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10 million years of interaction between terrestrial plant biodiversity and climate in the early Paleogene of the Helmstedt Mining District

Subject Area Geology
Term from 2017 to 2024
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 394329649
 
Final Report Year 2024

Final Report Abstract

The more than 200 m thick Paleogene succession of the former Helmstedt Lignite Mining District in northern Germany was situated in an estuary at the southern edge of the proto-North Sea. It includes the late Paleocene to lower Eocene Schöningen Formation and the middle Eocene Helmstedt Formation with about 13 lignite seams of up to 15 m thickness. The succession is covering the entire Paleogene greenhouse phase and its gentle demise almost continuously from the latest Paleocene to the middle Eocene, including the Early Eocene Climatic Optimum (EECO) and its steady but slow decline, the transition to the Middle Eocene Climatic Optimum (MECO) and some short-term warming events such as, e.g., the Paleocene-Eocene Thermal Maximum (PETM). Due to the interaction between changes in sea level, salt withdrawal in the underground and climate-related changes in runoff from the hinterland the area was subject to frequent changes between marine and terrestrial conditions, including peat formation. This nearly continuous section allows to trace the effects of long-term changes and short-term perturbations of the climate on the diversity and composition of plant communities across 10 million years during the last natural greenhouse phase by making use of pollen and spores as proxies and applying modern multivariate and biodiversity statistics to an extraordinary section.

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