Globorotalia inflata oxygen isotope (δ¹⁸O), Mg/Ca-derived thermocline temperature and ice-volume free seawater δ¹⁸O from subtropical western South Atlantic core GL-1090 during the last glacial cycle

These data contain the Monte Carlo ensemble δ¹⁸O, Mg/Ca-derived thermocline temperature and ice-volume free seawater δ¹⁸O from a thermocline-dweller planktic foraminifera (Globorotalia inflata) from the subtropical western South Atlantic (Santos Basin) analyzed in core GL-1090. The data reports the measured proxies and the Quantiles (Q0.025, Q0.16, Q0.84, Q0.975).

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