DATING THE CERUTTI MASTODON: U-TH ISOTOPE ANALYSES OF BONE TO DERIVE A 130-KA AGE SUPPORTING AN EARLY HOMININ SITE IN THE AMERICAS
Subsequently, bone specimens were dated using U-series disequilibrium. Living bone tissue has low U concentrations (0.005–0.05 µg/g); however, much higher values are present in CM fossil bones (mean=162±67 µg/g) reflecting substantial post-mortem U incorporation. Evaluating the U-uptake history is critical to establishing an accurate age. Multi-sample profiles consisting of 13 to 30 individual analyses across cortical layers of 2 limb and 1 rib bones were analyzed by thermal ionization mass spectrometry. Conventional closed-system 230Th/U ages range from 100.5±0.7 to 126.9±1.1 ka. Both U concentrations and 230Th/U ages yielded simple, υ-shaped profiles, which is consistent with models of continuous diffusion and adsorption of U into porous compact bone. Application of iDAD modeling (Diffusion-Adsorption-Decay; Sambridge et al., 2012; doi:10.1016/j.quageo.2012.02.010) using U-Th isotope compositions and positions across each profile yielded maximum-likelihood ages of 137.0±5.6 ka, 126.4±5.5 ka, and 130.2±2.7 ka (±2σ). Initial 234U/238U values are consistent with local water sources, and there is no evidence of U leaching that would result in erroneously old 230Th/U ages. The mean of the 3 iDAD ages weighted by their uncertainties yields a mean age of 130.7±9.4 ka. This date implies that hominins reached the Americas more than 100,000 years earlier than previously thought.