Work

Sea surface temperature variation in South China Sea between the Last Glacial Maximum and the Holocene constrained by carbonate clumped isotope thermometry in foraminifera

Year: 2023

Type: report

Abstract: This document contains traditional stable carbon and oxygen isotope ratios (δ13C, δ18O), clumped isotope ratio (Δ47), 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.

Source: Zenodo (CERN European Organization for Nuclear Research)

DOI: 10.5281/zenodo.7906980

Authors: Laskar, Amzad Hussain, Hrong, Chorng-Shern, Band, Shraddha, Chakraborty, Arindam, Banerjee, Sanchita, Huang, Kuo-Fang, Yui, Tzen-Fu, Wang, Yunshuen, Chen, Kou-Hang, Lin, Chun-Hung, Yang, Kai-Hsiang, Liang, Mao-Chang

Institutions: Physical Research Laboratory, Institute of Earth Sciences, Academia Sinica, Academia Sinica, National Taiwan University, University of Malaya, Ministry of Economic Affairs, Central Geological Survey, MOEA, National Cheng Kung University

Language: English

Topic: Geology and Paleoclimatology Research

Subfield: Atmospheric Science

Field: Earth and Planetary Sciences

Domain: Physical Sciences

SDGs: Climate action, Life below water

Open Access status: green

OpenAlex ID: W6894135779

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