Marine Polyphosphate: A Key Player in Geologic Phosphorus Sequestration
The in situ or authigenic formation of calcium phosphate minerals in marine sediments is a major sink for the vital nutrient phosphorus. However, because typical sediment chemistry is not kinetically conducive to the precipitation of these minerals, the mechanism behind their formation has remained a fundamental mystery. Here, we present evidence from high-sensitivity x-ray and electrodialysis techniques to describe a mechanism by which abundant diatom-derived polyphosphates play a critical role in the formation of calcium phosphate minerals in marine sediments. This mechanism can explain the puzzlingly dispersed distribution of calcium phosphate minerals observed in marine sediments worldwide.
- Research Organization:
- Brookhaven National Lab. (BNL), Upton, NY (United States). National Synchrotron Light Source
- Sponsoring Organization:
- Doe - Office Of Science
- DOE Contract Number:
- DE-AC02-98CH10886
- OSTI ID:
- 980324
- Report Number(s):
- BNL-93242-2010-JA; SCEHDK; TRN: US201015%%1709
- Journal Information:
- Science, Vol. 320; ISSN 0193-4511
- Country of Publication:
- United States
- Language:
- English
Similar Records
Marine polyphosphate : a key player in geologic phosphorus sequestration.
Characterization of minerals and organic phosphorus species in marine sediments using soft X-ray fluorescence spectromicroscopy.
Characterization of Minerals and Organic Phosphorus Species in Marine Sediments using Soft X-ray Fluorescence Spectromicroscopy
Journal Article
·
Thu May 01 00:00:00 EDT 2008
· Science
·
OSTI ID:980324
+4 more
Characterization of minerals and organic phosphorus species in marine sediments using soft X-ray fluorescence spectromicroscopy.
Journal Article
·
Mon Jan 01 00:00:00 EST 2007
· Mar. Chem.
·
OSTI ID:980324
Characterization of Minerals and Organic Phosphorus Species in Marine Sediments using Soft X-ray Fluorescence Spectromicroscopy
Journal Article
·
Mon Jan 01 00:00:00 EST 2007
· Marine Chemistry
·
OSTI ID:980324