MD01-2378 from the Timor Sea, which provide new insights into the variability of the
Indonesian outflow across the last two glacial terminations. Mg/Ca in Globigerinoides ruber
(white ss) indicates an overall increase of 3.2° C in sea surface temperature (SST) over
Termination I. Following an early Holocene plateau at 11.3–6.4 ka, SSTs cooled by 0.6° C
during the middle to late Holocene (6.4–0.7 ka). The early Holocene warming occurred in …