Foraminiferal stable isotopes and assemblages from Franz Victoria and St. Anna troughs
provide a valuable record of freshwater and Atlantic Water flows to the northern Barents and …

Publisher Summary Transfer functions, in a broad sense, are powerful methods that allow
complex biological assemblages analyzed by micropaleontologists to be translated into …

Distinct cyclicity in lithology and microfaunal distribution in sediment cores from the
Mendeleev Ridge in the western Arctic Ocean (water depths ca. 1.5 km) reflects contrasting …

Arctic paleoceanography and sea-ice history were reconstructed from epipelagic and
benthic ostracodes from a sediment core (HLY0503-06JPC, 800 m water depth) located on …

Paleo-sea-ice history in the Arctic Ocean was reconstructed using the sea-ice dwelling
ostracode Acetabulastoma arcticum from late Quaternary sediments from the Mendeleyev …

Analyses of benthic foraminifera in sediment cores taken at about 1000 m water depth at the
Yermak Plateau and the Barents Sea slope, adjacent to the position of the ice-sheet edge …

Oxygen isotope records of cores from the central Arctic Ocean yield evidence for a major
influx of meltwater at the beginning of the last deglaciation 15.7 thousand years ago (16,650 …

Late Quaternary ostracode assemblages from the North Atlantic Ocean were studied to
establish the effect of climatic changes of the past 210,000 yr (marine oxygen isotope stages …

The stratigraphic distributions of ostracodes and selected calcareous benthic and planktic
foraminiferal species were studied in sediment cores from~ 700 to 2700 m water depth on …

A high-resolution study including oxygen and carbon stable isotopes as well as carbonate
and total organic carbon contents, has been performed on undisturbed near-surface (0–40 …