The isotopic composition of soil organic carbon on a north-south transect in western interior Canada
The minor isotopes of carbon (13C and 14C) are widely used as tracers in studies of the global carbon cycle. We present carbon-isotope data for the 0-5 cm layer of soil on a transect from 49.6°N to 68°N, from mature forest and tundra ecosystems in the b
Published in: | European Journal of Soil Science |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Blackwell Publishing Ltd
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Subjects: | |
Online Access: | http://hdl.handle.net/1885/64889 https://doi.org/10.1046/j.1365-2389.2002.00444.x https://openresearch-repository.anu.edu.au/bitstream/1885/64889/7/MigratedxPub1015_2002.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/64889/9/MigratedxPub1015_RSD_2002.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/64889/11/01_Bird_The_isotopic_composition_of_2002.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/64889/13/02_Bird_The_isotopic_composition_of_2002.pdf.jpg |
Summary: | The minor isotopes of carbon (13C and 14C) are widely used as tracers in studies of the global carbon cycle. We present carbon-isotope data for the 0-5 cm layer of soil on a transect from 49.6°N to 68°N, from mature forest and tundra ecosystems in the b |
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