A chironomid-based reconstruction of late glacial summer temperatures in the southern Carpathians (Romania) |
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| Authors: | Mónika Tóth Enikő K Magyari Stephen J Brooks Mihály Braun Krisztina Buczkó Miklós Bálint Oliver Heiri |
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| Institution: | 1. Hungarian Academy of Sciences, Balaton Limnological Research Institute, Klebelsberg Kuno 3, HU-8237 Tihany, Hungary;2. HAS-NHMUS Research group for Paleontology, HU-1476 Budapest, P.O. Box 222, Hungary;3. Department of Entomology, The Natural History Museum, Cromwell Road, London SW7 5BD, UK;4. University of Debrecen, Department of Inorganic and Analytical Chemistry, HU-4010 Debrecen, P.O. Box 21, Hungary;5. Department of Botany, Hungarian Natural History Museum, HU-1476 Budapest, P.O. Box 222, Hungary;6. Biodiversität und Klima Forschungszentrum (BiK-F), Senckenberganlage 25, D-60325 Frankfurt am Main, Germany;7. Molecular Biology Center, Babe?-Bolyai University, Treboniu Laurian 42, 400271 Cluj, Romania;8. Institute of Environmental Biology, Utrecht University, Budapestlaan 4, CD-3584 Utrecht, The Netherlands;9. Institute of Plant Sciences and Oeschger Centre for Climate Change Research, University of Bern, Altenbergrain 21, CH-3013 Bern, Switzerland |
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| Abstract: | Late glacial and early Holocene summer temperatures were reconstructed based on fossil chironomid assemblages at Lake Brazi (Retezat Mountains) with a joint Norwegian–Swiss transfer function, providing an important addition to the late glacial quantitative climate reconstructions from Europe. The pattern of the late glacial temperature changes in Lake Brazi show both similarities and some differences from the NGRIP δ18O record and other European chironomid-based reconstructions. Our reconstruction indicates that at Lake Brazi (1740 m a.s.l.) summer air temperature increased by ~ 2.8°C at the Oldest Dryas/Bølling transition (GS-2/GI-1) and reached 8.1–8.7°C during the late glacial interstade. The onset of the Younger Dryas (GS-1) was characterized by a weak (< 1°C) decrease in chironomid-inferred temperatures. Similarly, at the GS-1/Holocene transition no major changes in summer temperature were recorded. In the early Holocene, summer temperature increased in two steps and reached ~ 12.0–13.3°C during the Preboreal. Two short-term cold events were detected during the early Holocene between 11,480–11,390 and 10,350–10,190 cal yr BP. The first cooling coincides with the Preboreal oscillation and shows a weak (0.7°C) temperature decrease, while the second is characterized by 1°C cooling. Both cold events coincide with cooling events in the Greenland ice core records and other European temperature reconstructions. |
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