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. 2022 Nov 8;12(1):19012.
doi: 10.1038/s41598-022-23206-9.

Javanese Homo erectus on the move in SE Asia circa 1.8 Ma

Collaborators, Affiliations

Javanese Homo erectus on the move in SE Asia circa 1.8 Ma

Laurent Husson et al. Sci Rep. .

Abstract

The migration of Homo erectus in Southeast Asia during Early Pleistocene is cardinal to our comprehension of the evolution of the genus Homo. However, the limited consideration of the rapidly changing physical environment, together with controversial datings of hominin bearing sites, make it challenging to secure the robust timeline needed to unveil the behavior of early humans. Here, we reappraise the first appearance datum of Javanese H. erectus by adding the most reliable age constraints based on cosmogenic nuclides [Formula: see text]Be and [Formula: see text]Al produced in situ to a compilation of earlier estimates. We find that H. erectus reached Java and dwelled at Sangiran, Java, ca. 1.8 Ma. Using this age as a baseline, we develop a probabilistic approach to reconstruct their dispersal routes, coupling ecological movement simulations to landscape evolution models forced by reconstructed geodynamic and climatic histories. We demonstrate that the hospitable terra firma conditions of Sundaland facilitated the prior dispersal of hominins to the edge of Java, where they conversely could not settle until the Javanese archipelago emerged from the sea and connected to Sundaland. The dispersal of H. erectus across Sundaland occurred over at least tens to hundreds kyr, a time scale over which changes in their physical environment, whether climatic or physiographic, may have become primary forcings on their behavior. Our comprehensive reconstruction method to unravel the peopling timeline of SE Asia provides a novel framework to evaluate the evolution of early humans.

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Conflict of interest statement

The authors declare no competing interests.

Figures

Figure 1
Figure 1
Geology of Sangiran. (a) Regional view. Black line delinates continental Sundaland (120 m isodepth). Stars indicate possible northern entry points (thereafter set to Myanmar, Thailand and Vietnam) for H. erectus. (b) Java island and main biostratigraphic sites (hominin-bearing sites: Sangiran (s), Mojokerto (m), Trinil (t), Ngandong (n); and faunal site Bumiayu (b). (c) 3D view of the Sangiran dome. Geological map redrawn from,. Red star locates Bukuran creek outcrop; skull is Sangiran-17. Maps on panels (a,b) were created using GMT 5 (www.generic-mapping-tools.org); on panel (c). using ArcGIS (www.arcgis.com).
Figure 2
Figure 2
Bukuran sampling site, stratigraphic setting, and analytical results. (a) General lithostratigraphy of the Sangiran Dome,,, depositional environment, and available datings. Blue bars indicate proven occurrence of H. erectus fossils remains, skull is Sangiran-17. (b) Stratigraphic log of the sampling site. (c) Sampling site, lithologies, and sample location (labeled by their sample name suffix: 1 is SAN18-1). The Bukuran stream flows at the bottom of the outcrop. (d,e): 10Be and 26Al concentrations and 26Al/10Be ratios over depth. Red and blue dots are 26Al and 10Be concentrations (S.I. Table 1). L. Lahar: Lower Lahar; U. Tuff: Upper Tuff; al.: alluvium; Gb.: Grenzbank unit. Earlier datings: H11, paleomag. L01, 40Ar/39Ar ; M20a, U-Pb and ZFT; M20b, U-Pb; M20c, U-Pb and ZFT; S94, 40Ar/39Ar; S00, 40Ar/39Ar, paleomag.; B04, 40Ar/39Ar.
Figure 3
Figure 3
Migration pathways of H. erectus across Sundaland during Early Pleistocene. (a) Reconstructed landscape ca. 1.8 Ma (model goSPL). The underlying physiography, with overprinted modeled rivers, converts into a map of resistance to displacement that serves to compute the migration pathways, either using a least-cost path algorithm shown for the Myanmar entry point (purple), or a mechanistic movement model (SiMRiv) exemplified for the Vietnam entry point (orange). Blue star locates the Thailand entry point. (b) Statistical analysis of the pathways of H. erectus migration to Sangiran, from 3000 simulations (1000 per entry point). The kernel density estimation (kde, normalized) indicates the likelihood that hominins came across a given region (combined for the three entry points). Map on panel (a,b). were respectively made using Paraview (www.paraview.org) and GMT 5 (www.generic-mapping-tools.org).
Figure 4
Figure 4
Travelled distance and time of H. erectus migration to Sangiran, statistical analysis (3000 simulations, 1000 per entry point - Myanmar, Thailand, and Vietnam). (a) Migration distance from the least-cost path (LCP) analysis and successful mechanistic movement realizations (Markovian random walk) for the three entry points, and all combined. (b) Travel times, for three dispersal speeds (slow: 1 km/yr, medium: 5 km/year, and fast: 10 km/yr).

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