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Sedimentary phosphorus dynamics and the evolution of bottom-water hypoxia
by
Reed, Daniel C.
, Gustafsson, Bo G.
, Slomp, Caroline P.
in
Animal and plant ecology
/ Animal, plant and microbial ecology
/ Biological and medical sciences
/ Earth sciences
/ Earth, ocean, space
/ Exact sciences and technology
/ External geophysics
/ Fundamental and applied biological sciences. Psychology
/ Geochemistry
/ Marine
/ Mineralogy
/ Physical and chemical properties of sea water
/ Physics of the oceans
/ Sea water ecosystems
/ Silicates
/ Synecology
/ Water geochemistry
2011
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Sedimentary phosphorus dynamics and the evolution of bottom-water hypoxia
by
Reed, Daniel C.
, Gustafsson, Bo G.
, Slomp, Caroline P.
in
Animal and plant ecology
/ Animal, plant and microbial ecology
/ Biological and medical sciences
/ Earth sciences
/ Earth, ocean, space
/ Exact sciences and technology
/ External geophysics
/ Fundamental and applied biological sciences. Psychology
/ Geochemistry
/ Marine
/ Mineralogy
/ Physical and chemical properties of sea water
/ Physics of the oceans
/ Sea water ecosystems
/ Silicates
/ Synecology
/ Water geochemistry
2011
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Do you wish to request the book?
Sedimentary phosphorus dynamics and the evolution of bottom-water hypoxia
by
Reed, Daniel C.
, Gustafsson, Bo G.
, Slomp, Caroline P.
in
Animal and plant ecology
/ Animal, plant and microbial ecology
/ Biological and medical sciences
/ Earth sciences
/ Earth, ocean, space
/ Exact sciences and technology
/ External geophysics
/ Fundamental and applied biological sciences. Psychology
/ Geochemistry
/ Marine
/ Mineralogy
/ Physical and chemical properties of sea water
/ Physics of the oceans
/ Sea water ecosystems
/ Silicates
/ Synecology
/ Water geochemistry
2011
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Sedimentary phosphorus dynamics and the evolution of bottom-water hypoxia
Journal Article
Sedimentary phosphorus dynamics and the evolution of bottom-water hypoxia
2011
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Overview
The present study examines oxygen and phosphorus dynamics at a seasonally hypoxic site in the Arkona basin of the Baltic Sea. A coupled benthic–pelagic reactive-transport model is used to describe the evolution of bottomwater solute concentrations, as well as pore-water and sediment profiles. Aerobic respiration dominates remineralization, with iron reduction, denitrification, and sulphate reduction playing secondary roles, while other pathways are negligible. Sediments represent a significant oxygen sink chiefly due to the aerobic degradation of organic matter, as well as nitrification and iron oxyhydroxide precipitation. Most phosphorus deposited in sediments is in organic matter, yet cycling is dominated by iron-bound phosphorus due to rapid dissimilatory iron reduction coupled with aerobic iron oxyhydroxide formation. Sustained hypoxia results in an initial decrease in sediment phosphorus content due to dissolution of phosphorus-bearing iron oxyhydroxides, resulting in a pulse of phosphate to overlying waters. Although an organic-rich layer is formed under low-oxygen conditions, enhanced remineralization of organic phosphorus relative to organic carbon tempers sedimentary phosphorus accumulation. Upon reoxygenation of bottom waters after a decade of sustained hypoxia, oxygen concentrations do not immediately achieve values observed prior to hypoxia because the organic-rich layer creates a higher benthic oxygen demand. Artificial reoxygenation of bottom waters leads to a substantial increase in the ironbound phosphorus pool; the total phosphorus content of the sediment, however, is unaffected. A relapse into hypoxia would consequently produce a large pulse of phosphate to the overlying waters potentially exacerbating the situation.
Publisher
John Wiley and Sons, Inc,American Society of Limnology and Oceanography
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