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  • 1
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The sinking of particulate organic matter from ocean surface waters transports carbon to the ocean interior, where almost all is then recycled. The unrecycled fraction of this organic matter can become buried in ocean sediments, thus sequestering carbon and so influencing atmospheric carbon ...
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillian Magazines Ltd.
    Nature 427 (2004), S. 336-339 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Marine sediments act as the ultimate sink for organic carbon, sequestering otherwise rapidly cycling carbon for geologic timescales. Sedimentary organic carbon burial appears to be controlled by oxygen exposure time in situ, and much research has focused on understanding the mechanisms of ...
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1432-1130
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology
    Notes: Abstract In a recent collaborative study intended to extend the variety of reference materials certified for iodine, three mineralization methods were developed to quantify the total iodine content of biological and nutritional materials by inductively coupled plasma mass spectrometry (ICP-MS). A mixture of water-soluble tertiary amines was used as the matrix solution for two oxygen combustion methods and for a simple extraction at room temperature. Calibrations with matrix-matched standards, internal calibration, and isotope dilution with 129I were used. Good agreement between neutron activation analysis (NAA) and the two combustion methods was observed except for 〈 0.1 mg kg–1 iodine concentrations. The amine extraction method gave the most reliable results for the mixed diet, milk powder, and infant formula samples but low recoveries for other biological materials owing to an incomplete extraction and solubilization of iodine. The NAA method, with its freedom from reagent blank, is a useful technique for the independent determination of iodine in biological, environmental and food matrices, especially for verification of iodine results obtained by ICP-MS.
    Type of Medium: Electronic Resource
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  • 4
    ISSN: 1572-8773
    Keywords: hypertension ; inductively coupled plasma-mass spectrometry ; inorganic content ; rat tissues
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Chemistry and Pharmacology
    Notes: Abstract The inorganic contents of bone, brain, erythrocyte, heart, kidney cortex, kidney medulla, liver, lung, muscle and plasma from spontaneously hypertensive rats were compared with those of the same tissues from healthy Sprague-Dawley rats. A general inductively coupled plasma-mass spectrometry method developed for multi-element determinations of most of the elements present in biological tissues was used. Variations were found not only for major elements, as expected, but also for many trace elements in several tissues.
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  • 5
    Publication Date: 2024-02-05
    Description: Palmitic acid (PA) is ubiquitous in the biosphere and its hydrogen isotopic composition (δ2HPA) was proposed as a potential paleoenvironmental proxy for salinity, with δ2HPA values increasing with salinity. In this study, we analyzed 40 surface sediment samples from Baffin Bay and the Labrador Sea to examine the isotopic composition of PA in relation to local environmental variables, including salinity. In contrast to expectations, our results show a negative relationship between the δ2HPA and sea-surface salinity, raising questions about its pertinence/usefulness as a salinity proxy. Instead, our results suggest that the relative abundance of distinct organisms that employ different metabolisms is key in determining the hydrogen isotopic fractionations in PA. Whereas we show that PA is mostly produced through photoautotrophic metabolisms by diatoms and dinoflagellates, varying contributions from heterotrophic metabolisms may obscure the stable isotope composition of PA. Surprisingly, we found no correlation between the stable carbon isotopic composition of the sedimentary organic matter (δ13Corg) and palmitic acid (δ13CPA), implying major differences in either the dominant organisms producing sedimentary PA or in carbon isotope fractionation during lipid biosynthesis. We also found that the presence of extended sea-ice cover leads to enriched carbon and hydrogen isotopic compositions in PA. These enriched values suggest heterotrophic biodegradation in the water column and/or in the sediment as well as an increase in grazing activities. We propose that sea-ice cover and surface water oxygenation modulate the relative impact of phototrophic and heterotrophic metabolisms, and therefore the isotopic composition of marine sedimentary PA.
    Keywords: Average chain length; Baffin Bay; BC; Bottom water salinity, annual mean; Bottom water temperature; Box corer; Carbon; Carbon, inorganic, total; Carbon, organic; Carbon isotopes; Carbon organic/Nitrogen, molar ratio; Carbon Preference Index; Davis Strait; DB3.02; DB3.08; DB3.10; DB3.14; DB3.31; DB3.32; DB3.34; DB3.35; DB6.02; DB6.04; DB6.05; DB6.07; DB6.08; DB6.09; DEPTH, sediment/rock; Dinoflagellate cyst, heterotrophic; Dinoflagellate cyst, per unit sediment mass; Dinoflagellate cyst, phototrophic; Event label; FB1.02; FB1.07; GeoB22315-3; GeoB22318-1; GeoB22319-1; GeoB22344-2; GeoB22350-2; GeoB22353-2; GeoB22356-2; GeoB22358-2; Grab; GRAB; HB2.04; Hexadecanoic acid, δ13C; Hexadecanoic acid, δ13C, standard deviation; Hudson Strait; Hydrogen isotopes; Labrador Sea; lipid biomarkers; Maria S. Merian; MSM45; MSM45_002-4; MSM45_009-3; MSM45_030-3; MSM45_401-4; MSM45_408-3; MSM45_417-3; MSM45_424-3; MSM45_430-3; MSM45-018-3; MSM45-024-3; MSM46; MSM46_11-5; MSM46_14-2; MSM46_25-1; MSM46_28-3; MSM66; MSM66/15-3; MSM66/18-1; MSM66/19-1; MSM66/44-2; MSM66/50-2; MSM66/53-2; MSM66/56-2; MSM66/58-2; MUC; MultiCorer; n-fatty acid C16, per unit mass total organic carbon; n-fatty acid C16, per unit sediment mass; n-fatty acid C16:1, per unit mass total organic carbon; n-fatty acid C16:1, per unit sediment mass; n-fatty acid C18, per unit mass total organic carbon; n-fatty acid C18, per unit sediment mass; n-fatty acid C18:1, per unit mass total organic carbon; n-fatty acid C18:1, per unit sediment mass; n-fatty acid C18:2, per unit mass total organic carbon; n-fatty acid C18:2, per unit sediment mass; Nitrate; Nitrogen; Oxygen, apparent utilization; Oxygen saturation; Paamiut; Paamiut2014; Palmitic acid; Palynomorpha, reworked per unit sediment mass; Phosphate; Pollen, per unit sediment mass; Primary production of carbon per area, yearly; Q7.03; Q7.04; Ratio; Saturated fatty acids, per unit mass total organic carbon; Saturated fatty acids, per unit sediment mass; Sea ice cover duration; Sea surface salinity, annual mean; Sea surface salinity, summer; Sea surface salinity, winter; Sea surface temperature, annual mean; Sea surface temperature, summer; Sea surface temperature, winter; Silicate; Site; Spores per unit sediment mass; U5.04; U5.10; U5.14; V4.03; δ13C, organic carbon; δ18O, water; δ Deuterium, palmitic acid; δ Deuterium, palmitic acid, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 2194 data points
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  • 6
    Publication Date: 2022-05-26
    Description: Author Posting. © The Authors, 2005. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Geochimica et Cosmochimica Acta 70 (2006): 1483-1494, doi:10.1016/j.gca.2005.12.001.
    Description: The chemical composition of the graphitic black carbon (GBC) fraction of marine organic matter was explored in several marine and freshwater sedimentary environments along the west coast of North America and the Pacific Ocean. Analysis by carbon x-ray absorption near edge structure (C-XANES) spectroscopy and scanning transmission x-ray microscopy (STXM) show the GBC-fraction of Stillaguamish River surface sediments to be dominated by more highly-ordered and impure forms of graphite, together forming about 80% of the GBC, with a smaller percent of an aliphatic carbon component. Eel River Margin surface sediments had very little highly-ordered graphite, and were instead dominated by amorphous carbon and to a lesser extent, impure graphite. However, the GBC of surface sediments from the Washington State Slope and the Mexico Margin were composed almost solely of amorphous carbon. Pre-anthropogenic, highly-oxidized deep-sea sediments from the open Equatorial Pacific Ocean contained over half their GBC in different forms of graphite as well as highly-aliphatic carbon, low aromatic/highly-acidic aliphatic carbon, low aromatic/highly aliphatic carbon, and amorphous forms of carbon. Our results clearly show the impact of graphite and amorphous C phases in the BC fraction in modern riverine sediments and nearby marine shelf deposits. The pre-anthropogenic Equatorial Pacific GBC fraction is remarkable in the existence of highly-ordered graphite.
    Description: This work was supported by NSF grants OCE-0221295 and OCE-0118036 (JAB), and OCE-9310364 (SGW), by a NSF Graduate Research Fellowship to A.F.D., and the Canadian National Science and Engineering Research Council to Y.G.
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: 255669 bytes
    Format: application/pdf
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