Climate variability and associated vegetation response throughout Central and Eastern Europe (CEE) between 60 and 8 ka

QUATERNARY SCIENCE REVIEWS

卷:106

Article

Feurdean, A.^1,2,3,4  Persoiu, A.⁵  Tantau, I.⁶  Stevens, T.⁷  Magyari, E. K.⁸  Onac, B. P.⁹  Markovic, S.¹⁰  Andric, M.¹¹  Connor, S.¹²  Farcas, S.¹³  Galka, M.^14,15  Gaudeny, T.¹⁶  Hoek, W.¹⁷  Kolaczek, P.^14,15  Kunes, P.¹⁸  Lamentowicz, M.^14,15  Marinova, E.¹⁹  Michczynska, D. J.²⁰  Persoiu, I.²¹  Plociennik, M.²²  Slowinski, M.^23,24  Stancikaite, M.²⁵  Sumegi, P.²⁶  Svensson, A.²⁷  Tamas, T.^4,6  Timar, A.²⁸  Tonkov, S.²⁹  Toth, M.³⁰  Veski, S.³¹  Willis, K. J.³²  Zernitskaya, V.³³ 

[1] Senckenberg Res Inst, D-60325 Frankfurt, Germany

[2] Nat Hist Museum, D-60325 Frankfurt, Germany

[3] Biodivers & Climate Res Ctr BiK F, Senckenberganlage 25, D-60325 Frankfurt, Germany

[4] Romanian Acad, Emil Racovita Inst Speleol, Cluj Napoca 400006, Romania

[5] Stefan Cel Mare Univ, Stable Isotope Lab, Suceava 720229, Romania

[6] Univ Babes Bolyai, Dept Geol, Cluj Napoca 400084, Romania

[7] Royal Holloway Univ London, Dept Geog, Ctr Quaternary Res, Egham TW20 0EX, Surrey, England

[8] Eotvos Lorand Univ, Dept Phys & Appl Geol, H-1117 Budapest, Hungary

[9] Univ S Florida, Sch Geosci, Tampa, FL 33620 USA

[10] Univ Novi Sad, Fac Sci, Lab Palaeoenvironm Reconstruct, Novi Sad 21000, Serbia

[11] Slovenian Acad Sci & Arts ZRC SAZU, Ctr Sci Res, Inst Archaeol, SI-1001 Ljubljana, Slovenia

[12] Monash Univ, Sch Geog & Environm Sci, Clayton, Vic 3800, Australia

[13] Inst Biol Res, Natl Inst Res & Dev Biol Sci, Cluj Napoca 400015, Romania

[14] Adam Mickiewicz Univ, Dept Biogeog & Palaeoecol, Fac Geog & Geol Sci, PL-61680 Poznan, Poland

[15] Adam Mickiewicz Univ, Lab Wetland Ecol & Monitoring, Fac Geog & Geol Sci, PL-61680 Poznan, Poland

[16] Serbian Acad Arts & Sci, Geog Inst Jovan CVIJIC, SRB-11000 Belgrade, Serbia

[17] Univ Utrecht, Fac Geosci, NL-3508 TC Utrecht, Netherlands

[18] Charles Univ Prague, Fac Sci, Dept Bot, Prague 12801, Czech Republic

[19] Univ Louvain, Ctr Archaeol Sci, B-3001 Louvain, Belgium

[20] Silesian Tech Univ, Inst Phys CSE, GADAM Ctr Excellence, PL-44100 Gliwice, Poland

[21] Stefan Cel Mare Univ, Dept Geog, Suceava 720229, Romania

[22] Univ Lodz, Dept Invertebrate Zool & Hydrobiol, PL-90237 Lodz, Poland

[23] Polish Acad Sci, Inst Geog, Dept Environm Resources & Geohazard, PL-87100 Torun, Poland

[24] GEZ German Res Ctr Geosci, D-14473 Potsdam, Germany

[25] Inst Geol & Geog, Nat Res Ctr, LT-03223 Vilnius, Lithuania

[26] Univ Szeged, H-6722 Szeged, Hungary

[27] Univ Copenhagen, Ctr Ice & Climate, Niels Bohr Inst, DK-2100 Copenhagen, Denmark

[28] Univ Babes Bolyai, Fac Environm Sci & Engn, Cluj Napoca 400294, Romania

[29] Sofia Univ St KlimentOhridski, Fac Biol, Palynol Lab, Dept Bot, Sofia, Bulgaria

[30] MTA Ctr Ecol Res, Balaton Limnol Inst, H-8237 Tihany, Hungary

[31] Tallinn Univ Technol, Inst Geol, EE-19086 Tallinn, Estonia

[32] Univ Oxford, Dept Zool, Long Term Ecol Lab, Biodivers Inst, Oxford OX1 3PS, England

[33] Natl Acad Sci Belarus, Inst Nat Management, Lab Geodynam & Paleogeog, Minsk 220114, BELARUS

关键词: Terrestrial records;    Climate;    Pollen;    Vegetation response;    INTIMATE;    Latitudinal gradients;    Glacial;    Holocene;   

DOI  :  10.1016/j.quascirev.2014.06.003

来源: Elsevier

【 摘 要 】

Records of past climate variability and associated vegetation response exist in various regions throughout Central and Eastern Europe (CEE). To date, there has been no coherent synthesis of the existing palaeo-records. During an INTIMATE meeting (Cluj Napoca, Romania) focused on identifying CEE paleo-records, it was decided to address this gap by presenting the palaeo-community with a compilation of high-quality climatic and vegetation records for the past 60-8 ka. The compilation should also serve as a reference point for the use in the modelling community working towards the INTIMATE project goals, and in data-model inter-comparison studies. This paper is therefore a compilation of up to date, best available quantitative and semi-quantitative records of past climate and biotic response from CEE covering this period. It first presents the proxy and archive used. Speleothems and loess mainly provide the evidences available for the 60-20 ka interval, whereas pollen records provide the main source of information for the Lateglacial and Holocene. It then examines the temporal and spatial patterns of climate variability inferred from different proxies, the temporal and spatial magnitude of the vegetation responses inferred from pollen records and highlights differences and similarities between proxies and sub-regions and the possible mechanisms behind this variability. Finally, it identifies weakness in the proxies and archives and their geographical distribution. This exercise also provides an opportunity to reflect on the status of research in the area and to identify future critical areas and subjects of research. (C) 2014 Elsevier Ltd. All rights reserved.

【 授权许可】

Free