Camptonectes (Costicamptonectes) milnelandensis Fursich 1982

Camptonectes ( Costicamptonectes ) aff. milnelandensis Fürsich, 1982 (Figure 10 H–K) 1982 aff. Camptonectes ( Costicamptonectes ) milnelandensis sp. nov. —Fürsich, p. 50, figs. 23 C–D, F, G. Material examined. Two poorly preserved right valves. In addition a single external mould with silicone rubbe...

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Main Authors: Hryniewicz, Krzysztof, Little, Crispin T. S., Nakrem, Hans Arne
Format: Text
Language:unknown
Published: Zenodo 2014
Subjects:
Online Access:https://dx.doi.org/10.5281/zenodo.5228250
https://zenodo.org/record/5228250
id ftdatacite:10.5281/zenodo.5228250
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
Mollusca
Bivalvia
Pectinoida
Pectinidae
Camptonectes
Camptonectes milnelandensis
spellingShingle Biodiversity
Taxonomy
Animalia
Mollusca
Bivalvia
Pectinoida
Pectinidae
Camptonectes
Camptonectes milnelandensis
Hryniewicz, Krzysztof
Little, Crispin T. S.
Nakrem, Hans Arne
Camptonectes (Costicamptonectes) milnelandensis Fursich 1982
topic_facet Biodiversity
Taxonomy
Animalia
Mollusca
Bivalvia
Pectinoida
Pectinidae
Camptonectes
Camptonectes milnelandensis
description Camptonectes ( Costicamptonectes ) aff. milnelandensis Fürsich, 1982 (Figure 10 H–K) 1982 aff. Camptonectes ( Costicamptonectes ) milnelandensis sp. nov. —Fürsich, p. 50, figs. 23 C–D, F, G. Material examined. Two poorly preserved right valves. In addition a single external mould with silicone rubber cast from the Dorsoplanites bed (PMO 226.604). See Appendix 1 for the list of specimens. Dimensions. 15–30.5 mm in length, 15–28.2 mm in height. See Appendix 2G for details. Description. Shell small to medium sized, very thin, appears to get shorter at later growth stages. Right valve suborbicular, moderately inflated, with small posterior and larger anterior auricle, ventrally delineated by a deep byssal notch. Ctenolium well developed. Antero- and posterodorsal margins subequal, anterodorsal margin slightly concave. Anterior margin slightly more convex than posterior margin, ventral margin evenly rounded. Preserved ornament consists of weak divaricating radial ribs, intersected by weak but dense growth lines. Anterodorsal margin ornamented by ca. 6 subparallel radial ribs. Left valve, musculature and dentition unknown. Remarks. We compare our specimens with C . ( Co. ) milnelandensis because of its ornament of commarginal growth lines accompanied by divaricate ribs and with additional radial ribs close to the anterodorsal margin. The Svalbard specimens have a slightly higher umbonal angle than comparatively sized specimens of C . ( Co. ) milnelandensis from Greenland (Fürsich 1982). However, no specimens larger than 18 mm were reported by Fürsich (1982) so we are unable to compare the ontogenetic changes of umbonal angle of specimens from both localities. In addition, the Svalbard material is composed of right valves only. Until more is known about C . ( Co. ) milnelandensis from both Greenland and Svalbard, we prefer to leave our species in open nomenclature. Occurrence. Camptonectes ( Co. ) milnelandensis : Upper Callovian–Upper Oxfordian of Milne Land, East Greenland (Fürsich 1982). Camptonectes ( Co. ) aff. milnelandensis : Seep 8 (Upper Volgian), Slottsmøya Member (Tab. 1); also Dorsoplanites bed (Middle Volgian), Svalbard. Palaeoecology. We assume that C . ( Co. ) aff. milnelandensis was a byssally attached suspension feeder, as indicated by the presence of a well-developed ctenolium. Byssal attachment is a characteristic feature for the genus Camptonectes , although larger species in the subgenus McLearnia Crickmay, 1930, probably lost a functional byssal attachment in maturity (e.g. Fürsich 1982). An expanded anterior auricle in pectinids is an adaptation for byssal attachment with the commissure non-perpendicular to the substrate (Stanley 1970). In such a position the auricle and anterior shell margin acts as a fulcrum and prevents the shell overturning from its set position. As in most of the pectinids, C . ( Co. ) aff. milnelandensis probably had the ability to swim to escape predation, although the umbonal angle is too acute to assume this was habitual (Stanley 1970). : Published as part of Hryniewicz, Krzysztof, Little, Crispin T. S. & Nakrem, Hans Arne, 2014, Bivalves from the latest Jurassic-earliest Cretaceous hydrocarbon seep carbonates from central Spitsbergen, Svalbard, pp. 1-66 in Zootaxa 3859 (1) on page 27, DOI: 10.11646/zootaxa.3859.1.1, http://zenodo.org/record/4930112 : {"references": ["Fursich, F. T. (1982) Upper Jurassic bivalves from Milne Land, East Greenland. GrOnlands Geologiske UndersOgelse, 144, 1 - 126.", "Crickmay, C. H. (1930) Fossils from Harrison Lake area, British Columbia. Bulletin of the National Museum of Canada, 63, 33 - 66, pls. 1 - 15.", "Stanley, S. M. (1970) Relation of shell form to life habits of the Bivalvia (Mollusca). The Geological Society of America Memoir, 125, 1 - 296. http: // dx. doi. org / 10.1130 / mem 125 - p 1"]}
format Text
author Hryniewicz, Krzysztof
Little, Crispin T. S.
Nakrem, Hans Arne
author_facet Hryniewicz, Krzysztof
Little, Crispin T. S.
Nakrem, Hans Arne
author_sort Hryniewicz, Krzysztof
title Camptonectes (Costicamptonectes) milnelandensis Fursich 1982
title_short Camptonectes (Costicamptonectes) milnelandensis Fursich 1982
title_full Camptonectes (Costicamptonectes) milnelandensis Fursich 1982
title_fullStr Camptonectes (Costicamptonectes) milnelandensis Fursich 1982
title_full_unstemmed Camptonectes (Costicamptonectes) milnelandensis Fursich 1982
title_sort camptonectes (costicamptonectes) milnelandensis fursich 1982
publisher Zenodo
publishDate 2014
url https://dx.doi.org/10.5281/zenodo.5228250
https://zenodo.org/record/5228250
long_lat ENVELOPE(-125.003,-125.003,54.000,54.000)
ENVELOPE(161.117,161.117,-78.033,-78.033)
ENVELOPE(-26.750,-26.750,70.683,70.683)
ENVELOPE(17.415,17.415,78.046,78.046)
geographic British Columbia
Canada
Fulcrum
Greenland
Milne Land
Slottsmøya
Svalbard
geographic_facet British Columbia
Canada
Fulcrum
Greenland
Milne Land
Slottsmøya
Svalbard
genre East Greenland
Greenland
Milne Land
Svalbard
Spitsbergen
genre_facet East Greenland
Greenland
Milne Land
Svalbard
Spitsbergen
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op_doi https://doi.org/10.5281/zenodo.5228250
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spelling ftdatacite:10.5281/zenodo.5228250 2023-05-15T16:03:51+02:00 Camptonectes (Costicamptonectes) milnelandensis Fursich 1982 Hryniewicz, Krzysztof Little, Crispin T. S. Nakrem, Hans Arne 2014 https://dx.doi.org/10.5281/zenodo.5228250 https://zenodo.org/record/5228250 unknown Zenodo http://zenodo.org/record/4930112 http://publication.plazi.org/id/5E0865359F19E3250471FFA5FFA82955 http://zoobank.org/24FCAAE1-AB7C-4FAD-8698-D0C9F12400EC https://zenodo.org/communities/biosyslit https://dx.doi.org/10.11646/zootaxa.3859.1.1 http://zenodo.org/record/4930112 http://publication.plazi.org/id/5E0865359F19E3250471FFA5FFA82955 https://dx.doi.org/10.5281/zenodo.5228099 http://zoobank.org/24FCAAE1-AB7C-4FAD-8698-D0C9F12400EC https://dx.doi.org/10.5281/zenodo.5228251 https://zenodo.org/communities/biosyslit Open Access info:eu-repo/semantics/openAccess Biodiversity Taxonomy Animalia Mollusca Bivalvia Pectinoida Pectinidae Camptonectes Camptonectes milnelandensis Taxonomic treatment article-journal Text ScholarlyArticle 2014 ftdatacite https://doi.org/10.5281/zenodo.5228250 https://doi.org/10.11646/zootaxa.3859.1.1 https://doi.org/10.5281/zenodo.5228099 https://doi.org/10.5281/zenodo.5228251 2022-02-08T12:07:57Z Camptonectes ( Costicamptonectes ) aff. milnelandensis Fürsich, 1982 (Figure 10 H–K) 1982 aff. Camptonectes ( Costicamptonectes ) milnelandensis sp. nov. —Fürsich, p. 50, figs. 23 C–D, F, G. Material examined. Two poorly preserved right valves. In addition a single external mould with silicone rubber cast from the Dorsoplanites bed (PMO 226.604). See Appendix 1 for the list of specimens. Dimensions. 15–30.5 mm in length, 15–28.2 mm in height. See Appendix 2G for details. Description. Shell small to medium sized, very thin, appears to get shorter at later growth stages. Right valve suborbicular, moderately inflated, with small posterior and larger anterior auricle, ventrally delineated by a deep byssal notch. Ctenolium well developed. Antero- and posterodorsal margins subequal, anterodorsal margin slightly concave. Anterior margin slightly more convex than posterior margin, ventral margin evenly rounded. Preserved ornament consists of weak divaricating radial ribs, intersected by weak but dense growth lines. Anterodorsal margin ornamented by ca. 6 subparallel radial ribs. Left valve, musculature and dentition unknown. Remarks. We compare our specimens with C . ( Co. ) milnelandensis because of its ornament of commarginal growth lines accompanied by divaricate ribs and with additional radial ribs close to the anterodorsal margin. The Svalbard specimens have a slightly higher umbonal angle than comparatively sized specimens of C . ( Co. ) milnelandensis from Greenland (Fürsich 1982). However, no specimens larger than 18 mm were reported by Fürsich (1982) so we are unable to compare the ontogenetic changes of umbonal angle of specimens from both localities. In addition, the Svalbard material is composed of right valves only. Until more is known about C . ( Co. ) milnelandensis from both Greenland and Svalbard, we prefer to leave our species in open nomenclature. Occurrence. Camptonectes ( Co. ) milnelandensis : Upper Callovian–Upper Oxfordian of Milne Land, East Greenland (Fürsich 1982). Camptonectes ( Co. ) aff. milnelandensis : Seep 8 (Upper Volgian), Slottsmøya Member (Tab. 1); also Dorsoplanites bed (Middle Volgian), Svalbard. Palaeoecology. We assume that C . ( Co. ) aff. milnelandensis was a byssally attached suspension feeder, as indicated by the presence of a well-developed ctenolium. Byssal attachment is a characteristic feature for the genus Camptonectes , although larger species in the subgenus McLearnia Crickmay, 1930, probably lost a functional byssal attachment in maturity (e.g. Fürsich 1982). An expanded anterior auricle in pectinids is an adaptation for byssal attachment with the commissure non-perpendicular to the substrate (Stanley 1970). In such a position the auricle and anterior shell margin acts as a fulcrum and prevents the shell overturning from its set position. As in most of the pectinids, C . ( Co. ) aff. milnelandensis probably had the ability to swim to escape predation, although the umbonal angle is too acute to assume this was habitual (Stanley 1970). : Published as part of Hryniewicz, Krzysztof, Little, Crispin T. S. & Nakrem, Hans Arne, 2014, Bivalves from the latest Jurassic-earliest Cretaceous hydrocarbon seep carbonates from central Spitsbergen, Svalbard, pp. 1-66 in Zootaxa 3859 (1) on page 27, DOI: 10.11646/zootaxa.3859.1.1, http://zenodo.org/record/4930112 : {"references": ["Fursich, F. T. (1982) Upper Jurassic bivalves from Milne Land, East Greenland. GrOnlands Geologiske UndersOgelse, 144, 1 - 126.", "Crickmay, C. H. (1930) Fossils from Harrison Lake area, British Columbia. Bulletin of the National Museum of Canada, 63, 33 - 66, pls. 1 - 15.", "Stanley, S. M. (1970) Relation of shell form to life habits of the Bivalvia (Mollusca). The Geological Society of America Memoir, 125, 1 - 296. http: // dx. doi. org / 10.1130 / mem 125 - p 1"]} Text East Greenland Greenland Milne Land Svalbard Spitsbergen DataCite Metadata Store (German National Library of Science and Technology) British Columbia ENVELOPE(-125.003,-125.003,54.000,54.000) Canada Fulcrum ENVELOPE(161.117,161.117,-78.033,-78.033) Greenland Milne Land ENVELOPE(-26.750,-26.750,70.683,70.683) Slottsmøya ENVELOPE(17.415,17.415,78.046,78.046) Svalbard