Changes in ecosystems, climate and societies in the Jura Mountains between 40 and 8 ka cal BP
International audience We present radiometric, palaeoclimatological, palaeoenvironmental and archaeological data for the period 40 000–8000 cal BP in the Jura Mountains (eastern France). These mountains culminate at ∼1700 m a.s.l. and are today characterised by a semi-continental climate. During the...
Published in: | Quaternary International |
---|---|
Main Authors: | , , , , , , , , , , , , , , |
Other Authors: | , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2015
|
Subjects: | |
Online Access: | https://hal.science/hal-01294941 https://hal.science/hal-01294941/document https://hal.science/hal-01294941/file/Cupillard%20et%20al%202015%28Jura_40_8%29.pdf https://doi.org/10.1016/j.quaint.2014.05.032 |
id |
ftunivparis10:oai:HAL:hal-01294941v1 |
---|---|
record_format |
openpolar |
spelling |
ftunivparis10:oai:HAL:hal-01294941v1 2024-06-23T07:53:41+00:00 Changes in ecosystems, climate and societies in the Jura Mountains between 40 and 8 ka cal BP Cupillard, Christophe Magny, Michel Bocherens, Hervé Bridault, Anne Bégeot, Carole Bichet, Vincent Bossuet, Gilles Drucker, Dorothée G. Gauthier, Emilie Jouannic, Gwénolé Millet, Laurent Richard, Hervé Rius, Damien Ruffaldi, Pascale Walter-Simonnet, Anne-Véronique Laboratoire Chrono-environnement (UMR 6249) (LCE) Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC) Université Bourgogne Franche-Comté COMUE (UBFC)-Université Bourgogne Franche-Comté COMUE (UBFC) Eberhard Karls Universität Tübingen = University of Tübingen Archéologies et Sciences de l'Antiquité (ArScAn) Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris 8 Vincennes-Saint-Denis (UP8)-Université Paris Nanterre (UPN)-Ministère de la Culture et de la Communication (MCC)-Centre National de la Recherche Scientifique (CNRS) 2015 https://hal.science/hal-01294941 https://hal.science/hal-01294941/document https://hal.science/hal-01294941/file/Cupillard%20et%20al%202015%28Jura_40_8%29.pdf https://doi.org/10.1016/j.quaint.2014.05.032 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quaint.2014.05.032 hal-01294941 https://hal.science/hal-01294941 https://hal.science/hal-01294941/document https://hal.science/hal-01294941/file/Cupillard%20et%20al%202015%28Jura_40_8%29.pdf doi:10.1016/j.quaint.2014.05.032 info:eu-repo/semantics/OpenAccess ISSN: 1040-6182 Quaternary International https://hal.science/hal-01294941 Quaternary International, 2015, Volume 378 (18 August 2015), pp.40-72. ⟨10.1016/j.quaint.2014.05.032⟩ [SDE.ES]Environmental Sciences/Environment and Society info:eu-repo/semantics/article Journal articles 2015 ftunivparis10 https://doi.org/10.1016/j.quaint.2014.05.032 2024-06-10T23:43:20Z International audience We present radiometric, palaeoclimatological, palaeoenvironmental and archaeological data for the period 40 000–8000 cal BP in the Jura Mountains (eastern France). These mountains culminate at ∼1700 m a.s.l. and are today characterised by a semi-continental climate. During the Last Glacial Maximum, the range supported a local ice cap. While recent data suggest a possible early ice-cap development during MIS 4, the chronology of the regional LGM and following deglaciation has still to be refined. The complete disappearance of the local ice cap at ca 17 000–16 600 cal BP marked the beginning of accumulation of sediment archives in the Jurassian lakes and mires, which favoured the reconstruction of past changes in climatic and environmental conditions, in addition to faunal remains found in caves and in archaeological sites. Three main successive stages may be distinguished regarding the history of societies. The first stage at ca 40 000–18 700 cal BP was characterized by very few archaeological sites with only discontinuous intermittent occupations, always located outside the Jura range. The second stage, around 18 700–11 700 cal BP, corresponded to an increase in the population density, as suggested by an increasing number of archaeological sites and a progressive colonisation of elevated areas of the Jura Mountains. The third stage at ca 11 700–8000 cal BP coincided with a reinforcement of settlement in the lowland areas as well as a development of long-term occupations in elevated areas. The millennial-scale GS-1 cold event had a more long-lasting and stronger impact on societies than did the 200 year-long 8.2 ka cold event. Article in Journal/Newspaper Ice cap Université Paris Nanterre: HAL Jura ENVELOPE(13.501,13.501,68.062,68.062) Quaternary International 378 40 72 |
institution |
Open Polar |
collection |
Université Paris Nanterre: HAL |
op_collection_id |
ftunivparis10 |
language |
English |
topic |
[SDE.ES]Environmental Sciences/Environment and Society |
spellingShingle |
[SDE.ES]Environmental Sciences/Environment and Society Cupillard, Christophe Magny, Michel Bocherens, Hervé Bridault, Anne Bégeot, Carole Bichet, Vincent Bossuet, Gilles Drucker, Dorothée G. Gauthier, Emilie Jouannic, Gwénolé Millet, Laurent Richard, Hervé Rius, Damien Ruffaldi, Pascale Walter-Simonnet, Anne-Véronique Changes in ecosystems, climate and societies in the Jura Mountains between 40 and 8 ka cal BP |
topic_facet |
[SDE.ES]Environmental Sciences/Environment and Society |
description |
International audience We present radiometric, palaeoclimatological, palaeoenvironmental and archaeological data for the period 40 000–8000 cal BP in the Jura Mountains (eastern France). These mountains culminate at ∼1700 m a.s.l. and are today characterised by a semi-continental climate. During the Last Glacial Maximum, the range supported a local ice cap. While recent data suggest a possible early ice-cap development during MIS 4, the chronology of the regional LGM and following deglaciation has still to be refined. The complete disappearance of the local ice cap at ca 17 000–16 600 cal BP marked the beginning of accumulation of sediment archives in the Jurassian lakes and mires, which favoured the reconstruction of past changes in climatic and environmental conditions, in addition to faunal remains found in caves and in archaeological sites. Three main successive stages may be distinguished regarding the history of societies. The first stage at ca 40 000–18 700 cal BP was characterized by very few archaeological sites with only discontinuous intermittent occupations, always located outside the Jura range. The second stage, around 18 700–11 700 cal BP, corresponded to an increase in the population density, as suggested by an increasing number of archaeological sites and a progressive colonisation of elevated areas of the Jura Mountains. The third stage at ca 11 700–8000 cal BP coincided with a reinforcement of settlement in the lowland areas as well as a development of long-term occupations in elevated areas. The millennial-scale GS-1 cold event had a more long-lasting and stronger impact on societies than did the 200 year-long 8.2 ka cold event. |
author2 |
Laboratoire Chrono-environnement (UMR 6249) (LCE) Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC) Université Bourgogne Franche-Comté COMUE (UBFC)-Université Bourgogne Franche-Comté COMUE (UBFC) Eberhard Karls Universität Tübingen = University of Tübingen Archéologies et Sciences de l'Antiquité (ArScAn) Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris 8 Vincennes-Saint-Denis (UP8)-Université Paris Nanterre (UPN)-Ministère de la Culture et de la Communication (MCC)-Centre National de la Recherche Scientifique (CNRS) |
format |
Article in Journal/Newspaper |
author |
Cupillard, Christophe Magny, Michel Bocherens, Hervé Bridault, Anne Bégeot, Carole Bichet, Vincent Bossuet, Gilles Drucker, Dorothée G. Gauthier, Emilie Jouannic, Gwénolé Millet, Laurent Richard, Hervé Rius, Damien Ruffaldi, Pascale Walter-Simonnet, Anne-Véronique |
author_facet |
Cupillard, Christophe Magny, Michel Bocherens, Hervé Bridault, Anne Bégeot, Carole Bichet, Vincent Bossuet, Gilles Drucker, Dorothée G. Gauthier, Emilie Jouannic, Gwénolé Millet, Laurent Richard, Hervé Rius, Damien Ruffaldi, Pascale Walter-Simonnet, Anne-Véronique |
author_sort |
Cupillard, Christophe |
title |
Changes in ecosystems, climate and societies in the Jura Mountains between 40 and 8 ka cal BP |
title_short |
Changes in ecosystems, climate and societies in the Jura Mountains between 40 and 8 ka cal BP |
title_full |
Changes in ecosystems, climate and societies in the Jura Mountains between 40 and 8 ka cal BP |
title_fullStr |
Changes in ecosystems, climate and societies in the Jura Mountains between 40 and 8 ka cal BP |
title_full_unstemmed |
Changes in ecosystems, climate and societies in the Jura Mountains between 40 and 8 ka cal BP |
title_sort |
changes in ecosystems, climate and societies in the jura mountains between 40 and 8 ka cal bp |
publisher |
HAL CCSD |
publishDate |
2015 |
url |
https://hal.science/hal-01294941 https://hal.science/hal-01294941/document https://hal.science/hal-01294941/file/Cupillard%20et%20al%202015%28Jura_40_8%29.pdf https://doi.org/10.1016/j.quaint.2014.05.032 |
long_lat |
ENVELOPE(13.501,13.501,68.062,68.062) |
geographic |
Jura |
geographic_facet |
Jura |
genre |
Ice cap |
genre_facet |
Ice cap |
op_source |
ISSN: 1040-6182 Quaternary International https://hal.science/hal-01294941 Quaternary International, 2015, Volume 378 (18 August 2015), pp.40-72. ⟨10.1016/j.quaint.2014.05.032⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quaint.2014.05.032 hal-01294941 https://hal.science/hal-01294941 https://hal.science/hal-01294941/document https://hal.science/hal-01294941/file/Cupillard%20et%20al%202015%28Jura_40_8%29.pdf doi:10.1016/j.quaint.2014.05.032 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1016/j.quaint.2014.05.032 |
container_title |
Quaternary International |
container_volume |
378 |
container_start_page |
40 |
op_container_end_page |
72 |
_version_ |
1802645445131894784 |