Articles | Volume 10, issue 2
https://doi.org/10.5194/bg-10-1193-2013
https://doi.org/10.5194/bg-10-1193-2013
Research article
 | 
25 Feb 2013
Research article |  | 25 Feb 2013

Warming increases carbon and nutrient fluxes from sediments in streams across land use

S.-W. Duan and S. S. Kaushal

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Cited articles

Aguilar, L. and Thibodeaux, L. J.: Kinetics of peat soil dissolved organic carbon release from bed sediment to water, Part 1, Laboratory simulation, Chemosphere, 58, 1309–1318, 2005.
Alexander, R. A., Smith, R. B., and Schwarz, G. E.: Effect of stream channel size on the delivery of nitrogen to the Gulf of Mexico, Nature, 403, 758–761, https://doi.org/10.1038/35001562, 2000.
Andersson, S., Nilsson, S. I., and Saetre, P.: Leaching of dissolved organic carbon (DOC) and dissolved organic nitrogen (DON) in mor humus as affected by temperature and pH, Soil Biol. Biochem., 32, 1–10, https://doi.org/10.1016/S0038-0717(99)00103-0, 2000.
Arango, C. P., Tank, L. J. L., Johnson, T., and Hamilton, S. K.: Assimilatory uptake rather than nitrification and denitrification determines nitrogen removal patterns in streams of varying land use, Limnol. Oceanogr., 53, 2558–2572, 2008.
Arnosti, C., Jørgensen, B. B., Sagemann, J., and Thamdrup, B.: Temperature dependence of microbial degradation of organic matter in marine sediments: polysaccharide hydrolysis, oxygen consumption, and sulfate reduction, Mar. Ecol.-Prog. Ser., 165, 59–70, https://doi.org/10.3354/meps165059, 1998.
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