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  • 1
    ISSN: 1432-1904
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Chemistry and Pharmacology , Natural Sciences in General
    Notes: Abstract  The distribution of partial pressure of carbon dioxide and the concentrations of nitrous oxide and methane were investigated in a cold water filament near the coastal upwelling region off Oman at the beginning of the southwest monsoon in 1997. The results suggest that such filaments are regions of intense biogeochemical activity which may affect the marine cycling of climatically relevant trace gases.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2020-02-06
    Description: Nitrous oxide (N2O) is one of the most important greenhouse gases and a major sink for stratospheric ozone. Estuaries are sites of intense biological production and N2O emissions. We aimed to identify hot spots of N2O production and potential pathways contributing to N2O concentrations in the surface water of the tidal Elbe estuary. During two research cruises in April and June 2015, surface water N2O concentrations were measured along the salinity gradient of the Elbe estuary by using a laser-based on-line analyzer coupled to an equilibrator. Based on these high-resolution N2O profiles, N2O saturations, and fluxes across the surface water/atmosphere interface were calculated. Additional measurements of DIN concentrations, oxygen concentration, and salinity were performed. Highest N2O concentrations were determined in the Hamburg port region reaching maximum values of 32.3 nM in April 2015 and 52.2 nM in June 2015. These results identify the Hamburg port region as a significant hot spot of N2O production, where linear correlations of AOU-N2Oxs indicate nitrification as an important contributor to N2O production in the freshwater part. However, in the region with lowest oxygen saturation, sediment denitrification obviously affected water column N2O saturation. The average N2O saturation over the entire estuary was 201% (SD: ±94%), with an average estuarine N2O flux density of 48 μmol m−2 d−1 and an overall emission of 0.18 Gg N2O y−1. In comparison to previous studies, our data indicate that N2O production pathways over the whole estuarine freshwater part have changed from predominant denitrification in the 1980s toward significant production from nitrification in the present estuary. Despite a significant reduction in N2O saturation compared to the 1980s, N2O concentrations nowadays remain on a high level, comparable to the mid-90s, although a steady decrease of DIN inputs occurred over the last decades. Hence, the Elbe estuary still remains an important source of N2O to the atmosphere.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2017-03-07
    Description: The distribution of partial pressure of carbon dioxide and the concentrations of nitrous oxide and methane were investigated in a cold water filament near the coastal upwelling region off Oman at the beginning of the southwest monsoon in 1997. The results suggest that such filaments are regions of intense biogeochemical activity which may affect the marine cycling of climatically relevant trace gases
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2017-01-31
    Repository Name: EPIC Alfred Wegener Institut
    Type: Miscellaneous , notRev
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  • 5
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Brase, Lisa; Bange, Hermann Werner; Lendt, Ralf; Sanders, Tina; Dähnke, Kirstin (2017): High Resolution Measurements of Nitrous Oxide (N2O) in the Elbe Estuary. Frontiers in Marine Science, 4, https://doi.org/10.3389/fmars.2017.00162
    Publication Date: 2023-07-06
    Description: Nitrous oxide (N2O) is one of the most important greenhouse gases and a major sink for stratospheric ozone. Estuaries are sites of intense biological production and N2O emissions. We aimed to identify hot spots of N2O production and potential pathways contributing to N2O concentrations in the surface water of the tidal Elbe estuary. During two research cruises in April and June 2015, surface water N2O concentrations were measured along the salinity gradient of the Elbe estuary by using a laser-based on-line analyzer coupled to an equilibrator. Based on these high-resolution N2O profiles, N2O saturations, and fluxes across the surface water/atmosphere interface were calculated. Additional measurements of DIN concentrations, oxygen concentration, and salinity were performed. Highest N2O concentrations were determined in the Hamburg port region reaching maximum values of 32.3 nM in April 2015 and 52.2 nM in June 2015. These results identify the Hamburg port region as a significant hot spot of N2O production, where linear correlations of AOU-N2Oxs indicate nitrification as an important contributor to N2O production in the freshwater part. However, in the region with lowest oxygen saturation, sediment denitrification obviously affected water column N2O saturation. The average N2O saturation over the entire estuary was 201% (SD: ±94%), with an average estuarine N2O flux density of 48 ?mol m-2 d-1 and an overall emission of 0.18 Gg N2O y-1. In comparison to previous studies, our data indicate that N2O production pathways over the whole estuarine freshwater part have changed from predominant denitrification in the 1980s toward significant production from nitrification in the present estuary. Despite a significant reduction in N2O saturation compared to the 1980s, N2O concentrations nowadays remain on a high level, comparable to the mid-90s, although a steady decrease of DIN inputs occurred over the last decades. Hence, the Elbe estuary still remains an important source of N2O to the atmosphere.
    Keywords: Ammonium; Continuous flow analyser (AA3, Seal Analytics, Germany); Date/Time of event; DEPTH, water; Elbe Estuary; Event label; FerryBox system; Helmholtz-Zentrum Geesthacht, Institute of Coastal Research; HZG; Latitude of event; Longitude of event; LP201504; LP201504_Stat_1_1; LP201504_Stat_1_10; LP201504_Stat_1_11; LP201504_Stat_1_12; LP201504_Stat_1_13; LP201504_Stat_1_14; LP201504_Stat_1_15; LP201504_Stat_1_16; LP201504_Stat_1_17; LP201504_Stat_1_18; LP201504_Stat_1_19; LP201504_Stat_1_2; LP201504_Stat_1_3; LP201504_Stat_1_4; LP201504_Stat_1_5; LP201504_Stat_1_6; LP201504_Stat_1_7; LP201504_Stat_1_8; LP201504_Stat_1_9; LP201504_Stat_10_1; LP201504_Stat_10_10; LP201504_Stat_10_11; LP201504_Stat_10_12; LP201504_Stat_10_13; LP201504_Stat_10_14; LP201504_Stat_10_15; LP201504_Stat_10_16; LP201504_Stat_10_17; LP201504_Stat_10_18; LP201504_Stat_10_19; LP201504_Stat_10_2; LP201504_Stat_10_20; LP201504_Stat_10_3; LP201504_Stat_10_4; LP201504_Stat_10_5; LP201504_Stat_10_6; LP201504_Stat_10_7; LP201504_Stat_10_8; LP201504_Stat_10_9; LP201504_Stat_11_1; LP201504_Stat_11_10; LP201504_Stat_11_11; LP201504_Stat_11_12; LP201504_Stat_11_13; LP201504_Stat_11_14; LP201504_Stat_11_15; LP201504_Stat_11_16; LP201504_Stat_11_17; LP201504_Stat_11_18; LP201504_Stat_11_19; LP201504_Stat_11_2; LP201504_Stat_11_20; LP201504_Stat_11_3; LP201504_Stat_11_4; LP201504_Stat_11_5; LP201504_Stat_11_6; LP201504_Stat_11_7; LP201504_Stat_11_8; LP201504_Stat_11_9; LP201504_Stat_12_1; LP201504_Stat_12_10; LP201504_Stat_12_2; LP201504_Stat_12_3; LP201504_Stat_12_4; LP201504_Stat_12_5; LP201504_Stat_12_6; LP201504_Stat_12_7; LP201504_Stat_12_8; LP201504_Stat_12_9; LP201504_Stat_13_1; LP201504_Stat_13_10; LP201504_Stat_13_11; LP201504_Stat_13_12; LP201504_Stat_13_13; LP201504_Stat_13_14; LP201504_Stat_13_15; LP201504_Stat_13_2; LP201504_Stat_13_3; LP201504_Stat_13_4; LP201504_Stat_13_5; LP201504_Stat_13_6; LP201504_Stat_13_7; LP201504_Stat_13_8; LP201504_Stat_13_9; LP201504_Stat_14_1; LP201504_Stat_14_2; LP201504_Stat_14_3; LP201504_Stat_14_4; LP201504_Stat_14_5; LP201504_Stat_14_6; LP201504_Stat_15_1; LP201504_Stat_15_2; LP201504_Stat_15_3; LP201504_Stat_15_4; LP201504_Stat_17_1; LP201504_Stat_17_10; LP201504_Stat_17_11; LP201504_Stat_17_12; LP201504_Stat_17_13; LP201504_Stat_17_14; LP201504_Stat_17_15; LP201504_Stat_17_16; LP201504_Stat_17_17; LP201504_Stat_17_2; LP201504_Stat_17_3; LP201504_Stat_17_4; LP201504_Stat_17_5; LP201504_Stat_17_6; LP201504_Stat_17_7; LP201504_Stat_17_8; LP201504_Stat_17_9; LP201504_Stat_18_1; LP201504_Stat_18_2; LP201504_Stat_18_3; LP201504_Stat_19_1; LP201504_Stat_19_10; LP201504_Stat_19_11; LP201504_Stat_19_12; LP201504_Stat_19_13; LP201504_Stat_19_14; LP201504_Stat_19_15; LP201504_Stat_19_16; LP201504_Stat_19_2; LP201504_Stat_19_3; LP201504_Stat_19_4; LP201504_Stat_19_5; LP201504_Stat_19_6; LP201504_Stat_19_7; LP201504_Stat_19_8; LP201504_Stat_19_9; LP201504_Stat_2_1; LP201504_Stat_2_10; LP201504_Stat_2_11; LP201504_Stat_2_12; LP201504_Stat_2_13; LP201504_Stat_2_14; LP201504_Stat_2_15; LP201504_Stat_2_16; LP201504_Stat_2_17; LP201504_Stat_2_18; LP201504_Stat_2_19; LP201504_Stat_2_2; LP201504_Stat_2_3; LP201504_Stat_2_4; LP201504_Stat_2_5; LP201504_Stat_2_6; LP201504_Stat_2_7; LP201504_Stat_2_8; LP201504_Stat_2_9; LP201504_Stat_20_1; LP201504_Stat_20_10; LP201504_Stat_20_11; LP201504_Stat_20_12; LP201504_Stat_20_13; LP201504_Stat_20_14; LP201504_Stat_20_15; LP201504_Stat_20_16; LP201504_Stat_20_17; LP201504_Stat_20_18; LP201504_Stat_20_2; LP201504_Stat_20_3; LP201504_Stat_20_4; LP201504_Stat_20_5; LP201504_Stat_20_6; LP201504_Stat_20_7; LP201504_Stat_20_8; LP201504_Stat_20_9; LP201504_Stat_21_1; LP201504_Stat_21_10; LP201504_Stat_21_11; LP201504_Stat_21_12; LP201504_Stat_21_13; LP201504_Stat_21_14; LP201504_Stat_21_15; LP201504_Stat_21_16; LP201504_Stat_21_17; LP201504_Stat_21_18; LP201504_Stat_21_19; LP201504_Stat_21_2; LP201504_Stat_21_20; LP201504_Stat_21_21; LP201504_Stat_21_22; LP201504_Stat_21_23; LP201504_Stat_21_24; LP201504_Stat_21_25; LP201504_Stat_21_26; LP201504_Stat_21_27; LP201504_Stat_21_28; LP201504_Stat_21_29; LP201504_Stat_21_3; LP201504_Stat_21_30; LP201504_Stat_21_31; LP201504_Stat_21_32; LP201504_Stat_21_33; LP201504_Stat_21_34; LP201504_Stat_21_4; LP201504_Stat_21_5; LP201504_Stat_21_6; LP201504_Stat_21_7; LP201504_Stat_21_8; LP201504_Stat_21_9; LP201504_Stat_22_1; LP201504_Stat_22_10; LP201504_Stat_22_11; LP201504_Stat_22_12; LP201504_Stat_22_13; LP201504_Stat_22_14; LP201504_Stat_22_15; LP201504_Stat_22_16; LP201504_Stat_22_17; LP201504_Stat_22_18; LP201504_Stat_22_2; LP201504_Stat_22_3; LP201504_Stat_22_4; LP201504_Stat_22_5; LP201504_Stat_22_6; LP201504_Stat_22_7; LP201504_Stat_22_8; LP201504_Stat_22_9; LP201504_Stat_23_1; LP201504_Stat_23_10; LP201504_Stat_23_11; LP201504_Stat_23_12; LP201504_Stat_23_13; LP201504_Stat_23_14; LP201504_Stat_23_15; LP201504_Stat_23_16; LP201504_Stat_23_2; LP201504_Stat_23_3; LP201504_Stat_23_4; LP201504_Stat_23_5; LP201504_Stat_23_6; LP201504_Stat_23_7; LP201504_Stat_23_8; LP201504_Stat_23_9; LP201504_Stat_24_1; LP201504_Stat_24_10; LP201504_Stat_24_11; LP201504_Stat_24_12; LP201504_Stat_24_13; LP201504_Stat_24_14; LP201504_Stat_24_15; LP201504_Stat_24_16; LP201504_Stat_24_17; LP201504_Stat_24_18; LP201504_Stat_24_19; LP201504_Stat_24_2; LP201504_Stat_24_3; LP201504_Stat_24_4; LP201504_Stat_24_5; LP201504_Stat_24_6; LP201504_Stat_24_7; LP201504_Stat_24_8; LP201504_Stat_24_9; LP201504_Stat_3_1; LP201504_Stat_3_10; LP201504_Stat_3_11; LP201504_Stat_3_12; LP201504_Stat_3_13; LP201504_Stat_3_14; LP201504_Stat_3_15; LP201504_Stat_3_16; LP201504_Stat_3_17; LP201504_Stat_3_18; LP201504_Stat_3_19; LP201504_Stat_3_2; LP201504_Stat_3_20; LP201504_Stat_3_3; LP201504_Stat_3_4; LP201504_Stat_3_5; LP201504_Stat_3_6; LP201504_Stat_3_7; LP201504_Stat_3_8; LP201504_Stat_3_9; LP201504_Stat_4_1; LP201504_Stat_4_10; LP201504_Stat_4_11; LP201504_Stat_4_12; LP201504_Stat_4_13; LP201504_Stat_4_14; LP201504_Stat_4_15; LP201504_Stat_4_16; LP201504_Stat_4_17; LP201504_Stat_4_18; LP201504_Stat_4_19; LP201504_Stat_4_2; LP201504_Stat_4_20; LP201504_Stat_4_3; LP201504_Stat_4_4; LP201504_Stat_4_5; LP201504_Stat_4_6; LP201504_Stat_4_7; LP201504_Stat_4_8; LP201504_Stat_4_9; LP201504_Stat_5_1; LP201504_Stat_5_10; LP201504_Stat_5_11; LP201504_Stat_5_12; LP201504_Stat_5_13; LP201504_Stat_5_14; LP201504_Stat_5_15; LP201504_Stat_5_16; LP201504_Stat_5_17; LP201504_Stat_5_18; LP201504_Stat_5_19; LP201504_Stat_5_2; LP201504_Stat_5_20; LP201504_Stat_5_3; LP201504_Stat_5_4; LP201504_Stat_5_5; LP201504_Stat_5_6; LP201504_Stat_5_7; LP201504_Stat_5_8; LP201504_Stat_5_9; LP201504_Stat_6_1; LP201504_Stat_6_10; LP201504_Stat_6_11; LP201504_Stat_6_12; LP201504_Stat_6_13; LP201504_Stat_6_14; LP201504_Stat_6_15; LP201504_Stat_6_16; LP201504_Stat_6_17; LP201504_Stat_6_18; LP201504_Stat_6_19; LP201504_Stat_6_2; LP201504_Stat_6_20; LP201504_Stat_6_3; LP201504_Stat_6_4; LP201504_Stat_6_5; LP201504_Stat_6_6; LP201504_Stat_6_7; LP201504_Stat_6_8; LP201504_Stat_6_9; LP201504_Stat_7_1; LP201504_Stat_7_10; LP201504_Stat_7_11; LP201504_Stat_7_12; LP201504_Stat_7_13; LP201504_Stat_7_14; LP201504_Stat_7_15; LP201504_Stat_7_16; LP201504_Stat_7_17; LP201504_Stat_7_18; LP201504_Stat_7_19; LP201504_Stat_7_2; LP201504_Stat_7_20; LP201504_Stat_7_3; LP201504_Stat_7_4; LP201504_Stat_7_5; LP201504_Stat_7_6; LP201504_Stat_7_7; LP201504_Stat_7_8; LP201504_Stat_7_9; LP201504_Stat_8_1; LP201504_Stat_8_2; LP201504_Stat_8_3; LP201504_Stat_9_1; LP201504_Stat_9_10; LP201504_Stat_9_11; LP201504_Stat_9_12; LP201504_Stat_9_13; LP201504_Stat_9_14; LP201504_Stat_9_15; LP201504_Stat_9_2; LP201504_Stat_9_3; LP201504_Stat_9_4; LP201504_Stat_9_5; LP201504_Stat_9_6; LP201504_Stat_9_7; LP201504_Stat_9_8; LP201504_Stat_9_9; LP201506; LP201506_Stat_25_1; LP201506_Stat_25_10; LP201506_Stat_25_11; LP201506_Stat_25_12; LP201506_Stat_25_13; LP201506_Stat_25_14; LP201506_Stat_25_15; LP201506_Stat_25_16; LP201506_Stat_25_2; LP201506_Stat_25_3; LP201506_Stat_25_4; LP201506_Stat_25_5;
    Type: Dataset
    Format: text/tab-separated-values, 3585 data points
    Location Call Number Limitation Availability
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  • 6
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    Unknown
    PANGAEA
    In:  Institute for Biogeochemistry and Marine Chemistry, Hamburg University
    Publication Date: 2024-02-01
    Keywords: CT; DATE/TIME; DEPTH, water; Fugacity of carbon dioxide (air, 100% humidity); Fugacity of carbon dioxide in seawater; JGOFS; JGOFS-IN-3; Joint Global Ocean Flux Study; LATITUDE; LONGITUDE; NDIR-based seawater-air equilibration technique; Pressure, atmospheric; Salinity; Ship based meteorological sensor; SO120; SO120-track; Sonne; Temperature, water; Thermosalinograph; TSG; Underway cruise track measurements; Volume fraction of carbon dioxide in dry air; Wind direction; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 229469 data points
    Location Call Number Limitation Availability
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  • 7
    facet.materialart.
    Unknown
    PANGAEA
    In:  Institute for Biogeochemistry and Marine Chemistry, Hamburg University
    Publication Date: 2024-02-01
    Keywords: CT; DATE/TIME; DEPTH, water; Fugacity of carbon dioxide (air, 100% humidity); Fugacity of carbon dioxide in seawater; JGOFS; JGOFS-IN-2; Joint Global Ocean Flux Study; LATITUDE; LONGITUDE; NDIR-based seawater-air equilibration technique; Pressure, atmospheric; Salinity; Ship based meteorological sensor; SO119; SO119-track; Sonne; Temperature, water; Thermosalinograph; TSG; Underway cruise track measurements; Volume fraction of carbon dioxide in dry air; Wind direction; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 194328 data points
    Location Call Number Limitation Availability
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  • 8
    facet.materialart.
    Unknown
    PANGAEA
    In:  Institute for Biogeochemistry and Marine Chemistry, Hamburg University
    Publication Date: 2024-02-17
    Keywords: 06BE19970515-track; Algorithm; CT; DATE/TIME; Depth, bathymetric, interpolated/gridded; DEPTH, water; Distance; extracted from GLOBALVIEW-CO2; extracted from the 2-Minute Gridded Global Relief Data (ETOPO2); extracted from the NCEP/NCAR 40-Year Reanalysis Project; extracted from the World Ocean Atlas 2005; Fugacity of carbon dioxide (water) at equilibrator temperature (wet air); Fugacity of carbon dioxide (water) at sea surface temperature (wet air); JGOFS-IN-2; LATITUDE; LONGITUDE; Pressure, atmospheric; Pressure, atmospheric, interpolated; Quality flag; Recomputed after SOCAT (Pfeil et al., 2013); Salinity; Salinity, interpolated; SO119; SOCAT; Sonne; Surface Ocean CO2 Atlas Project; Temperature, water; Underway cruise track measurements; xCO2 (air), interpolated
    Type: Dataset
    Format: text/tab-separated-values, 409672 data points
    Location Call Number Limitation Availability
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  • 9
    facet.materialart.
    Unknown
    PANGAEA
    In:  Institute for Biogeochemistry and Marine Chemistry, Hamburg University
    Publication Date: 2024-02-17
    Keywords: 06BE19970612-track; Algorithm; CT; DATE/TIME; Depth, bathymetric, interpolated/gridded; DEPTH, water; Distance; extracted from GLOBALVIEW-CO2; extracted from the 2-Minute Gridded Global Relief Data (ETOPO2); extracted from the NCEP/NCAR 40-Year Reanalysis Project; extracted from the World Ocean Atlas 2005; Fugacity of carbon dioxide (water) at equilibrator temperature (wet air); Fugacity of carbon dioxide (water) at sea surface temperature (wet air); JGOFS-IN-3; LATITUDE; LONGITUDE; Pressure, atmospheric; Pressure, atmospheric, interpolated; Quality flag; Recomputed after SOCAT (Pfeil et al., 2013); Salinity; Salinity, interpolated; SO120; SOCAT; Sonne; Surface Ocean CO2 Atlas Project; Temperature, water; Underway cruise track measurements; xCO2 (air), interpolated
    Type: Dataset
    Format: text/tab-separated-values, 488874 data points
    Location Call Number Limitation Availability
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  • 10
    Publication Date: 2024-02-01
    Keywords: Ammonium; Bacteria; Bacteria, biomass as carbon; Carbon, inorganic, dissolved; Carbon, organic, particulate; Carbon/nitrogen analyser (GF/F filtered); Carbon biomass estimation (unspec.); Chlorophyll a; Chlorophyll a, fluorometric determination (Grasshoff et al., 1983, Chemie GmbH); Conductivity; Continuous Flow Automated Analysis (Gordon et al., 1993, WOCE Tech Rpt 93-1); Coulometric titration (Knap et al., 1996, IOC Manuals and Guides 29, UNESCO); Counting by flow cytometer; CTD, Neil Brown, Mark III B, NB-4; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Epifluorescence microscopy; Epifluorescence microscopy after acridine orange staining; Eukaryotes; Event label; Fluorescence, chlorophyll; JGOFS; JGOFS-IN-3; Joint Global Ocean Flux Study; Latitude of event; Leucine uptake rate; Longitude of event; Nanoflagellates, heterotrophic; Nitrate; Nitrite; Nitrogen, organic, particulate; Oxidation; then autoanalysis (GF/F filtered); Oxidation (alkaline) with borate buffered potassium persulphate; Oxygen; Oxygen, Winkler (Culberson, 1991, WOCE Report 68/91); Phosphate; Phosphorus, particulate; Pressure, water; Salinity; Seawater analysis after Grasshoff et al., 1983 (Verlag Chemie GmbH Weinheim); Silicate; Silicon, particulate; SO120; SO120_CTD02_002; SO120_CTD03_003; SO120_CTD04_004; SO120_CTD05_005; SO120_CTD06_006; SO120_CTD07_007; SO120_CTD08_008; SO120_CTD09_009; SO120_CTD10_010; SO120_CTD11_011; SO120_CTD12_012; SO120_CTD13_013; SO120_CTD14_014; SO120_CTD15_016; SO120_CTD15_017; SO120_CTD15_019; SO120_CTD16_023; SO120_CTD17_024; SO120_CTD18_027; SO120_CTD18_029; SO120_CTD19_030; SO120_CTD20_033; SO120_CTD20_034; SO120_CTD21_037; SO120_CTD21_038; SO120_CTD22_040; SO120_CTD23_042; SO120_CTD23_043; SO120_CTD24_046; SO120_CTD24_047; SO120_CTD25_050; SO120_CTD25_051; SO120_CTD25_053; SO120_CTD25_054; SO120_CTD28_055; SO120_CTD28_056; SO120_CTD28_057; SO120_CTD31_058; SO120_CTD31_059; SO120_CTD31_060; SO120_CTD34_062; SO120_CTD34_063; SO120_CTD38_066; SO120_CTD39_068; SO120_CTD39_069; SO120_CTD41_071; SO120_CTD41_072; SO120_CTD43_074; SO120_CTD43_075; Sonne; Temperature, water; Thymidine incorporation; Thymidine uptake rate; Tritiated leucine incorporation (Knap et al., 1996, IOC Manuals and Guides 29)
    Type: Dataset
    Format: text/tab-separated-values, 11513 data points
    Location Call Number Limitation Availability
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