Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Jena Zumaque"'
Autor:
Mathieu Durand, Jena Zumaque, Meryem Mojtahid, Clément Lambert, Guillaume Charria, Yvan Pailler, Pierre-Olivier Coste, Pierre Stéphan, Maïwen Herlédan, Jérôme Goslin, Aurélie Penaud, Muriel Vidal, Frédérique Eynaud, Axelle Ganne
Publikováno v:
Quaternary Science Reviews
Quaternary Science Reviews, 2020, 229, pp.106135. ⟨10.1016/j.quascirev.2019.106135⟩
Quaternary Science Reviews, Elsevier, 2020, 229, pp.106135. ⟨10.1016/j.quascirev.2019.106135⟩
Quaternary Science Reviews, 2020, 229, pp.106135. ⟨10.1016/j.quascirev.2019.106135⟩
Quaternary Science Reviews, Elsevier, 2020, 229, pp.106135. ⟨10.1016/j.quascirev.2019.106135⟩
International audience; We discuss paleoenvironments of north-western France over the last 7 kyrs in terms of: i) long-term changes (relative sea-level rise and boreal summer insolation), ii) rapid climate changes (millennial-scale Bond events and mu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0bf795128750643bca3ce15c61c64283
https://hal.science/hal-02895508/document
https://hal.science/hal-02895508/document
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 468:403-413
Paleoceanographical changes during the Holocene were reconstructed from the study of core MD95-2002 situated in the northern Bay of Biscay, which is marked by the direct influence of the northeastern return branch of the North Atlantic Drift. Palynol
Autor:
Christophe Colin, Yannick Mary, Didier Swingedouw, Marie-Camille Gasparotto, Mélanie Wary, Frédérique Eynaud, Jena Zumaque
Publikováno v:
Global and Planetary Change
Global and Planetary Change, Elsevier, 2018, 170, pp.48-61. ⟨10.1016/j.gloplacha.2018.07.017⟩
Global and Planetary Change, Elsevier, 2018, 170, pp.48-61. ⟨10.1016/j.gloplacha.2018.07.017⟩
International audience; This paper illustrates a new compilation of sea-surface hydrographic data (SST mainly) derived from multiproxy reconstructions on high time-resolution (decadal to centennial) marine archives. This compilation is focussed on th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c70e4bf837a031763ca0958dab995be4
https://hal.archives-ouvertes.fr/hal-02092654
https://hal.archives-ouvertes.fr/hal-02092654
Autor:
E. Palis, Marjolaine Sabine, Linda Rossignol, Elisabeth Michel, Karine Charlier, Clémence Caulle, Sébastien Zaragosi, Mélanie Wary, Jena Zumaque, Aurélie Penaud, Frédérique Eynaud, Bruno Malaizé
Publikováno v:
Climate of the Past, Vol 11, Iss 11, Pp 1507-1525 (2015)
Climate Of The Past (1814-9324) (Copernicus Gesellschaft Mbh), 2015, Vol. 11, N. 11, P. 1507-1525
Climate of the Past
Climate of the Past, 2015, 11 (11), pp.1507-1525. ⟨10.5194/cp-11-1507-2015⟩
Climate of the Past, European Geosciences Union (EGU), 2015, 11 (11), pp.1507-1525. ⟨10.5194/cp-11-1507-2015⟩
Climate Of The Past (1814-9324) (Copernicus Gesellschaft Mbh), 2015, Vol. 11, N. 11, P. 1507-1525
Climate of the Past
Climate of the Past, 2015, 11 (11), pp.1507-1525. ⟨10.5194/cp-11-1507-2015⟩
Climate of the Past, European Geosciences Union (EGU), 2015, 11 (11), pp.1507-1525. ⟨10.5194/cp-11-1507-2015⟩
The last glacial period was punctuated by abrupt climatic events with extrema known as Heinrich and Dansgaard–Oeschger events. These millennial events have been the subject of many paleoreconstructions and model experiments in the past decades, but
Autor:
Mélanie Wary, Frédérique Eynaud, Didier Swingedouw, Valérie Masson-Delmotte, Jens Matthiessen, Catherine Kissel, Jena Zumaque, Linda Rossignol, Jean Jouzel
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::118950d9ac225519f2f3d796a6b2a479
https://doi.org/10.5194/cp-2017-14-supplement
https://doi.org/10.5194/cp-2017-14-supplement
Regional seesaw between North Atlantic and Nordic Seas during the last glacial abrupt climate events
Autor:
Mélanie Wary, Frédérique Eynaud, Didier Swingedouw, Valérie Masson-Delmotte, Jens Matthiessen, Catherine Kissel, Jena Zumaque, Linda Rossignol, Jean Jouzel
Dansgaard-Oeschger oscillations constitute one of the most enigmatic features of the last glacial cycle. Their cold atmospheric phases have been commonly associated with cold sea-surface temperatures and expansion of sea ice in the North Atlantic and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::31db2efa57f4e389f646939173c264d1
https://doi.org/10.5194/cp-2017-14
https://doi.org/10.5194/cp-2017-14
Autor:
Jens Matthiessen, Jena Zumaque, Frédérique Eynaud, Didier Swingedouw, Valérie Masson-Delmotte, Mélanie Wary, Catherine Kissel, Jean Jouzel, Linda Rossignol
Publikováno v:
Climate of the Past
Climate of the Past, 2017, 13 (6), pp.729-739. ⟨10.5194/cp-13-729-2017⟩
Climate of the Past, Vol 13, Pp 729-739 (2017)
Climate of the Past, European Geosciences Union (EGU), 2017, 13 (6), pp.729-739. ⟨10.5194/cp-13-729-2017⟩
Climate Of The Past (1814-9324) (Copernicus Gesellschaft Mbh), 2017-06-30, Vol. 13, N. 6, P. 729-739
EPIC3Climate of the Past, 13(6), pp. 729-739, ISSN: 1814-9332
Climate of the Past, 2017, 13 (6), pp.729-739. ⟨10.5194/cp-13-729-2017⟩
Climate of the Past, Vol 13, Pp 729-739 (2017)
Climate of the Past, European Geosciences Union (EGU), 2017, 13 (6), pp.729-739. ⟨10.5194/cp-13-729-2017⟩
Climate Of The Past (1814-9324) (Copernicus Gesellschaft Mbh), 2017-06-30, Vol. 13, N. 6, P. 729-739
EPIC3Climate of the Past, 13(6), pp. 729-739, ISSN: 1814-9332
Dansgaard–Oeschger oscillations constitute one of the most enigmatic features of the last glacial cycle. Their cold atmospheric phases have been commonly associated with cold sea-surface temperatures and expansion of sea ice in the North Atlantic a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::36cb1b8d6c8945a18d71e2168512e406
https://hal.science/hal-01584277/document
https://hal.science/hal-01584277/document
Autor:
E. Palis, C. Kissel, E. Michel, Jena Zumaque, Sébastien Zaragosi, Kenji Matsuzaki, Thomas Richter, D. M. Roche, F. Marret, Bruno Malaizé, Frédérique Eynaud, Isabelle Billy
The rapid climatic variability characterising the Marine Isotopic Stage (MIS) 3 (~ 60–30 CAL-ka BP) provides key issues to understand the atmosphere-ocean-cryosphere dynamics. Here we investigate the response of sea-surface paleoenvironments to the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6eeb930487b627676687722dc3624d52
https://doi.org/10.5194/cpd-8-3043-2012
https://doi.org/10.5194/cpd-8-3043-2012