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Chinese Academy of Sciences Institutional Repositories Grid
Environmental and climate reconstruction of the late-glacial-Holocene transition from a lake sediment sequence in Aubrac, French Massif Central: Chironomid and diatom evidence

文献类型:期刊论文

作者Gandouin, E.1; Rioual, P.2; Pailles, C.3; Brooks, S. J.4; Ponel, P.1; Guiter, F.1; Djamali, M.1; Andrieu-Ponel, V.1; Birks, H. J. B.5,6,9; Leydet, M.1
刊名PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
出版日期2016-11-01
卷号461页码:292-309
关键词Western Europe Past aquatic ecosystem Temperature reconstruction Palaeolimnology Corynocera ambigua Subfossil insects
DOI10.1016/j.palaeo.2016.08.039
文献子类Article
英文摘要The analysis of fossil chironomid and diatom assemblages from a sedimentary record from Les Roustieres peat bog (Massif Central, France, 1196 m asl) allows the reconstruction of past environmental and climate changes during the late-glacial and early Holocene. Chironomid assemblages showed that the infilling of the palaeolake had commenced during the Oldest Dryas (GS-2b) as suggested by the rapid decrease in chironomid species associated with the cold and deep zone of lakes and by their replacement by littoral and eutrophic taxa. Quantitative July temperature reconstructions, based on the chironomid data, suggest that mean July air temperature (Tjul) ranged between 6 degrees C and 11 degrees C at the termination of the Oldest Dryas period (GS-2b). Climate began to warm at the start of the Bolling period (GI-1e), between 15,000 and 14,800 cal yr BP, with a rise in Tjul of about 4 degrees C. This climate warming is contemporaneous with lake eutrophication as suggested by diatoms and chironomids. Maximum temperatures of 13-14 degrees C were reached around 13,600 cal yr BP during the Allered period (GI-1c-GI-1a). The Younger Dryas period (GS-1) is marked by a return to cold conditions with Tjul of about 10 degrees C during a first phase, then 13 degrees C in its terminal part. A probable increase in the duration of the ice-cover may have favoured arctic and alpine diatom species. The early-Holocene climate improvement is marked by a rise in Tjul of about 3 degrees C. (C) 2016 Elsevier B.V. All rights reserved.
WOS关键词LATEGLACIAL SUMMER TEMPERATURES ; FRESH-WATER MIDGES ; NORTHERN SWEDEN ; AIR-TEMPERATURE ; SWISS ALPS ; QUANTITATIVE RECONSTRUCTIONS ; INTERGLACIAL TRANSITION ; INFERENCE MODELS ; TROPHIC HISTORY ; BEETLE REMAINS
WOS研究方向Physical Geography ; Geology ; Paleontology
语种英语
WOS记录号WOS:000385599900024
资助机构CNRS-Eclipse program ; CNRS-Eclipse program ; CNRS-Eclipse program ; CNRS-Eclipse program
源URL[http://ir.iggcas.ac.cn/handle/132A11/53297]  
专题地质与地球物理研究所_中国科学院新生代地质与环境重点实验室
作者单位1.Avignon Univ, Aix Marseille Univ, CNRS, IRD,IMBE, Technopole Arbois Mediterranee,Bat Villemin BP 80, F-13545 Aix En Provence 04, France
2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, POB 9825, Beijing 100029, Peoples R China
3.Aix Marseille Univ, CNRS, Ctr Europeen Rech & Enseignement Geosci Environm, Technopole Arbois Mediterranee,BP 80, F-13545 Aix En Provence 04, France
4.Nat Hist Museum, Dept Life Sci, Cromwell Rd, London SW7 5BD, England
5.Univ Bergen, Dept Biol, POB 7803, N-5020 Bergen, Norway
6.Univ Bergen, Bjerknes Ctr Climate Res, POB 7803, N-5020 Bergen, Norway
7.Univ Innsbruck, Inst Bot, Sternwartestr 15, A-6020 Innsbruck, Austria
8.Lund Univ, Fac Sci, Box 118, SE-22100 Lund, Sweden
9.UCL, Environm Change Res Ctr, London WC1E 6BT, England
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Gandouin, E.,Rioual, P.,Pailles, C.,et al. Environmental and climate reconstruction of the late-glacial-Holocene transition from a lake sediment sequence in Aubrac, French Massif Central: Chironomid and diatom evidence[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2016,461:292-309.
APA Gandouin, E..,Rioual, P..,Pailles, C..,Brooks, S. J..,Ponel, P..,...&de Beaulieu, J. L..(2016).Environmental and climate reconstruction of the late-glacial-Holocene transition from a lake sediment sequence in Aubrac, French Massif Central: Chironomid and diatom evidence.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,461,292-309.
MLA Gandouin, E.,et al."Environmental and climate reconstruction of the late-glacial-Holocene transition from a lake sediment sequence in Aubrac, French Massif Central: Chironomid and diatom evidence".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 461(2016):292-309.

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来源:地质与地球物理研究所

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