| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6446743 | Quaternary Science Reviews | 2013 | 14 Pages |
Abstract
⺠Leaf-wax δD can be corrected for the effects of vegetation and evapotranspiration. ⺠C3 tree versus C4 grass changes are not the main control on leaf-wax δD variations. ⺠Wet season intensity was generally increased during the mid-Holocene. ⺠Wet season intensity was shifted southeastwards during the Last Glacial Maximum.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
James A. Collins, Enno SchefuÃ, Stefan Mulitza, Matthias Prange, Martin Werner, Thejna Tharammal, André Paul, Gerold Wefer,