Evidence for Younger Dryas-age cooling on the North Pacific coast of America
暂无分享,去创建一个
[1] L. Cwynar,et al. Accelerator-Mass-Spectrometer Ages for the Younger Dryas Event in Atlantic Canada , 1993, Quaternary Research.
[2] L. Cwynar,et al. A previously unrecognized late-glacial cold event in eastern North America , 1993, Nature.
[3] R. Patterson,et al. Evidence for a Younger Dryas-like cooling event on the British Columbia coast , 1993 .
[4] S. Lehman,et al. Sudden changes in North Atlantic circulation during the last deglaciation , 1992, Nature.
[5] D. Meidinger,et al. Revision of biogeoclimatic units of coastal British Columbia , 1991 .
[6] J. Smol,et al. Aller�d—Younger Dryas Lake Temperatures from Midge Fossils in Atlantic Canada , 1991, Science.
[7] John P. Smol,et al. An assessment of Chironomidae as quantitative indicators of past climatic change , 1991 .
[8] B. C. Hansen,et al. A Possible Younger Dryas Record in Southeastern Alaska , 1990, Science.
[9] W. Berger. The younger dryas cold spell—a quest for causes , 1990 .
[10] J. Clague,et al. Time of Maximum Late Wisconsin Glaciation, West Coast of Canada , 1990, Quaternary Research.
[11] J. Southon,et al. A record of past ocean‐Atmosphere radiocarbon differences from the northeast Pacific , 1990 .
[12] J. Southon,et al. Younger Dryas Climatic Reversal in Northeastern USA? AMS Ages for an Old Problem , 1990, Quaternary Research.
[13] J. Southon,et al. Radiocarbon Dating of Pollen by Accelerator Mass Spectrometry , 1989, Quaternary Research.
[14] J. White,et al. The abrupt termination of the Younger Dryas climate event , 1989, Nature.
[15] W. Watts,et al. Accelerator-Mass Spectrometer Ages for Late-Glacial Events at Ballybetagh, Ireland , 1989, Quaternary Research.
[16] J. Clague,et al. Late Pleistocene terrestrial deposits on the continental shelf of western Canada: Evidence for rapid sea-level change at the end of the last glaciation , 1989 .
[17] I. Walker,et al. Much ado about dead diptera , 1989 .
[18] I. Walker,et al. Early postglacial chironomid succession in southwestern British Columbia, Canada, and its paleoenvironmental significance , 1989 .
[19] I. Walker,et al. Chironomidae (Diptera) remains in surficial lake sediments from the Canadian Cordillera: analysis of the fauna across an altitudinal gradient , 1989 .
[20] L. Harvey. Modelling the younger dryas , 1989 .
[21] H. E. Wright. The amphi-atlantic distribution of the younger dryas paleoclimatic oscillation , 1989 .
[22] W. Broecker,et al. The chronology of the last deglaciation: implications to the cause of the Younger Dryas event , 1988 .
[23] P. W. Dunwiddie,et al. Macrofossil and Pollen Representation of Coniferous Trees in Modern Sediments From Washington , 1987 .
[24] P. Bartlein,et al. The northwestern U.S. during deglaciation; Vegetational history and paleoclimatic implications , 1987 .
[25] I. Walker,et al. Chironomidae (Diptera) and Postglacial Climate at Marion Lake, British Columbia, Canada , 1987, Quaternary Research.
[26] I. Walker. Chironomidae (Diptera) in paleoecology , 1987 .
[27] W. Broecker,et al. The impact of cold North Atlantic sea surface temperatures on climate: implications for the Younger Dryas cooling (11–10 k) , 1986 .
[28] R. Mott,et al. Late-glacial climatic oscillation in Atlantic Canada equivalent to the Allerød/younger Dryas event , 1986, Nature.
[29] D. Peteet. Modern Pollen Rain and Vegetational History of the Malaspina Glacier District, Alaska , 1986, Quaternary Research.
[30] J. Clague. Delaciation of the Prince Rupert – Kitimat area, British Columbia , 1985 .
[31] B. Warner. Late Quaternary paleoecology of eastern Graham Island, Queen Charlotte Islands, British Columbia, Canada , 1984 .
[32] C. Heusser. Holocene Vegetation History of the Prince William Sound Region, South-Central Alaska , 1983, Quaternary Research.
[33] J. Clague,et al. Stratigraphic relationships and paleoecology of a late-glacial peat bed from the Queen Charlotte Islands, British Columbia , 1982 .
[34] R. Mathewes,et al. A 12 000 year palynological record of temperature and precipitation trends in southwestern British Columbia , 1981 .
[35] J. Clague. Late Quaternary Geology and Geochronology of British Columbia Part 2 : Summary and Discussion of Radiocarbon-Dated Quaternary History , 1981 .
[36] J. Armstrong,et al. POST-VASHON WISCONSIN GLACIATION, FRASER LOWLAND, BRITISH COLUMBIA , 1981 .
[37] H. Sejrup,et al. Cassidulina reniforme and C. obtusa (Foraminifera), taxonomy, distribution, and ecology , 1980 .
[38] C. Heusser. Modern pollen rain of Washington , 1978 .
[39] C. Heusser. Quaternary Palynology of the Pacific Slope of Washington , 1977, Quaternary Research.
[40] J. Lowe,et al. The Scottish Lateglacial Environment: A Synthesis , 1977 .
[41] C. Heusser. Quaternary Vegetation, Climate, and Glaciation of the Hoh River Valley, Washington , 1974 .
[42] R. Mathewes. A palynological study of postglacial vegetation changes in the University Research Forest, southwestern British Columbia , 1973 .
[43] C. Heusser. Environmental Sequence following the Fraser Advance of the Juan de Fuca Lobe, Washington , 1973, Quaternary Research.
[44] J. Noble,et al. Late Pleistocene Stratigraphy and Chronology in Southwestern British Columbia and Northwestern Washington , 1965 .
[45] C. Heusser. Palynology of Four Bog Sections From the Western Olympic Peninsula, Washington , 1964 .
[46] C. Heusser. Late-Pleistocene Environments of North Pacific North America , 1961 .
[47] C. Heusser. POLLEN PROFILES FROM THE QUEEN CHARLOTTE ISLANDS, BRITISH COLUMBIA , 1955 .