Les séquences loessiques pléistocène supérieur d’Havrincourt (Pas-de-Calais, France) : stratigraphie, paléoenvironnements, géochronologie et occupations paléolithiques

Antoine, Pierre; Goval, Emilie; Jamet, Guillaume; Coutard, Sylvie; Moine, Olivier Le; Hérisson, David; Auguste, Patrick; Guérin, Gilles; Schmidt, Esther Dorothe; Robert, Vincent; Debenham, Nick; Meszner, Sascha; Bahain, Jean‐Jacques

doi:10.4000/quaternaire.7278

Cited by 54 publications

(20 citation statements)

References 57 publications

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“…The Middle Gravettian is situated within a period marked by multiple climatic phases, and during this interval one observes a trend towards a general opening of the landscape with respect to vegetation, as well as an increase in the frequency of periglacial features (Andrieux et al, 2018;Antoine et al, 2014). As for the Middle Gravettian Rayssian technical tradition, it is absent from the Pyrenees, and while it partially overlaps the geographic distribution of the Noaillian present north of the Pyrenees, it also extends well into higher latitudes (Klaric, 2017).…”

Section: Discussionmentioning

confidence: 97%

An application of hierarchical Bayesian modeling to better constrain the chronologies of Upper Paleolithic archaeological cultures in France between ca. 32,000–21,000 calibrated years before present

Banks

Bertrán

Ducasse

et al. 2019

Quaternary Science Reviews

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Investigations of chronology play a key role in the majority of archaeological research endeavors and are particularly pertinent to examinations of culture-environment relationships, especially during periods characterized by rapid and marked climatic variability and environmental reorganization. Rigorous evaluations of available data and robust methods are required if one wishes to reconstruct reliable chronologies, and this is especially the case when examining periods that are associated with a relatively few radiometric measurements. Such is the case for the Upper Paleolithic archaeological record documented in present-day France from 32,000 to 21,000 calibrated years BP. We take into account critically examined radiocarbon measurements from contextually secure archaeological contexts and employ a recently-developed method of Hierarchical Bayesian Modeling to reconstruct the chronology of archaeological cultures from the Middle Gravettian to the Badegoulian. The calculated chronological 2 intervals for each typo-technologically defined culture phase are compared to the Greenland ice core climatic record and a terrestrial paleoenvironmental record from Bergsee Lake (Southern Germany)itself expressed in calendar years calculated with the same calibration curve employed in our age model-thereby permitting each archaeological culture to be correlated accurately with documented paleoclimatic variability. 1.1. Late Pleistocene climatic variability 1 LabEx LaScArBx "IMPACT" (W. Banks, dir.) Programme Collectif de Recherches "SaM" (S. Ducasse and C. Renard, dirs.) Programme Collectif de Recherches "Cassegros" (S. Ducasse and J.-M. Le Tensorer, dirs.) Programme Collectif de Recherches "Casserole" (A. Lenoble and L. Detrain, dirs.

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Section: Discussionmentioning

confidence: 97%

An application of hierarchical Bayesian modeling to better constrain the chronologies of Upper Paleolithic archaeological cultures in France between ca. 32,000–21,000 calibrated years before present

Banks

Bertrán

Ducasse

et al. 2019

Quaternary Science Reviews

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“…Six sites contain Levallois points produced by convergent unipolar reduction: Bapaume-les-Osiers (series B, Tuffreau, 1976Tuffreau, , 1987Koehler, 2008), Havrincourt (series N0, Goval et al, 2013;Antoine et al, 2014), Le Pucheuil (series B, Delagnes, 1993;Delagnes and Ropars, 1996), Therdonne (series N3, Locht et al, 2010;H erisson, 2012), Champvoisy (Tuffreau, 1989) and Saint-Illiers-la-Ville (series S2N2, Blaser, 2013) [ Table 1 and Fig. 2].…”

Section: Site Corpus Presentationsmentioning

confidence: 99%

Levallois points and triangular flakes during the Middle Palaeolithic in northwestern Europe: Considerations on the status of these pieces in the Neanderthal hunting toolkit in northern France

Goval

Hérisson

Locht

et al. 2016

Quaternary International

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“…(i) In Figure , the pattern of more oblate AMS fabrics, with original K min directions, within intervals of water‐lain sediments, is not applicable to the whole section; an example is the interval from 135 to 145 m, which is dominated by eolian deposits, if the AMS fabrics are controlled by changes in lithology, the magnetic susceptibility ellipsoid should be prolate, with K min beginning to deviate from the bedding, but this is contrary to what is observed. In addition, the pattern is not applicable to the interval from 7 to 12 m. (ii) Although the magnetic anisotropy can be influenced by the depositional regime, the increase in slope or current can lead to an offset of the K min axes from vertical (Antoine et al, ; Taylor & Lagroix, ). But combine with the shape parameter ( T ) in Figure .…”

Section: Discussionmentioning

confidence: 99%

New Magnetic Constraints on Early‐Middle Miocene Uplift of the Liupan Shan, Northeastern Margin of the Tibetan Plateau

Chen

Xiong

et al. 2019

Geochem Geophys Geosyst

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New constraints on the uplift history of the Liupan Shan can improve our understanding of the tectonic consequences of the collision of the Indian and Asian plates, including the timing of the uplift of the Tibetan Plateau. Here we present a detailed magnetostratigraphy for the Kaimengou section near the piedmont of the Liupan Shan, which reveals that it spans the interval from 19.8 to 12.8 Myr. Together with the results of measurements of the anisotropy of magnetic susceptibility, rock magnetic measurements show that the anisotropy of magnetic susceptibility is dominated by antiferromagnetic hematite and/or paramagnetic minerals, both of which are mainly controlled by the preferred crystallographic orientation, which can be used to record the tectonic history. During 19.5–14.0 Myr, the maximum principal axis (Kmax) showed a pronounced N‐S orientation and Kmin began to exhibit a girdled distribution in an E‐W direction, indicating a slight to moderate tectonic strain in an E‐W direction. And the strain can be reconfirmed be the shape parameter (T). We attribute the strain to far‐field influence by the collision of the Indian and Asian plates. We also present a tentative conceptual model, which explains how the E‐W compression fits within the general tectonic scenario for the uplift of the Tibetan Plateau.

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Les séquences loessiques pléistocène supérieur d’Havrincourt (Pas-de-Calais, France) : stratigraphie, paléoenvironnements, géochronologie et occupations paléolithiques

Cited by 54 publications

References 57 publications

An application of hierarchical Bayesian modeling to better constrain the chronologies of Upper Paleolithic archaeological cultures in France between ca. 32,000–21,000 calibrated years before present

An application of hierarchical Bayesian modeling to better constrain the chronologies of Upper Paleolithic archaeological cultures in France between ca. 32,000–21,000 calibrated years before present

Levallois points and triangular flakes during the Middle Palaeolithic in northwestern Europe: Considerations on the status of these pieces in the Neanderthal hunting toolkit in northern France

New Magnetic Constraints on Early‐Middle Miocene Uplift of the Liupan Shan, Northeastern Margin of the Tibetan Plateau

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