Monthly Tahiti coral Sr/Ca and oxygen isotope data from IODP Hole 310-M0024A

The early last glacial termination was characterized by intense North Atlantic cooling and weak overturning circulation. This interval between ~18,000 and 14,600 years ago, known as Heinrich Stadial 1, was accompanied by a disruption of global climate and has been suggested as a key factor for the t...

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Bibliographic Details
Main Authors: Felis, Thomas, Merkel, Ute, Asami, Ryuji, Deschamps, Pierre, Hathorne, Ed C, Kölling, Martin, Bard, Edouard, Cabioch, Guy, Durand, Nicolas, Prange, Matthias, Schulz, Michael, Cahyarini, Sri Yudawati, Pfeiffer, Miriam
Format: Dataset
Language:English
Published: PANGAEA 2012
Subjects:
310-M0024A
Calculated
see reference(s)
DP Hunter
DRILL
Drilling/drill rig
Exp310
ICP-OES
Perkin-Elmer
Optima 3300R
Integrated Ocean Drilling Program / International Ocean Discovery Program
Internal coral chronology
IODP
Mass spectrometer Finnigan MAT 251
Porites sp.
Strontium/Calcium ratio
δ18O
Sample code/label
TAH-02A-5F
Tahiti
offshore Tiarei
Tahiti Sea Level
Pacific
North Atlantic
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.786743
https://doi.org/10.1594/PANGAEA.786743

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