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. 2021 Aug 26;16(8):e0253708. doi: 10.1371/journal.pone.0253708

Fig 8. Bayesian model of Bawa Yawan rockshelter.

Fig 8

Radiocarbon dates are calibrated using IntCal20 [43]; the model and boundaries were calculated using OxCal 4.3, including a General t-type Outlier Model [49]. Outliers prior and posterior probability are shown in square brackets. The chronology is compared to the North Greenland Ice Core Project (NGRIP) Greenland Ice Core Chronology 2005 (GICC05) δ18O palaeo-environmental record [50] with warm Dansgaard-Oeschger events (from 12 to 3) and Heinrich stadial 4(H4).