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  • Denitrification  (2)
  • 031-1; AGE; Bottom water temperature; DEPTH, sediment/rock; GC; Gravity corer; Ice volume corrected; Labrador Sea; Magnesium/Calcium ratio; Maria S. Merian; MSM45; MSM45_431-1; δ18O, calcite; δ18O, water  (1)
  • 031-1; Alkenones; GC; Gravity corer; Labrador Sea; Maria S. Merian; Mg/Ca paleothermometry; MSM45; MSM45_431-1; Stable isotopes  (1)
  • 8.2 ka event; ArcTrain; Beckman Coulter Laser diffraction particle size analyzer LS 13 320; Center for Marine Environmental Sciences; Davis Strait; DEPTH, sediment/rock; GC; GeoB19905-1; Gravity corer; Labrador Sea; Maria S. Merian; MARUM; MSM44; MSM44_331-1; Processes and impacts of climate change in the North Atlantic Ocean and the Canadian Arctic; Sample code/label; Size fraction 0.044-0.04 µm; Size fraction 0.048-0.044 µm; Size fraction 0.053-0.048 µm; Size fraction 0.058-0.053 µm; Size fraction 0.064-0.058 µm; Size fraction 0.07-0.064 µm; Size fraction 0.077-0.07 µm; Size fraction 0.084-0.077 µm; Size fraction 0.093-0.084 µm; Size fraction 0.102-0.093 µm; Size fraction 0.112-0.102 µm; Size fraction 0.123-0.112 µm; Size fraction 0.134-0.123 µm; Size fraction 0.148-0.134 µm; Size fraction 0.162-0.148 µm; Size fraction 0.178-0.162 µm; Size fraction 0.195-0.178 µm; Size fraction 0.214-0.195 µm; Size fraction 0.235-0.214 µm; Size fraction 0.258-0.235 µm; Size fraction 0.284-0.258 µm; Size fraction 0.311-0.284 µm; Size fraction 0.342-0.311 µm; Size fraction 0.375-0.342 µm; Size fraction 0.412-0.375 µm; Size fraction 0.452-0.412 µm; Size fraction 0.496-0.452 µm; Size fraction 0.545-0.496 µm; Size fraction 0.598-0.545 µm; Size fraction 0.657-0.598 µm; Size fraction 0.721-0.657 µm; Size fraction 0.791-0.721 µm; Size fraction 0.869-0.791 µm; Size fraction 0.953-0.869 µm; Size fraction 1.047-0.954 µm; Size fraction 1.149-1.047 µm; Size fraction 1.261-1.149 µm; Size fraction 1.385-1.261 µm; Size fraction 1.520-1.385 µm; Size fraction 1.669-1.520 µm; Size fraction 1.832-1.669 µm; Size fraction 10.78-9.819 µm; Size fraction 101.1-92.1 µm; Size fraction 1041-948.3 µm; Size fraction 11.83-10.78 µm; Size fraction 111-101.1 µm; Size fraction 1143-1041 µm; Size fraction 12.99-11.83 µm; Size fraction 121.8-111 µm; Size fraction 1255-1143 µm; Size fraction 133.7-121.8 µm; Size fraction 1377-1255 µm; Size fraction 14.26-12.99 µm; Size fraction 146.8-133.7 µm; Size fraction 15.65-14.26 µm; Size fraction 1512-1377 µm; Size fraction 161.2-146.8 µm; Size fraction 1660-1512 µm; Size fraction 17.18-15.65 µm; Size fraction 176.9-161.2 µm; Size fraction 18.86-17.18 µm; Size fraction 1822-1660 µm; Size fraction 194.2-176.9 µm; Size fraction 2.000-1.822 mm; Size fraction 2.010-1.832 µm; Size fraction 2.208-2.011 µm; Size fraction 2.423-2.208 µm; Size fraction 2.66-2.423 µm; Size fraction 2.92-2.66 µm; Size fraction 20.70-18.86 µm; Size fraction 213.2-194.2 µm; Size fraction 22.73-20.70 µm; Size fraction 234.1-213.2 µm; Size fraction 24.95-22.73 µm; Size fraction 256.9-234.1 µm; Size fraction 27.38-24.95 µm; Size fraction 282.1-256.9 µm; Size fraction 3.206-2.920 µm; Size fraction 3.519-3.206 µm; Size fraction 3.862-3.519 µm; Size fraction 30.07-27.38 µm; Size fraction 309.6-282.1 µm; Size fraction 33.01-30.07 µm; Size fraction 339.9-309.6 µm; Size fraction 36.24-33.01 µm; Size fraction 373.1-339.9 µm; Size fraction 39.77-36.24 µm; Size fraction 4.241-3.862 µm; Size fraction 4.656-4.241 µm; Size fraction 409.6-373.1 µm; Size fraction 43.67-39.78 µm; Size fraction 449.7-409.6 µm; Size fraction 47.94-43.67 µm; Size fraction 493.6-449.7 µm; Size fraction 5.111-4.656 µm; Size fraction 5.611-5.111 µm; Size fraction 52.63-47.94 µm; Size fraction 541.9-493.6 µm; Size fraction 57.77-52.63 µm; Size fraction 594.9-541.9 µm; Size fraction 6.159-5.611 µm; Size fraction 6.761-6.159 µm; Size fraction 63.42-57.77 µm; Size fraction 653.0-594.9 µm; Size fraction 69.62-63.42 µm; Size fraction 7.421-6.761 µm; Size fraction 716.9-653.0 µm; Size fraction 76.43-69.62 µm; Size fraction 786.9-716.9 µm; Size fraction 8.148-7.422 µm; Size fraction 8.944-8.147 µm; Size fraction 83.90-76.43 µm; Size fraction 863.9-786.9 µm; Size fraction 9.819-8.944 µm; Size fraction 92.1-83.9 µm; Size fraction 948.2-863.9 µm; sortable silt; West Greenland Current  (1)
Document type
Keywords
Years
  • 1
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2005. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Global Biogeochemical Cycles 19 (2005): GB4005, doi:10.1029/2005GB002508.
    Description: On the basis of the normalization to phosphate, a significant amount of nitrate is missing from the deep Bering Sea (BS). Benthic denitrification has been suggested previously to be the dominant cause for the BS nitrate deficit. We measured water column nitrate 15N/14N and 18O/16O as integrative tracers of microbial denitrification, together with pore water-derived benthic nitrate fluxes in the deep BS basin, in order to gain new constraints on the mechanism of fixed nitrogen loss in the BS. The lack of any nitrate isotope enrichment into the deep part of the BS supports the benthic denitrification hypothesis. On the basis of the nitrate deficit in the water column with respect to the adjacent North Pacific and a radiocarbon-derived ventilation age of ∼50 years, we calculate an average deep BS (〉2000 m water depth) sedimentary denitrification rate of ∼230 μmol N m−2 d−1 (or 1.27 Tg N yr−1), more than 3 times higher than high-end estimates of the average global sedimentary denitrification rate for the same depth interval. Pore water-derived estimates of benthic denitrification were variable, and uncertainties in estimates were large. A very high denitrification rate measured from the base of the steep northern slope of the basin suggests that the elevated average sedimentary denitrification rate of the deep Bering calculated from the nitrate deficit is driven by organic matter supply to the base of the continental slope, owing to a combination of high primary productivity in the surface waters along the shelf break and efficient down-slope sediment focusing along the steep continental slopes that characterize the BS.
    Description: This study was supported by NSF grants OCE-0136449 and OCE-9981479 to D. M. S., OCE-0118126 and OCE-0324987 to D. C. M., and DFG grant LE 1326/1-1 to M. F. L. The BS cruise was funded by grant OPP-9912122.
    Keywords: Bering Sea ; Denitrification ; Nitrate isotopes
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Format: text/plain
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2004. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 19 (2004): PA4007, doi:10.1029/2003PA001000.
    Description: An analysis of sedimentary nitrogen isotope records compiled from widely distributed marine environments emphasizes the global synchrony of denitrification changes and provides evidence for a strong temporal coupling of these variations to changes in nitrogen fixation as previously inferred. We explain the global coherence of these records by a simple physical control on the flux of dissolved oxygen to suboxic zones and the coupling to fixation via the supply of phosphorus to diazotrophs in suitable environments. According to our hypothesis, lower glacial-stage sea surface temperature increased oxygen solubility, while stronger winds in high-latitude regions enhanced the rate of thermocline ventilation. The resultant colder, rapidly flushed thermocline lessened the spatial extent of denitrification and, consequently, N fixation. During warm periods, sluggish circulation of warmer, less oxygen rich thermocline waters caused expansion of denitrification zones and a concomitant increase in N fixation. Local fluctuations in export productivity would have modulated this global signal.
    Description: Financial support for this work was provided by the Natural Sciences and Engineering Research Council of Canada and by a WHOI postdoctoral fellowship to MK.
    Keywords: Isotopes ; Fixation ; Denitrification
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2024-02-02
    Description: The disintegrated, inorganic grain-size distribution of sediment core GeoB19905-1 was determined every ten centimetres (and in parts higher resolution) to decipher patterns of sediment input to and transport on the southern west Greenland shelf. Prior to measurement, organic matter, calcium carbonate and biogenic silica were chemically removed from the bulk sediment. Measurements were then performed using a Beckman Coulter Laser Diffraction Particle Size Analyzer LS 13320.
    Keywords: 8.2 ka event; ArcTrain; Beckman Coulter Laser diffraction particle size analyzer LS 13 320; Center for Marine Environmental Sciences; Davis Strait; DEPTH, sediment/rock; GC; GeoB19905-1; Gravity corer; Labrador Sea; Maria S. Merian; MARUM; MSM44; MSM44_331-1; Processes and impacts of climate change in the North Atlantic Ocean and the Canadian Arctic; Sample code/label; Size fraction 0.044-0.04 µm; Size fraction 0.048-0.044 µm; Size fraction 0.053-0.048 µm; Size fraction 0.058-0.053 µm; Size fraction 0.064-0.058 µm; Size fraction 0.07-0.064 µm; Size fraction 0.077-0.07 µm; Size fraction 0.084-0.077 µm; Size fraction 0.093-0.084 µm; Size fraction 0.102-0.093 µm; Size fraction 0.112-0.102 µm; Size fraction 0.123-0.112 µm; Size fraction 0.134-0.123 µm; Size fraction 0.148-0.134 µm; Size fraction 0.162-0.148 µm; Size fraction 0.178-0.162 µm; Size fraction 0.195-0.178 µm; Size fraction 0.214-0.195 µm; Size fraction 0.235-0.214 µm; Size fraction 0.258-0.235 µm; Size fraction 0.284-0.258 µm; Size fraction 0.311-0.284 µm; Size fraction 0.342-0.311 µm; Size fraction 0.375-0.342 µm; Size fraction 0.412-0.375 µm; Size fraction 0.452-0.412 µm; Size fraction 0.496-0.452 µm; Size fraction 0.545-0.496 µm; Size fraction 0.598-0.545 µm; Size fraction 0.657-0.598 µm; Size fraction 0.721-0.657 µm; Size fraction 0.791-0.721 µm; Size fraction 0.869-0.791 µm; Size fraction 0.953-0.869 µm; Size fraction 1.047-0.954 µm; Size fraction 1.149-1.047 µm; Size fraction 1.261-1.149 µm; Size fraction 1.385-1.261 µm; Size fraction 1.520-1.385 µm; Size fraction 1.669-1.520 µm; Size fraction 1.832-1.669 µm; Size fraction 10.78-9.819 µm; Size fraction 101.1-92.1 µm; Size fraction 1041-948.3 µm; Size fraction 11.83-10.78 µm; Size fraction 111-101.1 µm; Size fraction 1143-1041 µm; Size fraction 12.99-11.83 µm; Size fraction 121.8-111 µm; Size fraction 1255-1143 µm; Size fraction 133.7-121.8 µm; Size fraction 1377-1255 µm; Size fraction 14.26-12.99 µm; Size fraction 146.8-133.7 µm; Size fraction 15.65-14.26 µm; Size fraction 1512-1377 µm; Size fraction 161.2-146.8 µm; Size fraction 1660-1512 µm; Size fraction 17.18-15.65 µm; Size fraction 176.9-161.2 µm; Size fraction 18.86-17.18 µm; Size fraction 1822-1660 µm; Size fraction 194.2-176.9 µm; Size fraction 2.000-1.822 mm; Size fraction 2.010-1.832 µm; Size fraction 2.208-2.011 µm; Size fraction 2.423-2.208 µm; Size fraction 2.66-2.423 µm; Size fraction 2.92-2.66 µm; Size fraction 20.70-18.86 µm; Size fraction 213.2-194.2 µm; Size fraction 22.73-20.70 µm; Size fraction 234.1-213.2 µm; Size fraction 24.95-22.73 µm; Size fraction 256.9-234.1 µm; Size fraction 27.38-24.95 µm; Size fraction 282.1-256.9 µm; Size fraction 3.206-2.920 µm; Size fraction 3.519-3.206 µm; Size fraction 3.862-3.519 µm; Size fraction 30.07-27.38 µm; Size fraction 309.6-282.1 µm; Size fraction 33.01-30.07 µm; Size fraction 339.9-309.6 µm; Size fraction 36.24-33.01 µm; Size fraction 373.1-339.9 µm; Size fraction 39.77-36.24 µm; Size fraction 4.241-3.862 µm; Size fraction 4.656-4.241 µm; Size fraction 409.6-373.1 µm; Size fraction 43.67-39.78 µm; Size fraction 449.7-409.6 µm; Size fraction 47.94-43.67 µm; Size fraction 493.6-449.7 µm; Size fraction 5.111-4.656 µm; Size fraction 5.611-5.111 µm; Size fraction 52.63-47.94 µm; Size fraction 541.9-493.6 µm; Size fraction 57.77-52.63 µm; Size fraction 594.9-541.9 µm; Size fraction 6.159-5.611 µm; Size fraction 6.761-6.159 µm; Size fraction 63.42-57.77 µm; Size fraction 653.0-594.9 µm; Size fraction 69.62-63.42 µm; Size fraction 7.421-6.761 µm; Size fraction 716.9-653.0 µm; Size fraction 76.43-69.62 µm; Size fraction 786.9-716.9 µm; Size fraction 8.148-7.422 µm; Size fraction 8.944-8.147 µm; Size fraction 83.90-76.43 µm; Size fraction 863.9-786.9 µm; Size fraction 9.819-8.944 µm; Size fraction 92.1-83.9 µm; Size fraction 948.2-863.9 µm; sortable silt; West Greenland Current
    Type: Dataset
    Format: text/tab-separated-values, 14742 data points
    Location Call Number Limitation Availability
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  • 4
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    PANGAEA
    In:  Supplement to: Lochte, Annalena Antonia; Schneider, Ralph R; Kienast, Markus; Repschläger, Janne; Blanz, Thomas; Garbe-Schönberg, Dieter; Andersen, Nils (2020): Surface and subsurface Labrador Shelf water mass conditions during the last 6000 years. Climate of the Past, 16(4), 1127-1143, https://doi.org/10.5194/cp-16-1127-2020
    Publication Date: 2024-06-26
    Description: The Labrador Sea is important for the modern global thermohaline circulation system through the formation of intermediate Labrador Sea Water (LSW) that has been hypothesized to stabilize the modern mode of North Atlantic deep-water circulation. The rate of LSW formation is controlled by the amount of winter heat loss to the atmosphere, the expanse of freshwater in the convection region and the inflow of saline waters from the Atlantic. The Labrador Sea, today, receives freshwater through the East and West Greenland Currents (EGC, WGC) and the Labrador Current (LC). Several studies have suggested the WGC to be the main supplier of freshwater to the Labrador Sea, but the role of the southward flowing LC in Labrador Sea convection is still debated. At the same time, many paleoceanographic reconstructions from the Labrador Shelf focussed on late Deglacial to early Holocene meltwater run-off from the Laurentide Ice Sheet (LIS), whereas little information exists about LC variability since the final melting of the LIS about 7,000 years ago. In order to enable better assessment of the role of the LC in deep-water formation and its importance for Holocene climate variability in Atlantic Canada, this study presents high-resolution middle to late Holocene records of sea surface and bottom water temperatures, freshening and sea ice cover on the Labrador Shelf during the last 6,000 years. Our records reveal that the LC underwent three major oceanographic phases from the Mid- to Late Holocene. From 6.2 to 5.6 ka BP, the LC experienced a cold episode that was followed by warmer conditions between 5.6 and 2.1 ka BP, possibly associated with the late Holocene Thermal Maximum. Although surface waters on the Labrador Shelf cooled gradually after 3 ka BP in response to the Neoglaciation, Labrador Shelf subsurface/bottom waters show a shift to warmer temperatures after 2.1 ka BP. Although such an inverse stratification by cooling of surface and warming of subsurface waters on the Labrador Shelf would suggest a diminished convection during the last two millennia compared to the mid-Holocene, it remains difficult to assess whether hydrographic conditions in the LC have had a significant impact on Labrador Sea deep-water formation.
    Keywords: 031-1; Alkenones; GC; Gravity corer; Labrador Sea; Maria S. Merian; Mg/Ca paleothermometry; MSM45; MSM45_431-1; Stable isotopes
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2024-06-26
    Keywords: 031-1; AGE; Bottom water temperature; DEPTH, sediment/rock; GC; Gravity corer; Ice volume corrected; Labrador Sea; Magnesium/Calcium ratio; Maria S. Merian; MSM45; MSM45_431-1; δ18O, calcite; δ18O, water
    Type: Dataset
    Format: text/tab-separated-values, 1091 data points
    Location Call Number Limitation Availability
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