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  • 1
    Call number: SR 90.0009(403)
    In: Memoir
    Type of Medium: Series available for loan
    Pages: 32 S. + 2 pl.
    ISBN: 0660111829
    Series Statement: Memoir / Geological Survey of Canada 403
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 2
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    PANGAEA
    In:  Supplement to: Pendleton, Simon; Miller, Gifford H; Anderson, Robert A; Crump, Sarah E; Zhong, Yafang; Jahn, Alexandra; Geirsdóttir, Áslaug (2017): Episodic Neoglacial expansion and rapid 20th Century retreat of a small ice cap on Baffin Island, Arctic Canada and modeled temperature change. Climate of the Past Discussions, 1-15, https://doi.org/10.5194/cp-2017-27
    Publication Date: 2023-01-13
    Description: Records of Neoglacial glacier activity in the Arctic constructed from moraines are often incomplete due to a preservation bias toward the most extensive advance, usually the Little Ice Age. Recent warming in the Arctic has caused extensive retreat of glaciers over the past several decades, exposing preserved landscapes complete with in situ tundra plants previously entombed by ice. The radiocarbon ages of these plants define the timing of snowline depression and glacier advance across the site, in response to local summer cooling. Although most dead plants recently exposed by ice retreat are rapidly removed from the landscape by erosion, where erosive processes are unusually weak, dead plants may remain preserved on the landscape for decades. In such settings, a transect of plant radiocarbon ages can be used to construct a near-continuous chronology of past ice margin advance. Here we present radiocarbon dates from the first such transect on Baffin Island, which directly dates the advance of a small ice cap over the past two millennia. The nature of ice expansion between 20 BCE and ~1000 CE is still uncertain, but episodic advances at ~1000, ~1200, and ~1500 CE led to the maximum Neoglacial dimensions ~1900 CE. We employ a two-dimensional numerical glacier model to reconstruct the pattern of ice expansion inferred from the radiocarbon ages and to explore the sensitivity of the ice cap to temperature change. Model experiments show that at least ~0.44 °C of cooling over the past 2 ka is required for the ice cap to reach its 1900 margin, and that the period from ~1000 to 1900 CE must have been at least 0.25 °C cooler than the previous millennium; results that agree with regional climate model simulations. However, ~3 °C of warming since 1900 CE is required to explain retreat to its present position, and, at the same rate of warming, the ice cap will disappear before 2100 CE.
    Keywords: Baffin Island; Divide_Ice_Cap; ICEM; Ice measurement
    Type: Dataset
    Format: application/zip, 754.2 kBytes
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  • 3
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    PANGAEA
    In:  Supplement to: Harning, David J; Andrews, John T; Belt, Simon T; Cabedo-Sanz, Patricia; Geirsdóttir, Áslaug; Dildar, Nadia; Miller, Gifford H; Sepúlveda, Julio (2019): Sea Ice Control on Winter Subsurface Temperatures of the North Iceland Shelf During the Little Ice Age: A TEX86 Calibration Case Study. Paleoceanography and Paleoclimatology, 34(6), 1006-1021, https://doi.org/10.1029/2018PA003523
    Publication Date: 2023-02-12
    Description: Holocene paleoceanographic reconstructions along the North Iceland Shelf have employed a variety of sea surface temperature and sea ice proxies. However, these surface proxies tend to have a seasonal bias toward spring/summer and thus only provide a discrete snapshot of surface conditions during one season. Furthermore, sea surface temperature proxies can be influenced by additional confounding variables resulting in markedly different Holocene temperature reconstructions. Here, we expand Iceland's marine paleoclimate toolkit with TEX86 L: a temperature proxy based on the distribution of archaeal glycerol dibiphytanyl glycerol tetraether (GDGT) lipids. We develop a local Icelandic calibration from 21 surface sediment samples covering a wide environmental gradient across Iceland's insular shelves. Locally calibrated GDGT results demonstrate that (1) TEX86 L reflects winter subsurface (0-200 m) temperatures on the North Iceland Shelf and (2) our calibration produces more realistic temperature estimates with substantially lower uncertainty (S.E. ±4 °C) over global calibrations. We then apply this new calibration to a high‐resolution marine sediment core (last millennium) collected from the central NIS with age control constrained by 14C‐dated mollusks. To test the veracity of the GDGT subsurface temperatures, we analyze quartz and calcite wt% and a series of highly branched isoprenoid alkenes, including the sea ice biomarker IP25, from the same core. The sediment records demonstrate that the development of thick sea ice during the Little Ice Age warmed the subsurface due to winter insulation. Importantly, this observation reflects a seasonal component of the sea ice/ocean feedback to be considered for the nonlinear cooling of the Little Ice Age in and around Iceland.
    Keywords: (9Z)-2,6,10,14-Tetramethyl-7-(3-methylpent-4-enyliden)pentadeca-9-ene per unit sediment mass; 2,6,10,14-Tetramethyl-7-(3-methylpent-4-enyl)pentadecane per unit sediment mass; Acyclic glycerol dialkyl glycerol tetraether; Age; AGE; B997-316; Crenarchaeol; Crenarchaeol regio-isomer; DEPTH, sediment/rock; Dicyclic glycerol dialkyl glycerol tetraether; Diene II per unit sediment mass; GGC; Giant gravity corer; Glycerol dialkyl glycerol tetraethers; Monocyclic glycerol dialkyl glycerol tetraether; North Icelandic Shelf; Sample ID; Temperature, water, winter; Tetraether index of 86 carbon atoms, low-temperature region; Tricyclic glycerol dialkyl glycerol tetraether
    Type: Dataset
    Format: text/tab-separated-values, 490 data points
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  • 4
    Publication Date: 2023-05-12
    Keywords: Age, 14C AMS; Age, dated; Age, dated standard deviation; Comment; D-Alloisoleucine/L-Isoleucine ratio; D-Alloisoleucine/L-Isoleucine ratio, standard deviation; ELEVATION; Nordenskiöld_Bay; Number; OUTCROP; Outcrop sample; Quaternary Environment of the Eurasian North; QUEEN; QUEEN_Exped; Sample code/label; Sample code/label 2; Sample comment; Species
    Type: Dataset
    Format: text/tab-separated-values, 182 data points
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  • 5
    Publication Date: 2023-05-12
    Keywords: Age, 14C milieu/reservoir corrected (-440 yr); Age, dated; Age, dated material; Age, dated standard deviation; ELEVATION; Nordenskiöld_Bay; OUTCROP; Outcrop sample; Quaternary Environment of the Eurasian North; QUEEN; QUEEN_Exped; Sample code/label; δ13C, organic carbon
    Type: Dataset
    Format: text/tab-separated-values, 45 data points
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  • 6
    Publication Date: 2023-05-12
    Keywords: Age, 14C milieu/reservoir corrected (-440 yr); Age, dated; Age, dated material; Age, dated standard deviation; ELEVATION; OUTCROP; Outcrop sample; Quaternary Environment of the Eurasian North; QUEEN; QUEEN_Exped; Sample code/label; Vise_Glacier; δ13C, organic carbon
    Type: Dataset
    Format: text/tab-separated-values, 10 data points
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  • 7
    Publication Date: 2023-05-12
    Keywords: Age, 14C milieu/reservoir corrected (-440 yr); Age, dated; Age, dated material; Age, dated standard deviation; ELEVATION; OUTCROP; Outcrop sample; Quaternary Environment of the Eurasian North; QUEEN; QUEEN_Exped; Sample code/label; Vilkitsky_Bay; δ13C, organic carbon
    Type: Dataset
    Format: text/tab-separated-values, 20 data points
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  • 8
    Publication Date: 2023-06-27
    Keywords: Age, 14C milieu/reservoir corrected; Age, dated; Age, dated material; Age, dated standard deviation; Core62Forman; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GC; Gravity corer; Quaternary Environment of the Eurasian North; QUEEN; QUEEN_Exped; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 41 data points
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  • 9
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    PANGAEA
    In:  Supplement to: Forman, Steven L; Lubinski, David J; Polyak, Leonid; Miller, Gifford H; Matishov, Gennady G; Tarasov, Gennadiy A (1999): Postglacial emergence and Late Quaternary glaciation on northern Novaya Zemlya, Arctic Russia. Boreas, 28(1), 133-145, https://doi.org/10.1111/j.1502-3885.1999.tb00210.x
    Publication Date: 2023-06-27
    Description: Recent observations on postglacial emergence and past glacier extent for one of the least accessible areas in the Arctic, northern Novaya Zemlya are here united. The postglacial marine limit formed 5 to 6 ka is registered on the east and west coasts of the north island at 10 ± 1 and 18 ± 2 m aht, respectively. This modest and late isostatic response along with deglacial ages of 〉9.2 ka on adjacent marine cores from the northern Barents Sea indicate either early (〉13 ka) deglaciation or modest ice sheet loading (〈1500 m thick ice sheet) of Novaya Zemlya. Older and higher (up to 50 m aht) raised beaches were identified beneath a discontinuous glacial drift. Shells from the drift and underlying sublittoral sediments yield minimum limiting 14C ages of 26 to 30 ka on an earlier deglacial event(s). The only moraines identified are within 4 km of present glacier margins and reflect at least three neoglacial advances in the past 2.4 ka.
    Keywords: Cape_SporyNavolok; Core62Forman; GC; Gravity corer; Nordenskiöld_Bay; OUTCROP; Outcrop sample; Quaternary Environment of the Eurasian North; QUEEN; QUEEN_Exped; Vilkitsky_Bay; Vise_Glacier
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 10
    Publication Date: 2023-05-12
    Keywords: Age, 14C milieu/reservoir corrected (-440 yr); Age, dated; Age, dated material; Age, dated standard deviation; Cape_SporyNavolok; ELEVATION; OUTCROP; Outcrop sample; Quaternary Environment of the Eurasian North; QUEEN; QUEEN_Exped; Sample code/label; δ13C, organic carbon
    Type: Dataset
    Format: text/tab-separated-values, 13 data points
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