Dataset - B2FIND

Diversity indices across the Drake Passage from CTD stations during POLARSTER...

This dataset has no description

North Atlantic (Rockall Plateau) coccolith assemblage data for MIS 5 of ODP H...

Calcareous nannoplankton analyses on late quaternary sediments from the eastern North Atlantic ODP Site 980 (55°29'N, 14°42'W) provide detailed insight into palaeoceanographic...

Benthic macrofauna abundance in surface sediment of core PLG93_BCORE7

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Benthic macrofauna abundance in surface sediment of core PLG93_BCORE6

This dataset has no description

Benthic macrofauna abundance in surface sediment of core PLG93_BCORE3

This dataset has no description

Benthic macrofauna abundance in surface sediment of core PLG93_BCORE2

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Benthic macrofauna abundance in surface sediment of core PLG93_BCORE1

This dataset has no description

Freshwater ostracod abundance in different water bodies from a polygonal tund...

Patterned ground of the polygonal tundra yields sensitive indicators of environmental and climate change. Polygon ponds, mires and cryosoils are typical components of Arctic...

Rhizopoda of sediment core PG-Kit-64

Analysed by Anatoly A Bobrov

Ostracoda of sediment core PG-Kit-64

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Drake passage benthic foraminiferal abundance during the last deglaciation

The Antarctic Cold Reversal (ACR; 14.7 to 13 ka) phase of the last deglaciation saw a pause in the rise of atmospheric pCO2 and Antarctic temperature, contrasted with warming in...

Plant macrofossil records from permafrost deposits of the Bykovsky Peninsula ...

Plant macrofossils from the Mamontovy Khayata permafrost sequence on the Bykovsky Peninsula reflect climate and plant biodiversity in west Beringia during the last cold stage....

Distribution and functional traits of polychaetes in a CO2 vent system: winne...

We report on fine taxonomic and functional analyses of polychaetes associated with rocky reefs along a gradient of ocean acidification (OA) at the volcanic CO2 vent system off...

Palynological analyses of the sediments around the Miocene/Pliocene boundary ...

The late Neogene evolution of the Arctic to Subarctic region is poorly understood due to few available records and poor age control. At the margin of the Arctic Ocean, Yermak...