Quick Summary:
- Microbes in carbon-rich soils, such as peatlands and permafrost, may increase thier rate of photosynthesis under warmer conditions, potentially offsetting some carbon dioxide emissions.
- Current climate models might overestimate total emissions from degrading landscapes as the planet heats up.
- Peatlands are critical carbon sinks; the northern hemisphere alone stores about 1.5 billion tonnes of carbon in permafrost.
- Thes natural ecosystems are expected to release stored carbon dioxide due to shifting microbial activity caused by rising global temperatures.
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