FastFind »   Lastname: doi:10.1029/ Year: Advanced Search  

AGU: Global Biogeochemical Cycles

 

Keywords

  • carbon dioxide
  • net ecosystem metabolism
  • dissolved organic carbon
  • temperature

Index Terms

  • Global Change: Biogeochemical cycles, processes, and modeling
  • Biogeosciences: Carbon cycling
  • Biogeosciences: Limnology
  • Global Change: Impacts of global change
Abstract
Cited By (21)
 

Abstract

Temperature independence of carbon dioxide supersaturation in global lakes

Sebastian Sobek

Limnology/Department of Ecology and Evolution, Uppsala University, Uppsala, Sweden

Lars J. Tranvik

Limnology/Department of Ecology and Evolution, Uppsala University, Uppsala, Sweden

Jonathan J. Cole

Institute of Ecosystem Studies, Milbrook, New York, USA

A growing body of evidence suggests that most of the world's lakes are supersaturated with CO2 and export significant amounts of CO2 to the atmosphere. Still, the temperature dependence of the partial pressure of CO2 (pCO2) in lakes, which is the main driver of carbon flux across the air-water interface, has not yet been assessed. Analyzing a global-scale database of 4902 lakes, we show that temperature is not an important regulator of pCO2 in lakes. Instead, the concentration of dissolved organic carbon (DOC), a substrate for microbial respiration, explains significant variation in lake pCO2. Contrary to what may be expected from the physiological constraints of temperature, effects of climate change on the carbon balance of lakes may not be due to rising temperature per se, but rather to climatically induced changes in the export of DOC from terrestrial soils to aquatic habitats.

Received 22 March 2004; accepted 18 February 2005; published 5 April 2005.

Citation: Sobek, S., L. J. Tranvik, and J. J. Cole (2005), Temperature independence of carbon dioxide supersaturation in global lakes, Global Biogeochem. Cycles, 19, GB2003, doi:10.1029/2004GB002264.

Cited By

Please wait one moment ...