Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6350364 | Palaeogeography, Palaeoclimatology, Palaeoecology | 2013 | 13 Pages |
Abstract
We do not propose that our findings invalidate the previous principal component analyses, but they do have the advantage of being based more clearly on the relationship between modern plant distributions and individual climatic variables. Results indicate that temperatures during both the warm and cold seasons were 6 ± 2 °C colder during the LGM and Younger Dryas, and that rainy season precipitation during the Last Glacial Maximum was ~ 50% of that during the mid-Holocene. Our results also imply that changes in precipitation at Wonderkrater generally track changes in Mozambique Channel sea-surface temperatures, with a steady increase following the Younger Dryas to a period of maximum water availability at Wonderkrater ~ 3-7 ka. These findings argue against a dominant role of a shifting Intertropical Convergence Zone in determining long-term environmental trends, and indicate that the northern and southern tropics experienced similar climatic trends during the last 20 kyr.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Loïc Truc, Manuel Chevalier, Charly Favier, Rachid Cheddadi, Michael E. Meadows, Louis Scott, Andrew S. Carr, Gideon F. Smith, Brian M. Chase,