Meng-Yang Lee

TL;DR: In this paper, the ages of geomagnetic reversals were calibrated by tuning the oxygen isotopic stratigraphy, yielding a chronology for the following subchrons: Matuyama/Brunhes boundary, 781 ± 3 ka (slightly above δ18O Stage 19.3); top of the Santa Rosa polarity interval, 920 ± 2 ka (Stage 23/24); base of the SPCI interval, 925 ± 1 ka (stage 24); Top of the Jaramillo subchron, 988 ± 3 Ka (Stage 27

TL;DR: In this article, microtektites from two deep-sea cores in the South China Sea and the West Philippine Sea are identified as belonging to the Australasian tektite strewn field based on the morphology, chronostratigraphic occurrence, and geographical location of these microtectites.

TL;DR: In this article, the authors report evidence for the eastward dispersal of the oldest Toba tuff in South China Sea sediments to 2500 km away from the source, according to the tephra occurrence between marine isotope stages 20 and 19.

TL;DR: In this paper, the authors presented the directional paleomagnetic secular variation pattern of core MD972151 taken from the southwestern South China Seaduring the IMAGES Ⅲ-IPHIS Cruise in 1997.

TL;DR: Stoll et al. as mentioned in this paper showed that different size shells have different Sr/Ca ratios; however, samples with shell sizes of 355-500 μm appear to have normally distributed Sr/CA ratios (1σ=1.8%).