TY - JOUR

T1 - Reconstructing the environmental conditions experienced by early modern humans at Tam Pà Ling (northeast Laos) using higher plant wax biomarkers

AU - McAllister-Hayward, M. S.

AU - Blyth, A. J.

AU - McInerney, F. A.

AU - Holman, A. I.

AU - Grice, K.

AU - Tyler, J. J.

AU - Westaway, K. W.

AU - Joannes-Boyau, R.

AU - Boualaphane, S.

AU - Bourgon, N.

AU - Dunn, T. E.

AU - Frangeul, S.

AU - Luangkhoth, T.

AU - Ponche, J.-L.

AU - Sichanthongtip, P.

AU - Souksavatdy, V.

AU - Suzzoni, E.

AU - Zachwieja, A.

AU - Zanolli, C.

AU - Bacon, A.-M.

AU - Duringer, P.

AU - Hublin, J.-J.

AU - Shackelford, L.

AU - Demeter, F.

AU - Morley, M. W.

N1 - Publisher Copyright: © 2024 The Authors

PY - 2024

Y1 - 2024

N2 - The sediments of Tam Pà Ling (TPL), northeastern Laos, have yielded the earliest evidence of Homo sapiens in mainland Southeast Asia (∼86 ka; marine isotope stage (MIS) 5 b) with a number of skeletal elements having been recovered from the sequence attesting to two populations of H. sapiens present in the vicinity between 77 ± 9 ka to 39 ± 9 ka. At present there has been very limited research into the environmental conditions that these populations encountered during MIS 5–4. In this study, we present the results of an analysis of higher plant biomarkers (n-alkanes and n-alkanols) from the sediments at TPL to reconstruct the palaeovegetation of the site and the human fossils. The n-alkane δ13C values demonstrate that H. sapiens encountered a predominantly C3 forest landscape in MIS 5 b-MIS 4 that prevailed until MIS 1. Observations of a fluctuation in δ13C values across MIS 5 b-MIS 1 (∼86–3 ka) indicates that moisture availability was non-uniform, most likely resulting in landscape changes in and around TPL. The presence of H. sapiens at TPL during the environmental conditions associated with MIS 5 b-MIS 3 highlights the adaptability of our species to environmental dynamics at this time.

AB - The sediments of Tam Pà Ling (TPL), northeastern Laos, have yielded the earliest evidence of Homo sapiens in mainland Southeast Asia (∼86 ka; marine isotope stage (MIS) 5 b) with a number of skeletal elements having been recovered from the sequence attesting to two populations of H. sapiens present in the vicinity between 77 ± 9 ka to 39 ± 9 ka. At present there has been very limited research into the environmental conditions that these populations encountered during MIS 5–4. In this study, we present the results of an analysis of higher plant biomarkers (n-alkanes and n-alkanols) from the sediments at TPL to reconstruct the palaeovegetation of the site and the human fossils. The n-alkane δ13C values demonstrate that H. sapiens encountered a predominantly C3 forest landscape in MIS 5 b-MIS 4 that prevailed until MIS 1. Observations of a fluctuation in δ13C values across MIS 5 b-MIS 1 (∼86–3 ka) indicates that moisture availability was non-uniform, most likely resulting in landscape changes in and around TPL. The presence of H. sapiens at TPL during the environmental conditions associated with MIS 5 b-MIS 3 highlights the adaptability of our species to environmental dynamics at this time.

KW - Homo sapiens

KW - n-alkanes

KW - n-alkanols

KW - palaeoenvironments

KW - stable isotopes

U2 - 10.1016/j.quascirev.2023.108471

DO - 10.1016/j.quascirev.2023.108471

M3 - Journal article

AN - SCOPUS:85182272881

VL - 325

JO - Quaternary Science Reviews

JF - Quaternary Science Reviews

SN - 0277-3791

M1 - 108471

ER -