Was the climate of the Eemian stable? A quantitative climate reconstruction from seven European pollen records

Cheddadi, Rachid; Mamakowa, K.; Guiot, Joël; Beaulieu, J.‐L. de; Reille, Maurice; Andrieu, Valérie; Granoszewski, Wojciech; Peyron, Odile

doi:10.1016/s0031-0182(98)00067-4

Cited by 153 publications

(86 citation statements)

References 37 publications

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“…Bartlein & Whitlock 1993;Cheddadi et al 1998a;Kerwin et al 2004;Nakagawa et al 2002;Sawada et al 2004;Peryon et al 2005;Ortu et al 2006Ortu et al , 2008Ortu et al , 2010Feurdean et al 2008aFeurdean et al , 2008bBordon et al 2009;. MAT has been extended by Guiot (1990), Guiot et al (1989;1992), and Cheddadi et al (1998b) to reconstruct several climatic variables from pollen assemblages for the last glacial-interglacial cycle using so-called 'palaeobioclimatic operators' as weights to emphasise preferentially the climatic signal within fossil pollen data (see below).…”

Section: The Assemblage Approach Basic Principlesmentioning

confidence: 99%

Strengths and Weaknesses of Quantitative Climate Reconstructions Based on Late-Quaternary Biological Proxies

Birks

2011

TOECOLJ

328

284

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Abstract:The importance of reconstructing past environments quantitatively in palaeoecology is reviewed by showing that many ecological questions asked of palaeoecological data commonly involve the reconstructions of past environment. Three basic approaches to reconstructing past climate from palaeoecological data are outlined and discussed in terms of their assumptions, strengths, and weaknesses. These approaches are the indicator-species approach involving bioclimateenvelope modelling; the assemblage approach involving modern analogue techniques and response surfaces; and the multivariate calibration-function approach. Topics common to all approaches are reviewed -presentation and interpretation, evaluation and validation, comparison, and general limitations of climate reconstructions. Challenges and possible future developments are presented and the potential future role of quantitative climate reconstructions in palaeoecology is summarised.

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Section: The Assemblage Approach Basic Principlesmentioning

confidence: 99%

Strengths and Weaknesses of Quantitative Climate Reconstructions Based on Late-Quaternary Biological Proxies

Birks

2011

TOECOLJ

328

284

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“…The method of direct analogues (Cheddadi et al, 1998; de Vernal and Hillaire-Marcel, 2000) was used, limiting the selection of potential analogues to those surface samples with annual temperature sum < 1200 °C days above 5°C, hence to those located beyond treeline or in Boreal or montane forests. This restriction was necessary in order to overcome the problem that frequently arises with relatively taxon-poor pollen spectra, such as those in this study, for which equally close analogues are often located in regions with very disparate climates (Huntley, 1993), leading to potentially very noisy or even quite misleading reconstructions if mean values are taken from analogues that are distributed bimodally with respect to the variable being reconstructed (Haslett et al, 2006).…”

Section: Palaeoclimate Reconstructionmentioning

confidence: 99%

Spatio-temporal patterns in Lateglacial and Holocene vegetation and climate of Finnmark, northernmost Europe

Huntley

Long

Allen

2013

Quaternary Science Reviews

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. (2013) 'Spatio-temporal patterns in late-glacial and Holocene vegetation and climate of Finnmark, northernmost Europe.', Quaternary science reviews., 70 . pp. 158-175. Further information on publisher's website:http://dx.doi.org/10. 1016/j.quascirev.2013.03.006 Publisher's copyright statement: NOTICE: this is the author's version of a work that was accepted for publication in Quaternary Science Reviews. 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 was subsequently published in Quaternary Science Reviews, 70, 2013Reviews, 70, , 10.1016Reviews, 70, /j.quascirev.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. Further work on precisely-dated marine sediment cores will be necessary to understand the factors leading to the periodic and longer-term variations in strength of the North Cape Current.

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“…6). Ces périodes ont été caractérisées par un climat tempéré humide de moyenne montagne proche des conditions actuelles, avec des températures moyennes aux environs de 0°C en hiver et des précipitations comprises générale-ment entre 800 et 1000 mm par an (Guiot et al, 1989 ;Cheddadi et al, 1998).…”

Section: -Interprétation Des Résultatsunclassified

“…Cette péjoration climatique a engendré une détérioration du couvert végétal qui a induit un pic d'érosion bien mis en évidence dans le bassin versant du Lac du Bouchet. Reille & de Beaulieu (1988, 1990, Guiot et al (1989Guiot et al ( , 1993, Cheddadi et al (1998). Reille & de Beaulieu (1988, 1990, Guiot et al (1989Guiot et al ( , 1993, Cheddadi et al (1998).…”

Section: -Interprétation Des Résultatsunclassified

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Environmental impact on the Late Pleistocene and Holocene soil erosion in the “Lac Du Bouchet” maar crater (Massif Central, France)

Degeai¹,

Pastre²

2009

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Was the climate of the Eemian stable? A quantitative climate reconstruction from seven European pollen records

Cited by 153 publications

References 37 publications

Strengths and Weaknesses of Quantitative Climate Reconstructions Based on Late-Quaternary Biological Proxies

Strengths and Weaknesses of Quantitative Climate Reconstructions Based on Late-Quaternary Biological Proxies

Spatio-temporal patterns in Lateglacial and Holocene vegetation and climate of Finnmark, northernmost Europe

Environmental impact on the Late Pleistocene and Holocene soil erosion in the “Lac Du Bouchet” maar crater (Massif Central, France)

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