Carbon geochemistry of plankton-dominated samples in the Laptev and East Siberian shelves: contrasts in suspended particle composition

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Carbon geochemistry of plankton-dominated samples in the Laptev and East Siberian shelves: contrasts in suspended particle composition

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im September 2017 veröffentlichter wissenschaftlicher Artikel

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wetenschappelijk artikel

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наукова стаття, опублікована у вересні 2017

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Carbon geochemistry of plankto ...... suspended particle composition

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Carbon geochemistry of plankto ...... suspended particle composition

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Carbon geochemistry of plankto ...... suspended particle composition

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Carbon geochemistry of plankto ...... suspended particle composition

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Carbon geochemistry of plankto ...... suspended particle composition

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Carbon geochemistry of plankto ...... suspended particle composition

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Carbon geochemistry of plankto ...... suspended particle composition

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Elena Panova

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Emma Karlsson

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Igor Semiletov

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Joan A. Salvado

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Jorien E. Vonk

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Lisa Bröder

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Marc C. Geibel

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Martin Kruså

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P2860

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Massive remobilization of permafrost carbon during post-glacial warming

Activation of old carbon by erosion of coastal and subsea permafrost in Arctic Siberia.

Pan-Arctic distributions of continental runoff in the Arctic Ocean

Observations of the PCB distribution within and in-between ice, snow, ice-rafted debris, ice-interstitial water, and seawater in the Barents Sea marginal ice zone and the North Pole area.

Increased freshwater discharge shifts the trophic balance in the coastal zone of the northern Baltic Sea.

The role of sea ice and other fresh water in the Arctic circulation

The importance of ice algae-produced carbon in the central Arctic Ocean ecosystem: Food web relationships revealed by lipid and stable isotope analyses

Dependence of phytoplankton carbon isotopic composition on growth rate and [CO2)aq: Theoretical considerations and experimental results

Effect of Phytoplankton Cell Geometry on Carbon Isotopic Fractionation

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735-748

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scholarly article

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10.5194/OS-13-735-2017

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2017-09-18T00:00:00Z

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