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) |
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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