Geoarchaeology of Pleistocene open-air sites in the Vila Nova da Barquinha-Santa Cita area (Lower Tejo River basin, central Portugal)

被引:29
作者
Martins, Antonio A. [1 ]
Cunha, Pedro P. [2 ]
Rosina, Pierluigi [3 ]
Osterbeek, Luiz [3 ]
Cura, Sara [4 ]
Grimaldi, Stefano [5 ]
Gomes, Jose [6 ]
Buylaert, Jan-Pieter [7 ]
Murray, Andrew S. [7 ]
Matos, Joao [8 ]
机构
[1] Univ Evora, Dept Geociencias, Ctr Geofis, P-7000671 Evora, Portugal
[2] Univ Coimbra, Dept Earth Sci, Marine & Environm Res Ctr, P-3000 Coimbra, Portugal
[3] Univ Coimbra, Inst Politecn Tomar, Ctr Geociencias, P-3000 Coimbra, Portugal
[4] Univ Coimbra, Museu Arte Prehist Macdo, Ctr Geociencias, P-3000 Coimbra, Portugal
[5] Univ Coimbra, Univ Studi Trento, Ctr Geociencias, P-3000 Coimbra, Portugal
[6] Univ Coimbra, Ctr Interpretacdo Arqueol Alto Ribatejo, Ctr Geociencias, P-3000 Coimbra, Portugal
[7] Aarhus Univ, Nord Lab Luminescence Dating, Rise Dtu, Denmark
[8] Univ Evora, Dept Geociencias, Bolseiro BIC Proj POCI CTE GEX 58120 2004, P-7000671 Evora, Portugal
关键词
Palaeolithic; Pleistocene; Luminescence dating; Terraces; Tejo River; Iberia; TAGUS VALLEY; CENTRAL SPAIN; LUMINESCENCE; TERRACES; DEPOSITS; RODAO;
D O I
10.1016/j.pgeola.2010.01.005
中图分类号
P5 [地质学];
学科分类号
070403 [天体物理学];
摘要
This paper aims to provide insight into human occupation and landscape change during the Pleistocene in a central area of the Lower Tejo basin (Portugal). Detailed geomorphological mapping, coupled with lithostratigraphy, sedimentology and luminescence dating, supports the identification of a complete terrace staircase sequence. It consists of six gravely terraces located below the culminant (Pliocene) basin unit. A chronological framework for the sedimentary sequences and associated human industries is proposed and correlated with marine oxygen isotope stages (MIS): T1 terrace, not dated; T2, not dated; T3, >300 ka; T4, similar to 300-160 ka (MIS8, MIS7 and MIS6); T5, similar to 136-75 ka (MIS5); T6, similar to 62-30 ka (MIS3); colluvium and aeolian sands, similar to 30-14 ka (MIS2); valley fill deposits, similar to 14 ka to present (MIS1). The oldest artefacts were found at the base of the T4 terrace, with the local stratigraphic level dated to >= 175 +/- 6 ka (Middle Pleistocene). The lithic assemblages collected from distinct stratigraphic levels (T4, T5 top, T6 terraces and colluvium) are characterized by the predominance of opportunistic technological choices, a feature that can be attributed partly to the preferential exploitation of the available raw material, dominated by local-sourced quartzites and quartz pebbles. The adaptation to local raw material (texture and volume), together with subsistence patterns and behaviours, could explain the rarity of Acheulian types (handaxes and cleavers) and picks in the T4 terraces of the Tejo tributaries; this is in contrast to the same terrace of the Tejo valley, in which these types are found. Interpretation of the environmental conditions (controlled by climate and glacio-eustatic sea-level changes) affecting the hunter-gatherer human groups is also presented. (C) 2010 The Geologists' Association. Published by Elsevier Ltd. All rights reserved.
引用
收藏
页码:128 / 140
页数:13
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