Variations in Mg/Ca‐based sea surface temperature and oxygen isotope ratio (δ18O) of the
surface water in the northern East China Sea (ECS) were reconstructed with high resolution …

The monsoon system represents one of the basic elements of global atmospheric
circulation. Its evolution and variability over long periods of geologic time play a significant …

Abstract East China Sea (ECS) is greatly influenced by East Asian Summer Monsoon
(EASM), precipitation discharge and differential inflow of the warm and saline Kuroshio …

The δ 18 O of seawater (δ 18 O w), an indirect indicator of sea surface salinity (SSS), in the
northern East China Sea (ECS) is reconstructed for the Holocene using paired analyses of …

Changes in the Southeast Asia monsoon winds and surface circulation patterns since the
last glaciation are inferred using multiple paleoceanographic indicators including planktic …

Upper water column dynamics in the southern South China Sea were reconstructed in order
to track changes in the activity of the East Asian winter monsoon (EAWM) since the Last …

High‐resolution studies of a planktonic foraminifer core record from the South China Sea
(SCS)(31KL: 18° 45.4′ N, 115° 52.4′ E, water depth 3360 m) reveal changes driven by …

High-resolution planktonic foraminifer Mg/Ca sea surface temperature (SST) and δ18O
records of IMAGES core MD052896 from the southern South China Sea (SCS) provide a …

Planktonic foraminiferal assemblages and benthic foraminiferal oxygen isotopes were
obtained in a gravity core NS07-25 (6° 39.945′ N, 113° 32.936′ E, water depth 2006m) …

High-resolution sea surface temperatures (SST) derived from Mg/Ca ratios of
Globeriginoides sacculifer at ODP Site 1144 were reported to reveal the SST changes …