ZooKeys 298: 39–76, doi: 10.3897/zookeys.298.1913
Revision of the genus Placospongia (Porifera, Demospongiae, Hadromerida, Placospongiidae) in the Indo-West Pacific
Leontine E. Becking 1,2,†
1 Naturalis Biodiversity Center, Marine Zoology Department, PO Box 9517, 2300 RA Leiden, The Netherlands
2 IMARES - Institute for Marine Resources and Ecosystem Studies, P.O. Box 57, 1780 AB Den Helder, The Netherlands

Corresponding author: Leontine E. Becking (lisa.becking@naturalis.nl; lisa.becking@wur.nl)

Academic editor: R. Pronzato

received 15 August 2011 | accepted 2 April 2013 | Published 13 May 2013


(C) 2013 Leontine E. Becking. This is an open access article distributed under the terms of the Creative Commons Attribution License 3.0 (CC-BY), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.


For reference, use of the paginated PDF or printed version of this article is recommended.

Abstract

Species of the genus Placospongia are common within the tropical Indo-West Pacific, demonstrating a wide variety of colors and either branching or encrusting growth forms. A revision of Indo-West Pacific Placospongia was undertaken based on a redescription of the holotypes of species of Placospongia from the Indian Ocean and Western Pacific and an examination of an additional 103 specimens of Placospongia ssp. collected from Indonesia (including Vosmaer and Vernhout 1902 material), Seychelles, India, Singapore and Micronesia. One mitochondrial (COI) and one nuclear (ITS) marker were subsequently used to differentiate species. All Placospongia species are characterized by selenasters and tylostyles in two size classes. The combination of microsclere diversity and morphology as well as megasclere size were shown to be informative morphometric characters, supported by molecular evidence. Live coloration and growth form is shown to be unreliable for diagnoses. The study of holotypes found that Placospongia mixta is a valid species and that two genus transfers are necessary: Geodinella anthosigma is a Placospongia and Placospongia labyrinthica is a Geodia. A new species is also described from an anchialine pool in Indonesia, Placospongia santodomingoae sp. n.; bringing the total fauna of Placospongia species in the Indo-West Pacific to five: Placospongia anthosigma, Placospongia carinata, Placospongia mixta, Placospongia melobesioides, and Placospongia santodomingoae sp. n. An identification key is given. Two additional species, possibly morphologically cryptic, have been identified by molecular markers.

Keywords

Sponge, Indonesia, marine lake, coral reef, mangrove, anchialine pool, ITS, COI

Introduction

Species of the genus Placospongia in the tropical Indo-West Pacific occur in a wide variety of habitats such as marine lakes, coral reefs and mangroves. They may display a variety of colors and growth forms, from encrusting to branching (Figs 1, 2). Generally only two species have been recorded in species checklists within the Indo-West Pacific (e.g. Burton 1959, Hooper and Wiedenmeyer 1994, Hooper et al. 2000, Becking et al. 2006, de Voogd et al. 2008, de Voogd et al. 2009): Placospongia melobesioides Gray 1867, and Placospongia carinata (Bowerbank 1858). A recent collection of over 100 Placospongia specimens during fieldtrips by the author to Indonesia in 2006 (Sulawesi), 2007 (Papua), 2008, 2009 (Berau), and to Micronesia in 2010 (Yap) revealed, however, that there were more than two species present in these faunas.

The taxonomic literature records six valid species of Placospongia worldwide, of which there are three from the Indian Ocean and Western Pacific: Placospongia carinata (type locality “South Sea”, presumably in the Pacific), Placospongia labyrinthica Kirkpatrick 1903 (type locality East London, South Africa, Indian Ocean), Placospongia melobesioides (type locality Borneo, Pacific). In 1900 Thiele described the species Placospongia mixta from Ternate (Indonesia), which was later synonymized with Placospongia carinata by Vosmaer and Vernhout in 1902. Vosmaer and Vernhout (1902) based their conclusions on a review of 26 specimens collected during the Siboga expedition to Indonesia, and this collection is presently housed at the Naturalis Biodiversity Center (Leiden, The Netherlands). Subsequently, according to the World Porifera Database (van Soest et al. 2011) Geodinella anthosigma Tanita and Hoshino 1989 (type locality Sagami Bay, Japan) should be transferred to the genus Placospongia, and Placospongia labyrinthica should in fact be transferred to the genus Geodia. These suggested genus transfers have, however, not yet been published in the peer-reviewed literature. A molecular phylogeny constructed using the internal transcribed spacer region (ITS) indicated that there were nine evolutionary lineages worldwide within the genus Placospongia of which there were five distinct clades in the Indo-Pacific (clades C3, C4, C5, C6 & C9) that may represent five species (Nichols and Barnes 2005). The authors did not investigate the spicule morphology of the specimens in their study, therefore it is unclear which species name can be assigned to the different clades.

The objectives of the present study were to revise the genus Placospongia in the Indo-West Pacific by examining the holotypes of Placospongia melobesioides, Placospongia carinata, Placospongia mixta, as well as 103 specimens of Placospongia spp. that were collected from Indonesia (including the Vosmaer & Vernhout material), Singapore, Seychelles, Madagascar, and Micronesia. In order to obtain a full view of the species from the Western Pacific and Indian Ocean the holotypes of the temperate species Geodinella anthosigma, and Placospongia labyrinthica were also examined. Subsequently it was determined if growth form and color can be used as diagnostic characteristics to identify different species of Placospongia in the field. Finally, the aim was to provide species names to the five clades of Indo-Pacific Placospongia as published by Nichols and Barnes (2005) by combining their published ITS sequences from GenBank with ITS sequences from identified species of Indo-Pacific Placospongia.

Material and methods

Specimens from Indonesia were collected via snorkeling in marine lakes and mangroves, and scuba diving in reefs. For a detailed description of marine lakes in Indonesia see Becking et al. (2011). Where possible material was preserved in 96% ethanol for DNA analysis, and voucher specimens were preserved in 70% ethanol and deposited in the collections of the Naturalis Biodiversity Center, Leiden, The Netherlands (RMNH POR.). Records were made on the external morphology, skeletal architecture and spicules of all material. Spicule dimensions were measured of a subset of specimens indicated in Table 1, based on 25 measurements (unless noted otherwise) and given in the text as minimum-average-maximum. The following dimensions were measured: tylostyles length × shaft width × head width; selenasters length × width; streptasters total length × ray length; spherasters diameter; rhabds length × width. Only fully developed spicules were measured. To study the skeletal architecture hand-cut perpendicular sections of the choanosome were made. The sections were air-dried, mounted in Durcupan® ACM on a microscope slide, and studied under a Leica high power microscope. Spicule preparations were made by dissolving the organic tissue of a small fragment of the specimen in commercial bleach, after which the spicules were washed >10 times with distilled water and once with 96% ethanol. The spicules were air-dried on microscope slides and mounted with Durcupan® ACM. The spicules were also mounted on aluminium stubs, coated with gold-palladium and studied with a Jeol Scanning Electron Microscope.

Table 1.

Measurements of spicules of Placospongia carinata, Placospongia melobesioides, Placospongia mixta, and Placospongia santodomingoae sp. n. Sample location, growth form, color and spicule measurements provided per specimen. Spicule dimensions are based on 25 measurements and given in the text as minimum-average-maximum. Spheraster measurements in Placospongia melobesioides based on less than ten measurements, due to low of abundance in specimens.

tylostyle blunt end tylostyle sharp end selenaster spheraster streptaster microrhabd
growthform color live length max width head width length max width head width length width diameter total length length ray length width
Placospongia carinata
R122b-86g-BK1390 (holotype) 500-710.4-800 10-13.4-15 10-15.3-18 140-317.4-450 5-8.4-12.5 8-9.3-13 80-90-98 60-71.3-85 23-33.8-43 8-11.6-15 8-12.0-18 2.5
RMNH POR. 4482 branching orange 660-726-800 10-12.3-15 10-14.5-18 180-263-410 3-5-7.5 8-7.5-8 65-71.5-75 50-58.5-65 15-34-48 10-13.0-15 8-11.7-15 2.5
RMNH POR. 4483 encrusting light brown 610-703.8-800 10-13.1-15 13-14.9-18 190-286.7-470 5-6.4-10 5-8.6-13 60-80-85 60-62.9-70 20-33.7-40 10-13.2-15 8-11.9-18 2.5
RMNH POR. 4484 encrusting cream 560-709.16-920 8-11.7-18 10-13.9-18 175-267.1-550 3-4.4-10 5-6.4-13 50-61.8-70 35-47.4-55 25-29.7-35 8-11.0-15 10-13.3-18 2.5
RMNH POR. 4485 branching dark brown 550-761.2-930 10-14-18 13-15.5-18 210-295.2-450 3-5.6-8 5-7.6-10 28-63-73 38-50-58 20-27.6-38 5-9.0-13 5-9.4-13 <2.5
RMNH POR. 744 encrusting purple 450-748.6-980 8-11.1-13 10-13.2-15 195-256.8-550 5-6.2-10 5-6.7-8 60-66.3-70 50-55.6-65 25-29.9-38 10-12.918 8-10.8-13 <2.5
RMNH POR. 754 encrusting white 540-705.8-830 10-12.8-15 13-15.2-18 280-355.5-500 5-7.0-10 5-8.6-13 55-67.7-75 45-51.8-55 25-30.9-38 8-9.5-13 8-12.3-18 2.5
RMNH POR. 755 encrusting cream 560-764.7-910 8-12.2-15 10-14.7-18 250-311.8-360 5-7.3-8 5-8.2-10 55-61.1-65 38-47.5-55 30-32.9-38 8-9.8-13 8-10.2-13 2.5
ZMA Por. 10727 encrusting - 620-738.7-840 8-11-13 13-15.5-18 240-258.3-270 3-3.3-5 3-4.6-8 50-58.8-78 35-42.5-63 25-27.6-38 8-11.1-15 8-8.1-10 <2.5
ZMA Por. 9189 branching - 550-703.3-820 10-12.8-15 13-15-18 210-318.8-410 5-7.5-10 5-9.7-13 63-72.2-78 50-56.8-65 30-35-48 8-10.7-15 8-9.2-13 2.5
Placospongia melobesioides
BMNH52.4.1.14 (holotype) branching dark brown 670-879.6-1010 10-13.2-18 10-16.3-20 205-293.4-420 5-9.9-13 5-9.9-13 58-63.1-68 45-51.7-68 15-16.8-18
RMNH POR. 4495 encrusting dark brown 480-717.6-1040 5-9.5-15 8-10.3-15 190-297.6-370 3-5.8-8 3-6.1-8 45-56.6-70 30-41.6-50
RMNH POR. 4496 branching dark brown 580-778.4-900 8-11.7-15 10-14.1-18 230-272.8-400 5-7.4-10 8-9.1-10 45-60-75 35-45-63
RMNH POR. 4497 branching dark brown 620-745.2-860 10-12.2-15 13-14.8-18 250-320.8-450 5-8.8-10 5-9.4-13 63-70.8-83 45-59.6-65
RMNH POR. 3935 encrusting dark brown 460-660.9-760 10-11.6-15 10-13.7-18 210-325.8-450 3-7.4-13 3-8.3-13 45-63.9-70 38-51.3-60 15-20
RMNH POR. 3166 encrusting dark brown 460-704.8-810 8-11.4-13 10-13.2-15 200-288-470 3-9.5-13 5-10.8-15 60-63.6-70 50-50.2-55
RMNH POR. 3976 branching dark brown 600-793.6-910 10-12-15 13-14-18 190-321.2-450 5-8.5-13 5-9.6-13 48-66.8-75 48-55.2-65
RMNH POR. 3977 branching brown 510-683.6-780 10-11.5-13 13-13.9-15 200-326-450 5-7.5-10 8-9.5-13 58-63.3-68 40-46-53
RMNH POR. 758 branching purple 630-853.2-1020 10-13.3-15 13-15.8-18 210-253.2-310 5-9.5-13 8-11.8-15 50-55.2-62.5 35-42.3-50 15
RMNH POR. 757 branching white 550-829.2-960 10-13.3-16 13-15.8-18 260-302.1-370 8-9.6-13 10-11.2-15 55-60.4-65 43-48.0-53
RMNH POR. 2464 branching - 710-933.4-1080 12.5-15-17.5 13-15.7-20 240-326.7-330 5-9.2-13 5-10.8-15 67.5-81-87.5 60-72.5-85
ZMA Por. 10459 branching brown 520-670.8-820 7.5-11.4-12.5 10-13.4-17.5 310-362.5-430 5-8.8-10 5-10.1-13 62.5-68.9-72.5 50-55.5-65
Placospongia mixta
ZMB3204 (holotype) encrusting - 355-672.4-940 8-12.1-18 8-15.6-20 165-226.4-275 3-6.1-8 3-7.8-10 55-69.8-75 43-55.4-73 20-25-30 15-23.9-33 3-7.6-13 5-7.1-10 <2.5
RMNH POR. 4112 encrusting red 480-870-1040 10-12.7-15 13-15.8-28 210-288-410 5-6.2-10 5-7.2-10 50-66.6-75 38-50.7-58 18-20.2-25 18-23.7-35 5-6.4-10 5-6.4-10 <2.5
RMNH POR. 4113 encrusting cream 550-817.6-1030 10-13.1-15 13-15.6-18 160-260-350 5-7.3-10 5-8.2-12.5 62.5-66-70 45-53-57.5 20-22.1-25 20-24.8-30 5-5.7-8 5-7.5-10 2, 5
RMNH POR. 742 branching red 550-759.2-850 10-11.9-15 10-14.9-20 120-230-380 3-5.9-10 3-7.6-10 50-65.4-73 33-46.5-56 22-23.4-25 15-22.2-35 2-5.7-8 5-7.4-10 <2.5
RMNH POR. 4489 encrusting cream 630-886.6-1010 10-12.9-15 13-15.4-19 175-221.5-320 3-3.9-8 2-7.2-10 60-68-75 43-50.8-58 18-20.6-25 20-26.1-35 8-10.8-15 8-8.5-10 <2.5
RMNH POR. 4490 encrusting cream 510-727.6-970 8-13.120 13-16.3-23 150-240-310 3-5.3-8 2-6.4-8 55-70.4-83 40-53.3-65 13-20.5-25 15-21.7-30 5-6.4-13 8-9.2-13 <2.5
RMNH POR. 4491 encrusting brown 780-1001.4-1200 10-14.8-18 15-17.5-20 240-284-350 5-6.3-8 5-8.3-10 60-71-75 48-57.5-63 18-23-25 20-27.3-35 5-7-10 5-6.3-8 2, 5
RMNH POR. 4492 encrusting white 610-995.8-1250 10-16-20 13-19-25 260-274-290 8-9-10 8-9-10 58-71-78 45-54.6-70 15-20.2-25 18-24.8-33 10-11.2-15 5-8.6-18 <2.5
RMNH POR. 3158 encrusting cream 550-990-1210 13-16.9-20 13-17.5-20 130-267.8-400 5-8.8-15 8-9-10 65-71-75 50-56.5-63 23-23.8-25 23-28.4-35 5-8.7-13 5-6.6-8 <2.5
RMNH POR. 745 encrusting red 760-914.1-1030 13-17-23 10-18-25 250-366.6-480 3-8-13 3-9-13 45-73.6-80 45-60-70 20-23.9-25 20-23.7-30 3-6.4-9 5-7.5-10 <2.5
RMNH POR. 4493 encrusting brown 460-761.6-1070 10-14.6-23 13-17.38-25 220-323.6-430 8-9.1-13 10-11.3-15 73-80.3-85 53-65.3-73 20-26.5-30 18-23.4-30 15-8.1-10 8-8.7-13 <2.5
RMNH POR. 4494 encrusting brown 540-758-900 10-12.2-18 10-13.8-20 180-216.9-350 3-3.3-5 4-4.4-8 50-59.1-68 35-42.3-58 15-20.9-28 23-26.9-30 8-10.4-13 8-8.5-10 <2.5
Placospongia santodomingoae sp.n.
RMNH POR. 4486 (holotype) branching brown 430-605.6-660 13-15.5-20 13-18.1-23 240-261.3-290 5-7.2-8 5-8.8-10 80-84.8-90 60-67.3-75 8-12.3-18 2.5-2.7-3.5
RMNH POR. 4487 branching orange 530-652.4-740 13-16-20 15-18.0-23 220-274.7-310 5-8.2-13 8-9.5-15 63-82.9-93 60-66.3-73 5-10.5-20 2.5-2.6-3.5
RMNH POR. 4488 branching orange 480-633.2-760 15-17.2-20 18-19.6-23 190-273.2-380 5-7.9-10 8-10.3-13 80-87-93 58-69-75 8-13.5-18 2.5-2.9-3.5

DNA extractions were made with Qiagen DNEasy animal blood and tissue extraction kit following the manufacturer’s protocol. The polymerase chain reaction (PCR) reaction volume was 25 μ l and contained 5 μ l Phire ® Hot Start reaction buffer, 1 unit Hotstart Phire® Hot Start DNA polymerase (Finnzymes), 2 μ l 1 mM dNTPs (Gibco), 1 μ l DNA template (5-20 ng) and 0.625 μ l of 10mM each primer. The standard DNA-barcoding fragment of the mitochondrial cytochrome oxidase subunit I (COI) fragment was amplified by using a specific forward primer designed by the author for Placospongia P-COI-F: GCA GG ATG ATA GGA ACA GGW TTT AG and the degenerated reverse primer from Folmer et al. (1994) designed by Meyer et al. (2005): dgHCO2198: TAA ACT TCA GGG TGA CCA AAR AAY CA. Temperature regime: 94°C for 30s; followed by 35 cycles of 94°C for 5s; 50°C for 5s; 72°C for 12 s; followed by 71°C for 1 min). ITS was amplified with primers from Wörheide (1998) RA2: GTC CCT GCC CTT TGT ACA CA and ITS2.2: CCT GGT TAG TTT CTT TTC CTC CGC). PCR products were purified and sequenced by Macrogen Inc (Korea and The Netherlands). The poriferan origin of the obtained sequences was verified through BLAST searches (http://blast.ncbi.nlm.nih.gov/Blast.cgi). Sequences were handled in SEQUENCHER 4.10.1 (Gene Codes Corporation) and aligned with CLUSTALW and MUSCLE implemented in DAMBE (Xia and Xie 2001). Species of the family Spirastrellidae were selected as outgroup for the phylogenetic analyses. For the COI genetree four specimens of Spirastrella aff. decumbens (RMNH POR. 4505, 4589, 4614) were taken. For the ITS genetree sequences of species from Spirastrellidae were taken from GenBank, as well as ITS sequences of Indo-Pacific Placospongia spp. from the study by Nichols & Barnes (2005), for GenBank accession numbers see Figure 11. The best-fit DNA substitution model was selected by the Akaike Information Criterion deployed in jMODELTEST v. 0.1.1 (Posada 2008) and this model (HKY for COI and GTR+G+I for ITS) was used for subsequent Bayesian and maximum likelihood phylogeny inferences. Phylogenetic reconstructions were performed under Bayesian inference criteria implemented in MrBayes v. 3.1.2. (Huelsenbeck and Ronquist 2001). Each analysis comprised two independent runs of four Metropolis-coupled Markov-chains, sampled at every 1000th generation at the default temperature (0.2). Analyses were terminated after the chains converged significantly as indicated by an average standard deviation of split frequencies <0.001. Convergence was also checked in Tracer v. 1.5.0 (Rambaut and Drummond 2007). For comparison, maximum likelihood bootstrap analyses were conducted using MEGA v. 5.01 (Tamura et al. 2011) using a heuristic search with 1000 bootstrap replicates. Within-group and between-group uncorrected p- distances were calculated in MEGA.

Abbreviations used in this manuscript: Naturalis Biodiversity Center, Leiden, The Netherlands (RMNH POR.), the Zoological Museum of the University of Amsterdam (ZMA Por.), Zoologisches Museum für Naturkunde an der Universität Humboldt zu Berlin, Berlin, Germany (ZMB), The Natural History Museum, London, United Kingdom (BMNH).

Taxonomy
Phylum Porifera Grant, 1836 Class Demospongiae Sollas, 1885 Order Hadromerida Topsent, 1894 Family Placospongiidae Gray, 1867 Genus Placospongia Gray, 1867
Placospongia Gray, 1867

http://species-id.net/wiki/Placospongia

Type species:

Placospongia melobesioides Gray, 1867 by monotypy

Description, amended from Systema Porifera (Hooper and van Soest 2002).

Encrusting to branching growth forms. Small encrustations of 3 cm2 to large surfaces of >2m2 to branching individual with total size of up to 45cm in length and branch diameter between 0.25-1.5cm. Total size of specimens is hard to establish as parts of the body may be encrusting within cracks. Dried material is hard, alcohol preserved and live specimens remain compressible as the choanosome is of more pliant material than the cortex. The surface is made up of smooth cortical plates separated by contractible grooves which form a kind of network on the surface while these are firmly closed in preserved specimens. See Vosmaer and Vernhout (1902) and Rützler (2002) for an extensive description of the genus. In live specimens grooves are open and oscules are visible inside contractile ridges, running between plates. Live color white, cream, orange, reddish brown to dark black-brown (Fig. 1, 2) and come color is usually retained after alcohol preservation. The contact lines between the plates ridge up slightly and are generally a different shade of the color of the plates.

Skeleton. The cortical plates consist of densely packed selenasters and can also contain auxiliary microscleres. Developmental stages of selenasters occur throughout the choanosome. Tylostyle tracts support the margins of the cortical plates. In branching specimens radial tylostyle tracts run from the centre core (consisting of densely packed selenaster) to the cortical plates, in encrusting specimens tracts run in direction from substrate to cortex. The sharp ends of the smaller tylostyles are projected beyond the cortex surface. Microscleres occur in the cortex and scattered in choanosomal skeleton. For a detailed description of external morphology and anatomy see Vosmaer and Vernhout (1902).

Spicules. Megascleres are tylostyles in two size classes, microscleres are selenasters, and can include choanosomal and ectosomal spirasters (slender-spined streptasters and acanthose microrhabds), spherasters, and/or spherules. Selenasters often remain pigmented after treatment with bleach or nitric acid.

Figure 1.

In situ underwater images of Placospongia spp. in Indonesia, displaying natural variation in color and growth form of live specimens. A Placospongia mixta (by L.E. Becking) B Placospongia carinata (by L.E. Becking) C Placospongia carinata (by L.E. Becking) D Placospongia melobesioides (by N.J. de Voogd).

Figure 2.

Gradation of external coloration in preserved specimens. A Placospongia mixta RMNH POR. 4492 B Placospongia mixta RMNH POR. 4113 C Placospongia carinata RMNH POR. 4482 D Placospongia carinata RMNH POR. 4483 E Placospongia mixta RMNH POR. 3979 F Placospongia melobesioides RMNH POR. 4114.

Placospongia anthosigma (Tanita & Hoshino, 1989)

http://species-id.net/wiki/Placospongia_anthosigma

Figure 3
Geodinella anthosigma Tanita & Hoshino, 1989: fig. 16, Plate III fig. 1
Material examined.

Holotype. NSMT-Po R288 (National Museum of Nature and Science, Tokyo, Japan), Japan, Kannonzuka-dashi, Amadaiba, Sagami Bay, 62–67m. depth.

Description.

HolotypeNSMT-Po R288 encrusting specimen in three pieces of 1–2cm2 and 5mm thick, beige to pink in alcohol (Figure 3A).

Spicules. Megascleres large tylostyles with blunt point 520-797-930 × 15-18-20 × 18-20-23 μ m, small tylostyles with blunt point 250-320-410 × 10-12-18 × 13-14-18 μ m; microscleres selenasters 85-90-98 × 70-73-80 μ m, spherasters 15-19-25 μ m, stout spirasters with two or three contortions and acanthose spines spirally placed on shaft 8-11-18 × 3-4.5-5 μ m (Fig. 3)

Skeleton. As description of genus with addition that spirasters form a layer over and amidst the selenaster cortex and are also prevalent in choanosomal tissue. Spherasters amidst selenaster cortex and dispersed in choanosome.

Figure 3.

Placospongia anthosigma holotype (NSMT-Po R288) A type specimen (image taken from website database of the Museum of Nature and Science, Tokyo, Japan) B selenaster C large tylostyle (head and blunt end) D spheraster E spirasters referred to as ‘anthosigma’ by Tanita & Hoshino (1989).

Distribution.

Typelocality Sagami Bay, Eastern Japan, presently not recorded from any other locality.

Ecology.

On rock substrate in deep temperate waters.

Remarks.

Originally described by Tanita and Hoshino (1989) as Geodinella anthosigma. Geodinella is no longer a valid genus. Geodinella anthosigma should be transferred to the genus Placospongia based on the external morphology with the characteristic cortical plates and the presence of selenasters, tylostyles and spherasters. Placospongia anthosigma is distinguished from the other Indo-Pacific Placospongia spp. by the presence of contorted, spirally ornamented spirasters referred to by Tanita and Hoshino (1989) as ‘anthosigma’ and the small class of tylostyles with blunt points.

Placospongia carinata (Bowerbank, 1858)

http://species-id.net/wiki/Placospongia_carinata

Figures 4, 5
Geodia carinata Bowerbank, 1858: plate XXV fig. 19.
Geodia carinata Bowerbank, 1874: plate XLVI figs 1–5.
Material examined.

Holotype. “South Sea”: BMNH R1228 - 86g - Bk.1390 (slide), R1275 - PE01 - Bk1390 (slide).

Vosmaer & Vernhout (1902), Siboga expedition: RMNH POR. 755; RMNH POR. 754; RMNH POR. 744. Other material: RMNH POR. 4484, RMNH POR. 3943, RMNH POR. 3944, RMNH POR. 4485, RMNH POR. 3945, RMNH POR. 3946, RMNH POR. 3947, RMNH POR. 3948, RMNH POR. 3949, RMNH POR. 3950; RMNH POR. 3951, RMNH POR. 3952, RMNH POR. 3953, RMNH POR. 3954, RMNH POR. 3955, RMNH POR. 4482, RMNH POR. 3956, RMNH POR. 3957, RMNH POR. 4483, RMNH POR. 3958; ZMA Por. 8813ZMA Por. 09578; ZMA Por. 11367, ZMA Por. 16584, ZMA Por. 10727, ZMA Por. 1818, ZMA Por. 10481, ZMA Por. 20735; ZMA POR.9189. (See Table 2 for full details per specimen)

Table 2.

Location details of reviewed specimens of Placospongia carinata.

registration number fieldcode country province region island locality habitat latitude longitude depth (m.) date collector
RMNH POR. 744 #1500 Indonesia Moluccas W of Aru Kur benthic hard 20-40 6.xii.1899 Siboga expedition
RMNH POR. 754 #1458 Philippines Sulu Sea Ubian islands anchorage off North Ubian lithothamnion 06°7.5'N, 120°26'E 23 28.vi.1899 Siboga expedition
RMNH POR. 755 #1848 Indonesia West Papua Raja Ampat Misool sand, stones 02°28'.5S, 131°3'.3E 32 20.viii.1899 Siboga expedition
RMNH POR. 3943 #KKB/mol716 Indonesia East Kalimantan Berau Kakaban Kakaban lake marine lake 02°08'57.3"N, 118°31'26.4"E 0-2 ix.2008 L.E.Becking
RMNH POR. 3944 #KKB/mol754 Indonesia East Kalimantan Berau Kakaban Kakaban lake marine lake 02°08'57.3"N, 118°31'26.4"E 0-2 ix.2008 L.E.Becking
RMNH POR. 3945 #KKB/mol780 Indonesia East Kalimantan Berau Kakaban Kakaban lake marine lake 02°08'57.3"N, 118°31'26.4"E 0-2 ix.2008 L.E.Becking
RMNH POR. 3946 #KKB/mol810 Indonesia East Kalimantan Berau Kakaban Kakaban lake marine lake 02°08'57.3"N, 118°31'26.4"E 0-2 ix.2008 L.E.Becking
RMNH POR. 3947 #KKB/mol814 Indonesia East Kalimantan Berau Kakaban Kakaban lake marine lake 02°08'57.3"N, 118°31'26.4"E 0-2 ix.2008 L.E.Becking
RMNH POR. 3948 #KKB/mol825 Indonesia East Kalimantan Berau Kakaban Kakaban lake marine lake 02°08'57.3"N, 118°31'26.4"E 0-2 ix.2008 L.E.Becking
RMNH POR. 3949 #KKB/mol713 Indonesia East Kalimantan Berau Kakaban Kakaban lake marine lake 02°08'57.3"N, 118°31'26.4"E 0-2 ix.2008 L.E.Becking
RMNH POR. 3950 #KKB/mol1068 Indonesia East Kalimantan Berau Kakaban Kakaban lake marine lake 02°08'57.3"N, 118°31'26.4"E 0-2 ix.2008 L.E.Becking
RMNH POR. 3951 #MA/mol700 Indonesia East Kalimantan Berau Maratua Haji Buang lake marine lake 02°12'31.2"N, 118°35'46.8"E 0-2 ix.2008 L.E.Becking
RMNH POR. 3952 #MA/mol975 Indonesia East Kalimantan Berau Maratua Haji Buang lake marine lake 02°12'31.2"N, 118°35'46.8"E 0-2 ix.2008 L.E.Becking
RMNH POR. 3953 #MA/mol947 Indonesia East Kalimantan Berau Maratua Haji Buang lake marine lake 02°12'31.2"N, 118°35'46.8"E 0-2 ix.2008 L.E.Becking
RMNH POR. 3954 #MA/mol1055 Indonesia East Kalimantan Berau Maratua Haji Buang lake marine lake 02°12'31.2"N, 118°35'46.8"E 0-2 ix.2008 L.E.Becking
RMNH POR. 3955 #MA/mol1012 Indonesia East Kalimantan Berau Maratua Haji Buang lake marine lake 02°12'31.2"N, 118°35'46.8"E 0-2 ix.2008 L.E.Becking
RMNH POR. 3956 #MA/mol1001 Indonesia East Kalimantan Berau Maratua Haji Buang lake marine lake 02°12'31.2"N, 118°35'46.8"E 0-2 ix.2008 L.E.Becking
RMNH POR. 3957 #MA/mol1009 Indonesia East Kalimantan Berau Maratua Haji Buang lake marine lake 02°12'31.2"N, 118°35'46.8"E 0-2 ix.2008 L.E.Becking
RMNH POR. 3958 #MA/mol1500 Indonesia East Kalimantan Berau Maratua Haji Buang lake marine lake 02°12'31.2"N, 118°35'46.8"E 0-2 ix.2008 L.E.Becking
RMNH POR. 4482 #MA/mol1061 Indonesia East Kalimantan Berau Maratua Haji Buang lake marine lake 02°12'31.2"N, 118°35'46.8"E 0-2 ix.2008 L.E.Becking
RMNH POR. 4483 #MA/LE172 Indonesia East Kalimantan Berau Maratua Haji Buang lake marine lake 02°12'31.2"N, 118°35'46.8"E 0-2 ix.2008 L.E.Becking
RMNH POR. 4484 #KKB/mol110 Indonesia East Kalimantan Berau Kakaban Kakaban lake marine lake 02°08'57.3"N, 118°31'26.4"E 0-2 ix.2008 L.E.Becking
RMNH POR. 4485 #KKB/mol763 Indonesia East Kalimantan Berau Kakaban Kakaban lake marine lake 02°08'57.3"N, 118°31'26.4"E 0-2 ix.2008 L.E.Becking
ZMA Por. 1818 Indonesia Maluku Banda islands Banda anchorage reef 04°32'23.3"S, 129°54'28.8"E 9-45 22.xi.1899 Siboga expedition
ZMA Por. 9578 Singapore Pulau Salu reef 01°12'59.0"N, 103°42'25.2"E 2 22.xii.1977 H. Moll
ZMA Por. 8813 Indonesia Nusa Tenggara Komodo NE cape reef 08°28'60.0"S, 119°34'4.8"E 30 19.ix.1984 R.W.M. van Soest (Snellius II Expedition)
ZMA Por. 9189 India Laccadive Islands Agatti 20-25 1987 National Institute of Oceanography
ZMA Por. 10481 Seychelles Mahé Mahé SE coast, near Pointe Cocos reef 35-45 24.xii.1992 R.W.M. van Soest
ZMA Por. 10727 Seychelles Mahé Mahé NE Point reef 04°34'59.9"S, 055°28'0.1"E 1 14.xii.1992 R.W.M. van Soest
ZMA Por. 11367 Seychelles Mahé N of Aride reef 04°10'59.9"S, 055°40'0.1"E 40 19.xii.1992 R.W.M. van Soest
ZMA Por. 16584 Seychelles Mahé Mahé SW coast, Baie Lazare, Anse Gaulettes reef 04°10'59.9"S, 055°40'0.1"E 1-4 6.xii.1992 R.W.M. van Soest
ZMA Por. 20735 Seychelles Mahé reef 1992 R.W.M. van Soest
Description.

Reviewed material is encrusting and/or branching. External morphology follows the description of the genus. Color of live specimens can be purple brown, chocolate brown, milk coffee brown, orange brown, orange, cream, or white (Fig. 1, 2). Color of choanosome is pale beige. After preservation in ethanol specimens retain some color of the live coloration.

Spicules. Holotype slide with spicules R1228-86g-Bk.1390 (BMNH) and slide with thick section R1275-PE01-Bk1390 (BMNH) (Fig. 4): megascleres large straight tylostyles with blunt ends 500-7 10-820 × 10-13-15 × 10-15-18 μm, small straight tylostyles with sharp ends 140-317-450 × 5-8-25 × 8-9-13 μm; microscleres selenasters 80-90-98 μm, streptasters with varying number of (spined) rays (5-10) with bifurcating endings or tufts 23-34-43 × 8-15 μm, acantho microrhabds 8-12-18 × 1-2.5 μm, spherasters absent. The range within the examined material (Table 1 & Fig. 5): megascleres large tylostyles 540-990 × 8-18 × 10-18 μ m, small tylostyles 175-550 × 3-10 × 3-13 μ m; microscleres selenasters 50-85 × 35-70 μ m, streptasters 15-48 × 5-18 μ m, acanthose microrhabds 5-18 × 1-2.5 μ m, spherasters absent.

Skeleton. As description of genus with addition that microrhabds form a layer over and amidst the selenaster cortex and are also prevalent in choanosomal tissue. Spirasters scattered in choanosome.

Figure 4.

Placospongia carinata slide of holotype (BMNH, R1228, 86g, Bk.1390; R1275, PE01, Bk1390). A large tylostyle (scale=200 μ m) B small tylostyle (scale=50 μ m) C selenaster (scale=50 μ m) D close up of large tylostyle (scale=50 μ m) E close up of small tylostyle F streptasters (scale=50 μ m) G acanthose microrhabds H original slide of thick section of holotype I original slide of spicules of holotype.

Figure 5.

Placospongia carinata (RMNH POR. 4483). A selenaster B large tylostyle (head and blunt end) C small tylostyle (head and hastate end) D streptasters, E. acanthose microrhabds.

Distribution.

East African coast to eastern Indonesia (Fig. 9, Table 2). Originally described from the ‘South Sea’, presumably the South Pacific Ocean. This has been interpreted by some (Rützler 2002, van Soest et al. 2011) to be Palau or Vanuatu, but this remains speculative. Based on the reviewed material and literature the minimal distribution is from Madagascar (Lévi 1956), to the Seychelles, and across Indonesia to the Aru Islands (Table 2). Distribution may extend further East.

Ecology.

Depth 0–45m. In Indonesia rarely found in reef environment, but high abundance in marine lakes. Possibly higher prevalence in reefs in Eastern Africa, based on the ZMA Por. collection from the Seychelles and the publication from Madagascar (Lévi 1956).

Remarks.

The Bowerbank description from 1858 should be considered as the original description of ‘Geodia carinata’, now accepted as Placospongia carinata, with plates XXV fig. 19 and XXVI fig. 10 representing the streptasters (“arborescent elongo-subsphero-stella”). Subsequently in 1874 Bowerbank published a more extensive description of “Geodia carinata” including a drawing of the streptasters (fig. 3, p.299) and spined microrhabds (“minute multiangulated cylindrical retentive spicula”, fig. 2, p.299) that he described as characteristic of the species. In neither publication registration numbers were provided, however. The habitus drawing in fig. 5, p.299 of Bowerbank publication in 1874 is identical to the specimen BMNH95.6.7.1 that I received from the BMNH after requesting the holotype for Placospongia carinata. In addition, I received the slides of spicules (codes: R1228, 86g, Bk.1390) and of the thick cut (codes: R1275, PE01, Bk1390) that were labeled to belong to the holotype (Fig. 5). Upon inspection I discovered that the specimen BMNH 95.6.7.1 is in fact a Placospongia melobesioides, while the two slides do indeed represent Placospongia carinata containing the characteristic streptasters with bifurcating endings and the microrhabds as indicated in the Bowerbank images and in the images taken from these slides in Fig. 5. The slides clearly do not come from the specimen BMNH 95.6.7.1. In the 16 years between Bowerbank’s 1858 and 1874 publications, I fear that there has been some exchange or misinterpretation of the labels of the specimens resulting in the incorrect assignment of specimen BMNH 95.6.7.1 to the slides and as the holotype of Placospongia carinata. This specimen BMNH 95.6.7.1, furthermore, has two labels attached to it: one with “Geodia carinata”, and one with “Placospongia melobesioides”. According to Bowerbank (1874) three specimens had been reviewed for his manuscript: one received from his friend Mr. Thos. Ingall in 1854, one placed by Dr. Baird from the coral to the sponge collection in the BMNH, and one specimen purchased by Bowerbank in 1864. The first mentioned specimen is presumably the holotype, but as this specimen has not been located, I propose to designate the slides R1228-86g-Bk.1390 and R1275-PE01-Bk1390 as representing the holotype of Placospongia carinata.

Placospongia melobesioides Gray, 1867

http://species-id.net/wiki/Placospongia_melobesioides

Figure 6
Placospongia melobesioides Gray (1867): figs 1–4.
Material examined.

Holotype. BMNH 52.4.1.14, Indonesia, Borneo island.

Vosmaer & Vernhout (1902), Siboga expedition: RMNH POR. 756, RMNH POR. 761, RMNH POR. 758, RMNH POR. 757, RMNH POR. 760, RMNH POR. 759. Other material:: RMNH POR. 4497, RMNH POR. 4496, RMNH POR. 4495, RMNH POR. 4114, RMNH POR. 3978, RMNH POR. 3977, RMNH POR. 3976, RMNH POR. 3942, RMNH POR. 3941, RMNH POR. 3940, RMNH POR. 3939, RMNH POR. 3938, RMNH POR. 3937, RMNH POR. 3935, RMNH POR. 3934, RMNH POR. 3933, RMNH POR. 3932, RMNH POR. 3177, RMNH POR. 3166, RMNH POR. 3154, RMNH POR. 2464, RMNH POR. 2463, ZMA Por. 13097, ZMA Por. 10459 (See Table 3 for full details per specimen)

Table 3.

Location details of reviewed specimens of Placospongia melobesioides.

registration number fieldcode country province region island locality habitat latitude longitude depth (m.) date collector
RMNH POR. 761 #1033 Indonesia S of Moluccas sand & rock 04°12'S, 129°20.4'E 45 1899 Siboga expedition
RMNH POR. 756 #660 Indonesia Nusa Tenggara N of Sumbawa sand & rock 07°12.6'S, 118°7.7'E 36 14.ii.1900 Siboga expedition
RMNH POR. 757 #1849 Indonesia Moluccas SE of Misool Banda islands sand & rock 32 1899 Siboga expedition
RMNH POR. 758 #1847 Indonesia Moluccas SE of Misool Banda islands sand & rock 32 1899 Siboga expedition
RMNH POR. 759 #1853 Indonesia Moluccas SE of Misool Banda islands sand & rock 32 1899 Siboga expedition
RMNH POR. 760 #1851 Indonesia Moluccas SE of Misool Banda islands sand & rock 32 1899 Siboga expedition
RMNH POR. 2463 #Sin05/270306/025 Singapore Semaku Pulau Semakau NW side reef 01°13'70"N, 103°45'61"E 10-12 iii.2006 N.J. de Voogd
RMNH POR. 2464 #Sin05/270306/026 Singapore Semaku Pulau Semakau NW side reef 01°13'70"N, 103°45'61"E 10-12 iii.2006 N.J. de Voogd
RMNH POR. 3154 #LEMD05/30 Indonesia North Sulawesi Bunaken Pangalisang reef 01°37'26"N, 124°46'55"E 9 24.ix.2006 L.E.Becking
RMNH POR. 3166 #LEMD13/69 Indonesia North Sulawesi Bunaken Pangalisang reef 01°37'26"N, 124°46'55"E 19 28.ix.2006 L.E.Becking
RMNH POR. 3177 #LEMD22/87 Indonesia North Sulawesi Bunaken Likuan2 reef 01°35'78"N, 124°46'06"E 21 13.x.2006 L.E.Becking
RMNH POR. 3932 #KKB/mol866 Indonesia East Kalimantan Berau Kakaban Kakaban lake marine lake 02°08'57.3"N, 118°31'26.4"E 0-2 ix.2008 L.E.Becking
RMNH POR. 3933 #KKB/mol766 Indonesia East Kalimantan Berau Kakaban Kakaban lake marine lake 02°08'57.3"N, 118°31'26.4"E 0-2 ix.2008 L.E.Becking
RMNH POR. 3934 #KKB/mol767 Indonesia East Kalimantan Berau Kakaban Kakaban lake marine lake 02°08'57.3"N, 118°31'26.4"E 0-2 ix.2008 L.E.Becking
RMNH POR. 3935 #BER113/mol689 Indonesia East Kalimantan Berau Maratua NE Maratua reef 02°17'32.3"N, 118°35'26.1"E 5-10 15.viii.2008 N.J. de Voogd
RMNH POR. 3937 #BER107/mol604 Indonesia East Kalimantan Berau Sangalaki E Sangalaki reef 02°05'36.6"N, 118°24'15.2"E 5-10 15.viii.2008 L.E.Becking
RMNH POR. 3938 #BER107/mol608 Indonesia East Kalimantan Berau Sangalaki E Sangalaki reef 02°05'36.6"N, 118°24'15.2"E 5-10 15.viii.2008 L.E.Becking
RMNH POR. 3939 #BER108/mol601 Indonesia East Kalimantan Berau Sangalaki W Sangalaki reef 02°05'07.7"N, 118°23'28.0"E 5-10 15.viii.2008 L.E.Becking
RMNH POR. 3940 #P-YAP1 Micronesia Yap Yap reefflat in front of mangrove 09°31'36.7"N, 138°07'48.7"E 1-3 28.viii.2010 L.E.Becking
RMNH POR. 3941 #P-YAP2 Micronesia Yap Yap reefflat in front of mangrove 09°31'36.7"N, 138°07'48.7"E 1-3 28.viii.2010 L.E.Becking
RMNH POR. 3942 #P-YAP3 Micronesia Yap Yap reefflat in front of mangrove 09°31'36.7"N, 138°07'48.7"E 1-3 28.viii.2010 L.E.Becking
RMNH POR. 3976 #PM-TER02 Indonesia Moluccas Ternate reef 5-10 xi.2009 N.J. de Voogd
RMNH POR. 3977 #PM-TER08 Indonesia Moluccas Ternate reef 5-10 xi.2009 N.J. de Voogd
RMNH POR. 3978 #PM-TER12 Indonesia Moluccas Ternate reef 5-10 xi.2009 N.J. de Voogd
RMNH POR. 4114 #KKB/mol795 Indonesia East Kalimantan Berau Kakaban Kakaban lake marine lake 02°08'57.3"N, 118°31'26.4"E 0-2 ix.2008 L.E.Becking
RMNH POR. 4495 #KKB/mol1075 Indonesia East Kalimantan Berau Kakaban Kakaban lake marine lake 02°08'57.3"N, 118°31'26.4"E 0-2 ix.2008 L.E.Becking
RMNH POR. 4496 #KKB/mol776 Indonesia East Kalimantan Berau Kakaban Kakaban lake marine lake 02°08'57.3"N, 118°31'26.4"E 0-2 ix.2008 L.E.Becking
RMNH POR. 4497 #BER107/mol603 Indonesia East Kalimantan Berau Sangalaki E Sangalaki reef 02°05'36.6"N, 118°24'15.2"E 5-10 15.viii.2008 L.E.Becking
ZMA Por. 10459 Seychelles Mahé Mahé NE coast, North East Point reef 04°34'59.9"S, 055°28'0.1"E 5 8.xii.1992 R.W.M. van Soest
ZMA Por. 10496 Seychelles Mahé Mahé North East Point reef 04°34'59.9"S, 055°28'0.1"E 14.xii.1992 R.W.M. van Soest
ZMA Por. 13097 Indonesia South Sulawesi Spermonde archipelago Samalona reef 5-30 27.iv.1997 N.J. de Voogd
Description.

Holotype BMNH 52.4.1.14 dry, chalky white angular branches, hard. Other examined material encrusting to branching, hard, thicker specimens slightly compressible. External morphology follows the description of the genus. Size ranging between 5-50 cm, though encrusting specimens may be larger growing within crevices. Ectosome color in life ranging from purple, dark black brown, chocolate brown, orange brown to light beige (Fig. 1, 2). Choanosome pale beige. After preservation color of ectosome is similar to live color.

Spicules. Holotype BMNH 52.4.1.14 (Fig. 6): Megascleres large straight tylostyles with blunt ends 670-880-1010 × 10-13-18 × 10-16-20 μm, small concave to straight tylostyles with sharp ends 205-293-420 × 5-10-13 × 5-10-13 μm. Microscleres selenasters 58-63-68 × 45-52-68 μm, spherasters 15-17-18 μm (five measurements, not abundant), spherules 1-2-3 μ m. The range within the examined material (Table 1): large tylostyles 460-1040 × 5-16 × 8-18 μ m, small tylostyles 190-470 × 3-13 × 3-15 μ m, selenasters 45-83 × 30-65 μ m, spherules 1-3 μ m, spherasters only found in singles in some individuals 15-20 μ m. Streptasters and microrhabds absent.

Skeleton. As description of genus with addition of sporadic spherasters lodged amidst selenasters in cortex and high abundance of spherules in choanosome and cortex.

Figure 6.

Placospongia melobesioides holotype (BMNH 52.4.1.14). A Holotype with two labels B selenaster C large tylostyle (head and blunt end) D small tylostyle (head and hastate end) E spheraster F spherules.

Ecology.

Depth: 0-45m. Reefs, rocky shores, reefflats, mangroves, and marine lakes.

Distribution.

Type locality: Borneo. Distribution from Seychelles to Micronesia (Fig. 9, Table 3). Possibly further east to Central Pacific.

Remarks.

In the original description by Gray (1867) there is no mention of two size classes of tylostyles. I reexamined the original slide and conclude that the holotype does contain two size classes of tylostyles. The Systema Porifera indicates that the holotype has two size classes, the large 720-963-1200 × 13-14.1-19 μm and the small 350-438.8-560 × 8-9.1-10.5 μm, based on 10 measurements per spicule type (Rützler 2002). These measurements deviate from the holotype measurements in the present study that were based on 25 measurements per spicule type (670-880-1010 × 10-13-18 μm and 205-293-420 × 5-10-13 μm respectively), and also deviate from the range of sizes within the examined material of this study (Table 1). There is great variation in tylostyle length and spherasters are only sporadically present, often absent.

Placospongia mixta Thiele 1900

http://species-id.net/wiki/Placospongia_mixta

Figure 7
Placospongia mixta Thiele, 1900: Plate III, fig. 25.
Material examined.

Holotype. ZMB 3204, Indonesia, Moluccas, Ternate.

Vosmaerand & Vernhout (1902), Siboga expedition: RMNH POR. 753, RMNH POR. 751, RMNH POR. 745, RMNH POR. 742. Other material: RMNH POR. 4494, RMNH POR. 4493, RMNH, POR. 4492, RMNH POR. 4491, RMNH POR. 4490, RMNH POR. 4489, RMNH POR. 4113, RMNH POR. 4112, RMNH, POR. 3979, RMNH POR. 3975, RMNH POR. 3974, RMNH POR. 3973, RMNH POR. 3972, RMNH POR. 3971, RMNH POR. 3970, RMNH POR. 3969, RMNH POR. 3968, RMNH POR. 3967, RMNH POR. 3966, RMNH POR. 3965, RMNH POR. 3964, RMNH POR. 3963, RMNH POR. 3962, RMNH POR. 3961, RMNH POR. 3960, RMNH POR. 3959, RMNH, POR. 3163, RMNH POR. 3158, RMNH POR. 3157, RMNH POR. 3155, RMNH POR. 3148, ZMA Por. 10495, ZMA Por. 896 (See Table 4 for full details per specimen)

Table 4.

Location details of reviewed specimens of Placospongia mixta.

registration number fieldcode country province region island locality habitat latitude longitude depth date collector
RMNH POR. 753 #311 Indonesia West Papua E. of Misool sand & rock 01°42.5'S, 130°47.5'E 32 20.viii.1899 Siboga expedition
RMNH POR. 751 #1857 Indonesia West Papua E. of Misool sand & rock 01°42.5'S, 130°47.5'E 32 20.viii.1899 Siboga expedition
RMNH POR. 745 #577 Indonesia South Sulawesi N. of Kabia Saleyer anchorage sand & rock 36 20.viii.1899 Siboga expedition
RMNH POR. 742 #163a Indonesia Moluccas Aru Pearl Banks, anchorage off Pulu Jedan reef 13 23.xii.1899 Siboga expedition
RMNH POR. 3148 #LEMD04/21 Indonesia North Sulawesi Bunaken Likuan 2 reef 01°35'78"N, 124°46'06"E 15 24.ix.2006 L.E. Becking
RMNH POR. 3155 #LEMD06/32 Indonesia North Sulawesi Lembeh Strait Nudi Reed Reed reef 01°24'06"N, 125°12'22"E 21 25.ix.2006 L.E. Becking
RMNH POR. 3157 #LEMD08/39 Indonesia North Sulawesi Lembeh Strait Nudi Fols reef 01°27'26"N, 125°13'05"E 6 25.ix.2006 L.E. Becking
RMNH POR. 3158 #LEMD08/42 Indonesia North Sulawesi Lembeh Strait Nudi Fols reef 01°27'26"N, 125°13'05"E 8 25.ix.2006 L.E. Becking
RMNH POR. 3163 #LEMD11/52 Indonesia North Sulawesi Bunaken 0.5-1km W. of Park administration office reef 01°36'57"N, 124°45'41"E 8 27.ix.2006 L.E. Becking
RMNH POR. 3959 #KKB/mol827 Indonesia East Kalimantan Berau Kakaban Kakaban lake marine lake 02°08'57.3"N, 118°31'26.4"E 0-2 ix.2008 L.E.Becking
RMNH POR. 3960 #KKB/mol829 Indonesia East Kalimantan Berau Kakaban Kakaban lake marine lake 02°08'57.3"N, 118°31'26.4"E 0-2 ix.2008 L.E.Becking
RMNH POR. 3961 #KKB/mol851 Indonesia East Kalimantan Berau Kakaban Kakaban lake marine lake 02°08'57.3"N, 118°31'26.4"E 0-2 ix.2008 L.E.Becking
RMNH POR. 3962 #BER111/mol1203 Indonesia East Kalimantan Berau Kakaban SW Kakaban reef 02°08'07.5"N, 118°30'23.3"E 10 17.viii.2008 N.J. de Voogd
RMNH POR. 3963 #BER111/1209 Indonesia East Kalimantan Berau Kakaban SW Kakaban reef 02°08'07.5"N, 118°30'23.3"E 10 17.viii.2008 N.J. de Voogd
RMNH POR. 3964 #BER111/1213 Indonesia East Kalimantan Berau Kakaban SW Kakaban reef 02°08'07.5"N, 118°30'23.3"E 10 17.viii.2008 N.J. de Voogd
RMNH POR. 3965 #BER111/mol1219 Indonesia East Kalimantan Berau Kakaban SW Kakaban reef 02°08'07.5"N, 118°30'23.3"E 10 17.viii.2008 N.J. de Voogd
RMNH POR. 3966 #RAJ23/mol195 Indonesia West Papua Raja Ampat Gam Ctenophore lake marine lake 00°27'17.5"S, 130°29'33.8"E 0-2 xi.2007 L.E. Becking
RMNH POR. 3967 #RAJ23/mol187 Indonesia West Papua Raja Ampat Gam Ctenophore lake marine lake 00°27'17.5"S, 130°29'33.8"E 0-2 xi.2007 L.E. Becking
RMNH POR. 3968 #RAJ64/mol429 Indonesia West Papua Raja Ampat Waigeo Teluk Mayabilit reef 00°18'17.0"S, 130°54'15.6"E 10 xii.2007 L.E. Becking
RMNH POR. 3969 #RAJ64/mol430 Indonesia West Papua Raja Ampat Waigeo Teluk Mayabilit reef 00°18'17.0"S, 130°54'15.6"E 10 xii.2007 L.E. Becking
RMNH POR. 3970 #RAJ64/mol431 Indonesia West Papua Raja Ampat Waigeo Teluk Mayabilit reef 00°18'17.0"S, 130°54'15.6"E 10 xii.2007 L.E. Becking
RMNH POR. 3971 #RAJ64/mol432 Indonesia West Papua Raja Ampat Waigeo Teluk Mayabilit reef 00°18'17.0"S, 130°54'15.6"E 10 xii.2007 L.E. Becking
RMNH POR. 3972 #RAJ64/mol433 Indonesia West Papua Raja Ampat Waigeo Teluk Mayabilit reef 00°18'17.0"S, 130°54'15.6"E 10 xii.2007 L.E. Becking
RMNH POR. 3973 #RAJ39/mol249 Indonesia West Papua Raja Ampat Fam rocky shore 00°36'01.5"S, 130°45'08"E 0-1 xi.2007 L.E. Becking
RMNH POR. 3974 #RAJ39/mol250 Indonesia West Papua Raja Ampat Fam rocky shore 00°36'01.5"S, 130°45'08"E 0-1 xi.2007 L.E. Becking
RMNH POR. 3975 #RAJ39/mol254 Indonesia West Papua Raja Ampat Fam rocky shore 00°36'01.5"S, 130°45'08"E 0-1 xi.2007 L.E. Becking
RMNH POR. 3979 #KKB/mol 779 Indonesia East Kalimantan Berau Kakaban Kakaban lake marine lake 02°08'57.3"N, 118°31'26.4"E 0-2 ix.2008 L.E.Becking
RMNH POR. 4112 #P-TER11 Indonesia Moluccas Ternate reef xi.2009 N.J. de Voogd
RMNH POR. 4113 #P-TER22 Indonesia Moluccas Ternate reef xi.2009 N.J. de Voogd
RMNH POR. 4489 #KKB/mol721 Indonesia East Kalimantan Berau Kakaban Kakaban lake marine lake 02°08'57.3"N, 118°31'26.4"E 0-2 ix.2008 L.E.Becking
RMNH POR. 4490 #KKB/mol830 Indonesia East Kalimantan Berau Kakaban Kakaban lake marine lake 02°08'57.3"N, 118°31'26.4"E 0-2 ix.2008 L.E.Becking
RMNH POR. 4491 #BER109/mol629 Indonesia East Kalimantan Berau lighthouse near Berau river reef 02°09'49.9"N, 118°10'12.8"E 10 16.viii.2008 L.E.Becking
RMNH POR. 4492 #BER111/mol666 Indonesia East Kalimantan Berau Kakaban SW Kakaban reef 02°08'07.5"N, 118°30'23.3"E 10 17.viii.2008 N.J. de Voogd
RMNH POR. 4493 #RAJ64/mol428) Indonesia West Papua Raja Ampat Waigeo Teluk Mayabilit reef 00°18'17.0"S, 130°54'15.6"E 10 xii.2007 L.E. Becking
RMNH POR. 4494 #RAJ23/mol199 Indonesia West Papua Raja Ampat Gam Ctenophore lake marine lake 00°27'17.5"S, 130°29'33.8"E 0-2 xi.2007 L.E. Becking
ZMA Por. 896 Indonesia South Sulawesi SW Salayer reef N of Pulau Bahuluang reef 06°27'00"S, 120°25'48"E 10-45 30.ix.1984 R.W.M. van Soest (Snellius Expedition II)
ZMA Por. 10495 Seychelles Mahé Mahé SE coast near Pointe Cocos 04°45'00"S, 055°32'60"E 35-45 24.xii.1992 R.W.M. van Soest
Description.

Holotype ZMB 3204 encrusting, size 5 × 2.5 cm and thickness 1–5 mm (as described by Thiele, now very small fragment), white after preservation in alcohol. The majority of the reviewed material is encrusting with a thickness of 4-10mm, but branching specimens also occur. External morphology follows the description of the genus. Color of the ectosome can be red, orange, brown orange, dark brown, chocolate brown, milk coffee brown, cream, or white (Fig. 1, 2). Color of choanosome is pale beige. After preservation in ethanol color is similar to live specimens, but lighter shade.

Spicules. Holotype ZMB 3204 (Fig. 6) Megascleres large straight tylostyles with blunt/rounded point 355-672-940 × 7.5-12-17.5 × 7.5-16-20 μm, small straight tylostyles with sharp point 165-226-275 × 2.5-6-7.5 × 2.5-8-10 μm; microscleres selenasters 55-70-75 × 42.5-55-72.5 μm, spherasters (abundant) 20-25-30 μm, streptasters typically with well developed axis and with 4-9 rays with hastate tips, rays are smooth or can be spined, but do not have bifurcations of the tips 15-24-32.5 × 2.5-8-12.5 μm; acanthose microrhabs with straight or zig-zag axis 5-7-10 × <2.5 μ m.The range within the examined material (Table 1): large tylostyles 460-1250 × 8-23 × 10-25 μ m, small tylostyles 120-430 × 3-15 × 2-15 μ m, selenasters 50-85 × 22-73 μ m, spherasters 13-30 μ m, streptasters 15-35 × 2-15 μ m, rays 5-18 × 1-2.5 μ m.

Skeleton. As description of genus with addition that microrhabds form a layer over and amidst the selenaster cortex and are also prevalent in choanosomal tissue. Streptasters scattered in choanosome. Spherasters amidst selenasters in cortex and scattered in choanosome.

Figure 7.

Placospongia mixta holotype (ZMB 3204). A selenaster B large tylostyle (head and blunt end) C small tylostyle (head and hastate end) D spheraster E streptasters F microacanthose microrhabds.

Distribution.

East African coast to eastern Indonesia (Fig. 9, Table 4). Possibly further east to Central Pacific. Pulitzer-Finali (1993) identified a ‘P. carinata’ from East Africa (Mombasa) that fits the description of Placospongia mixta based on the length of the tylostyles (up to 1200 μ m) and the presence of spherasters, but no Placospongia mixta specimens were observed in the Seychelles material deposited at ZMA.

Ecology.

Depth 0–45m. Common in reefs, also occurs in marine lakes.

Remarks.

In 1900 Thiele described a new species named Placospongia mixta, which was originally identified as Placospongia melobesioides by Kieschnick (1896). The specific epithet mixta was given because the specimen contained a mixture of spicules: both spirasters like Placospongia carinata as well as large spherasters like Placospongia intermedia and Placospongia melobesioides, which are absent in Placospongia carinata. In 1902 Vosmaer & Vernhout decided that Placospongia mixta was a junior synonym of Placospongia carinata, because they saw no distinction between the different shapes of streptasters and stated that spherasters are never very abundant – in some ‘exceedingly rare and in some we failed to find them at all’ – and could therefore not be seen as a distinguishing character. The specimens that were studied by Vosmaer and Vernhout (1902) were collected in Indonesia during the Siboga Expedition (1899-1900) and are housed in the collection of the Naturalis Biodiversity Center (Leiden, The Netherlands). In the present study these specimens were reexamined. After inspection, the specimens labeled ‘Placospongia carinata’ could be clearly and consistently divided into two species: Placospongia carinata without spherasters, with streptasters displaying bifurcating tips, and tylostyles up to 980 μ m, and Placospongia mixta with abundant spherasters, with streptasters displaying hastate tips, and tylostyles up to 1250 μ m. In none of the specimens of Vosmaer and Vernhout (1902), nor of the other specimens reviewed for this study was there a mixture of the two types of streptasters. These two species also show molecular distinction in both mitochondrial and nuclear markers (Fig. 10, 11, Table 6, 7).

Holotype.

RMNH POR. 4486, Indonesia, East Kalimantan province, Maratua island, Buli Halo anchialine pool, 02°11'16.4"N, 118°37'06.4"E, 0–1m. depth, xi.2008, coll. N.K. Santodomingo & Estradivari, #BER128/mol1147. Paratypes. RMNH POR. 4487, Indonesia, East Kalimantan province, Maratua island, Buli Halo anchialine pool, 02°11'16.4"N, 118°37'06.4"E, 0–1m. depth, xi.2008, coll. N. K. Santodomingo & Estradivari; RMNH POR. 4488, Indonesia, East Kalimantan province, Maratua island, Buli Halo anchialine pool, 02°11'16.4"N, 118°37'06.4"E, 0–1m. depth, xi.2008, coll. N. K. Santodomingo & Estradivari, #BER128/1156.

Description.

Holotype and paratypes are branching and encrusting, size 8cm in length. Total size of specimens in situ is hard to establish as parts of the body may be encrusting within cracks. Alcohol preserved and live specimens are hard but slightly compressible. The surface is made up with typical Placospongia cortical plates separated by contractible grooves which form a network on the surface. Oscules are present in the grooves. Live color of holotype was dark brown, the paratypes were orange, and these colors were mostly retained after alcohol preservation (Fig. 8A).

Spicules. Holotype (Fig. 8) megascleres large straight tylostyles with blunt point 430-605.5-660 × 13-15.5-20 × 13-18.1-23 μm, small straight tylostyles with sharp point 240-261.3-290 × 5-7.2-8 × 5-8.8-10 μm; microscleres selenasters 80-84.8-90 × 60-67.3-75 μm, acanthose microrhabds 8-12.3-18 × 2.5-2.7-3.5 μm. Range of the paratypes (Table 1) large straight tylostyles with blunt point 430-760 × 13-20 × 15-23 μm, small straight tylostyles with sharp point 190-380 × 5-13 × 8-15 μm, microscleres selenasters 63-93 × 58-75 μ m, acanthose microrhabds 5-20 × 2.5-3.5 μ m.

Skeleton. The cortical plates consist of densely packed selenasters, microrhabds form a layer over and amidst this selenaster cortex and are also prevalent in choanosomal tissue. Developmental stages of selenasters occur throughout the choanosome. Tylostyle tracts support the margins of the cortical plates in radial tracts from the centre core (consisting of densely packed selenaster) to the cortical plates. The sharp ends of the smaller tylostyles can be projected beyond the cortex surface.

Figure 8.

Placospongia santodomingoae sp. n. (RMNH POR. 4486). A ethanol preserved specimen B selenaster C large tylostyle (head and blunt end) D small tylostyle (head and hastate end) E microrhabds.

Distribution.

Presently only recorded from Buli Halo anchialine pool on Maratua island, Berau, East Kalimantan, Indonesia (Fig. 9). For a full description of the pool, see Becking et al. (2011)

Figure 9.

Distribution of Placospongia spp. in the Indo-West Pacific. Location of symbols is approximate.

Ecology.

Depth 0–2m. occurs in anchialine pool, can be exposed to air during low tide and can tolerate great fluctuations in salinity (from 24 to 33 ‰).

Etymology.

Named in honor of Nadiezhda K. Santodomingo, the collector of the types, for her years of tireless work in marine science including anchialine research.

Remarks.

Placospongia santodomingoae sp. n. is similar to Placospongia carinata, yet lacks streptasters and has shorter tylostyles. Placospongia santodomingoae sp. n. likewise differs from Placospongia mixta by the absence of streptasters as well as the absence of spherasters. Placospongia santodomingoae sp. n. differs from Placospongia anthosigma by the absence of anthosigma, and by having hastate endings of the smaller tylostyles.

Geodia labyrinthica (Kirkpatrick, 1903)

http://species-id.net/wiki/Geodia_labyrinthica

Placospongia labyrinthica Kirkpatrick 1903: Plate V fig. 1a–b, Plate VI fig. 1a–f.
Reviewed material.

Holotype. BMNH 02.11.16.1, South Africa, East London Coast, 33°06'30"S, 028°11'E.

Spicules. Megascleres styles, oxea; microscleres sterrasters, chiasters

Remarks.

This species was originally described as ‘Placospongia labyrinthica’, butdoes not have the characteristic cortical plates of Placospongia. The specimen furthermore has sieve pores, sterrasters with star-like plates, euasters, styles and oxea characteristic of the Geodiidae. In the original description, Kirkpatrick (1903) stated “the presence of chiasters is so exceptional that I thought at first that I had to deal with a geodine sponges, but there were no triaenes to be found” and as a result placed this species in the Placospongia rather than Geodia. Genus transfer to Geodia is, however, required as suggested on the World Porifera Database (van Soest et al. 2011).

Identification key for Indo-Pacific species of Placospongia
1 Streptasters absent 2
Streptasters present 3
2 Spherules present Placospongia melobesioides
Spherules absent 4
3 Streptasters have rays with birfurcating ends Placospongia carinata
Streptasters have rays with hastate ends, spherasters present Placospongia mixta
4 Spherasters present, microrhabds with short spines spirally places on shaft Placospongia anthosigma
Spherasters absent, acanthose microrhabds present Placospongia santodomingoae sp.n.
Genetic data analysis

All sequences were submitted to GenBank with accession numbers KC848421 - 41 (Table 5). Final alignments (excluding primers) were obtained for the sponge Placospongia of 581 bp for COI with three genetic variants (28 individuals) and 13 polymorphic sites. The three genetic variants correspond to the three species Placospongia melobesioides, Placospongia mixta, and Placospongia carinata that represent monophyletic groups which are strongly supported by both Bayesian and maximum likelihood inference methods (Fig. 10). There was no intra-specific variation within each species, regardless of geographic locality. The inter-specific p- distances ranged between 0.5-2.1% (Table 6).There were 11 substitutions between Placospongia melobesioides and Placospongia carinata, 12 substitutionsbetween Placospongia melobesioides and Placospongia mixta, and three substitutions between Placospongia mixta and Placospongia carinata. The specimens of Placospongia carinata and of Placospongia santodomingoae sp. n. had identical genotypes for COI. No molecular work could be done on the dried holotype of Placospongia anthosigma and fresh material was not available.

Final alignments (excluding primers) of 720 bp were obtained for ITS with 18 genetic variants from the present study (22 individuals). An additional 27 genetic variants from GenBank (for GenBank accession numbers see Fig. 11) were included in the phylogenetic analysis. The ITS sequences represented five clades that were strongly supported by both Bayesian and maximum likelihood inference methods (Fig. 11). These five divergent clades (see Table 7 for uncorrected p- distances) correspond to the clades C3, C4, C5, C6, and C9 as presented by the study of Nichols and Barnes (2005). Clade C9 represents specimens of the species Placospongia melobesioides, clade C5 Placospongia mixta, and clade C4 Placospongia carinata. Clades C6 is represented by one specimen from the Solomon Islands (QM317896) and clade C3 by one specimen from Bynoe Harbour, Northern Territory, Australia (QM303439); none of the samples that were sequenced in the present study fell into either C3 or C6 clade. The specimens of Placospongia santodomingoae sp. n. represented a separate lineage within the Placospongia carinata clade (C4) which was supported by Bayesian inference, but not by maximum likelihood analysis. The p- distancebetween Placospongia carinata specimens and the specimens of Placospongia santodomingoae sp. n. was 0.6%.

Figure 10.

Bayesian/maximum likelihood phylograms of Cytochrome Oxidase I (COI) sequences from Indo-Pacific Placospongia spp. See Table 5 for GenBank accession numbers. Only posterior probabilities of >90 and maximum likelihood values of >70 indicated. Scale bar indicates substitutions/site.

Figure 11.

Bayesian/maximum likelihood phylograms of genotypes of the internal transcribed spacer region of nuclear ribosomal operons (ITS) of Indo-Pacific Placospongia spp. found in this study and related species from the same genus collected from GenBank. Clades C3, C4, C5, C6 & C9 refer to the clades presented in the study by Nichols and Barnes (2005). Taxon labels are organized as follows: Specimen - Locality - Genbank code or RMNH POR. Number. Only posterior probabilities of >90 and maximum likelihood values of >70 indicated. Scale bar indicate substitutions/site.

Table 5.

Specimens of Placospongia studied for DNA analysis. Genbank accession numbers provided for sequences of Cytochrome Oxidase I (COI) and internal transcribed spacer region (ITS).

Registration number Species COI ITS
RMNH POR. 4482 Placospongia carinata KC848441 KC848429
RMNH POR. 4483 Placospongia carinata KC848441 KC848427
RMNH POR. 4484 Placospongia carinata KC848441 KC848428
RMNH POR. 4485 Placospongia carinata KC848441 KC848429
ZMA Por. 10727 Placospongia carinata KC848441 -
ZMA Por. 11367 Placospongia carinata KC848441 -
RMNH POR. 2464 Placospongia melobesioides KC848439 -
RMNH POR. 3942 Placospongia melobesioides KC848439 KC848422
RMNH POR. 3976 Placospongia melobesioides KC848439 -
RMNH POR. 4114 Placospongia melobesioides KC848439 KC848426
RMNH POR. 4495 Placospongia melobesioides KC848439 KC848436
RMNH POR. 4496 Placospongia melobesioides KC848439 KC848436
RMNH POR. 4497 Placospongia melobesioides KC848439 KC848437
RMNH POR.3166 Placospongia melobesioides KC848439 KC848422
ZMA Por. 10459 Placospongia melobesioides KC848439 KC848438
RMNH POR. 3158 Placospongia mixta KC848440 KC848421
RMNH POR. 3960 Placospongia mixta KC848440 KC848423
RMNH POR. 3979 Placospongia mixta KC848440 -
RMNH POR. 4113 Placospongia mixta KC848440 KC848425
RMNH POR. 4489 Placospongia mixta KC848440 -
RMNH POR. 4490 Placospongia mixta KC848440 KC848433
RMNH POR. 4491 Placospongia mixta KC848440 KC848433
RMNH POR. 4492 Placospongia mixta KC848440 KC848434
RMNH POR. 4493 Placospongia mixta KC848440 KC848435
RMNH POR. 4494 Placospongia mixta KC848440 KC848435
RMNH POR. 4486 Placospongia santodomingoae sp. n. KC848441 KC848430
RMNH POR. 4487 Placospongia santodomingoae sp. n. KC848441 KC848431
RMNH POR. 4488 Placospongia santodomingoae sp. n. KC848441 KC848432
Table 6.

The number of base differences per site from averaging over all Cytochrome Oxidase I (COI) sequence pairs between Placospongia spp. groups are shown (uncorrected p-distances). Standard error estimate (s) are shown above the diagonal in italic. The analysis involved 30 nucleotide sequences. There was no within-group difference. Spirastrella aff. decumbens was used as outgroup in the phylogenetic inference (see Fig. 10).

%p-distance COI Placospongia melobesioides Placospongia mixta Placospongia carinata Spirastrella aff. decumbens
Placospongia melobesioides * 0.6 0.6 1.3
Placospongia mixta 2.1 * 0.3 1.2
Placospongia carinata 1.9 0.5 * 1.3
Spirastrella aff. decumbens 12.2 11.5 11.7 *
Table 7.

The number of base differences per site from averaging over all internal transcribed spacer (ITS) sequence pairs between Placospongia spp. groups are shown (uncorrected p-distances). Standard error estimate (s) are shown above the diagonal. All positions with less than 5% site coverage were eliminated. Black cursive along the diagonal indicates within-group uncorrected p- distance. The analysis involved 73 nucleotide sequences. C9, C5, C6, C4, C3 refer to five clades in the Indo-West Pacific Placospongia as presented in Fig. 11.

%p-distance ITS Placospongia melobesioides Placospongia mixta Placospongia carinata Placospongia santodomingoae sp. n. C9 C5 C6 C4 C3
Placospongia melobesioides 0.1 1.3 1.4 1.4 0.3 1.3 1.3 1.3 1.3
Placospongia mixta 13.8 0.7 0.9 0.9 1.2 0.2 0.5 0.9 0.9
Placospongia carinata 14.7 6.3 0.4 0.2 1.3 0.9 0.9 0.2 0.9
Placospongia santodomingoae sp. n. 13.2 5.8 0.6 1.6 1.3 0.9 0.9 0.3 0.9
C9 0.9 13.5 14.6 13.6 0.1 1.2 1.2 1.2 1.2
C5 13.5 0.9 6.6 6.1 12.9 0.7 0.5 0.8 0.9
C6 14 2.2 6.4 6.1 13.2 2.2 0.1 0.8 0.8
C4 14.8 6.3 0.5 0.9 14.3 6.3 6 0.4 0.8
C3 15.2 7.1 6.1 5.9 14.5 6.9 6.3 5.6 0.9
Discussion
Different species

In the Indo-West Pacific at least five species of the genus Placospongia can be identified based on spicule morphology: Placospongia anthosigma, Placospongia carinata, Placospongia mixta, Placospongia melobesioides, and Placospongia santodomingoae sp. n. Placospongia melobesioides, Placospongia carinata, and Placospongia mixta can be distinguished with the DNA barcode marker (COI) and a nuclear marker (ITS). The species Placospongia santodomingoae sp. n. and Placospongia carinata have the same sequence of COI. The sequence variation of COI in sponges can be low (e.g. Wörheide 2006, Xavier et al. 2010, Pöppe et al. 2011) and this is also the case in species of Placospongia, e.g. only 0.5% nucleotide distance between the species Placospongia mixta and Placospongia carinata.There is furthermore no intraspecific variation in COI within each of the Placospongia species, not even between populations at 1000s of km distance from each other (e.g. specimens from the Seychelles are identical with specimens from Indonesia). The phylogenetic inference based on the ITS sequences does show a supported clade of Placospongia santodomingoae sp. n. within the clade of Placospongia carinata (Fig. 11), though the degree of divergence between the two species is low (0.6%) (Table 7). Placospongia santodomingoae sp. n. should, however, be designatedas a new species based on the spicule morphology: the absence of a distinguishing spicule type (streptasters) and consistently shorter and thicker tylostyles (maximum 760 × 20 μm) compared to Placospongia carinata (maximum 980 × 17.5 μm) are valid arguments to distinguish a separate species within this genus. The specimens of Placospongia santodomingoae sp. n. were collected from an anchialine pool. This kind of isolated environment has previously been shown to contain small, rapidly evolving populations, and many rare species across a large spectrum of taxa (e.g. Holthuis 1973, Tomascik and Mah 1994, Dawson and Hamner 2005, Becking et al. 2011, Becking et al. in press). The divergence of Placospongia santodomingoae sp. n. from Placospongia carinata is likely too recent to be expressed in the molecular markers that were used. Other, faster evolving, molecular markers might show a more distinct separation between species, but for the present significant morphometric differences in spicules are reliable characters in separating these sister species.

A molecular phylogeny using the internal transcribed spacer region (ITS) showed that there were five distinct clades within the genus Placospongia in the Indo-West Pacific (clades C3, C4, C5, C6 & C9) (Nichols & Barnes, 2005). Nichols and Barnes (2005) indicated that their results presented a conundrum that “specimens collected from Indonesian marine lakes that have been isolated from the surrounding marine environment since the Pleistocene are undifferentiated from individuals collected from the Seychelles indicating that populations from these geographically disparate regions are, or have recently been, connected by gene flow despite the lack of evidence of connectivity between these lakes and nearby reefs.” It is important to note here that the authors did not investigate the spicule morphology of the specimens in their study, while it is in fact the spicules that can largely explain the presented conundrum. In the present study over 30 specimens from the marine lakes Kakaban and Maratua and the adjacent reefs have been reviewed as well as the specimens from the ZMA Por. collection that were used in the Nichols and Barnes (2005) study. Clade C4 represents the material from the Seychelles (ZMA Por.11367) together with the marine lakes and can all be morphologically identified as P. carinata sensu stricto. The samples from the lakes and the Seychelles are thus conspecific, but the populations of the two locations are necessarily connected by gene flow. Subsequently clade C9 is Placospongia melobesioides (specimens from Indonesia, Miscronesia and the Seychelles) and clade C5 is of Placospongia mixta (specimens from Indonesia, Palau and Papua New Guinae). This explains three of the five clades from the Indo-West Pacific and leaves two undetermined: clade C3 represented by one specimen from Bynoe Harbour, Northern Territory, Australia (QM303439), and clade C6 represented by one specimen from the Solomon Islands (QM317896). The morphology of these specimens should be further studied in order to correctly identify the species and determine if they may represent morphologically cryptic species.

Natural variation

Each of the five species of the genus Placospongia in the Indo-West Pacific can be distinguished based on the composition and morphology of spicules. The external morphology, however, does not allow species distinction. The most common species from the tropical Indo-West Pacific (Placospongia melobesioides, Placospongia mixta, and Placospongia carinata) can have both encrusting and branching growth forms displaying a variety of colors from white to dark brown. The only observed consistent pattern was that all the red specimens belonged to Placospongia mixta, while all the dark black-brown specimens belonged to Placospongia melobesioides.These two colors may be useful for field identifications, yet both species can also display the range of other colors (white, cream, beige, light brown) as well. The density of canals/ridges (or size of cortical plates) appears to be related to environment as this is higher in specimens from high sediment locations such as the marine lakes than in specimens from the reefs (Fig. 1, 2). Within each species there is also some natural variation in the range of tylostyle length and spicule morphology. The streptaster morphology varies within species and even within individuals. Within one individual the number of rays can vary from 4-10 (Figs 3, 4) and between individuals the decoration and size of spines can be diverse. For example the streptasters of Placospongia carinata specimens from Haji Buang marine lake are micro-acanthose while the specimens from other locations are not. Spherasters are always present and abundant in Placospongia mixta and Placospongia anthosigma, but are in low abundances or absent in Placospongia melobesioides, as has been indicated previously by Vosmaer and Vernhout (1902). In Placospongia carinata and Placospongia santodomingoae sp. n. spherasters are always absent.

Ecology and distribution

Placospongia melobesioides and Placospongia mixta are common in the reef environment. Most of the collected material from the reefs in Indonesia were one of these two species. Placospongia carinata appears to be rare in the reefs, in Indonesia at least, while it is highly abundant in the marine lakes Haji Buang and Kakaban in East Kalimantan, Indonesia. Placospongia santodomingoae n.sp. is restricted to an anchialine pool. Placospongia anthosigma was not found in any of the examined collections from the tropical Western Pacific, this species is restricted to more temperate and deeper waters. Placospongia melobesioides is indicated in the Systema Porifera to have a distribution from the Indo-West Pacific to the Tropical Atlantic (Rützler, 2002). Both Placospongia melobesioides and Placospongia carinata have been recorded from the Atlantic (e.g. de Laubenfels 1936, Hechtel 1976, Coelho and Mello-Leitão 1978, Pulitzer-Finali 1986, González-Farías 1989), which would imply that these are pantropical species. Recent molecular and more detailed morphological studies have, however, shown that many cosmopolitan sponge species are in fact species complexes either delineated by morphology or molecules (e.g. Reveilleud et al. 2010, Xavier et al. 2010). Van Soest (2009) has indicated that there are at least five species of Placospongia in the Caribbean that are morphologically different from the holotypes of Placospongia melobesioides and Placospongia carinata.Rua et al. (2006) and Nichols and Barnes (2005), furthermore, show that there are distinct lineages in the Caribbean and Western Pacific, that are not shared between the two regions and that most likely represent undescribed species in the Caribbean. Considering these results as well as the large geographic distance between the Caribbean and the type localities of Placospongia melobesioides and Placospongia carinata (both Indo-West Pacific), it is highly unlikely that these species occur in the Tropical Atlantic. Further revision of the Atlantic and Eastern Pacific material will shed more light on this issue.

Future biodiversity surveys and species checklists both in the Atlantic as well as in the Pacific are advised to check the spicule morphology of Placospongia specimens in order to identify species, as the external morphology and color will not give an indication to the number of species. The different Placospongia spp. can occupy the same type of habitats in the tropics. An example of such sympatry is represented in Kakaban lake where in the 4 km2 area of the marine lake the three common tropical species of Placospongia co-exist side by side. Neglecting to review the spicule morphology would mean possibly missing the true diversity of species that are present in the location of study.

Acknowledgements

N.J. de Voogd, R.W.M. van Soest, and three reviewers provided valuable comments on the original manuscript. For the loan of the type-specimens I thank: E. Sherlock (British Museum of Natural History), H. Namikawa (National Museum of Nature and Science, Tokyo, Japan), and C. Eckert (Zoologisches Museum für Naturkunde). I am also grateful to the following people for their help in various ways in field- or labwork logistics: B.W Hoeksema, Suharsono, Y. Tuti, Y. Ise, S. Hoshino, Y. Nakao, N. K. Santodomingo, Estradivari, Bahruddin, M. Erdmann, M. Ammer, D. Erpenbeck, S. Menken, H. Breeuwer, J. van Ooyen, E. Beglinger, E. Kruidenier, and the staff of Papua Diving, of Nabucco Island Dive Resort, of Derawan Dive Resort, and of WWF/TNC Berau office. The present study was funded by the Netherlands Organisation for Scientific Research (NWO), division Earth and Life Sciences (ALW IPJ-07002, # 817.01.008; ALW-Rubicon # 825.12.007). Fieldwork in Indonesia was made possible through additional financial support of World Wildlife Foundation Netherlands-INNO Fund, the Schure-Beijerinck-Popping Fund of the Royal Dutch Academy of Science (KNAW), the Treub-Maatschappij Fund, the Lerner-Gray Fund for Marine Research (American Natural History Museum), the Leiden University Fund (LUF) /Slingelands, Singapore Airlines, the A.M. Buitendijk Fund and the J.J. ter Pelkwijk Fund. I thank the Indonesian Institute of Sciences (LIPI) and the Indonesian State Ministry of Research and Technology (RISTEK) for providing research permits in Indonesia.

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