Sequential extraction of sedimentary phosphorus in carbonate sediments of Florida Bay, USA

DOI

Phosphorus (P) limits seagrass and phytoplankton growth in much of Florida Bay. Dissolved phosphate concentrations in bay waters are as low as a few nanomolar (Zhang and Chi, 2002). Sedimentary phosphorus represents the largest phosphorus reservoir as carbonate sediments in the bay strongly retains phosphorus. In November 2000, surface sediments were collected from 40 stations in Florida Bay, USA. The total sedimentary P (TSP) was determined by single-step high temperature combustion of samples at 550°C. An improved sequential extraction technique was used in a subset of samples to fractionate TSP into five different pools: (1) exchangeable inorganic and organic P, (2) iron bound inorganic P, (3) biogenic calcium carbonate bound inorganic and organic P, (4) apatite and (5) refractory organic P. The dataset also include surface reactive iron by selective reduction and percent of calcium carbonate (CaCO₃) in Florida Bay sediments. This dataset provides the first detailed spatial distribution of TSP and its partitioning in five chemically distinguishable pools in the surface sediments of Florida Bay. A strong gradient of decreasing TSP concentration was observed from the west (14.6 µmol g⁻¹) to east (1.2 µmol g⁻¹) across the central bay. Among the five pools, the authigenic carbonate fluorapatite, biogenic apatite and CaCO₃ associated phosphorus account for the largest fraction (45%) of TSP, of which inorganic P is the dominant form, and organic P accounts for about 30% in regions of relatively high productivity and less than 10% in other areas of the bay. The second largest pools are the refractory organic P (24% of TSP) and Fe-bound inorganic P (19% of TSP). Readily exchangeable adsorbed P accounts for 8% of TSP, of which organic P is 60%. Detrital apatite phosphorus of igneous or metamorphic origin represents the smallest fraction, only 5% of TSP. Combining all five pools, organic P accounts for 38% of TSP.

Sea bed sediment samples were collected in an average sea bottom depth of ~1m with a maximum of 3m in Florida Bay.

Identifier
DOI https://doi.org/10.1594/PANGAEA.971485
Related Identifier References https://doi.org/10.1029/2004GB002255
Related Identifier References https://doi.org/10.1021/es011094v
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.971485
Provenance
Creator Zhang, Jia-Zhong ORCID logo
Publisher PANGAEA
Publication Year 2024
Funding Reference NOAA National Ocean Service https://doi.org/10.13039/100014522 Crossref Funder ID FY2000-FY2002 The Role of Sediments Resuspension in Phosphorus Cycle in Florida Bay South Florida Ecosystem Restoration Prediction and Modeling Program (SFERPM 2000)
Rights Creative Commons Attribution 4.0 International; https://creativecommons.org/licenses/by/4.0/
OpenAccess true
Representation
Resource Type Dataset
Format text/tab-separated-values
Size 520 data points
Discipline Earth System Research
Spatial Coverage (-81.096W, 24.876S, -80.497E, 25.184N)
Temporal Coverage Begin 2000-11-13T00:00:00Z
Temporal Coverage End 2000-11-15T00:00:00Z