Paleodiet of Lamini camelids (Mammalia: Artiodactyla) from the Pleistocene of southern Brazil: insights from stable isotope analysis (δ13C, δ18O)

Detalhes bibliográficos
Autor(a) principal: Carrasco, Thayara S. [UNESP]
Data de Publicação: 2022
Outros Autores: Scherer, Carolina S., Ribeiro, Ana Maria, Buchmann, Francisco S. [UNESP]
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da UNESP
Texto Completo: http://dx.doi.org/10.1017/pab.2022.10
http://hdl.handle.net/11449/240859
Resumo: Camelids (Camelidae) were a diverse and widely distributed group in South America during the Pleistocene. According to the fossil record, three species inhabited southern Brazil in the recent past: Hemiauchenia paradoxa, Lama guanicoe, and Vicugna vicugna. The analysis of carbon and oxygen stable isotope ratios in bioapatite provides insight into the paleobiology of nonliving animals and the environment they used to inhabit. We applied this tool to investigate the diet of camelids from two geological localities in southern Brazil: Touro Passo and Santa Vitória Formations (H. paradoxa, n = 7; L. guanicoe, n = 6; V. vicugna, n = 4). Carbon stable isotopes from enamel, dentin, and bone indicated that H. paradoxa and L. guanicoe had diets comprising mostly C3 grasses, but the latter showed a broader diet due to one individual with a mixed diet, whereas V. vicugna had a mixed C3-C4 diet. These different foraging behaviors may have minimized interspecific competition and favored niche partitioning and the coexistence of related species. Combined oxygen and carbon isotope data showed a consistent diet according to climate, probably due to the greater availability in glacial periods of cool-season grasses, which mainly use the C3 photosynthetic pathway. Given their adaptations to grazing, the climate amelioration, followed by the loss of grasslands, likely had a great impact on camelid populations, leading to their extinction in southern Brazil. These results, therefore, contribute to the understanding of the dynamics of paleocommunities in this region.
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spelling Paleodiet of Lamini camelids (Mammalia: Artiodactyla) from the Pleistocene of southern Brazil: insights from stable isotope analysis (δ13C, δ18O)Camelids (Camelidae) were a diverse and widely distributed group in South America during the Pleistocene. According to the fossil record, three species inhabited southern Brazil in the recent past: Hemiauchenia paradoxa, Lama guanicoe, and Vicugna vicugna. The analysis of carbon and oxygen stable isotope ratios in bioapatite provides insight into the paleobiology of nonliving animals and the environment they used to inhabit. We applied this tool to investigate the diet of camelids from two geological localities in southern Brazil: Touro Passo and Santa Vitória Formations (H. paradoxa, n = 7; L. guanicoe, n = 6; V. vicugna, n = 4). Carbon stable isotopes from enamel, dentin, and bone indicated that H. paradoxa and L. guanicoe had diets comprising mostly C3 grasses, but the latter showed a broader diet due to one individual with a mixed diet, whereas V. vicugna had a mixed C3-C4 diet. These different foraging behaviors may have minimized interspecific competition and favored niche partitioning and the coexistence of related species. Combined oxygen and carbon isotope data showed a consistent diet according to climate, probably due to the greater availability in glacial periods of cool-season grasses, which mainly use the C3 photosynthetic pathway. Given their adaptations to grazing, the climate amelioration, followed by the loss of grasslands, likely had a great impact on camelid populations, leading to their extinction in southern Brazil. These results, therefore, contribute to the understanding of the dynamics of paleocommunities in this region.Laboratório de Estratigrafia e Paleontologia Instituto de Biociências Universidade Estadual Paulista São VicenteCentro de Ciências Agrárias Ambientais e Biológicas Universidade Federal Do Recôncavo da Bahia, BahiaMuseu de Ciências Naturais Secretaria Do Meio Ambiente e Infraestrutura, Grande do SulLaboratório de Estratigrafia e Paleontologia Instituto de Biociências Universidade Estadual Paulista São VicenteUniversidade Estadual Paulista (UNESP)Universidade Federal Do Recôncavo da BahiaSecretaria Do Meio Ambiente e InfraestruturaCarrasco, Thayara S. [UNESP]Scherer, Carolina S.Ribeiro, Ana MariaBuchmann, Francisco S. [UNESP]2023-03-01T20:36:03Z2023-03-01T20:36:03Z2022-08-09info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/article513-526http://dx.doi.org/10.1017/pab.2022.10Paleobiology, v. 48, n. 3, p. 513-526, 2022.0094-8373http://hdl.handle.net/11449/24085910.1017/pab.2022.102-s2.0-85128472210Scopusreponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPengPaleobiologyinfo:eu-repo/semantics/openAccess2023-03-01T20:36:03Zoai:repositorio.unesp.br:11449/240859Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462023-03-01T20:36:03Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false
dc.title.none.fl_str_mv Paleodiet of Lamini camelids (Mammalia: Artiodactyla) from the Pleistocene of southern Brazil: insights from stable isotope analysis (δ13C, δ18O)
title Paleodiet of Lamini camelids (Mammalia: Artiodactyla) from the Pleistocene of southern Brazil: insights from stable isotope analysis (δ13C, δ18O)
spellingShingle Paleodiet of Lamini camelids (Mammalia: Artiodactyla) from the Pleistocene of southern Brazil: insights from stable isotope analysis (δ13C, δ18O)
Carrasco, Thayara S. [UNESP]
title_short Paleodiet of Lamini camelids (Mammalia: Artiodactyla) from the Pleistocene of southern Brazil: insights from stable isotope analysis (δ13C, δ18O)
title_full Paleodiet of Lamini camelids (Mammalia: Artiodactyla) from the Pleistocene of southern Brazil: insights from stable isotope analysis (δ13C, δ18O)
title_fullStr Paleodiet of Lamini camelids (Mammalia: Artiodactyla) from the Pleistocene of southern Brazil: insights from stable isotope analysis (δ13C, δ18O)
title_full_unstemmed Paleodiet of Lamini camelids (Mammalia: Artiodactyla) from the Pleistocene of southern Brazil: insights from stable isotope analysis (δ13C, δ18O)
title_sort Paleodiet of Lamini camelids (Mammalia: Artiodactyla) from the Pleistocene of southern Brazil: insights from stable isotope analysis (δ13C, δ18O)
author Carrasco, Thayara S. [UNESP]
author_facet Carrasco, Thayara S. [UNESP]
Scherer, Carolina S.
Ribeiro, Ana Maria
Buchmann, Francisco S. [UNESP]
author_role author
author2 Scherer, Carolina S.
Ribeiro, Ana Maria
Buchmann, Francisco S. [UNESP]
author2_role author
author
author
dc.contributor.none.fl_str_mv Universidade Estadual Paulista (UNESP)
Universidade Federal Do Recôncavo da Bahia
Secretaria Do Meio Ambiente e Infraestrutura
dc.contributor.author.fl_str_mv Carrasco, Thayara S. [UNESP]
Scherer, Carolina S.
Ribeiro, Ana Maria
Buchmann, Francisco S. [UNESP]
description Camelids (Camelidae) were a diverse and widely distributed group in South America during the Pleistocene. According to the fossil record, three species inhabited southern Brazil in the recent past: Hemiauchenia paradoxa, Lama guanicoe, and Vicugna vicugna. The analysis of carbon and oxygen stable isotope ratios in bioapatite provides insight into the paleobiology of nonliving animals and the environment they used to inhabit. We applied this tool to investigate the diet of camelids from two geological localities in southern Brazil: Touro Passo and Santa Vitória Formations (H. paradoxa, n = 7; L. guanicoe, n = 6; V. vicugna, n = 4). Carbon stable isotopes from enamel, dentin, and bone indicated that H. paradoxa and L. guanicoe had diets comprising mostly C3 grasses, but the latter showed a broader diet due to one individual with a mixed diet, whereas V. vicugna had a mixed C3-C4 diet. These different foraging behaviors may have minimized interspecific competition and favored niche partitioning and the coexistence of related species. Combined oxygen and carbon isotope data showed a consistent diet according to climate, probably due to the greater availability in glacial periods of cool-season grasses, which mainly use the C3 photosynthetic pathway. Given their adaptations to grazing, the climate amelioration, followed by the loss of grasslands, likely had a great impact on camelid populations, leading to their extinction in southern Brazil. These results, therefore, contribute to the understanding of the dynamics of paleocommunities in this region.
publishDate 2022
dc.date.none.fl_str_mv 2022-08-09
2023-03-01T20:36:03Z
2023-03-01T20:36:03Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://dx.doi.org/10.1017/pab.2022.10
Paleobiology, v. 48, n. 3, p. 513-526, 2022.
0094-8373
http://hdl.handle.net/11449/240859
10.1017/pab.2022.10
2-s2.0-85128472210
url http://dx.doi.org/10.1017/pab.2022.10
http://hdl.handle.net/11449/240859
identifier_str_mv Paleobiology, v. 48, n. 3, p. 513-526, 2022.
0094-8373
10.1017/pab.2022.10
2-s2.0-85128472210
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv Paleobiology
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
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dc.format.none.fl_str_mv 513-526
dc.source.none.fl_str_mv Scopus
reponame:Repositório Institucional da UNESP
instname:Universidade Estadual Paulista (UNESP)
instacron:UNESP
instname_str Universidade Estadual Paulista (UNESP)
instacron_str UNESP
institution UNESP
reponame_str Repositório Institucional da UNESP
collection Repositório Institucional da UNESP
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