Peatlands are carbon‐rich ecosystems that cover 185–423 million hectares (Mha) of the
earth's surface. The majority of the world's peatlands are in temperate and boreal zones …

The carbon balance of peatlands is predicted to shift from a sink to a source this century.
However, peatland ecosystems are still omitted from the main Earth system models that are …

Tropical forests are complex systems containing myriad interactions and feedbacks with
their biotic and abiotic environments, but as the world changes fast, the future of these …

Soil organic carbon (SOC) changes under future climate warming are difficult to quantify in
situ. Here we apply an innovative approach combining space-for-time substitution with meta …

Concerns are increasingly raised over the centrality of carbon removal in climate policy,
particularly in the guise of 'net-zero'targets. Most significantly perhaps, treating emissions …

Tropical peatlands are among the most carbon-dense ecosystems but land-use change has
led to the loss of large peatland areas, associated with substantial greenhouse gas …

Nonstructural carbohydrates (NSCs) facilitate the adaptation of trees to drought stress. There
have been a large number of studies exploring NSC changes in individual plant species and …

Tropical peatlands are threatened by climate change and land-use changes, but there
remain substantial uncertainties about their present and future role in the global carbon …

Dissolved organic matter (DOM) in groundwater is fundamentally important with respect to
biogeochemical reactions, global carbon cycling, heavy metal transport, water treatability …

The left must confront the politics of removing carbon from the atmosphere–a topic rapidly
making its way to the top of the climate agenda. We here examine the technology of direct …