Table 1.
Sample | Site | Genome Coverage | Human DNA Shotgun (%) | Human DNA Postcapture (%) | Radiocarbon Age (cal BCE, 1σ) | Sex | mtDNA Haplogroup | mtDNA Coverage | Contamination (%) |
---|---|---|---|---|---|---|---|---|---|
CB13 | Cova Bonica | 1.1085 | 5.68 | 28.23 | 5,470–5,360 | F | K1a2a | 353.29 | 0.11 |
CB14 | Cova Bonica | 0.0003 | 0.25 | — | —a | F | X2c | 4.1 | 1.35 |
F19 | Almonda cave | 0.0129 | 0.58 | 9.66 | 5,310–5,220 | F | H4a1a | 33.79 | 29.13 |
G21 | Almonda cave | 0.0039 | 0.09 | 1.27 | 5,330–5,230 | M | H3 | 63.55 | 1.97 |
H3C6 | Cova de l’Or | 0.0011 | 0.06 | 1.01 | 5,360–5,310 | M | H4a1a | 4.45 | 3.96 |
CS7675 | Cova de la Sarsa | 0.0012 | 0.08 | 1.14 | 5,321–5,227 | Mb | K1a4a1 | 0.69 | — |
aCB14 is not directly radiocarbon dated, although it comes from the same stratigraphic layer than CB13.
bCS7675 is determined to be a male from morphology.