Arctic sea-ice extent and volume are declining rapidly. Several studies project that the Arctic
Ocean may become seasonally ice-free by the year 2040 or even earlier. Putting this into …

Over a period of the past 15–20 years, the Russian Government implemented the Arctic
Mega Project for geological and comprehensive study of the Arctic Ocean. In this paper we …

Cenozoic biostratigraphic, cosmogenic isotope, magnetostratigraphic, and cyclostratigraphic
data derived from Integrated Ocean Drilling Program Expedition 302, the Arctic Coring …

Deep-water formation in the northern North Atlantic Ocean and the Arctic Ocean is a key
driver of the global thermohaline circulation and hence also of global climate. Deciphering …

We reconstruct eustatic variations during the latest Paleocene and earliest Eocene (∼ 58–
52 Ma). Dinoflagellate cysts, grain size fractions, and organic biomarkers in marine sections …

The Palaeocene–Eocene Thermal Maximum (PETM;∼ 55.5 Ma) is a geologically relatively
brief episode of extreme warmth. Both deep and surface ocean temperatures increased by …

The Cenozoic ice‐rafted debris (IRD) history of the central Arctic is reconstructed utilizing the
terrigenous coarse sand fraction in IODP 302 cores from 0 to 273 meters composite depth …

During the Arctic Coring Expedition (ACEX), a 428‐m‐thick sequence of Upper Cretaceous
to Quaternary sediments was penetrated. The mineralogical composition of the upper 300 m …

We present inorganic geochemical analyses of pore waters and sediments of two Late
Quaternary sediment cores from the western Arctic Ocean (southern Mendeleev Ridge, RV …

Despite its importance in the global climate system, age‐calibrated marine geologic records
reflecting the evolution of glacial cycles through the Pleistocene are largely absent from the …