and of particular importance for our study, CART
implements cross validation self-testing, resulting in more
robust and transferable trees when utilizing smaller data
sets (Steinberg & Golovnya 2006). Finally, unlike several
other classification methods, the CART process is both
transparent and interpretable, allowing for expert decisions
FIG. 2.11
An example of the relative error curve produced by CART modelling.
0.70
0.60
0.50
0.40
0 10 20 30 40 50 60 70
Number of Nodes
Relative Cost
0.488
55CHAPTER 2 FIELD SURVEY AND PROTOCOLS
56
FIG. 2.12
Final CART diagram for the Mitchell Plateau zonal vegetation units (detailed classification). The alpha-numerical
(and colour) coding of the classes is as follows: A, B, C (incl. D), E, F, H, I, M (incl. N), O (incl. P), R, S (incl. T, U, V).
(Communities G, J, K and L were not modelled.) Insert: Simplified CART classification tree showing the hierarchy of
classifiers (splitters).
2
2
1
3
4
1
57CHAPTER 2 FIELD SURVEY AND PROTOCOLS
43
58
FIG. 2.13
The mapping rule set for the Mitchell Plateau zonal vegetation data set.
/*Terminal Node 1*/
if
GEOLOGY$ == Bas ||
GEOLOGY$ == Dol
&&
PC6 <= -3.87293
{
terminalNode = 1;
class = R;
}
/*Terminal Node 2*/
if
GEOLOGY$ == Bas ||
GEOLOGY$ == Dol
&&
PC6 > -3.87293 &&
PC4 <= 6.54848 &&
PC2 <= -13.3268
{
terminalNode = 2;
class = M;
}
/*Terminal Node 3*/
if
GEOLOGY$ == Bas ||
GEOLOGY$ == Dol
&&
PC6 > -3.87293 &&
PC4 <= 6.54848 &&
PC2 > -13.3268 &&
B7 <= 62.5
{
terminalNode = 3;
class = O;
}
/*Terminal Node 4*/
if
GEOLOGY$ == Bas ||
GEOLOGY$ == Dol
&&
PC6 > -3.87293 &&
PC4 <= 6.54848 &&
PC2 > -13.3268 &&
B7 > 62.5
{
terminalNode = 4;
class = M;
}
/*Terminal Node 5*/
if
GEOLOGY$ == Bas ||
GEOLOGY$ == Dol
&&
PC6 > -3.87293 &&
PC4 > 6.54848
{
terminalNode = 5;
class = R;
}
/*Terminal Node 6*/
if
GEOLOGY$ == Lat ||
GEOLOGY$ == Sand
&&
B1 <= 15.5 &&
B2 <= 28 &&
NDWI <= 0.371848 &&
B5 <= 34.5
{
terminalNode = 6;
class = E;
}
/*Terminal Node 7*/
if
GEOLOGY$ == Lat ||
GEOLOGY$ == Sand
&&
B1 <= 15.5 &&
B2 <= 28 &&
NDWI <= 0.371848 &&
B5 > 34.5
{
terminalNode = 7;
class = C;
}
/*Terminal Node 8*/
if
GEOLOGY$ == Lat ||
GEOLOGY$ == Sand
&&
B1 <= 15.5 &&
B2 <= 28 &&
NDWI > 0.371848 &&
NDWI <= 0.410774
{
terminalNode = 8;
class = A;
}
/*Terminal Node 9*/
if
GEOLOGY$ == Lat ||
GEOLOGY$ == Sand
&&
B1 <= 15.5 &&
B2 <= 28 &&
NDWI > 0.410774 &&
PC4 <= 0.661713 &&
PC5 <= 0.875853
{
terminalNode = 9;
class = F;
}
/*Terminal Node 10*/
if
GEOLOGY$ == Lat ||
GEOLOGY$ == Sand
&&
B1 <= 15.5 &&
B2 <= 28 &&
NDWI > 0.410774 &&
PC4 <= 0.661713 &&
PC5 > 0.875853
{
terminalNode = 10;
class = B;
}
/*Terminal Node 11*/
if
GEOLOGY$ == Lat ||
GEOLOGY$ == Sand
&&
B1 <= 15.5 &&
B2 <= 28 &&
NDWI > 0.410774 &&
PC4 > 0.661713
{
terminalNode = 11;
class = B;
}
/*Terminal Node 12*/
if
GEOLOGY$ == Lat ||
GEOLOGY$ == Sand
&&
B1 <= 15.5 &&
B2 > 28
{
terminalNode = 12;
class = H;
}
/*Terminal Node 13*/
if
GEOLOGY$ == Lat ||
GEOLOGY$ == Sand
&&
B1 > 15.5
{
terminalNode = 13;
class = I;
}
59CHAPTER 2 FIELD SURVEY AND PROTOCOLS
4) The communities of the sandstone and laterite shrublands
were a priori placed into one mapping unit because of their
uniqueness and very high floristic variability.
5) Using the selected set of environmental predictors (see
above), CART analyses were run and the result was
evaluated according to ability of the CART to separate
(on predictors) the given mapping classes. In cases
where we deemed this separation weak or non-existent,
we further amalgamated the mapping classes.
6) The final step of this iterative process is depicted by
the final CART analysis of the zonal vegetation of
the Mitchell Plateau (Figure 2.12). In this decision
tree, Node 1 commences with all 65 sample points
representing the field observations and extracted
spectral values. The CART analysis determined that
Geology type was the best initial splitter, suggesting a
class of samples characteristic for basalt and dolerite.
This class consisted of 17 sample points, while the
remaining data (48 sample points) represented other
types. The further splits were based on PC6 and the B1
(the blue band of the Landsat image). Some terminal
nodes (leaves) of this tree failed to show pure pattern
(one class only). An example of this is the terminal
node 4, which shows a 50% split between classes
M and O (2 sample points each). Nevertheless this
tree was selected as the one with the best trade-o
between low relative cost and the highest number of
classes modelled.
terminal node that encompasses more than one class. This
is not advisable, however, as this increases the relative cost
of the CART and therefore decreases the accuracy of the
classification. There is then a trade-o between the number
of classes to be modelled and the accuracy of the modelled
classes, which requires a judgement call from the operator.
Another alternative is to merge the ambiguous classes,
should that be logical in the context of the analysis.
Ruleset for the Mitchell Plateau Region:
Iterations and Outcomes
The creation of the ruleset for the Mitchell Plateau region
was the critical part of the vegetation mapping process.
This comprised several iterations characterised by varying
spectrum and number of environmental variables. Initially
the number of predictors tested for the Kimberley CART
analyses was high—geology, elevation, slope, aspect,
NDWI and 19 of the BioClim climate variables were all
added to early CART analyses for each area. Additionally,
the values of the six Landsat bands and the six PCA
components were extracted to the field site points to
complement the environmental variables. Early CART
analyses showed a high informative (classification) value
of elevation, aspect and slope. These variables were,
however, deemed less reliable due to scale discrepancies
between the field estimates/measurements of the aspect
and slope and other GIS data used. The BioClim data are a
result of modelling based on interpolation between climatic
stations in the modelling area. Since the density of climatic
stations delivering real data for the Kimberley is known to
be extremely low, the modelled climatic surfaces have to
be used with utmost caution. We consequentially decided
to exclude the BioClim climatic variables from the CART
analyses due to their comparably low spatial resolution
(and reliability).
CART analysis was undertaken in two phases of modelling:
for zonal mapping units (see Box 2.1) and separately for
azonal vegetation.
The decision (CART) trees were derived using the following
predictors: geology type, the six Landsat bands, the six
principal components of the Landsat bands and NDWI.
The selection of classes (mapping units) was undertaken
according to the following procedure:
1) The complete vegetation classification system, as
revealed by the numerical-classification analyses (see
Table 2.4) was taken as the starting base.
2) The azonal and relic units were identified first and
excluded from the modelling.
3) Furthermore, the units represented by only one relevé
(such as G Terminalia canescens Community in the
Mitchell Plateau data) were also excluded.
60
FIG. 2.14
Final CART diagram for the Pantijan zonal vegetation units (detailed classification). The alpha-numerical (and colour)
coding of the classes is as follows: B (incl. C, D), E, G (incl. H), I, J, K, L. (Communities A, F, M were not modelled.).
Insert: Simplified CART classification tree showing the hierarchy of classifiers (splitters).
2
1
3
1
61CHAPTER 2 FIELD SURVEY AND PROTOCOLS
32
62
FIG. 2.15
The mapping rule set for the Pantijan zonal vegetation data set.
/*Terminal Node 1*/
if
GEOLOGY == 1
) &&
PC1 <= 71.7311
{
terminalNode = 1;
class = I;
}
/*Terminal Node 2*/
if
GEOLOGY == 1
) &&
PC1 > 71.7311 &&
NDWI <= 0.553033 &&
B2 <= 19.5
{
terminalNode = 2;
class = K;
}
/*Terminal Node 3*/
if
GEOLOGY == 1
) &&
PC1 > 71.7311 &&
NDWI <= 0.553033 &&
B2 > 19.5
{
terminalNode = 3;
class = J;
}
/*Terminal Node 4*/
if
GEOLOGY == 1
) &&
PC1 > 71.7311 &&
NDWI > 0.553033
{
terminalNode = 4;
class = K;
}
/*Terminal Node 5*/
if
GEOLOGY == 4
) &&
B5 <= 28.5
{
terminalNode = 5;
class = L;
}
/*Terminal Node 6*/
if
GEOLOGY == 4
) &&
B5 > 28.5 &&
B7 <= 57.5
{
terminalNode = 6;
class = E;
}
/*Terminal Node 7*/
if
GEOLOGY == 4
) &&
B5 > 28.5 &&
B7 > 57.5 &&
PC3 <= 103.507
{
terminalNode = 7;
class = G;
}
/*Terminal Node 8*/
if
GEOLOGY == 4
) &&
B5 > 28.5 &&
B7 > 57.5 &&
PC3 > 103.507
{
terminalNode = 8;
class = B;
}
/*Terminal Node 1*/
if
GEOLOGY == 1
) &&
PC1 <= 71.7311
{
terminalNode = 1;
class = I;
}
/*Terminal Node 2*/
if
GEOLOGY == 1
) &&
PC1 > 71.7311 &&
NDWI <= 0.553033 &&
B2 <= 19.5
{
terminalNode = 2;
class = K;
}
/*Terminal Node 3*/
if
GEOLOGY == 1
) &&
PC1 > 71.7311 &&
NDWI <= 0.553033 &&
B2 > 19.5
{
terminalNode = 3;
class = J;
}
/*Terminal Node 4*/
if
GEOLOGY == 1
) &&
PC1 > 71.7311 &&
NDWI > 0.553033
{
terminalNode = 4;
class = K;
}
/*Terminal Node 5*/
if
GEOLOGY == 4
) &&
B5 <= 28.5
{
terminalNode = 5;
class = L;
}
/*Terminal Node 6*/
if
GEOLOGY == 4
) &&
B5 > 28.5 &&
B7 <= 57.5
{
terminalNode = 6;
class = E;
}
/*Terminal Node 7*/
if
GEOLOGY == 4
) &&
B5 > 28.5 &&
B7 > 57.5 &&
PC3 <= 103.507
{
terminalNode = 7;
class = G;
}
/*Terminal Node 8*/
if
GEOLOGY == 4
) &&
B5 > 28.5 &&
B7 > 57.5 &&
PC3 > 103.507
{
terminalNode = 8;
class = B;
}
/*Terminal Node 1*/
if
GEOLOGY == 1
) &&
PC1 <= 71.7311
{
terminalNode = 1;
class = I;
}
/*Terminal Node 2*/
if
GEOLOGY == 1
) &&
PC1 > 71.7311 &&
NDWI <= 0.553033 &&
B2 <= 19.5
{
terminalNode = 2;
class = K;
}
/*Terminal Node 3*/
if
GEOLOGY == 1
) &&
PC1 > 71.7311 &&
NDWI <= 0.553033 &&
B2 > 19.5
{
terminalNode = 3;
class = J;
}
/*Terminal Node 4*/
if
GEOLOGY == 1
) &&
PC1 > 71.7311 &&
NDWI > 0.553033
{
terminalNode = 4;
class = K;
}
/*Terminal Node 5*/
if
GEOLOGY == 4
) &&
B5 <= 28.5
{
terminalNode = 5;
class = L;
}
/*Terminal Node 6*/
if
GEOLOGY == 4
) &&
B5 > 28.5 &&
B7 <= 57.5
{
terminalNode = 6;
class = E;
}
/*Terminal Node 7*/
if
GEOLOGY == 4
) &&
B5 > 28.5 &&
B7 > 57.5 &&
PC3 <= 103.507
{
terminalNode = 7;
class = G;
}
/*Terminal Node 8*/
if
GEOLOGY == 4
) &&
B5 > 28.5 &&
B7 > 57.5 &&
PC3 > 103.507
{
terminalNode = 8;
class = B;
}
the modelled coverage of the azonal vegetation based on
high environmental wetness did not reveal interpretable
patterns. Many patches of azonal vegetation were
suggested outside the influence of riparian (riverine) zones,
possibly linked to landscapes experiencing temporary
wetness. We concluded that we might not have optimal
NDWI coverage and abandoned the attempt to use NDWI to
model azonal vegetation.
As the final step in creating a ruleset, a sequence of ‘if-
then’ rules was created to classify the zonal vegetation
(Fig. 2.13). These rules were used to produce the vegetation
map by applying them to the segmented image of the
mapping area (see below) using Object-Oriented Image
Analysis (OBIA) in eCognition 8.0.
We admit that selecting a CART analysis was a risky
strategy as we had only 65 plots and created 10−15
classes. It appears, however, that the modelled zonal
vegetation patterns are entirely plausible. The apparent
success of the modelling exercise may be ascribed to the
strong link between the presumed ecological drivers and
the vegetation patterns.
A separate CART analysis was undertaken for the azonal
vegetation type Riparian Thickets. Only two classes were
required for this classification (zonal and azonal) and only
one predictor variable (NDWI) was used. The CART analysis,
therefore, essentially determined the optimum threshold
value of NDWI for the classification of azonal vegetation.
This value was then used to reclassify the NDWI layer in
ArcMap to create a Riparian Thickets layer. Inspection of
63CHAPTER 2 FIELD SURVEY AND PROTOCOLS
The advantages of OBIA over pixel-based classification
methods include the following (Benz et al. 2004, Bock et al.
2005, Hay et al. 2005):
• Moremeaningfulstatisticalcalculationofspectraland
textural qualities;
• Theavailabilitytotheclassicationprocessofobject
feature qualities such as shape and topology;
• Thecapacitytoconsiderintuitivespatialrelations
between real-world objects and image objects; and
• TheeaseofintegrationbetweenGISandremotesensing
environments and flexibility among dierent soware
platforms.
Additionally, the hierarchical nature of OBIA is ideally
suited to implement rulesets, a feature strongly supported
by eCognition 8.0.
Segmentation of the images into objects was carried out
using a multi-resolution segmentation algorithm on the
bands with the most spectral information: PC1 and PC2.
The CART ruleset was then applied to the image objects
as a set of ‘if-then’ rules, resulting in the sequential
classification of the image into the modelled target classes.
3.5 Step 5: Post-Modelling Adjustments to the Maps
3.5.1 Digitising Non-modelled Units
CART modelling was unsuccessful in depicting the extent
of azonal vegetation types. To correct for this, it was
necessary to implement a number of post-modelling
cartographic modifications. These adjustments involved
digitising the spatial extent of units which:
1) we were not able to model successfully using NDWI
(azonal vegetation);
2) we have not suciently studied in the field (neither by
our predecessors nor us) to yield the volume of spatial
data required to model their occurrence (freshwater
wetland vegetation, mangroves, saline flats, basalt
rocky outcrops, beaches and clis etc.); and
3) were of relic origin and hence their occurrence was
dicult to predict by using modern spatial data layers
(monsoonal rainforests).
The following units of azonal vegetation were digitised
from high-resolution aerial photographs or satellite
images:
a) riparian thickets, recognisable as dense, dark-coloured
patches fringing waterways and wetlands;
b) non-wooded freshwater wetlands, usually occurring
as river headwater grasslands or as belts around
backwaters and billabongs;
c) mangroves (no attempt was made to recognise
separate vegetation zones within mangrove
communities);
Ruleset for the Pantijan Region: Iterations and Outcomes
The experience gained performing CART analyses for
the Mitchell Plateau mapping area was valuable for the
analyses undertaken in the Pantijan area. As in the case
of the Mitchell Plateau map, the predictors for the Pantijan
area were limited to geology, the six Landsat bands, the six
principal components and NDWI. Several iterations were
modelled, starting with the selection of zonal mapping
units (for the full vegetation system see Table 2.6). Aer
the final iteration we settled on seven mapping units,
informed by the power of separation of the units in CART
and its ecological interpretability.
The final CART for the model of the Pantijan mapping area
is shown in Figure 2.14. As with the Mitchell Plateau region,
geology is the primary driver of vegetation patterns and it
was therefore identified as the first splitter in the CART. The
le branch, from Node 2, defines all the vegetation classes
found on either basalt or dolerite (Geology = 1). PC1, NDWI
and Band 2 (green band of the Landsat image) are used
as the splitters for Classes I, J and K. The right branch,
from Node 5, defines all the vegetation classes found on
either sandstone or laterite (Geology = 4). Bands 5 and 7
of the Landsat image and PC3 are used as the splitters for
Classes B, E, G and L. A noteworthy feature of the Pantijan
CART, as compared to the Mitchell Plateau equivalent, is
the high level of purity (one class only) of the terminal
nodes. Only Terminal Nodes 6 and 8 predict more than one
class and even in those instances, the overlap is minimal.
This is a remarkable result, given the constraints of the low
number of data points and high number of classes.
As in the Mitchell Plateau ruleset, segmentation of the
objects in the Pantijan ruleset was carried out using a
multi-resolution segmentation algorithm on the bands
with the most spectral information: the first two principal
components (PC1 and PC2). The CART ruleset was then
applied to the image as a set of ‘if-then’ rules, resulting in
the sequential classification of the image into the modelled
target classes. The Pantijan ruleset, as implemented in
eCognition 8.7, is shown in Figure 2.15. The application
of these rules resulted in a classification that was then
exported as a ti image and imported into ArcMap for
further treatment.
3.4.2 Image Segmentation
Object-Oriented Image Analysis (OBIA) is the delineation
and classification of homogeneous image segments in
much the same way as the human eye perceives and
identifies objects in the real world. The primary benefit of
this approach is the ability to analyse image features as an
intuitively-determined and meaningful unit, rather than an
arbitrarily defined image pixel.
64
3.6 Step 6: Verification
The validation of the Mitchell Plateau maps was undertaken
by comparing a validation dataset to the modeled map data.
Ninety-five validation data points were collected during a
field trip in August 2012. Selection of the points in the field
was semi-random, being constrained by proximity to roads
but placed randomly along these routes. At each sampling
point (see Fig. 2.3 for their position), a GPS reading was
taken and the identity of the sampled vegetation patch
established using the classification system defined for the
Mitchell Plateau mapping area (see Tables 2.3 and 2.4).
The classified validation dataset was then overlain on
the modeled map in ArcMap. A comparison between the
validation and modeled data sets was undertaken at both
the detailed (ML1) and simplified (ML2) mapping levels. The
result was that the modeled data agreed with the validation
data point at 43 of the 95 (45%) validation points at the
ML1 mapping level and at 75 of the 95 (79%) validation
points at the ML2 mapping level.
A second validation process was undertaken with a 100 m
buer applied to the validation data set. This determined
if a validation data point lay within 100 m, or about three
Landsat pixels, of a correctly modeled location. A 100 m
margin of error was deemed appropriate because the 30 m
pixel size of the Landsat images used in modeling means
that the location of a community may be more precisely
determined on the ground than it can be on Landsat images.
The result of the second round of validation was that
modeling agreed with the validation data point at 71 of the
95 (74%) locations at ML 1 and 84 of the 95 (88%) locations
at ML2.
3.7 Step 7: Presentation
The purpose of our maps of the Mitchell Plateau and Pantijan
areas is to illustrate the results of a modelling analysis,
highlight spatial relationships between vegetation mapping
units and facilitate understanding of the vegetation patterns.
We have aimed at maximising the ease of user interpretation
by following the principles of good cartography and
complying with accepted mapping conventions.
The Mitchell Plateau and Pantijan vegetation maps are
thematic in nature. This is usual for vegetation maps, as
information about vegetation is qualitative in nature and
as such is best communicated in a thematic manner. A
thematic map focuses on the geographic distribution and
spatial variation of a certain feature or theme; in this case
vegetation units. This is in contrast to general-purpose
maps, such as topographic maps, that communicate specific
quantitative data.
In symbolising the vegetation data on our maps, we
considered the visual distinctiveness of the colours used
and commonly accepted conventions for vegetation colour
d) mud (saline) flats;
e) beaches and coastal clis;
f) basalt rocky outcrops; and
g) monsoonal rainforests (vine thickets).
3.5.2 Further Adjustments of the
CART Modelling Outcomes
In addition to the amendments for azonal mapping units,
the following post-modelling adjustments were made to
the Mitchell Plateau map:
1) The CART analyses could not separate classes I and S
(Fig. 2.12). These two classes, which represent dierent
forms of Kimberley shrubland, were merged and
mapped as a single unit.
2) Class B (Eucalyptus miniata-Livistona eastonii
Community) was reclassified as Class A (Corymbia
nesophila-Livistona eastonii Community) where it
occurs on laterite.
3) Classes A and B were reclassified as Class C
(Eucalyptus tetrodonta-Hibbertia hooglandii
Community) where these clases occurred on
sandstone. This meant that Class B does not appear on
the final map.
The final vegetation maps of the Mitchell Plateau
and Pantijan areas are presented in Figs 16 and 17
respectively. They are also included in PDF format in the
Electronic Appendices of this report with the file names
Mitchell Plateau Vegetation Map_basic version and Pantijan
Vegetation Map_basic version.
3.5.3 Production of Simplified Versions of the
Vegetation Maps
We prepared simplified versions of the vegetation maps of
both the Mitchell Plateau and Pantijan areas, which map
the major vegetation groups. They are shown in Figs 18
(Mitchell Plateau) and 19 (Pantijan) and are also provided
in PDF format in the Electronic Appendices to this report
as Mitchell Plateau Vegetation Map_simplified version and
Pantijan Vegetation Map_simplified.
The simplified Mitchell Plateau vegetation map groups
Communities A, C, E, F and H into Kimberley Sandy
Woodlands; Communities M, N, O, P and R into Kimberley
Clayey Woodlands and Communities I, S, U, T and V into
Kimberley Sandy Shrublands. All the azonal vegetation
types were retained on the simplified map.
The simplified Pantijan vegetation map groups
Communities B, C, D, E and L into Kimberley Sandy
Woodlands. Communities I, J and K are grouped into
Kimberley Clayey Woodlands and Communities G and H
into Kimberley Sandy Shrublands. All the azonal vegetation
types were retained on the simplified map.
65CHAPTER 2 FIELD SURVEY AND PROTOCOLS
scale that will remain accurate when the map is printed at
dierent scales.
The final maps are provided electronically in printable
formats (PDF, TIFF and BMP) and as shape files in the
accompanying Electronic Appendices (CD).
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