#----------------------------------------------------------------------- # World Data Center for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program #----------------------------------------------------------------------- # NOTE: Please cite Publication, and Online_Resource and date accessed when using these data. If there is no publication information, please cite Investigators, Title, and Online_Resource and date accessed. # # Online_Resource: hurricane.ncdc.noaa.gov/pls/paleox/f?p=519:1:::::P1_STUDY_ID:14734 # Online_Resource: ftp://ftp.ncdc.noaa.gov/pub/data/paleo/paleolimnology/greenland/snoopy2013-1a-1n.txt # # Original_Source_URL: # # Description/Documentation lines begin with # # Data lines have no # # # Archive: Paleolimnology #-------------------- # Contribution_Date # Date: 2013-07-11 #-------------------- # Title # Study_Name: Liverpool Land east Greenland late Holocene expansion of Istorvet ice cap #-------------------- # Investigators # Investigators: Lowell,T,V.;Hall,B.L.;Kelly,M.A.;Bennike,O.;Lusas,A.R.;Honsaker,W.;Smith,C.A.;Levy,L.B.;Travis,S.;Denton,G.H. #-------------------- # Description_and_Notes Description: Data includes Loss-on-Ignition from two lakes (Half and Half and Snoopy) in Liverpool Land, East Greenland. Raw core information is at the Limnological Research Center(LRC)in Minneapolis, MN as are 1/2 of the archive cores. Working cores are at the University of Cincinnati. #-------------------- # Publication # Authors: Thomas V. Lowell, Brenda L. Hall, Meredith A. Kelly, Ole Bennike, Amanda R. Lusas, William Honsaker, Colby A. Smith, Laura B. Levy, Scott Travis,George H. Denton # Published_Date_or_Year: 2013 # Published_Title: Late Holocene expansion of Istorvet ice cap, Liverpool Land, east Greenland # Journal_Name: Quaternary Science Reviews # Volume: 63 # Edition: # Issue: # Pages: 128-140 # Report_Number: # DOI: # Publication_Place: # Publisher: # ISBN: # Online_Resource: # Other_Reference_Details: ISSN 0277-3791 # Full_Citation: # Abstract: The Greenland Ice Sheet is undergoing dynamic changes that will have global implications if they continue into the future. In this regard, an understanding of how the ice sheet responded to past climate changes affords a baseline for anticipating future behavior. Small, independent ice caps adjacent to the Greenland Ice Sheet (hereinafter called “local ice caps”) are sensitive indicators of the response of Greenland ice-marginal zones to climate change. Therefore, we reconstructed late Holocene ice-marginal fluctuations of the local Istorvet ice cap in east Greenland, using radiocarbon dates of subfossil plants, 10Be dates of surface boulders, and analyses of sediment cores from both threshold and control lakes. During the last termination, the Istorvet ice cap had retreated close to its maximum Holocene position by w11,730 cal yr BP. Radiocarbon dates of subfossil plants exposed by recent recession of the ice margin indicate that the Istorvet cap was smaller than at present from AD 200 to AD 1025. Sediments from a threshold lake show no glacial input until the ice cap advanced to within 365 m of its Holocene maximum position bywAD 1150. Thereafter the ice cap remained at or close to this position until at least AD 1660. The timing of this, the most extensive of the Holocene, expansion is similar to that recorded at some glaciers in the Alps and in southern Alaska. However, in contrast to these other regions, the expansion in east Greenland at AD 1150 appears to have been very close to, if not at, a maximum Holocene value. Comparison of the Istorvet ice-cap fluctuations with Holocene glacier extents in Southern Hemisphere middle-to-high latitude locations on the Antarctic Peninsula and in the Andes and the Southern Alps suggests an out-of-phase relationship. If correct, this pattern supports the hypothesis that a bipolar see-saw of oceanic and/or atmospheric circulation during the Holocene produced asynchronous glacier response at some localities in the two polar hemispheres. #------------------ # Funding_Agency # Funding_Agency_Name: National Science Foundation (USA) # Grant: ARC 0908081 #------------------ # Site_Information # Site_Name: Snoopy Lake # Location: # Region: # Country: Greenland # Northernmost_Latitude: 70.977 # Southernmost_Latitude: 70.977 # Easternmost_Longitude: -22.293 # Westernmost_Longitude: -22.293 # Elevation: 100 #------------------ # Data_Collection # Collection_Name: SPY-1A-1N # Earliest_Year: # Most_Recent_Year: # Time_Unit: # Core_Length: # Notes: #------------------ # Species: #------------------ # Chronology: #---------------- # Variables # Short_name What,Material,Error,Units, Seasonality,Archive,Details,Method,Data_type depth_cm Depth,,,cm,,,,,N LOI_percent Loss On Ignition,sediment,,percent,,paleolimnology,,,,N #---------------- # Data # Missing_Values: # # Data line format - tab-delimited text, variable short name as header depth_cm LOI_percent 0 34.1176 2 30.9278 4 28.1553 6 31.7647 8 27.7228 10 29.5455 12 27.7778 14 27.1739 16 25.2101 18 41.1765 20 37.3494 22 31.1828 24 36.4865 26 36.1446 28 31.5217 30 26.6055 32 20.5882 34 32.381 36 30.6122 38 31.3725 40 20.1258 42 29.4643 44 30.1724 46 26.1905 48 31.4286 50 31.7757 52 32.7273 54 30 56 33.3333 58 33.3333 60 35.3535 62 30.7692 64 35.7895 66 38.835 68 38.0952 70 33.9806 72 34.7826 74 39.7849 76 38.75 78 38.0952 80 26.7241 82 36.6667 84 33.3333 86 26.6055 88 37.2093 90 35.3535 92 34.375 94 36.3636 96 34.7826 98 43.5294 100 38.4615 102 29.2308 104 13.6364