Anthropogenic environmental changes, or 'stressors', increasingly threaten biodiversity and
ecosystem functioning worldwide. Multiple-stressor research is a rapidly expanding field of …

Numerous field studies have found changes in soil respiration and microbial abundance
under experimental warming. Yet, it is uncertain whether the magnitude of these responses …

Global soils store at least twice as much carbon as Earth's atmosphere,. The global soil-to-
atmosphere (or total soil respiration, RS) carbon dioxide (CO2) flux is increasing,, but the …

With accumulation of carbon cycle observations and model developments over the past
decades, exploring interannual variation (IAV) of terrestrial carbon cycle offers the …

Direct quantification of terrestrial biosphere responses to global change is crucial for
projections of future climate change in Earth system models. Here, we synthesized …

As the second-largest terrestrial carbon (C) flux, soil respiration (RS) has been stimulated by
climate warming. However, the magnitude and dynamics of such stimulations of soil …

The effects of long-term climate warming on soil respiration and its drivers remain unclear in
forests, which store approximately 40% of global soil carbon. Here we conducted a climate …

Altered precipitation regimes have a great impact on global climate change, with potentially
important effects on below-ground carbon dynamics. Soil microbes and carbon (C) …

Over the last few decades, there has been an increasing number of controlled‐manipulative
experiments to investigate how plants and soils might respond to global change. These …

The ratio of carbon (C) that is invested into microbial growth to organic C taken up is known
as microbial carbon use efficiency (CUE), which is influenced by environmental factors such …