Streams and rivers can substantially modify organic carbon (OC) inputs from terrestrial
landscapes, and much of this processing is the result of microbial respiration. While carbon …

Many freshwater systems receive substantial inputs of terrestrial organic matter. Terrestrially
derived dissolved organic carbon (t‐DOC) inputs can modify light availability, the spatial …

Collectively, reservoirs created by dams are thought to be an important source of
greenhouse gases (GHGs) to the atmosphere. So far, efforts to quantify, model, and manage …

Lakes and impoundments are important sources of greenhouse gases (GHG: ie, CO2, CH4,
N2O), yet global emission estimates are based on regionally biased averages and …

Burial in sediments removes organic carbon (OC) from the short-term biosphere-atmosphere
carbon (C) cycle, and therefore prevents greenhouse gas production in natural systems …

Dissolved organic matter (DOM) is recognized for its importance in freshwater ecosystems,
but historical reliance on DOM quantity rather than indicators of DOM composition has led to …

Large reservoirs are hotspots for carbon emissions, and the continued input and
decomposition of terrestrial dissolved organic matter (DOM) from upstream catchments is an …

Eutrophic lakes, especially shallow eutrophic lakes, disproportionately contribute to
greenhouse gas (GHG) emissions. To investigate the effects of eutrophication on GHG …

Methane (CH4) strongly contributes to observed global warming. As natural CH4 emissions
mainly originate from wet ecosystems, it is important to unravel how climate change may …

Lakes and ponds are important natural sources of the potent greenhouse gas methane
(CH4), with small shallow waters identified as particular hotspots,. Ebullition (bubbles) of …