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Role of lakes for organic carbon cycling in the boreal zone

Algesten, Grete, Sobek, Sebastian, Bergström, Ann‐Kristin, Ågren, Anneli, Tranvik, Lars J., Jansson, Mats·2004·Global Change Biology

Abstract

We calculated the carbon loss (mineralization plus sedimentation) and net CO 2 escape to the atmosphere for 79 536 lakes and total running water in 21 major Scandinavian catchments (size range 437–48 263 km 2). Between 30% and 80% of the total organic carbon that entered the freshwater ecosystems was lost in lakes. Mineralization in lakes and subsequent CO 2 emission to the atmosphere was by far the most important carbon loss process. The withdrawal capacity of lakes on the catchment scale was closely correlated to the mean residence time of surface water in the catchment, and to some extent to the annual mean temperature represented by latitude. This result implies that variation of the hydrology can be a more important determinant of CO 2 emission from lakes than temperature fluctuations. Mineralization of terrestrially derived organic carbon in lakes is an important regulator of organic carbon export to the sea and may affect the net exchange of CO 2 between the atmosphere and the boreal landscape.

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Metadata

Authors
Algesten, G., Sobek, S., Bergström, A., Ågren, A., Tranvik, L. J., & Jansson, M.
Venue
Global Change Biology
Publisher
Wiley
Published
2003-12-15
Volume
10
Issue
1
Pages
141-147
ISSN
  • 1354-1013 (ISSN-L)
  • 1365-2486
OpenAlex
W2147013329
Cited by
343
References
0
FWCI
8.22
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Role of lakes for organic carbon cycling in the boreal zone. https://app.cochat.ai/papers/10.1111/j.1365-2486.2003.00721.x
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Algesten, G., Sobek, S., Bergström, A., Ågren, A., Tranvik, L. J., & Jansson, M. (2004). Role of lakes for organic carbon cycling in the boreal zone. Global Change Biology. https://doi.org/10.1111/j.1365-2486.2003.00721.x

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Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.