Abstract
In summary, we are not convinced by the arguments of Garcin [2008] that either our interpretation of elevated Zr:Ti or biogenic silica during the Younger Dryas (southward shift of the ITCZ causing more prevalent northerly winds over the north basin of the lake) is in error, or that a similar mechanism was not at work during Greenland stadials in MIS-3.
| Original language | English (US) |
|---|---|
| Article number | L04702 |
| Journal | Geophysical Research Letters |
| Volume | 35 |
| Issue number | 4 |
| DOIs |
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| State | Published - Feb 28 2008 |
ASJC Scopus subject areas
- Geophysics
- General Earth and Planetary Sciences
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