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      Maritime hominin dispersals in the Pleistocene: advancing the debate

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      Antiquity
      Antiquity Publications

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          Abstract

          To what extent is there spatial and temporal patterning in the spread of our genus around the planet, and what environmental and behavioural factors specify this patterning? The prevailing model of Pleistocene dispersals of Homo holds that this process was essentially terrestrial, with oceans and seas inhibiting and directing the movement of hominins out of Africa (e.g. Mellars 2006; Dennell & Petraglia 2012; Gamble 2013), although some scholars propose short-range maritime hops at both the Strait of Gibraltar and Bab-el-Mandeb (Lambeck et al. 2011; Rolland 2013). The relatively recent discovery of stone tools with apparently Lower and Middle Palaeolithic characteristics on islands in the eastern Mediterranean and in Island Southeast Asia (ISEA) has, however, been used by some scholars to challenge this terrestrial model.

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          Revised stratigraphy and chronology for Homo floresiensis at Liang Bua in Indonesia.

          Homo floresiensis, a primitive hominin species discovered in Late Pleistocene sediments at Liang Bua (Flores, Indonesia), has generated wide interest and scientific debate. A major reason this taxon is controversial is because the H. floresiensis-bearing deposits, which include associated stone artefacts and remains of other extinct endemic fauna, were dated to between about 95 and 12 thousand calendar years (kyr) ago. These ages suggested that H. floresiensis survived until long after modern humans reached Australia by ~50 kyr ago. Here we report new stratigraphic and chronological evidence from Liang Bua that does not support the ages inferred previously for the H. floresiensis holotype (LB1), ~18 thousand calibrated radiocarbon years before present (kyr cal. BP), or the time of last appearance of this species (about 17 or 13-11 kyr cal. BP). Instead, the skeletal remains of H. floresiensis and the deposits containing them are dated to between about 100 and 60 kyr ago, whereas stone artefacts attributable to this species range from about 190 to 50 kyr in age. Whether H. floresiensis survived after 50 kyr ago--potentially encountering modern humans on Flores or other hominins dispersing through southeast Asia, such as Denisovans--is an open question.
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            Hominins on Flores, Indonesia, by one million years ago.

            Previous excavations at Mata Menge and Boa Lesa in the Soa Basin of Flores, Indonesia, recovered stone artefacts in association with fossilized remains of the large-bodied Stegodon florensis florensis. Zircon fission-track ages from these sites indicated that hominins had colonized the island by 0.88 +/- 0.07 million years (Myr) ago. Here we describe the contents, context and age of Wolo Sege, a recently discovered archaeological site in the Soa Basin that has in situ stone artefacts and that lies stratigraphically below Mata Menge and immediately above the basement breccias of the basin. We show using (40)Ar/(39)Ar dating that an ignimbrite overlying the artefact layers at Wolo Sege was erupted 1.02 +/- 0.02 Myr ago, providing a new minimum age for hominins on Flores. This predates the disappearance from the Soa Basin of 'pygmy' Stegodon sondaari and Geochelone spp. (giant tortoise), as evident at the nearby site of Tangi Talo, which has been dated to 0.90 +/- 0.07 Myr ago. It now seems that this extirpation or possible extinction event and the associated faunal turnover were the result of natural processes rather than the arrival of hominins. It also appears that the volcanic and fluvio-lacustrine deposits infilling the Soa Basin may not be old enough to register the initial arrival of hominins on the island.
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              Sea level and shoreline reconstructions for the Red Sea: isostatic and tectonic considerations and implications for hominin migration out of Africa

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                Author and article information

                Journal
                applab
                Antiquity
                Antiquity
                Antiquity Publications
                0003-598X
                1745-1744
                April 2017
                April 4 2017
                : 91
                : 356
                : 510-519
                Article
                10.15184/aqy.2017.16
                a40824e7-9e14-4f87-a7e2-0ff1f84c0687
                © 2017
                History

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