Late Pleistocene-Holocene coastal adaptation in central Mediterranean: Snapshots from Grotta d'Oriente (NW Sicily)

被引:14
|
作者
Colonese, A. C. [1 ]
Lo Vetro, D. [2 ,3 ]
Landini, W. [4 ]
Di Giuseppe, Z.
Hausmann, N. [1 ,5 ]
Demarchi, B. [1 ,6 ]
d'Angelo, C. [1 ]
Leng, M. J. [7 ,8 ]
Incarbona, A. [9 ]
Whitwood, A. C. [10 ]
Martini, F. [2 ,3 ]
机构
[1] Univ York, Dept Archaeol, BioArCh, York YO10 5DD, N Yorkshire, England
[2] Univ Firenze, Sez Archeol & Antico Oriente, Dipartimento Storia Archeol Geog Arte & Spettacol, Via S Gallo 10, I-50129 Florence, Italy
[3] Museo & Ist Fiorentino Preistoria, Via S Egidio 21, I-50122 Florence, Italy
[4] Univ Pisa, Dipartimento Sci Terra, Via Santa Maria 53, I-56126 Pisa, Italy
[5] Fdn Res & Technol Hellas, Inst Elect Struct & Laser, Nik Plastira 100, Iraklion 70013, Greece
[6] Univ Torino, Dipartimento Sci Vita & Biol Sisterni, V Accad Albertina 13, I-10123 Turin, Italy
[7] British Geol Survey, NERC Isotope Geosci Facil, Nottingham NG12 5GG, England
[8] Univ Nottingham, Sch Biosci, Ctr Environm Geochem, Sutton Bonington Campus, Loughborough, Leics, England
[9] Univ Palermo, Dipartimento Sci Terra & Mare, Via Archirafi 22, I-90123 Palermo, Italy
[10] Univ York, Dept Chem, York YO10 5DD, N Yorkshire, England
关键词
Central Mediterranean; NW Sicily; Upper Palaeolithic to Early Neolithic; Coastal adaptation; Environmental change; MARINE MOLLUSK EXPLOITATION; HUNTER-GATHERER SUBSISTENCE; STABLE-ISOTOPE ANALYSIS; LAST GLACIAL MAXIMUM; SAN-MIGUEL ISLAND; SEA-LEVEL; OSILINUS-TURBINATUS; LITTORAL RESOURCES; OXYGEN ISOTOPES; ALBORAN SEA;
D O I
10.1016/j.quaint.2018.06.018
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Marine faunal remains from Grotta d'Oriente (Favignana Island, NW Sicily) offer invaluable snapshots of human coastal environment interaction in the central Mediterranean from the Late Pleistocene to the Middle Holocene. The long-term shellfish and fish records reflect human exploitation of coastal environments undergoing considerable reorganizations during the postglacial sea level rise and the progressive isolation of Favignana from mainland Sicily. We detected an intensification of marine resource exploitation between similar to 9.6 ka and similar to 7.8 ka BP, which corresponds with the isolation of Favignana Island and, later on, with the introduction of early agro-pastoral economy in this region. We suggest that a higher investment in marine resource exploitation by late foragers and early farmers in NW Sicily was also supported by an increase in marine productivity in the south Tyrrhenian Sea in the Middle Holocene.
引用
收藏
页码:114 / 126
页数:13
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