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Revista de Biología Tropical, ISSN electrónico: 2215-2075 Vol. 69(S1): 66-79, March 2021 (Published Mar. 30, 2021)
Feeding habits of Holothuria (Stauropora) fuscocinerea
(Echinodermata: Holothuroidea) in a Mexican Pacific reef
Brenda Maya-Alvarado
1,2
Laura Georgina Calva-Benítez
2
Rebeca Granja-Fernández
3
Jessica Pérez-López
2
Andrés López-Pérez
2
*
1. Programa de Maestría en Ciencias en Biosistemática y Manejo de Recursos Naturales y Agrícolas, Centro
Universitario de Ciencias Biológicas y Agropecuarias, Universidad de Guadalajara, Av. Ing. Ramón Padilla Sánchez,
Zapopan, Jalisco, México; brenda.maya9471@alumnos.udg.mx
2. Laboratorio de Ecosistemas Costeros. Departamento de Hidrobiología, Universidad Autónoma Metropolitana Unidad
Iztapalapa, Av. San Rafael Atlixco, Col. Vicentina, Iztapalapa, Ciudad de México, México; cblg@xanum.uam.mx,
je_si13@hotmail.com, alopez@xanum.uam.mx (*Correspondence).
3. Laboratorio de Ecología Marina. Centro Universitario de la Costa, Universidad de Guadalajara, Av. Universidad,
Puerto Vallarta, Jalisco, México; beckygranja@gmail.com
Received 01-VI-2020. Corrected 10-IX-2020. Accepted 07-X-2020.
ABSTRACT
Introduction: The importance of holothuroids in marine ecosystems is related to their feeding activities, which
have been little studied in the eastern Pacific. Objective: To describe the feeding habits of the sea cucumber
Holothuria (Stauropora) fuscocinerea and their bioturbation potential in La Entrega reef, México. Methods:
The population size of H. (Stauropora) fuscocinerea was determined by means of four 20 x 4 m (320 m
2
) band
transects, while the available sediment for the sea cucumbers and their feces were characterized in three stations
(A-C) via granulometry and quantification of organic carbon and organic matter. Excretion rate was determined
every 4 hr over a 24 hr period and the relationship between sea cucumber length and biomass and the excretion
rate evaluated. Results: According to non-parametric permutation, ordination and percentage similarity analy-
ses, sea cucumber feces mostly comprised a large proportion of small grains compared to the available sediment,
indicating that H. (Stauropora) fuscocinerea is selective on grain size. Preliminary bioturbation potential of the
species may reach up to 8.71 ± 0.17 kg day of sediment in the study area. Conclusion: The spatial distribution
of H. (Stauropora) fuscocinerea in the study area is a product of its selective feeding activity, evidencing the
preliminary importance of the species in the trophic dynamics of La Entrega reef.
Key words: selectivity; distribution; food; bioturbation; sea cucumber.
Maya-Alvarado, B., Calva-Benítez, L.G., Granja-
Fernández, R., Pérez-López, J., & López-Pérez, A.
(2021). Feeding habits of Holothuria (Stauropora)
fuscocinerea (Echinodermata: Holothuroidea) in a
Mexican Pacific reef. Revista de Biología Tropical,
69(S1), 66-79. DOI 10.15517/rbt.v69iSuppl.1.46328
Holothuroids, commonly known as sea
cucumbers, are conspicuous and abundant
invertebrates that contribute largely to the bio-
mass of marine ecosystems (Hendler, Miller,
Pawson & Kier, 1995). As a result of their
feeding activity and diet, they can bioturbate
large amounts of sediments every year (i.e.
Crozier, 1918; Bonham & Held, 1963; Bakus,
1973; Uthicke, 1999; Purcell, Conand, Uthicke
& Byrne, 2016), contributing to important
DOI 10.15517/rbt.v69iSuppl.1.46328
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Revista de Biología Tropical, ISSN electrónico: 2215-2075, Vol. 69(S1): 66-79, March 2021 (Published Mar. 30, 2021)
chemical and physical processes on the sea-
floor, and promoting the continuous mixing
of the sediment particles (Thayer, 1983). Sea
cucumbers actively participate in the recycling
of nutrients and organic matter within marine
ecosystems (Bakus, 1973; Calva-Benítez,
2002), including coral reefs (Goldberg, 2013;
Sheppard, Davy, Pilling & Graham, 2017).
Despite being conspicuous and abundant
in coral reefs around the world (Sheppard et
al., 2017), the study of their feeding habits
and their importance in sediment bioturbation
in tropical reefs has focused mostly on holo-
thuroids from the Indo-Pacific (Yang et al.,
2005; Bucol, Cadivida & Wagey, 2018; Rioja,
Palomar-Abesamis & Juinio-Meñez, 2020).
Those studies have highlighted the selective
nature of the feeding habits of holothuroids,
as well as their capacity to remove large
amounts of sediment and the wide spatial and
temporal variation that exists among species
(Trefz, 1956; Glynn, 1965; Bakus, 1968, 1973;
Uthicke, 1999; Mezali & Soualili, 2013; Bel-
bachir, Mezali & Soualili, 2014).
Holothuria (Stauropora) fuscocinerea is
among the most common and widely dis-
tributed holothuroid in the Indo and eastern
tropical Pacific (Purcell, Samyn & Conand,
2012; Solís-Marín et al., 2013; Cortés et al.,
2017). However, little is known about its
biology, abundance and distribution, feeding
habits and generally, the role that this species
plays in the ecosystem. To date, the only study
of the species in the region is limited to its
annual reproductive periodicity on the coast
of Oaxaca, México (Benítez-Villalobos, Avila-
Poveda, & Gutiérrez-Méndez, 2013). In the
Mexican Pacific and the Gulf of California, sea
cucumbers such as Isostichopus fuscus (Herre-
ro-Pérezrul & Chávez, 2005) and Holothuria
(Halodeima) inornata are regularly exploited
commercially and are currently under the pro-
tection of Mexican laws (SEMARNAT, 2019).
On the other hand, H. (Stauropora) fuscoci-
nerea, is of commercial importance in China,
Malaysia and the Philippines (Purcell et al.,
2012), but lacks protection status in México.
Due to the paucity of information about the
species, its commercial importance and the rel-
evance of holothuroids for bioturbation in reef
ecosystems, this study aims to: a) determine the
feeding habits of H. (Stauropora) fuscocinerea
in a tropical reef in the Mexican Pacific, and b)
address their bioturbation potential. With this
information, inferences can be made in terms
of its small-scale distribution, along with its
feeding selectivity and its contribution to sedi-
ment bioturbation in a typical reef system of
the eastern tropical Pacific.
MATERIALS AND METHODS
Study area: The study was carried out at
La Entrega bay (15°44’34’ N & 96°07’35’ W),
located in southwest end of the Gulf of Tehu-
antepec, Oaxaca, México (Fig. 1). La Entrega
is a small (0.1 km
2
) embayment located on the
west side of Santa Cruz bay. The seafloor of La
Entrega consists of marine carbonate sediment
mixed with siliciclastic material derived from
the basaltic highlands of the Copalita river
basin (Estrada-Vargas, 2008). The center of
La Entrega is largely covered by an approxi-
mately 4.3 ha reef framework that follows a
southwest-northeast direction and reaches 12
m in depth (Glynn & Leyte-Morales, 1997).
The coral community is composed by 11 coral
species, live coral cover comprises 76.58 %
of the reef area, while the framework is built
mainly by Pocillopora spp. species (> 95 %),
followed by Pavona spp. and Porites pana-
mensis (López-Pérez & López-García, 2008;
Cabral-Tena et al., 2020).
The southwestern portion of the reef cor-
responds to the reef flat (2-5 m in depth) and
comprises most of the reef framework, while
the fore reef comprises ~ 30 % of the area.
While the former results of the interlocking of
Pocillopora spp. colonies, the fore reef area
is a transition zone where live coral cover
is severely reduced (~ 70 %) and branch-
ing Pocillopora spp. and the massive corals
Pavona gigantea and Pavona varians coexist
with the emerald coral P. panamensis, along
with sparse patches of sand and dead corals
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(Glynn & Leyte-Morales, 1997; López-Pérez
& Hernández-Ballesteros, 2004) (Fig. 1).
La Entrega reef is habitat of several marine
invertebrates, including echinoderms (López-
Pérez et al., 2019). Among the echinoderm
species, the sea cucumber H. (Stauropora) fus-
cocinerea is mainly distributed in the fore reef
transition zone between the reef flat and the
sandy area (transition zone A), as well as in the
live coral-coral rubble (zone B) but absent in
the sand area (C) (Fig. 1). Finally, La Entrega
has been subjected to intense touristic activity
and recurrent dredging at least yearly since the
early 1990’s, which has resulted in high quanti-
ties of organic matter, therefore diminishing the
health of the system (López-Pérez & Hernán-
dez-Ballesteros, 2004; Díaz-Díaz, 2017).
Fieldwork: The population density of H.
(Stauropora) fuscocinerea (Fig. 2A) in La
Entrega was determined during SCUBA div-
ing visual censuses, using four 20 x 4 m (320
m²) belt transects. During January 2018, visual
census was conducted at two stations parallel
to the coastline, called A and B, at a depth of
10 m (Fig. 1).
The available sediment was collected in
situ near the mouth and feces near the anus
of 20 specimens of H. (Stauropora) fuscoci-
nerea (Fig. 2A, 2B, 2C), randomly selected in
each of the stations A and B, in which coral
sand (A) and coral debris (B) predominate
(Fig. 1). The samples were collected manu-
ally with a plastic spoon, placed in individual
Fig. 1. Sampling stations (A, B, C [experimental cages]) and zoning of La Entrega reef, Mexican Pacific. See text for
information regarding sampling stations.
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sealable plastic bags, and stored frozen until
subsequent processing.
Furthermore, individuals of H. (Stauro-
pora) fuscocinerea were placed in individual
enclosures (one individual per enclosure, ten
enclosures) at station C in order to measure the
rate of excretion of the cucumbers over a total
period of 24 h. These enclosures were con-
structed of wire rod and cloth mesh and were 1
m in diameter (Fig. 3); on the upper and lateral
part, each enclosure was covered with the cloth
mesh, while the lower part allowed H. (Stau-
ropora) fuscocinerea to feed on the sediment.
The enclosures were anchored to the bottom to
prevent escape of the organisms. In each con-
finement, the feces of sea cucumbers were col-
lected at 4 h intervals over a 24 h period (T1 =
21:40 hr; T2 = 1:40 hr; T3 = 5:40 hr; T4 = 9:40
hr, T5 = 13:40 hr; T6 = 17:40 hr; T7 = 21:40
hr). In order to characterize the sediments from
which the sea cucumbers were feeding in each
enclosure, three sediment samples from each
enclosure (3 x 10 enclosures, N = 30) were col-
lected at the beginning (T1) of the experiment.
The collected fecal and sediment samples were
placed in individual sealable plastic bags and
stored at low temperature (≈ 4 °C) until subse-
quent analysis in the laboratory.
Finally, the length of the individuals that
remained in the enclosures was measured with
a metric tape (length/width) every 4 h and this
parameter was related to the wet weight, which
was obtained 90 seconds after removing the
animals from the water (Uthicke, 1999) at the
end of the experiment, using an Oahus CR2200
balance (± 1 g precision).
Laboratory work: Samples (sediment
and feces) were thawed, placed on aluminum
trays and dried at room temperature until dry.
Sediment texture analysis was then performed
and the content of organic carbon (O.C.) and
organic matter (O.M.) determined.
Granulometric analysis was performed
using the dry sieving technique. The dry
weights of the following fractions were deter-
mined: granules (2 000 µm), very coarse sand
(1 000 µm), coarse sand (500 µm), medium
sand (250 µm), fine sand (125 µm), very fine
sand (62.5 µm), and silt (28 µm).
The O.C. content was determined using the
technique proposed by Gaudette, Flight, Toner
& Folger (1974), which consists of drying the
sediments at room temperature and then siev-
ing them to remove gravel through a 62.5 µm
mesh (0.500 g of it is treated). The organic mat-
ter is then oxidized, and the excess potassium
dichromate titrated with ferrous sulfate. The
samples were analyzed in duplicates and two
blanks processed in the same way as controls.
With this technique, the presence of carbonates
does not produce interference, has an accuracy
of ± 0.25 %, and yields solid results (Shoham-
Frider et al., 2020). In addition, the technique
has been successfully used to evaluate the abil-
ity of holothuroids to remove organic matter
Fig. 2. A. Holothuria (Stauropora) fuscocinerea. B. Feces of Holothuria (Stauropora) fuscocinerea. C. Close-up feces.
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in eutrophic and hypereutrophic environments
(Emiroglu & Günay, 2007).
Finally, the organic matter (O.M.) con-
tent was estimated as the product of the O.C.
using the van Bemmelen factor (1.72; Grybos,
Davranche, Gruau & Petitjean, 2007) who
assume that, on average, 58 % of the O.M. is
composed of carbon.
Data analysis: In order to graphically
represent the relationships between sediment
samples and feces from the three stations (A, B,
C), the database (size fractions + O.C. + O.M.)
was analyzed using a principal components
analysis (PCA) from a normalized matrix.
Since PCA is an ordination technique and
does not have an associated statistical hypoth-
esis, statistical differences between sediment
and feces were evaluated using a permutations-
based unbalanced factor analysis of variance
(PERMANOVA). The stations (A, B, C) were
considered as a fixed factor (type I model).
The PERMANOVA was constructed from a
Euclidean distance matrix following the criteria
of Anderson, Gorley & Clarke (2008). Non-
parametric analysis was performed since data
did not meet the assumptions of normality and
homoscedasticity.
In order to explore the degree of selectivity
of the individuals during the feeding process, a
Fig. 3. Experimental cages used in the field study during January 2018. La Entrega reef, Mexican Pacific.
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percentage similarity test (SIMPER) was car-
ried out with the aim of estimating the similar-
ity/dissimilarity of the available sediment and
feces among the sampling stations, and also to
identify which variables contributed the most
to explaining these compositional differences.
Simple linear regression models were per-
formed to establish a relationship between the
length of the individuals and the biomass, as
well as between the length and dry weight
of the feces. On the other hand, in sampling
station C, it was evaluated if there were dif-
ferences in the excretion rate over time using
a one-way non-parametric analysis of variance
(ANOVA) with fixed effects. Finally, the pre-
liminary bioturbation potential of the species
in the study area was estimated considering
population density, the area inhabited, and the
excretion rate by H. (Stauropora) fuscocinerea
in La Entrega.
PCA, PERMANOVA and SIMPER were
performed using the PRIMER 6 + PER-
MANOVA software (Anderson et al., 2008).
The regression models and the non-parametric
ANOVA were carried out in the STATISTICA
v.7.1 software (Statsoft, 2020). All statistical
tests used α = 0.05.
RESULTS
Density and individual size: Holothu-
ria (Stauropora) fuscocinerea distribute dif-
ferentially across space in La Entrega reef. The
species is absent from the Pocillopora spp.
interlocking patch and the sandy area (0.0 ind/
m
2
), but in the transition and live coral/coral
rubble area may reach an average of 0.27 ind/
m
2
(± 0.02). Additionally, individuals had an
average length of 24.60 cm (± 5.77) and an
average weight of 142 g (± 41.64).
Sediment and feces composition: Sedi-
ment and feces composition of H. (Stauropora)
fuscocinerea for each sampling station are
presented in Table 1, and PCA ordination sum-
marize the trends among sediment and feces,
but also among stations.
From sampling station A to C, there is
an increase in large size fractions of sediment
(granule-very coarse sand), while the opposite
trend is recorded for coarse sand to fine sand
fractions, including organic carbon and matter;
meanwhile, for very fine sand and silt fractions,
large values were recorded in station B, fol-
lowed by station A and C, respectively (Table
1). The observed trend in sediment composition
(granulometry, C.O., and M.O.) across space
is supported by permutational analysis of vari-
ance (Pseudo-F
(2,26)
= 6, P = 0.0001); according
to the analysis, differences in sediment compo-
sition occurred among station A and C (Pseudo-
t = 2.81, P = 0.0008), and C and B (Pseudo-t
= 3.42, P = 0.0001), while sediment compo-
sition between station A and B is relatively
homogeneous. In station C, the sediments are
characterized by granules, very coarse sands
and coarse sands with O.C. content of 0.33
% and O.M. content of 0.56 % (Table 1). In
stations A and B, in addition to their O.C. and
O.M. characteristics, the sediments are highly
heterogeneous among samples within the same
station which translates in the wide overlap in
the characteristics between stations A and B
(Pseudo-t = 1.52, P = 0.07; Table 1, Fig. 4).
Regarding feces, for granules and silt,
station B had larger values than station A, fol-
lowed by station C; for very coarse sand and
coarse sand, station C showed larger values
than station B, followed by station A; finally,
for medium sand and fine sand fractions, feces
in station A showed larger values than stations
C and B, respectively (Table 1). Feces com-
position show a relative homogeneity among
samples from the same station (Fig. 4), and the
overlap between stations is relatively smaller,
suggesting there is less variation among feces
than among the sediment available to sea
cucumbers in each sampling station. In general,
the feces from station A are characterized by
their content of medium sand, coarse sand, fine
sand and very coarse sand along with moder-
ate values of O.C. (0.70 %) and O.M. (1.21
%) (Table 1). The feces from station B are
characterized by very coarse sand, granules,
coarse sand, medium sand, and relatively high
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O.C. (1.04 %) and O.M. (1.8 %) values, while
those at station C are dominated by very coarse
sand, coarse sand, medium sand, and relatively
low O.C. (0.51 %) and O.M. (0.87 %) values
(Table 1, Fig. 4).
Size selection of sediment particles: The
PERMANOVA indicated that there were differ-
ences between sediment and feces composition
in stations B (Pseudo-t = 1.90, P = 0.01) and C
(Pseudo-t = 2.74, P = 0.0007), but not between
Fig. 4. Ordination (Principal Components Analysis) of sediment (open figures) and feces (filled figures) composition across
space in La Entrega reef, Mexican Pacific. Sampling stations, A = green, B = blue, C = red. See Figure 1 for spatial location
of sampling stations. Vector longitude = relative importance of the variable in the ordination. OM = Organic matter, OC =
Organic carbon, G = Granule, VCS = Very coarse sand, CS = Coarse sand, MS = Medium sand, S = Sand, FS = Fine sand,
VFS = Very fine sand, S = Silt.
TABLE 1
Percentage of size fractions, organic carbon and organic matter of available sediments and feces
of Holothuria (Stauropora) fuscocinerea in La Entrega reef, Mexican Pacific
Size fraction
Sediment Feces
A B C A B C
Granule 12.81 ± 9.75 23.91 ± 7.82 36.28 ± 7.26 5.84 ± 8.78 26.62 ± 15.44 3.05 ± 1.59
Very coarse sand 17.08 ± 10.39 21.61 ± 6.34 27.65 ± 3.4 10.06 ± 12.27 28.1 ± 8.17 35.03 ± 11.04
Coarse sand 34.66 ± 10.45 29.76 ± 4.21 26.58 ± 6.05 23.45 ± 11.82 23.55 ± 6.94 29.52 ± 3.12
Medium sand 28.52 ± 14.86 18.35 ± 9.43 8.44 ± 3.95 36.55 ± 14.85 12.05 ± 4.03 22.2 ± 8.18
Fine sand 6.2 ± 6.34 4.65 ± 2.23 1 ± 0.5 19.68 ± 12.68 5.2 ± 2.8 6.23 ± 4.28
Very fine sand 0.57 ± 0.6 1.13 ± 0.42 0.01 ± 0.02 3.51 ± 2.7 3.04 ± 1.47 3.97 ± 3.3
Silt 0.16 ± 0.19 0.59 ± 0.47 0.04 ± 0.11 0.91 ± 1.45 1.44 ± 1 0.0 ± 0.0
Organic carbon 0.73 ± 0.71 0.63 ± 0.42 0.33 ± 0.19 0.70 ± 0.37 1.04 ± 0.42 0.51 ± 0.5
Organic matter 1.26 ± 1.22 1.09 ± 0.73 0.56 ± 0.33 1.21 ± 0.65 1.8 ± 0.73 0.87 ± 0.86
Values represents mean ± standard deviation. See Fig. 1 for location of sampling stations (A, B, C).
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the available sediments and feces from station
A (Pseudo-t = 0.86, P = 0.54). The statistical
differences observed between sediment and
feces at each station are clearly depicted by the
spatial distance between the open and filled
figures in the PCA ordination in stations B and
C (Fig. 4).
The SIMPER analysis between the char-
acteristics of the available sediment and feces
showed that the greatest differences in the
composition occurred in station C, followed by
station A, and finally station B (Table 2). The
difference between the sediment characteristics
of the feces and those of the available sedi-
ment had a relationship presenting the lowest
percentage of large sand grains (granules, very
coarse, coarse and medium sand), the highest
percentage of small grains (fine and very fine
sands, and silts), a higher percentage of O.C.
with respect to the available sediment in sta-
tions A and B, and a lower percentage of O.M.
and O.C. compared to that of the available sedi-
ment in station C (Table 2).
Sediment bioturbation: According to
data, H. (Stauropora) fuscocinerea bioturbated
0.1 g ind
-1
hr
-1
(± 0.15); across time, Kruskal-
Wallis test evidenced differences in bioturba-
tion (H
(5,57)
= 19.73, P = 0.001) between T1
(0.01 g ind
-1
hr
-1
± 0.04) and T2 (0.0 g ind
-1
hr
-1
± 0.0), regarding T4 (0.21 g ind
-1
hr
-1
± 0.21)
(T1 vs T4, H = 3.09, P = 0.03; T2 vs T4, H =
3.29, P = 0.01).
The simple regression model showed no
relationship between the sea cucumber length
and biomass (R² = 0.09, N = 10, P > 0.05), nor
between the length and weight of feces (R² =
0.08, N = 10, P > 0.05); therefore, available
data did not support that the amount of sedi-
ment that H. (Stauropora) fuscocinerea biotur-
bates through feeding activity varies according
to the size of the organism.
Finally, considering the population density
of the species obtained through visual censuses
(0.27 ± 0.02 ind m
-2
), the extension of the sta-
tions A (10 211 m2) and B (4 200 m
2
), and the
average bioturbation rate per sea cucumber per
TABLE 2
Summary of SIMPER results for feeding habits of Holothuria (Stauropora) fuscocinerea
in La Entrega reef, Mexican Pacific
Variable Av. Sediment Av. Feces Contribution %
Station A
Average squared distance = 2.05 x 10
8
O.M. 9.8 x 10
-3
1.1 x 10
-4
91.4
Station B
Average squared distance = 1.51 x 10
8
O.M. 6.42 x 10
-3
1.2 x 10
-4
94.59
Station C
Average squared distance = 8.73 x 10
8
Medium sand 3.16 x 10
-14
1.12 x 10
-14
18.27
O.C. 2.56 x 10
-14
2.32 x 10
-14
15.93
O.M. 3.02 x 10
-14
2.42 x 10
-14
15.51
Very fine sand 8.15 x 10
-13
1.88 x 10
-14
14.38
Fine sand 1.15 x 10
-14
1.77 x 10
-14
14.30
Granule 1.78 x 10
-14
1.58 x 10
-14
9.23
Very coarse sand 1.77 x 10
-14
7.65 x 10
-13
5.43
Average contribution (Av. %) of discriminating sedimentary characteristics in each sediment availability and feces group,
their contribution (%) to the dissimilarity between groups, and cumulative total (%) of contributions (90 % cut-off). O.C. =
organic carbon; O.M. = organic matter.
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day (2.24 ± 3.71 gr ind
-1
day), it is estimated
that 8.71 ± 0.17 kg of sediment in a single day
was bioturbated during the feeding activity of
the H. (Stauropora) fuscocinerea population in
the study area.
DISCUSSION
Studies addressing sediment composition
in eastern Pacific reef systems are scarce
(Estrada-Vargas, 2008; Granja-Fernández &
López-Pérez, 2008; Díaz-Díaz, 2017), while
the effect of sediment characteristics in the
distribution of organisms at small spatial scales
has been exclusively studied in asteroids (Luna-
Salguero & Reyes-Bonilla, 2010) and molluscs
(Barrientos-Lujan et al., 2019). In the same
way, the results of the present research indicate
that the spatial distribution of the sea cucumber
H. (Stauropora) fuscocinerea in La Entrega
reef is closely tied to sediment size distribution
and the amount of organic material associated
with very fine sand and silt fractions. Accord-
ing to data, the species selectively feeds on
sand in the transition zone, collecting sediment
and particles from the seabed with its mouth
tentacles. As a result of these feeding habits,
the species is generally found where granules,
very coarse sands or coarse sands represent less
than 30 % of the sediment, and where the pres-
ence of silts and very fine sands range from 0
to 4 %. Moreover, it is generally found where
the average O.C. content ranges 0.707-1.02 %
and O.M. averages 1.22-1.75 %. Consequently,
H. (Stauropora) fuscocinerea is distributed in
the transition area between the reef patch and
the adjacent sand (i.e. stations A and B), while
its presence is null on corals or in sites where
coarse and very coarse sands are the main
components (i.e. station C). This agrees with
the results of Bakus (1973), who states that
detritivores holothuroids predominate in fine
sediments, Yamanouchi (1939) who observed
that the population density of the sea cucumber
Bohadschia vitiens was lower where live corals
were abundant because there was a low pres-
ence of sand, and Massin & Jangoux (1976)
who indicated that Holothuria (Holothuria)
tubulosa lives exclusively in sandy sediments
and in the absence of a hard substrate. In
summary, the results of the present and afore-
mentioned studies indicate a close relationship
between sedimentary characteristics and the
distribution of holothuroids at small spatial
scales. This distribution could not only be
influenced by the proportion and size of the
sediments, but also by their nutritional value.
In detritivores holothuroids, the relation-
ship between sediment characteristics and the
distribution of organisms is closely related to
the selective feeding habits of the sea cucum-
bers (Massin & Jangoux, 1976; Hammond,
1983; Uthicke, 1994). Results related to the
spatial distribution of H. (Stauropora) fusco-
cinerea individuals within the reef, the large
percentage of smaller sediment fractions (fine
sands to silts) found in the feces compared
to the sediment available in the environment
(Table 1, Fig. 4) and the significant statistical
differences between the composition of the
feces and the available sediments, strongly sup-
ports the selective feeding habits of H. (Stauro-
pora) fuscocinerea in the study area. According
to both, the permutation analysis and SIMPER,
the greatest difference between sediment and
feces was found in station C, where there was
a lesser order of magnitude with very coarse
sands, fewer granules and medium sand. A
higher percentage of fine and very fine sand
in the feces of H. (Stauropora) fuscocinerea
(Table 2), suggested selectivity of small size
sediment fractions as observed in the Holothu-
ria (Roweothuria) poli sea cucumber (40-200
µm) (Mezali & Soualili, 2013; Belbachir et al.,
2014), as well as in Astichopus multifidus that
feeds on fine-grained calcareous sediments
(250 μm) (Glynn, 1965). The fine to very fine
fractions found in H. (Stauropora) fuscocinerea
feces, which were common in the sediments of
stations A and B but scarce in the sediments
of station C, possess a high concentration of
organic matter since the sorption capacity
and the surface-volume ratio increases in fine
fractions (Berthois, Crosnier & Le Calvez,
1968; Poppe, Knebel, Mlodzinska, Hastings &
Seekins, 2000). It seems feasible to suggest that
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Revista de Biología Tropical, ISSN electrónico: 2215-2075, Vol. 69(S1): 66-79, March 2021 (Published Mar. 30, 2021)
H. (Stauropora) fuscocinerea spatial distribu-
tion is related to the ability of the holothuroids
to locate patches enriched with organic matter
and to the efficiency of food assimilation, intes-
tinal transit time, and the cost of rejecting par-
ticles in these organisms, known as “Optimal
Food Theory” (Taghon, Self & Jumars, 1978;
Billet, Llewellyn & Watson, 1988).
Through their activities of ingestion and
excretion, holothuroids are known to be impor-
tant recyclers of nutrients in reef systems by
converting organic nutrients bound to sedi-
ments into inorganic nutrients dissolved in the
water column (Uthicke, 1999), and further into
biomass in upper trophic levels or as nutrients
that increase primary productivity (Purcell et
al., 2016). Although feces may be enrichened
in nutrients through their transit in the sea
cucumber gut (e.g. Massin, 1979; Hammond,
1983; Amon & Herndl, 1991), most of the time
when sediments pass through the intestines of
holothuroids, the defecated sediments can be
lower in nutrients than the ingested sediments,
and thus these organisms act as sediment-clean-
ers (Longbottom, 1970; Mercier, Battaglene &
Hamel, 1999; Uthicke, 1999; Michio et al.,
2003; Yuan et al., 2006; Zhou et al., 2006), and
have been considered as a means of restricting
or reversing the effects of pollution from aqua-
culture (Slater & Carton, 2009). Emiroglu &
Günary (2007), for example, suggested that H.
(Holothuria) tubulosa can eliminate biological
pollution and improve water quality in eutro-
phic and hypereutrophic environments of the
coastal regions. In this regard, heavily tourist
visits to coastal reef areas such as La Entrega
(FONATUR, 2008), where large amounts of
organic matter have been recorded (Díaz-Díaz,
2017) may benefit from H. (Stauropora) fusco-
cinerea presence and feeding activity.
Holothuroids actively ingest sediments,
but present varied feeding rates since they
are capable of feeding either continuously
(Yamanouchi, 1956; Bonham & Held, 1963;
Massin & Jangoux, 1976; Hammond, 1982;
Uthicke, 1994) or discontinuously within a
24 h cycle (Crozier, 1918; Bakus, 1968; Mas-
sin & Jangoux, 1976). The feeding rates of
holothuroids is related to light intensity, varia-
tions in temperature, and other environmental
conditions such as water movement (Massin &
Jangoux, 1976; Uthicke, 1994). According to
Massin and Jangoux (1976), H. (Holothuria)
tubulosa is a continuous feeder that, in sum-
mer, increases its feeding activity at night and
decreases it during the day, while juveniles
of Holothuria (Metriatyla) scabra feed con-
tinuously (Mercier et al., 1999). In the present
study, differences in the excretion rate in a 24 h
cycle were recorded; according to data, larger
excretion rates occurred early in the morning
probably related to intense feeding activity
during the night (Crozier, 1918; Bakus, 1968;
Massin & Jangoux, 1976), but also may have
resulted from changes in feeding activity of the
experimental organisms since they were relo-
cated to experimental cages in areas where H.
(Stauropora) fuscocinerea does not currently
distribute. More data, nevertheless, are needed
to accurately assess daily and seasonal feeding
rates changes in the species.
Concurrently, while some authors (Cro-
zier, 1918, Isostichopus badionotus; Ruiz,
Ibáñez & Cáceres, 2007, Athyonidium chilen-
sis) observed a relationship between the total
length of the holothuroids and the average
weight of the full alimentary tract, such that
the total length of the intestine increased with
the size of this species, results in La Entrega
indicated a lack of length-weight and weight-
excretion rate relationships in H. (Stauropora)
fuscocinerea individuals. Therefore, our results
should be considered with caution since sea
cucumber size is strongly subjected to changes
in response to handling or its resting state
(Ebert, 2021) and sample size may be insuf-
ficient to address meaningful relationships if
any. Preliminary data, nevertheless, may give
us insight on the bioturbation potential of
H. (Stauropora) fuscocinerea in the studied
area. If it is assumed that all H. (Stauropora)
fuscocinerea individuals in La Entrega have
similar sizes and weights, and hence feed-
ing rates are homogeneous among individu-
als, H. (Stauropora) fuscocinerea population
may have had the potential to bioturbate 8.71
76
Revista de Biología Tropical, ISSN electrónico: 2215-2075 Vol. 69(S1): 66-79, March 2021 (Published Mar. 30, 2021)
± 0.17 kg day of sediment over 14 411 m
2
corresponding to the area where the species
currently occurs in La Entrega reef. Prelimi-
nary bioturbation potential of H. (Stauropora)
fuscocinerea addressed in the studied area is
smaller than that reported for other species.
Coulon and Jangoux (1993) obtained different
values for the lower and upper part of the algal
grasslands of Lacco Ameno (Italy), at 5.9 and
12.9 kg of dry sediment per year, respectively;
while Uthicke (1999) showed that H. (Halo-
deima) atra removes up to 24.5 kg of sediment
per year and Stichopus chloronotus removes
21.5 kg per year at Lizard Island (Great Bar-
rier Reef). In order to establish meaningful
comparison with other studies, strong empirical
information regarding size-related bioturba-
tion changes, size-frequency distribution of
individuals, population size and their variation
across time are mandatory. It should be noted
that this study addressed the preliminary bio-
turbation potential of H. (Stauropora) fuscoci-
nerea, while the importance of other abundant
and widespread species such as Isostichopus
fuscus and Holothuria (Halodeima) inornata
remains unquantified. Addressing the bioturba-
tion potential of sea cucumbers without doubt,
it is of relevance for understanding the impor-
tance of the guild in the functioning of coastal
systems, particularly in reef systems with high
organic load such as those located on the east-
ern tropical Pacific.
Ethical statement: authors declare that
they all agree with this publication and made
significant contributions; that there is no con-
flict of interest of any kind; and that we fol-
lowed all pertinent ethical and legal procedures
and requirements. All financial sources are
fully and clearly stated in the acknowledge-
ments section. A signed document has been
filed in the journal archives.
ACKNOWLEDGMENTS
We are thankful to Buceo Huatulco for
logistical support in the field, particularly to
Carlos (Papi) Armería and to Tania (Torcy)
González for addressing reef size. This work
was conceived and carried out by the Reef
and Biodiversity Laboratory (ARBIOLAB)
in collaboration with the Coastal Ecosystem
Laboratory. The work was carried out with
funds from the Universidad Autónoma Met-
ropolitana and CONACYT (236654) granted
to ALP and LGCB. We thank four anonymous
reviewers and editor for commenting and
improving the manuscript.
RESUMEN
Hábitos alimenticios de Holothuria (Stauropora)
fuscocinerea (Echinodermata: Holothuroidea) en
un arrecife del Pacífico Mexicano
Introducción: La relevancia de los holoturoideos en
los ecosistemas marinos está relacionada con sus activida-
des alimenticias, las cuales han sido escasamente estudia-
das en el Pacífico oriental. Objetivo: Describir los hábitos
alimenticios del pepino de mar Holothuria (Stauropora)
fuscocinerea y su potencial de bioturbación en el arrecife
La Entrega, México. Métodos: Se determinó el tamaño
poblacional de H. (Stauropora) fuscocinerea mediante
cuatro transectos de banda de 20 x 4 m (320 m
2
), mientras
que la caracterización de los sedimentos disponibles y las
heces de los pepinos se realizó en tres estaciones (A-C)
mediante granulometría y cuantificación de carbono orgá-
nico y materia orgánica. Se determinó la tasa de excreción
cada 4 hr durante un periodo de 24 hr y se evaluó la rela-
ción entre la talla y la biomasa con la tasa de excreción.
Resultados: De acuerdo con un análisis no paramétrico
mediante permutaciones, ordenación y similitud, las heces
de los pepinos estuvieron compuestas en su mayoría por
una gran cantidad de granos pequeños en comparación
con el sedimento disponible, lo que sugiere que H. (Stau-
ropora) fuscocinerea es una especie selectiva respecto al
tamaño de grano. El potencial de bioturbación preliminar
de la especie puede alcanzar 8.71 ± 0.17 kg día en el área
de estudio. Conclusiones: La distribución espacial de H.
(Stauropora) fuscocinerea en el área de estudio es producto
de su selectividad alimenticia, evidenciando la importancia
de la especie en la dinámica trófica del arrecife La Entrega.
Palabras clave: selectividad; distribución; alimento; bio-
turbación; pepino de mar.
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