Lingua: Inglese
Editore: Cambridge University Press, 2021
ISBN 10: 1108810705 ISBN 13: 9781108810708
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Lingua: Inglese
Editore: Cambridge University Press, 2021
ISBN 10: 1108810705 ISBN 13: 9781108810708
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Lingua: Inglese
Editore: Cambridge University Press, 2021
ISBN 10: 1108810705 ISBN 13: 9781108810708
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Lingua: Inglese
Editore: Cambridge University Press, 2021
ISBN 10: 1108810705 ISBN 13: 9781108810708
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Lingua: Inglese
Editore: Cambridge University Press, Cambridge, 2021
ISBN 10: 1108810705 ISBN 13: 9781108810708
Da: Grand Eagle Retail, Bensenville, IL, U.S.A.
Paperback. Condizione: new. Paperback. Nitrogen is an essential nutrient for life, and its sources and cycling have varied over earth history. Stable isotope ratios of nitrogen compounds (expressed as d15N, in ) are preserved in the sedimentary record and track these changes, providing important insights into associated biogeochemical feedbacks. Here we review the use of nitrogen stable isotope geochemistry in unravelling the evolution of the global N cycle in deep time. We highlight difficulties with preservation, unambiguous interpretations, and local versus global effects. We end with several case studies illustrating how depositional and stratigraphic context is crucial in reliably interpreting d15N records in ancient marine sediments, both in ancient anoxic (Archean) and more recent well oxygenated (Phanerozoic) environments. Stable isotope ratios of nitrogen compounds are preserved in the sedimentary record and track these changes over Earth's history, providing important insights into associated biogeochemical feedbacks. Here we review the use of nitrogen stable isotope geochemistry in unravelling the evolution of the global N cycle in deep time. 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: 1108810705 ISBN 13: 9781108810708
Da: Majestic Books, Hounslow, Regno Unito
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Lingua: Inglese
Editore: Cambridge University Press, 2021
ISBN 10: 1108810705 ISBN 13: 9781108810708
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: 1108810705 ISBN 13: 9781108810708
Da: Biblios, Frankfurt am main, HESSE, Germania
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Lingua: Inglese
Editore: Cambridge University Press, 2021
ISBN 10: 1108810705 ISBN 13: 9781108810708
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Lingua: Inglese
Editore: Cambridge University Press, 2021
ISBN 10: 1108810705 ISBN 13: 9781108810708
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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: 1108810705 ISBN 13: 9781108810708
Da: CitiRetail, Stevenage, Regno Unito
EUR 31,59
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Aggiungi al carrelloPaperback. Condizione: new. Paperback. Nitrogen is an essential nutrient for life, and its sources and cycling have varied over earth history. Stable isotope ratios of nitrogen compounds (expressed as d15N, in ) are preserved in the sedimentary record and track these changes, providing important insights into associated biogeochemical feedbacks. Here we review the use of nitrogen stable isotope geochemistry in unravelling the evolution of the global N cycle in deep time. We highlight difficulties with preservation, unambiguous interpretations, and local versus global effects. We end with several case studies illustrating how depositional and stratigraphic context is crucial in reliably interpreting d15N records in ancient marine sediments, both in ancient anoxic (Archean) and more recent well oxygenated (Phanerozoic) environments. Stable isotope ratios of nitrogen compounds are preserved in the sedimentary record and track these changes over Earth's history, providing important insights into associated biogeochemical feedbacks. Here we review the use of nitrogen stable isotope geochemistry in unravelling the evolution of the global N cycle in deep time. 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: 1108810705 ISBN 13: 9781108810708
Da: AussieBookSeller, Truganina, VIC, Australia
EUR 46,35
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Aggiungi al carrelloPaperback. Condizione: new. Paperback. Nitrogen is an essential nutrient for life, and its sources and cycling have varied over earth history. Stable isotope ratios of nitrogen compounds (expressed as d15N, in ) are preserved in the sedimentary record and track these changes, providing important insights into associated biogeochemical feedbacks. Here we review the use of nitrogen stable isotope geochemistry in unravelling the evolution of the global N cycle in deep time. We highlight difficulties with preservation, unambiguous interpretations, and local versus global effects. We end with several case studies illustrating how depositional and stratigraphic context is crucial in reliably interpreting d15N records in ancient marine sediments, both in ancient anoxic (Archean) and more recent well oxygenated (Phanerozoic) environments. Stable isotope ratios of nitrogen compounds are preserved in the sedimentary record and track these changes over Earth's history, providing important insights into associated biogeochemical feedbacks. Here we review the use of nitrogen stable isotope geochemistry in unravelling the evolution of the global N cycle in deep time. 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. Stable isotope ratios of nitrogen compounds are preserved in the sedimentary record and track these changes over Earth s history, providing important insights into associated biogeochemical feedbacks. Here we review the use of nitrogen stable isotope geoche.