Carbon Cycling Processes Of Inland Waters are Important to Understanding Climate Change
In a paper titled "The Boundless Carbon Cycle," published in the September issue of Nature Geoscience, scientists from the University of Vienna, Uppsala University in Sweden, University of Antwerp, and the U.S. based Stroud™ Water Research Center argue that current international strategies to mitigate manmade carbon emissions and address climate change have overlooked a critical player - inland waters. Streams, rivers, lakes, reservoirs, and wetlands play an important role in the carbon cycle that is unaccounted for in conventional carbon cycling models.
The team of scientists points out that all current global carbon models consider inland waters static conduits that transfer carbon from the continents to the oceans. In reality, inland waters are dynamic ecosystems with the potential to alter the fates of terrestrial carbon delivered to them including: burial in sediments leading to long-term storage or sequestration; and metabolism in rivers and subsequent outgassing of respired carbon dioxide to the atmosphere.
"Twenty percent of the continental carbon sequestration actually occurs as burial in inland water sediments," said Dr. Lars Tranvik, Professor of Limnology at Uppsala University in Sweden.
"River outgassing of respired carbon, contributes carbon to the atmosphere in an amount equivalent to 13% of annual fossil fuel burning," said Dr. Anthony K. Aufdenkampe, a scientist at the Stroud Water Research Center. Because the amount of atmospheric carbon is well known and conservation of matter requires a balanced global carbon budget, this previously unaccounted for source of carbon to the atmosphere implies the existence of an additional continental carbon sink such as higher rates of biomass accrual in forests. "A larger accumulation of carbon in forest ecosystems that could offset the outgassing from rivers would be more consistent with current independently-derived estimates of carbon sequestration on the continents," said Dr. Sebastian Luyssaert of the department of Biology at University of Antwerp in Belgium.
Article continues: http://www.sciencedaily.com/releases/2009/09/090901143313.htm