As one descends a mountain, the temperature steadily increases. A new study by a team including Andrew Nottingham, a research associate at the Smithsonian Tropical Research Institute (STRI) and post-doctoral fellow at the University of Edinburgh, took advantage of this principle to predict what would happen as tropical soils warm. The team discovered that warmer tropical soils released more car-bon, the species of soil microbes changed and microbial activity increased.
