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History
- March 16, 2021.
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The copyright holder for this preprint is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under a CC-BY-NC 4.0 International license.
Author Information
- 1Department of Geobiology, Geoscience Center, Georg-August-Universität Göttingen, Goldschmidtstr. 3 37077 Göttingen, Germany
- 2Sedimentology & Organic Geochemistry Group, Department of Geosciences, Eberhard-Karls-University Tübingen, Schnarrenbergstr. 94-96 72076 Tübingen, Germany
- 3Department of Sedimentology and Environmental Geology, Geoscience Center, Georg-August-Universität Göttingen, Goldschmidtstr. 3 37077 Göttingen, Germany
- 4State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, 39 East Beijing Road, 210008 Nanjing, China
- 5Department of Geobiology, Geoscience Center, Georg-August-Universität Göttingen, Goldschmidtstr. 3 37077 Göttingen, Germany; ‘Origin of Life’ Group, Göttingen Academy of Sciences and Humanities, Theater Str. 7 37077 Göttingen, Germany
- ↵*Corresponding author; email: jreitne{at}gwdg.de
Posted March 16, 2021.
Late Anisian microbe-metazoan build-ups (“stromatolites”) in the Germanic Basin – aftermath of the Permian – Triassic Crisis
