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Volumn 312, Issue 5777, 2006, Pages 1146-1148

Was the Younger Dryas triggered by a flood?

Author keywords

[No Author keywords available]

Indexed keywords

COOLING; ECOSYSTEMS; ENVIRONMENTAL IMPACT; FLOOD CONTROL; WATER;

EID: 33744460469     PISSN: 00368075     EISSN: 10959203     Source Type: Journal    
DOI: 10.1126/science.1123253     Document Type: Review
Times cited : (177)

References (20)
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    • J. T. Teller, L. Clayton, Eds. (Geological Association of Canada, St. John's, Newfoundland)
    • J. T. Teller, L. H. Thorleifson, in Glacial Lake Agassiz, J. T. Teller, L. Clayton, Eds. (Geological Association of Canada, St. John's, Newfoundland, 1983), pp. 261-290.
    • (1983) Glacial Lake Agassiz , pp. 261-290
    • Teller, J.T.1    Thorleifson, L.H.2
  • 5
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    • T. V. Lowell et al., Eos 86, 365 (2005).
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    • Broecker, W.S.1
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    • D. C. Barber et al., Nature 400, 344 (1999).
    • (1999) Nature , vol.400 , pp. 344
    • Barber, D.C.1
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    • 0033519676 scopus 로고    scopus 로고
    • J. R. Petit et al., Nature 399, 429 (1999).
    • (1999) Nature , vol.399 , pp. 429
    • Petit, J.R.1
  • 20
    • 33744479501 scopus 로고    scopus 로고
    • note
    • I am indebted to G. Corner for financial backing and for initiating and participating in field expeditions to the Agassiz outlets and the glaciated mountain ranges of eastern and southern Greenland. These field trips have substantially advanced my thinking with regard to the Younger Dryas. Discussions with T. Lowell, T. Fisher, G. Denton, J. Teller, S. Hemming, and J. Schaefer have also been extremely helpful.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.