Ageria laxa Hansen 2019, n. sp.

Ageria laxa n. sp. Figs 29 C–E Diagnosis. An Ageria with approximately two smooth protoconch whorls. Teleoconch strongly and fairly densely sculptured; last whorl widening with base contour shifting from flat to strongly convex. Derivation of name. Refers to the strong widening of the last whorl see...

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Main Author: Hansen, Thomas
Format: Text
Language:unknown
Published: Zenodo 2019
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Online Access:https://dx.doi.org/10.5281/zenodo.5582884
https://zenodo.org/record/5582884
id ftdatacite:10.5281/zenodo.5582884
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
Gastropoda
Neotaenioglossa
Procerithiidae
Ageria
Ageria laxa
spellingShingle Biodiversity
Taxonomy
Animalia
Mollusca
Gastropoda
Neotaenioglossa
Procerithiidae
Ageria
Ageria laxa
Hansen, Thomas
Ageria laxa Hansen 2019, n. sp.
topic_facet Biodiversity
Taxonomy
Animalia
Mollusca
Gastropoda
Neotaenioglossa
Procerithiidae
Ageria
Ageria laxa
description Ageria laxa n. sp. Figs 29 C–E Diagnosis. An Ageria with approximately two smooth protoconch whorls. Teleoconch strongly and fairly densely sculptured; last whorl widening with base contour shifting from flat to strongly convex. Derivation of name. Refers to the strong widening of the last whorl seen on large specimens. Type material. The holotype MGUH 33227 is a nearly complete external mould with protoconch. Paratype MGUH 33228 is from the Cerithium Limestone Member at Stevns Klint. Additional material. ØSM.10042-133 and ØSM.10042-388-a comes from the Crab Layer in the Korsnaeb Member. A mould in the informally catalogued sample SR.296.B–C and an additional three external and internal moulds without numbers are from the Cerithium Limestone Member and belong to the Natural History Museum of Denmark. Type stratum and type locality. The Crab Layer, a hardground related lithified bed approximately two metres up in the Korsnaeb Member of the lower Danian Stevns Klint Formation at Stevns Klint. Occurrence. The lower Danian Cerithium Limestone Member of the Rødvig Formation and up into the Crab Layer, located about two metres up in the Korsnaeb Member of the Stevns Klint Formation at Stevns. Stevns Klint: Rødvig, Korsnaeb, Skeldervig, Højerup and Holtug Quarry. Description. Protoconch 0.3 mm high and 0.3 mm wide, consisting of around two smooth, slightly convex whorls forming a continuation of teleoconch spire. Teleoconch very slender coeloconoid; initial whorls slightly convex, becoming gradually more flattened abapically. Whorls moderately low, height on teleoconch whorl 16 corresponding to approximately 45 % the width. Suture narrow, distinct, but not deep. Keel sharp, located at transition to base at abapical suture line. Base flat with short anterior canal. Last whorl on large specimens may increase dramatically in width, becoming more convex with the keel changing to a more central location on the whorl before disappearing just behind aperture. Aperture rounded subrectangular with smooth, slightly concave columella. Teleoconch strongly sculptured adapically, becoming smoother abapically with only weak spiral ribs on base of inflated final whorl. First whorl with five to six strong transverse ribs on a half whorl, crossed by two weaker spiral ribs, forming two weak tubercles on transverse ribs. A third, narrower adapical spiral rib is added on third whorl. Spiral ribs increase rapidly in number while becoming finer. Transverse ribs may increase slowly or faster in number abapically, while tubercles become more pronounced, arranged in up to four rows. Keel carrying narrow spiral rib, which may be slightly serrated due to densely spaced growth lines. Base with single primary spiral rib slightly adaxially of keel rib and succeeded by closely spaced, weaker secondary spirals. Growth lines closely and evenly spaced, nearly straight adapically of keel, weakly opisthocyrt. Measurements. The holotype MGUH 33227 is 16.2 mm high and 4.8 mm wide with 19 whorls. Largest examined specimen is 15.4 mm wide. Remarks. The Danish early Danian Ageria laxa n. sp. resembles the Maastrichtian A. weeksi Wade, 1926 from the Ripley Formation of southern United States, but is distinguished by the higher number of tubercle rows on the later whorls and the apparently two and not three smooth protoconch whorls. It differs from the Maastrichtian Ageria gankinensis Kaim et al ., 2004 from northern Russia by having a more convex base, a stronger developed anterior canal and apparently by having only two protoconch whorls. It is furthermore distinguished from the two British late Albian species A. gaultina Abbass, 1973 and A. costata (Sowerby, 1827) by the distinctly less pronounced spiral ribs and growth line sculpture and by a slightly more convex base. The differences between Ageria laxa n. sp. and Ageria skeldervigensis n. sp. are presented above in the remarks for the latter species. : Published as part of Hansen, Thomas, 2019, Gastropods from the Cretaceous-Palaeogene boundary in Denmark, pp. 1-196 in Zootaxa 4654 (1) on page 124, DOI: 10.11646/zootaxa.4654.1.1, http://zenodo.org/record/3365803 : {"references": ["Wade, B. (1926) The fauna of the Ripley formation of Coon Creek, Tennessee. U. S. Geological Survey Professional Paper, 137, 1 - 272. https: // doi. org / 10.3133 / pp 137", "Kaim, A., Beisel, A. L. & Kurushin, N. I. (2004) Mesozoic gastropods from Siberia and Timan (Russia). Part 1: Vetigastropoda and Caenogastropoda (exclusive of Neogastropoda). Polish Polar Research, 25, 241 - 266.", "Abbass, H. L. (1973) Some British Cretaceous Gastropods belonging to the Families Procerithiidae, Cerithiidae and Cerithiopsidae (Cerithiacea). Bulletin of the British Museum (Natural History), Geology, 23 (2), 103 - 175, pls. 1 - 8.", "Sowerby, J. de C. (1827) The Mineral Conchology of Great Britain, or coloured figures and descriptions of those remains of testaceous animals or shells, which have been preserved at various times, and depths in the earth, 6, 94 - 99. [London, 87 - 156, pls. 546 - 580]"]}
format Text
author Hansen, Thomas
author_facet Hansen, Thomas
author_sort Hansen, Thomas
title Ageria laxa Hansen 2019, n. sp.
title_short Ageria laxa Hansen 2019, n. sp.
title_full Ageria laxa Hansen 2019, n. sp.
title_fullStr Ageria laxa Hansen 2019, n. sp.
title_full_unstemmed Ageria laxa Hansen 2019, n. sp.
title_sort ageria laxa hansen 2019, n. sp.
publisher Zenodo
publishDate 2019
url https://dx.doi.org/10.5281/zenodo.5582884
https://zenodo.org/record/5582884
long_lat ENVELOPE(-17.055,-17.055,65.344,65.344)
geographic Laxa
geographic_facet Laxa
genre Polish Polar Research
Siberia
genre_facet Polish Polar Research
Siberia
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spelling ftdatacite:10.5281/zenodo.5582884 2023-05-15T18:02:59+02:00 Ageria laxa Hansen 2019, n. sp. Hansen, Thomas 2019 https://dx.doi.org/10.5281/zenodo.5582884 https://zenodo.org/record/5582884 unknown Zenodo http://zenodo.org/record/3365803 http://publication.plazi.org/id/43218E4BA900FFE52B0BC14DFFA9FFE3 http://zoobank.org/CFD82CC0-3110-472E-972B-7ADC0C523A04 https://zenodo.org/communities/biosyslit https://dx.doi.org/10.11646/zootaxa.4654.1.1 http://zenodo.org/record/3365803 http://publication.plazi.org/id/43218E4BA900FFE52B0BC14DFFA9FFE3 https://dx.doi.org/10.5281/zenodo.3442114 http://zoobank.org/CFD82CC0-3110-472E-972B-7ADC0C523A04 https://dx.doi.org/10.5281/zenodo.5582883 https://zenodo.org/communities/biosyslit Open Access info:eu-repo/semantics/openAccess Biodiversity Taxonomy Animalia Mollusca Gastropoda Neotaenioglossa Procerithiidae Ageria Ageria laxa Text Taxonomic treatment article-journal ScholarlyArticle 2019 ftdatacite https://doi.org/10.5281/zenodo.5582884 https://doi.org/10.11646/zootaxa.4654.1.1 https://doi.org/10.5281/zenodo.3442114 https://doi.org/10.5281/zenodo.5582883 2021-11-05T12:55:41Z Ageria laxa n. sp. Figs 29 C–E Diagnosis. An Ageria with approximately two smooth protoconch whorls. Teleoconch strongly and fairly densely sculptured; last whorl widening with base contour shifting from flat to strongly convex. Derivation of name. Refers to the strong widening of the last whorl seen on large specimens. Type material. The holotype MGUH 33227 is a nearly complete external mould with protoconch. Paratype MGUH 33228 is from the Cerithium Limestone Member at Stevns Klint. Additional material. ØSM.10042-133 and ØSM.10042-388-a comes from the Crab Layer in the Korsnaeb Member. A mould in the informally catalogued sample SR.296.B–C and an additional three external and internal moulds without numbers are from the Cerithium Limestone Member and belong to the Natural History Museum of Denmark. Type stratum and type locality. The Crab Layer, a hardground related lithified bed approximately two metres up in the Korsnaeb Member of the lower Danian Stevns Klint Formation at Stevns Klint. Occurrence. The lower Danian Cerithium Limestone Member of the Rødvig Formation and up into the Crab Layer, located about two metres up in the Korsnaeb Member of the Stevns Klint Formation at Stevns. Stevns Klint: Rødvig, Korsnaeb, Skeldervig, Højerup and Holtug Quarry. Description. Protoconch 0.3 mm high and 0.3 mm wide, consisting of around two smooth, slightly convex whorls forming a continuation of teleoconch spire. Teleoconch very slender coeloconoid; initial whorls slightly convex, becoming gradually more flattened abapically. Whorls moderately low, height on teleoconch whorl 16 corresponding to approximately 45 % the width. Suture narrow, distinct, but not deep. Keel sharp, located at transition to base at abapical suture line. Base flat with short anterior canal. Last whorl on large specimens may increase dramatically in width, becoming more convex with the keel changing to a more central location on the whorl before disappearing just behind aperture. Aperture rounded subrectangular with smooth, slightly concave columella. Teleoconch strongly sculptured adapically, becoming smoother abapically with only weak spiral ribs on base of inflated final whorl. First whorl with five to six strong transverse ribs on a half whorl, crossed by two weaker spiral ribs, forming two weak tubercles on transverse ribs. A third, narrower adapical spiral rib is added on third whorl. Spiral ribs increase rapidly in number while becoming finer. Transverse ribs may increase slowly or faster in number abapically, while tubercles become more pronounced, arranged in up to four rows. Keel carrying narrow spiral rib, which may be slightly serrated due to densely spaced growth lines. Base with single primary spiral rib slightly adaxially of keel rib and succeeded by closely spaced, weaker secondary spirals. Growth lines closely and evenly spaced, nearly straight adapically of keel, weakly opisthocyrt. Measurements. The holotype MGUH 33227 is 16.2 mm high and 4.8 mm wide with 19 whorls. Largest examined specimen is 15.4 mm wide. Remarks. The Danish early Danian Ageria laxa n. sp. resembles the Maastrichtian A. weeksi Wade, 1926 from the Ripley Formation of southern United States, but is distinguished by the higher number of tubercle rows on the later whorls and the apparently two and not three smooth protoconch whorls. It differs from the Maastrichtian Ageria gankinensis Kaim et al ., 2004 from northern Russia by having a more convex base, a stronger developed anterior canal and apparently by having only two protoconch whorls. It is furthermore distinguished from the two British late Albian species A. gaultina Abbass, 1973 and A. costata (Sowerby, 1827) by the distinctly less pronounced spiral ribs and growth line sculpture and by a slightly more convex base. The differences between Ageria laxa n. sp. and Ageria skeldervigensis n. sp. are presented above in the remarks for the latter species. : Published as part of Hansen, Thomas, 2019, Gastropods from the Cretaceous-Palaeogene boundary in Denmark, pp. 1-196 in Zootaxa 4654 (1) on page 124, DOI: 10.11646/zootaxa.4654.1.1, http://zenodo.org/record/3365803 : {"references": ["Wade, B. (1926) The fauna of the Ripley formation of Coon Creek, Tennessee. U. S. Geological Survey Professional Paper, 137, 1 - 272. https: // doi. org / 10.3133 / pp 137", "Kaim, A., Beisel, A. L. & Kurushin, N. I. (2004) Mesozoic gastropods from Siberia and Timan (Russia). Part 1: Vetigastropoda and Caenogastropoda (exclusive of Neogastropoda). Polish Polar Research, 25, 241 - 266.", "Abbass, H. L. (1973) Some British Cretaceous Gastropods belonging to the Families Procerithiidae, Cerithiidae and Cerithiopsidae (Cerithiacea). Bulletin of the British Museum (Natural History), Geology, 23 (2), 103 - 175, pls. 1 - 8.", "Sowerby, J. de C. (1827) The Mineral Conchology of Great Britain, or coloured figures and descriptions of those remains of testaceous animals or shells, which have been preserved at various times, and depths in the earth, 6, 94 - 99. [London, 87 - 156, pls. 546 - 580]"]} Text Polish Polar Research Siberia DataCite Metadata Store (German National Library of Science and Technology) Laxa ENVELOPE(-17.055,-17.055,65.344,65.344)