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Solid-phase phosphorus pools in highly organic carbonate sediments of northeastern Florida Bay
Article
Koch, MS, Benz, RE, Rudnick, DT. (2001). Solid-phase phosphorus pools in highly organic carbonate sediments of northeastern Florida Bay .
Estuarine, Coastal and Shelf Science,
52(2), 279-291. 10.1006/ecss.2000.0751
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Koch, MS, Benz, RE, Rudnick, DT. (2001). Solid-phase phosphorus pools in highly organic carbonate sediments of northeastern Florida Bay .
Estuarine, Coastal and Shelf Science,
52(2), 279-291. 10.1006/ecss.2000.0751
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cited authors
Koch, MS; Benz, RE; Rudnick, DT
abstract
Currently, few studies have investigated sediment phosphorus (P) pools or identified the chemical processes important in the P cycle of fine-grained carbonate sediments, particularly in coastal estuaries with high organic matter. To determine the role of fine-grain calcium carbonate and high organic matter on sedimentary P, we investigated the solid-phase P pools in seagrass sediments of north-eastern (NE) Florida Bay at the Bay-mangrove ecotone. Sediments were fractionated by sequential extractions into seven chemically-defined groups: exchangeable inorganic and organic P, reducible inorganic and organic P (Fe-bound), acid extractable inorganic and organic P (Ca-bound), and residual organic P. Calcium-bound P accounted for approximately 56% of total P and 96% of inorganic P. Our total calcium-bound P was in the range (34-151 μg P g
-1
) reported for coarse-grained low organic sediments, while the organic P associated with this fraction was slightly (∼10%) higher than those reported for other carbonate systems. The second dominant P fraction was residual organic P (30-71 μg P g
-1
) accounting for 42% of TP. This high residual pool suggests the importance of fringing mangrove and seagrass detritus in long-term P storage. In contrast to temperate estuaries, the iron-bound P fraction in NE Florida Bay sediments was low (<70 μg g
-1
) at the surface and undetectable (<1 μg g
-1
) below 10 cm. Based on our findings, we hypothesize that carbonate chemisorption reactions, along with potential reactive organic surfaces, and the sequestering of P into recalcitrant organic pools, maintain low exchangeable and porewater P concentrations across the NE Florida Bay estuary, and account for the reported autotrophic P-limitation. © 2001 Academic Press.
authors
Rudnick, David
publication date
January 1, 2001
published in
Estuarine, Coastal and Shelf Science
Journal
Identifiers
Digital Object Identifier (DOI)
https://doi.org/10.1006/ecss.2000.0751
Additional Document Info
start page
279
end page
291
volume
52
issue
2