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Hominin Dispersal and Settlement East of Huxley’s Line: The Role of Sea Level Changes, Island Size, and Subsistence Behavior

O’Connor, Sue, Louys, Julien, Kealy, Shimona, Samper Carro, Sofía C.·2017·Current Anthropology
DOI 10.1086/694252
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Figure 1 Map of island Southeast Asia showing sites mentioned in text. Downward-pointing triangles indicate sites associated with archaic or ' unknown ' hominin localities, and upward-pointing triangles indicate sites associated with modern humans. A color version of this fi gure is available online.
Figure 1 Map of island Southeast Asia showing sites mentioned in text. Downward-pointing triangles indicate sites associated with archaic or ' unknown ' hominin localities, and upward-pointing triangles indicate sites associated with modern humans. A color version of this fi gure is available online.CC-BY-NC · From the PDF
Figure 2 Sea level for the past 100 kyr (Lambeck and Chappell 2001) adjusted for 0.5 m/kyr uplift as calculated in Kealy, Louys, and O ' Connor (2017, their table 1).
Figure 2 Sea level for the past 100 kyr (Lambeck and Chappell 2001) adjusted for 0.5 m/kyr uplift as calculated in Kealy, Louys, and O ' Connor (2017, their table 1).CC-BY-NC · From the PDF
Figure 3 Palaeo-shoreline reconstructions for Wallacea and neighbors for 100 ka, 60 ka, 55 ka, and 22 ka. Modeled using the General Bathymetric Chart of the Oceans 30 arc-second bathometry chart (Smith and Sandwell 1997). Sea levels are based on the adjusted curve in fi gure 2. A color version of this fi gure is available online.
Figure 3 Palaeo-shoreline reconstructions for Wallacea and neighbors for 100 ka, 60 ka, 55 ka, and 22 ka. Modeled using the General Bathymetric Chart of the Oceans 30 arc-second bathometry chart (Smith and Sandwell 1997). Sea levels are based on the adjusted curve in fi gure 2. A color version of this fi gure is available online.CC-BY-NC · From the PDF
Figure 4 Reconstructions of the Talaud and Sangihe island archipelagos at the time of the fi rst known occupation ( ∼ 35 ka at Leang Sarru) and during the peak of the last glacial maximum (~22 ka). Reconstructed using the uplift-adjusted sea level curve from fi gure 2 and the General Bathymetric Chart of the Oceans bathometry chart (Smith and Sandwell 1997). A color version of this fi gure is available online.
Figure 4 Reconstructions of the Talaud and Sangihe island archipelagos at the time of the fi rst known occupation ( ∼ 35 ka at Leang Sarru) and during the peak of the last glacial maximum (~22 ka). Reconstructed using the uplift-adjusted sea level curve from fi gure 2 and the General Bathymetric Chart of the Oceans bathometry chart (Smith and Sandwell 1997). A color version of this fi gure is available online.CC-BY-NC · From the PDF
Figure 5 Reconstructions of island size at the time of fi rst known occupation for Roti ( A ), Morotai ( B ), Gebe ( C ), Timor ( D ), Kisar ( E ), and Alor ( F ) islands. Reconstructed using the uplift-adjusted sea level curve from fi gure 2 and the General Bathymetric Chart of the Oceans bathometry chart (Smith and Sandwell 1997). A color version of this fi gure is available online.
Figure 5 Reconstructions of island size at the time of fi rst known occupation for Roti ( A ), Morotai ( B ), Gebe ( C ), Timor ( D ), Kisar ( E ), and Alor ( F ) islands. Reconstructed using the uplift-adjusted sea level curve from fi gure 2 and the General Bathymetric Chart of the Oceans bathometry chart (Smith and Sandwell 1997). A color version of this fi gure is available online.CC-BY-NC · From the PDF

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Metadata

Authors
O’Connor, S., Louys, J., Kealy, S., & Samper Carro, S. C.
Venue
Current Anthropology
Publisher
University of Chicago Press
Published
2017-12-01
Volume
58
Issue
S17
Pages
S567-S582
ISSN
  • 0011-3204
  • 1537-5382
DOI
10.1086/694252
Cited by
60
References
3
Language
en

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