Articles | Volume 21, issue 4
https://doi.org/10.5194/cp-21-841-2025
© Author(s) 2025. 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-21-841-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Middle Miocene climate evolution in the northern Mediterranean region (Digne–Valensole basin, SE France)
Armelle Ballian
CORRESPONDING AUTHOR
Senckenberg Biodiversity and Climate Research Centre (SBiK-F), Frankfurt am Main, Germany
Institute of Geosciences, Goethe University Frankfurt, Frankfurt am Main, Germany
Maud J. M. Meijers
Senckenberg Biodiversity and Climate Research Centre (SBiK-F), Frankfurt am Main, Germany
Department of Earth Sciences, NAWI Graz Geocenter, University of Graz, Graz, Austria
Isabelle Cojan
MinesParis, Centre de Géosciences, PSL University, Fontainebleau, France
Damien Huyghe
MinesParis, Centre de Géosciences, PSL University, Fontainebleau, France
Miguel Bernecker
Institute of Geosciences, Goethe University Frankfurt, Frankfurt am Main, Germany
Katharina Methner
Senckenberg Biodiversity and Climate Research Centre (SBiK-F), Frankfurt am Main, Germany
Institute for Earth System Science and Remote Sensing, University of Leipzig, Leipzig, Germany
Mattia Tagliavento
Institute of Geosciences, Goethe University Frankfurt, Frankfurt am Main, Germany
Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA, USA
Jens Fiebig
Institute of Geosciences, Goethe University Frankfurt, Frankfurt am Main, Germany
Andreas Mulch
Senckenberg Biodiversity and Climate Research Centre (SBiK-F), Frankfurt am Main, Germany
Institute of Geosciences, Goethe University Frankfurt, Frankfurt am Main, Germany
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Subject: Continental Surface Processes | Archive: Terrestrial Archives | Timescale: Cenozoic
Climatic and tectonic controls on shallow-marine and freshwater diatomite deposition throughout the Palaeogene
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Fluvio-deltaic record of increased sediment transport during the Middle Eocene Climatic Optimum (MECO), Southern Pyrenees, Spain
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Palaeo-environmental evolution of Central Asia during the Cenozoic: new insights from the continental sedimentary archive of the Valley of Lakes (Mongolia)
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Andre Baldermann, Oliver Wasser, Elshan Abdullayev, Stefano Bernasconi, Stefan Löhr, Klaus Wemmer, Werner E. Piller, Maxim Rudmin, and Sylvain Richoz
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We identified the provenance, (post)depositional history, weathering conditions and hydroclimate that formed the detrital and authigenic silicates and soil carbonates of the Valley of Lakes sediments in Central Asia during the Cenozoic (~34 to 21 Ma). Aridification pulses in continental Central Asia coincide with marine glaciation events and are caused by Cenozoic climate forcing and the exhumation of the Tian Shan, Hangay and Altai mountains, which reduced the moisture influx by westerly winds.
Y. X. Li, W. J. Jiao, Z. H. Liu, J. H. Jin, D. H. Wang, Y. X. He, and C. Quan
Clim. Past, 12, 255–272, https://doi.org/10.5194/cp-12-255-2016, https://doi.org/10.5194/cp-12-255-2016, 2016
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An integrated litho-, bio-, cyclo-, and magnetostratigraphy constrains the onset of a depositional environmental change from a lacustrine to a deltaic environment in the Maoming Basin, China, at 33.88 Ma. This coincides with the global cooling during the Eocene-Oligocene transition (EOT) at ~ 33.7–33.9 Ma. This change represents terrestrial responses of low-latitude Asia to the EOT. The greatly refined chronology permits detailed examination of the late Paleogene climate change in southeast Asia.
A. E. Chew
Clim. Past, 11, 1223–1237, https://doi.org/10.5194/cp-11-1223-2015, https://doi.org/10.5194/cp-11-1223-2015, 2015
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This project describes mammal faunal response in the zone of the ETM2 and H2 hyperthermals (rapid global warming events) of the early Paleogene in the south-central Bighorn Basin, WY. The response includes changes in faunal structure and species relative body size. Comparative analysis suggests that environmental moisture and rate of change are important moderators of response.
V. Wennrich, P. S. Minyuk, V. Borkhodoev, A. Francke, B. Ritter, N. R. Nowaczyk, M. A. Sauerbrey, J. Brigham-Grette, and M. Melles
Clim. Past, 10, 1381–1399, https://doi.org/10.5194/cp-10-1381-2014, https://doi.org/10.5194/cp-10-1381-2014, 2014
S. Frisia, A. Borsato, R. N. Drysdale, B. Paul, A. Greig, and M. Cotte
Clim. Past, 8, 2039–2051, https://doi.org/10.5194/cp-8-2039-2012, https://doi.org/10.5194/cp-8-2039-2012, 2012
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Short summary
During the Middle Miocene, the Earth transitioned from a warm to a colder period, significantly impacting ecosystems and climate. We present a 23–13 Ma climate record of soil carbonates from a northern Mediterranean basin. We propose that rapid temperature shifts in our data result from changes in atmospheric circulation patterns. Our climate record aligns well with contemporaneous terrestrial European and global marine records, enhancing our understanding of Miocene climate dynamics.
During the Middle Miocene, the Earth transitioned from a warm to a colder period, significantly...