Alfred Wegener Institute, Helmholtz Centre for Polar and Marine
Research, Polar Terrestrial Environmental Systems, Telegrafenberg A45, 14473
Potsdam, Germany
Amy Forster
Alfred Wegener Institute, Helmholtz Centre for Polar and Marine
Research, Polar Terrestrial Environmental Systems, Telegrafenberg A45, 14473
Potsdam, Germany
Institute for Biochemistry and Biology, University of Potsdam, 14469
Potsdam, Germany
Alfred Wegener Institute, Helmholtz Centre for Polar and Marine
Research, Polar Terrestrial Environmental Systems, Telegrafenberg A45, 14473
Potsdam, Germany
Institute of Geosciences, University of Potsdam, 14469 Potsdam,
Germany
Lyudmila A. Pestryakova
Institute of Natural Sciences, North-Eastern Federal University of Yakutsk, 677000 Sakha Republic,
Russia
Alfred Wegener Institute, Helmholtz Centre for Polar and Marine
Research, Polar Terrestrial Environmental Systems, Telegrafenberg A45, 14473
Potsdam, Germany
Alfred Wegener Institute, Helmholtz Centre for Polar and Marine
Research, Permafrost Research, 14473 Potsdam, Germany
Tim Kröger
Alfred Wegener Institute, Helmholtz Centre for Polar and Marine
Research, Polar Terrestrial Environmental Systems, Telegrafenberg A45, 14473
Potsdam, Germany
Institute of Geodesy and Geoinformation Science, Technische Universität Berlin, 10623 Berlin, Germany
Ulrike Herzschuh
Alfred Wegener Institute, Helmholtz Centre for Polar and Marine
Research, Polar Terrestrial Environmental Systems, Telegrafenberg A45, 14473
Potsdam, Germany
Institute for Biochemistry and Biology, University of Potsdam, 14469
Potsdam, Germany
Institute of Environmental Science and
Geography, University of Potsdam, 14469 Potsdam, Germany
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Lake sediment from the Russian Arctic was studied for microalgae and organic matter chemistry dated back to the last glacial 28 000 years. Species and chemistry responded to environmental changes such as the Younger Dryas cold event and the Holocene thermal maximum. Organic carbon accumulation correlated with rates of microalgae deposition only during warm episodes but not during the cold glacial.
Lake sediment from the Russian Arctic was studied for microalgae and organic matter chemistry...
