Historical rainfall levels are significant in carbon emissions from soil

Scientists have known that microbes living in the ground can play a major role in producing atmospheric carbon that can accelerate climate change, but now researchers from The University of Texas at Austin have discovered that soil microbes from historically wetter sites are more sensitive to moisture and emit significantly more carbon than microbes from historically drier regions. The findings, reported today in the Proceedings of the National Academy of Sciences, point the way toward more accurate climate modeling and improve scientists’ understanding of distinct regional differences in microbial life.