Articles | Volume 19, issue 3
https://doi.org/10.5194/cp-19-533-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-19-533-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
08 Mar 2023
Research article |
| 08 Mar 2023
| 08 Mar 2023
Fluvio-deltaic record of increased sediment transport during the Middle Eocene Climatic Optimum (MECO), Southern Pyrenees, Spain
Département des Sciences de la Terre, Université de
Genève, Geneva, 1205, Switzerland
Departament de Geologia, Universitat Autònoma de Barcelona, Bellaterra, Cerdanyola del Vallès, 08193, Spain
Luis Valero
Département des Sciences de la Terre, Université de
Genève, Geneva, 1205, Switzerland
Jorge E. Spangenberg
Institute of Earth Surface Dynamics (IDYST), University of Lausanne, Géopolis, Lausanne, 1015, Switzerland
Andreu Vinyoles
Departament de Dinàmica de la Terra i l'Oceà, Facultat de
Ciències de la Terra, Barcelona, 08028, Spain
Jean Verité
Département des Sciences de la Terre, Université de
Genève, Geneva, 1205, Switzerland
Départment des Geosciences, Université de Rennes, Rennes, UMR 6118, France
Thierry Adatte
Institute of Earth Sciences (ISTE), University of Lausanne,
Géopolis, Lausanne, 1015, Switzerland
Maxime Tremblin
Département des Sciences de la Terre, Université de
Genève, Geneva, 1205, Switzerland
Stephen Watkins
Département des Sciences de la Terre, Université de
Genève, Geneva, 1205, Switzerland
Nikhil Sharma
Département des Sciences de la Terre, Université de
Genève, Geneva, 1205, Switzerland
Miguel Garcés
Departament de Dinàmica de la Terra i l'Oceà, Facultat de
Ciències de la Terra, Barcelona, 08028, Spain
Cai Puigdefàbregas
Departament de Geologia, Universitat Autònoma de Barcelona, Bellaterra, Cerdanyola del Vallès, 08193, Spain
Sébastien Castelltort
Département des Sciences de la Terre, Université de
Genève, Geneva, 1205, Switzerland
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Cited
10 citations as recorded by crossref.
- Sediment supply variation control on Lower Eocene delta sequences (Tremp Basin, Spain) R. Vaucher et al. 10.1130/G52548.1
- Diverse ecological responses of foraminifera to the Middle Eocene Climatic Optimum (MECO) in shallow-water settings (Provençal Domain, NW Italy) A. Gandolfi et al. 10.1016/j.palaeo.2024.112697
- Middle Eocene Climatic Optimum drove palaeoenvironmental fluctuations and organic matter enrichment in lacustrine facies of the Bohai Bay Basin, China Y. Wu et al. 10.1016/j.palaeo.2024.112665
- Unraveling ecological signals related to the MECO onset through planktic and benthic foraminiferal records along a mixed carbonate-siliciclastic shallow-water succession A. Gandolfi et al. 10.1016/j.marmicro.2024.102388
- Iron-carbonate concretions with inverse magnetic fabrics; a record of environmental changes in the middle Eocene marine marls of the Southern Pyrenees? B. Oliva-Urcia et al. 10.1007/s41513-024-00271-9
- Nannofossils from the Middle Eocene Sabiñánigo Sandstone Formation in the Jaca Basin (southern Pyrenees): biostratigraphy and paleoenvironmental implications E. Lasluisa et al. 10.5194/jm-43-55-2024
- A Paleogene mixed carbonate-siliciclastic system in the western Tethys: spectral gamma-ray as a tool for the reconstruction of paleoclimate and transgressive-regressive cycles V. Giraldo-Gómez et al. 10.1016/j.marpetgeo.2024.106752
- Middle Eocene Climatic Optimum (MECO) and its imprint in the continental Escanilla Formation, Spain N. Sharma et al. 10.5194/cp-20-935-2024
- Short-term middle Eocene (Bartonian) paleoenvironmental changes in the sedimentary succession of Olivetta San Michele (NW Italy): the response of shallow-water biota to climate in NW Tethys L. Arena et al. 10.1007/s10347-023-00677-4
- Water discharge variations control fluvial stratigraphic architecture in the Middle Eocene Escanilla formation, Spain N. Sharma et al. 10.1038/s41598-023-33600-6
8 citations as recorded by crossref.
- Sediment supply variation control on Lower Eocene delta sequences (Tremp Basin, Spain) R. Vaucher et al. 10.1130/G52548.1
- Diverse ecological responses of foraminifera to the Middle Eocene Climatic Optimum (MECO) in shallow-water settings (Provençal Domain, NW Italy) A. Gandolfi et al. 10.1016/j.palaeo.2024.112697
- Middle Eocene Climatic Optimum drove palaeoenvironmental fluctuations and organic matter enrichment in lacustrine facies of the Bohai Bay Basin, China Y. Wu et al. 10.1016/j.palaeo.2024.112665
- Unraveling ecological signals related to the MECO onset through planktic and benthic foraminiferal records along a mixed carbonate-siliciclastic shallow-water succession A. Gandolfi et al. 10.1016/j.marmicro.2024.102388
- Iron-carbonate concretions with inverse magnetic fabrics; a record of environmental changes in the middle Eocene marine marls of the Southern Pyrenees? B. Oliva-Urcia et al. 10.1007/s41513-024-00271-9
- Nannofossils from the Middle Eocene Sabiñánigo Sandstone Formation in the Jaca Basin (southern Pyrenees): biostratigraphy and paleoenvironmental implications E. Lasluisa et al. 10.5194/jm-43-55-2024
- A Paleogene mixed carbonate-siliciclastic system in the western Tethys: spectral gamma-ray as a tool for the reconstruction of paleoclimate and transgressive-regressive cycles V. Giraldo-Gómez et al. 10.1016/j.marpetgeo.2024.106752
- Middle Eocene Climatic Optimum (MECO) and its imprint in the continental Escanilla Formation, Spain N. Sharma et al. 10.5194/cp-20-935-2024
2 citations as recorded by crossref.
- Short-term middle Eocene (Bartonian) paleoenvironmental changes in the sedimentary succession of Olivetta San Michele (NW Italy): the response of shallow-water biota to climate in NW Tethys L. Arena et al. 10.1007/s10347-023-00677-4
- Water discharge variations control fluvial stratigraphic architecture in the Middle Eocene Escanilla formation, Spain N. Sharma et al. 10.1038/s41598-023-33600-6
Latest update: 11 May 2025
Short summary
The Middle Eocene Climatic Optimum (MECO) was a global warming event that took place 40 Myr ago and lasted ca. 500 kyr, inducing physical, chemical, and biotic changes on the Earth. We use stable isotopes to identify the MECO in the Eocene deltaic deposits of the Southern Pyrenees. Our findings reveal enhanced deltaic progradation during the MECO, pointing to the important impact of global warming on fluvial sediment transport with implications for the consequences of current climate change.
The Middle Eocene Climatic Optimum (MECO) was a global warming event that took place 40 Myr ago...
