globalchange  > 气候减缓与适应
DOI: 10.1016/j.quascirev.2017.11.006
Scopus记录号: 2-s2.0-85034028389
论文题名:
The silence of the layers: Archaeological site visibility in the Pleistocene-Holocene transition at the Ebro Basin
作者: Alday A.; Domingo R.; Sebastián M.; Soto A.; Aranbarri J.; González-Sampériz P.; Sampietro-Vattuone M.M.; Utrilla P.; Montes L.; Peña-Monné J.L.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2018
卷: 184
起始页码: 85
结束页码: 106
语种: 英语
英文关键词: 14C dates ; Archaeological visibility ; Ebro Basin ; Geomorphology ; Magdalenian ; Mesolithic ; Neolithic ; Palaeoclimate ; Pleistocene-Holocene ; Western Europe
Scopus关键词: Architecture ; Geomorphology ; Landforms ; Ebro basin ; Holocenes ; Magdalenian ; Mesolithic ; Neolithic ; Palaeoclimate ; Western Europe ; ^14C dates ; Visibility ; archaeology ; geomorphology ; historical record ; Neolithic ; paleoclimate ; paleoenvironment ; Paleolithic ; Pleistocene-Holocene boundary ; prehistoric ; site effect ; Ebro Basin ; Pyrenees ; Spain
英文摘要: The Ebro Basin constitutes one of the most representative territories in SW Europe for the study of prehistoric societies during the Pleistocene-Holocene transition. The correlation of palaeoenvironmental and geomorphological proxies obtained from sedimentary records with chronologically well-constrained reference archaeological sites has allowed defining this time frame precisely, such that three main pilot areas haven been broadly depicted: the Alavese region, the Pre-Pyrenees and the Bajo Aragón. Overall, the human imprint in the Ebro Basin was rare during the Upper Palaeolithic, but more visible from the Upper Magdalenian (14500–13500 cal BP) to Neolithic times (up to 5500 cal BP). Local environmental resources were continuously managed by the prehistoric communities in the different areas of study. In fact, the Ebro Basin acted during those millennia as a whole, developing the same cultural trends, industrial techniques and settlement patterns in parallel throughout the territory. However, some gaps exist in the 14C frequency curve (SCDPD curve). This is partially related to prehistoric sites in particular lithologies and geological structures that could have partly been lost by erosional processes, especially during the Early Holocene. In addition, this gap also parallels the reconstructed climate trend for the Pre-Pyrenean and the Bajo Aragón areas, which are defined by high frequencies of xerophilous flora until ca. 9500 cal BP, suggesting that continental climate features could have hampered the presence of well-established human communities in inland regions. The interdisciplinary research (archaeology, geomorphology and palaeoclimatology) discussed in this paper offers clues to understand the existence of fills and gaps in the archaeological record of the Ebro Basin, and can be applied in other territories with similar geographic and climate patterns. © 2017 Elsevier Ltd
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/112275
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作者单位: Universidad del País Vasco/EHU, Área Prehistoria, C/ Tomás y Valiente s/n, Vitoria, 01006, Spain; Universidad de Zaragoza, Área Prehistoria, C/Pedro Cerbuna 12, Zaragoza, 50009, Spain; Universidad de Zaragoza, Área Didáctica Ciencias Sociales, C/Pedro Cerbuna 12, Zaragoza, 50009, Spain; Université Toulouse-Jean Jaurès. UMR TRACES, 5 allées A. Machado, Cedex 9, Toulouse, 31058, France; Universidad del País Vasco/EHU. Área Geografía Humana, C/ Tomás y Valiente s/n, Vitoria, 01006, Spain; Instituto Pirenaico de Ecología / CSIC, Campus de Aula Dei, Avda. Montañana 1005, Zaragoza, CP 50159, Spain; Univ Nacional de Tucumán-CONICET, Lab. de Geoarqueología, Miguel Lillo 205, San Miguel de Tucumán, Tucumán 4000, Argentina; Universidad de Zaragoza, Área Geografía Física, C/Pedro Cerbuna 12, Zaragoza, 50009, Spain

Recommended Citation:
Alday A.,Domingo R.,Sebastián M.,et al. The silence of the layers: Archaeological site visibility in the Pleistocene-Holocene transition at the Ebro Basin[J]. Quaternary Science Reviews,2018-01-01,184
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