Pleistocene calcareous macro-and-microfossils from the southernmost tip of South America as environmental proxies during the last interglacial period

Autores
Gordillo, Sandra; Cusminsky, Gabriela Catalina; Bernasconi, Emiliana; Ponce, Juan Federico; Rabassa, Jorge Oscar; Pino, Mario
Año de publicación
2009
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Macro-and-microfossils, including molluscs, cirripeds, echinoids, foraminifers and ostracods area significant component of a Pleistocene marine unit located along the southern coast of the BeagleChannel, on Navarino Island, Chile. This paleontological record represents the richest and most diversemacro-and-micro assemblage recovered from Pleistocene southern South America. In total, 97 taxa wereidentified: 34 molluscs, 57 foraminifers, and 6 ostracods. They comprise a mixture of specimensinhabiting shallow marine environments characterized by strong bottom currents and belonging todifferent local communities associated with the spatial heterogeneity in this basin. The taxonomiccomposition of this paleofauna shows remarkable similarities with present-day fauna, indicating thatboth groups developed under similar environmental conditions. However, slight different climaticconditions at the age of deposition cannot be ruled out. As well, an ecosystem transition towards a trulymarine environment with high number of taxa was recognized. Finally, a Hiatella-cirriped assemblagedeserves special attention since the polymorphic shell of fossil and living Hiatella is used as a paleo-environmental tool. In this regard, the small size of Hiatella in the studied marine unit is best related toits mode of life as a nestler within empty tests of barnacles, which apparently served as microenvi-ronments for this species. Nevertheless, more geochemical data on living and fossil Hiatella shells fromthe Beagle Channel will be necessary to test the suitability of using this species to evaluate paleo-temperatures and other sea water variations during the Quaternary.
Fil: Gordillo, Sandra. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones Paleobiológicas; Argentina
Fil: Cusminsky, Gabriela Catalina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigaciones en Biodiversidad y Medioambiente. Universidad Nacional del Comahue. Centro Regional Universidad Bariloche. Instituto de Investigaciones en Biodiversidad y Medioambiente; Argentina. Universidad Nacional del Comahue. Centro Regional Universitario Bariloche; Argentina
Fil: Bernasconi, Emiliana. Universidad Nacional del Comahue. Centro Regional Universitario Bariloche; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigaciones en Biodiversidad y Medioambiente. Universidad Nacional del Comahue. Centro Regional Universidad Bariloche. Instituto de Investigaciones en Biodiversidad y Medioambiente; Argentina
Fil: Ponce, Juan Federico. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina
Fil: Rabassa, Jorge Oscar. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de la Patagonia "San Juan Bosco"; Argentina
Fil: Pino, Mario. Universidad Austral de Chile; Chile
Materia
Pleistocene
Southernmost South America
Marine Mollusks
Last Interglacial
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/129616

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spelling Pleistocene calcareous macro-and-microfossils from the southernmost tip of South America as environmental proxies during the last interglacial periodGordillo, SandraCusminsky, Gabriela CatalinaBernasconi, EmilianaPonce, Juan FedericoRabassa, Jorge OscarPino, MarioPleistoceneSouthernmost South AmericaMarine MollusksLast Interglacialhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Macro-and-microfossils, including molluscs, cirripeds, echinoids, foraminifers and ostracods area significant component of a Pleistocene marine unit located along the southern coast of the BeagleChannel, on Navarino Island, Chile. This paleontological record represents the richest and most diversemacro-and-micro assemblage recovered from Pleistocene southern South America. In total, 97 taxa wereidentified: 34 molluscs, 57 foraminifers, and 6 ostracods. They comprise a mixture of specimensinhabiting shallow marine environments characterized by strong bottom currents and belonging todifferent local communities associated with the spatial heterogeneity in this basin. The taxonomiccomposition of this paleofauna shows remarkable similarities with present-day fauna, indicating thatboth groups developed under similar environmental conditions. However, slight different climaticconditions at the age of deposition cannot be ruled out. As well, an ecosystem transition towards a trulymarine environment with high number of taxa was recognized. Finally, a Hiatella-cirriped assemblagedeserves special attention since the polymorphic shell of fossil and living Hiatella is used as a paleo-environmental tool. In this regard, the small size of Hiatella in the studied marine unit is best related toits mode of life as a nestler within empty tests of barnacles, which apparently served as microenvi-ronments for this species. Nevertheless, more geochemical data on living and fossil Hiatella shells fromthe Beagle Channel will be necessary to test the suitability of using this species to evaluate paleo-temperatures and other sea water variations during the Quaternary.Fil: Gordillo, Sandra. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones Paleobiológicas; ArgentinaFil: Cusminsky, Gabriela Catalina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigaciones en Biodiversidad y Medioambiente. Universidad Nacional del Comahue. Centro Regional Universidad Bariloche. Instituto de Investigaciones en Biodiversidad y Medioambiente; Argentina. Universidad Nacional del Comahue. Centro Regional Universitario Bariloche; ArgentinaFil: Bernasconi, Emiliana. Universidad Nacional del Comahue. Centro Regional Universitario Bariloche; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigaciones en Biodiversidad y Medioambiente. Universidad Nacional del Comahue. Centro Regional Universidad Bariloche. Instituto de Investigaciones en Biodiversidad y Medioambiente; ArgentinaFil: Ponce, Juan Federico. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; ArgentinaFil: Rabassa, Jorge Oscar. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de la Patagonia "San Juan Bosco"; ArgentinaFil: Pino, Mario. Universidad Austral de Chile; ChilePergamon-Elsevier Science Ltd2009-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/129616Gordillo, Sandra; Cusminsky, Gabriela Catalina; Bernasconi, Emiliana; Ponce, Juan Federico; Rabassa, Jorge Oscar; et al.; Pleistocene calcareous macro-and-microfossils from the southernmost tip of South America as environmental proxies during the last interglacial period; Pergamon-Elsevier Science Ltd; Quaternary International; 221; 12-2009; 159-1741040-6182CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/abs/pii/S1040618209003802info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quaint.2009.10.025info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T09:59:02Zoai:ri.conicet.gov.ar:11336/129616instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-03 09:59:03.115CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Pleistocene calcareous macro-and-microfossils from the southernmost tip of South America as environmental proxies during the last interglacial period
title Pleistocene calcareous macro-and-microfossils from the southernmost tip of South America as environmental proxies during the last interglacial period
spellingShingle Pleistocene calcareous macro-and-microfossils from the southernmost tip of South America as environmental proxies during the last interglacial period
Gordillo, Sandra
Pleistocene
Southernmost South America
Marine Mollusks
Last Interglacial
title_short Pleistocene calcareous macro-and-microfossils from the southernmost tip of South America as environmental proxies during the last interglacial period
title_full Pleistocene calcareous macro-and-microfossils from the southernmost tip of South America as environmental proxies during the last interglacial period
title_fullStr Pleistocene calcareous macro-and-microfossils from the southernmost tip of South America as environmental proxies during the last interglacial period
title_full_unstemmed Pleistocene calcareous macro-and-microfossils from the southernmost tip of South America as environmental proxies during the last interglacial period
title_sort Pleistocene calcareous macro-and-microfossils from the southernmost tip of South America as environmental proxies during the last interglacial period
dc.creator.none.fl_str_mv Gordillo, Sandra
Cusminsky, Gabriela Catalina
Bernasconi, Emiliana
Ponce, Juan Federico
Rabassa, Jorge Oscar
Pino, Mario
author Gordillo, Sandra
author_facet Gordillo, Sandra
Cusminsky, Gabriela Catalina
Bernasconi, Emiliana
Ponce, Juan Federico
Rabassa, Jorge Oscar
Pino, Mario
author_role author
author2 Cusminsky, Gabriela Catalina
Bernasconi, Emiliana
Ponce, Juan Federico
Rabassa, Jorge Oscar
Pino, Mario
author2_role author
author
author
author
author
dc.subject.none.fl_str_mv Pleistocene
Southernmost South America
Marine Mollusks
Last Interglacial
topic Pleistocene
Southernmost South America
Marine Mollusks
Last Interglacial
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Macro-and-microfossils, including molluscs, cirripeds, echinoids, foraminifers and ostracods area significant component of a Pleistocene marine unit located along the southern coast of the BeagleChannel, on Navarino Island, Chile. This paleontological record represents the richest and most diversemacro-and-micro assemblage recovered from Pleistocene southern South America. In total, 97 taxa wereidentified: 34 molluscs, 57 foraminifers, and 6 ostracods. They comprise a mixture of specimensinhabiting shallow marine environments characterized by strong bottom currents and belonging todifferent local communities associated with the spatial heterogeneity in this basin. The taxonomiccomposition of this paleofauna shows remarkable similarities with present-day fauna, indicating thatboth groups developed under similar environmental conditions. However, slight different climaticconditions at the age of deposition cannot be ruled out. As well, an ecosystem transition towards a trulymarine environment with high number of taxa was recognized. Finally, a Hiatella-cirriped assemblagedeserves special attention since the polymorphic shell of fossil and living Hiatella is used as a paleo-environmental tool. In this regard, the small size of Hiatella in the studied marine unit is best related toits mode of life as a nestler within empty tests of barnacles, which apparently served as microenvi-ronments for this species. Nevertheless, more geochemical data on living and fossil Hiatella shells fromthe Beagle Channel will be necessary to test the suitability of using this species to evaluate paleo-temperatures and other sea water variations during the Quaternary.
Fil: Gordillo, Sandra. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones Paleobiológicas; Argentina
Fil: Cusminsky, Gabriela Catalina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigaciones en Biodiversidad y Medioambiente. Universidad Nacional del Comahue. Centro Regional Universidad Bariloche. Instituto de Investigaciones en Biodiversidad y Medioambiente; Argentina. Universidad Nacional del Comahue. Centro Regional Universitario Bariloche; Argentina
Fil: Bernasconi, Emiliana. Universidad Nacional del Comahue. Centro Regional Universitario Bariloche; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigaciones en Biodiversidad y Medioambiente. Universidad Nacional del Comahue. Centro Regional Universidad Bariloche. Instituto de Investigaciones en Biodiversidad y Medioambiente; Argentina
Fil: Ponce, Juan Federico. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina
Fil: Rabassa, Jorge Oscar. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de la Patagonia "San Juan Bosco"; Argentina
Fil: Pino, Mario. Universidad Austral de Chile; Chile
description Macro-and-microfossils, including molluscs, cirripeds, echinoids, foraminifers and ostracods area significant component of a Pleistocene marine unit located along the southern coast of the BeagleChannel, on Navarino Island, Chile. This paleontological record represents the richest and most diversemacro-and-micro assemblage recovered from Pleistocene southern South America. In total, 97 taxa wereidentified: 34 molluscs, 57 foraminifers, and 6 ostracods. They comprise a mixture of specimensinhabiting shallow marine environments characterized by strong bottom currents and belonging todifferent local communities associated with the spatial heterogeneity in this basin. The taxonomiccomposition of this paleofauna shows remarkable similarities with present-day fauna, indicating thatboth groups developed under similar environmental conditions. However, slight different climaticconditions at the age of deposition cannot be ruled out. As well, an ecosystem transition towards a trulymarine environment with high number of taxa was recognized. Finally, a Hiatella-cirriped assemblagedeserves special attention since the polymorphic shell of fossil and living Hiatella is used as a paleo-environmental tool. In this regard, the small size of Hiatella in the studied marine unit is best related toits mode of life as a nestler within empty tests of barnacles, which apparently served as microenvi-ronments for this species. Nevertheless, more geochemical data on living and fossil Hiatella shells fromthe Beagle Channel will be necessary to test the suitability of using this species to evaluate paleo-temperatures and other sea water variations during the Quaternary.
publishDate 2009
dc.date.none.fl_str_mv 2009-12
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/129616
Gordillo, Sandra; Cusminsky, Gabriela Catalina; Bernasconi, Emiliana; Ponce, Juan Federico; Rabassa, Jorge Oscar; et al.; Pleistocene calcareous macro-and-microfossils from the southernmost tip of South America as environmental proxies during the last interglacial period; Pergamon-Elsevier Science Ltd; Quaternary International; 221; 12-2009; 159-174
1040-6182
CONICET Digital
CONICET
url http://hdl.handle.net/11336/129616
identifier_str_mv Gordillo, Sandra; Cusminsky, Gabriela Catalina; Bernasconi, Emiliana; Ponce, Juan Federico; Rabassa, Jorge Oscar; et al.; Pleistocene calcareous macro-and-microfossils from the southernmost tip of South America as environmental proxies during the last interglacial period; Pergamon-Elsevier Science Ltd; Quaternary International; 221; 12-2009; 159-174
1040-6182
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
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info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quaint.2009.10.025
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dc.publisher.none.fl_str_mv Pergamon-Elsevier Science Ltd
publisher.none.fl_str_mv Pergamon-Elsevier Science Ltd
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