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  • Nitrate  (2)
  • Ammonium; Ammonium, standard deviation; Auto-analyzer II, Technicon; Carbon, organic, particulate; Carbon, organic, particulate, integrated; Carbon, organic, particulate, standard deviation; Carbon dioxide; Carbon dioxide, standard deviation; CORSACS II; DATE/TIME; Date/time end; Event label; International Polar Year (2007-2008); IPY; Mass spectrometer Finnigan MAT 252; Nathaniel B. Palmer; NBP0608; NBP0608_all; NBP9807; NBP9807_all; NBP9807_early; NBP9807_late; Nitrate; Nitrate, standard deviation; Nitrite; Nitrite, standard deviation; Nitrogen, inorganic; Nitrogen, inorganic, standard deviation; Nitrogen, particulate; Nitrogen, particulate, standard deviation; Phosphate; Phosphate, standard deviation; ROAVERRS; Ross Sea; Salinity, brine; Salinity, standard deviation; Sample amount, subset; Sample type; Silicate; Silicate, standard deviation; SNOW; Snow/ice sample; δ13C, carbon dioxide, atmospheric; δ13C, carbon dioxide, standard deviation; δ13C, particulate organic carbon; δ13C, standard deviation  (1)
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  • 1
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    PANGAEA
    In:  Supplement to: Munro, David R; Dunbar, Robert B; Mucciarone, David A; Arrigo, Kevin R; Long, Matthew C (2010): Stable isotope composition of dissolved inorganic carbon and particulate organic carbon in sea ice from the Ross Sea, Antarctica. Journal of Geophysical Research, 115(C9), C09005, https://doi.org/10.1029/2009JC005661
    Publikationsdatum: 2024-05-22
    Beschreibung: We examined controls on the carbon isotopic composition of sea ice brines and organic matter during cruises to the Ross Sea, Antarctica in November/December 1998 and November/December 2006. Brine samples were analyzed for salinity, nutrients, total dissolved inorganic carbon (sum CO2), and the 13C/12C ratio of Sum CO2 (d13C(sum CO2)). Particulate organic matter from sea ice cores was analyzed for percent particulate organic carbon (POC), percent total particulate nitrogen (TPN), and stable carbon isotopic composition (d13C(POC)). Sum CO2 in sea ice brines ranged from 1368 to 7149 µmol/kg, equivalent to 1483 to 2519 µmol/kg when normalized to 34.5 psu salinity (s sum CO2), the average salinity of Ross Sea surface waters. Sea ice primary producers removed up to 34% of the available sum CO2, an amount much higher than the maximum removal observed in sea ice free water. Carbonate precipitation and CO2 degassing may reduce s sum CO2 by a similar amount (e.g., 30%) in the most hypersaline sea ice environments, although brine volumes are low in very cold ice that supports these brines. Brine d13C(sum CO2) ranged from -2.6 to +8.0 per mil while d13C(POC) ranged from -30.5 to -9.2 per mil. Isotopic enrichment of the sum CO2 pool via net community production accounts for some but not all carbon isotopic enrichment of sea ice POC. Comparisons of s sum CO2, d13C(sum CO2), and d13C(POC) within sea ice suggest that epsilon p (the net photosynthetic fractionation factor) for sea ice algae is ~8 per mil smaller than the epsilon p observed for phytoplankton in open water regions of the Ross Sea. These results have implications for modeling of carbon uptake and transformation in the ice-covered ocean and for reconstruction of past sea ice extent based on stable isotopic composition of organic matter in sediment cores.
    Schlagwort(e): Ammonium; Ammonium, standard deviation; Auto-analyzer II, Technicon; Carbon, organic, particulate; Carbon, organic, particulate, integrated; Carbon, organic, particulate, standard deviation; Carbon dioxide; Carbon dioxide, standard deviation; CORSACS II; DATE/TIME; Date/time end; Event label; International Polar Year (2007-2008); IPY; Mass spectrometer Finnigan MAT 252; Nathaniel B. Palmer; NBP0608; NBP0608_all; NBP9807; NBP9807_all; NBP9807_early; NBP9807_late; Nitrate; Nitrate, standard deviation; Nitrite; Nitrite, standard deviation; Nitrogen, inorganic; Nitrogen, inorganic, standard deviation; Nitrogen, particulate; Nitrogen, particulate, standard deviation; Phosphate; Phosphate, standard deviation; ROAVERRS; Ross Sea; Salinity, brine; Salinity, standard deviation; Sample amount, subset; Sample type; Silicate; Silicate, standard deviation; SNOW; Snow/ice sample; δ13C, carbon dioxide, atmospheric; δ13C, carbon dioxide, standard deviation; δ13C, particulate organic carbon; δ13C, standard deviation
    Materialart: Dataset
    Format: text/tab-separated-values, 404 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Publikationsdatum: 2022-05-25
    Beschreibung: 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 Journal of Geophysical Research: Biogeosciences 122 (2017): 2409–2417, doi:10.1002/2017JG003881.
    Beschreibung: Measurements of late springtime nutrient concentrations in Arctic waters are relatively rare due to the extensive sea ice cover that makes sampling difficult. During the SUBICE (Study of Under-ice Blooms In the Chukchi Ecosystem) cruise in May–June 2014, an extensive survey of hydrography and prebloom concentrations of inorganic macronutrients, oxygen, particulate organic carbon and nitrogen, and chlorophyll a was conducted in the northeastern Chukchi Sea. Cold (〈−1.5°C) winter water was prevalent throughout the study area, and the water column was weakly stratified. Nitrate (NO3−) concentration averaged 12.6 ± 1.92 μM in surface waters and 14.0 ± 1.91 μM near the bottom and was significantly correlated with salinity. The highest NO3− concentrations were associated with winter water within the Central Channel flow path. NO3− concentrations were much reduced near the northern shelf break within the upper halocline waters of the Canada Basin and along the eastern side of the shelf near the Alaskan coast. Net community production (NCP), estimated as the difference in depth-integrated NO3− content between spring (this study) and summer (historical), varied from 28 to 38 g C m−2 a−1. This is much lower than previous NCP estimates that used NO3− concentrations from the southeastern Bering Sea as a baseline. These results demonstrate the importance of using profiles of NO3− measured as close to the beginning of the spring bloom as possible when estimating local NCP. They also show that once the snow melts in spring, increased light transmission through the sea ice to the waters below the ice could fuel large phytoplankton blooms over a much wider area than previously known.
    Beschreibung: NSF Office of Polar Programs Grant Numbers: PLR-1304563, PLR-1303617
    Beschreibung: 2018-03-18
    Schlagwort(e): Chukchi Sea ; Nitrate ; Phytoplankton
    Repository-Name: Woods Hole Open Access Server
    Materialart: Article
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Publikationsdatum: 2022-05-25
    Beschreibung: © The Author(s), 2018. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Frontiers in Marine Science 5 (2018): 362, doi:10.3389/fmars.2018.00362.
    Beschreibung: Major changes to Arctic marine ecosystems have resulted in longer growing seasons with increased phytoplankton production over larger areas. In the Chukchi Sea, the high productivity fuels intense benthic denitrification creating a nitrogen (N) deficit that is transported through the Arctic to the Atlantic Ocean, where it likely fuels N fixation. Given the rapid pace of environmental change and the potentially globally significant N deficit, we conducted experiments aimed at understanding phytoplankton and microbial N utilization in the Chukchi Sea. Ship-board experiments tested the effect of nitrate (NO3-) additions on both phytoplankton and heterotrophic prokaryote abundance, community composition, photophysiology, carbon fixation and NO3- uptake rates. Results support the critical role of NO3- in limiting summer phytoplankton communities to small cells with low production rates. NO3- additions increased particulate concentrations, abundance of large diatoms, and rates of carbon fixation and NO3- uptake by cells 〉1 μm. Increases in the quantum yield and electron turnover rate of photosystem II in +NO3- treatments suggested that phytoplankton in the ambient dissolved N environment were N starved and unable to build new, or repair damaged, reaction centers. While some increases in heterotrophic prokaryote abundance and production were noted with NO3- amendments, phytoplankton competition or grazers likely dampened these responses. Trends toward a warmer more stratified Chukchi Sea will likely enhance summer oligotrophic conditions and further N starve Chukchi Sea phytoplankton communities.
    Beschreibung: Fieldwork and analysis for the ICESCAPE program was supported by Ocean Biology and Biogeochemistry Program of the National Aeronautic and Space Administration under Grant No. NNX10AF42G to KA.
    Schlagwort(e): Phytoplankton ; Nitrogen ; Chukchi Sea ; Nitrate ; Nutrient limitation
    Repository-Name: Woods Hole Open Access Server
    Materialart: Article
    Standort Signatur Einschränkungen Verfügbarkeit
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