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
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/133792
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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 |
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reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
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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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1842269747372097536 |
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13.13397 |