Idioma: Inglés
Publicado por Cambridge University Press, 2021
ISBN 10: 1108810705 ISBN 13: 9781108810708
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Idioma: Inglés
Publicado por Cambridge University Press, 2021
ISBN 10: 1108810705 ISBN 13: 9781108810708
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Idioma: Inglés
Publicado por Cambridge University Press, 2021
ISBN 10: 1108810705 ISBN 13: 9781108810708
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Idioma: Inglés
Publicado por Cambridge University Press, 2021
ISBN 10: 1108810705 ISBN 13: 9781108810708
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Idioma: Inglés
Publicado por Cambridge University Press, Cambridge, 2021
ISBN 10: 1108810705 ISBN 13: 9781108810708
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Añadir al carritoPaperback. Condición: 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.
Idioma: Inglés
Publicado por Cambridge University Press, 2021
ISBN 10: 1108810705 ISBN 13: 9781108810708
Librería: Majestic Books, Hounslow, Reino Unido
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Idioma: Inglés
Publicado por Cambridge University Press, 2021
ISBN 10: 1108810705 ISBN 13: 9781108810708
Librería: Books Puddle, New York, NY, Estados Unidos de America
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Añadir al carritoCondición: New. Print on Demand 1st edition NO-PA16APR2015-KAP.
Idioma: Inglés
Publicado por Cambridge University Press, 2021
ISBN 10: 1108810705 ISBN 13: 9781108810708
Librería: Biblios, Frankfurt am main, HESSE, Alemania
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Idioma: Inglés
Publicado por Cambridge University Press, 2021
ISBN 10: 1108810705 ISBN 13: 9781108810708
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Añadir al carritoPaperback. Condición: Brand New. 75 pages. 8.75x6.25x0.25 inches. In Stock. This item is printed on demand.
Idioma: Inglés
Publicado por Cambridge University Press, 2021
ISBN 10: 1108810705 ISBN 13: 9781108810708
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Añadir al carritoPaperback / softback. Condición: New. This item is printed on demand. New copy - Usually dispatched within 5-9 working days.
Idioma: Inglés
Publicado por Cambridge University Press, Cambridge, 2021
ISBN 10: 1108810705 ISBN 13: 9781108810708
Librería: CitiRetail, Stevenage, Reino Unido
EUR 31,59
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Añadir al carritoPaperback. Condición: 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.
Idioma: Inglés
Publicado por Cambridge University Press, Cambridge, 2021
ISBN 10: 1108810705 ISBN 13: 9781108810708
Librería: AussieBookSeller, Truganina, VIC, Australia
EUR 46,35
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Añadir al carritoPaperback. Condición: 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.
Librería: moluna, Greven, Alemania
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Añadir al carritoCondición: 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.