Articles | Volume 21, issue 12
https://doi.org/10.5194/cp-21-2525-2025
https://doi.org/10.5194/cp-21-2525-2025
Research article
 | 
02 Dec 2025
Research article |  | 02 Dec 2025

Penultimate glacial sea surface temperature and hydrologic variability in the tropical South Pacific from 150 ka Tahiti corals

Ryuji Asami, Thomas Felis, Ryuichi Shinjo, Masafumi Murayama, and Yasufumi Iryu

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Cited articles

Asami, R., Felis, T., Deschamps, P., Hanawa, K., Iryu, Y., Bard, E., Durand, N., and Murayama, M.: Evidence for tropical South Pacific climate change during the Younger Dryas and the Bølling-Allerød from geochemical records of fossil Tahiti corals, Earth Planet. Sc. Lett., 288, 96–107, https://doi.org/10.1016/j.epsl.2009.09.011, 2009. 
Asami, R., Iryu, Y., Hanawa, K., Miwa, T., Holden, P., Shinjo, R., and Paulay, G.: MIS 7 interglacial sea surface temperature and salinity reconstructions from a southwestern subtropical Pacific coral, Quat. Res., 80, 575–585, https://doi.org/10.1016/j.yqres.2013.09.002, 2013. 
Asami, R., Yoshimura, N., Toriyabe, H., Minei, S., Shinjo, R., Hongo, C., Sakamaki, T., and Fujita, K.: High-resolution evidence for middle Holocene East Asian winter and summer monsoon variations: snapshots of fossil coral records, Geophys. Res. Lett., 47, e2020GL088509, https://doi.org/10.1029/2020GL088509, 2020. 
Asami, R., Felis, T., Shinjo, R., Murayama, M., and Iryu, Y.: Geochemical data from IODP Expedition 310 Tahiti fossil corals, PANGAEA [data set], https://doi.org/10.1594/PANGAEA.987216, 2025. 
Ayling, B. F., McCulloch, M. T., Gagan, M. K., Stirling, C. H., Andersen, M. B., and Blake, S. G.: Sr/Ca and δ18O seasonality in a Porites coral from the MIS 9 (339–303 ka) interglacial, Earth Planet. Sc. Lett., 248, 462–475, https://doi.org/10.1016/j.epsl.2006.06.009, 2006. 
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Short summary
We generated high resolution geochemical records from well-preserved fossil corals of the penultimate glacial (~150 000 years ago) and last glacial (~30 000 years ago) periods drilled at Tahiti in the central tropical South Pacific. The fossil records revealed that the glacial mean seawater temperature was 3–4 °C lower and had greater seasonality than present. Our coral-based reconstructions document oceanographic and hydroclimatological changes in glacial periods extremely different from today.
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