Les industries acheuléennes de la France septentrionale

Tuffreau, Alain; Lamotte, Agnès; Goval, Emilie

doi:10.1016/j.anthro.2008.01.003

Cited by 63 publications

(29 citation statements)

References 22 publications

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“…En el norte de Francia, destacan las dataciones de los yacimientos achelenses de Cagny-la Garenne (448-443 ka) y Cagny l´Epinette (318-289 ka) en niveles de terraza situados entre +40 y +30 m en los valles de los ríos Somme y Sena (Tuffreau et al, 2008;Antoine et al, 2010;Limondin-Lozouet et al, 2010 (Chevrier, 2006). En el curso bajo del río Tajo (Portugal), las dataciones OSL disponibles (Cunha et al, 2008(Cunha et al, , 2012Martins et al, 2009Martins et al, , 2010 indican que las terrazas de c. +30−48 m, con edades de c. 260-340 ka, poseen industrias achelenses (Monte do Famaco), mientras que la terraza inmediatamente inferior (+16−28 m) posee industrias claramente musterienses con fechas comprendidas entre 135 ka (base) y 73 ka (techo), dentro del tránsito Pleistoceno Medio-Superior (MIS 6 -MIS 5).…”

Section: Interpretaciónunclassified

Geocronología de los yacimientos achelenses de Pinedo y Cien Fanegas (Valle del Tajo) e implicaciones en la evolución fluvial en el entorno de Toledo (España)

López-Recio¹,

Silva²,

Roquero³

et al. 2015

Estud. geol.

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Section: Interpretaciónunclassified

Geocronología de los yacimientos achelenses de Pinedo y Cien Fanegas (Valle del Tajo) e implicaciones en la evolución fluvial en el entorno de Toledo (España)

López-Recio¹,

Silva²,

Roquero³

et al. 2015

Estud. geol.

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“…The origins of handaxe-making (Mode 2) behaviour are seen rather later, with the first Acheulean evidence in southern Europe generally appearing at around 600 ka, followed by a rapid colonization of the northwest at 500 ka (Coltorti et al, 2005;Tuffreau et al, 2008;Lefèvre et al, 2010;Jiménez-Arenas et al, 2011;Barsky and de Lumley, 2010;Moncel et al, 2013).…”

Section: Introductionmentioning

confidence: 99%

Climatic control on palaeohydrology and cyclical sediment distribution in the Plio-Quaternary deposits of the Guadix Basin (Betic Cordillera, Spain)

Pla-Pueyo

Viseras

Candy

et al. 2015

Quaternary International

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A cyclical pattern can be observed in the central sector of the Guadix Basin (southern Spain) in the Late Pliocene-Quaternary alluvial fan deposits prograding into its axial valley. A climatic significance has been attributed to this cyclicity on the basis of sedimentological and preliminary isotopic studies. The progradation phases of the alluvial fans are here attributed to more arid time intervals in which the vegetation cover would be less developed, erosion and sediment supply would be higher, and base level would be lower. In contrast, the time intervals during which the fluvial system sediments dominated the area are inferred to be wetter and base level higher, with vegetation cover retaining the soils and preventing erosion. Permanent water supply to the river would therefore facilitate the aggradation of the floodplain and prevent progradation of the fans. Starting from a litho-, bio-and magnetostratigraphical frame provided for the area, an age is assigned to the alternation of the reddish sediments of the transverse alluvial fans and the greyish to white fluvio-lacustrine sediments of the *Manuscript Click here to view linked ReferencesThis is a previous version of the article published in Quaternary International. 2015International. , 389: 56-69. doi:10.1016International. /j.quaint.2015 2 axial drainage system. A cyclicity of ca. 100 ky has been identified in most of the alluvial fan progradation phases, falling within Milankovitch high-frequency eccentricity periodicities. Correlation of the phases with insolation curves is accordingly discussed as a possible origin for the cyclicity. Finally, the results offer new insights into early hominin occupation patterns in the region, through the identification of predictable resources of permanent fresh water that would have remained available throughout the recorded time span (that includes the Early-Middle Pleistocene transition) even during times of aridification.

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“…Sites of this type have been investigated, for example, in the Chalk uplands of southern Britain (Wood Hill, ScottJackson 2000;Caddington, Sampson 1978), in limestone karsts of the Duero River Basin and adjacent plateaus in north-central Spain (Valdecampaňa 4;Diez-Martín et al, 2008), in northern France on interfluvial plateaux in the Somme basin (Gentilles, Tuffreau et al, 2008) and in south-west France (Creysse; Bourguignon et al, 2008;Guibert et al, 2008). Hominins were probably attracted to these sites by the availability of raw material, water supply from ponds formed in the solution hollows and the associated resources that could be utilised from upland locations.…”

Section: Introductionmentioning

confidence: 99%

“…At Gentilles, an infrared stimulated luminescence (IRSL) burial age of 194±21 ka was obtained with the fine grain fraction of reworked calcareous loess that formed the horizon from which horse bone was recovered (Tuffreau et al, 2008). However, in the case of solution hollows the processes that lead to their filling, involving episodic input and reworking of sediment during periods of active solution formation and including subsequent erosional processes, are likely to produce potentially complex sedimentary sequences, and this may account for the generally limited application of luminescence to the dating of the sedimentary fill of such features.…”

Section: Introductionmentioning

confidence: 99%

Luminescence dating of sediments from a Palaeolithic site associated with a solution feature on the North Downs of Kent, UK

Bailiff

Lewis

Drinkall

et al. 2013

Quaternary Geochronology

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White, M. (2013) 'Luminescence dating of sediments from a Palaeolithic site associated with a solution feature on the North Downs of Kent, UK.', Quaternary geochronology., 18 . pp. 135-148. Further information on publisher's website:http://dx.doi.org/10.1016/j.quageo.2013.04.001Publisher's copyright statement: NOTICE: this is the author's version of a work that has been accepted for publication in Quaternary geochronology. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be re ected in this document. Changes may have been made to this work since it was submitted for publication. A de nitive version has been published in Quaternary geochronology, 18, 2013Quaternary geochronology, 18, , 10.1016Quaternary geochronology, 18, /j.quageo.2013 Additional information: Use policyThe full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-pro t purposes provided that:• a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders.Please consult the full DRO policy for further details.

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Les industries acheuléennes de la France septentrionale

Cited by 63 publications

References 22 publications

Geocronología de los yacimientos achelenses de Pinedo y Cien Fanegas (Valle del Tajo) e implicaciones en la evolución fluvial en el entorno de Toledo (España)

Geocronología de los yacimientos achelenses de Pinedo y Cien Fanegas (Valle del Tajo) e implicaciones en la evolución fluvial en el entorno de Toledo (España)

Climatic control on palaeohydrology and cyclical sediment distribution in the Plio-Quaternary deposits of the Guadix Basin (Betic Cordillera, Spain)

Luminescence dating of sediments from a Palaeolithic site associated with a solution feature on the North Downs of Kent, UK

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