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1000 Titel
  • Stable oxygen isotopes of crocodilian tooth enamel allow tracking Plio-Pleistocene evolution of freshwater environments and climate in the Shungura Formation (Turkana Depression, Ethiopia)
1000 Autor/in
  1. Gardin, Axelle |
  2. Pucéat, Emmanuelle |
  3. Garcia, Géraldine |
  4. Boisserie, Jean-Renaud |
  5. Euriat, Adélaïde |
  6. Joachimski, Michael M. |
  7. Nutz, Alexis |
  8. Schuster, Mathieu |
  9. Otero, Olga |
1000 Verlag
  • Copernicus Publications
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-01-25
1000 Erschienen in
1000 Quellenangabe
  • 21(2):437-454
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/bg-21-437-2024 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:p>Abstract. This study adopts a new approach describing palaeohydrology and palaeoclimates based on the interpretation of stable oxygen isotopes (δ18Op) recorded in fossil crocodilian teeth. They represent an archive of prime interest for tracking freshwater palaeoenvironmental change, applicable to many palaeontological localities in the world: crocodilian teeth are abundant in continental basins and have been widely distributed since their diversification during the Mesozoic; the enamel phosphate is resistant to diagenesis and retains its original isotopic composition over geological timescales; and their δ18Op mainly relies on that of the crocodilian's home waterbody (δ18Ow), which in turn reflects waterbody types, regional climate, and evaporation conditions. This study presents the first application of this theoretical interpretative model to the Shungura Formation (Lower Omo Valley, Ethiopia), a key witness of the important environmental change in eastern Africa during the Plio-Pleistocene that impacted the evolution of regional faunas, including humans. In this complex and variable environmental context, the δ18Op of coexisting crocodilians allows for the fingerprinting of the diversity of aquatic environments they had access to at a local scale. This study sheds light on two important results: the δ18Op of crocodilian teeth (1) indicates stable aquatic environments in the northern Turkana Depression from 2.97 to ca. 2.57 Ma but a decline in local waterbodies diversity after 2.32 Ma, suggesting increasing aridity, and (2) shows, like previous geochemical studies on palaeosols and bivalves in the area, a significant increase in δ18Ow from 2.97 to ca. 1.14 Ma, likely due to the shifting air stream convergence zones between the West African and Indian Summer Monsoons and/or reduced rainfall over the Ethiopian Highlands. </jats:p>
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1000 Förderer
  1. Centre National de la Recherche Scientifique |
  2. Ministère de l'Europe et des Affaires Étrangères |
  3. Agence Nationale de la Recherche |
  4. Fondation Fyssen |
  5. Conseil Régional Aquitaine |
  6. Ministère de l'Enseignement Supérieur et de la Recherche |
  7. Université de Poitiers |
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1000 Dateien
1000 Förderung
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    1000 Förderer Centre National de la Recherche Scientifique |
    1000 Förderprogramm -
    1000 Fördernummer -
  2. 1000 joinedFunding-child
    1000 Förderer Ministère de l'Europe et des Affaires Étrangères |
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  3. 1000 joinedFunding-child
    1000 Förderer Agence Nationale de la Recherche |
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  4. 1000 joinedFunding-child
    1000 Förderer Fondation Fyssen |
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  5. 1000 joinedFunding-child
    1000 Förderer Conseil Régional Aquitaine |
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    1000 Förderer Ministère de l'Enseignement Supérieur et de la Recherche |
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    1000 Förderer Université de Poitiers |
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1000 Erstellt am 2024-05-24T04:18:03.078+0200
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1000 Objekt bearb. Mon May 27 10:23:54 CEST 2024
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