2012
DOI: 10.1017/s0003598x00048195
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Dealul Guran: evidence for Lower Palaeolithic (MIS 11) occupation of the Lower Danube loess steppe

Abstract: Owing to a thick blanket of loess and other later geological disruptions, the earliest hominins to reach Europe are hard to find. To a handful of possible sites, our authors add a new assemblage of lithics with a clear local context and corroborated OSL ages. Ancient humans were present in what is now Romania between 300 000 and 400 000 years ago.

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Cited by 25 publications
(19 citation statements)
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“…Based on our observations, the most common surface material that enters karst and pseudokarst features in Kazakhstan is aeolian loess. Topographic attributes including location, aspect, position, and slope morphology, as well as atmospheric circulation patterns like dust dynamics and wind direction greatly impact the deposition of this wind-blown sediment (Goldberg and Sherwood, 2006;Iovita et al, 2012). Therefore, we expect that local variations in loess cover (currently known on a very coarse scale, Figure 6) would determine the presence or absence of loess in natural cavities.…”
Section: Discussion: Possible Biases In the Archaeological Recordmentioning
confidence: 99%
“…Based on our observations, the most common surface material that enters karst and pseudokarst features in Kazakhstan is aeolian loess. Topographic attributes including location, aspect, position, and slope morphology, as well as atmospheric circulation patterns like dust dynamics and wind direction greatly impact the deposition of this wind-blown sediment (Goldberg and Sherwood, 2006;Iovita et al, 2012). Therefore, we expect that local variations in loess cover (currently known on a very coarse scale, Figure 6) would determine the presence or absence of loess in natural cavities.…”
Section: Discussion: Possible Biases In the Archaeological Recordmentioning
confidence: 99%
“…So far, only a cluster of recently re-excavated archaeological sites in the Romanian Banat (Româneşti-Dumbrăviţa/Coşava/Tincova; [93]) and the Petrovaradin Fortress site in Vojvodina (northern Serbia; [94]) appear to contain the relevant time intervals, but have not yet yielded information regarding tephra deposits, nor is the dating sufficiently precise to be sure that they were occupied at the precise time of the CI super-eruption. Recent systematic survey in Dobrogea has so far documented and dated a number of Palaeolithic sites, constrained to the later Middle Palaeolithic (Cuza Vodă; [95]) and last glacial period [96], but so far no sites have been identified that date to the CI super-eruption or HE4. Given existing data, it remains difficult to evaluate the impact of, and response to, the eruption in Eastern Europe.…”
Section: Discussionmentioning
confidence: 99%
“…Elaborating on this theme, Nikolai Sirakov (Bulgarian Academy of Sciences) and Jean‐Luc Guadelli (Bordeaux) gave a detailed synthesis of the findings from Kozarnika Cave, Bulgaria, which shows human occupation possibly dating back to before one million years ago. Similar issues were addressed by Adrian Dobos (Bucharest), Radu Iovita (Monrepos), and their colleagues, who communicated results from Dealul Guran, the first Lower Paleolithic site to be described in Romania . Valéry Sitlivy (Cologne) discussed in great detail the Balkan typo‐technological variability in lithic assemblages associated with the Middle‐Upper Paleolithic transition, commenting on the Initial/Early Upper Paleolithic technological fusion and the lack of a clear pattern in the geographic and chronological clustering of these “transitional” industries.…”
mentioning
confidence: 72%
“…Similar issues were addressed by Adrian Dobos (Bucharest), Radu Iovita (Monrepos), and their colleagues, who communicated results from Dealul Guran, the first Lower Paleolithic site to be described in Romania. 3 Drawing on his decades-long direction of excavations at renowned sites such as Hohle Fels, Vogelherd, and Geißenkl€ ostere, Conard furnished an excellent outline of the beginnings of the Upper Paleolithic as it is manifested in the Aurignacian findings from the Swabian Jura. He placed the Swabian data in a broader European/Eurasian context and commented on the three known models that have been put forth to interpret social-cultural innovation and the fostering of symbolic capabilities: the Danube corridor hypothesis, the population vacuum hypothesis, and the Kulturpumpe hypothesis.…”
mentioning
confidence: 99%