Stable Sr isotopes of fossil dental enamel reflect diet and digestive system differences among sympatric herbivores

Reconstructing the trophic (paleo)ecology and associated physiological traits of both extinct and extant taxa is essential for understanding the functioning of (past) ecosystems. In this context, novel metal stable isotope proxies offer promising tools for investigating ancient diets and, to some ex...

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Detalhes bibliográficos
Autores: Armaroli, Elena, Chelli Cheheb, Razika, Cipriani, Anna, Bernardini, Sara, Van der Made, Jan, Cáceres, Isabel, Sahnouni, Mohamed, Lugli, Federico
Tipo de documento: artigo
Estado:Versão publicada
Data de publicação:2025
País:España
Recursos:Consejo Superior de Investigaciones Científicas (CSIC)
Repositório:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:dnet:digitalcsic_::0536bfbb00ba90b6912cac347bb04e0a
Acesso em linha:http://hdl.handle.net/10261/431101
Access Level:Acceso aberto
Palavra-chave:Browsers
Grazers
Stable strontium isotopes
Tooth enamel
Trophic niche
Descrição
Resumo:Reconstructing the trophic (paleo)ecology and associated physiological traits of both extinct and extant taxa is essential for understanding the functioning of (past) ecosystems. In this context, novel metal stable isotope proxies offer promising tools for investigating ancient diets and, to some extent, the digestive adaptations of animals. In this study, we analyzed the stable strontium isotope composition (δSr), alongside δC, δO, and Sr/Sr ratios, in fossil dental remains of herbivorous mammals from the Early Pleistocene site of Tighennif, Algeria (∼1.2–1.0 Ma). Traditional carbon and oxygen isotope data indicate an environment dominated by C vegetation, while the Sr/Sr ratios suggest either a relatively homogeneous strontium baseline or limited geographic mobility of the animals. Our results demonstrate that δSr is sensitive to diagenetic alteration, with enamel samples retaining biogenic signatures comparable to those of modern mammals, whereas dentine exhibits δSr values shifted toward positive geogenic end-members. δSr patterns may reflect trophic niche differentiation among herbivores and potentially indicate distinct digestive physiologies, offering a novel alternative proxy for dietary and ecological reconstructions in the fossil record.