Global climate is changing faster than humankind has ever experienced. Model-based
predictions of future climate are becoming more complex and precise, but they still lack …

Soils associated with wet and ephemerally wet environments, ie wet soils, cover an area
greater than 12.1 million km 2; inland wetlands deliver at least Int $27.0 trillion in tangible …

Northern peatlands are an integral part of the global carbon cycle—a strong sink of
atmospheric carbon dioxide and source of methane. Increasing anthropogenic carbon …

To evaluate boreal peatland C losses from warming, novel technologies were used to
expose intact bog plots in northern Minnesota to a range of future temperatures (+ 0° C to+ …

Sphagnum mosses are keystone components of peatland ecosystems. They facilitate the
accumulation of carbon in peat deposits, but climate change is predicted to expose peatland …

Peatland ecosystems are globally important carbon stores. Disturbances, such as drainage
and climate drying, act to lower peatland water table depths, consequently enhancing soil …

Ecosystems are increasingly prone to climate extremes, such as drought, with long‐lasting
effects on both plant and soil communities and, subsequently, on carbon (C) cycling …

Anthropogenic climate change is increasing the incidence of climate extremes.
Consequences of climate extremes on biodiversity can be highly detrimental, yet few studies …

The Zoige peatlands are the largest peatland area in China, and the largest high‐altitude
peatland in the world. As with many peatlands worldwide, degradation from land …

Climate change will influence plant photosynthesis by altering patterns of temperature and
precipitation, including their variability and seasonality. Both effects may be important for …