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 paleoenvironmentally 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 dis parity 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.
Facultad de Ciencias Naturales y Museo
Materia
Ciencias Naturales
Paleocene
Salamanca Formation
plant diversity
Patagonia
South America
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/licenses/by/4.0/
Repositorio
SEDICI (UNLP)
Institución
Universidad Nacional de La Plata
OAI Identificador
oai:sedici.unlp.edu.ar:10915/131923

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spelling 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.Ciencias NaturalesPaleoceneSalamanca Formationplant diversityPatagoniaSouth AmericaFew 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 paleoenvironmentally 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 dis parity 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.Facultad de Ciencias Naturales y Museo2007info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionArticulohttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdf947-950http://sedici.unlp.edu.ar/handle/10915/131923enginfo:eu-repo/semantics/altIdentifier/issn/0091-7613info:eu-repo/semantics/altIdentifier/issn/1943-2682info:eu-repo/semantics/altIdentifier/doi/10.1130/g23889a.1info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by/4.0/Creative Commons Attribution 4.0 International (CC BY 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2025-09-17T10:14:55Zoai:sedici.unlp.edu.ar:10915/131923Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-09-17 10:14:55.812SEDICI (UNLP) - Universidad Nacional de La Platafalse
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
Ciencias Naturales
Paleocene
Salamanca Formation
plant diversity
Patagonia
South America
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 Ciencias Naturales
Paleocene
Salamanca Formation
plant diversity
Patagonia
South America
topic Ciencias Naturales
Paleocene
Salamanca Formation
plant diversity
Patagonia
South America
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 paleoenvironmentally 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 dis parity 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.
Facultad de Ciencias Naturales y Museo
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 paleoenvironmentally 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 dis parity 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
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language eng
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info:eu-repo/semantics/altIdentifier/issn/1943-2682
info:eu-repo/semantics/altIdentifier/doi/10.1130/g23889a.1
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/4.0/
Creative Commons Attribution 4.0 International (CC BY 4.0)
eu_rights_str_mv openAccess
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Creative Commons Attribution 4.0 International (CC BY 4.0)
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