Isotopic evidence for an early shift to C4 resources by Pliocene hominins in Chad

被引:88
|
作者
Lee-Thorp, Julia [1 ]
Likius, Andossa [2 ]
Mackaye, Hassane T. [2 ]
Vignaud, Patrick [3 ]
Sponheimer, Matt [4 ]
Brunet, Michel [3 ,5 ]
机构
[1] Univ Oxford, Res Lab Archaeol, Oxford OX1 3QY, England
[2] Univ NDjamena, Dept Paleontol, Ndjamena, Chad
[3] Univ Poitiers, CNRS, Unite Mixte Rech 7262, Inst Paleoprimatol Paleontol Humaine Evolut & Pal, F-86022 Poitiers, France
[4] Univ Colorado, Dept Anthropol, Boulder, CO 80309 USA
[5] Coll France, Chaire Paleontol Humaine, F-75232 Paris 05, France
基金
美国国家科学基金会;
关键词
UNDERGROUND-STORAGE ORGANS; PLANT FOODS; AUSTRALOPITHECUS-BAHRELGHAZALI; FALLBACK FOODS; DIET; ECOLOGY; STERKFONTEIN; SEASONALITY; EVOLUTION; MICROWEAR;
D O I
10.1073/pnas.1204209109
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
Foods derived from C-4 plants were important in the dietary ecology of early Pleistocene hominins in southern and eastern Africa, but the origins and geographic variability of this relationship remain unknown. Carbon isotope data show that Australopithecus bahrelghazali individuals from Koro Toro in Chad are significantly enriched in C-13, indicating a dependence on C-4 resources. As these sites are over 3 million years in age, the results extend the pattern of C-4 dependence seen in Paranthropus boisei in East Africa by more than 1.5 million years. The Koro Toro hominin fossils were found in argillaceous sandstone levels along with abundant grazing and aquatic faunal elements that, in combination, indicate the presence of open to wooded grasslands and stream channels associated with a greatly enlarged Lake Chad. In such an environment, the most abundant C-4 plant resources available to A. bahrelghazali were grasses and sedges, neither of which is usually considered as standard great ape fare. The results suggest an early and fundamental shift in hominin dietary ecology that facilitated the exploitation of new habitats.
引用
收藏
页码:20369 / 20372
页数:4
相关论文
共 24 条
  • [21] A strongly positive sulphur isotopic shift in late Ediacaran-early Cambrian seawater: evidence from evaporites in the Salt Range Formation, northern Pakistan
    Meng, Fanwei
    Zhang, Zhili
    Bukowski, Krzysztof
    Zhuo, Qingong
    Ahsan, Naveed
    Ur-Rehman, Saif
    Ni, Pei
    GEOLOGICAL QUARTERLY, 2021, 65 (02):
  • [22] Carbon isoscapes of rodent diets in the Great Plains USA deviate from regional gradients in C4 grass abundance due to a preference for C3 plant resources
    Haveles, Andrew W.
    Fox, David L.
    Fox-Dobbs, Kena
    PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 2019, 527 : 53 - 66
  • [23] Late Miocene changes in C3, C4 and aquatic plant vegetation in the Indus River basin: evidence from leaf wax δ13C from Indus Fan sediments
    Suzuki, Kenta
    Yamamoto, Masanobu
    Seki, Osamu
    GEOLOGICAL MAGAZINE, 2020, 157 (06) : 979 - 988
  • [24] Early indicators to C4 plant consumption in central Kazakhstan during the Final Bronze Age and Early Iron Age based on stable isotope analysis of human and animal bone collagen
    Ananyevskaya, E.
    Aytqaly, A. K.
    Beisenov, A. Z.
    Dmitriev, E. A.
    Garbaras, A.
    Kukushkin, I. A.
    Loman, V. G.
    Sapolaite, J.
    Usmanova, E. R.
    Varfolomeev, V. V.
    Voyakin, D. A.
    Zhuniskhanov, A. S.
    Matuzeviciute, Motuzaite G.
    ARCHAEOLOGICAL RESEARCH IN ASIA, 2018, 15 : 157 - 173