Authors: Zeng, Lingqi, Ruge, Dag B., Berger, Günther, Heck, Karin, Hölzl, Stefan, Reimer, Andreas, Jung, Dietmar, Arp, Gernot, Lingqi; 1Georg‐August‐Universität Göttingen Geowissenschaftliches Zentrum, Goldschmidtstrasse 3 Göttingen 37077 Germany, Dag B.; 1Georg‐August‐Universität Göttingen Geowissenschaftliches Zentrum, Günther; 2 Sudetenstraße 6 Pleinfeld Germany, Karin; 3Staatliche Naturwissenschaftliche Sammlungen Bayerns ‐ RiesKraterMuseum Nördlingen Eugene‐Shoemaker‐Platz 1 Nördlingen 86720 Germany, Stefan; 3Staatliche Naturwissenschaftliche Sammlungen Bayerns ‐ RiesKraterMuseum Nördlingen Eugene‐Shoemaker‐Platz 1 Nördlingen 86720 Germany, Andreas; 1Georg‐August‐Universität Göttingen Geowissenschaftliches Zentrum, Dietmar; 4Bayerisches Landesamt für Umwelt Geologischer Dienst, Hans‐Högn‐Straße 12 Hof/Saale 95030 Germany, Gernot; 1Georg‐August‐Universität Göttingen Geowissenschaftliches Zentrum
Venue: Sedimentology
Type: Publication
Abstract: Abstract The identification and distinction of fluvial from lacustrine deposits and the recognition of catchment changes are crucial for the reconstruction of climate changes in terrestrial environments. The investigated drill core succession shows a general evolution from red–brown claystones to white–grey marlstones and microcrystalline limestones, which all have previously been considered as relict deposits of an impact ejecta‐dammed lake, falling within the mid‐Miocene Climate Transition. However, recent mammal biostratigraphic dati...
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Topics: 
Paleontology
Geochemistry
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