The interplay between regeneration and scavenging fluxes drives ocean iron cycling

Iron is crucial for marine photosynthesis, but observational constraints on the magnitude of key iron cycle processes are lacking. Here the authors use a range of observational data sets to demonstrate that the balance between iron re-supply and removal in the subsurface controls upper ocean iron li...

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Autores principales:	Alessandro Tagliabue, Andrew R. Bowie, Timothy DeVries, Michael J. Ellwood, William M. Landing, Angela Milne, Daniel C. Ohnemus, Benjamin S. Twining, Philip W. Boyd
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2019
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/cb377adc0b0a4980978ede579c55c7cc
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spelling	oai:doaj.org-article:cb377adc0b0a4980978ede579c55c7cc2021-12-02T17:01:55ZThe interplay between regeneration and scavenging fluxes drives ocean iron cycling10.1038/s41467-019-12775-52041-1723https://doaj.org/article/cb377adc0b0a4980978ede579c55c7cc2019-10-01T00:00:00Zhttps://doi.org/10.1038/s41467-019-12775-5https://doaj.org/toc/2041-1723Iron is crucial for marine photosynthesis, but observational constraints on the magnitude of key iron cycle processes are lacking. Here the authors use a range of observational data sets to demonstrate that the balance between iron re-supply and removal in the subsurface controls upper ocean iron limitation.Alessandro TagliabueAndrew R. BowieTimothy DeVriesMichael J. EllwoodWilliam M. LandingAngela MilneDaniel C. OhnemusBenjamin S. TwiningPhilip W. BoydNature PortfolioarticleScienceQENNature Communications, Vol 10, Iss 1, Pp 1-8 (2019)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Alessandro Tagliabue Andrew R. Bowie Timothy DeVries Michael J. Ellwood William M. Landing Angela Milne Daniel C. Ohnemus Benjamin S. Twining Philip W. Boyd The interplay between regeneration and scavenging fluxes drives ocean iron cycling
description	Iron is crucial for marine photosynthesis, but observational constraints on the magnitude of key iron cycle processes are lacking. Here the authors use a range of observational data sets to demonstrate that the balance between iron re-supply and removal in the subsurface controls upper ocean iron limitation.
format	article
author	Alessandro Tagliabue Andrew R. Bowie Timothy DeVries Michael J. Ellwood William M. Landing Angela Milne Daniel C. Ohnemus Benjamin S. Twining Philip W. Boyd
author_facet	Alessandro Tagliabue Andrew R. Bowie Timothy DeVries Michael J. Ellwood William M. Landing Angela Milne Daniel C. Ohnemus Benjamin S. Twining Philip W. Boyd
author_sort	Alessandro Tagliabue
title	The interplay between regeneration and scavenging fluxes drives ocean iron cycling
title_short	The interplay between regeneration and scavenging fluxes drives ocean iron cycling
title_full	The interplay between regeneration and scavenging fluxes drives ocean iron cycling
title_fullStr	The interplay between regeneration and scavenging fluxes drives ocean iron cycling
title_full_unstemmed	The interplay between regeneration and scavenging fluxes drives ocean iron cycling
title_sort	interplay between regeneration and scavenging fluxes drives ocean iron cycling
publisher	Nature Portfolio
publishDate	2019
url	https://doaj.org/article/cb377adc0b0a4980978ede579c55c7cc
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The interplay between regeneration and scavenging fluxes drives ocean iron cycling

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