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
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/17574

id CONICETDig_f64d0b824e4dc17bbdc1718c854e49f3
oai_identifier_str oai:ri.conicet.gov.ar:11336/17574
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling 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
_version_ 1842981151696748544
score 12.48226