Response to Comment on "Permanent human occupation of the central Tibetan Plateau in the early Holocene"

被引：0

作者：

Meyer, M. C. ^{[1
]}

Hoffmann, D. L. ^{[2
]}

Aldenderfer, M. S. ^{[3
]}

Haas, W. R. ^{[4
]}

Dahl, J. A. ^{[5
]}

Wang, Z. ^{[1
]}

Degering, D. ^{[6
]}

Schluetz, F. ^{[7
]}

机构：

[1] Univ Innsbruck, Inst Geol, A-6020 Innsbruck, Austria

[2] Max Planck Inst Evolutionary Anthropol, Dept Human Evolut, D-04103 Leipzig, Germany

[3] Univ Calif Merced, Sch Social Sci Humanities & Arts, Merced, CA 95343 USA

[4] Univ Wyoming, Dept Anthropol, Laramie, WY 82071 USA

[5] Natl Isotope Ctr, Inst Geol & Nucl Sci GNS Sci, Lower Hutt 5040, New Zealand

[6] ADD Ideas Albrecht & Detlev Degering, Zum Erzengel Michael 19, D-01723 Mohorn, Germany

[7] Lower Saxony Inst Hist Coastal Res, D-26382 Wilhelmshaven, Germany

来源：

SCIENCE | 2017年 / 357卷 / 6351期

关键词：

MULTIPLE GRAINS; SINGLE; DEPOSITS; QUARTZ; SEDIMENTS; MODELS;

D O I：

10.1126/science.aan8575

中图分类号：

O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];

学科分类号：

07 ; 0710 ; 09 ;

摘要：

We show that Zhang and Li's sedimentological model for the Chusang travertine neglects the three-dimensional information from multiple outcrops and that their optically stimulated luminescence (OSL) age of about 20,000 years for the human imprints is untenable. We highlight the robustness of our chronology and explore reasons why Zhang and Li's OSL age is a gross overestimation of the real depositional age of the imprinted travertine.

引用

页数：3

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