2016
DOI: 10.1016/j.quascirev.2016.02.028
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Tooth enamel stable isotopes of Holocene and Pleistocene fossil fauna reveal glacial and interglacial paleoenvironments of hominins in Indonesia

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Cited by 43 publications
(29 citation statements)
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“…A prediction map of savanna corridor in the central of Sundaland is depicted in (figure 4). Based on data isotope on bovids and cervids teeth shows that's vegetation d18O values coinciding with C4-abundance during (inferred) glacial periods (Janssen et al 2016). It is possible for the glacial savanna in Sundaland to become an occupations and migration path for both humans and faunas.…”
Section: Potential Of Human Occupation In Sundalandmentioning
confidence: 95%
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“…A prediction map of savanna corridor in the central of Sundaland is depicted in (figure 4). Based on data isotope on bovids and cervids teeth shows that's vegetation d18O values coinciding with C4-abundance during (inferred) glacial periods (Janssen et al 2016). It is possible for the glacial savanna in Sundaland to become an occupations and migration path for both humans and faunas.…”
Section: Potential Of Human Occupation In Sundalandmentioning
confidence: 95%
“…Glacial-interglacial cycles generate eustatic sealevel fluctuations, periodically turning the Sumatra Islands of the Indonesian Archipelago into mountain ranges on the subaerially exposed Sunda Shelf (Janssen et al 2016;Voris 2000). This makes sense because it will not be easy to find sites in the lower Pleistocene in the present time, especially Homo erectus which suspected to live in the lowlands.It is very likely that we can find traces of humans in the lower Pleistocene on land that has now sunk underwater.The recurring land connection and greater extent of more open vegetation during glacial periods enabled repeated biotic migrations from mainland Asia into Sundaland.…”
Section: Potential Of Human Occupation In Sundalandmentioning
confidence: 99%
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“…In enamel, there is limited fractionation in δ 13 C composition with increasing trophic level (i.e., through carnivores and omnivores higher in the food chain, see Lee-Thorp and Sponheimer [2006]). Therefore, the δ 13 C of animal tissue preserves the δ 13 C value of the vegetation at the base of the food chain (Janssen et al 2016). The majority of global vegetation (>90%) uses the C 3 photosynthetic pathway, whereas the remainder is split between the C 4 and CAM (Crassulacean acid metabolism) pathways—both adaptations to hot, arid environments through increased water use efficiency and reduced photorespiration (Ehleringer and Monson 1993; Ehleringer et al 1992; Kohn 2010).…”
Section: Isotope Analyses As a Source Of Assessing Dietary And Enviromentioning
confidence: 99%
“…CAM plants have a range of value but typically fall closer to the C 4 range; nevertheless, CAM plants (e.g., succulents, orchids) rarely contribute to human diets and therefore are not considered as a food source in this study. The δ 13 C values of C 3 plants can be further influenced by environmental factors; water stress results in higher δ 13 C values, and a closed canopy environment shifts δ 13 C to very low values (Janssen et al 2016; Kohn 2010; Van der Merwe and Medina 1991). More positive δ 13 C values in vegetation and animal tissues may indicate a habitat with more open vegetation.…”
Section: Isotope Analyses As a Source Of Assessing Dietary And Enviromentioning
confidence: 99%