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      Deep classification of cut-marks on bones from Arroyo del Vizcaíno (Uruguay)

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          Abstract

          The earliest widely accepted presence of humans in America dates to approximately 17.5 cal kyr BP, at the end of the Last Glacial Maximum (LGM). Among other evidence, this presence is attested by stone tools and associated cut-marks and other bone surface modifications (BSM), interpreted as the result of the consumption of animals by humans. Claims of an older human presence in the continent have been made based on the proposed anthropogenic modification of faunal remains; however, these have been controversial due to the highly subjective nature of the interpretations. Here, we employ advanced deep learning algorithms to objectively increase the accuracy of BSM identification on bones. With several models that exhibit BSM classification accuracies greater than 94%, we use ensemble learning techniques to robustly classify a selected sample of BSM from the approximately 30 kyr BP site of Arroyo del Vizcaíno, Uruguay. Our results confidently show the presence of cut-marks imparted by stone tools on bones at the site. This result supports an earlier presence of humans in the American continent, expanding additional genetic and archaeological evidence of a human LGM and pre-LGM presence in the continent.

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          Deep Residual Learning for Image Recognition

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            Grad-CAM: Visual Explanations from Deep Networks via Gradient-Based Localization

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              The Last Glacial Maximum.

              We used 5704 14C, 10Be, and 3He ages that span the interval from 10,000 to 50,000 years ago (10 to 50 ka) to constrain the timing of the Last Glacial Maximum (LGM) in terms of global ice-sheet and mountain-glacier extent. Growth of the ice sheets to their maximum positions occurred between 33.0 and 26.5 ka in response to climate forcing from decreases in northern summer insolation, tropical Pacific sea surface temperatures, and atmospheric CO2. Nearly all ice sheets were at their LGM positions from 26.5 ka to 19 to 20 ka, corresponding to minima in these forcings. The onset of Northern Hemisphere deglaciation 19 to 20 ka was induced by an increase in northern summer insolation, providing the source for an abrupt rise in sea level. The onset of deglaciation of the West Antarctic Ice Sheet occurred between 14 and 15 ka, consistent with evidence that this was the primary source for an abrupt rise in sea level approximately 14.5 ka.
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                Author and article information

                Contributors
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                Journal
                Proceedings of the Royal Society B: Biological Sciences
                Proc. R. Soc. B.
                The Royal Society
                0962-8452
                1471-2954
                July 14 2021
                July 14 2021
                July 14 2021
                : 288
                : 1954
                : 20210711
                Affiliations
                [1 ]Instituto de Evolución en África (IDEA), Covarrubias 36, 28010 Madrid, Spain
                [2 ]Área de Prehistoria, Departamento de Historia y Filosofía, Universidad de Alcalá, Alcalá de Henares, Spain
                [3 ]Museo Arqueológico de la Comunidad de Madrid, Plaza de las Bernardas s/n, Alcalá de Henares, Madrid, Spain
                [4 ]Departamento de Paleontología, Facultad de Ciencias, Universidad de la República, Iguá 4225, 11400 Montevideo, Uruguay
                [5 ]Servicio Académico Universitario y Centro de Estudios Paleontológicos (SAUCE-P), Universidad de la República, Santa Isabel s/n, 91500 Sauce, Departamento de Canelones, Uruguay
                [6 ]Departamento de Arqueología, Facultad de Humanidades y Ciencias de la Educación, Universidad de la República, Uruguay 1695, 11200 Montevideo, Uruguay
                Article
                10.1098/rspb.2021.0711
                01f2671b-4eef-4c2c-a7cc-b0e000066b98
                © 2021

                https://royalsociety.org/journals/ethics-policies/data-sharing-mining/

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