Soil respiration (Rs), the soil‐to‐atmosphere flux of CO2, is a dominant but uncertain part of
the carbon cycle, even after decades of study. This review focuses on progress in …

Understanding the large-scale pattern of soil microbial carbon use efficiency (CUE) and its
temperature sensitivity (CUET) is critical for understanding soil carbon–climate feedback …

Estuarine wetlands are an important part of coastal blue carbon and play an essential role in
mitigating climate change. However, their geographical location typically exposes them to …

Soil microbes are essential for regulating carbon stocks under climate change. However, the
uncertainty surrounding how microbial temperature responses control carbon losses under …

Climate change and metals independently stress soil microbiomes, but their combined
effects remain unresolved. Here we show that future climate affects soil cadmium through …

Climate change is predicted to cause milder winters and thus exacerbate soil freeze–thaw
perturbations in the subarctic, recasting the environmental challenges that soil …

Substrate depletion and microbial community thermal adaptation are major mechanisms that
regulate the temperature sensitivity (Q 10) of soil microbial respiration. Traditionally, the Q …

Mangrove ecosystems can be both significant sources and sinks of greenhouse gases. The
restoration of mangrove forests is increasingly used as a natural climate solution tool to …

Mountain ecosystems, contributing substantially to the global carbon (C) and nitrogen (N)
biogeochemical cycles, are heavily impacted by global changes. Although soil respiration …

Soil respiration (R s) is a crucial component of the terrestrial ecosystem carbon (C) cycle,
which significantly regulates atmospheric CO 2 concentrations. Although previous studies …