Fig. 2: Physical and geochemical sediment properties from the Junín drill core.
From: Andean drought and glacial retreat tied to Greenland warming during the last glacial period
The similar XRF profiles of a Ti and b Si indicate both elements primarily represent clastic inputs, with slight differences attributable to different bedrock mineralogy and grain size. c Siliciclastic sediment flux (log scale). d Total organic carbon (TOC). e Dry bulk density. f Bacon age-depth model of 79 AMS radiocarbon ages on terrestrial macrofossils; error bars denote 95% probability range for calibrated ages. Ages excluded from the age model are listed in the supplemental. Gray vertical bars show the distribution of peat layers.
