Glaciation During the Late Paleozoic Ice Age

Autores: Isbell, John L.; Fedorchuk, N. D.; Pauls, Kathryn N.; Griffis, N. P.; Ives, L. R. W.; Moxness, Levi D.; Survis, S. R.; Vesely, F. F.; Montañez, I. P.; Limarino, Carlos Oscar; Iannuzzi, R.; Biakov, A. S.; da Rosa, E. L. M.; Mundil, R.; Taboada, Arturo Cesar; Pagani, María Alejandra; Ciccioli, Patricia Lucia; Schencman, Laura Jazmín; Alonso Muruaga, Pablo Joaquin; Davydov, V. I.; Vedernikov, I. L.; McNall, N. B.
Año de publicación: 2018
Idioma: inglés
Tipo de recurso: documento de conferencia
Estado: versión publicada
Descripción: The Late Paleozoic Ice Age (LPIA) was one of Earth’s most extreme climatic events where sea level and biotic restructuring were driven by linked oscillations in the climate system. Despite an evolving understanding of the ice age, the size, distribution, paleogeography, timing, depositional settings, and possible bipolarity of the glaciation remains unresolved. However, new and refined radioisotopic age dates are revising the timing and extent of individual stages of the ice age. Recent studies suggest numerous, ice centers fluctuated diachronously as glaciation shifted across Gondwana. The LPIA began in the Famennian in northern South America and Africa and ended in eastern Australia during the Wuchiapingian. Although glaciation was widespread, numerous ice-free areas occurred adjacent to major glacial centers. Deglaciation was also diachronous beginning in the Bashkirian in western Argentina, shifting to the Paraná Basin by the end of the Pennsylvanian, with deglaciation of the South Polar Region occurring during the late Early Permian. Deglaciation culminated in eastern Australia with the disappearance of high, mid-latitude, alpine glaciers during the Wuchiapingian at a time when Polar Gondwana was ice-free. Recent work on diamictites in northeastern Russia indicates that these strata were not glacigenic but instead were deposited as volcanic debris flows and slides/slumps associated with concurrent activity in the Okhotsk-Taigonos volcanic arc. Therefore, bipolar glaciation cannot be confirmed. Although fluctuations in greenhouse gases were a major driver of climate, paleogeography, tectonism, and other minor drivers also played a role in the nucleation and disappearance of LPIA glaciers.
Fil: Isbell, John L.. University of Wisconsin; Estados Unidos
Fil: Fedorchuk, N. D.. University of Wisconsin; Estados Unidos
Fil: Pauls, Kathryn N.. University of Wisconsin; Estados Unidos
Fil: Griffis, N. P.. University of California at Davis; Estados Unidos
Fil: Ives, L. R. W.. University of Wisconsin; Estados Unidos
Fil: Moxness, Levi D.. University of Wisconsin; Estados Unidos
Fil: Survis, S. R.. University of Wisconsin; Estados Unidos
Fil: Vesely, F. F.. Universidade Federal do Paraná; Brasil
Fil: Montañez, I. P.. University of California at Davis; Estados Unidos
Fil: Limarino, Carlos Oscar. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina
Fil: Iannuzzi, R.. Universidade Federal do Rio Grande do Sul; Brasil
Fil: Biakov, A. S.. Academia de Ciencias de Rusia; Rusia
Fil: da Rosa, E. L. M.. Universidade Federal do Paraná; Brasil
Fil: Mundil, R.. Berkeley Geochronology Center; Estados Unidos
Fil: Taboada, Arturo Cesar. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Centro de Investigación Esquel de Montaña y Estepa Patagónica. Universidad Nacional de la Patagonia "San Juan Bosco". Centro de Investigación Esquel de Montaña y Estepa Patagónica; Argentina
Fil: Pagani, María Alejandra. Museo Paleontológico Egidio Feruglio; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Centro Nacional Patagónico; Argentina
Fil: Ciccioli, Patricia Lucia. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina
Fil: Schencman, Laura Jazmín. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina
Fil: Alonso Muruaga, Pablo Joaquin. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina
Fil: Davydov, V. I.. Boise State University; Estados Unidos
Fil: Vedernikov, I. L.. Academia de Ciencias de Rusia; Rusia
Fil: McNall, N. B.. University of Wisconsin; Estados Unidos
VII Simposio Argentino del Paleozoico Superior
Esquel
Argentina
Centro de investigación Esquel de montaña y estepa patagónica
Materia: GLACIATION
PALEOZOIC
Nivel de accesibilidad: acceso abierto
Condiciones de uso: https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
Institución: Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador: oai:ri.conicet.gov.ar:11336/155900

Acceder

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spelling	Glaciation During the Late Paleozoic Ice AgeIsbell, John L.Fedorchuk, N. D.Pauls, Kathryn N.Griffis, N. P.Ives, L. R. W.Moxness, Levi D.Survis, S. R.Vesely, F. F.Montañez, I. P.Limarino, Carlos OscarIannuzzi, R.Biakov, A. S.da Rosa, E. L. M.Mundil, R.Taboada, Arturo CesarPagani, María AlejandraCiccioli, Patricia LuciaSchencman, Laura JazmínAlonso Muruaga, Pablo JoaquinDavydov, V. I.Vedernikov, I. L.McNall, N. B.GLACIATIONPALEOZOIChttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The Late Paleozoic Ice Age (LPIA) was one of Earth’s most extreme climatic events where sea level and biotic restructuring were driven by linked oscillations in the climate system. Despite an evolving understanding of the ice age, the size, distribution, paleogeography, timing, depositional settings, and possible bipolarity of the glaciation remains unresolved. However, new and refined radioisotopic age dates are revising the timing and extent of individual stages of the ice age. Recent studies suggest numerous, ice centers fluctuated diachronously as glaciation shifted across Gondwana. The LPIA began in the Famennian in northern South America and Africa and ended in eastern Australia during the Wuchiapingian. Although glaciation was widespread, numerous ice-free areas occurred adjacent to major glacial centers. Deglaciation was also diachronous beginning in the Bashkirian in western Argentina, shifting to the Paraná Basin by the end of the Pennsylvanian, with deglaciation of the South Polar Region occurring during the late Early Permian. Deglaciation culminated in eastern Australia with the disappearance of high, mid-latitude, alpine glaciers during the Wuchiapingian at a time when Polar Gondwana was ice-free. Recent work on diamictites in northeastern Russia indicates that these strata were not glacigenic but instead were deposited as volcanic debris flows and slides/slumps associated with concurrent activity in the Okhotsk-Taigonos volcanic arc. Therefore, bipolar glaciation cannot be confirmed. Although fluctuations in greenhouse gases were a major driver of climate, paleogeography, tectonism, and other minor drivers also played a role in the nucleation and disappearance of LPIA glaciers.Fil: Isbell, John L.. University of Wisconsin; Estados UnidosFil: Fedorchuk, N. D.. University of Wisconsin; Estados UnidosFil: Pauls, Kathryn N.. University of Wisconsin; Estados UnidosFil: Griffis, N. P.. University of California at Davis; Estados UnidosFil: Ives, L. R. W.. University of Wisconsin; Estados UnidosFil: Moxness, Levi D.. University of Wisconsin; Estados UnidosFil: Survis, S. R.. University of Wisconsin; Estados UnidosFil: Vesely, F. F.. Universidade Federal do Paraná; BrasilFil: Montañez, I. P.. University of California at Davis; Estados UnidosFil: Limarino, Carlos Oscar. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; ArgentinaFil: Iannuzzi, R.. Universidade Federal do Rio Grande do Sul; BrasilFil: Biakov, A. S.. Academia de Ciencias de Rusia; RusiaFil: da Rosa, E. L. M.. Universidade Federal do Paraná; BrasilFil: Mundil, R.. Berkeley Geochronology Center; Estados UnidosFil: Taboada, Arturo Cesar. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Centro de Investigación Esquel de Montaña y Estepa Patagónica. Universidad Nacional de la Patagonia "San Juan Bosco". Centro de Investigación Esquel de Montaña y Estepa Patagónica; ArgentinaFil: Pagani, María Alejandra. Museo Paleontológico Egidio Feruglio; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Centro Nacional Patagónico; ArgentinaFil: Ciccioli, Patricia Lucia. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; ArgentinaFil: Schencman, Laura Jazmín. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; ArgentinaFil: Alonso Muruaga, Pablo Joaquin. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; ArgentinaFil: Davydov, V. I.. Boise State University; Estados UnidosFil: Vedernikov, I. L.. Academia de Ciencias de Rusia; RusiaFil: McNall, N. B.. University of Wisconsin; Estados UnidosVII Simposio Argentino del Paleozoico SuperiorEsquelArgentinaCentro de investigación Esquel de montaña y estepa patagónicaUniversidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo2018info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjectSimposioJournalhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfapplication/pdfapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/155900Glaciation During the Late Paleozoic Ice Age; VII Simposio Argentino del Paleozoico Superior; Esquel; Argentina; 2018; 5R-5R2545-63772545-6369CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://publicaciones.fcnym.unlp.edu.ar/rmlp/article/view/2317Nacionalinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:42:06Zoai:ri.conicet.gov.ar:11336/155900instacron: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:34982025-09-29 10:42:06.363CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv	Glaciation During the Late Paleozoic Ice Age
title	Glaciation During the Late Paleozoic Ice Age
spellingShingle	Glaciation During the Late Paleozoic Ice Age Isbell, John L. GLACIATION PALEOZOIC
title_short	Glaciation During the Late Paleozoic Ice Age
title_full	Glaciation During the Late Paleozoic Ice Age
title_fullStr	Glaciation During the Late Paleozoic Ice Age
title_full_unstemmed	Glaciation During the Late Paleozoic Ice Age
title_sort	Glaciation During the Late Paleozoic Ice Age
dc.creator.none.fl_str_mv	Isbell, John L. Fedorchuk, N. D. Pauls, Kathryn N. Griffis, N. P. Ives, L. R. W. Moxness, Levi D. Survis, S. R. Vesely, F. F. Montañez, I. P. Limarino, Carlos Oscar Iannuzzi, R. Biakov, A. S. da Rosa, E. L. M. Mundil, R. Taboada, Arturo Cesar Pagani, María Alejandra Ciccioli, Patricia Lucia Schencman, Laura Jazmín Alonso Muruaga, Pablo Joaquin Davydov, V. I. Vedernikov, I. L. McNall, N. B.
author	Isbell, John L.
author_facet	Isbell, John L. Fedorchuk, N. D. Pauls, Kathryn N. Griffis, N. P. Ives, L. R. W. Moxness, Levi D. Survis, S. R. Vesely, F. F. Montañez, I. P. Limarino, Carlos Oscar Iannuzzi, R. Biakov, A. S. da Rosa, E. L. M. Mundil, R. Taboada, Arturo Cesar Pagani, María Alejandra Ciccioli, Patricia Lucia Schencman, Laura Jazmín Alonso Muruaga, Pablo Joaquin Davydov, V. I. Vedernikov, I. L. McNall, N. B.
author_role	author
author2	Fedorchuk, N. D. Pauls, Kathryn N. Griffis, N. P. Ives, L. R. W. Moxness, Levi D. Survis, S. R. Vesely, F. F. Montañez, I. P. Limarino, Carlos Oscar Iannuzzi, R. Biakov, A. S. da Rosa, E. L. M. Mundil, R. Taboada, Arturo Cesar Pagani, María Alejandra Ciccioli, Patricia Lucia Schencman, Laura Jazmín Alonso Muruaga, Pablo Joaquin Davydov, V. I. Vedernikov, I. L. McNall, N. B.
author2_role	author author author author author author author author author author author author author author author author author author author author author
dc.subject.none.fl_str_mv	GLACIATION PALEOZOIC
topic	GLACIATION PALEOZOIC
purl_subject.fl_str_mv	https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv	The Late Paleozoic Ice Age (LPIA) was one of Earth’s most extreme climatic events where sea level and biotic restructuring were driven by linked oscillations in the climate system. Despite an evolving understanding of the ice age, the size, distribution, paleogeography, timing, depositional settings, and possible bipolarity of the glaciation remains unresolved. However, new and refined radioisotopic age dates are revising the timing and extent of individual stages of the ice age. Recent studies suggest numerous, ice centers fluctuated diachronously as glaciation shifted across Gondwana. The LPIA began in the Famennian in northern South America and Africa and ended in eastern Australia during the Wuchiapingian. Although glaciation was widespread, numerous ice-free areas occurred adjacent to major glacial centers. Deglaciation was also diachronous beginning in the Bashkirian in western Argentina, shifting to the Paraná Basin by the end of the Pennsylvanian, with deglaciation of the South Polar Region occurring during the late Early Permian. Deglaciation culminated in eastern Australia with the disappearance of high, mid-latitude, alpine glaciers during the Wuchiapingian at a time when Polar Gondwana was ice-free. Recent work on diamictites in northeastern Russia indicates that these strata were not glacigenic but instead were deposited as volcanic debris flows and slides/slumps associated with concurrent activity in the Okhotsk-Taigonos volcanic arc. Therefore, bipolar glaciation cannot be confirmed. Although fluctuations in greenhouse gases were a major driver of climate, paleogeography, tectonism, and other minor drivers also played a role in the nucleation and disappearance of LPIA glaciers. Fil: Isbell, John L.. University of Wisconsin; Estados Unidos Fil: Fedorchuk, N. D.. University of Wisconsin; Estados Unidos Fil: Pauls, Kathryn N.. University of Wisconsin; Estados Unidos Fil: Griffis, N. P.. University of California at Davis; Estados Unidos Fil: Ives, L. R. W.. University of Wisconsin; Estados Unidos Fil: Moxness, Levi D.. University of Wisconsin; Estados Unidos Fil: Survis, S. R.. University of Wisconsin; Estados Unidos Fil: Vesely, F. F.. Universidade Federal do Paraná; Brasil Fil: Montañez, I. P.. University of California at Davis; Estados Unidos Fil: Limarino, Carlos Oscar. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina Fil: Iannuzzi, R.. Universidade Federal do Rio Grande do Sul; Brasil Fil: Biakov, A. S.. Academia de Ciencias de Rusia; Rusia Fil: da Rosa, E. L. M.. Universidade Federal do Paraná; Brasil Fil: Mundil, R.. Berkeley Geochronology Center; Estados Unidos Fil: Taboada, Arturo Cesar. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Centro de Investigación Esquel de Montaña y Estepa Patagónica. Universidad Nacional de la Patagonia "San Juan Bosco". Centro de Investigación Esquel de Montaña y Estepa Patagónica; Argentina Fil: Pagani, María Alejandra. Museo Paleontológico Egidio Feruglio; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Centro Nacional Patagónico; Argentina Fil: Ciccioli, Patricia Lucia. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina Fil: Schencman, Laura Jazmín. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina Fil: Alonso Muruaga, Pablo Joaquin. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina Fil: Davydov, V. I.. Boise State University; Estados Unidos Fil: Vedernikov, I. L.. Academia de Ciencias de Rusia; Rusia Fil: McNall, N. B.. University of Wisconsin; Estados Unidos VII Simposio Argentino del Paleozoico Superior Esquel Argentina Centro de investigación Esquel de montaña y estepa patagónica
description	The Late Paleozoic Ice Age (LPIA) was one of Earth’s most extreme climatic events where sea level and biotic restructuring were driven by linked oscillations in the climate system. Despite an evolving understanding of the ice age, the size, distribution, paleogeography, timing, depositional settings, and possible bipolarity of the glaciation remains unresolved. However, new and refined radioisotopic age dates are revising the timing and extent of individual stages of the ice age. Recent studies suggest numerous, ice centers fluctuated diachronously as glaciation shifted across Gondwana. The LPIA began in the Famennian in northern South America and Africa and ended in eastern Australia during the Wuchiapingian. Although glaciation was widespread, numerous ice-free areas occurred adjacent to major glacial centers. Deglaciation was also diachronous beginning in the Bashkirian in western Argentina, shifting to the Paraná Basin by the end of the Pennsylvanian, with deglaciation of the South Polar Region occurring during the late Early Permian. Deglaciation culminated in eastern Australia with the disappearance of high, mid-latitude, alpine glaciers during the Wuchiapingian at a time when Polar Gondwana was ice-free. Recent work on diamictites in northeastern Russia indicates that these strata were not glacigenic but instead were deposited as volcanic debris flows and slides/slumps associated with concurrent activity in the Okhotsk-Taigonos volcanic arc. Therefore, bipolar glaciation cannot be confirmed. Although fluctuations in greenhouse gases were a major driver of climate, paleogeography, tectonism, and other minor drivers also played a role in the nucleation and disappearance of LPIA glaciers.
publishDate	2018
dc.date.none.fl_str_mv	2018
dc.type.none.fl_str_mv	info:eu-repo/semantics/publishedVersion info:eu-repo/semantics/conferenceObject Simposio Journal http://purl.org/coar/resource_type/c_5794 info:ar-repo/semantics/documentoDeConferencia
status_str	publishedVersion
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dc.identifier.none.fl_str_mv	http://hdl.handle.net/11336/155900 Glaciation During the Late Paleozoic Ice Age; VII Simposio Argentino del Paleozoico Superior; Esquel; Argentina; 2018; 5R-5R 2545-6377 2545-6369 CONICET Digital CONICET
url	http://hdl.handle.net/11336/155900
identifier_str_mv	Glaciation During the Late Paleozoic Ice Age; VII Simposio Argentino del Paleozoico Superior; Esquel; Argentina; 2018; 5R-5R 2545-6377 2545-6369 CONICET Digital CONICET
dc.language.none.fl_str_mv	eng
language	eng
dc.relation.none.fl_str_mv	info:eu-repo/semantics/altIdentifier/url/https://publicaciones.fcnym.unlp.edu.ar/rmlp/article/view/2317
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dc.publisher.none.fl_str_mv	Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo
publisher.none.fl_str_mv	Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo
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Glaciation During the Late Paleozoic Ice Age

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