Polar Biology
https://doi.org/10.1007/s00300-020-02654-x
ORIGINAL PAPER
A new species of Isodictya (Porifera: Poecilosclerida) from the Southern
Ocean
Pilar Ríos1,2
· Ana Riesgo3
· Sergio Taboada3,4
· Javier Cristobo1,2
Received: 23 July 2019 / Revised: 17 March 2020 / Accepted: 19 March 2020
© Springer-Verlag GmbH Germany, part of Springer Nature 2020
Abstract
We discovered a new species of Porifera belonging to the genus Isodictya Bowerbank, 1864 during cruises aboard R/V
Hesperides in Antarctica. Collected samples are mostly part of the surveys of the Spanish project BENTART whose main
objective has been to study the benthic communities inhabiting sea bottoms of Livingston and Deception Island in the South
Shetlands archipelago and the Antarctic Peninsula. Isodictya filiformis sp. nov., described here, is characterized by its fragile
and thin morphology (very different from other known species in the area) and by having microxeas as additional microscleres. Three specimens were collected from Marguerite Bay, Low Island and Deception Island (Antarctic Peninsula) and one
specimen at Peter I Island (Bellingshausen Sea). Its presence in Peter Island is quite relevant as this location is 390 km away
from the nearest coast in the Bellingshausen Sea, an area that has scarcely been investigated in the past. However, results
from the Bentart 03 Expedition seem to indicate that Peter I Island has a wide variety of benthic organisms, in contrast to
the deep adjacent areas of Bellingshausen Sea. Apart from the morphological analyses, we place the new Isodictya species
within its phylogenetic context using two nuclear markers (18S rDNA and 28S rDNA) and provide some information about
the ecological preferences of the new species.
Keywords Taxonomy · Biodiversity · Phylogeny · Bellingshausen Sea · Peter I island · Antarctica
Introduction
Peter I is a very remote island in the middle of the Bellingshausen Sea in the Southern Ocean. Inaccessible nearly
all year-round due to the heavy surrounding pack ice, Peter
Electronic supplementary material The online version of this
article (https://doi.org/10.1007/s00300-020-02654-x) contains
supplementary material, which is available to authorized users.
* Pilar Ríos
pilar.rios@ieo.es; pilar.rios.lopez@gmail.com
1
Instituto Español de Oceanografía, Centro Oceanográfico de
Gijón, C/Príncipe de Asturias 70 Bis, 33212 Gijón, Asturias,
Spain
2
Dpto. Ciencias de la Vida, EU-US Marine Biodiversity
Group, Universidad de Alcalá, 28871 Alcalá de Henares,
Spain
3
Department of Life Sciences, The Natural History Museum
of London, Cromwell Road, London SW7 5BD, UK
4
Departamento de Biología (Zoología), Facultad de
Ciencias, Universidad Autónoma de Madrid, Cantoblanco,
28049 Madrid, Spain
I covers 158 km2 and is 95% glaciated. It was discovered
on January 21, 1821 by the Russian Fabian von Bellingshausen. Several expeditions, as The “Belgica” Expedition
(1897–1899) collected the first few specimens, then “Old I”
(1927), and later “Bahía Aguirre” (1954–1955) carried out
geographic and geologic studies at the island, but it was not
until 1965 (and 1969–1971) when the icebreaker “General
San Martín” made the first biological expedition in which
21 species of marine invertebrates were identified, with no
reports on the sponge fauna.
Even though information about the benthic macrofauna
of the Bellingshausen Sea and Peter I Island is scarce, in
the last decade, there has been a growing effort in studying
several aspects of it, particularly the soft-bottom molluscs
(Troncoso et al. 2007; Troncoso and Aldea 2008; Aldea
and Troncoso 2008, 2010; Aldea et al. 2008, 2011; Garcia-Alvarez et al. 2010), suprabenthic mysids (San Vicente
2007; San Vicente and Sorbe 2008; San Vicente et al. 2009),
cumaceans (Corbera and Ramos 2005; Corbera et al. 2009),
nemerteans (Fernández-Álvarez and Anadón, 2012, 2013),
other crustaceans (Klages et al. 1995; Arana and Retamal
1999; García-Raso et al. 2005), pycnogonids (Munilla and
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Soler-Membrives 2009, 2015), fishes (Matallanas and Olaso
2007; Eakin et al. 2008, 2009; Matallanas 2009a, b, 2010;
Matallanas et al. 2012), annelids (López 2011; Moreira and
Parapar 2011; Parapar et al. 2011, 2013), bryozoans (LópezFé 2005), echinoderms (Moya et al. 2012; O’Loughlin et al.
2009), ascidians (Varela and Ramos-Esplá 2008), invertebrate larvae (Ameneiro et al. 2012) and also the community
structure and spatial distribution of benthic fauna (Saiz et al.
2008). But in any case, the Bellingshausen Sea is still understudied and we know almost nothing about its sponge fauna.
The family Isodictyidae Dendy (1924) currently has two
genera: Coelocarteria Burton (1934) and Isodictya Bowerbank (1864) (Hajdu and Lôbo-Hajdu 2002). The genus
Coelocarteria, with three valid species, is known from the
Indian and Pacific Ocean. On the other hand, the genus Isodictya consists of 39 species (Van Soest et al. 2020). Interestingly, this genus is particularly rich in the Southern Ocean
with 17 valid species (Janussen and Downey 2014; Goodwin
et al. 2016). Here, we describe a new Antarctic member of
the genus Isodictya using a combined morphological and
molecular approach.
Material and methods
Sampling and preservation
The material examined was collected from Peter I Island
(Bellingshausen Sea, Antarctica, 68°49′ 37″ S; 90°48′ 47″
W), at a depth of 208–210 m in February 2003 on muddy
substrate with sand using a box corer (Fig. 1). Additional
material from Low Island (Antarctic Peninsula, 63° 26′ 13″
S; 62° 14′ 42″ W) and Marguerite Bay (Antarctic Peninsula,
68° 07′ 43″ S; 69° 35′ 28″ W) was also collected at a depth
of 97 m and 159 m, respectively, in February 2006. We collected one additional sample from Deception Island (62°
59.022′ S; 60° 35.847′ W) at 113 m depth in January 2006
using a modified Agassiz Trawl (Fig. 1). All materials were
collected during the Bentart 03, Bentart 06, ECOQUIM and
ACTIQUIM projects. Once on board, samples were photographed and subsequently preserved in 70% ethanol.
Morphological analysis
For the study of dissociated spicules, the organic matter was
digested with nitric acid taken to boiling point following the
methods of Rützler (1978) and Cristobo et al. (1993). The
skeleton sections were made following protocols as outlined
in Ríos (2006). Spicules of the holotype were examined
with a Leica S440 Scanning Electron Microscope, previously metalized with gold–palladium in a sputtering Polarun
SC 7640. The data for spicule sizes are based on 25 measurements for each spicule category, comprising minimum,
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average and maximum lengths in micrometers (µm). General
classification and the names of class, subclass, order and
suborders follow the classification proposed by Morrow and
Cárdenas (2015) and highlighted in the World Porifera Database (Van Soest et al. 2020).
The type material was deposited at the Museo Nacional
de Ciencias Naturales, Madrid, Spain (MNCN), Natural History Museum, London, United Kingdom (NHM)
and Museum National d’Histoire Naturelle, Paris, France
(MNHN).
DNA extraction, marker amplification
and phylogeny
DNA was extracted from a specimen of Isodictya filiformis
sp. nov. (28S MT032134 and 18S MT032130) and a sample
identified as Isodictya kerguelenensis (Ridley and Dendy
1886) (28S MT032133 and 18S MT032129) using a Qiagen DNeasy Blood and Tissue Kit (QIAgen) following an
adapted version of the protocol provided by the manufacturer (overnight incubation in lysis buffer and proteinase K).
We selected two molecular markers to amplify 18S rDNA
(18S) and 28S rDNA (28S). The complete 18S (1766 bp)
was amplified in three legs using the primers 1F-5R, 4F-7R,
and a.20-9R (Giribet and Wheeler 2001), and a fragment
of 589 bp of 28S (D6–D8 region) was amplified using the
primers CMPOR1490F and CMPOR2170R (Morrow et al.
2012). D6–D8 region was selected because these were the
most successful PCRs regarding 28S. All 18S fragments
were amplified using the PCR protocol 94 °C, 5 min; (94 °C,
1 min, 52 °C, 1 min, 72 °C, 1 min) × 38 cycles; 72 °C,
10 min. We used a different protocol for 28S of 94 °C, 5 min;
(94 °C, 1 min, 55 °C, 1 min, 72 °C, 1 min) × 38 cycles;
72 °C, 10 min. All DNA markers were amplified in 12.5 μL
reactions using 10.5 μL of VWR Red Taq DNA Polymerase
1.1 × Master Mix (VWR International bvba/sprl, Belgium),
0.5 μL of the forward and reverse primers, and 1 μL of DNA
template. PCR products, stained with GelRed® (Biotium,
USA), were visualized in a 2.5% agarose gel electrophoresis and run at 90 V for 30 min. Sequencing was conducted
on an ABI 3730XL DNA Analyser (Applied Biosystems,
USA) at the Molecular Core Labs (Sequencing Facility) of
the NHMUK, using the forward and reverse primers mentioned above. Sequences were deposited in GenBank under
accession numbers (See Online Resource 1).
Sequences were checked and cleaned using Geneious
Prime 2019.1.1 (https://www.geneious.com). Forward and
reverse reads were assembled into contigs and primers
were trimmed out. Alignments were built with MAFTT v.5
(Katoh and Standley 2013) and phylogenetic trees were built
using a GTR + G + I model in RAxML (Stamatakis 2006)
with 10 runs and 100 bootstrap replicates. Sequences for
Polar Biology
Fig. 1 Location of the collection sites of Isodictya filiformis sp. nov. in the Antarctic Peninsula and Bellingshausen Sea. The asterisks indicate
the exact collecting sites. 1, Peter I Island. 2, Marguerite Bay and Low Island. 3. Deception Island
18S and 28S from other sponge species were sourced from
NCBI (Online Resource 1).
Family ISODICTYIDAE Dendy (1924).
Genus Isodictya Bowerbank (1864).
Isodictya filiformis sp. nov.
(Figures 2, 3, 4 and 5).
Results and discussion
Type material
Systematics
Class DEMOSPONGIAE Sollas (1885).
Subclass HETEROSCLEROMORPHA Cárdenas et al.
(2012).
Order POECILOSCLERIDA Topsent (1928).
Holotype MNCN (MNCN 1.01/6 130 39), Museo Nacional
de Ciencias Naturales de Madrid. Peter I Island (Antarctic),
68° 49′ 37″ S; 90° 48′ 47″ W, 208–210 m depth, Coll. R/V
“Hespérides”, 05.02.2003. One specimen. Muddy substrate
with sand. In 70% ethanol.
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Fig. 2 Isodictya filiformis sp. nov. Habitus. a, Holotype, Peter I
Island. b, Paratype 1, Low Island. c, Paratype 2, Deception Island
Paratype 1 (NHMUK 2020.3.26.5), Natural History
Museum of London. Low Island (Antarctic Peninsula). 63°
26′ 13″ S; 62° 14′ 42″ W. 97 m depth. Coll. R/V “Hespérides”, 12.02.2006. One specimen. In 70% ethanol.
Paratype 2 (MNHN-IP-2019–13), Museum National
d’Histoire Naturelle, Paris. Deception Island (South Shetlands). 62° 59.022′ S; 60° 35.847′ W. 113 m depth. Coll. R/V
“Hespérides”, 07.01.2006. One specimen. In 70% ethanol.
Collection information of collected specimens was
archived in the PANGAEA data repository https://doi.panga
ea.de/10.1594/PANGAEA.913490.
Comparative material examined
Isodictya delicata var. megachela Burton (1934). Paratype
Natural History Museum of London: NHMUK 1933.3.17.7
(wet specimen) and NHMUK 1933.3.17.7a (slide); we
took a small fragment of the wet specimen to take the SEM
pictures. Type locality Seymour Island, Graham Land
(Antarctic).
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Fig. 3 Isodictya filiformis sp. nov. Skeleton. a, Section through the
distal area. b, Base of the sponge showing anchoring roots
Description
External morphology (Fig. 2a, b). Filiform specimens, fixed
to the substratum by means of small roots. Dimensions of
holotype, 24 cm long and 3 mm diameter in its middle part
and 1 cm at the top of the apex. Smooth and hard texture.
Flexible but consistent shaft. At first sight neither oscula
nor perforations observed. In its upper part, an apical multispicular axis can be made out, with secondary fibres in
perpendicular arrangement to this axis. Beige colour in vivo
and white in alcohol, except for its basal area and in its apical area, which were brown.
One specimen (collected during the 2006 expedition) has
the same external morphology with more organic material
in the apical area (Fig. 2c).
Skeleton (Fig. 3). Choanosomal skeleton made up of
bundles of oxeas along the stalk of the sponge. Ectosomal
skeleton made up of oxeas with few spicules, with scattered
isochelae not forming a defined layer, among which we may
Polar Biology
Etymology
The specific name is given because of the filiform morphology of the sponge.
Remarks
Fig. 4 Isodictya filiformis sp. nov. Spicules (SEM): a, Oxea. b,
Microxea. c–g, Palmate isochelae. h, Isochela malformation
also find microxeas. On the base of the sponge, there are formations that work as anchoring roots, also made up of spicular bundles, but in some specimens no isochelae noticed.
Roots normally accumulate sand grains.
Spicules (Fig. 4). Megascleres. Erect or slightly curved
oxeas, ending in a very short tip. Its axial channel can be
noticed. Some spicules present deformations such as central enlargements, junction of one of the ends, in which one
of them is atrophied and even some of the spicules have
become styles. Spicules of the shaft shorter than apical or
root areas. Size: 215 − 400.43 − 580 × 5 − 14.37 − 22.5 µ
m. Microscleres. Palmate isochelae with side alae slightly
longer than its front palms. These have a triangular aspect
with slightly rounded edges. In the centre of the palm, a
small fold that points at the outer part of the spicule can be
clearly noticed. The shaft is straight. Size: 35 − 52.35 − 7
5 × 12.5 − 19.55 − 27.5 µm. Microxeas are mostly frequent
in the lower part of the sponge with similar appearance to
the root of a plant. Spicules are straight, with slightly erect
pointed ends, not found in the sample from Marguerite Bay.
Size: 47.5 − 131.87 − 257.5 µm long.
To date, 20 valid species of Isodictya are present in the
Southern Ocean and South Atlantic (Goodwin et al. 2016).
The peculiar morphology of the collected specimens is
similar to the design of Isodictya delicata var. megachela
described by Koltun (1964). The spicular dimensions of the
specimen of Bentart 03 and paratypes 1 and 2 are slightly
shorter than the ones given by Burton (1934), Koltun (1964)
and Desqueyroux (1975) in their descriptions of I. delicata
var. megachela, who, in any case, did not report the presence
of microxeas (Table 1). In the current specimens studied, an
additional spicular category was also observed, the microxeas, which were never described in the other Isodictya species from the Southern Ocean.
Most Isodictya species present in the Southern Ocean
have oxeas as main spicules and its microscleres are isochelae and canonochelae (genus Cercidochela Kirkpatrick
(1907), synonymised by Hajdu and Lobo-Hajdu 2002 with
Isodictya). To our knowledge, the presence of additional
microscleres has only been recorded in Isodictya erinacea
(Topsent 1916) and Isodictya toxophila Burton (1932). For
I. erinacea, the presence of raphides was common in the
preparation of the type, but in other specimens studied, their
presence could not be confirmed. In the case of I. toxophila,
the presence of toxas could be corroborated in all the specimens that were preserved in good condition (Ríos 2006).
The original description of Isodictya delicata var. megachela was carried out using two specimens; the holotype
(887A) is flabellate and stipitate with even but coarsely hispid surface, and oscules arranged in linear series along the
margin of the sponge. The other specimen (889) was very
similar in shape as the one determined by Stephens (1915) as
Homoeodictya compressa (Esper 1794) from South Africa,
but it had the same skeleton and the spicular dimensions
matched those of the I. delicata var. megachela holotype. I.
delicata (Thiele 1905) differs in the dimensions of the size
of isochelae (Burton 1934).
As Burton (1934) never made any illustration of I. delicata var. megachela and the picture drawn by Koltun (1964)
was similar to what has been observed in our specimens, we
proceeded to the study the type of this species. Some photographs of the preparations of the paratype sent from the
NHM of London were taken and the spicules were observed
using SEM (Fig. 5). These did not match with the new species; in the case of the preparations of the paratype, it can
be seen a skeletal arrangement and isochelae are similar to
those in Isodictya bentarti Ríos et al. (2004). However, it
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Table 1 Comparison of spicule sizes between Isodictya delicata var. megachela Burton (1934) and Isodictya filiformis sp. nov
References
Burton (1934) (I.
delicata var. megachela)
Koltun (1964) (I.
delicata var. megachela)
Desqueyroux (1975)
(I. delicata var.
megachela)
Bentart 03 (Isodictya filiformis sp.
nov.) Holotype
Bentart 06 (I.
filiformis sp. nov.)
Paratype 1
Ecoquim 06 (I.
filiformis sp. nov.)
Paratype 2
Bentart 06 (I. filiformis sp. nov.)
Morphology
Flabellate and
stipitate
400–520
Microscleres (µm)
Isochela
70
Fan-shaped, borne
on a stalk
400–520 × 17–20
54–63
Costa Knox and
George V
920
Flabellate and
stipitate
390 × 14
57
Deception Island
45
Filiform
265–380.8–
460 × 7.5–12.15–
15
270–380.6–
430 × 10–15–
18.75
215–334.16–
430 × 7.5–12.66–
17.5
430–519.4–
580 × 5–18–22.5
35–47.37–
52.5 × 12.5–
15.99–20
37.5–46.2–
57.5 × 12.5–18.5–
22.5
40–50.43–
57.5 × 15–20.75–
25
57.5–65–
75 × 20–23.2–27.5
47.5–70.45–92.5
Peter I Island
208–210
157.5–212.75–
257.5
Low Island
97
47.5–50.83–55
Deception Island
113
No found
Marguerite Bay
159
Filiform
Filiform
Filiform
Megascleres (µm)
Oxea
also possesses sigmas, spicules that are not present in I. bentarti and I. filiformis sp. nov. The spicules observed in the
fragment from the paratype, the same isochelae as those of
I. kerguelenensis were observed as prevailing, therefore they
seem to be two different species and, in any case, they are
different from I. filiformis sp. nov.
I. filiformis sp. nov. is characterized by its fragile and thin
morphology and by the fact that it has microxeas as additional microscleres. Its presence in Pedro I Island is quite
significant as this is 390 km away from the nearest coast in
Bellingshausen Sea and very few taxonomical results have
been published in this area (Klages et al. 1995; Eakin et al.
2009), as it has been seldom visited by scientific expeditions.
However, the Bentart 03 Expedition seems to indicate that
it has a wide variety of benthic organisms, in contrast to the
deep adjacent areas of Bellingshausen Sea.
Phylogenetic analyses
In our analyses, 18S showed more resolution for family level
relationships than 28S within Poecilosclerida (Thacker et al.
2013). The Maximum Likelihood analysis of 18S place I.
filiformis sp. nov. in a well-supported clade with four other
species of Isodictya: I. kerguelenensis, I. frondosa (Pallas
1766), and I. compressa (Esper 1794), and the type species I. palmata (Ellis and Solander 1786). In addition, the
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Locality
Depth (m)
Seymour Island,
Graham Land
150
Microxea
species Amphilectus fucorum (Esper 1794), which belongs
to the family Esperiopsidae, Hentschel (1923), also clustered with Isodictya species (Fig. 6a). Similarly, the phylogenetic hypothesis for 28S place I. filiformis sp. nov. and I.
kerguelenensis closely related to A. fucorum and all the rest
of Isodictya species forming a monophyletic group (Fig. 6b).
Previously, a close relationship of the families Isodictyidae
and Esperiopsidae was obtained using 18S and 28S (Redmond et al. 2013; Thacker et al. 2013). Morphologically,
the choanosomal skeleton of Esperiopsidae consists of a
reticulation of tracts of styles, without a special ectosomal
skeleton. Microscleres, if present, are palmate isochelae and/
or sigmas (Van Soest and Hajdu 2002). In turn, the Isodictyidae have (plumo)reticulate skeletal architecture, formed by
thick tracts of oxeas, and rarely styles. The ectosomal skeleton is a dense tangential reticulation of strongyles or tufts
of oxeas or styles. (Hajdu and Lôbo-Hajdu 2002). In light
of our and previous results (Redmond et al. 2013; Thacker
et al. 2013), it seems necessary to undertake a revision of
Esperiopsiidae & Isodictyidae, and to obtain sequences of
type species of the genera of both families to understand
clearly their relationships.
Interestingly, in the 18S topology, the species Isodictya ectofibrosa (Lévi 1963) was not recovered within the
Isodictyidae clade, but as sister group of the families Coelosphaeridae Dendy (1922) and Hymedesmiidae Topsent
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Fig. 5 Isodictya delicata var.
megachela Burton (1934).
Natural History Museum of
London (NHM): 33.3.17.7a.
a, b, Paratype, fragment of the
NHMUK 1933.3.17.7 specimen
to take the photographs with the
Scanning Electron Microscope. c, Slide of the Paratype.
d–f, Skeleton. g, Isochelae and
sigma. h, Isochela. i, Oxea. j, k,
Isochelae
(1928), as in Redmond et al. (2013). In fact, the spicules in
I. ectofibrosa make it more similar to known Hymedesmiidae, and therefore a review of its status might be necessary. Neither in the phylogenetic hypothesis for 18S or 28S
the relationship of the clade formed by family Isodictyidae
(and Esperiopsidae) could be resolved (Fig. 6a). While in
the topology of the 18S seemed to be a sister clade to the
rest of families of Poecilosclerida except for Lévi (1963)
(Fig. 6a), in that of 28S (Fig. 6b), they appeared to be
closely related to a clade formed by the families Myxillidae Dendy (1922), Coelosphaeridae Dendy (1922), and
Tedaniidae (Ridley and Dendy 1886).
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a
Halichondria bowerbanki
100
Order SUBERITIDA
Halichondria magniconulosa
Family Crambeidae
Monanchora arbuscula
Amphilectus fucorum
Isodictya palmata
86
100
Family Esperiopsidae
Isodictya kerguelenensis Actiquim_103
100
Isodictya filiformis PAR2
98
100
Family Isodictyidae
Isodictya compressa
Isodictya frondosa
100
Guitarra sp.
99
Family Guitarridae
Guitarra antarctica
93
Mycale alagoana
100
Family Mycalidae
Mycale rotalis
90
Clathria barleei
93
Lissodendoryx isodictyalis
82
Family Microcionidae
Family Coelospheridae
Myxilla anchorata
Trachytedania cf. ferrolensis
18S rDNA
Family Myxillidae + Tedaniidae
Myxilla incrustans
Phorbas dives
78
84
Family Hymedesmiidae
Phorbas punctatus
Phorbas plumosus
Myxilla fimbriata
Family Myxillidae
Isodictya ectofibrosa
Plocamionida ambigua
82
*
Family Hymedesmiidae
Phorbas amaranthus
Hamigera hamigera
Family Coelosphaeridae
Lissodendoryx jenjonesae
Hemimycale columella
Crella rosea
79
98
Order POECILOSCLERIDA
Latrunculia lunaviridis
0.07
Family Hymedesmiidae
Crella elegans
Crella plana
Polymastia thielei
Sphaerotylus sp.
Polymastia tenax
Axos flabelliformis
1 0 0 Trachycladus stylifer
Trachycladus sp.
100
Halichondria bowerbanki
Halichondria panicea
Mycale laevis
Mycale titubans
95
Monanchora arbuscula
Monanchora unguiculata
Guitarra fimbriata
Order POLYMASTIIDA
Order AXINELLIDA
Order TRACHYCLADIDA
Order SUBERITIDA
78
94
91
100
94
Mycale macilenta
Mycale subclavata
Mycale rotalis
100
87
Phorbas punctatus
Phorbas bihamiger
Crella incrustans
Lissodendoryx arenaria
Phorbas dives
Spanioplon armaturum
Plocamionida ambigua
Lissodendoryx jenjonesae
Lissodendoryx fibrosa
97
Lissodendoryx fibrosa 2
Lissodendoryx sp.
Acanthanchora sp. n.
Crella rosea
75
Crella elegans
Antho sp.
Clathria barleei
Antho inconstans
Antho involvens
Clathria armata
Clathria reinwardti
Echinoclathria dichotoma
Clathria eccentrica
Echinochalina sp.
Zyzzya fuliginosa
9 8 Tsitsikamma pedunculata
Latrunculia lunaviridis
Lissodendoryx sigmata
Lissodendoryx colombiensis
Tedania tubulifera
Tedania strongylostyla
Forcepia sp.
Trachytedania cf. ferrolensis
Myxilla anchorata
Myxilla cf. rosacea
Isodictya grandis
100
Isodictya frondosa 1
Isodictya frondosa 2
Isodictya compressa
F. Esperiopsidae
Amphilectus fucorum
70
Isodictya filiformis PAR2
9 6 Is o d ic t y a k e r g u e le n e n s is Ac t iq u im_ 1 0 3
Mycale setosa
Mycale mirabilis
Family Mycalidae
Family Hymedesmiidae
85
0.1
Family Microcionidae
28S rDNA
78
Family Acarnidae
Family Latrunculiidae
Families Coelosphaeridae + Tedaniidae
Family Isodictyidae
Order POECILOSCLERIDA
82
b
Fig. 6 Phylogenetic hypotheses for the relationships of Isodictya filiformis sp. nov. within the order Poecilosclerida using 18S rDNA (a) and 28S
rDNA (b). The phylogeny was obtained with Maximum Likelihood (bootstrap values over branches, only > 60 shown)
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Acknowledgements We are grateful to Clare Valentine of the Natural
History Museum of London (NHM) who kindly provided the material
of material Isodictya delicata var. megachela NHMUK 1933.3.17.7
(wet specimen) and NHMUK 1933.3.17.7a (slide) for examination. We
would like to thank the crew and UTM technicians of R/V ‘Hespérides’,
who helped in the collection of samples, Ana Ramos and the colleagues
of BENTART team and to Manuel Ballesteros, Conxita Avila and
Laura Núñez-Pons, colleagues of ECOQUIM and ACTIQUIM, who
helped in several parts of this work. We also thank the reviewers for
their constructive comments to a previous version of this manuscript.
Funding This study was funded by the BENTART projects: Spanish
Ministry of Science and Technology REN2001-1074ANT, REN200301881/ANT, REN2003-00545/ANT and MEC CGL2004-21066-E
and a contribution to the ECOQUIM-2 (CGL2004-03356/ANT) and
ACTIQUIM (CGL2007-65453/ANT) projects. The ‘BENTART-06′
cruise was funded by the Antarctic Programme GLC2004-01856/
ANT of the Spanish Government. Sequencing was performed using
internal funds to AR at the Natural History Museum of London (DIF:
SDF14029).
Compliance with ethical standards
Conflict of interest The authors declare that they have no conflict of
interest.
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