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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...
Autores principales: | Dijkstra, Nikki, Kraal, Peter, Kuypers, Marcel M. M., Schnetger, Bernhard, Slomp, Caroline P. |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Public Library of Science
2014
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Materias: | |
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 |
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