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Seasons, life cycles and memory in the Danube Gorges, c. 10000-5500 BC

, 2002
This thesis was digitised by the British Library from microfilm. You can acquire a single copy of this thesis for research purposes by clicking on the padlock icon on the thesis file. Please be aware that the text in the supplied thesis pdf file may not be as clear as text in a thesis that was born digital or digitised directly from paper due to the ...
D. Borić
semanticscholar   +2 more sources

Sulphur isotope evidence for freshwater fish consumption: a case study from the Danube Gorges, SE Europe

Journal of Archaeological Science, 2010
Abstract To explore the use of sulphur isotopes as an indicator of the consumption of freshwater fish, we undertook sulphur isotope analysis on bone collagen extracted from humans and animals from five archaeological sites from the Danube Gorges region dating from the Mesolithic to the middle Neolithic periods.
Olaf Nehlich   +3 more
semanticscholar   +5 more sources

Mesolithic-Neolithic Transformations: The Populations of the Danube Gorges

2014
In the Danube Gorges that lie between Serbia and Romania, several archeological sites critical for the understanding of the transitions between the Mesolithic and Neolithic in southeastern Europe have been discovered. In particular, several preserved burial sites, containing around 500 individual skeletal remains, offer a unique opportunity to examine ...
Borić, Dušan   +2 more
openaire   +1 more source

Danube Bend: Miocene Half-Caldera and Pleistocene Gorge

2015
The Danube Bend, a river curvature, called Visegrad Gorge in its deepest and narrowest part, is one of the most picturesque landscapes in Hungary. Its origin and relief evolution has been a long-standing problem in Hungarian earth sciences. A number of geomorphological theories have been put forward in explaining the valley with a U-shaped planform ...
openaire   +1 more source

Quaternary evolution of the Danube along Lower Danube Gorge (Iron Gates) and Oltenia Plain (Romania, SE Europe) – a literature review

Recent investigations on the sedimentary infill of the western Dacian Basin suggest that between ~4.8 Ma and 4.2 Ma (Dacian) the Danube and its tributaries formed a deltaic front at the exit from the Lower Danube Gorge (LDG) known also as Iron Gates. The appearance of a large fluvial system (the proto-Danube) connecting the two basins was dated to ~4.0
Ioana Perșoiu   +4 more
openaire   +1 more source

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