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Coral boring Aka-species (Porifera: Phloeodictyidae) from Mexico with description of Aka cryptica sp. nov

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This paper focuses on Aka species boring coral of the East Pacific Ocean and the Caribbean Sea (Mexico). The new species Aka cryptica sp. nov. is described from Mexican Pacific coral reefs, which constitutes the first time that a species of the genus Aka is reported from the East Pacific Ocean. The new species lives cryptically boring coral species of the genus Pocillopora. It is characterized by the small size of their papillae (from 1 to 4.5 mm high and from 0.8 to 1.8 mm in diameter), and oxeas (from 67 to 120 μm), and their exposed parts blend in well with background colours which tend to be overlooked during benthic marine surveys. In addition, Aka coralliphaga and Aka brevitubulata from Mexican Caribbean coral reefs are redescribed. The latter species is reported for the first time in Mexico.
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J. Mar. Biol. Ass. U.K. (2007), 87, 1477–1484
Printed in the United Kingdom
Journal of the Marine Biological Association of the United Kingdom (2007)
doi: 10.1017/S0025315407055373
Coral boring Aka-species (Porifera: Phloeodictyidae) from Mexico
with description of Aka cryptica sp. nov.
This paper focuses on Aka species boring coral of the East Pacific Ocean and the Caribbean Sea (Mexico).
The new species Aka cryptica sp. nov. is described from Mexican Pacific coral reefs, which constitutes the f irst
time that a species of the genus Aka is reported from the East Pacific Ocean. The new species lives cryptically
boring coral species of the genus Pocillopora. It is characterized by the small size of their papillae (from 1 to 4.5
mm high and from 0.8 to 1.8 mm in diameter), and oxeas (from 67 to 120 µm), and their exposed parts blend
in well with background colours which tend to be overlooked during benthic marine surveys. In addition,
Aka coralliphaga and Aka brevitubulata from Mexican Caribbean coral reefs are redescribed. The latter species is
reported for the first time in Mexico.
INTRODUCTION
The genus Aka Laubenfels, 1936 comprises a small group
of excavating sponges living in calcareous substrata, with a
skeleton formed only by oxeas, and characterized by fistulose
tubes which are externally visible (Desqueyroux-Faúndez &
Valentine, 2002).
The genus was originally included in the family
Clionaidae (Hancock, 1849), but it was later moved to the
family Phloeodictyidae by Rützler & Stone (1986), who
recognized characters described for Siphonodictyon Bergquist,
1965 and consequently referred Aka as a senior synonym of
Siphonodictyon. Even though there is still some debate as to
the validity of this synonymy (see for example Desqueyroux-
Faúndez & Valentine, 2002), we considered it valid until
more information is available.
Aka-species bore calcitic substrata such as mollusc shells,
but they have also been described as an important agent
of destruction of coral reef ecosystems in the Indo-Pacific
(Bergquist, 1965; Thomas, 1968, 1973) and Caribbean areas
(Rützler, 1971; Pang, 1973). Cliona-species usually infest the
non-living basal parts of corals and only harm the living
colony if the attachment is weakened and the coral breaks
loose (Goreau & Hartman, 1963). In contrast, the genus
Aka attacks living corals and harms the polyps (Goreau &
Hartman, 1963; Rützler, 1971).
These species have been reported from different localities
in the Caribbean, West Africa, Mediterranean, Atlantic
coast and central Pacific (Johnson, 1899; Laubenfels, 1954;
Thomas, 1968; Fromont, 1993; Desqueyroux-Faúndez &
Valentine, 2002), but curiously, no present records of Aka
exist in the north-eastern Pacific Ocean, since the only
reference found is about a fossil Aka in Arizona (USA)
(Reitner & Keupp, 1991).
The eastern Pacific Ocean has been explored for boring
sponges for several years now and this has provided a general
vision of the diversity and distribution of this very important
sponge group in the area (Carballo et al., 2004; Carballo
& Cruz-Barraza, 2005; Bautista-Guerrero et al., 2006).
This paper focuses on Aka-species boring coral reefs species
from the East Pacific Ocean and the Caribbean (Mexico).
Three species were identified; Aka cryptica sp. nov., in the
Pacific Ocean and Aka coralliphaga (Rützler, 1971) and Aka
brevitubulata (Pang, 1973), in the Caribbean; the latter species
is reported for first time in Mexico. This is the first time that
a species of the genus Aka has been reported from the East
Pacific Ocean.
MATERIALS AND METHODS
The material was collected by SCUBA diving along the
Pacific and Caribbean coast of Mexico. Sampling locations
are presented in Figure 1.
The specimens were preserved with their coral substrate
in 10% formalin for 24 hours and later transferred to 75%
ethanol for storage. External morphology such as colour,
texture and size of the papillae, skeletal elements and
their arrangement were recorded for each species. Spicule
preparation for light microscopy (LM) involved dissolving
sponge tissue in 60% nitric acid, rinsing with water,
dehydrating in ethanol and mounting in Canada balsam.
Spicule measurements were obtained from a minimum of
25 spicules chosen at random for each specimen. Length,
width of oxeas were measured under light microscope. Coral
José Luis Carballo*, Leanne Hepburn, Héctor H. Nava*, José Antonio Cruz-Barraza*
and Eric Bautista-Guerrero*
*Instituto de Ciencias del Mar y Limnología, (Estación Mazatlán), Universidad Nacional Autónoma de México,
Apartado postal 811, Mazatlán 82000, México. Department of Biological Sciences, University of Essex,
Wivenhoe Park, Colchester, CO4 3SQ, UK. Corresponding author, e-mail: jlcarballo@ola.icmyl.unam.mx
1478 J.L. Carballo et al. Coral boring Aka-species from Mexico
Journal of the Marine Biological Association of the United Kingdom (2007)
pieces were broken and examined in detail for excavating
patterns. Scanning electron micrographs (SEM) were made
on sodium hypochloride-cleaned limestone coral skeletons.
The specimens examined were deposited in the Museo
Nacional de Ciencias Naturales (MNCN; Madrid, Spain),
Natural History Museum (BMNH; London, UK), in the
Colección de Esponjas of the Instituto de Ciencias del Mar
y Limnología, Universidad Nacional Autónoma de México
(LEB-ICML-UNAM), (Mazatlán, México).
SYSTEMATICS
Order HAPLOSCLERIDA Topsent, 1928
Family PHLOEODICTYIDAE Carter, 1882
Genus Aka de Laubenfels, 1936
Diagnosis
Excavating sponges boring calcitic substrata. Spicules are
oxeas forming sinuous bands arranged in bundles, producing
fistulose tubes. Externally visible by their fistulose tubes.
Skeleton formed only of spicule-bundles in sinuous bands,
not in a network, lining walls of fistules. Spicules short,
slender, curved oxeas. Without microscleres (Desqueyroux-
Faúndez & Valentine, 2002).
Acca Johnson, 1899: 461 (preoccupied)
Aka de Laubenfels, 1936: 155; Thomas, 1968: 250; Rützler
& Stone, 1986: 663; Reitner & Keupp, 1991: 102.
Aka cryptica sp. nov.
(Figures 2–4)
Material examined
Holotype: [MNCN 1.01/363]. Bahía de San Agustín
(Huatulco, Oaxaca), 15°41'09"N 96°13'46"W; 6 m depth; 09
May 2005.
Paratypes: [BMNH 2006.6.30.1]. Bahía de La Entrega
(Huatulco, Oaxaca), 15°44'34"N 96°07'35"W; 6 m depth;
04 July 2005. Specimen excavating alive and dead Pocillopora
damicornis colonies. LEB-ICML-UNAM-1196; Bahía de San
Agustín (Huatulco, Oaxaca), 15°41'09"N 96°13'46"W; 7 m
depth; 09 May 2005. Specimen excavating alive and dead
Pocillopora damicornis colonies. LEB-ICML-UNAM-1233;
Bahía de La Entrega (Huatulco, Oaxaca), 15°44'34"N
96°07'35"W; 6 m depth; 04 July 2005. LEB-ICML-UNAM-
1325; Cerro Pelón (Isla Isabel), 21°51'21"N 105°52'42"W; 21
m depth; 28 October 2005. Specimen excavating alive Pavona
sp. colonies. LEB-ICML-UNAM-1328; Antiguo Corral del
Figure 1. Sampling localities (letters) and distribution of the Aka-species along the coast of Mexico (numbers in parentheses) (1) Aka
cryptica sp. nov.; (2) Aka brevitubulata; (3) Aka coralliphaga.
Journal of the Marine Biological Association of the United Kingdom (2007)
1479Coral boring Aka-species from Mexico J.L. Carballo et al.
Risco (Punta Mita, Nayarit), 20°46'20"N 105°32'49"W; 2 m
depth; 18 March 2006. Specimen excavating alive and dead
Pocillopora verrucosa colonies. LEB-ICML-UNAM-1340; Isla
Cacaluta (Huatulco, Oaxaca), 15°43'08"N 96°09'43"W; 3 m
depth; 04 July 2005.
Description
Boring sponge found within corals, visible externally only
by the presence of erect, hollow fistules from 1 to 4.5 mm high
and from 0.8 to 1.8 mm in diameter (Figure 2A,B). Fistule
walls are from 31.5 to 75.6 µm in thickness. Most specimens
have from 2 to 4 fistules, but the holotype has numerous
fistules (from 2 to 5 fistules cm-2) and covers an area of 10
cm in diameter. Fistules are from 2 to 7.5 mm apart and they
are regularly spread on the substratum surface. The tops of
the fistules are covered with a sieve-like reticulation bearing
many ostia (Figure 3C), or end in an oscule of 0.7 to 1 mm
in diameter. Ostial fistules are circular or oval in section,
and characteristically distally widened (Figure 2A). Oscular
fistules are commonly straight or slightly curved, sometimes
gradually tapering from the middle (Figure 2B). Fistules
are compressible, brittle, and easily broken, and fusion (two
fistules) has only been observed in one specimen. Fistules
are white and pale yellow at the base close to the substrate,
and they are hardly distinguishable at first sight because this
species lives cryptically, and their exposed parts often blend
in well with background colours. In alcohol fistules turn
dark yellow. Inside the coral the sponge tissue is beige, and
pale brown in alcohol. The tissue inside the coral consists of
a pulpy organic mass secreting mucus.
Spicules: the spicules are slender oxeas, mostly slightly
curved at the centre or straight, ending in symmetrical
points, sometimes with mucronate tips. Very slim oxeas that
are also common in some specimens probably represent
young spicules (Figure 2C). They measure 67.5–(101.3)–
122.5 µm long and 1.3–(3.9)–6.3 µm in width (Table 1).
Figure 3. SEM images of skeletal characteristics of Aka cryptica
sp. nov. (A) External view of the oscular fistule; (B) cross section of
the ostial fistule showing the internal structure; (C) top view of an
ostial fistule.
Figure 2. Aka cryptica sp. nov. (A) Detail of the ostial fistule; (B) detail
of the oscular fistule; (C) SEM images of oxeas and derived spicules;
(D, E) choanosomal structure of the basal mass inside the coral.
Aka cryptica specimens Oxeas
Holotype: Length×width shaft
MNCN 1.01/363 90–(106)–117×2.5–(4)–5
Paratypes
BMNH 2006.6.30.1 87.5–(101.5)–120×3–(4.5)–5.5
LEB-ICML-UNAM-1196 90–(100.5)–112.5×2–(3.7)–5
LEB-ICML-UNAM-1233 80–(101.8)–115×2–(4)–5
LEB-ICML-UNAM-1325 90–(98)–103×2.5–(2.7)–3.8
LEB-ICML-UNAM-1328 87.5–(103.5)–122.5×1.3–(3.5)–5
LEB-ICML-UNAM-1340 67.5–(94.3)–110×2.5–(3.9)–6.3
Table 1. Comparative data for the dimensions of the oxeas (in µm) of
Aka cryptica sp. nov. specimens. Values in parentheses are means.
1480 J.L. Carballo et al. Coral boring Aka-species from Mexico
Journal of the Marine Biological Association of the United Kingdom (2007)
Figure 4. Excavating characteristics of Aka cryptica sp. nov. (A) Excavating pattern in a cross section of a coral branch; (B) excavating pat-
tern in a longitudinal section of a coral branch, (the arrows show the diaphragms); (C) SEM image of patterns erosion; (D) SEM images of
erosion scars on the walls of excavated chambers.
Skeleton: spicules are strewn in confusion or grouped in
directionless loose tracts in the basal mass inside the coral
(Figure 2D,E). In the outer wall of the fistule the oxeas form
a confused ill-def ined tangential ectosomal skeleton (Figure
3A). Towards the basal part of the f istule, and below the
surface it is possible to distinguish sinuous bands of spicule
bundles (from 15 to 18 spicules) running up, connected
transversally by narrower bundles (from 5 to 8 spicules), and
forming meshes from 150 to 240 µm wide, but without a clear
network. It is possible to distinguish this structure up to the
lower third of the fistule length, but after that, the skeleton
becomes a somewhat isodictyal reticulation of multispicular
bundles (from 20 to 45 µm thick), forming meshes from 125
to 255 µm wide (Figure 3B).
Erosion pattern: network of reticulate galleries with
irregularly spherical or ovoid chambers densely distributed
in the coral (Figure 4A). They measure from 0.6 to 2 mm
long and from 0.5 to 1 mm wide. Wall between adjacent
chambers is from 0.2 to 0.8 mm in thickness, and the
interconnection between the chambers is by means of a
diaphragm from 0.2 to 0.4 mm in diameter. Chambers
can be fused, forming long chambers parallel to the coral
surface. This species also occupies the natural pores of the
coral boring only the walls that separate the septa of the
coral and producing long chambers parallel to the coral
surface (Figure 4B), from 3.7 to 11 mm long and from 0.7 to
1 mm wide. The walls of the chambers and tunnels, present
a pitted surface where chips have been removed (Figure
Journal of the Marine Biological Association of the United Kingdom (2007)
1481Coral boring Aka-species from Mexico J.L. Carballo et al.
4C,D). They are sub-spherical in form and measure 20–50
µm in diameter.
Etymology
The specific name refers to the cryptic habitat where the
new species lives.
Distribution and ecology
Mexican Pacific Ocean (Nayarit and Oaxaca) (Figure 1).
Common in shallow water, from 2 to 7 m depth. The species
mainly bores dead and live stems and branches of the species
Pocillopora damicornis and P. verrucosa.
Remarks
This new species can be compared with the Aka-species
from the Indo-Pacific region. Aka diagonoxea Thomas, 1968
described from the Gulf of Mannar (Thomas, 1968) has
fistules that branch dichotomously or polychotomously, and
they are longer (up to 50 mm long) and wider (up to 4 mm
in diameter) than those in the new species. Moreover, it has
double angulated oxeas, and it excavates chambers 2 cm or
more in diameter inside coral. Aka paratypica Fromont, 1993
is similar to A. diagonoxea in colour, shape and size of oxeas
(Fromont, 1993), and it also has fistules longer than the
new species (40–60 mm). Aka mucosa (Bergquist, 1965) has
Figure 5. Aka brevitubulata (Rützler, 1974). (A) Ocular fistule (ex-current); (B) ostial fistule (in-current); (C) oxeas; (D) tissue filled boreholes
showing mucus covered tissue and fistules (the arrows show the fistules); (E) internal tissue and canals; (F) SEM image of erosion scars
(sponge chips removed).
1482 J.L. Carballo et al. Coral boring Aka-species from Mexico
Journal of the Marine Biological Association of the United Kingdom (2007)
very long (up to 50 mm high) and wide (7 mm in diameter)
black fistules and two categories of oxeas, characteristics
that are clearly different from the new species. Finally, Aka
maldiviensis Calcinai et al., 2000 also has longer fistules (5–7
cm high). The species nearest to ours is Aka minuta Thomas,
1972 recorded from the Gulf of Mannar, Seychelles and
Mozambique (Thomas, 1972, 1973, 1979), which also bores
colonies of Pocillopora damicornis (Linnaeus). However, this
species has oxeas with a sharp angle at the centre, it does
not form f istules, and it excavates chambers of up to 5 mm
in diameter, characteristics that are very different in the new
species. The species Aka trachys de Laubenfels, 1954 from
the central Pacific does not seem to be a valid species of
Aka since it has spined oxeas (named acanthostyles by the
author) (de Laubenfels, 1954).
The new species is also different from the species in the
Caribbean in the size of the fistule and excavating patterns.
For example, A. xamaycaensis Pulitzer-Finali, 1986 has white
fistules up to 11 cm long, and oxeas slightly curved (110–
125×4.5–6 µm) (excavation pattern is not described). Aka
brevitubulata (Pang, 1973) has yellow and longer fistules (9
mm high) than the new species, and produces a single large
spherical chamber completely filled with sponge tissue (Pang,
1973 and present study) (oxea dimensions: 119–148×6.9–9.1
µm); A. cachacrouensis (Rützler, 1971) has larger oxeas (up to
203.9×6.9 µm) than A. cryptica sp. nov., and dark greyish
brown fistules (up to 2.5 cm high) and produces a single
large chamber of 500 cm3. Aka coralliphaga (Rützler, 1971)
also has longer yellow fistules (up to 4 cm high) and oxeas
(142.1–156.3×5.0–6.4 µm), and it excavates a single chamber
of 20–130 cm3. Aka siphona has yellow to brown fistules up
to 15 cm long, excavates large galleries up to 20 cm across,
and has oxeas from 120 to 200 µm long (Laubenfels, 1949;
Hofman & Kielman, 1992).
Aka brevitubulata (Pang, 1973)
Synonymy: Siphonodictyon brevitubulatum Pang, 1973
(Figure 5)
Material examined
Holotype: [YPM No. 8717]. Discovery Bay, Jamaica;
Montastraea annularis; 15 m depth; collected by R. Keeley; 16
October 1968.
Specimens: BMNH 2006.6.29.12, Puerto Morelos
(Quintana Roo), 20.5°24'16.5"N 86°49.5'26.67"W, 09
September 2002, excavating Acropora palmata, back-reef 2
m. BMNH 2006.6.29.13, BMNH 2006.6.29.14, BMNH
Figure 6. Aka coralliphaga (Rützler, 1971). (A) Internal chamber filled with mucus-secreting tissue. The arrow shows a longitudinal-section
through fistule; (B) excavation chamber completely filled with tissue still adhering to the erosion scars (also Aka brevitubulata and unidenti-
fied nestling species); (C) oxeas; (D) SEM image of erosion scars created by chemical etching of sponge chips inside excavation galleries.
Journal of the Marine Biological Association of the United Kingdom (2007)
1483Coral boring Aka-species from Mexico J.L. Carballo et al.
2006.6.29.15, BMNH 2006.6.29.16, Puerto Morelos (Q.
Roo), 20.5°24'16.5"N 86°49.5'26.67"W, 11 November
2002, Acropora palmata, reef-front 5 m. BMNH 2006.6.29.17,
BMNH 2006.6.29.18, BMNH 2006.6.29.19, Puerto Morelos
(Q. Roo), 20.5°24'16.5"N 86°49.5'26.67"W, 28 July 2003,
Acropora palmata, reef crest, 1m. BMNH 2006.6.29.20, BMNH
2006.6.29.21, Puerto Morelos (Q. Roo), 20.5°24'16.5"N
86°49.5'26.67"W, 14 September 2003, Montastraea annularis
back-reef, 3 m.
Description
The tissue has a glistening appearance due to mucus
secretion. Fistules (between 3 and 9 mm high) are relatively
few in number (1–2 cm apart) due to the nature of excavation
activity of this sponge, which usually produces a large single
excavation. Oscular and ostial papillae do not fuse and, nor
has this species been observed to overgrow the substrate
(Figure 5A,B). Oscules are 2–5 mm wide. In life, fistules are
yellow. The internal sponge tissue is a dull, dark yellow.
Spicules: the oxeas are abundant and smooth, although
some with rather abrupt points at either end. Oxeas are
curved around the mid-region, with the degree of curvation
varying between individual oxeas. Some are almost straight
and some have a sharper bent mid-region, giving a more
curved ‘boomerang’ type appearance (Figure 5C). However,
there is little variation in observed length/width or curvation
of oxeas. Oxea length(s): 109.5–142 µm (mean: 133.7 µm)
width: 3.7–5.5 µm (mean: 4.2 µm).
Skeleton: oxea are abundant but without orientation in
the choanosome. Spicule arrangement within fistules is
confused, although the basal part of the f istule shows a
tendancy for oxeas to be placed tangentially.
Erosion pattern: this species characteristically forms a large
single spherical/subspherical excavation completely filled
with tissue (Figure 5D). It constructs galleries without clearly
outlined chambers or ducts. Long narrow channels connect
the chamber with the substrate surface (Figure 5E). These
canals may be up to 15 mm reaching an excavation of up to
4–5 cm in massive substrates. Borehole diameter is less in
branching substrates.
Distribution and ecology
This is a relatively common species at Puerto Morelos,
Mexican Caribbean (Figure 1). It was previously described
by Pang (1973) in Jamaica, and Hofman & Kielman (1992)
in Santa Marta (Colombia).
Remarks
First record in Mexico.
Aka coralliphaga (Rützler 1971)
(Figure 6)
Synonymy: Siphonodictyon coralliphagum forma obruta
Rützler, 1971
Material examined
Holotype: [USNM 24098]. Barbados, West Indies; 25 m
depth; 5 July 1969.
Specimens: BMNH 2006.6.29.22, Puerto Morelos
(Q. Roo), 20.5°24'16.5"N 86°49.5'26.67"W, 02
September 2002, Siderastrea siderea, reef-front 5 m.
BMNH 2006.6.29.23, BMNH 2006.6.29.24, BMNH
2006.6.29.25, Puerto Morelos (Q. Roo), 20.5°24'16.5"N
86°49.5'26.67"W, 14 November 2002, Siderastrea
siderea, reef front 8 m. BMNH 2006.6.29.26, BMNH
2006.6.29.27, BMNH 2006.6.29.28, Puerto Morelos (Q.
Roo), 20.5°24'16.5"N 86°49.5'26.67"W, 05 August 2003,
Diploria strigosa, reef crest, 1.5 m. BMNH 2006.6.29.29,
BMNH 2006.6.29.30, BMNH 2006.6.29.31, Puerto
Morelos (Q. Roo), 20.5°24'16.5"N 86°49.5'26.67"W, 19
September 2003, Diploria strigosa, back reef, 3 m.
Description
Cream/tan/yellow mucus-secreting tissue fills chambers.
This species does not encrust substrate. Ostial and oscular
fistules are separate. The ostial fistules are conspicuous,
creamy coloured globular protrusions of 2–4 mm height
and similar diameter (Figure 6A). Ostia are distributed
over the entire surface of the f istules with fusion of ostial
tubes observed in some samples. Oscular structures are of
lower relief (1–2 mm), but comparable diameter; they are
open-ended cylindrical tubes which bear a single osculum.
Fistules are circular and irregularly spaced with at least one
per bored chamber.
Spicules: tissue is dense in this species with abundant oxeas
exhibiting no clear orientation. Spiculation consists solely of
oxeas which are bent in the mid-region (Figure 6C). There
may be slight variation in the extent of the curvation with
some being almost straight. Oxea length(s): 98.5–149.6 µm
(mean: 145.5 µm) width: 1.8–7.3 µm (mean: 4.7 µm).
Skeleton: spicules are strewn in confusion forming no clear
skeletal pattern.
Erosion pattern: canals and connecting tunnels may be long
(3–8 mm length/1.5–2.5 mm diameter). Endolithic chambers
are large, although diameter can be variable (average 13–
20 mm). They are roughly subspherical, with some being
slightly more elongate than others; longest axis parallel to
substrate surface (Figure 6B). Chambers extend deep from
the substrate surface where the substrate allows (e.g. 1.5–2
cm), and may be 2–3 cm apart. The chambers are covered
by erosion scars created by the sponge (Figure 6D).
Distribution and ecology
This is a common species at Puerto Morelos reef (Figure
1). It was found in dead rubble substrate of Acropora palmata,
Montastraea annularis complex and Diploria strigosa. Aka
coralliphaga is widely distributed throughout the Caribbean.
The species has been cited in Barbados, Puerto Rico,
Jamaica, Dominica (Rützler, 1971), Colombia (Hofman
& Kielman, 1992) and Mexico (Cozumel, Quintana Roo)
(Lehnert, 1993).
Remarks
Rützler (1971) described two new species of the genus
Aka (A. cachacrouensis and A. coralliphaga) from the Caribbean
Sea (both as Siphonodictyon). The present specimens are most
closely related to A. coralliphaga, however, oxeas are longer
and thinner than those found in the present species.
1484 J.L. Carballo et al. Coral boring Aka-species from Mexico
Journal of the Marine Biological Association of the United Kingdom (2007)
We are grateful to the following sources of funding CONACYT
SEP-2003-C02-42550, CONABIO FB666/S019/99, CONABIO
FB789/AA004/02 and CONABIO DJ007/26. We thank Israel
Gradilla Martínez (Centro de Ciencias de la Materia Condensada)
for the SEM photographs, Clara Ramírez Jáuregui (ICML-
Mazatlán) for help with the literature, Alejandra Torres Ariño
for her hospitality during the sampling in Oaxaca. We are also
grateful to the personnel of the National Park isla Isabel for the
availability and the permission conferred for the collection of the
samples in the Isabel Island, and especially to Cayetano Robles
Carrillo, Gonzalo Perez Lozano and Jorge Castrejón for their help
during the samplings.
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Submitted 22 July 2006. Accepted 2 May 2007.
... Distribution and previous records. S. crypticum was described by Carballo et al. (2007) from Nayarit, Mexico. Only three later reports are available and were again for the Mexican Pacific (Carballo et al. 2008a(Carballo et al. , 2008b(Carballo et al. , 2013. ...
... Remarks. We presently did not provide a very comprehensive description, because of the recent date and the detail of the original description (Carballo et al. 2007). Our material agreed well with that of Carballo et al. (2007), and further information can be taken from that publication. ...
... We presently did not provide a very comprehensive description, because of the recent date and the detail of the original description (Carballo et al. 2007). Our material agreed well with that of Carballo et al. (2007), and further information can be taken from that publication. ...
Thesis
Excavating sponges are organisms that erode calcareous substrates such as polychaete tubes, mollusk shells, calcareous algae, and coral reef; among others. Most of these species are including in the family Clionaidae (Demospongiae: Clionaida), which harbors 10 genera, with Cliona as the most diverse with 160 species. The taxonomy of Clionaidae is based mainly on the morphology of the spicules, and probably most of the genera, mainly Cliona, are considered polyphyletic. This research emerged to clarify the systematics of the excavating sponges from the Pacific and the Caribbean of Mexico. However, in an attempt to obtain the greatest morphological variability, species from other regions, such as the Pacific of Central America, the Caribbean (Costa Rica), the Mediterranean (including the Adriatic, Ligurian, and Alboran seas), the Indo-West Pacific (Mozambique), and the Indo-Central Pacific (Great Barrier Reef) were included. We presents the diagnosis of the species studied and also include information from other species from the literature, which has allowed us to have a better idea of the morphological variety of the family Clionaidae. Additionally, the possible taxonomic value of the excavation pattern was evaluated: galleries, junction channels, and erosion footprints. The information obtained suggests that these one do not have taxonomic value at the species level, but it has at the family and order levels. For molecular analysis, the markers, COI, 28S, and 18S were obtained. Also sequences available in the GenBank database were used. Three phylogenies were obtained, and these were consistent among them. A morphological phylogeny was also carried out based mainly on the spicular elements, which, although it did not have a good resolution, it supported the molecular phylogenies. Based on the obtained results, four species complexes are proposed, Cliona amplicavata, C. californiana, C. mucronata, and C. vermifera. Of these, the C. mucronata complex has been described in this thesis, based on morphological evidence and molecular markers, and two new species C. mariae in the Eastern Pacific and C. yorkin in the Caribbean Sea were described. It is proposed to resurrect and amend the genus Bernatia originally described from a Mediterranean species. The genus Cliona is amended, and the creation of two new genera are proposed; one characterized by variations in the tylostyles, and the other one by the presence of spirasters similar to those that are present in the family Spirastrellidae. The genus Cervicornia is also synonymized with Spheciospongia, and the diagnosis of this is amended. Some species of the genus Cliona should also be included in this genus. However, studies to include more species are necessary to strengthen this hypothesis. Finally, the genera Spiroxya and Volzia, according to molecular, spicular evidence and erosion pattern, seems to be very far away from the rest of the species of the family Clionaidae, suggesting the creation of a new family.
... Distribution and previous records. S. crypticum was described by Carballo et al. (2007) from Nayarit, Mexico. Only three later reports are available and were again for the Mexican Pacific (Carballo et al. 2008a(Carballo et al. , 2008b(Carballo et al. , 2013. ...
... Remarks. We presently did not provide a very comprehensive description, because of the recent date and the detail of the original description (Carballo et al. 2007). Our material agreed well with that of Carballo et al. (2007), and further information can be taken from that publication. ...
... We presently did not provide a very comprehensive description, because of the recent date and the detail of the original description (Carballo et al. 2007). Our material agreed well with that of Carballo et al. (2007), and further information can be taken from that publication. ...
Article
Full-text available
Excavating sponges are one of the main groups of bioeroders in coral reefs. Their diversity has been thoroughly studied in some regions: in the Caribbean, the Mediterranean, and the Indo-Pacific, including the Mexican Pacific. However, there is a lack of information from the Pacific of Central America, with only a few records from Panama and Costa Rica. This study provides additional distributional records and taxonomic descriptions of species collected between 2011 and 2016 at nine localities along the Pacific coast of El Salvador, Nicaragua, Costa Rica and Panama. A total of fourteen species of excavating sponges from three orders, three families, and five genera are considered valid in this area. Nine are new records for Central America, six are new records for El Salvador, three are new records for Nicaragua and eleven are new records for Costa Rica. The species collected from Panama were already recorded before. The species here described are Cliona amplicavata, Cliona californiana, Cliona euryphylle, Cliona microstrongylata, Cliona aff. mucronata, Cliona pocillopora, Cliona tropicalis, Cliona vermifera, Cliothosa tylostrongylata, Pione cf. carpenteri, Pione mazatlanensis, Thoosa calpulli, Thoosa mismalolli and Siphonodictyon crypticum. We also reviewed the literature related to excavating sponges from Central America, and the taxonomic status of respective species was updated. We provide a faunistic record of 14 excavating sponge species for Central America. Our data are expected to be useful for management and conservation purposes.
... Sodium hypochlorite was used to digest the organic material in the sample (Carballo et al., 2004), and the spicules were then examined under an optical microscope (Primo Star, Carl Zeiss Microscopy, Thomwood, USA). Species descriptions provided by Carballo et al. (2004Carballo et al. ( , 2007, Bautista-Guerrero et al. (2006) and Cruz-Barraza et al. (2011) were consulted to identify each sponge species to the highest taxonomic level possible. The incidence of each boring sponge species in each sample was considered as a record to calculate their abundance (FI) relative to the overall samples either per site or substrata category. ...
Article
Boring sponges are an important component of bioeroder assemblages in tropical coral reefs. They are considered as a potential threat for coral reef health, and the increase of dead corals is expected to promote their abundance. The relationship between the availability of dead coral substrata and the development of boring sponge assemblages was evaluated during El Niño 2015–16 at five reefs from Zihuatanejo, Guerrero, Mexico. Environment and substrate quality were assessed. Overall, environment conditions remained normal in relation to previous studies in the area. Only water temperature showed unusually high records at all sites and coincided with bleaching and mortality of corals, possibly caused by the effects of the El Niño event. Abundance of boring sponges in dead corals and coral rubble was lower than during previous studies. Although sponge abundance was not directly related to cover of both dead corals and coral rubble, cover of dead corals showed a high correlation with the variation in the structure of sponge assemblages across sites. Cliona vermifera dominated sponge assemblages at all sites, and its abundance was high under conditions of high cover of live corals and low cover of bleached corals. Since overall sponge abundance responded in a similar way, these results suggest that boring sponge assemblages dominated by C. vermifera are enhanced by conditions favourable for corals. Our results imply that El Niño events in the Mexican Pacific are not likely to cause immediate population outbreaks of boring sponges.
... In the ETP, only Siphonodictyon and Spheciospongia species are considered tolerant of high sedimentation, since their aquiferous system is not easily overloaded (Rützler 1971). The abundance of Siphonodictyon crypticum on Mexican coral reefs under high sedimentation supports this relationship (Carballo et al. 2007. ...
Chapter
Bioerosion, the weakening and erosion of hard substrates by boring, etching, and grazing organisms, is a major structuring force on coral reefs of the Eastern Tropical Pacific (ETP). Bioerosional processes are the main source of reef erosion, and facilitate recycling of reefal carbonate. In healthy reefs, a dynamic balance exists between destructive (i.e. bioerosion) and constructive (i.e. bioaccretion) processes, allowing for maintenance and growth of reef frameworks. In changing environments, however, bioerosion rates can exceed those of coral calcification, leading to reduced reef development and the destruction of reef frameworks. In the ETP, high rates of bioerosion are promoted by nutrient-rich upwelling and high primary productivity conditions, recurrent coral bleaching and mortality events, and a chemical environment characterized by high-pCO2 and low aragonite saturation state. Here we examine bioerosion in ETP coral habitats and the variable roles of reef-dwelling bioeroder taxa: microbial euendoliths (microendoliths), sponges, polychaetes, sipunculans, crustaceans, molluscs, echinoids, and reef fishes. Among these agents of bioerosion, sponges, sipunculans, bivalves, and echinoderms have been relatively well studied in this region, while information is currently lacking or limited for microendolith assemblages, polychaetes and reef fishes. The frequency of coral invasion by clionaid sponges (e.g., Cliona vermifera and Thoosa mismalolli) is variable between ETP coral habitats. Dense boring sponge assemblages can lead to high rates of carbonate losses exceeding those of bioaccretion. Boring bivalves (i.e., species of Lithophaga and Gastrochaena) are very abundant on many actively accreting reefs and are generally more prominent contributors to reef erosion in the ETP than in other regions. Sea urchins are by far the most destructive grazers of coral substrates in habitats where abundant. Following ENSO-associated coral mortality events, intense bioerosion by sea urchins has impeded coral recovery and compromised reef health at many eastern Pacific sites. This chapter reviews factors important in ETP bioerosion, and current knowledge of bioeroder populations in the region.
... Accordingly, isolation by distance is a potential mechanism of differentiation and both low dispersal potential and physical factors, such as hydrological conditions, may play a significant role in shaping the genetic structure of sponges (Duran et al. 2004c). In the Mexican Pacific (MP), studies concerned with coral-excavating sponges have focused primarily on their taxonomic description and classification, reproductive biology, and ecological role in reef communities (Carballo et al. 2004;Carballo and Cruz-Barraza 2005;Bautista-Guerrero et al. 2006;Carballo et al. 2007;Nava and Carballo 2008;Bautista-Guerrero et al. 2010;Cruz-Barraza et al. 2011;Carballo et al. 2013b;Bautista-Guerrero et al. 2014). At present, the population genetic structure of coral-excavating sponges in this region remains unexplored. ...
Article
Cliona vermifera is one of the most abundant excavating sponges in Mexican coral reefs, and represents a potential threat to their health. It appears to have limited dispersal potential, but, paradoxically, it is widespread over much of the 2000 km of Mexican Pacific waters, suggesting mechanisms of long-distance dissemination. Despite its ecological importance, nothing is known about its patterns of genetic structure and connectivity in space and time. In this study, we assess levels of genetic structure and test the hypothesis of limited dispersal and isolation by distance among coral reef systems in the Mexican Pacific. Genetic diversity levels were consistently low in DNA sequences from two mitochondrial genes and one nuclear gene; however, they revealed strong and significant genetic differentiation throughout the study region. Patterns of genetic differentiation from the slow-evolving mitochondrial, but not the nuclear, genes were geographic scale dependent. We found higher mitochondrial genetic similarity among localities at 10–100s km than at larger scales (100–1000s km). However, all samples were genetically differentiated at the nuclear locus, which is inconsistent with frequent long-distance dispersal. Significant isolation by distance is consistent with life history traits shared by boring sponges: a short larval period and larval philopatric behavior. The patterns of genetic differentiation in C. vermifera concur with those found in other sympatric coral species, and suggest the influence of community-wide ecological and genetic mechanisms on the genetic makeup of coral reef species in the Mexican Pacific. Fixed genetic differences suggest that the southern population of Oaxaca may be experiencing incipient speciation.
Article
Full-text available
Bioeroded carbonate clasts from a Pliocene shallow-marine succession of Almería (SE Spain, Betic Cordillera) were analysed with computed tomography (CT). This revealed the detailed 3D architecture of bioerosion structures hidden within and allowed for their ichnotaxonomic identification (14 ichnospecies of 5 ichnogenera) and quantification. Borings are produced by worms, mostly polychaetes and sipunculids dominated, followed by bivalves and lastly by sponges. The crosscutting relationship between the borings and their preservation characteristics points to a complex colonization history of the clasts with repeated bioerosive episodes interrupted by physical disturbances, including overturning and abrasion of the clasts followed by their recolonization. Our findings facilitated paleoenvironmental interpretation and can be compared to analogous modern-day ecological succession. The sharp dominance of worm borings — early successional species — may be related to frequent, periodic, physical disturbance that possibly prevented the cobble-dwelling macroboring community from being overtaken by sponges — late successional taxa. CT, hand sample and petrographic observations detected, aside from borings, other irregularly shaped pores which are interpreted to be generated by diagenetic processes including dolomitization, silicification and dissolution, representing an intraparticle moldic and moldic enlarged porosity. Boring porosity crosscutting the diagenetically altered grains suggests the later occurrence of bioerosion processes. Irregular shapes ranging from roughly spherical, elongate sub-polyhedral to amoeboid resemble morphologies produced by modern sponges. Moldic pores possibly acted as primary domiciles for boring sponges, which infested, altered and enlarged pre-existing pores as they grew (as happens in the modern), providing an example of how biological and non-biological processes interacted and together influenced endolithic palaeocommunity development.
Article
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Sponges are an important component of coral reef communities. The present study is the first devoted exclusively to coral reef sponges from Eastern Tropical Pacific (ETP). Eighty-seven species were found, with assemblages dominated by very small cryptic patches and boring sponges such as Cliona vermifera; the most common species in ETP reefs. We compared the sponge patterns from ETP reefs, Caribbean reefs (CR) and West Pacific reefs (WPR), and all have in common that very few species dominate the sponge assemblages. However, they are massive or large sun exposed sponges in CR and WPR, and small encrusting and boring cryptic species in ETP. At a similar depth, CR and WPR had seven times more individuals per m2, and between four (CR) and five times (WPR) more species per m2 than ETP. Perturbation, at local and large scale, rather than biological factors, seems to explain the low prevalence and characteristics of sponge assemblages in ETP reefs, which are very frequently located in shallow water where excessive turbulence, abrasion and high levels of damaging light occur. Other factors such as the recurrence of large-scale phenomena (mainly El Niño events), age of the reef (younger in ETP), isolation (higher in ETP), difficulty to gain recruits from distant areas (higher in ETP), are responsible for shaping ETP sponge communities. Such great differences in sponge fauna between the three basins might have consequences for coral reef structure and dynamics.
Chapter
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Shallow coral reefs worldwide occupy 1.2% of the world’s continental shelf area but support an estimated 35% of all known marine biodiversity. Nevertheless, our knowledge of reef-associated biodiversity in southern Mexican Pacific systems is scarce. Here, we synthesize the knowledge regarding the biodiversity of reef-associated organisms including algae, sponges, cnidarians, polychaetes, mollusks, malacostraceans, echinoderms, and fishes across coral systems located in Guerrero and Oaxaca. To date, 97 localities have been referred as harboring reef corals in the area, and 18 sites can be considered as harboring true reefs dominated by Pocillopora spp. (>90%) and to a lesser extent by Pavona spp. (<5%) and Porites spp. Coral systems harbors 989 operational taxonomic units (177 algae, 40 sponges, 36 cnidarians, 131 polychaetes, 196 mollusks, 126 malacostraceans, 73 echinoderms, and 210 fishes). Nonparametric models indicate that richness is far from reaching the asymptote in all taxonomic groups, particularly in algae (22.5%) and polychaetes (56%), although cnidarians (83.7%) and fishes (82.6%) are relatively close to reach the richness suggested by the models. Species richness patterns, if any, are influenced by sampling bias. Finally, it is expected that future sampling of unprospected habitats, sites, and taxa employing traditional and novel techniques may render far more species than expected. Additionally, biodiversity should be seen as a master variable for practically evaluating both the health of ecosystems and the success of management efforts, and hence, a standardized and systematic monitoring protocol under a marine biodiversity observation network is necessary for effective reef management.
Chapter
Bioeroding sponges play a central role in carbonate cycling on corals reefs. They may respond differently to habitat deterioration than many other benthic invertebrates, because at some locations, their abundances increased after disturbance. We reviewed literature on these sponges in context of environmental change and provide meta-analyses at global level. A difficult taxonomy and scarce scientific expertise leave them inadequately studied, even though they are the best-known internal bioeroders. They are sheltered within the substrate they erode, appear to be comparatively resilient against environmental change and can have heat-resistant photosymbionts and ‘weedy’ traits, including multiple pathways to reproduce or disperse and fast growth and healing abilities. Especially temperature stress appears to disable calcifiers stronger than bioeroding sponges. Moreover, increases in bioeroding sponge abundances have been related to eutrophication and disturbances that led to coral mortality. Chemical sponge bioerosion is forecast to double with doubled partial pressure of carbon dioxide, but reduced substrate density may counteract this effect, as dominant sponges erode more in denser substrates. Case examples portray shifting impacts of bioeroding sponges with environmental change, with some reefs already being erosional. Most available data and the largest known species record are from the Caribbean. Data from the Coral Triangle and India are largely restricted to faunistic records. Red Sea, Japanese and cold-water reef bioeroding sponges are the least studied. We need more quality research on functions and interaction effects, about which we are still insufficiently informed. With many calcifiers increasingly failing and bioeroding sponges still doing well, at least at intermediate levels of local and global change, these sponges may continue to significantly affect coral reef carbonate budgets. This may transform them from valuable and necessary recyclers of calcium carbonate to problem organisms.
Chapter
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The biodiversity of coral reefs is dominated by invertebrates. Many of these invertebrates live in close association with scleractinian corals, relying on corals for food, habitat or settlement cues. Given their strong dependence on corals, it is of great concern that our knowledge of coral-associated invertebrates is so limited, especially in light of severe and ongoing degradation of coral reef habitats and the potential for species extinctions. This review examines the taxonomic extent of coral-associated invertebrates, the levels of dependence on coral hosts, the nature of associations between invertebrates and corals, and the factors that threaten coral-associated invertebrates now and in the future. There are at least 860 invertebrate species that have been described as coral associated , of which 310 are decapod crustaceans. over half of coral-associated invertebrates appear to have an obligate dependence on live corals. Many exhibit a high degree of preference for one or two coral species, with species in the genera Pocillopora, Acropora and Stylophora commonly preferred. This level of habitat specialization may place coral-associated invertebrates at a great risk of extinction, particularly because preferred coral genera are those most susceptible to coral bleaching and mortality. In turn, many corals are also reliant on the services of particular invertebrates, leading to strong feedbacks between abundance of corals and their associated invertebrates. The loss of even a few preferred coral taxa could lead to a substantial decline in invertebrate biodiversity and have far-reaching effects on coral reef ecosystem function. A full appreciation of the consequences of further coral reef degradation for invertebrate biodiversity awaits a more complete description of the diversity of coral-associated invertebrates, the roles they play in coral reef ecosystems, their contribution to reef resilience and their conservation needs.
Article
Full-text available
A collection of boring sponges from the Maldives and Seychelles coral reefs was studied. From the etched organogenous material, 16 boring sponge species (belonging to seven genera and five families), were identified; three of these species are new and two are reported for the Indian Ocean for the first time. A list of the boring species hitherto recorded from the area is given. The boring sponge faunas from the Maldives and Seychelles show certain affinities among them and also with that of the entire Indo‐Pacific region.
Article
A new species of excavating sponge of the family Clionaidae, Cliona microstrongylata sp. nov. was found in detritic bottoms from the Sea of Cortes at 26 m depth. The type grows in alpha stage boring a dead bivalve shell. It presents very small orange-red papillae (from 150 to 850 μm in diameter), which are regularly distributed on the surface of the shell. They are level with the surface of the substratum and don't fuse. The boring activity of the species produces a network of reticulate spherical-ovoid or quadrangulate chambers with the longer axis from 1.6 to 2.6 mm in length. Tylostyles are thin or ensiform (shaft thicker in central part). Reduced tylostrongyles occasionally appear. However, the most notable characteristic of the new species is the presence of unusual oval and curved bean-like microstrongyles, which are unique in the genus Cliona so far. Eggs from 70 to 90 μm in diameter were present in different parts of the choanosome. After the present study, the number of boring species along the Mexican Pacific coast has increased to 15 species.
Chapter
Only few publications deal with Recent species of the genus Aka or Siphonodictyon, a younger synonym of Aka (Johnson 1899; de Laubenfels 1936; Bergquist 1965; Rutzler 1971; Thomas 1972; Pang 1973). In the literature, only two publications figure and describe fossil Aka spicule arrangements — Müller (1978) and Reitner (1987a). Aka spicules are commonly found within burrows in Jurassic and Cretaceous shallow marine carbonates.
Article
From June till December 1987 an inventory of the excavating sponges of the Santa Marta area, Colombian Caribbean, was made by scuba diving to depths not exceeding 18 m. Sixteen species were recorded and compared morphologically,using spicule sizes, papillae shapes, and excavation characteristics. Four little-known species are fully described and illustrated by submarine color photographs in situ . One appears to be a new species: Axinyssa flavolivescens , belonging to a genus not known to excavate so far. The other three species could not be identified with certainty: Aka aff. xamaycaensis , Aka aff. brevitubulata , and Cliona aff. flavifodina . A key to the excavating sponges of the area studied is provided.
Article
DURING an extensive collection of sponges from the coral rocks of the Gulf of Mannar, the author has come across two new species of sponges. The first one, Aka diagonoxea, is a boring sponge and the other, Damirina papillata, usually grows with its base rooted deep in the coral. Detailed descriptions of these species are given here. All specimens are deposited in the Reference Collection Museum of the Central Marine Fisheries Research Institute. Family CLIONIDAE Gray Genus Aka de Laubenfels de Laubenfels proposed this new name in 1936 for Acca Johnson (1899) with type Acca insidiosa. Johnson originally described three species, A. insidiosa, A. rodens and A. infesta from Madeira. Of these, the first was found boring into the shells of Ostreaaad Chama ; the second into the coral Dendrophyllia ramea and the third from a shell attached to another sponge. The other species transferred to this genus by de Laubenfels include Cliorm nodosa, C. labyrinthica, both by Hancock (1849), and C. coralliophaga Stephens (1915). Aka trachys de Laubenfels (1954), from West Central Pacific, has acanthoxeas. Aka diagonoxea n. sp.