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  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: Elvert, Marcus; Pohlman, John W; Becker, Kevin W; Gaglioti, Benjamin V; Hinrichs, Kai-Uwe; Wooller, Matthew J (2016): Methane turnover and environmental change from Holocene lipid biomarker records in a thermokarst lake in Arctic Alaska. The Holocene, 26(11), 1766-1777, https://doi.org/10.1177/0959683616645942
    Publication Date: 2023-05-12
    Description: Arctic lakes and wetlands contribute a substantial amount of methane to the contemporary atmosphere, yet profound knowledge gaps remain regarding the intensity and climatic control of past methane emissions from this source. In this study, we reconstruct methane turnover and environmental conditions, including estimates of mean annual and summer temperature, from a thermokarst lake (Lake Qalluuraq) on the Arctic Coastal Plain of northern Alaska for the Holocene by using source-specific lipid biomarkers preserved in a radiocarbon-dated sediment core. Our results document a more prominent role for methane in the carbon cycle when the lake basin was an emergent fen habitat between ~12,300 and ~10,000 cal yr BP, a time period closely coinciding with the Holocene Thermal Maximum (HTM) in North Alaska. Enhanced methane turnover was stimulated by relatively warm temperatures, increased moisture, nutrient supply, and primary productivity. After ~10,000 cal yr BP, a thermokarst lake with abundant submerged mosses evolved, and through the mid-Holocene temperatures were approximately 3°C cooler. Under these conditions, organic matter decomposition was attenuated, which facilitated the accumulation of submerged mosses within a shallower Lake Qalluuraq. Reduced methane assimilation into biomass during the mid-Holocene suggests that thermokarst lakes are carbon sinks during cold periods. In the late-Holocene from ~2700 cal yr BP to the most recent time, however, temperatures and carbon deposition rose and methane oxidation intensified, indicating that more rapid organic matter decomposition and enhanced methane production could amplify climate feedback via potential methane emissions in the future.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 5 datasets
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-06-27
    Keywords: AGE; Alaska, USA; Center for Marine Environmental Sciences; Core; CORE; DEPTH, sediment/rock; Diploptene + Hop-21(22)-ene; Friedel-3-ene; Gas chromatography - Flame Ionization Detection (GC-FID); Hop-17(21)-ene; Hop-20(21)-ene; Lake_Qalluuraq; MARUM; n-Alkane, average chain length; n-Alkane C21, per unit sediment mass; n-Alkane C23, per unit sediment mass; n-Alkane C25, per unit sediment mass; n-Alkane C25:2, per unit sediment mass; n-Alkane C27, per unit sediment mass; n-Alkane C29, per unit sediment mass; n-Alkane C31, per unit sediment mass; Taraxer-14-ene
    Type: Dataset
    Format: text/tab-separated-values, 221 data points
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  • 3
    Publication Date: 2023-06-27
    Keywords: AGE; Alaska, USA; Center for Marine Environmental Sciences; Core; CORE; DEPTH, sediment/rock; Diploptene + Hop-21(22)-ene, δ13C; Friedel-3-ene, δ13C; Gas chromatography - Isotope ratio mass spectrometer (GC-IRMS); Hop-17(21)-ene, δ13C; Hop-20(21)-ene, δ13C; Lake_Qalluuraq; MARUM; n-Alkane C21, δ13C; n-Alkane C23, δ13C; n-Alkane C25, δ13C; n-Alkane C25:2, δ13C; n-Alkane C27, δ13C; n-Alkane C29, δ13C; n-Alkane C31, δ13C; Taraxer-14-ene, δ13C
    Type: Dataset
    Format: text/tab-separated-values, 166 data points
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  • 4
    Publication Date: 2023-06-27
    Keywords: AGE; Alaska, USA; Bishomohopanol, δ13C; Center for Marine Environmental Sciences; Cholesterol, δ13C; Core; CORE; DEPTH, sediment/rock; Diplopterol, δ13C; Gas chromatography - Isotope ratio mass spectrometer (GC-IRMS); Lake_Qalluuraq; MARUM; n-Alcohol C22, δ13C; n-Alcohol C24, δ13C; n-Alcohol C26, δ13C; n-Alcohol C28, δ13C; Sitostanol, δ13C; Sitosterol, δ13C
    Type: Dataset
    Format: text/tab-separated-values, 151 data points
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  • 5
    Publication Date: 2023-06-27
    Keywords: AGE; Alaska, USA; Center for Marine Environmental Sciences; Core; CORE; DEPTH, sediment/rock; Diploptene + Hop-21(22)-ene, δD; Friedel-3-ene, δD; Gas chromatography - Isotope ratio mass spectrometer (GC-IRMS); Hop-17(21)-ene, δD; Hop-20(21)-ene, δD; Lake_Qalluuraq; MARUM; n-Alkane C21, δD; n-Alkane C23, δD; n-Alkane C25, δD; n-Alkane C25:2, δD; n-Alkane C27, δD; n-Alkane C29, δD; n-Alkane C31, δD; Taraxer-14-ene, δD
    Type: Dataset
    Format: text/tab-separated-values, 174 data points
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  • 6
    Publication Date: 2023-06-27
    Keywords: AGE; Alaska, USA; Bishomohopanol; Center for Marine Environmental Sciences; Cholesterol; Core; CORE; DEPTH, sediment/rock; Diplopterol; Gas chromatography - Flame Ionization Detection (GC-FID); Lake_Qalluuraq; MARUM; n-Alcohol C22; n-Alcohol C24; n-Alcohol C26; n-Alcohol C28; Sitostanol; Sitosterol
    Type: Dataset
    Format: text/tab-separated-values, 153 data points
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  • 7
    Publication Date: 2019-03-12
    Description: Vast mosaics of lakes, wetlands, and rivers on the Arctic Coastal Plain give the impression of water surplus. Yet long winters lock freshwater resources in ice, limiting freshwater habitats and water supply for human uses. Increasingly the petroleum industry relies on lakes to build temporary ice roads for winter oil exploration. Permitting water withdrawal for ice roads in Arctic Alaska is dependent on lake depth, ice thickness, and the fish species present. Recent winter warming suggests that more winter water will be available for ice- road construction, yet high interannual variability in ice thickness and summer precipitation complicates habitat impact assessments. To address these concerns, multidisciplinary researchers are working to understand how Arctic freshwater habitats are responding to changes in both climate and water use in northern Alaska. The dynamics of habitat availability and connectivity are being linked to how food webs support fish and waterbirds across diverse freshwater habitats. Moving toward watershed-scale habitat classification coupled with scenario analysis of climate extremes and water withdrawal is increasingly relevant to future resource management decisions in this region. Such progressive refinement in understanding responses to change provides an example of adaptive management focused on ensuring responsible resource development in the Arctic.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 8
    Publication Date: 2022-05-26
    Description: Author Posting. © American Geophysical Union, 2014. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research: Biogeosciences 119 (2014): 1630–1651, doi:10.1002/2014JG002688.
    Description: Continued warming of the Arctic may cause permafrost to thaw and speed the decomposition of large stores of soil organic carbon (OC), thereby accentuating global warming. However, it is unclear if recent warming has raised the current rates of permafrost OC release to anomalous levels or to what extent soil carbon release is sensitive to climate forcing. Here we use a time series of radiocarbon age-offsets (14C) between the bulk lake sediment and plant macrofossils deposited in an arctic lake as an archive for soil and permafrost OC release over the last 14,500 years. The lake traps and archives OC imported from the watershed and allows us to test whether prior warming events stimulated old carbon release and heightened age-offsets. Today, the age-offset (2 ka; thousand of calibrated years before A.D. 1950) and the depositional rate of ancient OC from the watershed into the lake are relatively low and similar to those during the Younger Dryas cold interval (occurring 12.9–11.7 ka). In contrast, age-offsets were higher (3.0–5.0 ka) when summer air temperatures were warmer than present during the Holocene Thermal Maximum (11.7–9.0 ka) and Bølling-Allerød periods (14.5–12.9 ka). During these warm times, permafrost thaw contributed to ancient OC depositional rates that were ~10 times greater than today. Although permafrost OC was vulnerable to climate warming in the past, we suggest surface soil organic horizons and peat are presently limiting summer thaw and carbon release. As a result, the temperature threshold to trigger widespread permafrost OC release is higher than during previous warming events.
    Description: National Science Foundation. Grant Number: ARC-0902169
    Description: 2015-02-22
    Keywords: Radiocarbon ; Lake sediment ; Carbon cycling ; Permafrost ; Paleoclimatology ; Younger Dryas
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: text/plain
    Format: application/pdf
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  • 9
    Publication Date: 2024-01-30
    Description: The formation, growth and drainage of lakes in Arctic and boreal lowland permafrost regions influence landscape and ecosystem processes. These lake and drained lake basin (L-DLB) systems occupy 〉20% of the circumpolar Northern Hemisphere permafrost region and ~50% of the area below 300 m above sea level. Climate change is causing drastic impacts to L-DLB systems, with implications for permafrost dynamics, ecosystem functioning, biogeochemical processes and human livelihoods in lowland permafrost regions. In this Review, we discuss how an increase in the number of lakes as a result of permafrost thaw and an intensifying hydrologic regime are not currently offsetting the land area gained through lake drainage, enhancing the dominance of drained lake basins (DLBs). The contemporary transition from lakes to DLBs decreases hydrologic storage, leads to permafrost aggradation, increases carbon sequestration and diversifies the shifting habitat mosaic in Arctic and boreal regions. However, further warming could inhibit permafrost aggradation in DLBs, disrupting the trajectory of important microtopographic controls on carbon fluxes and ecosystem processes in permafrost-region L-DLB systems. Further research is needed to understand the future dynamics of L-DLB systems to improve Earth system models, permafrost carbon feedback assessments, permafrost hydrology linkages, infrastructure development in permafrost regions and the well-being of northern socio-ecological systems.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 10
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    Unknown
    Springer Nature
    In:  EPIC3Scientific Reports, Springer Nature, 12(1), pp. 7123-7123, ISSN: 2045-2322
    Publication Date: 2024-01-30
    Description: Beavers were not previously recognized as an Arctic species, and their engineering in the tundra is considered negligible. Recent findings suggest that beavers have moved into Arctic tundra regions and are controlling surface water dynamics, which strongly influence permafrost and landscape stability. Here we use 70 years of satellite images and aerial photography to show the scale and magnitude of northwestward beaver expansion in Alaska, indicated by the construction of over 10,000 beaver ponds in the Arctic tundra. The number of beaver ponds doubled in most areas between ~ 2003 and ~ 2017. Earlier stages of beaver engineering are evident in ~ 1980 imagery, and there is no evidence of beaver engineering in ~ 1952 imagery, consistent with observations from Indigenous communities describing the influx of beavers over the period. Rapidly expanding beaver engineering has created a tundra disturbance regime that appears to be thawing permafrost and exacerbating the effects of climate change.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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