Title
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Phosphorus cycling and burial in sediments of a seasonally hypoxic marine basin
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Author
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Abstract
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Recycling of phosphorus (P) from sediments contributes to the development of bottom-water hypoxia in many coastal systems. Here, we present results of a year-long assessment of P dynamics in sediments of a seasonally hypoxic coastal marine basin (Lake Grevelingen, the Netherlands) in 2012. Sequential phosphorus extractions (SEDEX) and X-ray absorption spectroscopy (XAS) indicate that P was adsorbed to Fe-(III)-(oxyhydr)oxides when cable bacteria were active in the surface sediments in spring. With the onset of summer hypoxia, sulphide-induced dissolution of the Fe-(III)-(oxyhydr)oxides led to P release to the pore water and overlying water. The similarity in authigenic Ca-P concentrations in the sediment and suspended matter suggest that Ca-P is not formed in situ. The P burial efficiency was ≤ 32%. Hypoxia-driven sedimentary P recycling had a major impact on the water-column chemistry in the basin in 2012. Water-column monitoring data indicate up to ninefold higher surface water concentrations of phosphate in the basin in the late 1970s and a stronger hypoxia-driven seasonal P release from the sediment. The amplified release of P from the sediment in the past is attributed to the presence of a larger pool of Fe-bound P in the basin prior to the first onset of hypoxia. Given that P is not limiting, primary production in the basin has not been affected by the decadal changes in P availability and recycling over the past 40 years. The changes in P dynamics on decadal time scales were not recorded in sediment profiles of total P or organic C/total P. |
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Language
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English
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Source (journal)
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Estuaries and coasts / Coastal and Estuarine Research Federation [Lawrence, Mass.] - Lawrence, Mass., 2006, currens
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Publication
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Lawrence, Mass.
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Coastal and Estuarine Research Federation
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2018
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ISSN
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1559-2723
[print]
1559-2731
[online]
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DOI
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10.1007/S12237-017-0324-0
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Volume/pages
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41
:4
(2018)
, p. 921-939
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ISI
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000430990300001
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Full text (Publisher's DOI)
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Full text (open access)
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