A Paleocene lowland macroflora from Patagonia reveals significantly greater richness than North American analogs
- Autores
- Iglesias, Ari; Wilf, Peter; Johnson, Kirk R.; Zamuner, Alba Berta; Cúneo, N. Rubén; Matheos, Sergio Daniel; Singer, Bradley S.
- Año de publicación
- 2007
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Few South American macrofloras of Paleocene age are known, and this limits our knowledge of diversity and composition between the end-Cretaceous event and the Eocene appearance of high floral diversity. We report new, unbiased collections of 2516 compression specimens from the Paleocene Salamanca Formation (ca. 61.7 Ma) from two localities in the Palacio de los Loros exposures in southern Chubut, Patagonia, Argentina. Our samples reveal considerably greater richness than was previously known from the Paleocene of Patagonia, including 36 species of angiosperm leaves as well as angiosperm fruits, flowers, and seeds; ferns; and conifer leaves, cones, and seeds. The floras, which are from siltstone and sandstone channel-fills deposited on low-relief floodplain landscapes in a humid, warm temperate climate, are climatically and paleoenviromnentally comparable to many quantitatively collected Paleocene floras from the Western Interior of North America. Adjusted for sample size, there are >50% more species at each Palacio de los Loros quarry than in any comparable U.S. Paleocene sample. These results indicate more vibrant terrestrial ecosystems in Patagonian than in North American floodplain environments ∼4 m.y. after the end-Cretaceous extinction, and they push back the time line 10 m.y. for the evolution of high floral diversity in South America. The cause of the disparity is unknown but could involve reduced impact effects because of greater distance from the Chicxulub site, higher latest Cretaceous diversity, or faster recovery or immigration rates.
Fil: Iglesias, Ari. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo; Argentina
Fil: Wilf, Peter. State University of Pennsylvania; Estados Unidos. University Park; Estados Unidos
Fil: Johnson, Kirk R.. Denver Museum of Nature & Science; Estados Unidos
Fil: Zamuner, Alba Berta. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Área Paleobotánica; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Cúneo, N. Rubén. Museo Paleontológico Egidio Feruglio; Argentina
Fil: Matheos, Sergio Daniel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
Fil: Singer, Bradley S.. University of Wisconsin; Estados Unidos - Materia
-
PALEOCENE
PATAGONIA
PLANT DIVERSITY
SALAMANCA FORMATION
SOUTH AFRICA - 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:11336/215824
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CONICET Digital (CONICET) |
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A Paleocene lowland macroflora from Patagonia reveals significantly greater richness than North American analogsIglesias, AriWilf, PeterJohnson, Kirk R.Zamuner, Alba BertaCúneo, N. RubénMatheos, Sergio DanielSinger, Bradley S.PALEOCENEPATAGONIAPLANT DIVERSITYSALAMANCA FORMATIONSOUTH AFRICAhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Few South American macrofloras of Paleocene age are known, and this limits our knowledge of diversity and composition between the end-Cretaceous event and the Eocene appearance of high floral diversity. We report new, unbiased collections of 2516 compression specimens from the Paleocene Salamanca Formation (ca. 61.7 Ma) from two localities in the Palacio de los Loros exposures in southern Chubut, Patagonia, Argentina. Our samples reveal considerably greater richness than was previously known from the Paleocene of Patagonia, including 36 species of angiosperm leaves as well as angiosperm fruits, flowers, and seeds; ferns; and conifer leaves, cones, and seeds. The floras, which are from siltstone and sandstone channel-fills deposited on low-relief floodplain landscapes in a humid, warm temperate climate, are climatically and paleoenviromnentally comparable to many quantitatively collected Paleocene floras from the Western Interior of North America. Adjusted for sample size, there are >50% more species at each Palacio de los Loros quarry than in any comparable U.S. Paleocene sample. These results indicate more vibrant terrestrial ecosystems in Patagonian than in North American floodplain environments ∼4 m.y. after the end-Cretaceous extinction, and they push back the time line 10 m.y. for the evolution of high floral diversity in South America. The cause of the disparity is unknown but could involve reduced impact effects because of greater distance from the Chicxulub site, higher latest Cretaceous diversity, or faster recovery or immigration rates.Fil: Iglesias, Ari. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo; ArgentinaFil: Wilf, Peter. State University of Pennsylvania; Estados Unidos. University Park; Estados UnidosFil: Johnson, Kirk R.. Denver Museum of Nature & Science; Estados UnidosFil: Zamuner, Alba Berta. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Área Paleobotánica; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaFil: Cúneo, N. Rubén. Museo Paleontológico Egidio Feruglio; ArgentinaFil: Matheos, Sergio Daniel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; ArgentinaFil: Singer, Bradley S.. University of Wisconsin; Estados UnidosGeological Society of America2007-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/215824Iglesias, Ari; Wilf, Peter; Johnson, Kirk R.; Zamuner, Alba Berta; Cúneo, N. Rubén; et al.; A Paleocene lowland macroflora from Patagonia reveals significantly greater richness than North American analogs; Geological Society of America; Geology; 35; 10; 12-2007; 947-9500091-7613CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://pubs.geoscienceworld.org/gsa/geology/article/35/10/947/129743/A-Paleocene-lowland-macroflora-from-Patagoniainfo:eu-repo/semantics/altIdentifier/doi/10.1130/G23889A.1info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-15T14:47:29Zoai:ri.conicet.gov.ar:11336/215824instacron: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:34982025-10-15 14:47:30.16CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
A Paleocene lowland macroflora from Patagonia reveals significantly greater richness than North American analogs |
title |
A Paleocene lowland macroflora from Patagonia reveals significantly greater richness than North American analogs |
spellingShingle |
A Paleocene lowland macroflora from Patagonia reveals significantly greater richness than North American analogs Iglesias, Ari PALEOCENE PATAGONIA PLANT DIVERSITY SALAMANCA FORMATION SOUTH AFRICA |
title_short |
A Paleocene lowland macroflora from Patagonia reveals significantly greater richness than North American analogs |
title_full |
A Paleocene lowland macroflora from Patagonia reveals significantly greater richness than North American analogs |
title_fullStr |
A Paleocene lowland macroflora from Patagonia reveals significantly greater richness than North American analogs |
title_full_unstemmed |
A Paleocene lowland macroflora from Patagonia reveals significantly greater richness than North American analogs |
title_sort |
A Paleocene lowland macroflora from Patagonia reveals significantly greater richness than North American analogs |
dc.creator.none.fl_str_mv |
Iglesias, Ari Wilf, Peter Johnson, Kirk R. Zamuner, Alba Berta Cúneo, N. Rubén Matheos, Sergio Daniel Singer, Bradley S. |
author |
Iglesias, Ari |
author_facet |
Iglesias, Ari Wilf, Peter Johnson, Kirk R. Zamuner, Alba Berta Cúneo, N. Rubén Matheos, Sergio Daniel Singer, Bradley S. |
author_role |
author |
author2 |
Wilf, Peter Johnson, Kirk R. Zamuner, Alba Berta Cúneo, N. Rubén Matheos, Sergio Daniel Singer, Bradley S. |
author2_role |
author author author author author author |
dc.subject.none.fl_str_mv |
PALEOCENE PATAGONIA PLANT DIVERSITY SALAMANCA FORMATION SOUTH AFRICA |
topic |
PALEOCENE PATAGONIA PLANT DIVERSITY SALAMANCA FORMATION SOUTH AFRICA |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
Few South American macrofloras of Paleocene age are known, and this limits our knowledge of diversity and composition between the end-Cretaceous event and the Eocene appearance of high floral diversity. We report new, unbiased collections of 2516 compression specimens from the Paleocene Salamanca Formation (ca. 61.7 Ma) from two localities in the Palacio de los Loros exposures in southern Chubut, Patagonia, Argentina. Our samples reveal considerably greater richness than was previously known from the Paleocene of Patagonia, including 36 species of angiosperm leaves as well as angiosperm fruits, flowers, and seeds; ferns; and conifer leaves, cones, and seeds. The floras, which are from siltstone and sandstone channel-fills deposited on low-relief floodplain landscapes in a humid, warm temperate climate, are climatically and paleoenviromnentally comparable to many quantitatively collected Paleocene floras from the Western Interior of North America. Adjusted for sample size, there are >50% more species at each Palacio de los Loros quarry than in any comparable U.S. Paleocene sample. These results indicate more vibrant terrestrial ecosystems in Patagonian than in North American floodplain environments ∼4 m.y. after the end-Cretaceous extinction, and they push back the time line 10 m.y. for the evolution of high floral diversity in South America. The cause of the disparity is unknown but could involve reduced impact effects because of greater distance from the Chicxulub site, higher latest Cretaceous diversity, or faster recovery or immigration rates. Fil: Iglesias, Ari. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo; Argentina Fil: Wilf, Peter. State University of Pennsylvania; Estados Unidos. University Park; Estados Unidos Fil: Johnson, Kirk R.. Denver Museum of Nature & Science; Estados Unidos Fil: Zamuner, Alba Berta. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Área Paleobotánica; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina Fil: Cúneo, N. Rubén. Museo Paleontológico Egidio Feruglio; Argentina Fil: Matheos, Sergio Daniel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina Fil: Singer, Bradley S.. University of Wisconsin; Estados Unidos |
description |
Few South American macrofloras of Paleocene age are known, and this limits our knowledge of diversity and composition between the end-Cretaceous event and the Eocene appearance of high floral diversity. We report new, unbiased collections of 2516 compression specimens from the Paleocene Salamanca Formation (ca. 61.7 Ma) from two localities in the Palacio de los Loros exposures in southern Chubut, Patagonia, Argentina. Our samples reveal considerably greater richness than was previously known from the Paleocene of Patagonia, including 36 species of angiosperm leaves as well as angiosperm fruits, flowers, and seeds; ferns; and conifer leaves, cones, and seeds. The floras, which are from siltstone and sandstone channel-fills deposited on low-relief floodplain landscapes in a humid, warm temperate climate, are climatically and paleoenviromnentally comparable to many quantitatively collected Paleocene floras from the Western Interior of North America. Adjusted for sample size, there are >50% more species at each Palacio de los Loros quarry than in any comparable U.S. Paleocene sample. These results indicate more vibrant terrestrial ecosystems in Patagonian than in North American floodplain environments ∼4 m.y. after the end-Cretaceous extinction, and they push back the time line 10 m.y. for the evolution of high floral diversity in South America. The cause of the disparity is unknown but could involve reduced impact effects because of greater distance from the Chicxulub site, higher latest Cretaceous diversity, or faster recovery or immigration rates. |
publishDate |
2007 |
dc.date.none.fl_str_mv |
2007-12 |
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/11336/215824 Iglesias, Ari; Wilf, Peter; Johnson, Kirk R.; Zamuner, Alba Berta; Cúneo, N. Rubén; et al.; A Paleocene lowland macroflora from Patagonia reveals significantly greater richness than North American analogs; Geological Society of America; Geology; 35; 10; 12-2007; 947-950 0091-7613 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/215824 |
identifier_str_mv |
Iglesias, Ari; Wilf, Peter; Johnson, Kirk R.; Zamuner, Alba Berta; Cúneo, N. Rubén; et al.; A Paleocene lowland macroflora from Patagonia reveals significantly greater richness than North American analogs; Geological Society of America; Geology; 35; 10; 12-2007; 947-950 0091-7613 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://pubs.geoscienceworld.org/gsa/geology/article/35/10/947/129743/A-Paleocene-lowland-macroflora-from-Patagonia info:eu-repo/semantics/altIdentifier/doi/10.1130/G23889A.1 |
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info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
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openAccess |
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https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
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application/pdf application/pdf application/pdf |
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Geological Society of America |
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Geological Society of America |
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CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
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dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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