Soil carbon dioxide emissions controlled by an extracellular oxidative metabolism identifiable by its isotope signature
Soil heterotrophic respiration is a major determinant of the carbon (C) cycle and its interactions with climate. Given the complexity of the respiratory machinery, it is traditionally considered that oxidation of organic C into carbon dioxide (CO<sub>2</sub>) strictly results from int...
| Main Authors: | , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2016-11-01
|
| Series: | Biogeosciences |
| Online Access: | https://www.biogeosciences.net/13/6353/2016/bg-13-6353-2016.pdf |