| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6350680 | Palaeogeography, Palaeoclimatology, Palaeoecology | 2011 | 22 Pages |
Abstract
The study results indicate a continuous fluvial sedimentation environment for the Laptev Sea shelf in the region of the second Lena Delta terrace during the late Pleistocene, and confirm the presence of a dynamic channel system of the paleo-Lena River that flowed at the same time as the nearby subaerial Ice Complex deposits were being formed.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Lutz Schirrmeister, Guido Grosse, Moritz Schnelle, Margret Fuchs, Matthias Krbetschek, Mathias Ulrich, Viktor Kunitsky, Mikhail Grigoriev, Andrei Andreev, Frank Kienast, Hanno Meyer, Olga Babiy, Irina Klimova, Anatoly Bobrov, Sebastian Wetterich,