(Q59070141)

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A latitudinal gradient in carbon turnover times in forest soils

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A latitudinal gradient in carbon turnover times in forest soils (English)

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Michael I. Bird

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Allan Chivas

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Allan R. Chivas

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John Head

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English

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publication date

May 1996

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Nature

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volume

381

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issue

6578

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page(s)

143-146

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exact match

https://scigraph.springernature.com/pub.10.1038/381143a0

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Partitioning of ocean and land uptake of CO2as inferred by δ13C measurements from the NOAA Climate Monitoring and Diagnostics Laboratory Global Air Sampling Network

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Atmospheric carbon dioxide and the ocean

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13C discrimination during CO2 assimilation by the terrestrial biosphere.

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Ice core record of the 13C/12C ratio of atmospheric CO2 in the past two centuries

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A biochemical model of photosynthetic CO2 assimilation in leaves of C 3 species.

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Leaf carbon isotope and mineral composition in subtropical plants along an irradiance cline

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A global survey of carbon isotope discrimination in plants from high altitude.

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Tree cellulose 13C/12C isotope ratios and climatic change

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Climatic, edaphic, and biotic controls over storage and turnover of carbon in soils

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Biomass and carbon budget of European forests, 1971 to 1990

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On the Temperature Dependence of Soil Respiration

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Recent change of Arctic tundra ecosystems from a net carbon dioxide sink to a source

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Effect of altitude on the carbon-isotope composition of forest and grassland soils from Papua New Guinea

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10.1038/381143A0

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1025637343

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(Q59070141)

A latitudinal gradient in carbon turnover times in forest soils

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