Geological and geomorphological evolution of a sedimentary periglacial landscape in Northeast Siberia during the Late Quaternary

Author:

Grosse Guido,Schirrmeister Lutz,Siegert Christine,Kunitsky Viktor V.,Slagoda Elena A.,Andreev Andrei A.,Dereviagyn Alexander Y.

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference67 articles.

1. Paleoenvironmental changes in north-eastern Siberia during the Late Quaternary — evidence from pollen records of the Bykovsky Peninsula;Andreev;Polarforschung,2002

2. Chronology of the Holocene transgression at the North Siberian margin;Bauch;Global and Planetary Change,2001

3. Insolation values for the climate of the last 10 million years;Berger;Quaternary Science Reviews,1991

4. Testate amoebae (Protozoa: Testacealobosea and Testaceafilosea) as bioindicators in the Late Quaternary deposits of the Bykovsky Peninsula, Laptev Sea, Russia;Bobrov;Palaeogeography, Palaeoclimatology, Palaeoecology,2004

5. Evidence for general instability of past climate from a 250-kyr ice-core record;Dansgaard;Nature,1993

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