A latitudinal gradient in carbon turnover times in forest soils

[1]  Philippe Ciais,et al.  Partitioning of ocean and land uptake of CO2 as inferred by δ13C measurements from the NOAA Climate Monitoring and Diagnostics Laboratory Global Air Sampling Network , 1995 .

[2]  D. Schimel,et al.  Terrestrial ecosystems and the carbon cycle , 1995 .

[3]  Thomas H. Painter,et al.  Climatic, edaphic, and biotic controls over storage and turnover of carbon in soils , 1994 .

[4]  J. Lloyd,et al.  On the temperature dependence of soil respiration , 1994 .

[5]  A. Chivas,et al.  Effect of altitude on the carbon-isotope composition of forest and grassland soils from Papua New Guinea , 1994 .

[6]  D. Schindler,et al.  The biosphere as an increasing sink for atmospheric carbon: Estimates from increased nitrogen depostion , 1993 .

[7]  J. Balesdent,et al.  Site-Related ^(13)C of Tree Leaves and Soil Organic Matter in a Temperate Forest , 1993 .

[8]  U. Siegenthaler,et al.  Atmospheric carbon dioxide and the ocean , 1993, Nature.

[9]  S. Trumbore.  Comparison of carbon dynamics in tropical and temperate soils using radiocarbon measurements , 1993 .

[10]  Walter C. Oechel,et al.  Recent change of Arctic tundra ecosystems from a net carbon dioxide sink to a source , 1993, Nature.

[11]  Pekka E. Kauppi,et al.  Biomass and Carbon Budget of European Forests, 1971 to 1990 , 1992, Science.

[12]  E. Medina,et al.  Photosynthesis and sup 13 C/ sup 12 C ratios in Amazonian rain forests , 1989 .

[13]  M. Stuiver,et al.  Tree cellulose 13C/12C isotope ratios and climatic change , 1987, Nature.

[14]  H. Friedli,et al.  Ice core record of the 13C/12C ratio of atmospheric CO2 in the past two centuries , 1986, Nature.