Global deglaciation and the re-appearance of microbial matground-dominated ecosystems in the late Paleozoic of Gondwana
- Autores
- Buatois, Luis Alberto; Netto, R. G.; Mangano, Maria Gabriela; Carmona, Noelia Beatriz
- Año de publicación
- 2013
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The extensive matgrounds in Carboniferous-Permian open-marine deposits of western Argentina constitute an anachronistic facies, because with the onset of penetrative bioturbation during the early Paleozoic microbial mats essentially disappeared from these settings. Abundant microbially induced sedimentary structures in the Argentinean deposits are coincident with the disappearance of trace and body fossils in the succession and with a landward facies shift indicative of transgressive conditions. Deposits of the Late Carboniferous–Early Permian glacial event are well developed in adjacent basins in eastern Argentina, Brazil, South Africa and Antarctica, but do not occur in the western Andean basins of Argentina. However, the deglaciation phase is indirectly recorded in the studied region by a rapid rise in sea level referred to as the Stephanian-Asselian transgression. We suggest that an unusual release of meltwater during the final deglaciation episode of the Gondwana Ice Age may have dramatically freshened peri-Gondwanan seas, impacting negatively on coastal and shallow-marine benthic faunas. Suppression of bioturbation was therefore conducive to a brief re-appearance of matground-dominated ecosystems, reminiscent of those in the precambrian. Bioturbation is essential for ecosystem performance and plays a major role in ocean and sediment geochemistry. Accordingly, the decimation of the mixed layer during deglaciation in the Gondwana basins may have altered ecosystem functioning and geochemical cycling.
Fil: Buatois, Luis Alberto. University Of Saskatchewan; Canadá. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Netto, R. G.. Universidade do Vale do Rio dos Sinos; Brasil
Fil: Mangano, Maria Gabriela. University Of Saskatchewan; Canadá. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Carmona, Noelia Beatriz. University Of Saskatchewan; Canadá. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina - Materia
-
Microbial Mats
Gondwana
Paleozoic
Deglaciation - 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:11336/17574
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Global deglaciation and the re-appearance of microbial matground-dominated ecosystems in the late Paleozoic of GondwanaBuatois, Luis AlbertoNetto, R. G.Mangano, Maria GabrielaCarmona, Noelia BeatrizMicrobial MatsGondwanaPaleozoicDeglaciationhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The extensive matgrounds in Carboniferous-Permian open-marine deposits of western Argentina constitute an anachronistic facies, because with the onset of penetrative bioturbation during the early Paleozoic microbial mats essentially disappeared from these settings. Abundant microbially induced sedimentary structures in the Argentinean deposits are coincident with the disappearance of trace and body fossils in the succession and with a landward facies shift indicative of transgressive conditions. Deposits of the Late Carboniferous–Early Permian glacial event are well developed in adjacent basins in eastern Argentina, Brazil, South Africa and Antarctica, but do not occur in the western Andean basins of Argentina. However, the deglaciation phase is indirectly recorded in the studied region by a rapid rise in sea level referred to as the Stephanian-Asselian transgression. We suggest that an unusual release of meltwater during the final deglaciation episode of the Gondwana Ice Age may have dramatically freshened peri-Gondwanan seas, impacting negatively on coastal and shallow-marine benthic faunas. Suppression of bioturbation was therefore conducive to a brief re-appearance of matground-dominated ecosystems, reminiscent of those in the precambrian. Bioturbation is essential for ecosystem performance and plays a major role in ocean and sediment geochemistry. Accordingly, the decimation of the mixed layer during deglaciation in the Gondwana basins may have altered ecosystem functioning and geochemical cycling.Fil: Buatois, Luis Alberto. University Of Saskatchewan; Canadá. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Netto, R. G.. Universidade do Vale do Rio dos Sinos; BrasilFil: Mangano, Maria Gabriela. University Of Saskatchewan; Canadá. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Carmona, Noelia Beatriz. University Of Saskatchewan; Canadá. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaWiley2013-07info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/17574Buatois, Luis Alberto; Netto, R. G.; Mangano, Maria Gabriela; Carmona, Noelia Beatriz; Global deglaciation and the re-appearance of microbial matground-dominated ecosystems in the late Paleozoic of Gondwana; Wiley; Geobiology; 11; 4; 7-2013; 307-3171472-4677enginfo:eu-repo/semantics/altIdentifier/doi/10.1111/gbi.12038info:eu-repo/semantics/altIdentifier/url/http://onlinelibrary.wiley.com/doi/10.1111/gbi.12038/abstractinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-10T13:21:01Zoai:ri.conicet.gov.ar:11336/17574instacron: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:34982025-09-10 13:21:01.313CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Global deglaciation and the re-appearance of microbial matground-dominated ecosystems in the late Paleozoic of Gondwana |
title |
Global deglaciation and the re-appearance of microbial matground-dominated ecosystems in the late Paleozoic of Gondwana |
spellingShingle |
Global deglaciation and the re-appearance of microbial matground-dominated ecosystems in the late Paleozoic of Gondwana Buatois, Luis Alberto Microbial Mats Gondwana Paleozoic Deglaciation |
title_short |
Global deglaciation and the re-appearance of microbial matground-dominated ecosystems in the late Paleozoic of Gondwana |
title_full |
Global deglaciation and the re-appearance of microbial matground-dominated ecosystems in the late Paleozoic of Gondwana |
title_fullStr |
Global deglaciation and the re-appearance of microbial matground-dominated ecosystems in the late Paleozoic of Gondwana |
title_full_unstemmed |
Global deglaciation and the re-appearance of microbial matground-dominated ecosystems in the late Paleozoic of Gondwana |
title_sort |
Global deglaciation and the re-appearance of microbial matground-dominated ecosystems in the late Paleozoic of Gondwana |
dc.creator.none.fl_str_mv |
Buatois, Luis Alberto Netto, R. G. Mangano, Maria Gabriela Carmona, Noelia Beatriz |
author |
Buatois, Luis Alberto |
author_facet |
Buatois, Luis Alberto Netto, R. G. Mangano, Maria Gabriela Carmona, Noelia Beatriz |
author_role |
author |
author2 |
Netto, R. G. Mangano, Maria Gabriela Carmona, Noelia Beatriz |
author2_role |
author author author |
dc.subject.none.fl_str_mv |
Microbial Mats Gondwana Paleozoic Deglaciation |
topic |
Microbial Mats Gondwana Paleozoic Deglaciation |
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 extensive matgrounds in Carboniferous-Permian open-marine deposits of western Argentina constitute an anachronistic facies, because with the onset of penetrative bioturbation during the early Paleozoic microbial mats essentially disappeared from these settings. Abundant microbially induced sedimentary structures in the Argentinean deposits are coincident with the disappearance of trace and body fossils in the succession and with a landward facies shift indicative of transgressive conditions. Deposits of the Late Carboniferous–Early Permian glacial event are well developed in adjacent basins in eastern Argentina, Brazil, South Africa and Antarctica, but do not occur in the western Andean basins of Argentina. However, the deglaciation phase is indirectly recorded in the studied region by a rapid rise in sea level referred to as the Stephanian-Asselian transgression. We suggest that an unusual release of meltwater during the final deglaciation episode of the Gondwana Ice Age may have dramatically freshened peri-Gondwanan seas, impacting negatively on coastal and shallow-marine benthic faunas. Suppression of bioturbation was therefore conducive to a brief re-appearance of matground-dominated ecosystems, reminiscent of those in the precambrian. Bioturbation is essential for ecosystem performance and plays a major role in ocean and sediment geochemistry. Accordingly, the decimation of the mixed layer during deglaciation in the Gondwana basins may have altered ecosystem functioning and geochemical cycling. Fil: Buatois, Luis Alberto. University Of Saskatchewan; Canadá. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Netto, R. G.. Universidade do Vale do Rio dos Sinos; Brasil Fil: Mangano, Maria Gabriela. University Of Saskatchewan; Canadá. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Carmona, Noelia Beatriz. University Of Saskatchewan; Canadá. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina |
description |
The extensive matgrounds in Carboniferous-Permian open-marine deposits of western Argentina constitute an anachronistic facies, because with the onset of penetrative bioturbation during the early Paleozoic microbial mats essentially disappeared from these settings. Abundant microbially induced sedimentary structures in the Argentinean deposits are coincident with the disappearance of trace and body fossils in the succession and with a landward facies shift indicative of transgressive conditions. Deposits of the Late Carboniferous–Early Permian glacial event are well developed in adjacent basins in eastern Argentina, Brazil, South Africa and Antarctica, but do not occur in the western Andean basins of Argentina. However, the deglaciation phase is indirectly recorded in the studied region by a rapid rise in sea level referred to as the Stephanian-Asselian transgression. We suggest that an unusual release of meltwater during the final deglaciation episode of the Gondwana Ice Age may have dramatically freshened peri-Gondwanan seas, impacting negatively on coastal and shallow-marine benthic faunas. Suppression of bioturbation was therefore conducive to a brief re-appearance of matground-dominated ecosystems, reminiscent of those in the precambrian. Bioturbation is essential for ecosystem performance and plays a major role in ocean and sediment geochemistry. Accordingly, the decimation of the mixed layer during deglaciation in the Gondwana basins may have altered ecosystem functioning and geochemical cycling. |
publishDate |
2013 |
dc.date.none.fl_str_mv |
2013-07 |
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/11336/17574 Buatois, Luis Alberto; Netto, R. G.; Mangano, Maria Gabriela; Carmona, Noelia Beatriz; Global deglaciation and the re-appearance of microbial matground-dominated ecosystems in the late Paleozoic of Gondwana; Wiley; Geobiology; 11; 4; 7-2013; 307-317 1472-4677 |
url |
http://hdl.handle.net/11336/17574 |
identifier_str_mv |
Buatois, Luis Alberto; Netto, R. G.; Mangano, Maria Gabriela; Carmona, Noelia Beatriz; Global deglaciation and the re-appearance of microbial matground-dominated ecosystems in the late Paleozoic of Gondwana; Wiley; Geobiology; 11; 4; 7-2013; 307-317 1472-4677 |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/doi/10.1111/gbi.12038 info:eu-repo/semantics/altIdentifier/url/http://onlinelibrary.wiley.com/doi/10.1111/gbi.12038/abstract |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
dc.format.none.fl_str_mv |
application/pdf application/pdf |
dc.publisher.none.fl_str_mv |
Wiley |
publisher.none.fl_str_mv |
Wiley |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
reponame_str |
CONICET Digital (CONICET) |
collection |
CONICET Digital (CONICET) |
instname_str |
Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.name.fl_str_mv |
CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.mail.fl_str_mv |
dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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1842981151696748544 |
score |
12.48226 |