Tropical wet season runoff mobilises younger carbon in rainforest streams but older carbon in agricultural streams
Clément Duvert,Vanessa Solano,Dioni I. Cendón,Francesco Ulloa-Cedamanos,Liza K. McDonough,Robert G. M. Spencer,Niels C. Munksgaard,Lindsay B. Hutley,Jean-Sébastien Moquet,and David E. Butman
Research Institute for the Environment and Livelihoods, Charles Darwin University, Darwin, NT, Australia
College of Science and Engineering, James Cook University, Cairns, QLD, Australia
Vanessa Solano
Research Institute for the Environment and Livelihoods, Charles Darwin University, Darwin, NT, Australia
now at: Groupe de Recherche Interuniversitaire en Limnologie, Département des Sciences Biologiques, Université du Québec à Montréal, Montréal, QC, Canada
Australian Nuclear Science and Technology Organisation, Lucas Heights, NSW, Australia
School of Biological, Earth and Environmental Sciences, UNSW Sydney, Sydney, NSW, Australia
Robert G. M. Spencer
National High Magnetic Field Laboratory Geochemistry Group, Department of Earth, Ocean, and Atmospheric Science, Florida State University, Tallahassee, FL, USA
Niels C. Munksgaard
College of Science and Engineering, James Cook University, Cairns, QLD, Australia
This study examines the age and composition of carbon in tropical streams. We find that dissolved organic carbon (DOC) is centuries to millennia old, while dissolved inorganic carbon (DIC) is consistently younger, indicating a decoupling between the two. DOC age varies seasonally, with rainforest streams exporting younger DOC during high flow, while agricultural streams mobilise older DOC. Our results suggest land conversion alters carbon export, potentially worsening with climate change.
This study examines the age and composition of carbon in tropical streams. We find that...