Quaternary molluscan faunas from the island of Tierra del Fuego after the Last Glacial Maximum
Palaeontological studies on postglacial molluscan faunas from marine deposits located along the northern coast of the Beagle Channel (lat. 54°55’S, long. 68°34’-67°11’W) showed differences of various molluscan assemblages during a period of climatic stability after deglaciation. Oceanographic change...
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2005
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ftjscientiamarin:oai:scientiamarina.revistas.csic.es:article/338 2023-05-15T13:41:51+02:00 Quaternary molluscan faunas from the island of Tierra del Fuego after the Last Glacial Maximum Faunas cuaternarias de moluscos de la isla de Tierra del Fuego después del último máximo glacial Gordillo, Sandra Coronato, Andrea Maria Josefa Rabassa, Jorge Oscar 2005-12-30 application/pdf https://scientiamarina.revistas.csic.es/index.php/scientiamarina/article/view/338 https://doi.org/10.3989/scimar.2005.69s2337 eng eng Consejo Superior de Investigaciones Científicas https://scientiamarina.revistas.csic.es/index.php/scientiamarina/article/view/338/338 https://scientiamarina.revistas.csic.es/index.php/scientiamarina/article/view/338 doi:10.3989/scimar.2005.69s2337 Copyright (c) 2005 Consejo Superior de Investigaciones Científicas (CSIC) https://creativecommons.org/licenses/by/4.0 CC-BY Scientia Marina; Vol. 69 No. S2 (2005); 337-348 Scientia Marina; Vol. 69 Núm. S2 (2005); 337-348 1886-8134 0214-8358 10.3989/scimar.2005.69s2 mollusc assemblages Tierra del Fuego Beagle Channel palaeoenvironments Quaternary asociaciones de moluscos Canal Beagle paleoambientes Cuaternario info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer-reviewed article Artículo revisado por pares 2005 ftjscientiamarin https://doi.org/10.3989/scimar.2005.69s2337 https://doi.org/10.3989/scimar.2005.69s2 2022-03-20T16:30:24Z Palaeontological studies on postglacial molluscan faunas from marine deposits located along the northern coast of the Beagle Channel (lat. 54°55’S, long. 68°34’-67°11’W) showed differences of various molluscan assemblages during a period of climatic stability after deglaciation. Oceanographic changes, different local environmental conditions and/or episodes of minor climatic fluctuations are pointed out as causes for the variations in faunal composition. Comparison with Quaternary molluscs from Antarctica showed that these palaeofaunas overlap slightly at the species level, but have a considerable number of genera (23%) and families (50%) in common. These affinities and relationships are better explained on the basis of more recent migrating taxa than by ancient connections when the two regions formed part of the Weddellian Province. Estudios paleontológicos en faunas de moluscos postglaciales hallados en depósitos marinos sobre la costa norte del Canal Beagle (lat. 54°55’S; long. 68°34’-67°11’O) demostraron que las diferencias en varias asociaciones de moluscos ocurridas en un período de estabilidad climática después de la última deglaciación se deben a variaciones en la composición faunística que siguen a los cambios oceanográficos, a situaciones ambientales localmente diferentes y/o episodios con fluctuaciones climáticas menores. La comparación con moluscos cuaternarios de Antártica muestra que estas faunas tienen un ligero solapamiento a nivel especie, pero un considerable número de géneros (23%) y familias en común (50%). Estas afinidades y relaciones se explican mejor en base a migraciones recientes de taxones, que en base a antiguas conexiones cuando las dos regiones formaban parte de la Provincia Weddelliana Article in Journal/Newspaper Antarc* Antarctica Antártica Tierra del Fuego Scientia Marina (E-Journal) Scientia Marina 69 S2 337 348 |
institution |
Open Polar |
collection |
Scientia Marina (E-Journal) |
op_collection_id |
ftjscientiamarin |
language |
English |
topic |
mollusc assemblages Tierra del Fuego Beagle Channel palaeoenvironments Quaternary asociaciones de moluscos Canal Beagle paleoambientes Cuaternario |
spellingShingle |
mollusc assemblages Tierra del Fuego Beagle Channel palaeoenvironments Quaternary asociaciones de moluscos Canal Beagle paleoambientes Cuaternario Gordillo, Sandra Coronato, Andrea Maria Josefa Rabassa, Jorge Oscar Quaternary molluscan faunas from the island of Tierra del Fuego after the Last Glacial Maximum |
topic_facet |
mollusc assemblages Tierra del Fuego Beagle Channel palaeoenvironments Quaternary asociaciones de moluscos Canal Beagle paleoambientes Cuaternario |
description |
Palaeontological studies on postglacial molluscan faunas from marine deposits located along the northern coast of the Beagle Channel (lat. 54°55’S, long. 68°34’-67°11’W) showed differences of various molluscan assemblages during a period of climatic stability after deglaciation. Oceanographic changes, different local environmental conditions and/or episodes of minor climatic fluctuations are pointed out as causes for the variations in faunal composition. Comparison with Quaternary molluscs from Antarctica showed that these palaeofaunas overlap slightly at the species level, but have a considerable number of genera (23%) and families (50%) in common. These affinities and relationships are better explained on the basis of more recent migrating taxa than by ancient connections when the two regions formed part of the Weddellian Province. Estudios paleontológicos en faunas de moluscos postglaciales hallados en depósitos marinos sobre la costa norte del Canal Beagle (lat. 54°55’S; long. 68°34’-67°11’O) demostraron que las diferencias en varias asociaciones de moluscos ocurridas en un período de estabilidad climática después de la última deglaciación se deben a variaciones en la composición faunística que siguen a los cambios oceanográficos, a situaciones ambientales localmente diferentes y/o episodios con fluctuaciones climáticas menores. La comparación con moluscos cuaternarios de Antártica muestra que estas faunas tienen un ligero solapamiento a nivel especie, pero un considerable número de géneros (23%) y familias en común (50%). Estas afinidades y relaciones se explican mejor en base a migraciones recientes de taxones, que en base a antiguas conexiones cuando las dos regiones formaban parte de la Provincia Weddelliana |
format |
Article in Journal/Newspaper |
author |
Gordillo, Sandra Coronato, Andrea Maria Josefa Rabassa, Jorge Oscar |
author_facet |
Gordillo, Sandra Coronato, Andrea Maria Josefa Rabassa, Jorge Oscar |
author_sort |
Gordillo, Sandra |
title |
Quaternary molluscan faunas from the island of Tierra del Fuego after the Last Glacial Maximum |
title_short |
Quaternary molluscan faunas from the island of Tierra del Fuego after the Last Glacial Maximum |
title_full |
Quaternary molluscan faunas from the island of Tierra del Fuego after the Last Glacial Maximum |
title_fullStr |
Quaternary molluscan faunas from the island of Tierra del Fuego after the Last Glacial Maximum |
title_full_unstemmed |
Quaternary molluscan faunas from the island of Tierra del Fuego after the Last Glacial Maximum |
title_sort |
quaternary molluscan faunas from the island of tierra del fuego after the last glacial maximum |
publisher |
Consejo Superior de Investigaciones Científicas |
publishDate |
2005 |
url |
https://scientiamarina.revistas.csic.es/index.php/scientiamarina/article/view/338 https://doi.org/10.3989/scimar.2005.69s2337 |
genre |
Antarc* Antarctica Antártica Tierra del Fuego |
genre_facet |
Antarc* Antarctica Antártica Tierra del Fuego |
op_source |
Scientia Marina; Vol. 69 No. S2 (2005); 337-348 Scientia Marina; Vol. 69 Núm. S2 (2005); 337-348 1886-8134 0214-8358 10.3989/scimar.2005.69s2 |
op_relation |
https://scientiamarina.revistas.csic.es/index.php/scientiamarina/article/view/338/338 https://scientiamarina.revistas.csic.es/index.php/scientiamarina/article/view/338 doi:10.3989/scimar.2005.69s2337 |
op_rights |
Copyright (c) 2005 Consejo Superior de Investigaciones Científicas (CSIC) https://creativecommons.org/licenses/by/4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.3989/scimar.2005.69s2337 https://doi.org/10.3989/scimar.2005.69s2 |
container_title |
Scientia Marina |
container_volume |
69 |
container_issue |
S2 |
container_start_page |
337 |
op_container_end_page |
348 |
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1766159218701762560 |