Latrunculia (Latrunculia) multirotalis Topsent 1905

Latrunculia (Latrunculia) multirotalis Topsent, 1905 (Figs 1H, 2, 4F; Tables 2 & 3) Latrunculia multirotalis Topsent 1905: 8; Latrunculia multirotalis Topsent 1928: 222, PL. VII, FIG. 19. Holotype material. MNHN L.B.I.M. No D.CL. 1265, spicule slide, W. de Florès (Central Atlantic­ Azores), stn...

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Main Authors: Samaai, Toufiek, Gibbons, Mark J., Kelly, Michelle
Format: Text
Language:unknown
Published: Zenodo 2006
Subjects:
Online Access:https://dx.doi.org/10.5281/zenodo.5057852
https://zenodo.org/record/5057852
id ftdatacite:10.5281/zenodo.5057852
record_format openpolar
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Biodiversity
Taxonomy
Animalia
Porifera
Demospongiae
Poecilosclerida
Latrunculiidae
Latrunculia
Latrunculia multirotalis
spellingShingle Biodiversity
Taxonomy
Animalia
Porifera
Demospongiae
Poecilosclerida
Latrunculiidae
Latrunculia
Latrunculia multirotalis
Samaai, Toufiek
Gibbons, Mark J.
Kelly, Michelle
Latrunculia (Latrunculia) multirotalis Topsent 1905
topic_facet Biodiversity
Taxonomy
Animalia
Porifera
Demospongiae
Poecilosclerida
Latrunculiidae
Latrunculia
Latrunculia multirotalis
description Latrunculia (Latrunculia) multirotalis Topsent, 1905 (Figs 1H, 2, 4F; Tables 2 & 3) Latrunculia multirotalis Topsent 1905: 8; Latrunculia multirotalis Topsent 1928: 222, PL. VII, FIG. 19. Holotype material. MNHN L.B.I.M. No D.CL. 1265, spicule slide, W. de Florès (Central Atlantic­ Azores), stn 2210; depth 1229 m. Description. Small encrusting sponge 2 x 2 x 2 cm diameter. Surface smooth, slightly wrinkled, without distinct openings. Texture unknown. Colour in life unknown; in preservative light brownish olive unknown ( after Topsent ). Skeleton. The choanosomal skeleton consists of styles arranged in a wispy polygonalmeshed reticulation (Fig. 4F). The ectosomal skeleton consists of a paratangential layer of styles with a palisade of erect anisodiscorhabds on the surface. These are also scattered in the choanosome (after Topsent). Spicules. The megascleres are smooth, often slightly polytylote styles, centrally thickened, fusiform and straight, 342 (309–364) x 11 (11) m, n=20. Microscleres (Fig. 1H): anisodiscorhabds are long and hold several spined whorls. The manubrium does not have an expanded, candelabrum­like base, but keeps the form of a straight stem, 6–7 µm thick, armoured with a basal whorl which consists of three horizontal whorls of spines followed by a smooth slender, cylindrical shaft 9 µm long and 7 µm wide. The median whorl is 43–45 µm in diameter and composed of five spines spread out horizontally and divided into three groups, which give eight sets for each of them, and is the largest of the whorls. The subsidiary whorl is slanted upwards. The serrated margins of the median and subsidiary whorls are microspined. The shaft, which thickens between the two discs, fades progressively becoming thinner towards the apical whorl, and having either three, four or even five supplementary subsidiary whorls along the shaft. The apical whorl resembles a small coup edged with teeth and blunt terminally spined cylindrical spines appearing somewhat crown­like. Anisodiscorhabd length, 142 (117–186) µm, n=20. Substratum, depth range and ecology. Found in on muddy environment at a depth of 1229 m. Geographic distribution (Fig. 2). Azores Remarks. One of the key characters that differentiate species within the Latrunculia complex is the development (ontogeny) pattern and structure of the acanthodiscorhabd. As stated above the acanthodiscorhabds of Latrunculia s.s have a straight uniform shaft bearing whorls of crenulated discs (Carter 1879; Samaai and Kelly 2002; Samaai 2002) and develop from a straight protorhabd as indicated by Dendy, (1917) (see also Samaai and Kelly 2002; Samaai 2002 and Samaai et al . 2003; Samaai et al . 2004). All these characters (based only on the acanthodiscorhabds) are visible in L. multirotalis , suggesting that it is a valid species of Latrunculia . Apart from this it also possesses the basal whorl just above the manubrium as indicative of the subgenus Latrunculia This species is most distinctive, however, as it differs substantially from other Latrunculia species in the size and structure of the anisodiscorhabds (Table 3); it possesses multi­crenulated discs along a long shaft. Hinde and Holmes (1892) (PG. 219, FIG. 34, 35) (see also Wiedenmayer, 1994) recorded a fossil anisodiscorhabd with multiple whorls from the Oamaru Diatomite, New Zealand, for a species ( Latrunculia. sp Hinde and Holmes, PG 218, PL. XI, FIG. 35) that occurred during the late Eocene­early Oligocene era. These authors also suggested that this form was a modification of a common plane (two whorls), which ultimately gave rise to the multi­crenulated discs as found in L. multirotalis . The discorhabd structure of the extant Latrunculia multirotalis differs however from the fossil spicule in that the shaft possess multiple spines (as appose to whorls) and in the length of the spicule, which is much larger in size (206 µm) than what is recorded for L. multirotalis . It is difficult to say whether the fossil acanthodiscorhabds are homologous to that found in the extant species, but it does suggest that several species of "latrunculids" must have coexisted at the source of this assemblage (See also Wiedenmayer 1994). The species L. multirotalis was only ever recorded from the North Atlantic off Azores (Table 2). : Published as part of Samaai, Toufiek, Gibbons, Mark J. & Kelly, Michelle, 2006, Revision of the genus Latrunculia du Bocage, 1869 Porifera: Demospongiae: Latrunculiidae) with descriptions of new species from New Caledonia and the Northeastern Pacific (, pp. 1-71 in Zootaxa 1127 (1) on pages 36-38, DOI: 10.11646/zootaxa.1127.1.1, http://zenodo.org/record/5057828 : {"references": ["Topsent, E. (1905) Spongiaires des Acores. Resultats Des campagnes scientifiques accomplies par le Prince Albert I, Monaco, 25, 1 - 280, pls 1 - 18.", "Topsent, E. (1928) Spongiaires de l'Atlantique et de la Mediteranee provenant de croisieres du Prince Albert ler de Monaco. Resultats Des campagnes scientifiques accomplies par le Prince Albert I, Monaco, 74, 376 pp., 11 pls.", "Carter, H. J. (1879) Contribution to our knowledge of the Spongida. Annals and Magazine of Natural History, (5) 3, 284 - 304, 343 - 360, pls 25 - 29.", "Samaai, T. & Kelly, M. (2002) Family Latrunculiidae. In: Hooper, J. N. A., & R. W. M. Soest, Van (eds). Systema Porifera. Guide to the supraspecific classification of sponges and spongiomorphs (Porifera). Plenum, New York, pp. 708 - 719.", "Samaai, T., Gibbons, M. J., Kelly, M & Davies-Coleman, M. (2003) South African Latrunculiidae (Porifera: Demospongiae: Poecilosclerida): descriptions of new species of Latrunculia du Bocage, Strongylodesma Levi, and Tsitsikamma Samaai & Kelly. Zootaxa, 371, 1 - 26", "Samaai, T. Govender, V and Kelly, M. (2004) Cyclacanthia n. g. (Demospongiae: Poecilosclerida: Latrunculiidae incertea sedis), a new genus of marine sponges from South African waters, and description of two new species. Zootaxa, 725, 1 - 18.", "Hinde, G. J. & Holmes, W. M. (1892) On the sponge-remains in the lower Tertiary Strata near Oamaru, Otago, New Zealand. Journal of the Linnean Society. Zoology, 24, 177 - 262.", "Wiedenmayer, F. (1994) Contributions to the knowledge of post-Palaeozoic neritic and archibenthal sponges (Porifera). The stratigraphic record, ecology, and global distribution of intermediate and higher taxa. Schweizerische Palaontologische Abhandlungen, 116, 1 - 147."]}
format Text
author Samaai, Toufiek
Gibbons, Mark J.
Kelly, Michelle
author_facet Samaai, Toufiek
Gibbons, Mark J.
Kelly, Michelle
author_sort Samaai, Toufiek
title Latrunculia (Latrunculia) multirotalis Topsent 1905
title_short Latrunculia (Latrunculia) multirotalis Topsent 1905
title_full Latrunculia (Latrunculia) multirotalis Topsent 1905
title_fullStr Latrunculia (Latrunculia) multirotalis Topsent 1905
title_full_unstemmed Latrunculia (Latrunculia) multirotalis Topsent 1905
title_sort latrunculia (latrunculia) multirotalis topsent 1905
publisher Zenodo
publishDate 2006
url https://dx.doi.org/10.5281/zenodo.5057852
https://zenodo.org/record/5057852
long_lat ENVELOPE(163.400,163.400,-77.533,-77.533)
geographic Coleman
New Zealand
Pacific
geographic_facet Coleman
New Zealand
Pacific
genre North Atlantic
genre_facet North Atlantic
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spelling ftdatacite:10.5281/zenodo.5057852 2023-05-15T17:37:36+02:00 Latrunculia (Latrunculia) multirotalis Topsent 1905 Samaai, Toufiek Gibbons, Mark J. Kelly, Michelle 2006 https://dx.doi.org/10.5281/zenodo.5057852 https://zenodo.org/record/5057852 unknown Zenodo http://zenodo.org/record/5057828 http://publication.plazi.org/id/FFB46370135EFFB9FFDFFFBE3668F90A http://zoobank.org/E3B8BACE-1E5B-4E07-AB94-A4947F966483 https://zenodo.org/communities/biosyslit https://dx.doi.org/10.11646/zootaxa.1127.1.1 http://zenodo.org/record/5057828 http://publication.plazi.org/id/FFB46370135EFFB9FFDFFFBE3668F90A https://dx.doi.org/10.5281/zenodo.5057830 https://dx.doi.org/10.5281/zenodo.5057832 http://zoobank.org/E3B8BACE-1E5B-4E07-AB94-A4947F966483 https://dx.doi.org/10.5281/zenodo.5057851 https://zenodo.org/communities/biosyslit Open Access info:eu-repo/semantics/openAccess Biodiversity Taxonomy Animalia Porifera Demospongiae Poecilosclerida Latrunculiidae Latrunculia Latrunculia multirotalis Text Taxonomic treatment article-journal ScholarlyArticle 2006 ftdatacite https://doi.org/10.5281/zenodo.5057852 https://doi.org/10.11646/zootaxa.1127.1.1 https://doi.org/10.5281/zenodo.5057830 https://doi.org/10.5281/zenodo.5057832 https://doi.org/10.5281/zenodo.5057851 2021-11-05T12:55:41Z Latrunculia (Latrunculia) multirotalis Topsent, 1905 (Figs 1H, 2, 4F; Tables 2 & 3) Latrunculia multirotalis Topsent 1905: 8; Latrunculia multirotalis Topsent 1928: 222, PL. VII, FIG. 19. Holotype material. MNHN L.B.I.M. No D.CL. 1265, spicule slide, W. de Florès (Central Atlantic­ Azores), stn 2210; depth 1229 m. Description. Small encrusting sponge 2 x 2 x 2 cm diameter. Surface smooth, slightly wrinkled, without distinct openings. Texture unknown. Colour in life unknown; in preservative light brownish olive unknown ( after Topsent ). Skeleton. The choanosomal skeleton consists of styles arranged in a wispy polygonalmeshed reticulation (Fig. 4F). The ectosomal skeleton consists of a paratangential layer of styles with a palisade of erect anisodiscorhabds on the surface. These are also scattered in the choanosome (after Topsent). Spicules. The megascleres are smooth, often slightly polytylote styles, centrally thickened, fusiform and straight, 342 (309–364) x 11 (11) m, n=20. Microscleres (Fig. 1H): anisodiscorhabds are long and hold several spined whorls. The manubrium does not have an expanded, candelabrum­like base, but keeps the form of a straight stem, 6–7 µm thick, armoured with a basal whorl which consists of three horizontal whorls of spines followed by a smooth slender, cylindrical shaft 9 µm long and 7 µm wide. The median whorl is 43–45 µm in diameter and composed of five spines spread out horizontally and divided into three groups, which give eight sets for each of them, and is the largest of the whorls. The subsidiary whorl is slanted upwards. The serrated margins of the median and subsidiary whorls are microspined. The shaft, which thickens between the two discs, fades progressively becoming thinner towards the apical whorl, and having either three, four or even five supplementary subsidiary whorls along the shaft. The apical whorl resembles a small coup edged with teeth and blunt terminally spined cylindrical spines appearing somewhat crown­like. Anisodiscorhabd length, 142 (117–186) µm, n=20. Substratum, depth range and ecology. Found in on muddy environment at a depth of 1229 m. Geographic distribution (Fig. 2). Azores Remarks. One of the key characters that differentiate species within the Latrunculia complex is the development (ontogeny) pattern and structure of the acanthodiscorhabd. As stated above the acanthodiscorhabds of Latrunculia s.s have a straight uniform shaft bearing whorls of crenulated discs (Carter 1879; Samaai and Kelly 2002; Samaai 2002) and develop from a straight protorhabd as indicated by Dendy, (1917) (see also Samaai and Kelly 2002; Samaai 2002 and Samaai et al . 2003; Samaai et al . 2004). All these characters (based only on the acanthodiscorhabds) are visible in L. multirotalis , suggesting that it is a valid species of Latrunculia . Apart from this it also possesses the basal whorl just above the manubrium as indicative of the subgenus Latrunculia This species is most distinctive, however, as it differs substantially from other Latrunculia species in the size and structure of the anisodiscorhabds (Table 3); it possesses multi­crenulated discs along a long shaft. Hinde and Holmes (1892) (PG. 219, FIG. 34, 35) (see also Wiedenmayer, 1994) recorded a fossil anisodiscorhabd with multiple whorls from the Oamaru Diatomite, New Zealand, for a species ( Latrunculia. sp Hinde and Holmes, PG 218, PL. XI, FIG. 35) that occurred during the late Eocene­early Oligocene era. These authors also suggested that this form was a modification of a common plane (two whorls), which ultimately gave rise to the multi­crenulated discs as found in L. multirotalis . The discorhabd structure of the extant Latrunculia multirotalis differs however from the fossil spicule in that the shaft possess multiple spines (as appose to whorls) and in the length of the spicule, which is much larger in size (206 µm) than what is recorded for L. multirotalis . It is difficult to say whether the fossil acanthodiscorhabds are homologous to that found in the extant species, but it does suggest that several species of "latrunculids" must have coexisted at the source of this assemblage (See also Wiedenmayer 1994). The species L. multirotalis was only ever recorded from the North Atlantic off Azores (Table 2). : Published as part of Samaai, Toufiek, Gibbons, Mark J. & Kelly, Michelle, 2006, Revision of the genus Latrunculia du Bocage, 1869 Porifera: Demospongiae: Latrunculiidae) with descriptions of new species from New Caledonia and the Northeastern Pacific (, pp. 1-71 in Zootaxa 1127 (1) on pages 36-38, DOI: 10.11646/zootaxa.1127.1.1, http://zenodo.org/record/5057828 : {"references": ["Topsent, E. (1905) Spongiaires des Acores. Resultats Des campagnes scientifiques accomplies par le Prince Albert I, Monaco, 25, 1 - 280, pls 1 - 18.", "Topsent, E. (1928) Spongiaires de l'Atlantique et de la Mediteranee provenant de croisieres du Prince Albert ler de Monaco. Resultats Des campagnes scientifiques accomplies par le Prince Albert I, Monaco, 74, 376 pp., 11 pls.", "Carter, H. J. (1879) Contribution to our knowledge of the Spongida. Annals and Magazine of Natural History, (5) 3, 284 - 304, 343 - 360, pls 25 - 29.", "Samaai, T. & Kelly, M. (2002) Family Latrunculiidae. In: Hooper, J. N. A., & R. W. M. Soest, Van (eds). Systema Porifera. Guide to the supraspecific classification of sponges and spongiomorphs (Porifera). Plenum, New York, pp. 708 - 719.", "Samaai, T., Gibbons, M. J., Kelly, M & Davies-Coleman, M. (2003) South African Latrunculiidae (Porifera: Demospongiae: Poecilosclerida): descriptions of new species of Latrunculia du Bocage, Strongylodesma Levi, and Tsitsikamma Samaai & Kelly. Zootaxa, 371, 1 - 26", "Samaai, T. Govender, V and Kelly, M. (2004) Cyclacanthia n. g. (Demospongiae: Poecilosclerida: Latrunculiidae incertea sedis), a new genus of marine sponges from South African waters, and description of two new species. Zootaxa, 725, 1 - 18.", "Hinde, G. J. & Holmes, W. M. (1892) On the sponge-remains in the lower Tertiary Strata near Oamaru, Otago, New Zealand. Journal of the Linnean Society. Zoology, 24, 177 - 262.", "Wiedenmayer, F. (1994) Contributions to the knowledge of post-Palaeozoic neritic and archibenthal sponges (Porifera). The stratigraphic record, ecology, and global distribution of intermediate and higher taxa. Schweizerische Palaontologische Abhandlungen, 116, 1 - 147."]} Text North Atlantic DataCite Metadata Store (German National Library of Science and Technology) Coleman ENVELOPE(163.400,163.400,-77.533,-77.533) New Zealand Pacific