Access the full text.
Sign up today, get DeepDyve free for 14 days.
(1984)
A kinetic model for detritus nitrogen: the role of the associated microflora in nitrogen accumulation
J. Hedges, P. Parker (1976)
Land-derived organic matter in surface sediments from the Gulf of MexicoGeochimica et Cosmochimica Acta, 40
M. McGroddy, T. Daufresne, L. Hedin (2004)
SCALING OF C:N:P STOICHIOMETRY IN FORESTS WORLDWIDE: IMPLICATIONS OF TERRESTRIAL REDFIELD‐TYPE RATIOSEcology, 85
B. Lapointe, M. Littler, D. Littler (1992)
Nutrient availability to marine macroalgae in siliciclastic versus carbonate-rich coastal watersEstuaries, 15
M. Atkinson, S. Smith (1983)
C:N:P ratios of benthic marine plants [carbon:nitrogen:phosphorus].Limnology and Oceanography
R. Briggs, J. Padilla‐Gamiño, R. Bidigare, R. Gates, K. Ruttenberg (2013)
Impact of coral spawning on the biogeochemistry of a Hawaiian reefEstuarine Coastal and Shelf Science, 134
W. Anderson, J. Fourqurean (2003)
Intra- and interannual variability in seagrass carbon and nitrogen stable isotopes from south Florida, a preliminary studyOrganic Geochemistry, 34
K. Ruttenberg, M. Goñi (1997)
31. DEPTH TRENDS IN PHOSPHORUS DISTRIBUTION AND C:N:P RATIOS OF ORGANIC MATTER IN AMAZON FAN SEDIMENTS: INDICES OF ORGANIC MATTER SOURCE AND BURIAL HISTORY 1, 155
JI Hedges, RG Keil, R Benner (1997)
What happens to terrestrial organic matter in the ocean?Org Geochem, 27
Mikyung Lee, W. Bae, J. Chung, H. Jung, H. Shim (2008)
Seasonal and spatial characteristics of seawater and sediment at Youngil Bay, southeast coast of Korea.Marine pollution bulletin, 57 6-12
P. Meyers (1994)
Preservation of elemental and isotopic source identification of sedimentary organic matterChemical Geology, 114
C. Wild, R. Tollrian, M. Huettel (2004)
Rapid recycling of coral mass-spawning products in permeable reef sedimentsMarine Ecology Progress Series, 271
M. Lehmann, S. Bernasconi, A. Barbieri, J. Mckenzie (2002)
Preservation of organic matter and alteration of its carbon and nitrogen isotope composition during simulated and in situ early sedimentary diagenesisGeochimica et Cosmochimica Acta, 66
J. Bray, O. Bricker, B. Troup (1973)
Phosphate in Interstitial Waters of Anoxic Sediments: Oxidation Effects during Sampling ProcedureScience, 180
Haiyang Zhang, Honghui Wu, Qiang Yu, Zhengwen Wang, Cunzheng Wei, Min Long, J. Kattge, Melinda Smith, Xingguo Han (2013)
Sampling Date, Leaf Age and Root Size: Implications for the Study of Plant C:N:P StoichiometryPLoS ONE, 8
J. Cotner, W. Makino, B. Biddanda (2006)
Temperature Affects Stoichiometry and Biochemical Composition of Escherichia coliMicrobial Ecology, 52
T. Freudenthal, T. Wagner, F. Wenzhöfer, M. Zabel, G. Wefer (2001)
Early diagenesis of organic matter from sediments of the eastern subtropical Atlantic: evidence from stable nitrogen and carbon isotopesGeochimica et Cosmochimica Acta, 65
M. Hemminga, F. Slim, J. Kazungu, Gerald Ganssen, J. Nieuwenhuize, N. Kruyt (1994)
Carbon outwelling from a mangrove forest with adjacent seagrass beds and coral reefs (Gazi Bay, Kenya)Marine Ecology Progress Series, 106
G. Muller-parker, C. Cook, C. D’Elia (1994)
Elemental Composition of the Coral Pocillopora damicornis Exposed to Elevated Seawater Ammonium
A. Redfield, B. Ketchum, F. Richards (1963)
The influence of organisms on the composition of sea-water, 2
C. Wild, A. Haas, M. Naumann, C. Mayr, M. el-Zibdah (2009)
Comparative investigation of organic matter release by corals and benthic reef algae – implications for pelagic and benthic microbial metabolism
M. Frissel (1982)
Some perspectives of the major biogeochemical cycles, scope 17: Gene E. Likens (Editor), John Wiley, Chichester, 1981, xiii + 175 pp., £11.00, ISBN 0-471-27989-7Agro-ecosystems, 8
Priscilla Decottignies, P. Beninger, Y. Rincé, R. Robins, P. Riera (2007)
Exploitation of natural food sources by two sympatric, invasive suspension-feeders: Crassostrea gigas and Crepidula fornicataMarine Ecology Progress Series, 334
C. Wild, Holger Woyt, M. Huettel (2005)
Influence of coral mucus on nutrient fluxes in carbonate sandsMarine Ecology Progress Series, 287
S. Larned (1998)
Nitrogen- versus phosphorus-limited growth and sources of nutrients for coral reef macroalgaeMarine Biology, 132
D. Rice, K. Tenore (1981)
Dynamics of carbon and nitrogen during the decomposition of detritus derived from estuarine macrophytesEstuarine Coastal and Shelf Science, 13
L. Muscatine, C. Goiran, L. Land, J. Jaubert, J. Cuif, D. Allemand (2005)
Stable isotopes (δ13C and δ15N) of organic matrix from coral skeletonProceedings of the National Academy of Sciences of the United States of America, 102
AC Redfield, BH Ketchum, FA Richards (1963)
The sea
Elizabeth Gordon, M. Goñi (2003)
Sources and distribution of terrigenous organic matter delivered by the Atchafalaya River to sediments in the northern Gulf of MexicoGeochimica et Cosmochimica Acta, 67
P. Kraal, C. Slomp, A. Forster, M. Kuypers, A. Sluijs (2009)
Pyrite oxidation during sample storage determines phosphorus fractionation in carbonate-poor anoxic sedimentsGeochimica et Cosmochimica Acta, 73
M. Graham, M. Eaves, J. Farmer, J. Dobson, A. Fallick (2001)
A Study of Carbon and Nitrogen Stable Isotope and Elemental Ratios as Potential Indicators of Source and Fate of Organic Matter in Sediments of the Forth Estuary, ScotlandEstuarine Coastal and Shelf Science, 52
K. Ruttenberg, M. Goñi (1997)
Phosphorus distribution, C:N:P ratios, and δ13Coc in arctic, temperate, and tropical coastal sediments: tools for characterizing bulk sedimentary organic matterMarine Geology, 139
P Gearing, FE Plucker, PL Parker (1977)
Organic carbon stable isotope ratios of continental sedimentsMar Chem, 5
J. Cloern, E. Canuel, D. Harris (2002)
Stable carbon and nitrogen isotope composition of aquatic and terrestrial plants of the San Francisco Bay estuarine systemLimnology and Oceanography, 47
V. Ramaswamy, B. Gaye, P. Shirodkar, P. Rao, A. Chivas, D. Wheeler, Swe Thwin (2008)
Distribution and sources of organic carbon, nitrogen and their isotopic signatures in sediments from the Ayeyarwady (Irrawaddy) continental shelf, northern Andaman SeaMarine Chemistry, 111
A. Grottoli, L. Rodrigues, C. Juárez (2004)
Lipids and stable carbon isotopes in two species of Hawaiian corals, Porites compressa and Montipora verrucosa, following a bleaching eventMarine Biology, 145
K. Grasshoff, K. Kremling, M. Ehrhardt (1999)
Methods of seawater analysis
N. Ogrinc, G. Fontolan, J. Faganeli, S. Covelli (2005)
Carbon and nitrogen isotope compositions of organic matter in coastal marine sediments (the Gulf of Trieste, N Adriatic Sea): indicators of sources and preservationMarine Chemistry, 95
F. Yu, Y. Zong, J. Lloyd, Guangqing Huang, M. Leng, C. Kendrick, A. Lamb, W. Yim (2010)
Bulk organic δ13C and C/N as indicators for sediment sources in the Pearl River delta and estuary, southern ChinaEstuarine Coastal and Shelf Science, 87
Plim Nlim, Nlim V, Plim. (1999)
The nutrient stoichiometry of benthic microalgal growth : Redfield proportions are optimal
(1981)
Interaction between major biogeochemical cycles
N. Loneragan, S. Bunn, D. Kellaway (1997)
Are mangroves and seagrasses sources of organic carbon for penaeid prawns in a tropical Australian estuary? A multiple stable-isotope studyMarine Biology, 130
R. Benner (2004)
What happens to terrestrial organic matter in the oceanMarine Chemistry, 92
O. Hoegh‐Guldberg, L. Muscatine, C. Goiran, Dorthe Siggaard, G. Marion (2004)
Nutrient-induced perturbations to δ13C and δ15N in symbiotic dinoflagellates and their coral hostsMarine Ecology Progress Series, 280
’. MIGUELA.GoFa (2001)
Sources and reactivities of marine-derived organic matter in coastal sediments as determined by alkaline CuO oxidation
M. Hemminga, M. Mateo (1996)
Stable carbon isotopes in seagrasses: variability in ratios and use in ecological studiesMarine Ecology Progress Series, 140
J. Hedges, R. Keil (1995)
Sedimentary organic matter preservation: an assessment and speculative synthesisMarine Chemistry, 49
O Hoegh-Guldberg, L Muscatine, C Goiran, D Siggaard, G Marion (2004)
Nutrient-induced perturbations to delta13C and delta15 N in symbiotic dinoflagellates and their coral hostsMar Ecol Prog Ser, 280
M. Goñi, K. Ruttenberg, T. Eglinton (1998)
A REASSESSMENT OF THE SOURCES AND IMPORTANCE OF LAND-DERIVED ORGANIC MATTER IN SURFACE SEDIMENTS FROM THE GULF OF MEXICOGeochimica et Cosmochimica Acta, 62
C. Wild, C. Jantzen, U. Struck, O. Hoegh‐Guldberg, M. Huettel (2008)
Biogeochemical responses following coral mass spawning on the Great Barrier Reef: pelagic–benthic couplingCoral Reefs, 27
J. Hedges, W. Clark, P. Quay, J. Richey, A. Devol, M. Santos (1986)
Compositions and fluxes of particulate organic material in the Amazon River1Limnology and Oceanography, 31
M. Goñi, K. Ruttenberg, T. Eglinton (1997)
Sources and contribution of terrigenous organic carbon to surface sediments in the Gulf of MexicoNature, 389
M. Yamamuro, H. Kayanne, Masao Minagawao (1995)
Carbon and nitrogen stable isotopes of primary producers in coral reef ecosystemsLimnology and Oceanography, 40
P. Meyers, R. Ishiwatari (1993)
Lacustrine organic geochemistry—an overview of indicators of organic matter sources and diagenesis in lake sedimentsOrganic Geochemistry, 20
S. Thornton, J. McManus (1994)
Application of Organic Carbon and Nitrogen Stable Isotope and C/N Ratios as Source Indicators of Organic Matter Provenance in Estuarine Systems: Evidence from the Tay Estuary, ScotlandEstuarine Coastal and Shelf Science, 38
M. Atkinson, S. Smith (1983)
C:N:P ratios of benthic marine plants1Limnology and Oceanography, 28
Elizabeth Gordon, M. Goñi (2004)
Controls on the distribution and accumulation of terrigenous organic matter in sediments from the Mississippi and Atchafalaya river marginMarine Chemistry, 92
P. Meyers (1997)
Organic geochemical proxies of paleoceanographic, paleolimnologic, and paleoclimatic processesOrganic Geochemistry, 27
GE Likens, FH Bormann, NM Johnson (1981)
Some perspectives of the major biogeochemical cycles-SCOPE 17
H. Hillebrand, U. Sommer (1999)
The nutrient stoichiometry of benthic microalgal growth: Redfield proportions are optimalLimnology and Oceanography, 44
J. Middelburg, J. Nieuwenhuize (1998)
Carbon and nitrogen stable isotopes in suspended matter and sediments from the Schelde EstuaryMarine Chemistry, 60
J. Fourqurean, J. Zieman, G. Powell (1992)
Relationships between porewater nutrients and seagrasses in a subtropical carbonate environmentMarine Biology, 114
(2008)
salt-marsh estuaries of Sapelo Island, Georgia
K. Arzayus, E. Canuel (2005)
Organic matter degradation in sediments of the York River estuary: Effects of biological vs. physical mixingGeochimica et Cosmochimica Acta, 69
R. Gächter, J. Meyer (1993)
The role of microorganisms in mobilization and fixation of phosphorus in sedimentsHydrobiologia, 253
P. Gearing, F. Plucker, P. Parker (1977)
Organic carbon stable isotope ratios of continental margin sedimentsMarine Chemistry, 5
J. Volkman (1986)
A review of sterol markers for marine and terrigenous organic matterOrganic Geochemistry, 9
R. Glud, B. Eyre, N. Patten (2008)
Biogeochemical responses to mass coral spawning at the Great Barrier Reef: Effects on respiration and primary productionLimnology and Oceanography, 53
Yelin Wu, Jing Zhang, Daoji Li, H. Wei, R. Lu (2003)
Isotope variability of particulate organic matter at the PN section in the East China SeaBiogeochemistry, 65
Christopher Cornelisen, S. Wing, K. Clark, M. Bowman, Russell Frew, C. Hurd (2007)
Patterns in the δ13C and δ15N signature of Ulva pertusa: Interaction between physical gradients and nutrient source poolsLimnology and Oceanography, 52
E. Perdue, J. Koprivnjak (2007)
Using the C/N ratio to estimate terrigenous inputs of organic matter to aquatic environmentsEstuarine Coastal and Shelf Science, 73
B. Peterson, R. Howarth (1987)
Sulfur, carbon, and nitrogen isotopes used to trace organic matter flow in the salt‐marsh estuaries of Sapelo Island, Georgia1Limnology and Oceanography, 32
G. Cowie, J. Hedges (1994)
Biochemical indicators of diagenetic alteration in natural organic matter mixturesNature, 369
C. Wild, M. Huettel, A. Klueter, Stephan Kremb, M. Rasheed, B. Jørgensen (2004)
Coral mucus functions as an energy carrier and particle trap in the reef ecosystemNature, 428
K. Ruttenberg, M. Goñi (1997)
DEPTH TRENDS IN PHOSPHORUS DISTRIBUTION AND C : N : P RATIOS OF ORGANIC MATTER IN AMAZON FAN SEDIMENTS : INDICES OF ORGANIC MATTER SOURCE AND BURIAL HISTORY
B. Fry, E. Sherr (1989)
δ13C Measurements as Indicators of Carbon Flow in Marine and Freshwater Ecosystems
W. Andersona, J. Fourqureana (2003)
Intra-and interannual variability in seagrass carbon and nitrogen stable isotopes from south Florida , a preliminary study
K. Aspila, H. Agemian, A. Chau (1976)
A semi-automated method for the determination of inorganic, organic and total phosphate in sediments.The Analyst, 101 1200
Molar organic carbon to total nitrogen to organic phosphorus (OC:TN:OP) ratios are used in tandem with carbon isotopic values to constrain sources of organic matter (OM) to marine sediments in a tropical coastal embayment. Analysis of end-members specific to the study site indicates that the bulk OM pool cannot be modeled as a simple mixture of two end-members (terrestrial vs. marine OM), but rather reflects a more complex, multicomponent mixture. Mangrove, coral reef ecosystems, and bacterial biomass contribute OM to tropical coastal marine sediments that is compositionally distinct from traditional marine and terrestrial end-members and thus preclude the application of a classical two end-member mixing model of the sort that has been used traditionally in sediments from temperate environments. A survey of elemental ratios and carbon isotopic values of potential OM end-members reported in the literature, as well as depth profiles before and after whole-core incubation experiments conducted as part of this study, were used to evaluate the strength of OC:TN versus OC:OP ratios as OM source indices. Our study suggests that OC:TN ratios are a weaker indicator of OM source than OC:OP ratios, because: (1) the more restricted dynamic range of OC:TN ratios prevents clear distinction of terrestrial-from marine-derived OM, and (2) post-depositional changes in OC:TN ratios occur during diagenesis, obscuring the source signature of initially deposited OM. The fidelity of OM indices during early diagenesis underscores the importance of quantifying OP in sediments to assess sedimentary OM source.
Aquatic Geochemistry – Springer Journals
Published: Feb 1, 2014
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.