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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...
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| Main Authors: | , , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Public Library of Science
2014
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4079231/ https://ncbi.nlm.nih.gov/pubmed/24988389 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1371/journal.pone.0101139 |
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