A new concept for the paleoceanographic evolution of Heinrich event 1 in the North Atlantic
New records of planktonic foraminiferal δ18O and lithic and foraminiferal counts from Eirik Drift are combined with published data from the Nordic Seas and the " Ice Rafted Debris (IRD) belt" , to portray a sequence of events through Heinrich event 1 (H1
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|Source:||Quaternary Science Reviews|
|01_Stanford_A_new_concept_for_the_2011.pdf||2.58 MB||Adobe PDF||Request a copy|
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