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Open AccessGlobal turnover of soil mineral-associated and particulate organic carbon
Soil organic carbon (SOC) persistence is predominantly governed by mineral protection, consequently, soil mineral-associated (MAOC) and particulate organic carbon (POC) turnovers have different impacts on the ...
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Article
Open AccessWhole-soil warming leads to substantial soil carbon emission in an alpine grassland
The sensitivity of soil organic carbon (SOC) decomposition in seasonally frozen soils, such as alpine ecosystems, to climate warming is a major uncertainty in global carbon cycling. Here we measure soil CO2 emiss...
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Article
Open AccessPrognostic and risk factor analysis of cancer patients after unplanned ICU admission: a real-world multicenter study
To investigate the occurrence and 90-day mortality of cancer patients following unplanned admission to the intensive care unit (ICU), as well as to develop a risk prediction model for their 90-day prognosis. W...
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Open AccessExperimental warming causes mismatches in alpine plant-microbe-fauna phenology
Long-term observations have shown that many plants and aboveground animals have changed their phenology patterns due to warmer temperatures over the past decades. However, empirical evidence for phenological s...
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Open AccessGlobal soil profiles indicate depth-dependent soil carbon losses under a warmer climate
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-analysis to SOC measuremen...
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Article
Open AccessTropical forest soils serve as substantial and persistent methane sinks
Although tropical forest soils contributed substantially global soil methane uptake, observations on soil methane fluxes in tropical forests are still sparse, especially in Southeast Asia, leading to large unc...
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Article
Open AccessRegulation of priming effect by soil organic matter stability over a broad geographic scale
The modification of soil organic matter (SOM) decomposition by plant carbon (C) input (priming effect) represents a critical biogeochemical process that controls soil C dynamics. However, the patterns and driv...
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Article
Open AccessPrecipitation overrides warming in mediating soil nitrogen pools in an alpine grassland ecosystem on the Tibetan Plateau
Soils in the alpine grassland store a large amount of nitrogen (N) due to slow decomposition. However, the decomposition could be affected by climate change, which has profound impacts on soil N cycling. We in...