Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6441809 | Marine Geology | 2012 | 13 Pages |
Abstract
⺠In Maxwell Bay, during last 3 kyr, increases in open-marine influence took place. ⺠At 2 cal kyr BP, glacial influence increased, lasting at least until 800 cal ky BP. ⺠δ18O changes correlate with the beginning of Neoglacial, MWP and post-LIA warming. ⺠A significant increase in sediment accumulation rate is marked in ~ 1980. ⺠At our sites, climate variability has overall little impact on benthic foraminifera.
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Authors
Wojciech Majewski, Julia S. Wellner, Witold SzczuciÅski, John B. Anderson,