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Palynology of sediment cores from site GS15-198-38
This dataset has no description
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Late Miocene and Pliocene dinoflagellate cysts, acritarchs and terrestrial pa...
The globally warm climate of the early Pliocene gradually cooled from 4 million years ago, synchronous with decreasing atmospheric CO2 concentrations. In contrast,... -
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...
