Geoarchaeology in an urban context: the uses of space in a Phoenician monumental building at Tel Dor (Israel)

被引:126
作者
Shahack-Gross, R [1 ]
Albert, RM
Gilboa, A
Nagar-Hilman, O
Sharon, I
Weiner, S
机构
[1] Weizmann Inst Sci, Dept Struct Biol, IL-76100 Rehovot, Israel
[2] Univ Barcelona, ICREA, Dept Prehist Ancient Hist & Archaeol, E-08028 Barcelona, Spain
[3] Univ Haifa, Zinman Inst Archaeol, IL-31905 Haifa, Israel
[4] Hebrew Univ Jerusalem, Inst Archaeol, IL-91905 Jerusalem, Israel
关键词
mineralogy; micromorphology; phoenician architecture; phytoliths; Tel Dor; iron age; site formation processes;
D O I
10.1016/j.jas.2005.04.001
中图分类号
Q98 [人类学];
学科分类号
030303 ;
摘要
Interpretation of past urban societies in the Near East, whose settlements are known mostly as tell sites, is largely based on macro-stratigraphy and on the association of architecture with macroscopic artifacts. Analyses of sediments, common in prehistoric sites, are rare in tell sites. Here we show the results of a detailed geoarchaeological study of the micro-stratigraphy of a sedimentary sequence associated with early Iron Age Phoenician monumental architecture. The study involves mineralogical, micromorphological and phytolith analyses and provides new insights into the stratigraphic sequence and the use of architectural spaces. The sedimentary sequence examined comprises alternating layers of gray 'fill' deposits and white 'floors'. We show that 'floors' made from local calcareous sandstone in the lower part of the sedimentary sequence were heated and are thus in effect 'plaster floors'. A concentration of micro-laminated, trampled fish remains above the most elaborate of these plaster 'floors' indicates activities related to fish processing. Fine white layers in the upper part of the sedimentary sequence that were considered as plaster based on macroscopic examination are in fact composed almost entirely of opaline grass phytoliths. The phytoliths appear in an undulating micro-laminated structure and are associated with dung spherulites and phosphate nodules, thus probably reflecting livestock penning. The formation of 'phytolith floors' involves extensive volume reduction due to the degradation of the organic material and this may result in 'floor' subsidence, a phenomenon that is often observed in archaeological sites. Most 'fill' deposits include macroscopic and microscopic remains of wood ash, bones, phytoliths, charcoal, ceramics, plaster and mollusk shells, reflecting the debris produced from household activities. This study shows how a combination of macro-stratigraphy with microscopic and mineralogical analyses of the sediments within architectural spaces can provide information on the varying ways in which the space was used through time, and also contributes to solving macro-stratigraphic problems. (c) 2005 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1417 / 1431
页数:15
相关论文
共 44 条
[1]  
Affonso M.T.C, 1996, OLD POTTERS ALMANAK, V4, P1
[2]   Mode of occupation of Tabun Cave, Mt Carmel, Israel during the Mousterian Period: A study of the sediments and phytoliths [J].
Albert, RM ;
Lavi, O ;
Estroff, L ;
Weiner, S ;
Tsatskin, A ;
Ronen, A ;
Lev-Yadun, S .
JOURNAL OF ARCHAEOLOGICAL SCIENCE, 1999, 26 (10) :1249-1260
[3]  
Albert RM, 2001, PHYTOLITHS: APPLICATIONS IN EARTH SCIENCES AND HUMAN HISTORY, P251
[4]  
ALBERT RM, UPPER MIDDLE PALEOLI, V1
[5]   OPTICAL PETROGRAPHY AS A TOOL FOR EXAMINING GYPSUM AND LIME PLASTER PYROTECHNOLOGY [J].
BARNETT, WK .
JOURNAL OF FIELD ARCHAEOLOGY, 1991, 18 (02) :253-255
[6]   SHEPHERDS AND SEDIMENTS - GEO-ETHNOARCHAEOLOGY OF PASTORAL SITES [J].
BROCHIER, JE ;
VILLA, P ;
GIACOMARRA, M ;
TAGLIACOZZO, A .
JOURNAL OF ANTHROPOLOGICAL ARCHAEOLOGY, 1992, 11 (01) :47-102
[8]  
Bullock P., 1985, Handbook for soil thin section description.
[9]   The production and preservation of faecal spherulites: Animals, environment and taphonomy [J].
Canti, MG .
JOURNAL OF ARCHAEOLOGICAL SCIENCE, 1999, 26 (03) :251-258
[10]   An investigation of microscopic calcareous spherulites from herbivore dungs [J].
Canti, MG .
JOURNAL OF ARCHAEOLOGICAL SCIENCE, 1997, 24 (03) :219-231