Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Ciprian Astalos"'
Mountain landscapes were first exploited by farming populations at the very beginning of the Neolithic. However, there are controversies regarding when and where these specific types of human behaviour developed as a result of adaptation processes to
Publikováno v:
Journal of Archaeological Science. 104:19-33
The study of size and shape of ceramic fragments is a common approach used for unraveling the depositional and post-depositional history of archaeological assemblages. Similar to sediment particles, the size and shape of a potsherd are altered under
Publikováno v:
Materiale și Cercetări Arheologice, Vol 14, Pp 13-23 (2018)
Boroneanț, A, Virag, C, Astaloș, C & Bonsall, C 2018, ' Sourcing obsidian from prehistoric sites in northwest Romania ', Materiale şi Cercetari Arheologice, vol. N.S. 14, pp. 13-23 .
University of Edinburgh-PURE
Boroneanț, A, Virag, C, Astaloș, C & Bonsall, C 2018, ' Sourcing obsidian from prehistoric sites in northwest Romania ', Materiale şi Cercetari Arheologice, vol. N.S. 14, pp. 13-23 .
University of Edinburgh-PURE
Portable X‐ ray Fluorescence Spectroscopy (pXRF) was used to reveal the chemical signatures of 75 obsidian artefacts from seven sites in the Satu Mare region, ranging in age from Early Neolithic (late Starčevo‐ Criș culture) to Late Copper Age.
Autor:
Thomas Hickler, Alida Timar-Gabor, Ciprian Astalos, Elena Marinova, Angelica Feurdean, Daniel Veres, Johan Liakka, Mihály Braun, Simon M. Hutchinson, Volker Mosburgger, Anne Birgitte Nielsen
Publikováno v:
Journal of Biogeography. 42:951-963
Aim The forest steppe of the Transylvanian Plain is a landscape of exceptionally diverse steppe-like and semi-natural grasslands. Is this vegetation a remnant of a once continuous temperate forest extensively cleared by humans, or has the area, since
Publikováno v:
The Holocene. 19:967-981
The Apuseni Natural Park (ANP) in northwestern Romania was founded in 1990 to protect the old-growth forests in this region and their high species diversity. We present results from palaeoecological investigation (pollen, micro- and macrocharcoal) of