Trilobites in early Cambrian tidal flats and the landward expansion of the Cambrian explosion

Autores
Mángano, M. Gabriela; Buatois, Luis A.; Astini, Ricardo Alfredo; Rindsberg, Andrew K.
Año de publicación
2014
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The timing of the early invasion of the continents, the routes to the land, and the environmental breadth of the Cambrian explosion are important topics because they are at the core of our understanding of early evolutionary breakthroughs. Illuminating some aspects of these problems are trilobite trace fossils in tidal-flat deposits from the lower Cambrian Rome Formation in the southern Appalachian Mountains of Tennessee (USA). Morphologic details and size range of the trace fossils suggest production by olenellid trilobites, which occur as body fossils in the same unit. The occurrence of this ichnofauna, together with physical structures indicative of periodic subaerial exposure (desiccation cracks) and deposition within the intertidal zone (flat-topped ripples), shows that trilobites forayed into the upper intertidal zone during the Cambrian. Our finding supports the migration of subtidal organisms into marginal-marine, intertidal settings at the dawn of the Phanerozoic, suggesting that trilobites contributed to the establishment of the intertidal ecosystem during the Cambrian. The sequence of events involved in the colonization of early Paleozoic tidal flats is consistent with the idea that most terrestrial taxa originated from marine rather than freshwater ancestors, and that direct routes to the land from marginal-marine ecosystems were involved in the colonization of continental environments early in the Phanerozoic.
Fil: Mángano, M. Gabriela. University of Saskatchewan; Canadá
Fil: Buatois, Luis A.. University of Saskatchewan; Canadá
Fil: Astini, Ricardo Alfredo. 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
Fil: Rindsberg, Andrew K.. University of West Alabama; Estados Unidos
Materia
Cambrian explosion
Trilobite trace fossils
Rome Formation
Appalachians
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:11336/133792

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spelling Trilobites in early Cambrian tidal flats and the landward expansion of the Cambrian explosionMángano, M. GabrielaBuatois, Luis A.Astini, Ricardo AlfredoRindsberg, Andrew K.Cambrian explosionTrilobite trace fossilsRome FormationAppalachianshttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The timing of the early invasion of the continents, the routes to the land, and the environmental breadth of the Cambrian explosion are important topics because they are at the core of our understanding of early evolutionary breakthroughs. Illuminating some aspects of these problems are trilobite trace fossils in tidal-flat deposits from the lower Cambrian Rome Formation in the southern Appalachian Mountains of Tennessee (USA). Morphologic details and size range of the trace fossils suggest production by olenellid trilobites, which occur as body fossils in the same unit. The occurrence of this ichnofauna, together with physical structures indicative of periodic subaerial exposure (desiccation cracks) and deposition within the intertidal zone (flat-topped ripples), shows that trilobites forayed into the upper intertidal zone during the Cambrian. Our finding supports the migration of subtidal organisms into marginal-marine, intertidal settings at the dawn of the Phanerozoic, suggesting that trilobites contributed to the establishment of the intertidal ecosystem during the Cambrian. The sequence of events involved in the colonization of early Paleozoic tidal flats is consistent with the idea that most terrestrial taxa originated from marine rather than freshwater ancestors, and that direct routes to the land from marginal-marine ecosystems were involved in the colonization of continental environments early in the Phanerozoic.Fil: Mángano, M. Gabriela. University of Saskatchewan; CanadáFil: Buatois, Luis A.. University of Saskatchewan; CanadáFil: Astini, Ricardo Alfredo. 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; ArgentinaFil: Rindsberg, Andrew K.. University of West Alabama; Estados UnidosGeological Society of America2014-02info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/133792Mángano, M. Gabriela; Buatois, Luis A.; Astini, Ricardo Alfredo; Rindsberg, Andrew K.; Trilobites in early Cambrian tidal flats and the landward expansion of the Cambrian explosion; Geological Society of America; Geology; 42; 2; 2-2014; 143-1460091-76131943-2682CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1130/G34980.1info:eu-repo/semantics/altIdentifier/url/https://pubs.geoscienceworld.org/gsa/geology/article-abstract/42/2/143/131437/Trilobites-in-early-Cambrian-tidal-flats-and-the?redirectedFrom=fulltextinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T10:02:15Zoai:ri.conicet.gov.ar:11336/133792instacron: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 10:02:15.897CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Trilobites in early Cambrian tidal flats and the landward expansion of the Cambrian explosion
title Trilobites in early Cambrian tidal flats and the landward expansion of the Cambrian explosion
spellingShingle Trilobites in early Cambrian tidal flats and the landward expansion of the Cambrian explosion
Mángano, M. Gabriela
Cambrian explosion
Trilobite trace fossils
Rome Formation
Appalachians
title_short Trilobites in early Cambrian tidal flats and the landward expansion of the Cambrian explosion
title_full Trilobites in early Cambrian tidal flats and the landward expansion of the Cambrian explosion
title_fullStr Trilobites in early Cambrian tidal flats and the landward expansion of the Cambrian explosion
title_full_unstemmed Trilobites in early Cambrian tidal flats and the landward expansion of the Cambrian explosion
title_sort Trilobites in early Cambrian tidal flats and the landward expansion of the Cambrian explosion
dc.creator.none.fl_str_mv Mángano, M. Gabriela
Buatois, Luis A.
Astini, Ricardo Alfredo
Rindsberg, Andrew K.
author Mángano, M. Gabriela
author_facet Mángano, M. Gabriela
Buatois, Luis A.
Astini, Ricardo Alfredo
Rindsberg, Andrew K.
author_role author
author2 Buatois, Luis A.
Astini, Ricardo Alfredo
Rindsberg, Andrew K.
author2_role author
author
author
dc.subject.none.fl_str_mv Cambrian explosion
Trilobite trace fossils
Rome Formation
Appalachians
topic Cambrian explosion
Trilobite trace fossils
Rome Formation
Appalachians
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 timing of the early invasion of the continents, the routes to the land, and the environmental breadth of the Cambrian explosion are important topics because they are at the core of our understanding of early evolutionary breakthroughs. Illuminating some aspects of these problems are trilobite trace fossils in tidal-flat deposits from the lower Cambrian Rome Formation in the southern Appalachian Mountains of Tennessee (USA). Morphologic details and size range of the trace fossils suggest production by olenellid trilobites, which occur as body fossils in the same unit. The occurrence of this ichnofauna, together with physical structures indicative of periodic subaerial exposure (desiccation cracks) and deposition within the intertidal zone (flat-topped ripples), shows that trilobites forayed into the upper intertidal zone during the Cambrian. Our finding supports the migration of subtidal organisms into marginal-marine, intertidal settings at the dawn of the Phanerozoic, suggesting that trilobites contributed to the establishment of the intertidal ecosystem during the Cambrian. The sequence of events involved in the colonization of early Paleozoic tidal flats is consistent with the idea that most terrestrial taxa originated from marine rather than freshwater ancestors, and that direct routes to the land from marginal-marine ecosystems were involved in the colonization of continental environments early in the Phanerozoic.
Fil: Mángano, M. Gabriela. University of Saskatchewan; Canadá
Fil: Buatois, Luis A.. University of Saskatchewan; Canadá
Fil: Astini, Ricardo Alfredo. 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
Fil: Rindsberg, Andrew K.. University of West Alabama; Estados Unidos
description The timing of the early invasion of the continents, the routes to the land, and the environmental breadth of the Cambrian explosion are important topics because they are at the core of our understanding of early evolutionary breakthroughs. Illuminating some aspects of these problems are trilobite trace fossils in tidal-flat deposits from the lower Cambrian Rome Formation in the southern Appalachian Mountains of Tennessee (USA). Morphologic details and size range of the trace fossils suggest production by olenellid trilobites, which occur as body fossils in the same unit. The occurrence of this ichnofauna, together with physical structures indicative of periodic subaerial exposure (desiccation cracks) and deposition within the intertidal zone (flat-topped ripples), shows that trilobites forayed into the upper intertidal zone during the Cambrian. Our finding supports the migration of subtidal organisms into marginal-marine, intertidal settings at the dawn of the Phanerozoic, suggesting that trilobites contributed to the establishment of the intertidal ecosystem during the Cambrian. The sequence of events involved in the colonization of early Paleozoic tidal flats is consistent with the idea that most terrestrial taxa originated from marine rather than freshwater ancestors, and that direct routes to the land from marginal-marine ecosystems were involved in the colonization of continental environments early in the Phanerozoic.
publishDate 2014
dc.date.none.fl_str_mv 2014-02
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/11336/133792
Mángano, M. Gabriela; Buatois, Luis A.; Astini, Ricardo Alfredo; Rindsberg, Andrew K.; Trilobites in early Cambrian tidal flats and the landward expansion of the Cambrian explosion; Geological Society of America; Geology; 42; 2; 2-2014; 143-146
0091-7613
1943-2682
CONICET Digital
CONICET
url http://hdl.handle.net/11336/133792
identifier_str_mv Mángano, M. Gabriela; Buatois, Luis A.; Astini, Ricardo Alfredo; Rindsberg, Andrew K.; Trilobites in early Cambrian tidal flats and the landward expansion of the Cambrian explosion; Geological Society of America; Geology; 42; 2; 2-2014; 143-146
0091-7613
1943-2682
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1130/G34980.1
info:eu-repo/semantics/altIdentifier/url/https://pubs.geoscienceworld.org/gsa/geology/article-abstract/42/2/143/131437/Trilobites-in-early-Cambrian-tidal-flats-and-the?redirectedFrom=fulltext
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 Geological Society of America
publisher.none.fl_str_mv Geological Society of America
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
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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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