| one publication added to basket [391028] | A new insight of the MIS 3 Dansgaard-Oeschger climate oscillations in western Europe from the study of a Belgium isotopically equilibrated speleothem
Peral, M.; Marchegiano, M.; Verheyden, S.; Goderis, S.; Van Helden, T.; Vanhaecke, F.; Van Acker, T.; Jia, X.; Cheng, H.; Fiebig, J.; Fourcade, T.; Snoeck, C.; Claeys, P. (2024). A new insight of the MIS 3 Dansgaard-Oeschger climate oscillations in western Europe from the study of a Belgium isotopically equilibrated speleothem, in: EGU General Assembly 2024. Vienna, Austria & Online, 14-19 April 2024. pp. EGU24-8463. https://dx.doi.org/10.5194/egusphere-egu24-8463 In: (2024). EGU General Assembly 2024. Vienna, Austria & Online, 14-19 April 2024. European Geosciences Union: [s.l.]. , more |  |
| Available in | Authors | | Document type: Summary
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| Authors | | Top | - Peral, M., more
- Marchegiano, M., more
- Verheyden, S., more
- Goderis, S., more
- Van Helden, T., more
| - Vanhaecke, F., more
- Van Acker, T., more
- Jia, X.
- Cheng, H.
| - Fiebig, J.
- Fourcade, T.
- Snoeck, C., more
- Claeys, P., more
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| Abstract | The Marine Isotope Stage (MIS) 3 records abrupt transitions from cold stadial to temperate interstadial climate conditions, termed Dansgaard-Oeschger (DO) events. Reconstructing these rapid climate changes is crucial for documenting the prevailing climatic conditions in Europe. However, only few continental records are available to define the continental climatic responses to DO changes. Here, the elemental and stable isotope compositions of a flowstone speleothem in Belgium covering the MIS 3 are documented. This speleothem precipitated under equilibrium conditions based on Δ48 thermometry, allowing the use of Δ47 thermometry with confidence. The acquired unique thermometry paleoclimatic dataset enables the reconstruction of temperature based on the hydrological information (oxygen-18 of drip water; δ18Ow) and sheds new light on the DO climate variations. A temperature differential of ~7°C is associated with alternating temperate warm and wet Interstadials to cold and dry stadials. The DO-12 is the most pronounced MIS 3 interstadial in the record and appears to be marked by a delay of 1000 years between climate enhancement (warmer temperature) and water availability (moisture increase). By combining our speleothem record with other continental and marine archive, the spatial variability of DO changes in western Europe during the MIS 3 is defined. A gradual climate deterioration with colder and drier conditions, associated with the Heinrich 4 event, progressed southwards through Europe. Interestngly, this spatial climatic degradation occured during the last phase of Neanderthal populations occupation in Europe. Our data provides better understanding on proxy interpretation thanks to our clumped isotope measurement but also on environmental constraints for human mobility models. |
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