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Olinia chimanimani (Penaeaceae), a new species endemic to the Chimanimani Mountains of Mozambique and Zimbabwe

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Abstract

Olinia chimanimani T. Shah & I. Darbysh. is described as a distinct species from the Chimanimani mountains in Mozambique and Zimbabwe, based on morphological evidence. It differs from other species of Olinia sect. Rochetiana in its smaller leaf size, sessile leaf attachment, glabrous flowers and galled flowers becoming narrowly swollen without prominent tubercles when infected. A species description, key and illustration, distribution map and ecological information are provided. The populations have been studied in the field, and it is only known from two locations. It is potentially under threat from burning due to human activity associated with illegal artisanal mining activity, and thus has been evaluated as Endangered (EN) using the IUCN Red List categories and criteria.
Olinia chimanimani (Penaeaceae), a new species endemic
to the Chimanimani Mountains of Mozambique and Zimbabwe
Toral Shah
1
, Iain Darbyshire
1
& Hermenegildo Matimele
2
Summary.Olinia chimanimani T. Shah & I. Darbysh. is described as a distinct species from the Chimanimani moun-
tains in Mozambique and Zimbabwe, based on morphological evidence. It differs from other species of Olinia sect.
Rochetiana in its smaller leaf size,sessile leaf attachment, glabrous owers and galled owers becoming narrowly swollen
without prominent tubercles when infected. A species description, key and illustration, distribution map and ecological
information are provided. The populations have been studied in the eld, and it is only known from two locations. It is
potentially under threat from burning due to human activity associated with illegal artisanal mining activity, and thus
has been evaluated as Endangered (EN) using the IUCN Red List categories and criteria.
Key Words. conservation, Endangered, IUCN Red List assessment, key, morphology, Oliniaceae, restricted range.
Introduction
The Chimanimani Nyanga Highlands in Southeast
Africa are the most isolated component of the African
Great Escarpment (Clark et al.2011) and are noted for
their signicantly high levels of endemism (Wild 1964).
The Chimanimani Mountain range is situated on the
border of Zimbabwe and Mozambique (approx. 33°00E,
19°50S) and forms part of the Eastern Afromontane
hotspot (BirdLife International 2012). Its relative isola-
tion from other mountains and an unusual underlying
geology, with extensive outcrops of nutrient-poor quartz-
ite, have given rise to a biodiversity hotspot with high
plant endemism.
The region has been of long-standing interest for
botanists, with the majority of information and plant
collections derived from the Zimbabwe portion whilst the
larger Mozambican side of the massif has been far less
well studied. Recent surveys under a Critical Ecosystem
Partnership Fund (CEPF) project In from the cold:
providing the knowledge base for comprehensive biodiversity
conservation in the Chimanimani Mountains, Mozambique
have addressed this gap by facilitating a botanical study of
the Mozambique side, resulting in a better understanding
of the endemic species, their distribution, threats and
conservation status (Timberlake et al.2016). This work has
resulted in a comprehensive checklist of species with a
restricted distribution occurring on quartzite and scrub
above 1200 m, with 74 strict endemic and 19 near-
endemic taxa documented (Wursten et al.2017). These
recent surveys have also uncovered several potentially
new species to science, as well as providing more
collections for species that had previously only been
considered to be tentatively distinct and not formally
described, such as Empogona jenniferae Cheek (Cheek et al.
in press). The number of endemic plant species on
Chimanimani is therefore sure to continue to rise.
The most recent taxonomic revision of the genus Olinia
Thunb. was carried out by Sebola & Balkwill (2013)
supported by a phenetic analysis (Sebola & Balkwill 2009).
They recognised ten species divided into two sections; sect.
Olinia and sect. Rochetiana, readily separated by their
morphology. Sect. Olinia has inconspicuous tertiary veins
on the adaxial surface with tertiary veins looping only once
at the margin and sect. Rochetiana, has conspicuous tertiary
venation on the adaxial surface with tertiary veins looping
twice at the margin (Sebola & Balkwill 2013). Olinia has
previously been placed in its own monogeneric family,
Oliniaceae (see e.g. Verdcourt 1978;Heywoodet al.2007).
However, it has recently been transferred to the
Penaeaceae family based on molecular evidence, where it
is recognised as one of three tribes, Olinieae Horan.
alongside Rhynchocalyceae Beusekom and Penaeeae DC.
(APG IV 2016).
During the rstofthreeCEPFsurveysin2014,two
collections of an unusually small-leaved species of Olinia
were made by the third author of this paper on the
Mozambican side of Chimanimani. These specimens were
matched to existing specimens from the Chimanimani
Mountains in the Kew (K) herbarium. The rst ever
collection of this small-leaved Olinia was made by Hiram
Wild (Wild 3606) in 1950 on the Zimbabwe side of the
Accepted for publication 23 May 2018.
1
Herbarium, Library, Art & Archives, Royal Botanic Gardens, Kew, Richmond, Surrey, TW9 3AE, UK. e-mail: t.shah@kew.org
2
Instituto de Investigacão Agrária de Mocambique, IIAM, Maputo, Mozambique.
KEW BULLETIN (2018) 73:36
DOI 10.1007/S12225-018-9757-2
ISSN: 0075-5974 (print)
ISSN: 1874-933X (electronic)
© The Author(s), 2018
massif. This specimen, and the later collection Whellan 2203
(K), were recognised by Verdcourt (1978)intheFlora
Zambesiaca treatment of Oliniaceae as a pathological form of
Olinia vanguerioides Baker f., but he noted that the specimens
had much smaller leaves. Sebola & Balkwill (2013)didnot
discuss or cite these collections, or a third, owering
specimen Linder 3990 (K) within any of their delimited
species. A further botanical expedition to the Chimanimani
Mountains in 2016, during which this Olinia species was
specically targeted, resulted in additional collections with
similar characteristics growing in similar habitats to the older
specimens. All the specimens are restricted to higher
elevation regions of Chimanimani. These specimens were
closely compared with sympatric and morphologically
similar species of Olinia in order to assess its taxonomic
status and it is concluded that the Chimanimani taxon is a
distinct species, described here as Olinia chimanimani T.
Shah & I. Darbysh.
Further, it was brought to light during this study,
that whilst Sebola and Balkwill (2013) recognised two
sections in Olinia, these were not validated according
to Article 40.1 of the Botanical Code (ICN, McNeill
et al. 2012). To rectify this, we validate sect. Rochetiana
in the taxonomic treatment below.
Material and Methods
Morphological characters for the new species were
measured on herbarium specimens at the Kew her-
barium. Other herbaria with holdings of Zimbabwean
and Mozambican specimens (BM, LMA, SRGH) were
checked for additional material of the new species, but
none were found. All characters were measured on
dry material, except internal oral characters which
were measured from a rehydrated ower under a
dissecting microscope. Characters deemed to be of
taxonomic signicance follow the most recent mono-
graphic revision of Olinia (Sebola & Balkwill 2013) and
the terminology is according to Beentje (2010). A
species conservation assessment was made using the
categories and criteria of IUCN (2012).
Taxonomic Treatment
Olinia sect. Rochetiana Sebola & Balkwill ex T. Shah
sect. nov. Type species: Olinia rochetiana A. Juss., Comp.
Rend. Hebd. Séances Acad. Sci. 22: 812 (Jussieu 1846).
http://www.ipni.org/urn:lsid:ipni.org:names:77178774-1
Olinia chimanimani T. Shah. & I. Darbysh. sp. nov. Type:
Zimbabwe, Manicaland, Chimanimani Mountains, at W
base of (Pnt.?) 71, Linder 3990 (holotype K! [K000963156]).
http://www.ipni.org/urn:lsid:ipni.org:names:77178775-1
Shrub or small tree up to 5 m. Bark thin, pale grey
(white) to brown. Branchlets grey to brown, convexly
quadrangular with ridges. Leaves sessile, simple, entire,
opposite except on young (or sapling) branches when
ternate, blade coriaceous, obovate to oblanceolate
occasionally elliptic, (19.0 ) 25.0 40.0 mm long,
10.0 25.0 mm wide, base attenuate, apex retuse with
short mucro often with pink tinge, margins involute,
sometimes with pink tinge, adaxial lamina green,
glossy, glabrous, primary vein slightly impressed drying
pink at base, secondary venation 6 14 pairs, not
prominent, tertiary venation conspicuous, abaxial
lamina pale green, glabrous, primary vein raised,
secondary veins slightly raised, tertiary vernation
conspicuous. Inorescences terminal compound cymes,
total inorescence length 21 48 mm; primary
inorescence unit 0.4 1.5 mm long, puberulent;
secondary inorescence unit 2.1 4.4 mm long,
puberulent; tertiary and quaternary inorescence
units pubescent, pink (Fig. 1). Bracts leaf-like in
morphology, located on primary and secondary ino-
rescence axis, variable, 3.3 12.5 mm long, 1.6
3.6 mm wide. Flowers 5-merous, actinomorphic, pinkish
when fresh, in groups of three. Hypanthium glabrous,
narrow, thinly walled, 1.5 4.7 mm long. Sepals highly
reduced and not discernible. Petals 5, slightly thick and
eshy, spathulate, 1.2 2.25 (4.0) mm long, 0.9
1.4 mm wide, apex with short mucro, glabrous, pale
yellow when dry. Scales located on the inside of petals,
0.35 1.2 mm long, 0.4 0.6 mm wide, densely
pubescent on both surfaces. Stamens all attached along
the same radius of inner hypanthium tube reaching
the mouth of the ower, anthers 0.55 0.6 mm long.
Ovary inferior, glabrous, 1.2 2.5 mm long, 5-locular;
style puberulent, shorter than the oral tube, approx.
0.6 mm; stigma globular. Galled owers somewhat
swollen but linear, 2.0 3.3 (3.9) mm long, 0.35
0.7 (1.65) mm wide, drying dark, without conspicuous
tubercles. Drupes globose, glabrous, ± 6.0 mm in diam.,
5-locular, pinkish, drying pale brown. Pericarp thinly
eshy, endocarp brown, woody, not smooth. Seeds
ellipsoid to horse-shoe shaped, smooth, with spiral
marking on the surface, ± 2.45 mm diam., usually only
one seed per fruit due to abortion of other ovules
(only immature seeds seen). Figs 1,2and 3.
RECOGNITION. Olinia chimanimani has previously been
confused with O. vanguerioides as their ranges overlap.
However, morphologically the two species are clearly
distinct. O. chimanimani can be distinguished by its
smaller leaf size ((19.0 ) 25.0 40.1 mm long), sessile
leaf attachment, and galled owers becoming thinly
swollen when infected, without prominent tubercles,
compared to O. vanguerioides which has larger (40.1
170.0 mm long), petiolate leaves and owers forming
conspicuous elongate-tuberculate galls when infected.
36 Page 2 of 7 KEW BULLETIN (2018) 73:36
© The Author(s), 2018
Additionally, O. chimanimani may be confused with
O. huillensis A. Fern. & R. Fern. and in particular with
subsp. discolor (Mildbr.) Sebola; however,
O. chimanimani differs from this taxon in having a leaf
texture that is strictly coriaceous, smaller leaves ((19.0
) 25.0 40.0 mm long) with a strictly sessile leaf
attachment, smaller petals (1.2 2.25 (4.0)) mm
long, 0.9 1.4 mm wide), glabrous inner and outer
petal indumentum and strictly glabrous hypanthium
indumentum (1.5 4.7 mm long). O. huillensis subsp.
discolor, on the other hand, has a variable leaf texture
of chartaceous to coriaceous, larger leaves (33
77 mm long) with short petiole (1.0 5.8 mm long),
larger petals ((1.0 ) 2.0 2.9 mm long, (1.2 ) 1.5
2.8 mm wide), pubescent inner petals often with stiff
hairs on the margin of the inner petal, and a
pubescent and larger hypanthium ((2.0) 4.5
7.0 mm long). Furthermore, the two taxa differ with
the gall formation of O. chimanimani having smaller
linear galls (0.35 0.7 (1.65) mm wide) and
O. huillensis subsp. discolor has rounded, more swollen
galls (1.2 2.1 mm wide). Table 1shows the diagnostic
characters to differentiate the two species and
O. huillensis A. Fern. & R. Fern. s.l., a key to species is
found in the Notes section.
DISTRIBUTION. Only known from Chimanimani Moun-
tains on the border of Zimbabwe and Mozambique
(Map 1).
SPECIMENS EXAMINED.MOZAMBIQUE. Chimanimani
Mts, riverine above Bundi R., galled . Dec. 1964,
Whellan 2203 (K!); Manica, Pedza (Peza) mountain in
Chimanimani, -19.74400, 33.99764, alt. 1887 m, fr., 18
April 2014, Matimele 2082 (K!, LMA); Manica,
Nhamudima mountain in Chimanimani, -19.75722,
33.09328, alt. 1673 m, . & fr., 21 April 2014, Matimele
2094 (K!, LMA); Chimanimani Mts, -19.75747,
33.09236, alt. 1702 m, 4 May 2016, Shah 007 (K!,
LMA, SRGH); Chimanimani Mts, -19.72530, 33.09201,
alt. 1786 m, 6 May 2016, Shah 013 (K!, LMA, SRGH);
Chimanimani Mts, -19.725195, 33.09177, alt. 1776 m, 6
May 2016, Shah 014 (K!, SRGH). ZIMBABWE. Mt Peza,
among crags, Chimanimani Mts, imm. & galled ., 15
Oct. 1950, Wild 3606 (K!); Manicaland, Chimanimani
Mts, W base of (Pnt.?) 71, ., 20 Nov. 1986, Linder 3990
(K! holotype).
HABITAT. This species is found growing in evergreen
scrub within rocky quartzite crags and gullies and at
the base of quartzite blocks on steep slopes, between
1500 1890 m elevation.
CONSERVATION STATUS. Olinia chimanimani is restricted
to the Chimanimani Mountains on the border of
central Zimbabwe and Mozambique and is currently
known from eight collections, with the estimated
Extent of Occurrence (EOO) and Area of Occupancy
(AOO) of 40 and 28 km
2
respectively (calculated using
Geocat 2015). Furthermore, the total area of
Chimanimani sandstone/quartzite is approximately
380 km
2
. Of this, the area covered by rocky quarzitic
crags and associated grassland, which is the favoured
habitat for this species, is approximately 270 km
2
; this
could be taken as the maximum possible AOO for this
species. The species is only known from two locations;
the Zimbabwean side of the Massif which is fairly well-
protected under the Chimanimani National Park
(CNP) and the Mozambique portion under the
National Reserve of Chimanimani (RNC) with limited
protection (Schneider et al.2005). Additionally, al-
though the species occurs in rocky crags, it is highly
prone to burning by man, associated with the illegal
artisanal mining activity present on the Mozambique
side of the Chimanimani massif (Dondeyne et al.
2009). This threat has signicantly declined since its
peak in 2004 2005, as gold discoveries have lessened
(Timberlake et al.2016). However, if it were to rise
again in the future, the increase of human habitation
would very likely lead to a further increased frequency
of res, which would almost certainly have an impact
upon the specieshabitat and number of mature
individuals. Severe re damage was observed on some
individuals in 2016. Furthermore, being one of the few
woody species occurring at a high altitude, it will burn
more easily and may be targeted as a fuel source for
the miners. The species was noted to be locally rare in
2016, and with a restricted distribution and a plausible
threat to its habitat, it is therefore assessed as
Endangered (EN B1ab(iii, v) + B2ab(iii, v)).
Fig. 1. Inorescence arrangement in Olinia species, adapted
from Sebola & Balkwill (2009).
Page 3 of 7 36 KEW BULLETIN (2018) 73:36
© The Author(s), 2018
Fig. 2. ANOlinia chimanimani:Ahabit; Bjuvenile shoot showing ternate leaf arrangement; Cabaxial leaf surface, conspicuous
venation, margins involute; Dstem with grooves; Eower; Fdissected ower with stamens, style and stigma, reexed scales,
internal view; Genlarged scale outer surface; Hanther, lateral view; Janther, face view; Kinfructescence; Lfruit cross-section; M
seed; Ngalled ower. A, C Jfrom Linder 3990, Bfrom Shah 007, KMfrom Matimele 2094, Nfrom Whellan 2203. DRAWN BY
ANDREW BROWN.
36 Page 4 of 7 KEW BULLETIN (2018) 73:36
© The Author(s), 2018
ETYMOLOGY. Olinia chimanimani is named for the only
mountain range on which the species occurs.
NOTES. This taxon is restricted to the higher elevations
of the Chimanimani Mountains. Although once
thought to be a pathological form of its close range
relative, Olinia vanguerioides by Verdcourt (1978)in
Flora Zambesiaca, it is now clear that it is morpholog-
ically distinct by having signicantly smaller leaves,
sessile leaf attachment, smaller owers and narrow,
linear galls that form without tubercles when infected
(Table 1). Additionally, Sebola & Balkwill (2009)
stated the presence of the variable taxon O. huillensis
Fig. 3. Mature fruits of Olinia chimanimani photographed in the Chimanimani Mountains. PHOTO:BART WURS TEN (http://
www.mozambiqueora.com).
Table 1. Comparison of diagnostic characters between Olinia chimanimani and two closely related species.
Characters Olinia chimanimani Olinia vanguerioides Olinia huilliensis s.l.
Leaf shape obovate to
oblanceolate
elliptic obovate (young) to elliptic
Leaf size (mm)(length) (19) 25 40.1 40.1 170 (29) 33 77
Leaf size (mm) (width) 10 25 20.2 44 15 29
Leaf texture coriaceous coriaceous chartaceous (sometimes coriaceous)
Leaf attachment sessile petiolate shortly petiolate
Leaf margin involute, glabrous involute, pubescent when young at to slightly involute, glabrous
Leaf lamina adaxial/ abaxial glabrous/ glabrous glabrous/ glabrous
(pubescent near petiole)
glabrous/ glabrous
Petal shape spathulate spathulate oblong
Petal apex mucronate truncate to shortly apiculate truncate
Petal size (mm) (length) 1.2 2.25 ( 4) 0.9 1.9 (1) 2 2.9
Petal size (mm) (width) 0.4 0.6 0.5 1.1 2 3.9
Petal indumentum inner/
outer surface
glabrous/ glabrous sparsely hairy (young)/ glabrous pubescent/ glabrous
Hypanthium length (mm) 1.5 4.7 1.5 526.4
Hypanthium surface glabrous glabrous pubescent
Gall formation narrow, linear elongate, tuberculate swollen, rounded
Page 5 of 7 36 KEW BULLETIN (2018) 73:36
© The Author(s), 2018
subsp. discolor in the Chimanimani Mountains. How-
ever, they did not cite any specimens of this taxon
from the Chimanimani Mountains, Mozambique or
Zimbabwe nor gave any indication of this on the
distribution map for subsp. discolor. It is possible that
the authors included this new taxon within the limits
of O. huillensis subsp. discolor, although the specimens
of the new taxon that were loaned to Sebola (J) at the
time of that revision were not annotated as such.
However, when closely examined, O. chimanimani
always has a strictly sessile leaf attachment, glabrous
inner and outer petals, a glabrous and smaller
hypanthium and linear gall formation, characters
that differ from O. huillensis including subsp.
discolor.Table1shows the morphological character
differences between O. chimanimani, O. vanguerioides
and O. huillensis s.l. because the delimitation of
O. huillensis subsp.discolormust necessarily t
within the larger taxonomic concept of
O. huillensis s.l. Therefore, the subspecies is not
included in the table in order to compare taxa at
the species level. With recent developments in
molecular analysis it would be desirable to carry
out Next Generation Sequencing (NGS) to more
accurately resolve the species limits within this
genus. However, at present, morphological analysis
provides the best conclusions for species delimita-
tion. A modied key to the species of Olinia sect.
Rochetiana is presented below to help with the
identication of the closely related taxa, a key to
the infraspecictaxaofO. huillensis s.l. is available
in Sebola & Balkwill (2013).
Key to taxa within Olinia sect. Rochetiana (adapted from Sebola & Balkwill 2009)
1. Leaf lamina narrowly elliptic, 40.1 170 × 20.2 44 mm; petioles puberulent, 6 9 mm long; galled owers
narrow with conspicuous elongate tubercles . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . O. vanguerioides
Leaf lamina obovate to oblanceolate, (19.0) 25 40.1 × 10 25 mm; leaves sessile or petioles < 6 mm long; galled
owers either swollen or if narrow and linear then lacking elongate tubercles . . . . . . . . . . . . . . . . . . . . . . 2
2. Leaf lamina with conspicuous reticulate venation on both surfaces; leaves strictly sessile; petals 0.35 1.2 × 0.4
0.6 mm, glabrous on both sides; hypanthium glabrous; galled owers narrow and linear . O. chimanimani
Leaf lamina with conspicuous reticulate venation on undersurface only; leaves shortly petiolate; petals 3 5×12mm,
pubescent on the inside or at least on petal margins; galled owersswollen........................... 3
3. Leaves somewhat chartaceous; up to 7 inorescence units along inorescence axes . . . . . . . . O. huillensis
Leaves coriaceous; between 9 11 inorescence units along inorescence axes . . . . . . . . . . . . . . . . . . . . 4
4. Leaf lamina discolorous, broader than long; internodes on terminal branches longer than inorescence
axes .............................................................. O. ruandensis
Leaf lamina concolorous, longer than broad; internodes on terminal branches shorter or equal to inorescence
axes ............................................................................ 5
5. Petals 5 on lateral owers;scalesshorterthan1mm,rarelysealingthehypanthiumopening/throat.... O. rochetiana
Petals 4 on lateral owers;scaleslongerthan1mm,oftensealingthehypanthiumopening/throat ....
................................................................... O. usambarensis
Acknowledgements
Research on the ora of the high Chimanimani
Mountains and its endemic species was supported by
the Critical Ecosystems Partnership Fund Grant 63512:
In from the cold: providing the knowledge base for
comprehensive biodiversity conservation in the Chimanimani
Mountains, Mozambique; botanical survey component
completed in 2016; see http://www.cepf.net/
SiteCollectionDocuments/eastern_afromontane/
FinalReport_RBC_ChimanimaniMountains.pdf.
Toral Shahs participation in the eld expedition to
the Mozambique Chimanimani in May 2016 was
supported by the Bentham-Moxon Trust. Joanna
Osborne, Jonathan Timberlake, Anthony Mapaura,
Aurelio Banze, Daglasse Muassinar, João Massunde,
Bart Wursten, Petra Ballings and all other participants
Map 1. Distribution of Olinia chimanimani in southeastern
Africa. Red triangle represents the cited collections.
36 Page 6 of 7 KEW BULLETIN (2018) 73:36
© The Author(s), 2018
are thanked for their collaboration in these eld
expeditions. We are grateful to the Micaia Foundation
for their support and collaboration on this project and
their logistical eld support. We also thank Andrew
Brown for the excellent illustration of the new species
and Bart Wursten for allowing us to use the photo-
graph of the new species.
Open Access This article is distributed under the
terms of the Creative Commons Attribution 4.0
International License (http://creativecommons.org/
licenses/by/4.0/), which permits unrestricted use,
distribution, and reproduction in any medium, pro-
vided you give appropriate credit to the original
author(s) and the source, provide a link to the
Creative Commons license, and indicate if changes
were made.
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© The Author(s), 2018
... The region is characterised by montane grasslands and ericaceous shrublands, as well as some patches of montane woodlands and moist, evergreen forests in its lower-lying parts (Childes and Mundy 2001). Additionally, the Chimanimani uplands are part of the Eastern Afromontane Biodiversity Hotspot (Shah et al. 2018) and it was recently declared a Biosphere Reserve (UNESCO 2022). The physical setting of the phytoregion favours plant diversity with more than 1000 plant species, of which 60 are endemic and are found mostly in the Chimanimani Mountains, Nyanga area, and Chirinda Forest. ...
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Biological invasions can have major social-ecological consequences for rural communities across the world. However, the dimensions (characteristics, infestation and socio-ecological impacts) of emerging invasive alien plants are often less known and urgent information is needed to guide policy and management. In light of this, this paper assesses the social-ecological impacts of Vernonanthura polyanthes, an emerging invasive alien plant found in a Zimbabwean upland landscape which supports conservation and livelihoods. The paper employs qualitative methods—community mapping, time series analysis, and key informant interviews—involving individuals from diverse socio-economic backgrounds, to examine the socio-ecological and economic implications of V. polyanthes and its management in Chimanimani, Zimbabwe. We found that there are nuanced perspectives regarding this invasive alien plant among different socio-economic groups in the region who have different experiences of living with V. polyanthes. Some are embracing it for apiculture, firewood, and ethnomedicine while, on the other hand, some see the tree as negatively affecting key livelihoods (crop farming, pastoralism, and tourism) that are common in the region. Local people also identified that V. polyanthes is associated with ecological impacts that include loss of biodiversity, promoting pests, and negatively affecting watersheds and associated water sources. These mixed experiences concerning the plant are leading to different management practices, in turn inducing some conflicts among various actors. Based on our findings, we suggest more should be done to better manage this invasive alien plant in the region before negative impacts become too great, particularly in protected areas.
... In the last 15 years this has changed to an upsurge in botanical exploration and discovery as reported in Cheek et al. (2018c). Since that date Olinia chimanimani T.Shah (Shah et al. 2018) from Chimanimani and Eriolaena rulkensii Dorr in the Dombeyaceae (Dorr & Wurdack 2018) from near Pemba in NE Mozambique have been published. The latter is the first time that a member of this genus, previously thought restricted to Asia, has been recognised in continental Africa. ...
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Cola cheringoma is described from the limestone gorge forest of the Cheringoma Plateau in Sofala Province of Central Mozambique. Tentatively treated previously as C. clavata Mast., it differs in being restricted to limestone substrate, the leaves drying white-green below (not on sandy soils, drying dark grey-brown). The tepal number of female flowers is 5 (not (5 –) 6), staminode number 5 (not 8), and the indumentum of the outer perianth covers only 50 – 60% of the surface with two distinct hair classes (not 100% coverage with a single hair type). The species is assessed as EN B2ab(iii) using the IUCN 2012 standard due to threats from the low number of locations, quarrying, and habitat modification. The Cola species growing in forest on limestone in tropical Africa are mapped and reviewed with respect to their status as obligate or facultative calcicoles, and with respect to their probable evolutionary origin. Based on morphological characters, adaptation to limestone habitats has probably occurred at least four times in the genus. Forests on limestone are rare and threatened in tropical Africa: only thirteen locations are known with certainty: these occur in Kenya (10 locations), Tanzania (2 locations) and Mozambique (1 location).
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The Chimanimani Mountains, located at the Mozambique-Zimbabwe border, are geologically unique in that they consist of quartzites giving rise to peaks and outcrops between zones of schist supporting grasslands. The nutrient-poor quartzitic soils house a high number of endemic plant species. One of these is Sericanthe chimanimaniensis, which is here described as new for science. We give a detailed description and distribution map, illustrations, information on ecology and phenology, and an assessment on the conservation status. An identification key to closely allied species is presented.
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Extending over 530 km 2 on both sides of the Mozambique-Zimbabwe border, and primarily defined by its underlying geology, the Chimanimani massif is renowned for its montane vegetation and a high number of endemic taxa. A detailed vascular plant checklist from the area above 1200 m altitude was produced by Goodier and Phipps in 1961, but focussed mostly on the Zimbabwe side. Here we present a revision of that checklist with updated nomenclature and family circumscriptions, incorporating many recent additional records particularly from Mozambique. It is recognised that a fully comprehensive list for the montane area on both sides of the border would probably use a lower limit of 800 m and cover moist forests in more detail. The revised checklist covers 977 taxa, 956 of them native, from 142 families (including ferns and gymnosperms); the 74 Chimanimani strict montane endemics, 7.7% of the flora, are indicated along with 19 near-endemic taxa. Comparison with checklists for other montane massifs in the Flora Zambesiaca area shows that the Chimanimani is not particularly species-rich, however it covers a smaller area with lesser altitudinal range. Despite the lower number of species recorded, the number of endemics on the Chimanimanis is significantly greater. Aspects of the botanical significance of the area are discussed.
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The biodiversity of the 5,000 km-long Great Escarpment of southern Africa is currently poorly known, despite hosting half of the subcontinent’s centres of plant endemism and to have a rich endemic vertebrate fauna, particularly in the north-west and east. A country-based overview of endemism, data deficiencies and conservation challenges is provided, with Angola being the country in most need of Escarpment research and conservation. Given that the Escarpment provides most of the subcontinent’s fresh water, protection and restoration of Escarpment habitat providing such ecological services is urgently required. Key research needs are exhaustive biodiversity surveys, systematic studies to test refugia and migration hypotheses, and the effects of modern climate change. Such research results can then be consolidated into effective conservation planning and co-ordinated international efforts to protect the rich biodiversity of the Escarpment and the ecological services it provides.
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This paper analyses current policy and legislation in relation to the praxis of artisanal gold mining in Mozambique. Approximately 20,000 people are involved in artisanal mining in central Mozambique, producing annually 480-600kg of gold, 85-90% of which remains in the informal economy. The current legislation, however, is inadequate: artisanal mining is supposed to take place in predetermined "designated areas", none of which are gold-rich, and, artisanal miners are supposed to get an individual mining pass from provincial authorities, which rarely occurs. Artisanal miners' associations get support from the Mining Development Fund. Yet, as these organisations are only viable where ore permits long lasting exploitation, their members represent less than 30% of the workforce. Hence the scope for improving miners' working conditions and limiting their environmental impact through this type of organisation is limited. On the other hand, siltation of rivers and their pollution with heavy metals goes unchecked while the prohibition of artisanal mining, in and around conservation areas has proven counterproductive. The design of more appropriate policies, particularly those pertaining to the environment, hinges upon a better understanding of the socio-economic dynamics of the sector.
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Empogona jenniferae is described from the upper quartzitic slopes of Mt Chimanimani on both sides of the Zimbabwe-Mozambique border, a prospective Tropical Important Plant Area. Its conservation status is assessed as Critically Endangered under the 2012 IUCN criteria. A figure and notes on the endemic plant species of Chimanimani are provided. Two additional names in Empogona, E. congesta and E. congesta subsp. chasei are published.
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An update of the Angiosperm Phylogeny Group (APG) classification of the orders and families of angiosperms is presented. Several new orders are recognized: Boraginales, Dilleniales, Icacinales, Metteniusiales and Vahliales. This brings the total number of orders and families recognized in the APG system to 64 and 416, respectively. We propose two additional informal major clades, superrosids and superasterids, that each comprise the additional orders that are included in the larger clades dominated by the rosids and asterids. Families that made up potentially monofamilial orders, Dasypogonaceae and Sabiaceae, are instead referred to Arecales and Proteales, respectively. Two parasitic families formerly of uncertain positions are now placed: Cynomoriaceae in Saxifragales and Apodanthaceae in Cucurbitales. Although there is evidence that some families recognized in APG III are not monophyletic, we make no changes in Dioscoreales and Santalales relative to APG III and leave some genera in Lamiales unplaced (e.g. Peltanthera). These changes in familial circumscription and recognition have all resulted from new results published since APG III, except for some changes simply due to nomenclatural issues, which include substituting Asphodelaceae for Xanthorrhoeaceae (Asparagales) and Francoaceae for Melianthaceae (Geraniales); however, in Francoaceae we also include Bersamaceae, Ledocarpaceae, Rhynchothecaceae and Vivianiaceae. Other changes to family limits are not drastic or numerous and are mostly focused on some members of the lamiids, especially the former Icacinaceae that have long been problematic with several genera moved to the formerly monogeneric Metteniusaceae, but minor changes in circumscription include Aristolochiaceae (now including Lactoridaceae and Hydnoraceae; Aristolochiales), Maundiaceae (removed from Juncaginaceae; Alismatales), Restionaceae (now re-including Anarthriaceae and Centrolepidaceae; Poales), Buxaceae (now including Haptanthaceae; Buxales), Peraceae (split from Euphorbiaceae; Malpighiales), recognition of Petenaeaceae (Huerteales), Kewaceae, Limeaceae, Macarthuriaceae and Microteaceae (all Caryophyllales), Petiveriaceae split from Phytolaccaceae (Caryophyllales), changes to the generic composition of Ixonanthaceae and Irvingiaceae (with transfer of Allantospermum from the former to the latter; Malpighiales), transfer of Pakaraimaea (formerly Dipterocarpaceae) to Cistaceae (Malvales), transfer of Borthwickia, Forchhammeria, Stixis and Tirania (formerly all Capparaceae) to Resedaceae (Brassicales), Nyssaceae split from Cornaceae (Cornales), Pteleocarpa moved to Gelsemiaceae (Gentianales), changes to the generic composition of Gesneriaceae (Sanango moved from Loganiaceae) and Orobanchaceae (now including Lindenbergiaceae and Rehmanniaceae) and recognition of Mazaceae distinct from Phrymaceae (all Lamiales).
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Morphological variation within the Oliniaceae is discussed with reference to diagnostic characters used to delimit species and infraspecific taxa. The Oliniaceae is hereby considered to comprise a single genus, Olinia Thunb. with ten species assigned to two sections: sect. Olinia, and sect. Rochetiana. The two sections are distinguishable on the basis of the pattern of leaf venation, shape of leaves and petals. Section Olinia comprises O. capensis, O emarginata, O. micrantha, O. ventosa, O. radiata and O. vanguerioides; whereas section Rochetiana includes O. huillensis, O. rochetiana, O. ruandensis and O. usambarensis. O. huillensis Welw. shows infraspecific variation categorised as O. huillensis subsp. huillensis, O. huillensis subsp. burttdavii and O. huillensis subsp. discolor occurring mainly in southern Africa. Floral features provide useful and reliable distinguishing characters that consistently separate taxa at specific and infraspecific ranks. In particular, the following features are taxonomically useful: flowers which are organised into either tightly compact inflorescences or loose and open inflorescences, floral whorls comprising either four or five units, and variation in the shape and length of petal lobes. A full taxonomic account of Olinia over its total geographic distribution is provided with an identification key, descriptions, illustrations and distribution maps for all recognised taxa.
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A checklist of vertebrates of Mozambique was elaborated by means of revision of monographic and web-based resources. During interviews of native speakers made in various parts of Mozambique, vernacular names of vertebrates in the 20 most important languages were assessed and included in the checklist as well as their common names in Portuguese and English. Additional information such as the category of Red List of threatened species, conservation status according to the Forest and Wildlife Law and Regulation of Mozambique, the Convention on the International Trade in Endangered Species of Flora and Fauna (CITES) and the Convention on Migratory Species (CMS) is provided. According to this analysis, 3470 vertebrate species occur in Mozambique, of which 271 (7.8%) species are mammals, 816 (23.5%) species of birds, 280 (8.0%) species of reptiles, 84 (2.4%) species of amphibians and 2019 (58.2%) species of fish. 503 vertebrate species are considered as threatened by extinction and protected by national and international legislation, i.e. 38.7% of the mammal species, 36.0% of the birds, 11.8% of the reptiles, 3.6% of the amphibians and 3.4% of the fish species. Mozambique has 234 endemic or near endemic species of vertebrates, which are 7.7% of the mammal species, 14.1% of the birds, 32.5% of the reptiles, 2.4% of the amphibians and 0.2% of the fish species. 20 (0.6%) vertebrate species were introduced into Mozambique, i.e. 1.1% of the mammals, 0.4% of the birds, 0.4% of the reptiles and 0.6% of the fish species. Digitizing, vectorization, georeferencing and processing of distribution maps using MapScan 1.0 and ArcView GIS 3.2 enabled the superposition of the distribution maps and the subsequent identification of diversity centres of vertebrates as well as 'hotspots' of endemic, threatened and protected terrestrial vertebrate species of Mozambique. In Mozambique, these conservation 'hotspots' generally occur in (i) the region of Mount Gorongosa -Rift Valley -Marromeu Complex in Sofala and Manica Provinces, (ii) the mountains of the Chimanimani region in Manica Province, (iii) along the Lebombo mountain range in Gaza and Maputo Provinces, (iv) along the coast of Inhambane, Gaza and Maputo Provinces, (v) the Mozambican part of Maputaland region in the south of Maputo Province, (iv) the region of Panda in Inhambane Province and (v) the Great Inselberg Archipelago in Zambézia and Nampula Provinces including Mount Chiperone and Mount Namúli. A comparison shows, that some conservation 'hotspots' are not adequately represented in the existing network of protected areas of Mozambique. These areas are the mountains in the north of the Chimanimani National Reserve in Manica Province, the coastal area north of Beira in Sofala Province, the coastal areas of Inhambane, Gaza e Maputo Provinces, the region of Panda in Inhambane Province as well as the Great Inselberg Archipelago in Zambézia and Nampula Provinces. The lack of information on the occurrence and distribution of vertebrates in Mozambique north of the Zambeze River greatly limited the identification of conservation 'hotspots' in this part of the country.
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Previous circumscriptions of Olinia rochetiana A. Juss. (Oliniaceae) presented a taxonomically variable and widespread species complex in central and tropical East Africa. Results of numerical phenetic analyses of morphological variation within O. rochetiana sensu lato indicate the existence of four taxa which are recognisable at specific rank corresponding to O. huillensis Welw. ex A. & R. Fern., O. ruandensis Gilg, O. rochetiana A. Juss. sensu stricto and O. usambarensis Gilg ex Engl. The analyses also indicate that O. huillensis, hitherto reported to occur only in Angola, occurs widely in southern Africa and shows geographic segregates characterised as O. huillensis Welw. subsp. huillensis, O. huillensis subsp. burttdavii Sebola and O. huillensis subsp. discolor Sebola (Map 2). The major delimiting characters were found to be the shapes of petals and leaves, presence or absence of indumentum and the degree of hairiness on floral parts, and the form of inflorescence units (i.e. being either compact or spreading). Phenetic and ecological concepts of species are applied at the specific and subspecific ranks, respectively. Keys to distinguish between the species and infraspecific taxa are presented, and full descriptions and citations of examined specimens are provided.