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Constraining Sources of Organic Matter to Tropical Coastal Sediments: Consideration of Nontraditional End-members

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Abstract

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.

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References

  • Anderson WT, Fourqurean JW (2003) Intra- and interannual variability in seagrass carbon and nitrogen stable isotopes from south Florida, a preliminary study. Org Geochem 34(2):185–194

    Article  Google Scholar 

  • Arzayus KM, Canuel EA (2004) Organic matter degradation in sediments of the York River estuary: effects of biological vs. physical mixing. Geochim Cosmochim Acta 69(2):455–463

    Article  Google Scholar 

  • Aspila KI, Agemian H, Chau ASY (1976) A semi-automated method for the determination of inorganic, organic and total phosphate in sediments. Analyst 101:187–197

    Article  Google Scholar 

  • Atkinson MJ, Smith SV (1983) C: N: P ratios of benthic marine plants. Limnol Oceanogr 28:568–574

    Article  Google Scholar 

  • Bray JT, Bricker OP, Troup BN (1973) Phosphate in interstitial waters of anoxic sediments: oxidation effects during sampling procedure. Science 180(4093):1362–1364

    Article  Google Scholar 

  • Briggs RA, Padilla-Gamino JL, Bidigare RR, Gates RD, Ruttenberg KC (2013) Impact of coral spawning on the biogeochemsitry of a Hawaiian reef. Estuar Coast Shelf Sci 134(2013):57–68

    Article  Google Scholar 

  • Cloern JE, Canuel EA, Harris D (2002) Stable carbon and nitrogen isotope composition of aquatic and terrestrial plants of the San Francisco Bay estuarine system. Limnol Oceanogr 47(3):713–729

    Article  Google Scholar 

  • Cornelisen CD et al (2007) Patterns in the d13C and d15 N signature of Ulva pertusa: interaction between physical gradients and nutrient source pools. Limnol Oceanogr 52(2):820–832

    Article  Google Scholar 

  • Cotner JB, Makino W, Biddanda BA (2006) Temperature affects stoichiometry and biochemical composition of Escherichia coli. Microb Ecol 52:26–33. doi:10.1007/s00248-006-9049-1

    Article  Google Scholar 

  • Cowie GL, Hedges JI (1994) Biochemical indicators of diagenetic alteration in natural organic matter mixtures. Nature 369:304–307

    Article  Google Scholar 

  • Decottignies P, Beninger PG, Rince Y, Robins RJ, Riera P (2007) Exploitation of natural food sources by two sympatric, invasive suspension-feeders: Crassostrea gigas and Crepidula fornicata. Mar Ecol Prog Ser 334:179–192

    Article  Google Scholar 

  • Fourqurean JW, Zieman JC, Powell GVN (1992) Relationships between porewater nutrients and seagrasses in a subtropical carbonate environment. Mar Biol 114(1):57–65

    Google Scholar 

  • Freudenthal T, Wagner T, Wenzhöfer F, Zabel M, Wefer G (2001) Early diagenesis of organic matter from sediments of the eastern subtropical Atlantic: evidence from stable nitrogen and carbon isotopes. Geochim Cosmochim Acta 65(11):1795–1808

    Article  Google Scholar 

  • Fry B, Sherr EB (1984) d13C measurements as indicators of carbon flow in marine and freshwater ecosystems. Contrib Mar Sci 27:13–47

    Google Scholar 

  • Gächter R, Meyer JS (1993) The role of microorganisms in mobilization and fixation of phosphorus in sediments. Hydrobiol 253:103–121

    Google Scholar 

  • Gearing P, Plucker FE, Parker PL (1977) Organic carbon stable isotope ratios of continental sediments. Mar Chem 5:251–266

    Article  Google Scholar 

  • Glud RN, Eyre BD, Patten N (2008) Biogeochemical responses to mass coral spawning at the Great Barrier Reef: effects on respiration and primary production. Limnol Oceanogr 53(3):1014–1024

    Article  Google Scholar 

  • Goñi MA, Hedges JI (1995) Sources and reactivities of marine-derived organic matter in coastal sediments as determined by alkaline CuO oxidation. Geochim Cosmochim Acta 59(14):2965–2981

    Article  Google Scholar 

  • Goñi MA, Ruttenberg KC, Eglinton TI (1997) Sources and contributions of terrigenous organic carbon to surface sediments in the Gulf of Mexico. Nature 389:275–278

    Article  Google Scholar 

  • Goñi MA, Ruttenberg KC, Eglinton TI (1998) A reassessment of the sources and importance of land-derived organic matter in surface sediments from the Gulf of Mexico. Geochim Cosmochim Acta 62(18):3055–3075

    Article  Google Scholar 

  • Gordon ES, Goñi MA (2003) Sources and distribution of terrigenous organic matter delivered by the Atchafalaya River to sediments in the northern Gulf of Mexico. Geochimica Cosmochimica Acta 67:2359–2375

    Article  Google Scholar 

  • Gordon ES, Goñi MA (2004) Controls on the distribution and accumulation of terrigenous organic matter in sediments from the Mississippi and Atchafalaya river margin. Mar Chem 92:331–352

    Article  Google Scholar 

  • Graham MC, Eaves MA, Framer JG, Dobson J, Fallick AE (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, Scotland. Estuar Coast Shelf Sci 52:375–380

    Article  Google Scholar 

  • Grasshoff K, Ehrhardt M, Kremling K (eds) (1983) Methods of seawater analysis. Verlag Chemie, Weinheim, p 419

    Google Scholar 

  • Grottoli AG, Rodrigues LJ, Juarez C (2004) Lipids and stable carbon isotopes in two species of Hawaiian corals, Porites compressa and Montipora verrucosa, following a bleaching event. Mar Biol 145(3):621–631

    Article  Google Scholar 

  • Hedges JI, Keil RG (1995) Sedimentary organic matter preservation: an assessment and speculative synthesis. Mar Chem 49(2-3):81–115

    Google Scholar 

  • Hedges JI, Parker PL (1976) Land-derived organic matter in surface sediments from the Gulf of Mexico. Geochim Cosmochim Acta 40(9):1019–1029

    Article  Google Scholar 

  • Hedges JI, Clark WA, Quay PD, Richey JE, Devol AH, Santos UDM (1986) Compositions and fluxes of particulate organic material in the Amazon River. Limnol Oceanogr 31:717–738

    Article  Google Scholar 

  • Hedges JI, Keil RG, Benner R (1997) What happens to terrestrial organic matter in the ocean? Org Geochem 27(5/6):195–212

    Article  Google Scholar 

  • Hemminga MA, Mateo MA (1996) Stable carbon isotopes in seagrasses: variability in ratios and use in ecological studies. Mar Ecol Prog Ser 140:285–298

    Article  Google Scholar 

  • Hemminga MA et al (1994) Carbon outwelling from a mangrove forest with adjacent seagrass beds and coral reefs (Gazi Bay, Kenya). Mar Ecol Prog Ser 106:291–301

    Google Scholar 

  • Hillebrand H, Sommer U (1999) The nutrient stoichiometry of benthic microalgal growth: redfield proportions are optimal. Limnol Oceanogr 44(2):440–446

    Article  Google Scholar 

  • Hoegh-Guldberg O, Muscatine L, Goiran C, Siggaard D, Marion G (2004) Nutrient-induced perturbations to delta13C and delta15 N in symbiotic dinoflagellates and their coral hosts. Mar Ecol Prog Ser 280:105–114

    Article  Google Scholar 

  • Kraal P, Slomp CP, Forster A, Kuypers MMM, Sluijs A (2009) Pyrite oxidation during sample storage determines phosphorus fractionation in carbonate-poor anoxic sediments. Geochim Cosmochim Acta 73:3277–3290

    Article  Google Scholar 

  • Lapointe B, Littler M, Littler D (1992) Nutrient availability to marine macroalgae in siliciclastic versus carbonate-rich coastal waters. Estuaries Coasts 15(1):75–82

    Article  Google Scholar 

  • Larned ST (1998) Nitrogen- versus phosphorus-limited growth and sources of nutrients for coral reef macroalgae. Mar Biol 132(3):409–421

    Article  Google Scholar 

  • Lee M, Bae W, Chung J, Jung H-S, Shim H (2008) Seasonal and spatial characteristics of seawater and sediment at Youngil bay, Southeast Coast of Korea. Mar Pollut Bull 57(6–12):325–334

    Article  Google Scholar 

  • Lehmann MF, Bernasconi SM, Barbieri A, McKenzie JA (2002) Preservation of organic matter and alteration of its carbon and nitrogen isotope composition during simulated and in situ early sedimentary diagenesis. Geochim Cosmochim Acta 66(20):3573–3584

    Article  Google Scholar 

  • Likens GE, Bormann FH, Johnson NM (1981) Interaction between major biogeochemical cycles in terrestrial ecosystems. In: Likens GE (ed) Some perspectives of the major biogeochemical cycles-SCOPE 17. Wiley, New York, pp 93–112

    Google Scholar 

  • Loneragan NR, Bunn SE, Kellaway DM (1997) Are mangroves and seagrasses sources of organic carbon for penaeid prawns in a tropical Australian estuary? A multiple stable-isotope study. Mar Biol 130(2):289–300

    Article  Google Scholar 

  • Luria SE (1960) The bacterial protoplasm: composition and organization. In: Gunsalus IC, Stanler RY (ed) The Bacteria, vol 1. Academic Press, New York, Chap 1

  • McGroddy ME, Daufresne T, Hedin LO (2004) Scaling of C: N: P stoichiometry in forests worldwide: implications of terrestrial Redfield-type ratios. Ecology 85(9):289–302

    Article  Google Scholar 

  • Meyers PA (1994) Preservation of elemental and isotopic source identification of sedimentary organic matter. Chem Geol 114:289–302

    Article  Google Scholar 

  • Meyers PA (1997) Organic geochemical proxies of paleoceanographic, paleolimnologic, and paleoclimatic processes. Org Geochem 27(5–6):213–250

    Article  Google Scholar 

  • Meyers PA, Ishiwatari R (1993) Lacustrine organic geochemistry—an overview of indicators of organic matter sources and diagenesis in lake sediments. Org Geochem 20(7):867–900

    Article  Google Scholar 

  • Middelburg JJ, Nieuwenhuize J (1998) Carbon and nitrogen stable isotopes in suspended matter and sediments from the Schelde Estuary. Mar Chem 60(3–4):217–225

    Article  Google Scholar 

  • Muller-Parker G, Cook CB, D’Elia CF (1994) Elemental composition of coral Pocillopora damicornis exposed to elevated seawater ammonium. Pac Sci 48(3):234–246

    Google Scholar 

  • Muscatine L et al (2004) Stable isotopes (d13C and d15 N) of organic matrix from coral skeleton. Proc Natl Acad Sci 102(5):1525–1530

    Article  Google Scholar 

  • Ogrinc N, Fontolan G, Faganeli J, Covelli S (2005) Carbon and nitrogen isotope compositions of organic matter in coastal marine sediments (the Gulf of Trieste, N Adriatic Sea): indicators of sources and preservation. Mar Chem 95(3–4):163–181

    Article  Google Scholar 

  • Perdue EM, Koprivnjak J-F (2007) Using the C/N ratio to estimate terrigenous inputs of organic matter to aquatic environments. Estuar Coast Shelf Sci 73:65–72

    Article  Google Scholar 

  • Peterson BJ, Howarth RW (1987) Sulfur, carbon, and nitrogen isotopes used to trace organic matter flow in the salt-marsh estuaries of Sapelo Island, Georgia. Limnol Oceanogr 32(6):1195–1213

    Article  Google Scholar 

  • Ramaswamy V, Gaye B, Shirodkar PV, Chivas AR, Wheeler D, Thwin S (2008) Distribution and sources of organic carbon, nitrogen and their isotopic signatures in sediments from the Ayeyarwady (Irrawaddy) continental shelf, northern Andaman Sea. Mar Chem 111(3e4):137e150

    Google Scholar 

  • Redfield AC, Ketchum BH, Richards FA (1963) The influence of organisms on the composition of sea-water. In: Hill MN (ed) The sea. Interscience, New York, pp 26–77

    Google Scholar 

  • Rice DL, Hanson RB (1984) A kinetic model for detritus nitrogen: the role of the associated microflora in nitrogen accumulation. Bull Mar Sci 35(3):326–340

    Google Scholar 

  • Rice DL, Tenore KR (1981) Dynamic of carbon and nitrogen during the decomposition of detritus derived from estuarine macrophytes. Estuar Coast Shelf Sci 13:153–162

    Article  Google Scholar 

  • Ruttenberg KC, Goñi MA (1997a) 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. Proc ODP Sci Results 155:505–517

    Google Scholar 

  • Ruttenberg KC, Goñi MA (1997b) Phosphorus distribution, C: N: P ratios, and δ13Coc in arctic, temperate, and tropical coastal sediments: tools for characterizing bulk sedimentary organic matter. Mar Geol 139(1–4):123–145

    Article  Google Scholar 

  • Thornton SF, McManus J (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, Scotland. Estuar Coast Shelf Sci 38:219–233

    Article  Google Scholar 

  • Volkman JK (1986) A review of sterol markers for marine and terrigenous organic matter. Org Geochem 9(2):83–99

    Article  Google Scholar 

  • Wild C et al (2004a) Coral mucus functions as an energy carrier and particle trap in the reef ecosystem. Nature 428(6978):66–70

    Article  Google Scholar 

  • Wild C, Tollrian R, Huettel M (2004b) Rapid recycling of coral mass-spawning products in permeable reef sediments. Marine Ecol Progress Series 271:159–166

    Article  Google Scholar 

  • Wild C, Woyt H, Huettel M (2005) Influence of coral mucus on nutrient fluxes in carbonate sands. Mar Ecol Prog Ser 287:87–98

    Article  Google Scholar 

  • Wild C, Haas A, Naumann M, Mayr C, el-Zibday M (2008a) Comparative investigation of organic matter release by corals and benthic reef algae-implications for pelagic and benthic microbial metabolism. In: Proceedings of the 11th International Coral Reef Symposium, Ft. Lauderdale, FL

  • Wild C, Jantzen C, Struck U, Hoegh-Guldberg O, Huettel M (2008b) Biogeochemical responses following coral mass spawning on the Great Barrier Reef: pelagic-benthic coupling. Coral Reefs 27(1):123–132

    Article  Google Scholar 

  • Wu Y, Zhang J, Li DJ, Wei H, Lu RX (2003) Isotope variability of particulate organic matter at the PN section in the East China Sea. Biogeochemistry 65:31–49

    Google Scholar 

  • Yamamuro M, Kayanne H, Minagawa M (1995) Carbon and nitrogen stable isotopes of primary producers in coral reef ecosystems. Limnol Oceanogr 40(3):617–621

    Article  Google Scholar 

  • Yu F, Yongqiang Z, Lloyd JM, Huang G, Leng MJ, Kendrick C, Lamb AL, Yim WW-S (2010) Bulk organic d13C and C/N as indicators for sediment sources in the Pearl River delta and estuary, southern China. Estuar Coast Shelf Sci 87:618–630

    Article  Google Scholar 

  • Zhang H, Wu H, Yu Q, Wang Z, Wei C, Long M, Kattge J, Smith M, Han X (2013) Sampling date, leaf age and root size: implications for the study of plant C: N: P stoichiometry. PLoS One 8(4):e60360

    Article  Google Scholar 

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Acknowledgments

We are grateful to In Chieh Chen who assisted with field preparations, sample collection, and laboratory analyses. We thank Craig Glenn for access to his coulometer. This paper is funded in part by a grant/cooperative agreement from the National Oceanic and Atmospheric Administration, Project No. R/SS-2, which is sponsored by the University of Hawaii Sea Grant College Program, School of Ocean and Earth Science and Technology, under Institutional Grant No. NA09OAR4170060 Office of Sea Grant, Department of Commerce. RAB was partially sponsored by NSF-OCE550851. The views expressed herein are those of the author(s) and do not necessarily reflect the views of NOAA or any of its subagencies. UNIHI-SEAGRANT-JC-13-10. This is SOEST contribution #9039.

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Correspondence to R. A. Briggs.

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Briggs, R.A., Ruttenberg, K.C., Glazer, B.T. et al. Constraining Sources of Organic Matter to Tropical Coastal Sediments: Consideration of Nontraditional End-members. Aquat Geochem 19, 543–563 (2013). https://doi.org/10.1007/s10498-013-9219-2

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