Isotopic Approach to Soil Carbonate Dynamics and Implications for Paleoclimatic Interpretations
January 1, 1994
The radiocarbon content and stable isotope composition of soil carbonate are best described by a dynamic system in which isotopic reequilibration occurs as a result of recurrent dissolution and reprecipitation. Depth of water penetration into the soil profile, as well as soil age, determines the degree of carbonate isotope reequilibration. We measured ??13C, ??18O and radiocarbon content of gravel rinds and fine (
Citation Information
| Publication Year | 1994 |
|---|---|
| Title | Isotopic Approach to Soil Carbonate Dynamics and Implications for Paleoclimatic Interpretations |
| DOI | 10.1006/qres.1994.1054 |
| Authors | E. G. Pendall, J.W. Harden, S.E. Trumbore, O.A. Chadwick |
| Publication Type | Article |
| Publication Subtype | Journal Article |
| Series Title | Quaternary Research |
| Index ID | 70017518 |
| Record Source | USGS Publications Warehouse |