The climate in Europe during the Eemian: a multi-method approach using pollen data

[1]  C. Gebhardt,et al.  Reconstruction of Quaternary temperature fields by dynamically consistent smoothing , 2008 .

[2]  J. Jouzel,et al.  Transferring radiometric dating of the last interglacial sea level high stand to marine and ice core records , 2008 .

[3]  Simon Brewer,et al.  Climatic changes in Eurasia and Africa at the last glacial maximum and mid-Holocene: reconstruction from pollen data using inverse vegetation modelling , 2007 .

[4]  B. Huntley,et al.  Evidence for last interglacial chronology and environmental change from Southern Europe , 2007, Proceedings of the National Academy of Sciences.

[5]  J. Guiot,et al.  Pollen data as climate proxies , 2007 .

[6]  U. Cubasch,et al.  Simulations of the Eemian interglacial and the subsequent glacial interception with a coupled ocean-atmosphere general circulation model , 2007 .

[7]  Scott A. Elias,et al.  Encyclopedia of quaternary science , 2007 .

[8]  M. New,et al.  Tropical snowline changes at the last glacial maximum: A global assessment , 2005 .

[9]  F. Sirocko,et al.  A late Eemian aridity pulse in central Europe during the last glacial inception , 2005, Nature.

[10]  S. Klotz,et al.  Cyclic climate fluctuations during the last interglacial in central Europe , 2005 .

[11]  U. Cubasch,et al.  A model‐data comparison of European temperatures in the Eemian interglacial , 2005 .

[12]  R. Gersonde,et al.  Sea-surface temperature and sea ice distribution of the Southern Ocean at the EPILOG Last Glacial Maximum—a circum-Antarctic view based on siliceous microfossil records , 2005 .

[13]  P. Valdes,et al.  High-resolution simulations of the last glacial maximum climate over Europe: a solution to discrepancies with continental palaeoclimatic reconstructions? , 2005 .

[14]  M. Loutre,et al.  Increasing vegetation and climate gradient in Western Europe over the Last Glacial Inception (122-110 ka): data-model comparison , 2005 .

[15]  G. Kukla,et al.  North Atlantic Current and European environments during the declining stage of the last interglacial , 2004 .

[16]  C. Ritz,et al.  Quantifying ice‐sheet feedbacks during the last glacial inception , 2004 .

[17]  J Schwander,et al.  High-resolution record of Northern Hemisphere climate extending into the last interglacial period , 2004, Nature.

[18]  V. Mosbrugger,et al.  Eemian to early Würmian climate dynamics: history and pattern of changes in Central Europe , 2004 .

[19]  N. Kühl,et al.  Quantitative time series reconstruction of Eemian temperature at three European sites using pollen data , 2003 .

[20]  J. Guiot,et al.  Continental European Eemian and early Würmian climate evolution: comparing signals using different quantitative reconstruction approaches based on pollen , 2003 .

[21]  Simon Brewer,et al.  The temperature of Europe during the Holocene reconstructed from pollen data , 2003 .

[22]  N. Shackleton,et al.  Marine Isotope Substage 5e and the Eemian Interglacial , 2003 .

[23]  André Berger,et al.  An Exceptionally Long Interglacial Ahead? , 2002, Science.

[24]  M. Loutre,et al.  Transient simulations over the last interglacial period (126–115 kyr BP): feedback and forcing analysis , 2002 .

[25]  W. Broecker,et al.  Last Interglacial Climates , 2002, Quaternary Research.

[26]  J. Guiot,et al.  Synchroneity between marine and terrestrial responses to millennial scale climatic variability during the last glacial period in the Mediterranean region , 2002 .

[27]  R. Battarbee,et al.  High-resolution record of climate stability in France during the last interglacial period , 2001, Nature.

[28]  G. Ramstein,et al.  Simulating the amplification of orbital forcing by ocean feedbacks in the last glaciation , 2001, Nature.

[29]  F. Eynaud,et al.  Direct land/sea correlation of the Eemian, and its comparison with the Holocene: a high-resolution palynological record off the Iberian margin , 2000, Netherlands Journal of Geosciences.

[30]  U. Müller A Late-Pleistocene pollen sequence from the Jammertal, south-western Germany with particular reference to location and altitude as factors determining Eemian forest composition , 2000 .

[31]  Richard B. Alley,et al.  The Younger Dryas cold interval as viewed from central Greenland , 2000 .

[32]  Jörg Keller,et al.  Rapid environmental changes in southern Europe during the last glacial period , 1999, Nature.

[33]  F. Eynaud,et al.  High resolution palynological record off the Iberian margin: direct land-sea correlation for the Last Interglacial complex , 1999 .

[34]  Didier Paillard,et al.  Changes in Meridional Temperature and Salinity Gradients in the North Atlantic Ocean (30°–72°N) during the Last Interglacial Period , 1999 .

[35]  J. Guiot,et al.  Was the climate of the Eemian stable? A quantitative climate reconstruction from seven European pollen records , 1998 .

[36]  J. Duplessy,et al.  Improving past sea surface temperature estimates based on planktonic fossil faunas , 1998 .

[37]  Odile Peyron,et al.  Climatic Reconstruction in Europe for 18,000 YR B.P. from Pollen Data , 1998, Quaternary Research.

[38]  J. Severinghaus,et al.  Timing of abrupt climate change at the end of the Younger Dryas interval from thermally fractionated gases in polar ice , 1998, Nature.

[39]  G. Kukla,et al.  How long and how stable was the last interglacial , 1997 .

[40]  Aurélie Botta,et al.  Possible role of atmosphere-biosphere interactions in triggering the last glaciation , 1996 .

[41]  Mark A. Maslin,et al.  Sultry last interglacial gets a sudden chill , 1996 .

[42]  Ge Yu,et al.  The climate of Europe 6000 years ago , 1996 .

[43]  J. Kutzbach,et al.  Role of orbitally induced changes in tundra area in the onset of glaciation , 1996, Nature.

[44]  R. Tibshirani,et al.  Generalized additive models for medical research , 1995, Statistical methods in medical research.

[45]  K. Bennett,et al.  Confidence intervals for age estimates and deposition times in late-Quaternary sediment sequences , 1994 .

[46]  E. Cortijo,et al.  Eemian cooling in the Norwegian Sea and North Atlantic ocean preceding continental ice-sheet growth , 1994, Nature.

[47]  B. Huntley,et al.  Eemian climate fluctuations observed in a European pollen record , 1994, Nature.

[48]  P. Tzedakis Long-term tree populations in northwest Greece through multiple Quaternary climatic cycles , 1993, Nature.

[49]  C.J.F. ter Braak,et al.  Weighted Averaging Partial Least Squares regression (WA-PLS): definition and comparison with other methods for species-environment calibration , 1993 .

[50]  S. Wegmüller Vegetationsgeschichtliche und stratigraphische Untersuchungen an Schieferkohlen des nördlichen Alpenvorlandes , 1992 .

[51]  G. Kukla,et al.  Insolation Regime of the Warm to Cold Transitions , 1992 .

[52]  J. Guiot,et al.  Methodology of the last climatic cycle reconstruction in France from pollen data , 1990 .

[53]  J. Guiot,et al.  A 140,000-year continental climate reconstruction from two European pollen records , 1989, Nature.

[54]  W. Cleveland,et al.  Locally Weighted Regression: An Approach to Regression Analysis by Local Fitting , 1988 .

[55]  Patrick J. Bartlein,et al.  Climatic response surfaces from pollen data for some eastern North American taxa , 1986 .

[56]  J. Overpeck,et al.  Quantitative Interpretation of Fossil Pollen Spectra: Dissimilarity Coefficients and the Method of Modern Analogs , 1985, Quaternary Research.

[57]  E. Grüger Die Seeablagerungen vom Samerberg/Obb. und ihre Stellung im Jungpleistozän , 1979 .

[58]  André Berger,et al.  Long-term variations of daily insolation and Quaternary climatic changes , 1978 .

[59]  G. Woillard Grande Pile Peat Bog: A Continuous Pollen Record for the Last 140,000 Years , 1978, Quaternary Research.

[60]  Z. Janczyk-kopikowa Eemian interglacial at Golkow near Warsaw , 1966 .