Articles | Volume 20, issue 1
https://doi.org/10.5194/bg-20-271-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-20-271-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Contrasts in dissolved, particulate, and sedimentary organic carbon from the Kolyma River to the East Siberian Shelf
Department of Earth Sciences, Vrije Universiteit, Amsterdam, the
Netherlands
Lisa Bröder
Department of Earth Sciences, Vrije Universiteit, Amsterdam, the
Netherlands
Geological Institute, Swiss Federal Institute of Technology,
Zürich, Switzerland
Tommaso Tesi
Institute of Polar Sciences, National Research Council, Bologna,
Italy
Kirsi H. Keskitalo
Department of Earth Sciences, Vrije Universiteit, Amsterdam, the
Netherlands
Nikita Zimov
Pacific Geographical Institute, Far East Branch, Russian Academy of
Sciences, Northeast Science Station, Cherskiy, Russia
Anna Davydova
Pacific Geographical Institute, Far East Branch, Russian Academy of
Sciences, Northeast Science Station, Cherskiy, Russia
Philip Pika
Department of Earth Sciences, Vrije Universiteit, Amsterdam, the
Netherlands
Negar Haghipour
Geological Institute, Swiss Federal Institute of Technology,
Zürich, Switzerland
Timothy I. Eglinton
Geological Institute, Swiss Federal Institute of Technology,
Zürich, Switzerland
Jorien E. Vonk
CORRESPONDING AUTHOR
Department of Earth Sciences, Vrije Universiteit, Amsterdam, the
Netherlands
Data sets
The Circum-Arctic Sediment Carbon Database — CASCADE. Dataset version 2 Jannik Martens, Evgeny Romankevich, Igor Semiletov, Birgit Wild, Bart van Dongen, Jorien Vonk, Tommaso Tesi, Natalia Shakhova, Oleg V. Dudarev, Denis Kosmach, Alexander Vetrov, Leopold Lobkovsky, Nikolay Belyaev, Robie Macdonald, Anna J. Pieńkowski, Timothy I. Eglinton, Negar Haghipour, Salve Dahle, Michael L. Carroll, Emmelie K. L. Åström, Jacqueline M. Grebmeier, Lee W. Cooper, Göran Possnert, and Örjan Gustafsson https://doi.org/10.17043/cascade-2
Short summary
With this study, we want to highlight the importance of studying both land and ocean together, and water and sediment together, as these systems function as a continuum, and determine how organic carbon derived from permafrost is broken down and its effect on global warming. Although on the one hand it appears that organic carbon is removed from sediments along the pathway of transport from river to ocean, it also appears to remain relatively ‘fresh’, despite this removal and its very old age.
With this study, we want to highlight the importance of studying both land and ocean together,...
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