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      Aspects of human physical and behavioural evolution during the last 1 million years

      1 , 2 , 1
      Journal of Quaternary Science
      Wiley

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          African climate change and faunal evolution during the Pliocene–Pleistocene

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            Plio-Pleistocene African climate.

            Marine records of African climate variability document a shift toward more arid conditions after 2.8 million years ago (Ma), evidently resulting from remote forcing by cold North Atlantic sea-surface temperatures associated with the onset of Northern Hemisphere glacial cycles. African climate before 2.8 Ma was regulated by low-latitude insolation forcing of monsoonal climate due to Earth orbital precession. Major steps in the evolution of African hominids and other vertebrates are coincident with shifts to more arid, open conditions near 2.8 Ma, 1.7 Ma, and 1.0 Ma, suggesting that some Pliocene (Plio)-Pleistocene speciation events may have been climatically mediated.
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              New fossils from Jebel Irhoud, Morocco and the pan-African origin of Homo sapiens

              Fossil evidence points to an African origin of Homo sapiens from a group called either H. heidelbergensis or H. rhodesiensis. However, the exact place and time of emergence of H. sapiens remain obscure because the fossil record is scarce and the chronological age of many key specimens remains uncertain. In particular, it is unclear whether the present day ‘modern’ morphology rapidly emerged approximately 200 thousand years ago (ka) among earlier representatives of H. sapiens or evolved gradually over the last 400 thousand years. Here we report newly discovered human fossils from Jebel Irhoud, Morocco, and interpret the affinities of the hominins from this site with other archaic and recent human groups. We identified a mosaic of features including facial, mandibular and dental morphology that aligns the Jebel Irhoud material with early or recent anatomically modern humans and more primitive neurocranial and endocranial morphology. In combination with an age of 315 ± 34 thousand years (as determined by thermoluminescence dating), this evidence makes Jebel Irhoud the oldest and richest African Middle Stone Age hominin site that documents early stages of the H. sapiens clade in which key features of modern morphology were established. Furthermore, it shows that the evolutionary processes behind the emergence of H. sapiens involved the whole African continent.
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                Author and article information

                Journal
                Journal of Quaternary Science
                J Quaternary Sci
                Wiley
                0267-8179
                1099-1417
                August 14 2019
                August 14 2019
                Affiliations
                [1 ]Centre for Human Evolution Research (CHER), Department of Earth SciencesNatural History MuseumLondon UK
                [2 ]School of Environment and TechnologyUniversity of BrightonBrighton UK
                Article
                10.1002/jqs.3137
                78c677eb-f2e2-4cf9-99b3-c4a9ff5329c2
                © 2019

                http://doi.wiley.com/10.1002/tdm_license_1.1

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