Early Holocene (c. 11.0 - 9.5 ka BP) trace element data from stalagmite NAH14, north-eastern Yucatan Peninsula

This dataset from a speleothem record from the north-eastern Yucatán peninsula (Mexico) provides a high reslution stable isotope and trace elemental record for the early Holocene between 11,040 and 9,520 a BP on up to sub-decadal scale. Line scans of Element/Calcium ratios of the speleothem were measured by laser ablation ICPMS. The chronology is based on 17 U-Th ages (Warken et al., 2021) calculated with the half lives of Cheng et al., 2013. The age-depth model was constructed using the algorithm COPRA (Breitenbach et al., 2012).