2017
DOI: 10.1016/j.quaint.2015.12.033
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Neandertal subsistence strategies during the Quina Mousterian at Roc de Marsal (France)

Abstract: Recent excavations at the cave site of Roc de Marsal (in the Dordogne region of SW France) have yielded several Mousterian assemblages rich in well-preserved faunal remains. The Layer 4 faunal assemblage, associated with a rich Quina Mousterian occupation, provides an opportunity to investigate Neandertal prey selection, transport decisions and reindeer carcass processing strategies. One of the most striking characteristics of the Roc de Marsal Layer 4 faunal assemblage is an apparent lack of spongy parts that… Show more

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Cited by 36 publications
(37 citation statements)
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“…For both Pech de l'Azé IV and Roc de Marsal, while understanding the duration and intensity of individual occupation events is difficult at best, it is clear that these were both consistently used as occupation sites. The significant concentrations of stone tools (made and used in all components of both sites) and heavily butchered faunal remains throughout the entire sequences (Castel et al 2016;Hodgkins et al 2016;Niven 2013) are evidence of this. It would be very difficult to argue that at times, the sites served more ephemeral purposes (e.g., that they were kill sites or secondary butchery sites) where the use of fire may have been less likely.…”
Section: How Can We Explain These Patterns?mentioning
confidence: 96%
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“…For both Pech de l'Azé IV and Roc de Marsal, while understanding the duration and intensity of individual occupation events is difficult at best, it is clear that these were both consistently used as occupation sites. The significant concentrations of stone tools (made and used in all components of both sites) and heavily butchered faunal remains throughout the entire sequences (Castel et al 2016;Hodgkins et al 2016;Niven 2013) are evidence of this. It would be very difficult to argue that at times, the sites served more ephemeral purposes (e.g., that they were kill sites or secondary butchery sites) where the use of fire may have been less likely.…”
Section: How Can We Explain These Patterns?mentioning
confidence: 96%
“…Although faunal data are incomplete for Roc de Marsal, it is clear that while the prey species varies throughout both site sequences, the kinds of anatomical elements represented are virtually indistinguishable in layers with fire versus those without (see fig. 5; Castel et al 2016;Hodgkins et al 2016;Dibble et al 2017, pt. 3).…”
Section: How Can We Explain These Patterns?mentioning
confidence: 99%
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“…The use of projectile technology permits the targeting of a wider variety of large-to medium-sized terrestrial game while, importantly, mitigating risk by allowing the killing of prey at a distance. Despite ample evidence that Neanderthals were skilled and proficient hunters in a range of environments and across a broad time range (Gaudzinski 1995(Gaudzinski , 1999Steele 2004;Niven et al 2012;Gaudzinski-Windheuser et al 2014aSmith 2015;Castel et al 2017;Jaouen et al 2019), there is an absence of either clearly identifiable projectile points or impact damage from Middle Palaeolithic contexts, compared to other time periods (Table 1) (Noe-Nygaard 1973;Austin et al 1999;Smith 2010Smith , 2013Gaudzinski-Windheuser et al 2018). Invariably, this has led to the hypothesis that the absence of both recognisable projectile technology and hunting lesions before the late Upper Palaeolithic is simply that these implements were not a regular part of hunting technology (Gaudzinski-Windheuser 2016).…”
Section: Resultsmentioning
confidence: 99%
“…Based on a number of recent numeric dates obtained through a variety of techniques (Guérin et al 2012; Jankowski 2018), we are able to demonstrate the overlap in the sequences of Roc de Marsal and Pech IV and tentatively assign them to various OIS stages. However, we used other data, such as macrofauna (Hodgkins 2018;Hodgkins et al 2016;Niven 2013Niven , 2018Castel et al 2016), microfauna (Marquay as reported in Sandgathe et al 2008), phytoliths (Cabanes as reported in Sandgathe et al 2008), and sedimentology (Sandgathe et al 2008;Goldberg et al 2018) to reach conclusions about the climate at the time a layer was being deposited Reille and De Beaulieu, 1990) and the occupations took place. Not only at Roc de Marsal and Pech IV, but also at other sites, for example, La Ferrassie, La Quina, Chez Pinaud Jonzac, and Abri Peyrony, there is particularly good faunal preservation resulting in significant assemblages for paleontological analysis and paleoclimatic reconstruction, corroborated by chronometric dates and geological evidence.…”
Section: How Well Does the Evidence Hold Up At Other Sites?mentioning
confidence: 99%