Continuity or discontinuity in the European Early Pleistocene human settlement: the Atapuerca evidence

被引:58
|
作者
Maria Bermudez de Castro, Jose [1 ]
Martinon-Torres, Maria [1 ]
Blasco, Ruth [2 ]
Rosell, Jordi [3 ,4 ]
Carbonell, Eudald [3 ,4 ,5 ]
机构
[1] Ctr Natl Invest Evoluc Humana CENIEH, Burgos 09002, Spain
[2] Gibraltar Museum, Gibraltar, Gibraltar
[3] Univ Rovira & Virgili, Area Prehist, Tarragona 43002, Spain
[4] Inst Catala Paleoecol Humana & Evolucio Social, Tarragona 43003, Spain
[5] IVPP, Beijing, Peoples R China
关键词
Early Pleistocene; Europe; Atapuerca; SIMA DEL ELEFANTE; GEOMETRIC MORPHOMETRIC-ANALYSIS; EARLY HUMAN OCCUPATION; GRAN-DOLINA SITE; MIDDLE-PLEISTOCENE; SUBSISTENCE STRATEGIES; ARCHAEOLOGICAL-SITE; DENTAL DEVELOPMENT; PALEOLITHIC SITES; EARLIEST EVIDENCE;
D O I
10.1016/j.quascirev.2013.06.023
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The nature, timing, pattern, favourable circumstances and impediments of the human occupation of the European continent during the Early Pleistocene are hot topics in Quaternary studies. In particular, the problem of the (dis) continuity of the settlement of Europe in this period is an important matter of discussion, which has been approached in the last decade from different points of view. The Gran Dolina (TD) and Sima del Elefante (TE) cave sites in the Sierra de Atapuerca, (Spain) include large and quasi-continuous stratigraphic sequences that stretch back from at least 1.2 million years ago (Ma) to the Matuyama/Brunhes boundary. The archaeological and paleontological record from these sites can help to test different hypotheses about the character of the human settlement in this region and period. Furthermore, the TD6 level has yielded a large collection of human fossil remains attributed to Homo antecessor. According to different geochronological methods, as well as to paleomagnetic and bio-stratigraphical analyses, these hominins belong to an age range of 0.96-0.80 Ma. Unfortunately, the finding in 2007 of some human fossil remains in the TE9 level, dated to about 1.22 Ma, was not enough to conclude whether H. antecessor had deep roots in the European Early Pleistocene. A set of derived features of H. antecessor shared with both the Neanderthal lineage and modern humans suggests that this species is related, and not far, from the most recent common ancestor (MRCA) of Homo neanderthalensis and Homo sapiens. If we assume that there was a lineal biological relationship between the TE9 and TD6 hominins, we should reconsider many of the conclusions achieved in previous paleontological and genetic studies. In addition, we would be obliged to build a highly complicated paleogeographical scenario for the origin of the MRCA. Although continuity in the settlement of Europe during the entire late Early Pleistocene is not discarded (e.g. in refuge areas), it seems that this Western extreme of Eurasia, and the Iberian Peninsula in particular, was occupied by at least two different hominin populations. (c) 2013 Elsevier Ltd. All rights reserved.
引用
收藏
页码:53 / 65
页数:13
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