Paleovegetation reconstruction using δ<sup>13</sup>C of Soil Organic Matter

The relative contributions of C<sub>3</sub> and C<sub>4</sub> plants to vegetation at a given locality may be estimated by means of δ<sup>13</sup>C of soil organic matter. This approach holds a great potential for paleoecological reconstruction using paleosols. Ho...

Full description

Bibliographic Details
Main Authors: F. Su, W. Tan, L. Zhou, X. Feng, J. Han, G. Wang
Format: Article
Language:English
Published: Copernicus Publications 2008-09-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/5/1325/2008/bg-5-1325-2008.pdf