Access the full text.
Sign up today, get DeepDyve free for 14 days.
J. Hedges, J. Baldock, Y. Gélinas, Cindy Lee, M. Peterson, S. Wakeham (2002)
The biochemical and elemental compositions of marine plankton: A NMR perspectiveMarine Chemistry, 78
Stephen Smith, W. Kimmerer, T. Walsh (1986)
Vertical flux and biogeochemical turnover regulate nutrient limitation of net organic production in the North Pacific GyreLimnology and Oceanography, 31
J. Koprivnjak, P. Pfromm, E. Ingall, T. Vetter, P. Schmitt‐Kopplin, N. Hertkorn, M. Frommberger, H. Knicker, E. Perdue (2009)
Chemical and spectroscopic characterization of marine dissolved organic matter isolated using coupled reverse osmosis-electrodialysis.Geochimica et Cosmochimica Acta, 73
Lisa Moore, M. Ostrowski, D. Scanlan, K. Feren, T. Sweetsir (2005)
Ecotypic variation in phosphorus-acquisition mechanisms within marine picocyanobacteriaAquatic Microbial Ecology, 39
A. Cook, C. Daughton, M. Alexander (1978)
Phosphonate utilization by bacteriaJournal of Bacteriology, 133
J. Koprivnjak, E. Perdue, P. Pfromm (2006)
Coupling reverse osmosis with electrodialysis to isolate natural organic matter from fresh waters.Water research, 40 18
L. Kolowith, E. Ingall, R. Benner (2001)
Composition and cycling of marine organic phosphorusLimnology and Oceanography, 46
L. Clark, E. Ingall, R. Benner (1998)
Marine phosphorus is selectively remineralizedNature, 393
S. Dyhrman, P. Chappell, S. Haley, James Moffett, E. Orchard, J. Waterbury, E. Webb (2006)
Phosphonate utilization by the globally important marine diazotroph TrichodesmiumNature, 439
G. Jackson, P. Williams (1985)
Importance of dissolved organic nitrogen and phosphorus to biological nutrient cycling, 32
E. Ingall (2008)
Oceanography: Making methaneNature Geoscience, 1
D. Karl, L. Beversdorf, K. Björkman, M. Church, Asunción Martínez, E. Delong (2008)
Aerobic production of methane in the seaNature Geoscience, 1
J. Diaz, E. Ingall, C. Benitez‐Nelson, D. Paterson, M. Jonge, I. McNulty, J. Brandes (2008)
Marine Polyphosphate: A Key Player in Geologic Phosphorus SequestrationScience, 320
E. Romankevich (1984)
Geochemistry of organic matter in the ocean
K. Kennedy, G. Thompson (1970)
Phosphonolipids: Localization in Surface Membranes of TetrahymenaScience, 168
Andrew Biersmith, R. Benner (1998)
Carbohydrates in phytoplankton and freshly produced dissolved organic matterMarine Chemistry, 63
J. Pakulski, R. Benner (1994)
Abundance and distribution of carbohydrates in the oceanLimnology and Oceanography, 39
C. Daughton, A. Cook, M. Alexander (1979)
Bacterial conversion of alkylphosphonates to natural products via carbon-phosphorus bond cleavageJournal of Agricultural and Food Chemistry, 27
K. Bjorkman, D. Karl (1994)
Bioavailability of inorganic and organic phosphorus compounds to natural assemblages of microorganisms m Hawaiian coastal watersMarine Ecology Progress Series, 111
S. Rittenberg, R. Hespell (1975)
Energy efficiency of intraperiplasmic growth of Bdellovibrio bacteriovorusJournal of Bacteriology, 121
DM Karl, K Bjorkman (2002)
Biochemistry of marine dissolved organic matter
S. Wakeham, Cindy Lee, J. Hedges, P. Hernes, Michael Peterson (1997)
Molecular indicators of diagenetic status in marine organic matterGeochimica et Cosmochimica Acta, 61
B. Gurtler, T. Vetter, E. Perdue, E. Ingall, J. Koprivnjak, P. Pfromm (2008)
Combining reverse osmosis and pulsed electrical current electrodialysis for improved recovery of dissolved organic matter from seawaterJournal of Membrane Science, 323
D. Karl, K. Björkman (2001)
Phosphorus cycle in seawater: Dissolved and particulate pool inventories and selected phosphorus fluxesMethods in Microbiology, 30
Poulomi Sannigrahi, E. Ingall, R. Benner (2005)
Cycling of dissolved and particulate organic matter at station Aloha: Insights from 13C NMR spectroscopy coupled with elemental, isotopic and molecular analyses, 52
K. Orrett, D. Karl (1987)
Dissolved organic phosphorus production in surface seawaters1Limnology and Oceanography, 32
M. Pasek (2008)
Rethinking early Earth phosphorus geochemistryProceedings of the National Academy of Sciences, 105
T. Vetter, E. Perdue, E. Ingall, J. Koprivnjak, P. Pfromm (2007)
Combining reverse osmosis and electrodialysis for more complete recovery of dissolved organic matter from seawaterSeparation and Purification Technology, 56
Poulomi Sannigrahi, E. Ingall (2005)
Polyphosphates as a source of enhanced P fluxes in marine sediments overlain by anoxic waters: Evidence from 31P NMRGeochemical Transactions, 6
(1973)
Phosphonolipids, In: Ansell GB, Hawthorne JN, Dawson RMC (ed.), Form and function of phosphonolipids
M. Weiss, U. Abele, J. Weckesser, W. Welte, E. Schiltz, G. Schulz (1991)
Molecular architecture and electrostatic properties of a bacterial porin.Science, 254 5038
Poulomi Sannigrahi, E. Ingall, R. Benner (2006)
Nature and dynamics of phosphorus-containing components of marine dissolved and particulate organic matterGeochimica et Cosmochimica Acta, 70
H Rosenburg (1973)
Form and function of phosphonolipids
K. Björkman, D. Karl (2005)
Presence of dissolved nucleotides in the North Pacific Subtropical Gyre and their role in cycling of dissolved organic phosphorusAquatic Microbial Ecology, 39
A. Paytan, B. Cade‐Menun, K. McLaughlin, K. Faul (2003)
Selective phosphorus regeneration of sinking marine particles: evidence from 31P-NMRMarine Chemistry, 82
J. Yan, N. Packer, A. Gooley, K. Williams (1998)
Protein phosphorylation: technologies for the identification of phosphoamino acids.Journal of chromatography. A, 808 1-2
S. Myklestad (1995)
Release of extracellular products by phytoplankton with special emphasis on polysaccharidesScience of The Total Environment, 165
H. Hassan, D. Pratt (1977)
Biochemical and physiological properties of alkaline phosphatases in five isolates of marine bacteriaJournal of Bacteriology, 129
D. Karl, K. Björkman (2002)
Chapter 6 – Dynamics of DOP
A. Skoog, R. Benner (1997)
Aldoses in various size fractions of marine organic matter: Implications for carbon cyclingLimnology and Oceanography, 42
D. Karl, K. Yanagi (1997)
Partial characterization of the dissolved organic phosphorus pool in the oligotrophic North Pacific OceanLimnology and Oceanography, 42
L. Clark, E. Ingall, R. Benner (1999)
MARINE ORGANIC PHOSPHORUS CYCLING: NOVEL INSIGHTS FROM NUCLEAR MAGNETIC RESONANCEAmerican Journal of Science, 299
C. Benitez‐Nelson (2000)
The biogeochemical cycling of phosphorus in marine systemsEarth-Science Reviews, 51
C. Benitez‐Nelson, K. Buesseler (1999)
Variability of inorganic and organic phosphorus turnover rates in the coastal oceanNature, 398
Ralph Smith, W. Harrison, L. Harris (1985)
Phosphorus exchange in marine microplankton communities near HawaiiMarine Biology, 86
The dominant phosphorus compound classes were characterized in marine samples using a new, high recovery method for isolating and concentrating bulk dissolved organic matter (DOM) called combined electrodialysis + reverse osmosis (ED/RO). In contrast to earlier studies that use ultrafiltration (UF) to recover only the high molecular weight DOM, ED/RO is capable of isolating both low molecular weight (LMW) and high molecular weight (HMW) DOM. Samples were collected from a broad range of marine environments: along a transect incorporating coastal and offshore waters off the Southeastern United States, in Effingham Inlet, a Pacific fjord located on Vancouver Island, British Columbia and in the Amundsen Sea, Antarctica. Results from phosphorus nuclear magnetic resonance (31P NMR) analysis reveal a similar abundance of P compound classes among samples, phosphate esters (80–85%), phosphonates (5–10%) and polyphosphates (8–13%). These samples contain significantly higher proportions of polyphosphate P and P esters and lower proportions of phosphonates than measured in previous studies using the UF method. The much higher levels of polyphosphate detected in our samples suggests that polyphosphate is present mainly in the LMW dissolved matter fraction. Polyphosphates in dissolved matter may be present as (or derived from) dissolved nucleotides or organismal polyphosphate bodies, or both. Low molecular weight P esters are possibly composed of phosphoamino acids and small carbohydrates, like simple sugar phosphates and/or dissolved nucleotides. Phosphonates in DOM are more prevalent as HMW phosphonate compounds, which suggests that LMW phosphonates are more readily utilized in marine ecosystems. Overall, the investigation of DOM across a size spectrum that includes both the HMW and the LMW fractions reveals a new picture of phosphorus distribution, cycling and bioavailability.
Aquatic Geochemistry – Springer Journals
Published: Jan 7, 2010
Read and print from thousands of top scholarly journals.
Already have an account? Log in
Bookmark this article. You can see your Bookmarks on your DeepDyve Library.
To save an article, log in first, or sign up for a DeepDyve account if you don’t already have one.
Copy and paste the desired citation format or use the link below to download a file formatted for EndNote
Access the full text.
Sign up today, get DeepDyve free for 14 days.
All DeepDyve websites use cookies to improve your online experience. They were placed on your computer when you launched this website. You can change your cookie settings through your browser.