Savignaster septemtrionalis Rousseau & Gale & Thuy 2018, sp. nov.
Savignaster septemtrionalis Rousseau & Gale sp. nov. urn:lsid:zoobank.org:act: EF6444E7-C91F-478B-9575-F7E67E4C58D2 Fig. 3 Diagnosis Savignaster in which the ambulacral bases and shafts are very elongated and poorly differentiated. Etymology The specific epithet is from the Latin ‘ septemtrional...
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2018
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Online Access: | https://dx.doi.org/10.5281/zenodo.3816171 https://zenodo.org/record/3816171 |
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ftdatacite:10.5281/zenodo.3816171 |
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openpolar |
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Open Polar |
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DataCite Metadata Store (German National Library of Science and Technology) |
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topic |
Biodiversity Taxonomy Animalia Echinodermata Asteroidea Velatida Pterasteridae Savignaster Savignaster septemtrionalis |
spellingShingle |
Biodiversity Taxonomy Animalia Echinodermata Asteroidea Velatida Pterasteridae Savignaster Savignaster septemtrionalis Rousseau, Julie Gale, Andrew Scott Thuy, Ben Savignaster septemtrionalis Rousseau & Gale & Thuy 2018, sp. nov. |
topic_facet |
Biodiversity Taxonomy Animalia Echinodermata Asteroidea Velatida Pterasteridae Savignaster Savignaster septemtrionalis |
description |
Savignaster septemtrionalis Rousseau & Gale sp. nov. urn:lsid:zoobank.org:act: EF6444E7-C91F-478B-9575-F7E67E4C58D2 Fig. 3 Diagnosis Savignaster in which the ambulacral bases and shafts are very elongated and poorly differentiated. Etymology The specific epithet is from the Latin ‘ septemtrionalis ’, northern, in reference to the high latitudinal position of the locality. Material examined Holotype NORWAY: central Spitsbergen, Knorringfjellet, 78°18′04.4″ N, 16°16′02.0″ E (PMO 218.000). Paratypes NORWAY: same location as for holotype (PMO 217.976, PMO 217.977, PMO 217.978, PMO 218.008). Ten partial specimens were found at the type locality. Type stratum Middle Volgian (Tithonian), Slottsmøya Member, Agardhfjellet Formation. Description The holotype PMO 218.000 (Fig. 3 A–B) is an articulated arm and interradial area, which also shows some portions of a second arm belonging to the same individual. Ambulacrals and adambulacrals are clearly exposed in a transverse section of the groove and disc. The arms are triangular and taper rapidly, and the interradius is acutely angled. The major radius of the holotype (R) is 45 mm, the minor radius (r) 15 mm. The base of the arm is 20 mm across. There are over 30 pairs of ambulacrals and adambulacrals present in each half radius and the two plate rows are of approximately equal width. The ambulacral heads have a large triangular proximal extension and are imbricated proximally. The ambulacrals shafts and bases are elongated and narrow and set nearly at right angles to the axis of the arm. Paratypes PMO 217.976 (Fig. 3C) and PMO 217.977 (Fig. 3D) also show the arrangement of the ambulacral ossicles. Ambulacrals and adambulacrals alternate, and the adambulacrals are slanted laterally and distally. The adambulacrals comprise two parts; a thicker adradial region and a narrow, parallel sided elongated adambulacral extension as in Savignaster wardi (Gale 2011 a, 2011b). The adradial portions are thickened where spine bases were present. In the holotype, scattered abactinal ossicles lie alongside the lateral margin of the adambulacrals (Fig. 3 A–B) and, evidently, the individual was obliquely compacted with the abactinal surface pushed over the adambulacrals. The abactinal ossicles are poorly preserved, but include forms with a pedicel and at least some are identifiable as megapaxillae. Interradial chevron ossicles are present in the interradial region. They form a laterally diverging V-arrangement of nine to ten closely spaced plate pairs situated symmetrically across the interradial line (Fig. 4 A–B). In paratype specimen PMO 217.978, poorly preserved flattened spines are seen attached to the lateral margins of the adambulacrals (Fig. 3E). These have a rounded basal portion and a flattened, trellis-like distal part; they are comparable in shape with spines on the holotype of Savignaster wardi (Gale 2011a: pl. 21 figs 2, 5). This particular spine morphology is also clearly visible in paratype PMO 218.008 (Fig. 3F), a partial arm preserving multiple articulated spines. Remarks The specimens consist of individuals which have split horizontally approximately along the plane of the ambitus, an unusual preservation mode. The presence of interradial chevron ossicles permit placement of the new species in the clade including Korethrasteridae and Pterasteridae (Gale 2011 a, 2011b). It can furthermore be assigned to Savignaster based on the similarity of the shape (long adambulacral extensions) of the adambulacrals to those of S. wardi Gale, 2011. The ambulacrals differ significantly in shape from those of both S. wardi and S. trimbachensis (Gale 2011a: pl. 23) in which club-shaped, quite well-differentiated ambulacral bases are present; the ambulacral shafts and bases are considerably elongated, undifferentiated, and very short with parallel sides in S. septemtrionalis sp. nov. Savignaster was identified by Gale (2011 a, 2011b) as a basal pterasterid, which possesses most, but not all of the synapomorphies of extant members of the family. Savignaster is known from the Bathonian of Kutch, India (A.S. Gale, pers. obs.), the Oxfordian of Switzerland and France (Gale 2011 a, 2011b) and now from the Volgian of Spitsbergen. The Knorringfjellet specimens represent the first articulated material of the genus Savignaster in which the arrangement of the ambulacral groove ossicles can be seen. In the original description of the genus Savignaster , Gale (2011a) inferred that the type species lacked the abactinal canopy typically present in pterasterids. In Savignaster , the abactinal and lateral adambulacral spines are enlarged and highly muscularized, features which would prevent their enclosure within a canopy membrane. However, as noted by Gale (2011a), Savignaster was probably capable of reducing its coelomic volume by contracting muscles present between abactinal ossicles, thus pushing out the papulae and increasing its respiratory surface. Nance & Braithwaite (1972) discussed a similar contraction capacity in Recent mucus-secreting Pteraster tesselatus and Gale (2011a) suggested improvement of oxygen uptake as a driver of specialized pterasterid evolution. Accordingly, Savignaster septemtrionalis sp. nov. would have been well adapted to the fluctuating oxygen availability in the Late Jurassic Palaeo- Barents Sea of Spitsbergen. : Published as part of Rousseau, Julie, Gale, Andrew Scott & Thuy, Ben, 2018, New articulated asteroids (Echinodermata, Asteroidea) and ophiuroids (Echinodermata, Ophiuroidea) from the Late Jurassic (Volgian / Tithonian) of central Spitsbergen, pp. 1-26 in European Journal of Taxonomy 411 on pages 9-10, DOI: 10.5852/ejt.2018.411, http://zenodo.org/record/3805999 : {"references": ["Gale A. S. 2011 a. Phylogeny of the Neoasteroidea (post-Palaeozoic Asteroidea, Echinodermata). Special Papers in Palaeontology 85: 1 - 112.", "Gale A. S. 2011 b. Asteroidea (Echinodermata) from the Oxfordian (Late Jurassic) of Savigna, Departement du Jura, France. Swiss Journal of Palaeontology 130: 69 - 89. https: // doi. org / 10.1007 / s 13358 - 010 - 0008 - x", "Nance J. M. & Braithwaite L. F. 1972. The function of mucus secretions in the cushion star Pteraster tesselatus Ives. Journal of Experimental Marine Biology and Ecology 40: 259 - 266."]} |
format |
Text |
author |
Rousseau, Julie Gale, Andrew Scott Thuy, Ben |
author_facet |
Rousseau, Julie Gale, Andrew Scott Thuy, Ben |
author_sort |
Rousseau, Julie |
title |
Savignaster septemtrionalis Rousseau & Gale & Thuy 2018, sp. nov. |
title_short |
Savignaster septemtrionalis Rousseau & Gale & Thuy 2018, sp. nov. |
title_full |
Savignaster septemtrionalis Rousseau & Gale & Thuy 2018, sp. nov. |
title_fullStr |
Savignaster septemtrionalis Rousseau & Gale & Thuy 2018, sp. nov. |
title_full_unstemmed |
Savignaster septemtrionalis Rousseau & Gale & Thuy 2018, sp. nov. |
title_sort |
savignaster septemtrionalis rousseau & gale & thuy 2018, sp. nov. |
publisher |
Zenodo |
publishDate |
2018 |
url |
https://dx.doi.org/10.5281/zenodo.3816171 https://zenodo.org/record/3816171 |
long_lat |
ENVELOPE(13.501,13.501,68.062,68.062) ENVELOPE(-59.617,-59.617,-62.500,-62.500) ENVELOPE(18.833,18.833,78.083,78.083) ENVELOPE(17.415,17.415,78.046,78.046) ENVELOPE(16.128,16.128,78.296,78.296) |
geographic |
Barents Sea Norway Jura Rousseau Agardhfjellet Slottsmøya Knorringfjellet |
geographic_facet |
Barents Sea Norway Jura Rousseau Agardhfjellet Slottsmøya Knorringfjellet |
genre |
Barents Sea Spitsbergen |
genre_facet |
Barents Sea Spitsbergen |
op_relation |
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op_rights |
Open Access Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode cc0-1.0 info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC0 |
op_doi |
https://doi.org/10.5281/zenodo.3816171 https://doi.org/10.5852/ejt.2018.411 https://doi.org/10.5281/zenodo.3806009 https://doi.org/10.5281/zenodo.3806013 https://doi.org/10.5281/zenodo.3816170 |
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spelling |
ftdatacite:10.5281/zenodo.3816171 2023-05-15T15:39:14+02:00 Savignaster septemtrionalis Rousseau & Gale & Thuy 2018, sp. nov. Rousseau, Julie Gale, Andrew Scott Thuy, Ben 2018 https://dx.doi.org/10.5281/zenodo.3816171 https://zenodo.org/record/3816171 unknown Zenodo http://zenodo.org/record/3805999 http://publication.plazi.org/id/417EFFD0FFB4D367097AFFA4FFBC0019 http://zoobank.org/20D7A744-CE8B-4E6C-92DA-71A9B8C3D805 https://zenodo.org/communities/biosyslit https://dx.doi.org/10.5852/ejt.2018.411 http://zenodo.org/record/3805999 http://publication.plazi.org/id/417EFFD0FFB4D367097AFFA4FFBC0019 https://dx.doi.org/10.5281/zenodo.3806009 https://dx.doi.org/10.5281/zenodo.3806013 http://zoobank.org/20D7A744-CE8B-4E6C-92DA-71A9B8C3D805 https://dx.doi.org/10.5281/zenodo.3816170 https://zenodo.org/communities/biosyslit Open Access Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode cc0-1.0 info:eu-repo/semantics/openAccess CC0 Biodiversity Taxonomy Animalia Echinodermata Asteroidea Velatida Pterasteridae Savignaster Savignaster septemtrionalis article-journal ScholarlyArticle Text Taxonomic treatment 2018 ftdatacite https://doi.org/10.5281/zenodo.3816171 https://doi.org/10.5852/ejt.2018.411 https://doi.org/10.5281/zenodo.3806009 https://doi.org/10.5281/zenodo.3806013 https://doi.org/10.5281/zenodo.3816170 2022-03-10T10:45:56Z Savignaster septemtrionalis Rousseau & Gale sp. nov. urn:lsid:zoobank.org:act: EF6444E7-C91F-478B-9575-F7E67E4C58D2 Fig. 3 Diagnosis Savignaster in which the ambulacral bases and shafts are very elongated and poorly differentiated. Etymology The specific epithet is from the Latin ‘ septemtrionalis ’, northern, in reference to the high latitudinal position of the locality. Material examined Holotype NORWAY: central Spitsbergen, Knorringfjellet, 78°18′04.4″ N, 16°16′02.0″ E (PMO 218.000). Paratypes NORWAY: same location as for holotype (PMO 217.976, PMO 217.977, PMO 217.978, PMO 218.008). Ten partial specimens were found at the type locality. Type stratum Middle Volgian (Tithonian), Slottsmøya Member, Agardhfjellet Formation. Description The holotype PMO 218.000 (Fig. 3 A–B) is an articulated arm and interradial area, which also shows some portions of a second arm belonging to the same individual. Ambulacrals and adambulacrals are clearly exposed in a transverse section of the groove and disc. The arms are triangular and taper rapidly, and the interradius is acutely angled. The major radius of the holotype (R) is 45 mm, the minor radius (r) 15 mm. The base of the arm is 20 mm across. There are over 30 pairs of ambulacrals and adambulacrals present in each half radius and the two plate rows are of approximately equal width. The ambulacral heads have a large triangular proximal extension and are imbricated proximally. The ambulacrals shafts and bases are elongated and narrow and set nearly at right angles to the axis of the arm. Paratypes PMO 217.976 (Fig. 3C) and PMO 217.977 (Fig. 3D) also show the arrangement of the ambulacral ossicles. Ambulacrals and adambulacrals alternate, and the adambulacrals are slanted laterally and distally. The adambulacrals comprise two parts; a thicker adradial region and a narrow, parallel sided elongated adambulacral extension as in Savignaster wardi (Gale 2011 a, 2011b). The adradial portions are thickened where spine bases were present. In the holotype, scattered abactinal ossicles lie alongside the lateral margin of the adambulacrals (Fig. 3 A–B) and, evidently, the individual was obliquely compacted with the abactinal surface pushed over the adambulacrals. The abactinal ossicles are poorly preserved, but include forms with a pedicel and at least some are identifiable as megapaxillae. Interradial chevron ossicles are present in the interradial region. They form a laterally diverging V-arrangement of nine to ten closely spaced plate pairs situated symmetrically across the interradial line (Fig. 4 A–B). In paratype specimen PMO 217.978, poorly preserved flattened spines are seen attached to the lateral margins of the adambulacrals (Fig. 3E). These have a rounded basal portion and a flattened, trellis-like distal part; they are comparable in shape with spines on the holotype of Savignaster wardi (Gale 2011a: pl. 21 figs 2, 5). This particular spine morphology is also clearly visible in paratype PMO 218.008 (Fig. 3F), a partial arm preserving multiple articulated spines. Remarks The specimens consist of individuals which have split horizontally approximately along the plane of the ambitus, an unusual preservation mode. The presence of interradial chevron ossicles permit placement of the new species in the clade including Korethrasteridae and Pterasteridae (Gale 2011 a, 2011b). It can furthermore be assigned to Savignaster based on the similarity of the shape (long adambulacral extensions) of the adambulacrals to those of S. wardi Gale, 2011. The ambulacrals differ significantly in shape from those of both S. wardi and S. trimbachensis (Gale 2011a: pl. 23) in which club-shaped, quite well-differentiated ambulacral bases are present; the ambulacral shafts and bases are considerably elongated, undifferentiated, and very short with parallel sides in S. septemtrionalis sp. nov. Savignaster was identified by Gale (2011 a, 2011b) as a basal pterasterid, which possesses most, but not all of the synapomorphies of extant members of the family. Savignaster is known from the Bathonian of Kutch, India (A.S. Gale, pers. obs.), the Oxfordian of Switzerland and France (Gale 2011 a, 2011b) and now from the Volgian of Spitsbergen. The Knorringfjellet specimens represent the first articulated material of the genus Savignaster in which the arrangement of the ambulacral groove ossicles can be seen. In the original description of the genus Savignaster , Gale (2011a) inferred that the type species lacked the abactinal canopy typically present in pterasterids. In Savignaster , the abactinal and lateral adambulacral spines are enlarged and highly muscularized, features which would prevent their enclosure within a canopy membrane. However, as noted by Gale (2011a), Savignaster was probably capable of reducing its coelomic volume by contracting muscles present between abactinal ossicles, thus pushing out the papulae and increasing its respiratory surface. Nance & Braithwaite (1972) discussed a similar contraction capacity in Recent mucus-secreting Pteraster tesselatus and Gale (2011a) suggested improvement of oxygen uptake as a driver of specialized pterasterid evolution. Accordingly, Savignaster septemtrionalis sp. nov. would have been well adapted to the fluctuating oxygen availability in the Late Jurassic Palaeo- Barents Sea of Spitsbergen. : Published as part of Rousseau, Julie, Gale, Andrew Scott & Thuy, Ben, 2018, New articulated asteroids (Echinodermata, Asteroidea) and ophiuroids (Echinodermata, Ophiuroidea) from the Late Jurassic (Volgian / Tithonian) of central Spitsbergen, pp. 1-26 in European Journal of Taxonomy 411 on pages 9-10, DOI: 10.5852/ejt.2018.411, http://zenodo.org/record/3805999 : {"references": ["Gale A. S. 2011 a. Phylogeny of the Neoasteroidea (post-Palaeozoic Asteroidea, Echinodermata). Special Papers in Palaeontology 85: 1 - 112.", "Gale A. S. 2011 b. Asteroidea (Echinodermata) from the Oxfordian (Late Jurassic) of Savigna, Departement du Jura, France. Swiss Journal of Palaeontology 130: 69 - 89. https: // doi. org / 10.1007 / s 13358 - 010 - 0008 - x", "Nance J. M. & Braithwaite L. F. 1972. The function of mucus secretions in the cushion star Pteraster tesselatus Ives. Journal of Experimental Marine Biology and Ecology 40: 259 - 266."]} Text Barents Sea Spitsbergen DataCite Metadata Store (German National Library of Science and Technology) Barents Sea Norway Jura ENVELOPE(13.501,13.501,68.062,68.062) Rousseau ENVELOPE(-59.617,-59.617,-62.500,-62.500) Agardhfjellet ENVELOPE(18.833,18.833,78.083,78.083) Slottsmøya ENVELOPE(17.415,17.415,78.046,78.046) Knorringfjellet ENVELOPE(16.128,16.128,78.296,78.296) |