Journal cover Journal topic
Biogeosciences An interactive open-access journal of the European Geosciences Union
Journal topic
Volume 2, issue 1
Biogeosciences, 2, 15–26, 2005
© Author(s) 2005. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.
Biogeosciences, 2, 15–26, 2005
© Author(s) 2005. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.

  17 Feb 2005

17 Feb 2005

The carbon budget of terrestrial ecosystems at country-scale – a European case study

I. A. Janssens1, A. Freibauer2, B. Schlamadinger3, R. Ceulemans1, P. Ciais4, A. J. Dolman5, M. Heimann2, G.-J. Nabuurs6,7, P. Smith8, R. Valentini9, and E.-D. Schulze2 I. A. Janssens et al.
  • 1Department of Biology, Universiteit Antwerpen, Belgium
  • 2Max-Planck-Institute for Biogeochemistry, Jena, Germany
  • 3Joanneum Research, Graz, Austria
  • 4Laboratoire des Sciences du Climat et de l’Environnement, Gif sur Yvette, France
  • 5Department of Geo-Environmental Sciences, Free University Amsterdam, The Netherlands
  • 6Alterra, Wageningen, The Netherlands
  • 7European Forest Institute, Joensuu, Finland
  • 8School of Biological Sciences, University of Aberdeen, UK
  • 9Department of Forest Science and Environment, University of Tuscia, Italy

Abstract. We summed estimates of the carbon balance of forests, grasslands, arable lands and peatlands to obtain country-specific estimates of the terrestrial carbon balance during the 1990s. Forests and grasslands were a net sink for carbon, whereas croplands were carbon sources in all European countries. Hence, countries dominated by arable lands tended to be losing carbon from their terrestrial ecosystems, whereas forest-dominated countries tended to be sequestering carbon. In some countries, draining and extraction of peatlands caused substantial reductions in the net carbon balance.

Net terrestrial carbon balances were typically an order of magnitude smaller than the fossil fuel-related carbon emissions. Exceptions to this overall picture were countries where population density and industrialization are small. It is, however, of utmost importance to acknowledge that the typically small net carbon balance represents the small difference between two large but opposing fluxes: uptake by forests and grasslands and losses from arable lands and peatlands. This suggests that relatively small changes in either or both of these large component fluxes could induce large effects on the net total, indicating that mitigation schemes should not be discarded a priori.

In the absence of carbon-oriented land management, the current net carbon uptake is bound to decline soon. Protecting it will require actions at three levels; a) maintaining the current sink activity of forests, b) altered agricultural management practices to reduce the emissions from arable soils or turn into carbon sinks and c) protecting current large reservoirs (wetlands and old forests), since carbon is lost more rapidly than sequestered.

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