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The Growth Response of Two Diatom Species to Atmospheric Dust from the Last Glacial Maximum

Relief of iron (Fe) limitation in the surface Southern Ocean has been suggested as one driver of the regular glacial-interglacial cycles in atmospheric carbon dioxide (CO(2)). The proposed cause is enhanced deposition of Fe-bearing atmospheric dust to the oceans during glacial intervals, with conseq...

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Detalles Bibliográficos
Autores principales:	Conway, Tim M., Hoffmann, Linn J., Breitbarth, Eike, Strzepek, Robert F., Wolff, Eric W.
Formato:	Online Artículo Texto
Lenguaje:	English
Publicado:	Public Library of Science 2016
Materias:	Research Article
Acceso en línea:	https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4934930/ https://www.ncbi.nlm.nih.gov/pubmed/27384948 http://dx.doi.org/10.1371/journal.pone.0158553

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