Carbon, nitrogen, and oxygen isotopes of ostrich eggshells provide site-scale Pleistocene-Holocene paleoenvironmental records for eastern African archaeological sites

被引：7

作者：

Niespolo, E. M. ^{[1
,2
]}

Sharp, W. D. ^{[2
]}

Tryon, C. A. ^{[3
]}

Faith, J. T. ^{[4
,5
]}

Lewis, J. ^{[6
,7
]}

Ranhorn, K. ^{[10
]}

Mambelli, S. ^{[8
]}

Miller, M. J. ^{[9
]}

Dawson, T. E. ^{[8
]}

机构：

[1] Univ Calif Berkeley, Dept Earth & Planetary Sci, Berkeley, CA 94720 USA

[2] Berkeley Geochronol Ctr, Berkeley, CA USA

[3] Univ Connecticut, Dept Anthropol, Storrs, CT USA

[4] Univ Utah, Nat Hist Museum Utah, Salt Lake City, UT USA

[5] Univ Utah, Dept Anthropol, Salt Lake City, UT 84112 USA

[6] SUNY Stony Brook, Turkana Basin Inst, Stony Brook, NY 11794 USA

[7] SUNY Stony Brook, Dept Anthropol, Stony Brook, NY 11794 USA

[8] Univ Calif Berkeley, Dept Integrat Biol, Berkeley, CA 94720 USA

[9] Univ Calif Berkeley, Archaeol Res Facil, Berkeley, CA 94720 USA

[10] Arizona State Univ, Sch Human Evolut & Social Change, Tempe, AZ USA

来源：

QUATERNARY SCIENCE REVIEWS | 2020年 / 230卷

基金：

美国国家科学基金会;

关键词：

Africa; Stable isotopes; Ostrich eggshell; Quaternary paleoecology; Paleoclimatology; Middle Stone Age; Later Stone Age; LATER STONE-AGE; LOW-LEVEL JET; STABLE-ISOTOPES; SOUTH-AFRICA; ENVIRONMENTAL-CHANGE; GLOBAL PATTERNS; LUKENYA HILL; LEAF WATER; LAKE EYASI; CLIMATE;

D O I：

10.1016/j.quascirev.2019.106142

中图分类号：

P9 [自然地理学];

学科分类号：

0705 ; 070501 ;

摘要：

Quantitative, well-dated, local paleoenvironmental records are necessary to 1) evaluate responses to regional to global-scale climate change at the scale of human habitats, and 2) test hypotheses regarding the effects of environmental change and human biological and cultural evolution. Ostrich eggshell (OES) fragments are common in African archaeological sequences, are amenable to C-14 and Th-230/U dating, and their stable carbon (delta C-13 values) and nitrogen (delta N-15 values) isotopic compositions track local vegetation and mean annual precipitation (MAP), respectively. We review previous interpretations of the stable isotopic composition of OES, apply a novel calibration to estimate paleo-MAP (PMAP) from delta N-15 values, and show that oxygen isotopes (delta O-18 values) record evapotranspiration, which is controlled by temperature, relative humidity, and/or photosynthetic performance, if other components of the water cycle are constrained. The stable isotopic compositions of the organic fraction of OES remain unaltered to at least similar to 50 ka, indicating potential to examine even older OES. We present a similar to 50-4 ka record of OES delta C-13, delta N-15, and delta O-18 values from archaeological sites recording the Middle to Later Stone Age (MSA/LSA) transition at Lukenya Hill (Kenya) and Kisese II (Tanzania). Stable isotope proxies indicate contrasting but subtle changes in local paleoenvironment throughout the records at both sites, likely explained by local ecological and climatological effects that are not resolved by regional-scale paleoclimate records. These records highlight the need for additional local studies to assess the covariance of paleoenvironments and material culture. Furthermore, they indicate that the MSA/LSA transition at the two sites did not result from paleoenvironmental change. (C) 2019 Elsevier Ltd. All rights reserved.

引用

页数：20