New records of marsupials from the Miocene of Western Amazonia, Acre, Brazil

The Amazonian region covers a significant part of the South American continent and harbors outstanding biodiversity. However, much of its history is still unknown. This situation has begun to change with paleontological field efforts over the last decades, which have been proving that fossils can be...

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Main Authors: Narla S. Stutz, Patricia Hadler, Francisco R. Negri, Laurent Marivaux, Pierre-Olivier Antoine, François Pujos, Tiago R. Jacó, Emmanuelle M. Fontoura, Leonardo Kerber, Annie S. Hsiou, Roberto Ventura Santos, André M.V. Alvim, Ana Maria Ribeiro
Format: Article
Language:English
Published: Institute of Paleobiology PAS 2023-09-01
Series:Acta Palaeontologica Polonica
Subjects:
Online Access:https://www.app.pan.pl/archive/published/app68/app010572023.pdf
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author Narla S. Stutz
Patricia Hadler
Francisco R. Negri
Laurent Marivaux
Pierre-Olivier Antoine
François Pujos
Tiago R. Jacó
Emmanuelle M. Fontoura
Leonardo Kerber
Annie S. Hsiou
Roberto Ventura Santos
André M.V. Alvim
Ana Maria Ribeiro
author_facet Narla S. Stutz
Patricia Hadler
Francisco R. Negri
Laurent Marivaux
Pierre-Olivier Antoine
François Pujos
Tiago R. Jacó
Emmanuelle M. Fontoura
Leonardo Kerber
Annie S. Hsiou
Roberto Ventura Santos
André M.V. Alvim
Ana Maria Ribeiro
author_sort Narla S. Stutz
collection DOAJ
description The Amazonian region covers a significant part of the South American continent and harbors outstanding biodiversity. However, much of its history is still unknown. This situation has begun to change with paleontological field efforts over the last decades, which have been proving that fossils can be common in this region. Despite their great current species richness and abundance in the area today, marsupials have a sparse fossil record, restricted to a few specimens from handful Cenozoic Amazonian localities. Here we present new records of fossil marsupial teeth from the Solimões Formation (lower Eocene–Pliocene), on the Juruá and Envira riverbanks (Acre, Northwestern Brazil). The localities investigated yield at least four distinct didelphid didelphimorphians at PRE 06 (Ponto Rio Envira: Marmosini ?Marmosa sp., Didelphis cf. D. solimoensis, Thylamys? colombianus, plus unidentified didelphids), and two paucituberculatans from the Juruá River localities (Ponto Rio Juruá: the palaeothentid Palaeothentinae indet. at PRJ 25 and PRJ 33’, and Abderitidae indet. from PRJ 33). In agreement with the associated mammalian faunas, most of the didelphids, except for Thylamys? colombianus from PRE 06, indicate a (?early) Late Miocene age for this locality. Conversely, the abderitid specimens found in situ at PRJ 33 would match a Middle Miocene age. The palaeothentids found at PRJ 25 and PRJ 33’ localities cannot be considered for biostratigraphic inferences, since they were found outside a stratigraphic context. Nevertheless, these paucituberculatans considerably add to our knowledge, as they are the first ever recorded in Brazilian Amazonia.
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spelling doaj.art-6b51b590d83e4e218c9bf0c5778556ee2023-11-15T14:42:13ZengInstitute of Paleobiology PASActa Palaeontologica Polonica0567-79201732-24212023-09-0168345747510.4202/app.01057.2023New records of marsupials from the Miocene of Western Amazonia, Acre, BrazilNarla S. Stutz0https://orcid.org/0000-0002-1937-3902Patricia Hadler1https://orcid.org/0000-0003-4897-3111Francisco R. Negri2https://orcid.org/0000-0001-7396-0334Laurent Marivaux3https://orcid.org/0000-0002-2882-0874Pierre-Olivier Antoine4https://orcid.org/0000-0001-9122-1818François Pujos5https://orcid.org/0000-0002-6267-3927Tiago R. Jacó6https://orcid.org/0000-0002-5903-4673Emmanuelle M. Fontoura7https://orcid.org/0000-0002-3907-618XLeonardo Kerber8https://orcid.org/0000-0001-8139-1493Annie S. Hsiou9https://orcid.org/0000-0003-2392-6191Roberto Ventura Santos10https://orcid.org/0000-0001-6071-8100André M.V. Alvim11https://orcid.org/0000-0001-5050-4977Ana Maria Ribeiro12https://orcid.org/0000-0003-4167-8558Programa de Pós-Graduação em Geociências, Universidade Federal do Rio Grande do Sul, Av. Bento Gonçalves 9500, 91501-970, Porto Alegre, Rio Grande do Sul, Brazil, and Laboratoire de Paléontologie, Institut des Sciences de l’Évolution de Montpellier (ISE-M, UMR 5554, CNRS/IRD), Université de Montpellier, Place Eugène Bataillon, 34095, Montpellier, France.Laboratório de Paleontologia, Universidade Federal de Santa Catarina, Campus Universitário s/n, 88040-900, Florianópolis, Santa Catarina, Brazil.Laboratório de Paleontologia, Campus Floresta, Universidade Federal do Acre, Estrada do Canela Fina Km 12, 69980-000, Cruzeiro do Sul, Acre, Brazil.Laboratoire de Paléontologie, Institut des Sciences de l’Évolution de Montpellier (ISE-M, UMR 5554, CNRS/IRD), Université de Montpellier, Place Eugène Bataillon, 34095, Montpellier, FranceLaboratoire de Paléontologie, Institut des Sciences de l’Évolution de Montpellier (ISE-M, UMR 5554, CNRS/IRD), Université de Montpellier, Place Eugène Bataillon, 34095, Montpellier, FranceConsejo Nacional de Investigaciones Científicas y Técnicas (CONICET), and Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales (IANIGLA), CONICET-UNCUYO-Mendoza, Av. Ruiz Leal s/n, Parque Gral. San Martín, 5500, Mendoza, Argentina. Programa de Pós-Graduação em Sistemática e Conservação da Diversidade Biológica (PPGSCBIO), Secretaria do Meio Ambiente e Infraestrutura do Rio Grande do Sul, Universidade Estadual do Rio Grande do Sul, R. Dr. Salvador França 1427, 90690-000, Porto Alegre, Rio Grande do Sul, Brazil.Programa de Pós-Graduação em Biodiversidade Animal (PPGBA), Universidade Federal de Santa Maria, Av. Roraima 1000, 97105-900, Santa Maria, Rio Grande do Sul, and Centro de Apoio à Pesquisa Paleontológica da Quarta Colônia (CAPPA), Universidade Federal de Santa Maria, R. Maximiliano Vizzotto 598, 97230-000, São João do Polêsine, Rio Grande do Sul, Brazil.Centro de Apoio à Pesquisa Paleontológica da Quarta Colônia (CAPPA), Universidade Federal de Santa Maria, R. Maximiliano Vizzotto 598, 97230-000, São João do Polêsine, Rio Grande do Sul, Brazil. Laboratório de Paleontologia, Universidade de São Paulo, Av. Bandeirantes 3900, 14040-901, Ribeirão Preto, São Paulo, Brazil.Laboratório de Geocronologia, Instituto de Geociências, Universidade de Brasília (UnB), Campus Universitário Darcy Ribeiro ICC - Ala Central, 70910-900, Brasília, Distrito Federal, Brazil.Laboratório de Geocronologia, Instituto de Geociências, Universidade de Brasília (UnB), Campus Universitário Darcy Ribeiro ICC - Ala Central, 70910-900, Brasília, Distrito Federal, Brazil.Seção de Paleontologia, Museu de Ciências Naturais, Secretaria do Meio Ambiente e Infraestrutura, R. Dr. Salvador França 1427, 90690-000, Porto Alegre, Rio Grande do Sul, and Programa de Pós-Graduação em Geociências, Universidade Federal do Rio Grande do Sul, Av. Bento Gonçalves 9500, 91501-970, Porto Alegre, Rio Grande do Sul, Brazil.The Amazonian region covers a significant part of the South American continent and harbors outstanding biodiversity. However, much of its history is still unknown. This situation has begun to change with paleontological field efforts over the last decades, which have been proving that fossils can be common in this region. Despite their great current species richness and abundance in the area today, marsupials have a sparse fossil record, restricted to a few specimens from handful Cenozoic Amazonian localities. Here we present new records of fossil marsupial teeth from the Solimões Formation (lower Eocene–Pliocene), on the Juruá and Envira riverbanks (Acre, Northwestern Brazil). The localities investigated yield at least four distinct didelphid didelphimorphians at PRE 06 (Ponto Rio Envira: Marmosini ?Marmosa sp., Didelphis cf. D. solimoensis, Thylamys? colombianus, plus unidentified didelphids), and two paucituberculatans from the Juruá River localities (Ponto Rio Juruá: the palaeothentid Palaeothentinae indet. at PRJ 25 and PRJ 33’, and Abderitidae indet. from PRJ 33). In agreement with the associated mammalian faunas, most of the didelphids, except for Thylamys? colombianus from PRE 06, indicate a (?early) Late Miocene age for this locality. Conversely, the abderitid specimens found in situ at PRJ 33 would match a Middle Miocene age. The palaeothentids found at PRJ 25 and PRJ 33’ localities cannot be considered for biostratigraphic inferences, since they were found outside a stratigraphic context. Nevertheless, these paucituberculatans considerably add to our knowledge, as they are the first ever recorded in Brazilian Amazonia.https://www.app.pan.pl/archive/published/app68/app010572023.pdfmammaliametatheriadidelphimorphiapaucituberculatasystematicshistorical biogeographymiocenebrazil
spellingShingle Narla S. Stutz
Patricia Hadler
Francisco R. Negri
Laurent Marivaux
Pierre-Olivier Antoine
François Pujos
Tiago R. Jacó
Emmanuelle M. Fontoura
Leonardo Kerber
Annie S. Hsiou
Roberto Ventura Santos
André M.V. Alvim
Ana Maria Ribeiro
New records of marsupials from the Miocene of Western Amazonia, Acre, Brazil
Acta Palaeontologica Polonica
mammalia
metatheria
didelphimorphia
paucituberculata
systematics
historical biogeography
miocene
brazil
title New records of marsupials from the Miocene of Western Amazonia, Acre, Brazil
title_full New records of marsupials from the Miocene of Western Amazonia, Acre, Brazil
title_fullStr New records of marsupials from the Miocene of Western Amazonia, Acre, Brazil
title_full_unstemmed New records of marsupials from the Miocene of Western Amazonia, Acre, Brazil
title_short New records of marsupials from the Miocene of Western Amazonia, Acre, Brazil
title_sort new records of marsupials from the miocene of western amazonia acre brazil
topic mammalia
metatheria
didelphimorphia
paucituberculata
systematics
historical biogeography
miocene
brazil
url https://www.app.pan.pl/archive/published/app68/app010572023.pdf
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