Are Iron-Phosphate Minerals a Sink for Phosphorus in Anoxic Black Sea Sediments?

Phosphorus (P) is a key nutrient for marine organisms. The only long-term removal pathway for P in the marine realm is burial in sediments. Iron (Fe) bound P accounts for a significant proportion of this burial at the global scale. In sediments underlying anoxic bottom waters, burial of Fe-bound P i...

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Detalles Bibliográficos
Autores principales: Dijkstra, Nikki, Kraal, Peter, Kuypers, Marcel M. M., Schnetger, Bernhard, Slomp, Caroline P.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Public Library of Science 2014
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4079231/
https://www.ncbi.nlm.nih.gov/pubmed/24988389
http://dx.doi.org/10.1371/journal.pone.0101139

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4079231/
https://www.ncbi.nlm.nih.gov/pubmed/24988389
http://dx.doi.org/10.1371/journal.pone.0101139

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