Northern Hemisphere summer insolation and ice volume driven variations in hydrological environment in southwest China

<p>This dataset from a stalagmite record from Chongqing, Southwest China, provides a high-resolution trace element record from the Last Glacial-Interglacial (116.09 to 4.07 ka BP) up to the sub-centennial scale. Line scans of Element/Calcium ratios of the speleothem were measured by laser ablation ICPMS. Chronology is based on 58 U-Th ages.</p>