Measurements of the production and consumption of organic material have been a focus of
aquatic science for more than 80 years. Over the last century, a variety of approaches have …

The retention of peatland carbon (C) and the ability to continue to draw down and store C
from the atmosphere is not only important for the UK terrestrial carbon inventory, but also for …

Carbon dioxide (CO2) transfer from inland waters to the atmosphere, known as CO2
evasion, is a component of the global carbon cycle. Global estimates of CO2 evasion have …

The eutrophication of lowland lakes in Europe by excess nitrogen (N) and phosphorus (P) is
severe because of the long history of land‐cover change and agricultural intensification. The …

Evasion of gaseous carbon (C) from streams is often poorly quantified in landscape C
budgets. Even though the potential importance of the capillary network of streams as C …

Peatland streams have repeatedly been shown to be highly supersaturated in both CO2 and
CH4 with respect to the atmosphere, and in combination with dissolved (DOC) and …

Accounting for greenhouse gas (GHG) emissions and removals in managed ecosystems
has generally focused on direct land–atmosphere fluxes, but in peatlands a significant …

Boreal ecosystems store significant quantities of organic carbon (C) that may be vulnerable
to degradation as a result of a warming climate. Despite their limited coverage on the …

We tested the hypothesis that CO2 supersaturation along the aquatic conduit over Sweden
can be explained by processes other than aquatic respiration. A first generalized‐additive …

The development of complete regional carbon (C) budgets for different biomes is an integral
step in the effort to predict global response and potential feedbacks to a changing climate …