Carbon storage by the ocean and by the land is usually quantified separately, and does not
fully take into account the land-to-ocean transport of carbon through inland waters …

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 …

Northern peatlands have accumulated large stocks of organic carbon (C) and nitrogen (N),
but their spatial distribution and vulnerability to climate warming remain uncertain. Here, we …

Globally, inland waters receive a significant but ill‐defined quantity of terrestrial carbon (C).
When summed, the contemporary estimates for the three possible fates of C in inland waters …

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 Arctic is a water-rich region, with freshwater systems covering about 16% of the northern
permafrost landscape. Permafrost thaw creates new freshwater ecosystems, while at the …

CO2 evasion from rivers (FCO2) is an important component of the global carbon budget.
Here we present the first global maps of CO2 partial pressures (pCO2) in rivers of stream …

Inland water ecosystems dynamically process, transport, and sequester carbon. However,
the transport of carbon through aquatic environments has not been quantitatively integrated …

Northern permafrost soils store a vast reservoir of carbon, nearly twice that of the present
atmosphere. Current and projected climate warming threatens widespread thaw of these …

As Arctic regions warm and frozen soils thaw, the large organic carbon pool stored in
permafrost becomes increasingly vulnerable to decomposition or transport. The transfer of …