Abstract
Planktonic foraminiferal Mg/Ca ratios and oxygen isotopic compositions of a spliced sediment record from Feni Drift, NE Atlantic Ocean (box core M200309 and piston core ENAM9606) trace late Holocene sea surface temperature (SST) and salinity changes over the past 2400 years. At this location, the variability of SST and oxygen isotopic composition of seawater (δ
Original language | English |
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Pages (from-to) | 1941-1955 |
Number of pages | 15 |
Journal | Quaternary Science Reviews |
Volume | 28 |
Issue number | 19-20 |
DOIs | |
Publication status | Published - 2009 |