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

Bibliographic Details
Published in:European Journal of Soil Science
Main Authors: Bird, Michael, Santruckova, H, Lloyd, J, Lawson, Ewan
Format: Article in Journal/Newspaper
Language:unknown
Published: Blackwell Publishing Ltd
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
Description
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