The climate of the Last Glacial period (10,000-110,000
years ago) was characterized by rapid millennial-scale climate fluctuations termed Dansgaard/Oeschger (D/O) and Heinrich (H) events. We present results from a speleothem-derived proxy of the South American Summer Monsoon (SASM) from 16,000-50,000 years ago that demonstrate the occurrence of D/O cycl...
| Other Authors: | |
|---|---|
| Format: | Text |
| Language: | English |
| Subjects: | |
| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.699.6155 |
| Summary: | years ago) was characterized by rapid millennial-scale climate fluctuations termed Dansgaard/Oeschger (D/O) and Heinrich (H) events. We present results from a speleothem-derived proxy of the South American Summer Monsoon (SASM) from 16,000-50,000 years ago that demonstrate the occurrence of D/O cycles and Heinrich events. This tropical Southern Hemisphere monsoon reconstruction illustrates an anti-phase relationship to Northern Hemisphere monsoon intensity at the millennial scale. Our results also show an influence of Antarctic millennial-scale climate fluctuations on the SASM. This high-resolution, precisely dated, tropical precipitation record can be used to establish the timing of climate events in the high latitudes of the Northern and Southern Hemispheres. |
|---|