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  • 1
    Publication Date: 2013-02-26
    Description: [1]  Three vertical profiles of rare earth element concentrations and Nd isotopic compositions have been measured in the remote southeast Pacific Ocean. The three stations represent contrasting environments: the oligotrophic center of the gyre (station GYR), the “transition zone” east of the South Tropical Front (station EGY), and the Peru-Chile upwelling marked by a pronounced oxygen minimum (station UPX). Rare earth concentrations display nutrient like vertical profiles except at UPX where surface waters are enriched. At this station Nd isotopic compositions are clearly more radiogenic than in the open ocean, suggesting that boundary exchange process is releasing lithogenic rare earth element from the volcanic Andes. Unexpected radiogenic values ( ε Nd reaching –3.7) are also observed at 2000 m at station GYR in the Upper Circumpolar Deep Water that commonly have ε Nd values around –6. Exchange processes related to hydrothermal activity are suspected to produce this increase in ε Nd in the vicinity of the East Pacific Rise. These results provide some guidance for higher resolution studies planned in this region by the international GEOTRACES program.
    Electronic ISSN: 1525-2027
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 2
    Publication Date: 2011-06-30
    Description: Nd isotopic compositions ($\varepsilon$Nd) of seawater profiles and deep-sea corals collected off the coast of Iberia and from the Bay of Biscay were measured (1) to constrain the Nd isotopic composition of water masses along the southwest European margin, (2) to track the Mediterranean Outflow Water (MOW) during its northward propagation, and (3) to establish hydrological changes during the last 1500 years. The Eastern North Atlantic Central Water (ENACW) is characterized by Nd isotopic composition of around −12.0. Mediterranean Sea Water (MSW) is collected from 800 and 1200 m depth and is characterized by $\varepsilon$Nd values ranging from −10.9, off the coast of Iberia, to −11.6 in the Bay of Biscay. These $\varepsilon$Nd results suggest a strong dilution of the pure MOW at the Strait of Gibraltar ($\varepsilon$Nd −9.4) of approximately 40% and 30% along its northward circulation pathway essentially with a contribution from ENACW. At around 2000 m depth, $\varepsilon$Nd water profiles display the occurrence of a nonradiogenic water mass ($\varepsilon$Nd −13), originating from the Labrador Sea (Labrador Sea Water). Fossil deep-sea corals, dated between 84 and 1500 years, display Nd isotopic compositions that vary moderately from present-day seawater values, suggesting a weaker influence of MOW in the formation of MSW during the Dark Ages and the Little Ice Age. These recent cold events seem to be associated with a reduction in the northward penetration of MSW, which may result from a greater eastward extension of the middepth subpolar gyre and/or a reduction of MSW formation, likely tied to a variation in deep Mediterranean water production.
    Electronic ISSN: 1525-2027
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 3
    Publication Date: 2016-01-09
    Description: Human activity is leaving a pervasive and persistent signature on Earth. Vigorous debate continues about whether this warrants recognition as a new geologic time unit known as the Anthropocene. We review anthropogenic markers of functional changes in the Earth system through the stratigraphic record. The appearance of manufactured materials in sediments, including aluminum, plastics, and concrete, coincides with global spikes in fallout radionuclides and particulates from fossil fuel combustion. Carbon, nitrogen, and phosphorus cycles have been substantially modified over the past century. Rates of sea-level rise and the extent of human perturbation of the climate system exceed Late Holocene changes. Biotic changes include species invasions worldwide and accelerating rates of extinction. These combined signals render the Anthropocene stratigraphically distinct from the Holocene and earlier epochs.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Waters, Colin N -- Zalasiewicz, Jan -- Summerhayes, Colin -- Barnosky, Anthony D -- Poirier, Clement -- Galuszka, Agnieszka -- Cearreta, Alejandro -- Edgeworth, Matt -- Ellis, Erle C -- Ellis, Michael -- Jeandel, Catherine -- Leinfelder, Reinhold -- McNeill, J R -- Richter, Daniel deB -- Steffen, Will -- Syvitski, James -- Vidas, Davor -- Wagreich, Michael -- Williams, Mark -- Zhisheng, An -- Grinevald, Jacques -- Odada, Eric -- Oreskes, Naomi -- Wolfe, Alexander P -- New York, N.Y. -- Science. 2016 Jan 8;351(6269):aad2622. doi: 10.1126/science.aad2622.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉British Geological Survey, Keyworth, Nottingham NG12 5GG, UK. ; Department of Geology, University of Leicester, University Road, Leicester LE1 7RH, UK. ; Scott Polar Research Institute, Cambridge University, Lensfield Road, Cambridge CB2 1ER, UK. ; Department of Integrative Biology, Museum of Paleontology, and Museum of Vertebrate Zoology, University of California-Berkeley, Berkeley, CA 94720, USA. ; Morphodynamique Continentale et Cotiere, Universite de Caen Normandie, Centre National de la Recherche Scientifique (CNRS), 24 Rue des Tilleuls, F-14000 Caen, France. ; Geochemistry and the Environment Division, Institute of Chemistry, Jan Kochanowski University, 15G Swietokrzyska Street, 25-406 Kielce, Poland. ; Departamento de Estratigrafia y Paleontologia, Facultad de Ciencia y Tecnologia, Universidad del Pais Vasco/Euskal Herriko Unibertsitatea, Apartado 644, 48080 Bilbao, Spain. ; School of Archaeology and Ancient History, University of Leicester, University Road, Leicester LE1 7RH, UK. ; Department of Geography and Environmental Systems, University of Maryland-Baltimore County, Baltimore, MD 21250, USA. ; Laboratoire d'Etudes en Geophysique et Oceanographie Spatiales (CNRS, Centre National d'Etudes Spatiales, Institut de Recherche pour le Developpement, Universite Paul Sabatier), 14 Avenue Edouard Belin, 31400 Toulouse, France. ; Department of Geological Sciences, Freie Universitat Berlin, Malteserstrasse 74-100/D, 12249 Berlin, Germany. ; Georgetown University, Washington, DC, USA. ; Nicholas School of the Environment, Duke University, Box 90233, Durham, NC 27516, USA. ; The Australian National University, Canberra, Australian Capital Territory 0200, Australia. ; Department of Geological Sciences, University of Colorado-Boulder, Box 545, Boulder, CO 80309-0545, USA. ; Marine Affairs and Law of the Sea Programme, The Fridtjof Nansen Institute, Lysaker, Norway. ; Department of Geodynamics and Sedimentology, University of Vienna, A-1090 Vienna, Austria. ; State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, Beijing Normal University, Beijing 100875, China. ; Institut de Hautes Etudes Internationales et du Developpement, Chemin Eugene Rigot 2, 1211 Geneve 11, Switzerland. ; Department of Geology, University of Nairobi, Nairobi, Kenya. ; Department of the History of Science, Harvard University, Cambridge, MA 02138, USA. ; Department of Biological Sciences, University of Alberta, Edmonton, Alberta T6G 2E9, Canada.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/26744408" target="_blank"〉PubMed〈/a〉
    Keywords: Aluminum/analysis ; *Biota ; Carbon Cycle ; Climate ; Construction Materials/analysis ; *Earth (Planet) ; Fossil Fuels/adverse effects ; Geologic Sediments/*chemistry ; *Human Activities ; Humans ; Ice/analysis ; Introduced Species ; Plastics/analysis ; Radioactive Fallout/analysis ; Radioisotopes/analysis
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 4
    Publication Date: 2013-03-23
    Description: [1]  Three vertical profiles of rare earth element concentrations and Nd isotopic compositions have been measured in the remote southeast Pacific Ocean. The three stations represent contrasting environments: the oligotrophic center of the gyre (station GYR), the “transition zone” east of the South Tropical Front (station EGY), and the Peru-Chile upwelling marked by a pronounced oxygen minimum (station UPX). Rare earth concentrations display nutrient like vertical profiles except at UPX where surface waters are enriched. At this station Nd isotopic compositions are clearly more radiogenic than in the open ocean, suggesting that boundary exchange process is releasing lithogenic rare earth element from the volcanic Andes. Unexpected radiogenic values ( ε Nd reaching –3.7) are also observed at 2000 m at station GYR in the Upper Circumpolar Deep Water that commonly have ε Nd values around –6. Exchange processes related to hydrothermal activity are suspected to produce this increase in ε Nd in the vicinity of the East Pacific Rise. These results provide some guidance for higher resolution studies planned in this region by the international GEOTRACES program.
    Electronic ISSN: 1525-2027
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 5
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Earth and Planetary Science Letters 117 (1993), S. 581-591 
    ISSN: 0012-821X
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    European journal of clinical pharmacology 43 (1992), S. 295-297 
    ISSN: 1432-1041
    Keywords: Sodium fluoride ; osteoporosis, single-dose pharmacokinetics, age
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Medicine
    Notes: Summary Sodium fluoride (NaF) is used in the treatment of axial osteoporosis and so is mostly given to old patients. Since its pharmacokinetics has not been studied in the elderly, the pharmacokinetics of an enteric-coated tablet containing 50 mg NaF has been investigated in 15 aged inpatients (aged 65 to 75 y) and 12 young healthy volunteers (aged 21 to 26 y). The serum AUC of fluoride was 1.7-time higher in older than in younger subjects. There was a strong inverse correlation between the AUC and either body surface area (BSA) or glomerular filtration rate (GFR), both of which were very much lower in the elderly. This concluded that if efficacy or safety are related to the bioavailability of fluoride, it maybe valuable to adjust the dosage of fluoride accordingly to the GFR and BSA.
    Type of Medium: Electronic Resource
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  • 7
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    Mineralogical Society of America
    In: Elements
    Publication Date: 2018
    Description: 〈span〉Progress in the development of seawater sampling systems, analytical procedures and mass spectrometry have allowed measurements of trace elements and their isotopes in the ocean at spatial resolutions and at concentrations never achieved before. Marine geochemists are now exploiting these new developments to measure, for the first time, the stable isotopes of trace metals that are essential for marine life (e.g. Fe, Cu, Ni, Mo, Zn). The new data have already produced new insights into the interaction between ocean life and dissolved trace constituents and into the sources and sinks of those trace elements.〈/span〉
    Print ISSN: 1811-5209
    Electronic ISSN: 1811-5217
    Topics: Geosciences
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  • 8
    Publication Date: 2015-06-12
    Description: A recently published analysis by Lewis and Maslin (Lewis SL and Maslin MA (2015) Defining the Anthropocene. Nature 519: 171–180) has identified two new potential horizons for the Holocene–Anthropocene boundary: 1610 (associated with European colonization of the Americas), or 1964 (the peak of the excess radiocarbon signal arising from atom bomb tests). We discuss both of these novel suggestions, and consider that there is insufficient stratigraphic basis for the former, whereas placing the latter at the peak of the signal rather than at its inception does not follow normal stratigraphical practice. Wherever the boundary is eventually placed, it should be optimized to reflect stratigraphical evidence with the least possible ambiguity.
    Print ISSN: 2053-0196
    Electronic ISSN: 2053-020X
    Topics: Geography
    Published by Sage
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  • 9
    Publication Date: 2010-10-01
    Print ISSN: 0304-4203
    Electronic ISSN: 1872-7581
    Topics: Geosciences
    Published by Elsevier
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  • 10
    Publication Date: 1984-06-01
    Print ISSN: 0304-4203
    Electronic ISSN: 1872-7581
    Topics: Geosciences
    Published by Elsevier
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