Published June 30, 2023
| Version v1
Sea surface temperature variation in South China Sea between the Last Glacial Maximum and the Holocene constrained by clumped isotope thermometry in foraminifera
Authors/Creators
- 1. Physical Research Laboratory, Ahmedabad
- 2. Institute of Earth Sciences, Academia Sinica, Taipei, Taiwan
- 3. Department of Geosciences, National Taiwan University, Taipei, Taiwan
- 4. Department of Geology, Faculty of Science, Universiti Malaya, Kuala Lumpur, Malaysia
- 5. Central Geological Survey, Ministry of Economic Affairs, Taiwan
- 6. Department of Earth Sciences, National Cheng Kung University, Taiwan
Description
This document contains traditional stable carbon and oxygen isotope ratios (δ13C, δ18O), clumped isotope ratio (Δ47), radiocarbon ages, Mg/Ca ratios and diatom data from a sediment core recovered from the northern South China Sea. Also calibration data for clumped isotopic measurements, results of standards measured along with the samples and ecological preferences of the major diatom taxa are presented in this document.