Late-Glacial climatic changes in Eastern France (Lake Lautrey) from pollen, lake-levels, and chironomids
暂无分享,去创建一个
L. Millet | S. Brewer | G. Yu | O. Heiri | E. Van Campo | O. Peyron | C. Bégeot | M. Magny | P. Ruffaldi | G. Yu | O. Peyron | C. Bégeot | S. Brewer | O. Heiri | M. Magny | L. Millet | P. Ruffaldi | E. Van Campo | E. Campo | S. Brewer | Ge Yu
[1] J. Guiot,et al. Quantitative Reconstruction of Younger Dryas to Mid-Holocene Paleoclimates at Le Locle, Swiss Jura, Using Pollen and Lake-Level Data , 2001, Quaternary Research.
[2] H. Richard,et al. Le Tardiglaciaire du massif jurassien: bilan et perspectives de recherches.: bilan et perspectives de recherches. , 2000 .
[3] G. Hannon,et al. High-altitude vegetational pattern on the Iberian Mountain Chain (north-central Spain) during the Holocene , 1999 .
[4] F. Gasse,et al. Holocene environmental changes in Bangong Co basin (Western Tibet). Part 4: Discussion and conclusions , 1996 .
[5] H. Birks,et al. Late‐glacial climatic oscillations as recorded in Swiss lake sediments , 1992 .
[6] A. Lotter,et al. A chironomid-based Holocene summer air temperature reconstruction from the Swiss Alps , 2003 .
[7] S. Bohncke,et al. Mean July Temperatures during the Younger Dryas in Northwestern and Central Europe as Inferred from Climate Indicator Plant Species , 1999, Quaternary Research.
[8] D. Post,et al. Rapid and widespread vegetation responses to past climate change in the North Atlantic region , 2002 .
[9] H. H. Birks. The importance of plant macrofossils in the reconstruction of Lateglacial vegetation and climate: examples from Scotland, western Norway, and Minnesota, USA , 2003 .
[10] M. Gaillard,et al. Lateglacial insect assemblages from Grand-Marais, southwestern Switzerland - climatic implications and comparison with pollen and plant macrofossil data , 1994 .
[11] J. Schwander,et al. Isotope signature of the Younger Dryas and two minor oscillations at Gerzensee (Switzerland): palaeoclimatic and palaeolimnologic interpretation based on bulk and biogenic carbonates , 2000 .
[12] L. Millet,et al. Reconstruction of Late Glacial summer temperatures from chironomid assemblages in Lac Lautrey (Jura, France) , 2005 .
[13] A. Lotter,et al. The Würmian Late-glacial in lowland Switzerland , 1994 .
[14] W. Watts,et al. Palaeoclimate, chronology and vegetation history of the Weichselian Lateglacial: comparative analysis of data from three cores at Lago Grande di Monticchio, southern Italy , 1999 .
[15] H. Birks,et al. Quantification of biotic responses to rapid climatic changes around the Younger Dryas — a synthesis , 2000 .
[16] B Huntley,et al. Reconstructing biomes from palaeoecological data: a general method and its application to European pollen data at 0 and 6 ka , 1996 .
[17] Dorthe Dahl-Jensen,et al. Oxygen isotope and palaeotemperature records from six Greenland ice‐core stations: Camp Century, Dye‐3, GRIP, GISP2, Renland and NorthGRIP , 2001 .
[18] J. Vandenberghe,et al. Periglacial environments during the Weichselian Late Glacial in the Maas valley, the Netherlands. , 1993 .
[19] Odile Peyron,et al. Climate of East Africa 6000 14C Yr B.P. as Inferred from Pollen Data , 2000, Quaternary Research.
[20] J. Lowe,et al. An event stratigraphy for the Last Termination in the North Atlantic region based on the Greenland ice-core record: a proposal by the INTIMATE group , 1998 .
[21] Odile Peyron,et al. Contrasting patterns of hydrological changes in Europe in response to Holocene climate cooling phases. , 2003 .
[22] Chris S. M. Turney,et al. Devensian Lateglacial environmental changes in Britain: a multi-proxy environmental record from Llanilid, South Wales, UK , 2003 .
[23] W. Haeberli,et al. Environment and climate in southwestern Switzerland during the last termination, 15-10 ka BP☆ , 1994 .
[24] J. Guiot,et al. Methodology of the last climatic cycle reconstruction in France from pollen data , 1990 .
[25] J. Bos. Lateglacial and Early Holocene vegetation history of the northern Wetterau and the Amöneburger Basin (Hessen), central-west Germany. , 2001, Review of palaeobotany and palynology.
[26] M. Walker. Rapid climate change during the last glacial–interglacial transition; implications for stratigraphic subdivision, correlation and dating ☆ , 2001 .
[27] H. E. Wright,et al. Palaeoecological Events During the Last 15,000 Years: Regional Synthesis of Palaeoecological Studies of Lakes and Mires in Europe. , 1996 .
[28] G. Lemdahl. Lateglacial and Early Holocene insect assemblages from sites at different altitudes in the Swiss Alps—implications on climate and environment , 2000 .
[29] P. Cour,et al. Holocene environmental changes in Bangong Co basin (Western Tibet). Part 2: The pollen record , 1996 .
[30] G. Coope,et al. The environment of Upper Palaeolithic (Magdalenian and Azilian) hunters at Hauterive-Champréveyres, Neuchâtel, Switzerland, interpreted from coleopteran remains , 2000 .
[31] Sandy P. Harrison,et al. Climate and biome simulations for the past 21 , 1998 .
[32] Sandy P. Harrison,et al. Reconstruction of Holocene Precipitation Patterns in Europe Using Pollen and Lake-Level Data , 1993, Quaternary Research.
[33] Ge Yu,et al. Modern pollen samples from alpine vegetation on the Tibetan Plateau , 2002 .
[34] H. H. Birks,et al. Two terrestrial records of rapid climatic change during the glacial-Holocene transition (14,000- 9,000 calendar years B.P.) from Europe. , 2000, Proceedings of the National Academy of Sciences of the United States of America.
[35] A. Brauer,et al. High resolution sediment and vegetation responses to Younger Dryas climate change in varved lake sediments from Meerfelder Maar, Germany , 1999 .
[36] H. Birks,et al. Younger Dryas and Allerød summer temperatures at Gerzensee (Switzerland) inferred from fossil pollen and cladoceran assemblages , 2000 .
[37] D. Jacob,et al. Simulation of the Younger Dryas climate in Europe using a regional climate model nested in an AGCM: preliminary results , 2001 .
[38] Odile Peyron,et al. Climatic Reconstruction in Europe for 18,000 YR B.P. from Pollen Data , 1998, Quaternary Research.
[39] W. Hoek. Vegetation response to the ∼14.7 and ∼11.5 ka cal. BP climate transitions: is vegetation lagging climate? , 2001 .
[40] H. Renssen,et al. The two major warming phases of the last deglaciation at ; 14.7 and ; 11.5 ka cal BP in Europe: climate reconstructions and AGCM experiments , 2001 .
[41] Rachid Cheddadi,et al. The climate in Western Europe during the last Glacial/Interglacial cycle derived from pollen and insect remains , 1993 .
[42] J. Guiot,et al. Continental European Eemian and early Würmian climate evolution: comparing signals using different quantitative reconstruction approaches based on pollen , 2003 .
[43] M. Magny. Palaeohydrological changes as reflected by lake-level fluctuations in the Swiss Plateau, the Jura Mountains and the northern French Pre-Alps during the Last Glacial–Holocene transition: a regional synthesis , 2001 .
[44] H. Renssen,et al. Rapid climatic warming: palaeo-data analysis and modeling , 2001 .
[45] G. Bossuet,et al. Enregistrement pollinique des changements climatiques de l'Interstade Bolling/Allerod dans l'est de la France , 2000 .
[46] B. Ammann. Biotic responses to rapid climatic changes , 2000 .