Los micromamíferos (Eulipotyphla, Chiroptera, Rodentia y Lagomorpha) del yacimiento del Pleistoceno Superior de la cueva de El Sidrón (Asturias)
© 2018 CSIC. [EN]In the Late Pleistocene site of El Sidrón cave, with a date of ~ 49,000 ky, known for its numerous fossil remains of Neanderthals, some remains of micromammals were found, whose detailed study is carried out in this work. The determined faunal association is the following: Sorex ara...
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Consejo Superior de Investigaciones Científicas (España)
2018
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Online Access: | http://hdl.handle.net/10261/193119 https://doi.org/10.3989/egeol.43122.481 https://doi.org/10.13039/501100006382 https://doi.org/10.13039/100011941 |
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ftcsic:oai:digital.csic.es:10261/193119 2024-02-11T10:05:50+01:00 Los micromamíferos (Eulipotyphla, Chiroptera, Rodentia y Lagomorpha) del yacimiento del Pleistoceno Superior de la cueva de El Sidrón (Asturias) The micromammals (Eulipotyphla, Chiroptera, Rodentia and Lagomorpha) from the Late Pleistocene site of the El Sidrón cave (Asturias) Sesé, Carmen Rasilla, Marco de la Duarte Matías, E. Principado de Asturias Universidad de Oviedo CSIC - Museo Nacional de Ciencias Naturales (MNCN) Universidad de Salamanca 2018-01 http://hdl.handle.net/10261/193119 https://doi.org/10.3989/egeol.43122.481 https://doi.org/10.13039/501100006382 https://doi.org/10.13039/100011941 unknown Consejo Superior de Investigaciones Científicas (España) Publisher's version https://doi.org/10.3989/egeol.43122.481 Sí doi:10.3989/egeol.43122.481 issn: 0367-0449 e-issn: 1988-3250 Estudios Geologicos 74(1): e76 (2018) http://hdl.handle.net/10261/193119 http://dx.doi.org/10.13039/501100006382 http://dx.doi.org/10.13039/100011941 open Late Pleistocene Cantabrian Region Paleoecología Paleoclimatología Paleoecology Paleoclimatology Región cantábrica Micromammals Micromamíferos Pleistoceno Superior artículo http://purl.org/coar/resource_type/c_6501 2018 ftcsic https://doi.org/10.3989/egeol.43122.48110.13039/50110000638210.13039/100011941 2024-01-16T10:44:49Z © 2018 CSIC. [EN]In the Late Pleistocene site of El Sidrón cave, with a date of ~ 49,000 ky, known for its numerous fossil remains of Neanderthals, some remains of micromammals were found, whose detailed study is carried out in this work. The determined faunal association is the following: Sorex araneus-Sorex coronatus, Neomys cf. fodiens, Talpa sp., Rhinolophus euryale-Rhinolophus mehelyi, Marmota cf. marmota, Eliomys quercinus, Glis glis, Arvicola terrestris, Chionomys nivalis, Microtus arvalis-Microtus agrestis, Microtus lusitanicus, Microtus oeconomus, Clethrionomys glareolus, Apodemus sylvaticus-Apodemus flavicollis and Oryctolagus cuniculus. These taxa are present in the current fauna of Asturias and Cantabrian Region except for Microtus oeconomus that disappeared from the Iberian Peninsula in historical times and is currently in northernmost Eurasian regions. The fauna of micromammals as a whole seems to indicate a predominantly open space environment, generally of certain moisture meadows and vegetation development at ground level, although there would also be wooded areas of some entity and some watercourse. The presence, although with few remains, of some thermophilic species, and the absence of cold climate indicator species, seem to indicate that the climate during the formation of the fossiliferous deposits would be relatively temperate and humid, probably similar to the current one in the area. [ES]: En el yacimiento del Pleistoceno Superior de la cueva de El Sidrón, con una datación de ~49.000 ka, conocido por sus numerosos restos fósiles de neandertales, se han recuperado restos de micromamíferos cuyo estudio detallado se realiza en este trabajo. La asociación determinada es la siguiente: Sorex araneus–Sorex coronatus, Neomys cf. fodiens, Talpa sp., Rhinolophus euryale-Rhinolophus mehelyi, Marmota cf. marmota, Eliomys quercinus, Glis glis, Arvicola terrestris, Chionomys nivalis, Microtus arvalis-Microtus agrestis, Microtus lusitanicus, Microtus oeconomus, Clethrionomys glareolus, Apodemus ... Article in Journal/Newspaper Microtus arvalis Digital.CSIC (Spanish National Research Council) Cueva ENVELOPE(-62.600,-62.600,-64.150,-64.150) Fósiles ENVELOPE(-56.866,-56.866,-64.300,-64.300) |
institution |
Open Polar |
collection |
Digital.CSIC (Spanish National Research Council) |
op_collection_id |
ftcsic |
language |
unknown |
topic |
Late Pleistocene Cantabrian Region Paleoecología Paleoclimatología Paleoecology Paleoclimatology Región cantábrica Micromammals Micromamíferos Pleistoceno Superior |
spellingShingle |
Late Pleistocene Cantabrian Region Paleoecología Paleoclimatología Paleoecology Paleoclimatology Región cantábrica Micromammals Micromamíferos Pleistoceno Superior Sesé, Carmen Rasilla, Marco de la Duarte Matías, E. Los micromamíferos (Eulipotyphla, Chiroptera, Rodentia y Lagomorpha) del yacimiento del Pleistoceno Superior de la cueva de El Sidrón (Asturias) |
topic_facet |
Late Pleistocene Cantabrian Region Paleoecología Paleoclimatología Paleoecology Paleoclimatology Región cantábrica Micromammals Micromamíferos Pleistoceno Superior |
description |
© 2018 CSIC. [EN]In the Late Pleistocene site of El Sidrón cave, with a date of ~ 49,000 ky, known for its numerous fossil remains of Neanderthals, some remains of micromammals were found, whose detailed study is carried out in this work. The determined faunal association is the following: Sorex araneus-Sorex coronatus, Neomys cf. fodiens, Talpa sp., Rhinolophus euryale-Rhinolophus mehelyi, Marmota cf. marmota, Eliomys quercinus, Glis glis, Arvicola terrestris, Chionomys nivalis, Microtus arvalis-Microtus agrestis, Microtus lusitanicus, Microtus oeconomus, Clethrionomys glareolus, Apodemus sylvaticus-Apodemus flavicollis and Oryctolagus cuniculus. These taxa are present in the current fauna of Asturias and Cantabrian Region except for Microtus oeconomus that disappeared from the Iberian Peninsula in historical times and is currently in northernmost Eurasian regions. The fauna of micromammals as a whole seems to indicate a predominantly open space environment, generally of certain moisture meadows and vegetation development at ground level, although there would also be wooded areas of some entity and some watercourse. The presence, although with few remains, of some thermophilic species, and the absence of cold climate indicator species, seem to indicate that the climate during the formation of the fossiliferous deposits would be relatively temperate and humid, probably similar to the current one in the area. [ES]: En el yacimiento del Pleistoceno Superior de la cueva de El Sidrón, con una datación de ~49.000 ka, conocido por sus numerosos restos fósiles de neandertales, se han recuperado restos de micromamíferos cuyo estudio detallado se realiza en este trabajo. La asociación determinada es la siguiente: Sorex araneus–Sorex coronatus, Neomys cf. fodiens, Talpa sp., Rhinolophus euryale-Rhinolophus mehelyi, Marmota cf. marmota, Eliomys quercinus, Glis glis, Arvicola terrestris, Chionomys nivalis, Microtus arvalis-Microtus agrestis, Microtus lusitanicus, Microtus oeconomus, Clethrionomys glareolus, Apodemus ... |
author2 |
Principado de Asturias Universidad de Oviedo CSIC - Museo Nacional de Ciencias Naturales (MNCN) Universidad de Salamanca |
format |
Article in Journal/Newspaper |
author |
Sesé, Carmen Rasilla, Marco de la Duarte Matías, E. |
author_facet |
Sesé, Carmen Rasilla, Marco de la Duarte Matías, E. |
author_sort |
Sesé, Carmen |
title |
Los micromamíferos (Eulipotyphla, Chiroptera, Rodentia y Lagomorpha) del yacimiento del Pleistoceno Superior de la cueva de El Sidrón (Asturias) |
title_short |
Los micromamíferos (Eulipotyphla, Chiroptera, Rodentia y Lagomorpha) del yacimiento del Pleistoceno Superior de la cueva de El Sidrón (Asturias) |
title_full |
Los micromamíferos (Eulipotyphla, Chiroptera, Rodentia y Lagomorpha) del yacimiento del Pleistoceno Superior de la cueva de El Sidrón (Asturias) |
title_fullStr |
Los micromamíferos (Eulipotyphla, Chiroptera, Rodentia y Lagomorpha) del yacimiento del Pleistoceno Superior de la cueva de El Sidrón (Asturias) |
title_full_unstemmed |
Los micromamíferos (Eulipotyphla, Chiroptera, Rodentia y Lagomorpha) del yacimiento del Pleistoceno Superior de la cueva de El Sidrón (Asturias) |
title_sort |
los micromamíferos (eulipotyphla, chiroptera, rodentia y lagomorpha) del yacimiento del pleistoceno superior de la cueva de el sidrón (asturias) |
publisher |
Consejo Superior de Investigaciones Científicas (España) |
publishDate |
2018 |
url |
http://hdl.handle.net/10261/193119 https://doi.org/10.3989/egeol.43122.481 https://doi.org/10.13039/501100006382 https://doi.org/10.13039/100011941 |
long_lat |
ENVELOPE(-62.600,-62.600,-64.150,-64.150) ENVELOPE(-56.866,-56.866,-64.300,-64.300) |
geographic |
Cueva Fósiles |
geographic_facet |
Cueva Fósiles |
genre |
Microtus arvalis |
genre_facet |
Microtus arvalis |
op_relation |
Publisher's version https://doi.org/10.3989/egeol.43122.481 Sí doi:10.3989/egeol.43122.481 issn: 0367-0449 e-issn: 1988-3250 Estudios Geologicos 74(1): e76 (2018) http://hdl.handle.net/10261/193119 http://dx.doi.org/10.13039/501100006382 http://dx.doi.org/10.13039/100011941 |
op_rights |
open |
op_doi |
https://doi.org/10.3989/egeol.43122.48110.13039/50110000638210.13039/100011941 |
_version_ |
1790603035521581056 |