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BRAZILIAN JOURNAL OF OCEANOGRAPHY, 65(1):79-96;2017
Quesada-Silva et al.: Impact of terrigenous input on Polychaeta
79
Looking at the soft-bottom around a coastal coral reef: the impact of
terrigenous input on Polychaeta (Annelida) community
Erosion on coral reefs produces fragments of the
constructor organisms that are scattered all around,
thus enlarging the reef boundaries. Statistical
modelling approach was used to investigate whether
the Polychaeta community around Sebastião Gomes
sediment characteristics and/or by position related to
the reef, that are variables related to the terrigenous
coastal reefs, sediment samples were taken on four
transects perpendicular to the reef (S, W, N and E) and
The most abundant species was the carnivorous
Goniadides carolinae and the model selected for
total macrofauna and polychaete abundance. These
models represented higher abundance in coarse
carbonate sediments on windward reef faces, where
there is almost no terrigenous sediment. On the other
hand, the Polychaeta richness did not depend on the
transects. Sebastião Gomes reef is one of the many
coastal reefs from Abrolhos Bank, whose healthy is
probably in danger because of the increase of mud
related to human activities, as deforestation and,
recently, mining waste.
AbstrAct
Michele Quesada-Silva*, Ana Maria Setubal Pires-Vanin
Descriptors: Sebastião Gomes, Abrolhos Bank,
Macrobenthos, Statistical modelling.
Fragmentos dos recifes de coral constituem parte do
sedimento ao redor dos mesmos, ampliando os limites
do recife. Modelos estatísticos foram criados para
recife Sebastião Gomes (Banco dos Abrolhos, Brasil)
recifes, amostras de sedimento foram coletadas em
foi o carnívoro Goniadides carolinae e o modelo
selecionado para descrever a distribuição desta espécie
foi muito semelhante aos ajustados tanto para a
modelos apresentaram alta abundância em sedimentos
pela posição dos transectos. Sebastião Gomes é um
dos muitos recifes costeiros do Banco dos Abrolhos,
relacionada a atividades humanas, como desmatamento
e, recentemente, rejeitos da mineração.
resumo
Descritores: Sebastião Gomes, Banco dos Abrolhos,
Macrofauna bentônica, Modelagem estatística.
BJOCE
BRAZILIAN JOURNAL OF OCEANOGRAPHY, 65(1):79-96;2017
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80
INTRODUCTION
reef structure. They are autogenic engineers as they change
the conditions of the physical environment (e.g., current
speeds and sedimentation rates) by means of their own
algae, and destruction via physical and biological erosion
produces fragments of the constructor organisms that are
scattered around the reefs, thus enlarging their boundaries
around reefs, few research projects have investigated the
community ecology of the macrofauna in reef complexes.
macrofauna of reef complexes started, the main aim has
reef habitats (pools, lagoons or the sublittoral zone around
more on biological interactions, while larger commonly
macrofauna. Another less studied aspect is the variability
of the composition and distribution of the macrofauna due
to its position in relation to the reef, in other words, as to
of macrobenthic species found throughout the oceans
respect, the scavengers are the main organisms responsible
for stimulating the biogeochemical processes of nutrient
ecosystem constitutes the community structure, while the
description of species traits is related to the functional
approach is now being increasingly used, mainly when
applied to studies of community responses to disturbances
better understand the dynamics of ecosystem functioning
has been considered a proxy to simplify the understanding
of the functional groups (functional community), even
knowing that the assumption includes other factors such
as mobility of organisms for instance, which is related to
The statistical modelling approach was selected to
investigate whether the structure and function (trophic
habit) of the polychaete community around a coastal reef
sediment characteristics and by position in relation to the
reef or exclusively by one or other. We have also sought to
polychaetes corresponds to that of the total macrofauna,
in order to verify the viability of the use of Polychaeta
as a good indicator of the macrofaunal patterns in reef
sediments. The focus on sediment characteristics was
sedimentation rates may be higher than the maximum of
day
Studies of the statistical modelling of marine
spatial and temporal patterns in benthic communities
are well suited to statistical modelling too. According
distribution of invertebrates that, in general, disperse less
to model the habitat preference of a Polychaeta species
indicated the need of further research into the modelling
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81
species through descriptive models so as later to be able
to create predictive models, important tools for ecosystem
management and conservation.
MATERIAL AND METHODS
The Abrolhos Bank is situated on the East Brazilian
) and
climate is characterized by two main seasons, summer and
winter. During summer, winds are N/NE and mean water
wind direction changes to S/SE due to the Atlantic Polar
is terrigenous (siliciclastic), whilst around the reefs it is
carbonate, and a mix of both types occurs between the reef
cm day
The Sebastião Gomes reef complex is located in the
river mouth, and is part of the Ponta da Baleia/Abrolhos
Marine Protected Area. This reef was chosen because
it lies inside the area with the highest sedimentation
polychaete community.
were placed at increasing distance from the reef, and up to
in the laboratory, under the stereomicroscope and the
sediment to analyze grain size and percentages of total
organic matter (TOM) and carbonates. Grain size, which
is a variable related to the interstitial space available to
the fauna, was determined using sieving and pipetting
variable related to reef origin of sediments, was determined
modelling approach based on maximum likelihood was
(predictor variables) on the macrofauna and Polychaeta
community (response variables). The law of likelihood
states that there are many models (hypotheses) which may
explain the response variable and that each one has some
probability of occurring, and, further, that the model with
the distance between the proposed model and the true
likelihood and the number of parameters of the model.
reef distance on community, the sedimentary variables
reef, sediment should be more carbonate and coarser
due to fragments of corals, resulting in more interstitial
a high content of TOM, a food resource for macrofauna
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82
Figure 1. Location of Abrolhos Bank on the East Brazilian continental shelf (a) and
sample stations around Sebastião Gomes reef (b).
models, one of whose premises is that predictor variables
must be independent, in this study. Because of this, score 1
these variables was used to represent the sediment and
only the distance between sample stations and the reef
as predictor variable was also created to verify whether
unrelated to sediment.
The generalized linear models created to test whether
sediment and/or the position in relation to the reef (on
transects S, W, N and E) are predictor variables of
community distribution patterns were based on negative
binomial probability distribution. Some ecologists have
realized that count data of aggregate organisms are better
omnivores, species which have two or more feeding
habits. This same study was used to classify species
according to the feeding habit of their families, but
sediment (Sed) and/or transect (Tr) as predictor variables
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Table 1. Distance from the reef, depth and geographic coordinates of sediment samples around Sebastiao Gomes reef complex.
Transect Station Distance (m) Depth (m) Latitude (S) Longitude (W)
S 1
S
S
S
S
S
W
W
W
W
W11
W
N
N
N
N
N
N 11
E
E
E
E
E
E
Figure 2. Schematic representation showing how interstitial space for
macrofauna inhabits increases with grain size.
(trophic groups).
RESULTS
The sediment distribution pattern corresponded to
expectations, i.e., near the reef, sediment contained
more carbonate and was coarser, except on transect S
variance of the data and its positive values (hereinafter
referred to as the “Sed” variable) represented carbonate
sediment stations near the reef while the negative values
were recorded, respectively, in transects S, W, N and
other two transects (S and N) it was more uniform along
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Figure 3.
Figure 4.
variables of soft bottom around Sebastião Gomes reef.
which considers only sediment as a predictable variable.
Both abundances of macrofauna and polychaetes were
as with the sediment characteristics, those of transect S
explain the distribution of macrofauna and polychaetes
took sediment and transect (position in relation to reef)
associated with coarser carbonate sediment of the N and E
With regard to the total abundance of polychaetes,
the most abundant species were Goniadides carolinae
Aphelochaeta Leodamas
treadwelli Lumbrineris cf. tetraura
abundance of polychaetes around Sebastião Gomes reef,
but only the model selected for G. carolinae was similar
of the phylum Annelida. The most plausible model to
explain the distribution pattern of G. carolinae presented
did total abundance model, but in this case, transect N
was more favorable to this species and no individual was
abundant species, L. treadwelli, sediment with an additive
Aphelochaeta sp. and L. cf.
tetraura were sampled at almost all stations on all four
transects, but only occurred in much greater abundance at
We chose not to calculate models to describe
most abundant species, Goniadides carolinae, represented
for carnivore polychaetes was the additive between the
variables “Sed” and “Tr”, with higher abundance in the
coarser sediments on all the transects, mainly to the north
at one station on each transect, though positioned at
DISCUSSION
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Table 2.
Family Species Stations
Ampharetidae Amphicteis sp.
Amphinomidae Eurythoe complanata
Amphinomidae Linopherus ambígua
Capitellidae sp.1
Capitellidae
Dasybranchus caducus
Mediomastus sp.
Neopseudocapitella brasiliensis
Notomastus hemipodus
Notomastus lobatos
Scyphoproctus sp.1
Scyphoproctus
Scyphoproctus
Bhawania brunnea
Aphelochaeta sp.
Caulleriella sp.1
Caulleriella
Caulleriella cf. apícula
Caulleriella cf. pacica
Chaetozone cf. armata
Chaetozone sp.1
Chaetozone
Monticellina sp.
Cossura sp.
Dorvilleidae Meiodorvillea sp.
Dorvilleidae Schistomeringos pectinata
Eulepethidae Grubeulepis mbriata
Eunicidae Eunice cf. vittata
Eunicidae Euniphysa sp.
Eunicidae Lysidice hebes
Eunicidae Marphysa sp.
Eunicidae Palola sp.
Fabriciidae Fabriciola sp.
Fabriciidae Novafabricia sp.
Fauveliopsidae Fauveliopsis sp.
Flabelligeridae Pherusa sp.
Goniadidae Goniadides carolinae
Lumbrineridae Lumbrineriopsis cf. mucronata
Lumbrineridae Lumbrineris sp.
Lumbrineridae Lumbrineris cf. tretaura
Lumbrineridae Ninoe brasiliensis
Magelonidae Magelona nonatoi
Magelonidae Magelona papillicornis
Magelonidae Magelona posterolongata
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Maldanidae Maldanidae sp.1
Maldanidae Maldanidae
Nephtyidae Aglaophamus juvenalis
Nephtyidae Aglaophamus uruguayi
Nereididae Ceratocephale oculata
Nereididae Neanthes bruaca
Nereididae Nereididae sp.1
Nereididae Nereididae
Nereididae Nereididae
Nereididae Nereis lanai
Nereididae Nereis serrata
Nereididae Nicon sp.1
Nereididae Nicon
Onuphidae Diopatra sp.1
Onuphidae Diopatra
Onuphidae Diopatra tridentata
Onuphidae Kinbergonuphis sp.1
Onuphidae Kinbergonuphis
Onuphidae Kinbergonuphis cf. fauchaldi
Onuphidae Kinbergonuphis cf. orensanzi
Opheliidae Armandia maculata
Opheliidae Ophelina cylindricaudata
Opheliidae Ophelina sp.
Opheliidae Polyophthalmus pictus
Orbiniidae Scoloplos agrestis
Orbiniidae Scoloplos (Leodamas) rubra
Orbiniidae Leodamas treadwelli
Oweniidae Owenia sp.
Paraonidae Aricidea sp.
Paraonidae Aricidea (Aricidea) albatrossae
Paraonidae Aricidea (Acmira) catherinae
Paraonidae Cirrophorus americanos
Paraonidae Cirrophorus branchiatus
Paraonidae Levinsenia cf. gracilis
Paraonidae Paradoneis lyra
Pectinariidae Pectinariidae sp.1
Pectinariidae Pectinariidae
Pholoididae Pholoe sp.
Phyllodocidae Phyllodoce sp.
Pilargidae Ancistrosyllis jonesi
Pilargidae Ancistrosyllis sp.
Pilargidae Cabira incerta
Pilargidae Litocorsa sp.
Pilargidae Sigambra sp.
Polynoidae Eunoe serrata
Polynoidae Harmothoe cf. aculeata
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Polynoidae Malmgreniella cf. macginitiei
Polynoidae Ysideria sp.
Sabellariidae Sabellaria sp.
Sabellidae Amphicorina sp.
Sabellidae Amphiglena sp.
Sabellidae Pseudobranchiomma sp.
Serpullidae Salmacina sp.
Sigalionidae Fimbriosthenelais marianae
Sphaerodoridae Sphaerodoropsis sp.
Spionidae Aonides mayaguezensis
Spionidae Laonice sp.
Spionidae Microspio sp.
Spionidae Prionospio sp.
Spionidae Prionospio heterobranchia
Syllidae Exogone sp.1
Syllidae Exogone
Syllidae Exogone
Syllidae Exogone arenosa
Syllidae Exogone díspar
Syllidae Exogone simplex
Syllidae Odontosyllis aracaensis
Syllidae Perkinsyllis biota
Syllidae Perkinsyllis augeneri
Syllidae Sphaerosyllis piriferopsis
Syllidae Syllis cf. botosaneanui
Syllidae Syllis cf. cruzi
Syllidae Syllis garciai
Syllidae Syllis gracilis
Syllidae Syllis lutea
Syllidae Syllis magellanica
Terebellidae Polycirrus cf. tenuiseti
Figure 5. Distribution pattern of Polychaeta richness around Sebastião Gomes reef (circles are
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Table 3.
Gomes reef, as well as patterns of the most abundant species (Goniadides carolinae, Aphelochaeta sp., Leodamas treadwelli
and Lumbrineris cf. tetraura
Total
Macrofauna
Total polychaetes Omnivores
Model Par
Null
Dist
Sed 342.3 0.0
Tr
NA NA
739.9 0.0 572.9 0.0 431.8 0.0 439.2 0.0 343.1 0.8
Polychaeta richness Goniadides carolinae Aphelochaeta sp. Leodamas treadwelli Lumbrineris cf. tetraura
Model Par
Null
Dist
Sed 394.4 1.2
Tr 177.8 0.0 238.2 0.0
179.1 1.3 238.8 0.6
393.3 0.0 166.8 0.0 178.3 0.5 244.1 0.0 238.2 0.0
associated with the intense hydrodynamics which occur
station immediately adjacent to face S (station 1) was
deposit them at the base of reef face S. Nevertheless,
during summer, station 1 was composed of thick and
carbonate sediment (unpublished data), in agreement with
the above postulate.
Percentages of carbonates were calculated for the
entire sample sediment and not for each grain fraction,
ergo, it is impossible to know if all the fractions contain
of the hypothesis of resuspension of sediments to the south
which is the main suspended mineral around Sebastião
and so, higher values of TOM were found at stations with
of food resources for polychaetes.
generated by winds and determine the sediment deposition
so transects N and E lie to windward.
Biodiversity Assessment, which consisted in six small
Piromis robertii, family Flabelligeridae
Polychaeta family with the largest number of species
the most richness families were Nereididae, Sabellidae
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Figure 6. Distribution patterns of macrofauna (a) and polychaete (c) abundance around Sebastião Gomes reef
small size of the species of this family, we recommend
that people who work with reef sediment has redoubled
attention during the sorting process.
the coarse carbonate sediment is responsible for the
distribution. The two richest transects were W and E, so
and leeward reef faces.
macrofauna and total polychaetes around Sebastião
Gomes reef was composed of higher percentages of
the present results show that the distribution is more
related to grain size than to grain composition. Studies
carried out with ecosystems without carbonate sediments
have shown higher abundance of macrofauna in coarser
related to an increased availability of interstitial space
composition of coarse grains underlines the importance
of fragments from coral reefs for the establishment of an
abundant macrofauna around coral reefs, mainly in coastal
higher abundance of total macrofauna and polychaetes on
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Figure 7. Distribution patterns of Goniadides carolinae (a) and Leodamas treadwelli (c) around Sebastião Gomes
to these latter authors, winds generate topographically
controlled currents that aggregate zooplankton near the
planktonic larvae, so these currents could prevent the
spread of the species.
species, the distribution of the most abundant polychaete
Goniadides carolinae was similar to that of the total
macrofauna and of the total polychaetes. G. carolinae is
greater abundance in coarse sediments was probably related
to high abundance of macrofauna prey items at these sites.
Leodamas treadwelli was the only case whose selected
the general distribution pattern of total polychaetes is not
the same for all abundant polychaete species. L. treadwelli
the literature does not indicate any grain size preference of
L. treadwelli
on the Abrolhos Bank, although other species of the genus
Scoloplos (previous genus of L. treadwelli) are commonly
No distribution pattern was determined for the
Aphelochaeta sp. and despite its being
records of Aphelochaeta are reported for Brazil, none for
Aphelochaeta
their few taxonomic characters. One of the characteristics
of the species of this family is that they succeed in
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Figure 8. Distribution of Aphelochaeta sp. (a) and Lumbrineris cf. tetraura (b) around Sebastião
Figure 9.
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occupying any kind of sediment through employing
food with their palps or directly with the mouth while
enables them to feed while remaining buried, protecting
themselves from physical disturbance and predation.
oxygenated sediments.
As well as Aphelochaeta sp., the last species studied
Lumbrineris cf. tetraura did not present any distribution
pattern in the Sebastião Gomes reef complex. The same
result was also found in an investigation conducted in a
present study, the high abundance of L. cf. tetraura was
found at the station most abundant in total polychaetes,
which might be an indication of a high number of prey items
macrofauna, their distribution pattern is representative
of that of the global macrofauna, which reinforces the
idea that the taxon can be properly taken to represent
the general distribution pattern of the macrofaunal
the most abundant species studied, it is interesting to note
that only G. carolinae followed the same pattern as the
total polychaetes and that other abundant species even
to highlight that further research into the behavior and
feeding habits of these species of polychaetes is essential
to understand their distributions.
The carnivores represented the commonest trophic
habit in view of the great abundance of Goniadides
carolinae and Lumbrineris cf. tetraura, which resulted in
the selection of a model similar to that for G. carolinae but
are common in coarse sediments, where interstitial space
is greater and allows the simultaneous presence of both
important group, although they can generally be the
Aphelochaeta
Leodamas treadwelli
Aricidea albatrossae Magelona papillicornis
and Aricidea catherinae
expected that their distribution would be similar to the
model selected for L. treadwelli.
occur and our results were similar to those of others who
feeders can change their habit, feeding on suspended
matter when this supply increases, as the species of the
apud
to the input of recent detritus from plankton that sinks
Leodamas treadwelli
abundance of these two trophic groups has also been
them. The presence of carnivores can reduce competition
size and allowing the coexistence of species of the same
trophic habit. Thus perhaps L. cf. tetraura is playing this
role on transect E.
expected near the reef, where seaweeds are more abundant.
The presence of exclusively herbivorous polychaetes in
Even in studies on polychaetes associated with algae,
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no one family of polychaetes is exclusively herbivorous.
considered omnivores.
expected for species that can change their trophic habit
in accordance with the available food resource and adapt
representatives around Sebastião Gomes reef were few.
similar to those for macrofauna and total Polychaeta
favored by coarse grains and transects related to windward
the fauna, but reef sediment did. This conclusion arises
by polar fronts.
Ecological studies of marine communities through the
approach (e.g., multiple linear regression and p
Generalized linear models (glm) and model selection
the present study showed the same patterns of abundance
as do classic studies based on multivariate analysis of
which do not depend of the Gaussian distribution of
itself to be a useful method to the study of descriptive
patterns of macrofauna community and should be used
more often, once variables as macrofauna abundance
and richness usually do not present Gaussian distribution
even after logarithmic transformations. We also highlight
distribution of macrofauna through descriptive models
to then create predictive models based on environmental
changes, which are important for the management and
conservation of reef complexes.
experiencing its worst environmental disaster, which
is related to the Samarco mining waste dam collapse
in direction to Abrolhos Bank and reached the area in
the reefs, the abundance and the diversity of macrofauna
community can decrease dramatically, and the coastal
Bank. This work is the most detailed study in Sebastião
Gomes reef and we think that these results, previous
monitor the area.
These results also can be used in others researches
related to environmental disturbances, as climate change
may be one of the most impacted marine ecosystems
builders, e.g., by carbonate dissolution and the decrease of
mainly that in coarse sediments.
ACKNOWLEDGMENTS
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is part of the interdisciplinary project called “Productivity,
sustainability and utilization of the Abrolhos Bank
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