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Multiple proxy analysis of lake sediment records are crucial for understanding changes in environmental and climate conditions over historical and geological time. Most recently, the use of biomarker ...
Until now, the lack of time-continuous, terrestrial paleoenvironmental data from the Pleistocene Arctic has made model simulations of past interglacials difficult to assess. Here, we compare climate s...
The closure of the Anyui oceanic basin is expressed in western Chukotka by Mesozoic terrigenous turbidite and fragments of both Paleozoic and Mesozoic ophiolite sequences, the South Anyui suture. Howe...

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