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  • PANGAEA  (8)
  • John Wiley & Sons  (1)
  • 2015-2019  (7)
  • 2000-2004  (2)
Document type
Keywords
Years
Year
  • 1
    Publication Date: 2023-02-24
    Keywords: Barium; CAA_Coppermine; Calcium; Canadian Arctic Archipelago; Carbon, organic, dissolved; Chloride; Comment; DATE/TIME; Geochemistry; GEOTRACES; Global marine biogeochemical cycles of trace elements and their isotopes; inorganic carbon; Magnesium; major ions; Potassium; River; rivers; Sodium; Strontium; Sulfate; water isotopes; δ18O, water; δ Deuterium, water
    Type: Dataset
    Format: text/tab-separated-values, 371 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-02-24
    Keywords: Barium; CAA_Freshwater_Creek; Calcium; Canadian Arctic Archipelago; Carbon, organic, dissolved; Chloride; Comment; DATE/TIME; Geochemistry; GEOTRACES; Global marine biogeochemical cycles of trace elements and their isotopes; inorganic carbon; Magnesium; major ions; Potassium; River; rivers; Sodium; Strontium; Sulfate; water isotopes; δ18O, water; δ Deuterium, water
    Type: Dataset
    Format: text/tab-separated-values, 280 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2023-02-24
    Keywords: Alkalinity, total; Barium; CAA_Akpat_Kuunga; CAA_Burnside_River; CAA_Charles_York_River; CAA_Coppermine; CAA_Creswell_River; CAA_Cunningham_River; CAA_Devon_Island; CAA_Ehoktok_Lake; CAA_Ekalluk_River; CAA_Ekalulia_Lake_out; CAA_Ellice_River; CAA_Elu_Inlet; CAA_Ferguson_Lake; CAA_Freshwater_Creek; CAA_Garnier_River; CAA_Glacier_River; CAA_Greiner_LS_Greiner_Lake_in; CAA_Greiner_LS_Greiner_Lake_out; CAA_Greiner_LS_Long_Lake_at_Mount_Pelly; CAA_Greiner_LS_Second_Lake; CAA_Greiner_LS_Upper_Long_Lake; CAA_Halokvik_River; CAA_Jayko_River; CAA_Koignuk_River; CAA_Lake_in_Upper_Tree_River; CAA_Le_Feuvre_Inlet; CAA_Marcil_Creek; CAA_Mecham_River; CAA_Pasley_River; CAA_Rain_Cambridge_Bay_NU; CAA_Rain_Kugluktuk_NU; CAA_Saaqu_River; CAA_Simpson_River; CAA_Small_Lake_North_of_Ehoktok_Lake; CAA_Tingmeak_River; CAA_Tree_River; CAA_Wentzel_Lake; CAA_Western_River; Calcium; Canadian Arctic Archipelago; Carbon, inorganic, dissolved; Carbon, organic, dissolved; Chloride; Comment; DATE/TIME; Event label; Geochemistry; GEOTRACES; Global marine biogeochemical cycles of trace elements and their isotopes; inorganic carbon; LATITUDE; LONGITUDE; Magnesium; major ions; Potassium; River; rivers; Salinity; Sodium; Station label; Strontium; Sulfate; water isotopes; δ18O, water; δ Deuterium, water
    Type: Dataset
    Format: text/tab-separated-values, 634 data points
    Location Call Number Limitation Availability
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  • 4
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    Unknown
    PANGAEA
    Publication Date: 2023-01-13
    Description: Expansion (version 2.0) of the original Land2Sea database of exorheic rivers (Peucker-Ehrenbrink, 2009, doi:10.1029/2008GC002356) that contains information on 1519 rivers, with additional literature estimates of basin size, water discharge (runoff) under current conditions and prior to human intervention, suspended sediment discharge under current conditions and prior to human intervention, estimate of sediment bedload flux, dissolved strontium concentration and radiogenic isotope value as well as particulate (silt or clay) neodymium concentration, isotope composition and Nd model ages. A large addition to the original river database that contains a significant amount of data from the compilation of Meybeck and Ragu (1996) is from Milliman and Farnsworth (2011). The compilation is not yet geo-referenced. The 2156 rivers are sorted alphabetically within each large-scale drainage region (Graham et al., 1999, 2000). In addition, the compilation includes data on sizes of, and sediment discharge from 48 small islands in Oceania with very high sediment yields. Any errors in transcribing data or converting units from their primary sources into this compilation are entirely mine. Acknowledgements: BPE acknowledges financial support from NSR-EAR-0087697, -0125873, -1226818 and ICER-1639557, as well as from WHOI's Investment in Research and Development Fund.
    Type: Dataset
    Format: application/zip, 90.8 kBytes
    Location Call Number Limitation Availability
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  • 5
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    Unknown
    PANGAEA
    In:  Supplement to: Coppola, Alysha I; Wiedemeier, Daniel B; Galy, Valier; Haghipour, Negar; Hanke, Ulrich M; Nascimento, Gabriela S; Usman, Muhammed Ojoshogu; Blattmann, Thomas Michael; Reisser, Moritz; Freymond, Chantal V; Zhao, Meixun; Voss, Britta; Wacker, Lukas; Schefuß, Enno; Peucker-Ehrenbrink, Bernhard; Abiven, Samuel; Schmidt, Michael W I; Eglinton, Timothy Ian (2018): Global-scale evidence for the refractory nature of riverine black carbon. Nature Geoscience, 11(8), 584-588, https://doi.org/10.1038/s41561-018-0159-8
    Publication Date: 2023-01-13
    Description: Wildfires and incomplete combustion of fossil fuel produce large amounts of black carbon. Black carbon production and transport are essential components of the carbon cycle. Constraining estimates of black carbon exported from land to ocean is critical, given ongoing changes in land use and climate, which affect fire occurrence and black carbon dynamics. Here, we present an inventory of the concentration and radiocarbon content (∆14C) of particulate black carbon for 18 rivers around the globe. We find that particulate black carbon accounts for about 15.8 ± 0.9% of river particulate organic carbon, and that fluxes of particulate black carbon co-vary with river-suspended sediment, indicating that particulate black carbon export is primarily controlled by erosion. River particulate black carbon is not exclusively from modern sources but is also aged in intermediate terrestrial carbon pools in several high-latitude rivers, with ages of up to 17,000 14C years. The flux-weighted 14C average age of particulate black carbon exported to oceans is 3,700 ± 400 14C years. We estimate that the annual global flux of particulate black carbon to the ocean is 0.017 to 0.037 Pg, accounting for 4 to 32% of the annually produced black carbon. When buried in marine sediments, particulate black carbon is sequestered to form a long-term sink for CO2.
    Type: Dataset
    Format: application/vnd.openxmlformats-officedocument.spreadsheetml.sheet, 29.3 kBytes
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  • 6
    Publication Date: 2024-01-09
    Keywords: AGE; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Inductively coupled plasma - mass spectrometry (ICP-MS); Italy; Massignano; Ocean Drilling Program; ODP; Osmium; Osmium-187/Osmium-188, error; Osmium-187/Osmium-188 ratio; OUTCROP; Outcrop sample; Rhenium; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 82 data points
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  • 7
    Publication Date: 2024-06-25
    Description: This data set describes geochemical samples collected from 25 rivers and 11 lakes throughout the Canadian Arctic Archipelago (CAA). CAA rivers were sampled as part of the Canadian Arctic Archipelago Rivers Program (CAA-RP) and the Canadian Arctic GEOTRACES program with access via land, water, and air during the summer seasons of August 1-September 9, 2014, and August 11-19, 2015. Time series observations were also collected from the Coppermine River in Kugluktuk, Nunavut (NU) (year-round; August 5, 2014 to August 23, 2016), and from Freshwater Creek in Cambridge Bay, NU (open water only; June 19, 2014 to September 16, 2016). Lake samples were collected opportunistically during float plane air-surveys in 2014 and 2015 as part of the CAA-RP study in the southern CAA. Precipitation was collected during two significant rain events in Kugluktuk, NU (August 25, 2015) and Cambridge Bay, NU (August 20, 2016). River water samples were collected according to methods developed by the Arctic Great Rivers Observatory (Arctic-GRO; http://www.arcticgreatrivers.org/); lake sampling followed the same general methods, with collection carried out in deeper waters away from the shore; rain samples were collected using an HCl cleaned plastic box and processed immediately the morning following the rain event in order to limit the influences of evaporation. Sampling and analytical methods are described in detail in Brown et al., 2020. This data set includes the raw data supplied in Supplementary Tables S2 (Geochemical Data for the CAA-Rivers Project, collected from 2014 - 2016) and S3 (Geochemical Time Series Data for the Coppermine River and Freshwater Creek collected from 2014 - 2016) that accompany Brown et al., 2020. In addition to geochemical observations, the following calculated parameters can be found in Supplementary Table S2 of Brown et al., 2020: drainage basin area; predominant bedrock lithology; percent coverage of lakes; and surficial geology characteristics. These parameters were determined for each river drainage basin as described in the text and associated references found in Brown et al., 2020.
    Keywords: Canadian Arctic Archipelago; Geochemistry; GEOTRACES; Global marine biogeochemical cycles of trace elements and their isotopes; inorganic carbon; major ions; rivers; water isotopes
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
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  • 8
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    Unknown
    PANGAEA
    In:  Supplement to: Ravizza, Gregory E; Peucker-Ehrenbrink, Bernhard (2003): Chemostratigraphic Evidence of Deccan Volcanism from the Marine Osmium Isotope Record. Science, 302(5629), 1392-1395, https://doi.org/10.1126/science.1089209
    Publication Date: 2024-07-02
    Description: Continental flood basalt (CFB) volcanism is hypothesized to have played a causative role in global climate change and mass extinctions. Uncertainties associated with radiometric dating preclude a clear chronological assessment of the environmental consequences of CFB volcanism. Our results document a 25% decline in the marine 187Os/188Os record that predates the Cretaceous-Tertiary boundary (KTB) and coincides with late Maastrichtian warming. We argue that this decline provides a chemostratigraphic marker of Deccan volcanism and thus constitutes compelling evidence that the main environmental consequence of Deccan volcanism was a transient global warming event of 3° to 5°C that is fully resolved from the KTB mass extinction.
    Keywords: 25-245; 74-525A; 86-577_Site; AGE; COMPCORE; Composite Core; Deep Sea Drilling Project; Depth, relative; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Glomar Challenger; Indian Ocean//BASIN; Leg25; Leg74; Leg86; Negative-thermal ionization mass spectrometry (N-TIMS); North Pacific; Osmium; Osmium-187/Osmium-188, error; Osmium-187/Osmium-188 ratio; Sample code/label; South Atlantic/CREST
    Type: Dataset
    Format: text/tab-separated-values, 109 data points
    Location Call Number Limitation Availability
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  • 9
    Publication Date: 2022-05-26
    Description: Author Posting. © American Geophysical Union, 2017. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geochemistry, Geophysics, Geosystems 18 (2017): 3946–3963, doi:10.1002/2017GC007071.
    Description: The sources of terrestrial material delivered to the California margin over the past 7 Myr were assessed using 187Os/188Os, Nd, and Pb isotopes in hydrogenetic ferromanganese crusts from three seamounts along the central and southern California margin. From 6.8 to 4.5 (±0.5) Ma, all three isotope systems show more radiogenic values at Davidson Seamount, located near the base of the Monterey Canyon System, than in Fe-Mn crusts from the more remote Taney and Hoss Seamounts. At the Taney Seamounts, approximately 225 km farther offshore from Davidson Seamount, 187Os/188Os values, but not Pb and Nd isotope ratios, also deviate from the Cenozoic seawater curve toward more radiogenic values from 6.8 to 4.5 (±0.5) Ma. However, none of the isotope systems in Fe-Mn crusts deviate from seawater at Hoss Seamount located approximately 450 km to the south. The regional gradients in isotope ratios indicate that substantial input of dissolved and particulate terrestrial material into the Monterey Canyon System is responsible for the local deviations in the seawater Nd, Pb, and Os isotope compositions from 6.8 to 4.5 (±0.5) Ma. The isotope ratios recorded in Fe-Mn crusts are consistent with a southern Sierra Nevada or western Basin and Range provenance of the terrestrial material which was delivered by rivers to the canyon. The exhumation of the modern Monterey Canyon must have begun between 10 and 6.8 ± 0.5 Ma, as indicated by our data, the age of incised strata, and paleo-location of the Monterey Canyon relative to the paleo-coastline.
    Description: Funding was provided by the United States Geological Survey Pacific Coastal and Marine Science Center Marine Minerals Group, the University of California Santa Cruz Scholarship for Re-Entry Women in Science, and the UCSC Earth and Planetary Science Department Waters Award.
    Description: 2018-05-15
    Keywords: Ferromanganese crusts ; Osmium isotopes ; Neodymium isotopes ; Lead isotopes ; Monterey Canyon System ; Seawater
    Repository Name: Woods Hole Open Access Server
    Type: Article
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