Lingua: Inglese
Editore: Cambridge University Press, 2021
ISBN 10: 110879257X ISBN 13: 9781108792578
Da: GreatBookPrices, Columbia, MD, U.S.A.
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Lingua: Inglese
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ISBN 10: 110879257X ISBN 13: 9781108792578
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EUR 27,48
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Lingua: Inglese
Editore: Cambridge University Press, 2021
ISBN 10: 110879257X ISBN 13: 9781108792578
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Lingua: Inglese
Editore: Cambridge University Press, 2021
ISBN 10: 110879257X ISBN 13: 9781108792578
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Lingua: Inglese
Editore: Cambridge University Press, 2021
ISBN 10: 110879257X ISBN 13: 9781108792578
Da: Kennys Bookshop and Art Galleries Ltd., Galway, GY, Irlanda
EUR 29,84
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Lingua: Inglese
Editore: Cambridge University Press, 2021
ISBN 10: 110879257X ISBN 13: 9781108792578
Da: GreatBookPricesUK, Woodford Green, Regno Unito
EUR 25,67
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Lingua: Inglese
Editore: Cambridge University Press, 2021
ISBN 10: 110879257X ISBN 13: 9781108792578
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EUR 36,64
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Lingua: Inglese
Editore: Cambridge University Press, 2021
ISBN 10: 110879257X ISBN 13: 9781108792578
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Lingua: Inglese
Editore: Cambridge University Press, Cambridge, 2021
ISBN 10: 110879257X ISBN 13: 9781108792578
Da: Grand Eagle Retail, Bensenville, IL, U.S.A.
Paperback. Condizione: new. Paperback. The stable chromium (Cr) isotope system has emerged over the past decade as a new tool to track changes in the amount of oxygen in earth's ocean-atmosphere system. Much of the initial foundation for using Cr isotopes (d53Cr) as a paleoredox proxy has required recent revision. However, the basic idea behind using Cr isotopes as redox tracers is straightforwardthe largest isotope fractionations are redox-dependent and occur during partial reduction of Cr(VI). As such, Cr isotopic signatures can provide novel insights into Cr redox cycling in both marine and terrestrial settings. Critically, the Cr isotope systemunlike many other trace metal proxiescan respond to short-term redox perturbations (e.g., on timescales characteristic of Pleistocene glacial-interglacial cycles). The Cr isotope system can also be used to probe the earth's long-term atmospheric oxygenation, pointing towards low but likely dynamic oxygen levels for the majority of Earth's history. The stable chromium (Cr) isotope system has emerged over the past decade as a new tool to track changes in the amount of oxygen in earth's ocean-atmosphere system. Cr isotopic signatures can provide novel insights into Cr redox cycling in both marine and terrestrial settings. This item is printed on demand. Shipping may be from multiple locations in the US or from the UK, depending on stock availability.
Lingua: Inglese
Editore: Cambridge University Press, 2021
ISBN 10: 110879257X ISBN 13: 9781108792578
Da: Revaluation Books, Exeter, Regno Unito
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Aggiungi al carrelloPaperback. Condizione: Brand New. 75 pages. 8.75x6.25x0.25 inches. In Stock. This item is printed on demand.
Lingua: Inglese
Editore: Cambridge University Press, 2021
ISBN 10: 110879257X ISBN 13: 9781108792578
Da: Majestic Books, Hounslow, Regno Unito
EUR 26,44
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Lingua: Inglese
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ISBN 10: 110879257X ISBN 13: 9781108792578
Da: Books Puddle, New York, NY, U.S.A.
Condizione: New. Print on Demand 1st edition NO-PA16APR2015-KAP.
Lingua: Inglese
Editore: Cambridge University Press, 2021
ISBN 10: 110879257X ISBN 13: 9781108792578
Da: Biblios, Frankfurt am main, HESSE, Germania
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Lingua: Inglese
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ISBN 10: 110879257X ISBN 13: 9781108792578
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EUR 26,17
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Aggiungi al carrelloPaperback / softback. Condizione: New. This item is printed on demand. New copy - Usually dispatched within 5-9 working days.
Lingua: Inglese
Editore: Cambridge University Press, Cambridge, 2021
ISBN 10: 110879257X ISBN 13: 9781108792578
Da: CitiRetail, Stevenage, Regno Unito
EUR 31,54
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Aggiungi al carrelloPaperback. Condizione: new. Paperback. The stable chromium (Cr) isotope system has emerged over the past decade as a new tool to track changes in the amount of oxygen in earth's ocean-atmosphere system. Much of the initial foundation for using Cr isotopes (d53Cr) as a paleoredox proxy has required recent revision. However, the basic idea behind using Cr isotopes as redox tracers is straightforwardthe largest isotope fractionations are redox-dependent and occur during partial reduction of Cr(VI). As such, Cr isotopic signatures can provide novel insights into Cr redox cycling in both marine and terrestrial settings. Critically, the Cr isotope systemunlike many other trace metal proxiescan respond to short-term redox perturbations (e.g., on timescales characteristic of Pleistocene glacial-interglacial cycles). The Cr isotope system can also be used to probe the earth's long-term atmospheric oxygenation, pointing towards low but likely dynamic oxygen levels for the majority of Earth's history. The stable chromium (Cr) isotope system has emerged over the past decade as a new tool to track changes in the amount of oxygen in earth's ocean-atmosphere system. Cr isotopic signatures can provide novel insights into Cr redox cycling in both marine and terrestrial settings. This item is printed on demand. Shipping may be from our UK warehouse or from our Australian or US warehouses, depending on stock availability.
Lingua: Inglese
Editore: Cambridge University Press, Cambridge, 2021
ISBN 10: 110879257X ISBN 13: 9781108792578
Da: AussieBookSeller, Truganina, VIC, Australia
EUR 46,44
Quantità: 1 disponibili
Aggiungi al carrelloPaperback. Condizione: new. Paperback. The stable chromium (Cr) isotope system has emerged over the past decade as a new tool to track changes in the amount of oxygen in earth's ocean-atmosphere system. Much of the initial foundation for using Cr isotopes (d53Cr) as a paleoredox proxy has required recent revision. However, the basic idea behind using Cr isotopes as redox tracers is straightforwardthe largest isotope fractionations are redox-dependent and occur during partial reduction of Cr(VI). As such, Cr isotopic signatures can provide novel insights into Cr redox cycling in both marine and terrestrial settings. Critically, the Cr isotope systemunlike many other trace metal proxiescan respond to short-term redox perturbations (e.g., on timescales characteristic of Pleistocene glacial-interglacial cycles). The Cr isotope system can also be used to probe the earth's long-term atmospheric oxygenation, pointing towards low but likely dynamic oxygen levels for the majority of Earth's history. The stable chromium (Cr) isotope system has emerged over the past decade as a new tool to track changes in the amount of oxygen in earth's ocean-atmosphere system. Cr isotopic signatures can provide novel insights into Cr redox cycling in both marine and terrestrial settings. This item is printed on demand. Shipping may be from our Sydney, NSW warehouse or from our UK or US warehouse, depending on stock availability.
Da: moluna, Greven, Germania
EUR 29,40
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Aggiungi al carrelloCondizione: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. The stable chromium (Cr) isotope system has emerged over the past decade as a new tool to track changes in the amount of oxygen in earth s ocean-atmosphere system. Cr isotopic signatures can provide novel insights into Cr redox cycling in both marine and te.