| Literature DB >> 33986297 |
Katharina J Peters1, Frédérik Saltré2, Tobias Friedrich3, Zenobia Jacobs4, Rachel Wood5,6, Matthew McDowell7, Sean Ulm8, Corey J A Bradshaw2.
Abstract
Entities:
Year: 2021 PMID: 33986297 PMCID: PMC8119422 DOI: 10.1038/s41597-021-00918-7
Source DB: PubMed Journal: Sci Data ISSN: 2052-4463 Impact factor: 6.444
Fig. 1Genus-level corrected, sampled-in-bin diversity index calculated from FosSahul 2.0 high-quality ages (i.e., scored A* and A) for megafauna specimens (from Sahul = green; from south-eastern Australia = orange), number of megafauna records (based on the full dataset = light grey; high-quality ages only = dark grey; high- quality ages for south-eastern Australia only = thin black bars), mean annual temperature (°C) and precipitation anomaly (mm day-1) relative to the present day, temperature velocity (m year-1), and precipitation velocity (m year-1) across time (in thousands of years before present). Both the ‘corrected, sampled-in-bin diversity index’ and the ‘number of records’ are calculated using 10,000-year time increments, with the oldest records dated to 180,000 years before present. Climate variable plots show the median value (solid line), and the 25th and 75th percentiles (light shading) calculated across Sahul. Yellow shading represents putative arrival window (including uncertainties) of humans in Sahul; see Bradshaw et al.[6] for discussion. This is a corrected version of Figure 3 from the original publication[2] which contained an error in the calculation of temperature and precipitation anomalies.