chronology data not available; bibliographic citation (taken from PANGAEA) seems incorrect. missing UK37 data; no Bayesian recalibration

Emeis, Kay-Christian; Dawson, Alastair G.

Holocene palaeoclimate records over Europe and the North Atlantic

2 core names available: GIK16160‐3 and M75_3_137_3; missing underlying data; on Bayesian recalibration

The UK′37 index was converted into SST using the calibration based on core‐top sediments derived from Indian Ocean [Sonzogni et al., 1997] with a slope of 0.023 [Bard et al., 1997], because this calibration provides the best SST estimate for the 24°C–29°C temperature range for western Indian Ocean [Bard et al., 1997; Sonzogni et al., 1997].

calibration based on core‐top sediments derived from Indian Ocean [Sonzogni et al., 1997] with a slope of 0.023 [Bard et al., 1997]

To convert Mg/Ca into temperature, we used the species‐specific calibration equations with a given uncertainty of ±1.2°C for the 250–350 µm G. ruber size fraction [Anand et al., 2003].

species‐specific calibration equations for the 250–350 um G. ruber size fraction [Anand et al., 2003]

Globigerinoides ruber + G. trilobus + G. sacculifer

Wang, Yiming V.; Leduc, Guillaume; Regenberg, Marcus; Andersen, Nils; Larsen, Thomas; Blanz, Thomas; Schneider, Ralph R.

Northern and southern hemisphere controls on seasonal sea surface temperatures in the Indian Ocean during the last deglaciation

age gap between 8.8 and 3.7 ka; six ages over Holocene; retain to improve SH coverage

sensu stricto. The foraminiferal samples were homogenized and split for stable isotope analyses (~1/3) and for Mg/Ca analyses (~2/3); including the reductive step with hydrazine to remove metal oxides

“species specific” calibration for G. ruber of Regenberg et al. [2009].

The foraminiferal samples were homogenized and split for stable isotope analyses (~1/3) and for Mg/Ca analyses (~2/3); including the reductive step with hydrazine to remove metal oxides

SST calculated from d18O (TSid=RwsnEN3SLKp) using the bayfoxm program bayfox_predict.  Parameters: prior_mean=23.5778, prior_std=10, species=ruber, bayes=unspecified;  For d18osw, values are specified to change through time, and are calculated using the getvardelo.m program from Jess Tierney, based on the modern value of d18osw (0.27088) for the archive location and using the ages