Isotopes and Mg/Ca-derived sea-surface temperature records of sediment core MD01-2386

δ18O values (versus Pee Dee belemnite standard) of C. wuellerstorfi (3-10 specimens, >154µm) and G. ruber (white) sensu stricto (8-12 specimens, 250-350µm). The stable isotope composition was measured by Finnigan-MAT253 mass spectrometer equipped with an automatic carbonate preparation device (Ki...

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Hauptverfasser: Jian, Zhimin, Wang, Yue, Dang, Haowen, Lea, David W, Liu, Zhengyu, Jin, Haiyan, Yin, Yaqian
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Wang, Yue
Dang, Haowen
Lea, David W
Liu, Zhengyu
Jin, Haiyan
Yin, Yaqian
description δ18O values (versus Pee Dee belemnite standard) of C. wuellerstorfi (3-10 specimens, >154µm) and G. ruber (white) sensu stricto (8-12 specimens, 250-350µm). The stable isotope composition was measured by Finnigan-MAT253 mass spectrometer equipped with an automatic carbonate preparation device (Kiel III) at the State Key Laboratory of Marine Geology, Tongji University. The isotopic results were calibrated on the Pee Dee Belemnite scale using the China National standard NBS 19. The SD is ±0.07‰. Sample preparation for Mg/Ca measurements on G. ruber samples followed Lea et al. (2000; doi:10.1126/science.289.5485.1719). The Mg/Ca measurements for the upper 400 cm were done using on ICP-MS at the Department of Earth Sciences, University of California, Santa Barbara, the remaining samples were analyzed at the State Key Laboratory of Marine Geology, Tongji University. The Mg/Ca to temperature conversion followed Hollstein et al. (2017; doi:10.1002/2017PA003122). The records cover the last ~142 kyr.
doi_str_mv 10.1594/pangaea.966831
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The stable isotope composition was measured by Finnigan-MAT253 mass spectrometer equipped with an automatic carbonate preparation device (Kiel III) at the State Key Laboratory of Marine Geology, Tongji University. The isotopic results were calibrated on the Pee Dee Belemnite scale using the China National standard NBS 19. The SD is ±0.07‰. Sample preparation for Mg/Ca measurements on G. ruber samples followed Lea et al. (2000; doi:10.1126/science.289.5485.1719). The Mg/Ca measurements for the upper 400 cm were done using on ICP-MS at the Department of Earth Sciences, University of California, Santa Barbara, the remaining samples were analyzed at the State Key Laboratory of Marine Geology, Tongji University. The Mg/Ca to temperature conversion followed Hollstein et al. (2017; doi:10.1002/2017PA003122). 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The stable isotope composition was measured by Finnigan-MAT253 mass spectrometer equipped with an automatic carbonate preparation device (Kiel III) at the State Key Laboratory of Marine Geology, Tongji University. The isotopic results were calibrated on the Pee Dee Belemnite scale using the China National standard NBS 19. The SD is ±0.07‰. Sample preparation for Mg/Ca measurements on G. ruber samples followed Lea et al. (2000; doi:10.1126/science.289.5485.1719). The Mg/Ca measurements for the upper 400 cm were done using on ICP-MS at the Department of Earth Sciences, University of California, Santa Barbara, the remaining samples were analyzed at the State Key Laboratory of Marine Geology, Tongji University. The Mg/Ca to temperature conversion followed Hollstein et al. (2017; doi:10.1002/2017PA003122). 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identifier DOI: 10.1594/pangaea.966831
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language eng
recordid cdi_datacite_primary_10_1594_pangaea_966831
source DataCite
subjects AGE
AMS 14C ages
Calculated from Mg/Ca ratios (Hollstein et al. 2017)
Cibicidoides wuellerstorfi, δ18O
d18O
DEPTH, sediment/rock
Giant piston corer
Globigerinoides ruber white, Magnesium/Calcium ratio
Globigerinoides ruber white, δ18O
isotopes
Marion Dufresne
Mass spectrometer, Finnigan, MAT 253
MD122
Measured
Mg/Ca
Sea surface temperature, annual mean
SST
title Isotopes and Mg/Ca-derived sea-surface temperature records of sediment core MD01-2386
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