Nature Communications (Apr 2020)
East Siberian Arctic inland waters emit mostly contemporary carbon
- Joshua F. Dean,
- Ove H. Meisel,
- Melanie Martyn Rosco,
- Luca Belelli Marchesini,
- Mark H. Garnett,
- Henk Lenderink,
- Richard van Logtestijn,
- Alberto V. Borges,
- Steven Bouillon,
- Thibault Lambert,
- Thomas Röckmann,
- Trofim Maximov,
- Roman Petrov,
- Sergei Karsanaev,
- Rien Aerts,
- Jacobus van Huissteden,
- Jorien E. Vonk,
- A. Johannes Dolman
Affiliations
- Joshua F. Dean
- Department of Earth Sciences, Vrije Universiteit Amsterdam
- Ove H. Meisel
- Department of Earth Sciences, Vrije Universiteit Amsterdam
- Melanie Martyn Rosco
- Department of Earth Sciences, Vrije Universiteit Amsterdam
- Luca Belelli Marchesini
- Department of Sustainable Agro-ecosystems and Bioresources, Research and Innovation Centre, Fondazione Edmund Mach
- Mark H. Garnett
- Natural Environment Research Council Radiocarbon Facility
- Henk Lenderink
- Department of Earth Sciences, Vrije Universiteit Amsterdam
- Richard van Logtestijn
- Department of Ecological Sciences, Vrije Universiteit Amsterdam
- Alberto V. Borges
- Chemical Oceanography Unit, University of Liège
- Steven Bouillon
- Department of Earth and Environmental Science, Katholieke Universiteit Leuven
- Thibault Lambert
- Chemical Oceanography Unit, University of Liège
- Thomas Röckmann
- Institute for Marine and Atmospheric Research, Utrecht University
- Trofim Maximov
- Institute for Biological Problems of the Cryolithozone, Siberian Branch Russian Academy of Sciences
- Roman Petrov
- Institute for Biological Problems of the Cryolithozone, Siberian Branch Russian Academy of Sciences
- Sergei Karsanaev
- Institute for Biological Problems of the Cryolithozone, Siberian Branch Russian Academy of Sciences
- Rien Aerts
- Department of Ecological Sciences, Vrije Universiteit Amsterdam
- Jacobus van Huissteden
- Department of Earth Sciences, Vrije Universiteit Amsterdam
- Jorien E. Vonk
- Department of Earth Sciences, Vrije Universiteit Amsterdam
- A. Johannes Dolman
- Department of Earth Sciences, Vrije Universiteit Amsterdam
- DOI
- https://doi.org/10.1038/s41467-020-15511-6
- Journal volume & issue
-
Vol. 11,
no. 1
pp. 1 – 10
Abstract
The release of ancient carbon from thawing permafrost is thought to have an important impact on global biogeochemistry through positive feedbacks. Here Dean and colleagues show that in Siberian permafrost, warming could liberate more contemporary carbon relative to aged counterparts.
