Middle to late Holocene chironomid-inferred July temperatures for the central Northwest Territories, Canada
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  • 作者:Lindsay M. Upiter (1) (2)
    Jesse C. Vermaire (3) (8)
    R. Timothy Patterson (1) (2)
    Carley A. Crann (1) (2)
    Jennifer M. Galloway (4)
    Andrew L. Macumber (1) (2)
    Lisa A. Neville (1) (2)
    Graeme T. Swindles (5)
    Hendrik Falck (6)
    Helen M. Roe (7)
    Michael F. J. Pisaric (8) (9)
  • 关键词:Chironomids ; Middle to late Holocene ; Paleoclimate ; Northwest Territories ; Particle size analysis ; Loss ; on ; ignition
  • 刊名:Journal of Paleolimnology
  • 出版年:2014
  • 出版时间:August 2014
  • 年:2014
  • 卷:52
  • 期:1-2
  • 页码:11-26
  • 全文大小:1,389 KB
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  • 作者单位:Lindsay M. Upiter (1) (2)
    Jesse C. Vermaire (3) (8)
    R. Timothy Patterson (1) (2)
    Carley A. Crann (1) (2)
    Jennifer M. Galloway (4)
    Andrew L. Macumber (1) (2)
    Lisa A. Neville (1) (2)
    Graeme T. Swindles (5)
    Hendrik Falck (6)
    Helen M. Roe (7)
    Michael F. J. Pisaric (8) (9)

    1. Ottawa-Carleton Geoscience Centre, Carleton University, Ottawa, ON, K1S 5B6, Canada
    2. Department of Earth Sciences, Carleton University, Ottawa, ON, K1S 5B6, Canada
    3. Institute of Environmental Science, Carleton University, Ottawa, ON, K1S 5B6, Canada
    8. Department of Geography and Environmental Studies, Carleton University, Ottawa, ON, K1S 5B6, Canada
    4. Geological Survey of Canada Calgary, 3303-33rd Street NW, Calgary, AB, T2L 2A, Canada
    5. School of Geography, University of Leeds, Leeds, LS2 9JT, UK
    6. Northwest Territories Geoscience Office, P.O. Box 1500, Yellowknife, NT, X1A 2R3, Canada
    7. School of Geography, Archaeology and Palaeoecology, Queen’s University of Belfast, Belfast, BT7 1NN, UK
    9. Department of Geography, Brock University, St. Catharines, ON, L2S 3A1, Canada
  • ISSN:1573-0417
文摘
We analyzed subfossil chironomids, sediment organic matter and sediment particle size data from a 1.11-m-long freeze core collected from Carleton Lake (unofficial name), located approximately 120?km north of the modern treeline. This well-dated core spans the last ca. 6,500?years. Two chironomid transfer functions were applied to infer mean July air temperatures. Our results indicated that the chironomid-inferred temperatures from this lake sediment record did not pass a significance test, suggesting that other factors in addition to temperature may have been important in structuring the chironomid community through time. Although not statistically significant, the chironomid-inferred temperatures from this site do follow a familiar pattern, with highest inferred temperatures occurring during the Holocene Thermal Maximum (~6-?cal?kyr BP), followed by a long-term cooling trend, which is reversed during the last 600?years. The largest change in the chironomid assemblage, which occurred between ca. 4,600 and 3,900?cal?yr BP is possibly related to the well-documented northward advance and subsequent retreat of treeline in this region.

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