A global calculation of the δ13C of soil respired carbon: Implications for the biospheric uptake of anthropogenic CO2
- 1 June 1999
- journal article
- Published by American Geophysical Union (AGU) in Global Biogeochemical Cycles
- Vol. 13 (2) , 519-530
- https://doi.org/10.1029/98gb00072
Abstract
No abstract availableKeywords
This publication has 24 references indexed in Scilit:
- Monitoring the isotopic composition of atmospheric CO2: Measurements from the NOAA Global Air Sampling NetworkJournal of Geophysical Research: Atmospheres, 1996
- A 1° × 1° distribution of carbon dioxide emissions from fossil fuel consumption and cement manufacture, 1950–1990Global Biogeochemical Cycles, 1996
- Partitioning of ocean and land uptake of CO2 as inferred by δ13C measurements from the NOAA Climate Monitoring and Diagnostics Laboratory Global Air Sampling NetworkJournal of Geophysical Research: Atmospheres, 1995
- Climatic, edaphic, and biotic controls over storage and turnover of carbon in soilsGlobal Biogeochemical Cycles, 1994
- Observations and modeling of biomass and soil organic matter dynamics for the grassland biome worldwideGlobal Biogeochemical Cycles, 1993
- Oceanic 13C/12C observations: A new window on ocean CO2 uptakeGlobal Biogeochemical Cycles, 1993
- The climate induced variation of the continental biosphere: A model simulation of the Last Glacial MaximumGeophysical Research Letters, 1992
- Changes in the landscape of Latin America between 1850 and 1985 II. Net release of CO2 to the atmosphereForest Ecology and Management, 1991
- Evidence for 13C/12C fractionation between tree leaves and woodNature, 1982
- The Concentration and Isotopic Abundances of Carbon Dioxide in the AtmosphereTellus, 1960