SwePub
Sök i LIBRIS databas

  Utökad sökning

WFRF:(Curry S.)
 

Sökning: WFRF:(Curry S.) > An updated radiocar...

LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00007029naa a2201357 4500
001oai:gup.ub.gu.se/293435
003SwePub
008240528s2020 | |||||||||||000 ||eng|
024a https://gup.ub.gu.se/publication/2934352 URI
024a https://doi.org/10.1016/j.quascirev.2020.1062232 DOI
040 a (SwePub)gu
041 a eng
042 9 SwePub
072 7a ref2 swepub-contenttype
072 7a art2 swepub-publicationtype
100a Dalton, A. S.4 aut
2451 0a An updated radiocarbon-based ice margin chronology for the last deglaciation of the North American Ice Sheet Complex
264 1b Elsevier BV,c 2020
520 a The North American Ice Sheet Complex (NAISC; consisting of the Laurentide, Cordilleran and Innuitian ice sheets) was the largest ice mass to repeatedly grow and decay in the Northern Hemisphere during the Quaternary. Understanding its pattern of retreat following the Last Glacial Maximum is critical for studying many facets of the Late Quaternary, including ice sheet behaviour, the evolution of Holocene landscapes, sea level, atmospheric circulation, and the peopling of the Americas. Currently, the most up-to-date and authoritative margin chronology for the entire ice sheet complex is featured in two publications (Geological Survey of Canada Open File 1574 [Dyke et al., 2003]; 'Quaternary Glaciations - Extent and Chronology, Part II' [Dyke, 2004]). These often-cited datasets track ice margin recession in 36 time slices spanning 18 ka to 1 ka (all ages in uncalibrated radiocarbon years) using a combination of geomorphology, stratigraphy and radiocarbon dating. However, by virtue of being over 15 years old, the ice margin chronology requires updating to reflect new work and important revisions. This paper updates the aforementioned 36 ice margin maps to reflect new data from regional studies. We also update the original radiocarbon dataset from the 2003/2004 papers with 1541 new ages to reflect work up to and including 2018. A major revision is made to the 18 ka ice margin, where Banks and Eglinton islands (once considered to be glacial refugia) are now shown to be fully glaciated. Our updated 18 ka ice sheet increased in areal extent from 17.81 to 18.37 million km(2), which is an increase of 3.1% in spatial coverage of the NAISC at that time. Elsewhere, we also summarize, region-by-region, significant changes to the deglaciation sequence. This paper integrates new information provided by regional experts and radiocarbon data into the deglaciation sequence while maintaining consistency with the original ice margin positions of Dyke et al. (2003) and Dyke (2004) where new information is lacking; this is a pragmatic solution to satisfy the needs of a Quaternary research community that requires up-to-date knowledge of the pattern of ice margin recession of what was once the world's largest ice mass. The 36 updated isochrones are available in PDF and shapefile format, together with a spreadsheet of the expanded radiocarbon dataset (n = 5195 ages) and estimates of uncertainty for each interval. (C) 2020 Elsevier Ltd. All rights reserved.
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskapx Naturgeografi0 (SwePub)105072 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Physical Geography0 (SwePub)105072 hsv//eng
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskapx Geologi0 (SwePub)105042 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Geology0 (SwePub)105042 hsv//eng
653 a Quaternary
653 a Glaciation
653 a North America
653 a Ice margin chronology
653 a Radiocarbon
653 a glacial lake agassiz
653 a early holocene deglaciation
653 a late wisconsinan
653 a glaciation
653 a baffin-island
653 a younger dryas
653 a hudson strait
653 a new-york
653 a cosmogenic radionuclides
653 a atmospheric circulation
653 a quaternary glaciation
653 a Physical Geography
653 a Geology
700a Margold, M.4 aut
700a Stokes, C. R.4 aut
700a Tarasov, L.4 aut
700a Dyke, A. S.4 aut
700a Adams, R. S.4 aut
700a Allard, S.4 aut
700a Arends, H. E.4 aut
700a Atkinson, N.4 aut
700a Attig, J. W.4 aut
700a Barnett, P. J.4 aut
700a Barnett, R. L.4 aut
700a Batterson, M.4 aut
700a Bernatchez, P.4 aut
700a Borns, H. W.4 aut
700a Breckenridge, A.4 aut
700a Briner, J. P.4 aut
700a Brouard, E.4 aut
700a Campbell, J. E.4 aut
700a Carlson, A. E.4 aut
700a Clague, J. J.4 aut
700a Curry, B. B.4 aut
700a Daigneault, R. A.4 aut
700a Dube-Loubert, H.4 aut
700a Easterbrook, D. J.4 aut
700a Franzi, D. A.4 aut
700a Friedrich, H. G.4 aut
700a Funder, S.4 aut
700a Gauthier, M. S.4 aut
700a Gowan, A. S.4 aut
700a Harris, K. L.4 aut
700a Hetu, B.4 aut
700a Hooyer, T. S.4 aut
700a Jennings, C. E.4 aut
700a Johnson, Mark D.,d 1954u Gothenburg University,Göteborgs universitet,Institutionen för geovetenskaper,Department of Earth Sciences4 aut0 (Swepub:gu)xjohnm
700a Kehew, A. E.4 aut
700a Kelley, S. E.4 aut
700a Kerr, D.4 aut
700a King, E. L.4 aut
700a Kjeldsen, K. K.4 aut
700a Knaeble, A. R.4 aut
700a Lajeunesse, P.4 aut
700a Lakeman, T. R.4 aut
700a Lamothe, M.4 aut
700a Larson, P.4 aut
700a Lavoie, M.4 aut
700a Loope, H. M.4 aut
700a Lowell, T. V.4 aut
700a Lusardi, B. A.4 aut
700a Manz, L.4 aut
700a McMartin, I.4 aut
700a Nixon, F. C.4 aut
700a Occhietti, S.4 aut
700a Parkhill, M. A.4 aut
700a Piper, D. J. W.4 aut
700a Pronk, A. G.4 aut
700a Richard, P. J. H.4 aut
700a Ridge, J. C.4 aut
700a Ross, M.4 aut
700a Roy, M.4 aut
700a Seaman, A.4 aut
700a Shaw, J.4 aut
700a Stea, R. R.4 aut
700a Teller, J. T.4 aut
700a Thompson, W. B.4 aut
700a Thorleifson, L. H.4 aut
700a Utting, D. J.4 aut
700a Veillette, J. J.4 aut
700a Ward, B. C.4 aut
700a Weddle, T. K.4 aut
700a Wright, H. E.4 aut
710a Göteborgs universitetb Institutionen för geovetenskaper4 org
773t Quaternary Science Reviewsd : Elsevier BVg 234q 234x 0277-3791
856u http://dro.dur.ac.uk/30354/1/30354.pdf
8564 8u https://gup.ub.gu.se/publication/293435
8564 8u https://doi.org/10.1016/j.quascirev.2020.106223

Hitta via bibliotek

Till lärosätets databas

Kungliga biblioteket hanterar dina personuppgifter i enlighet med EU:s dataskyddsförordning (2018), GDPR. Läs mer om hur det funkar här.
Så här hanterar KB dina uppgifter vid användning av denna tjänst.

 
pil uppåt Stäng

Kopiera och spara länken för att återkomma till aktuell vy