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SUMMARY:The release of Δ14C and δ18O-depleted water from the Arctic Ocea
 n upon glacial termination - Dr. David Thornalley (Woods Hole Oceanographi
 c Institution\, USA)
DTSTART:20130110T170000Z
DTEND:20130110T183000Z
UID:TALK42376@talks.cam.ac.uk
CONTACT:Philip GIBBARD
DESCRIPTION:Abstract not available
LOCATION:Thirkill Room\, Clare College
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