TAO Jing, MA Weiwei, ZHU Maoxu, LI Tie, YANG Rujun. Characterization of iron diagenesis in marine sediments using refined iron speciation and quantized iron(Ⅲ)-oxide reactivity: a case study in the Jiaozhou Bay, China[J]. Acta Oceanologica Sinica, 2017, 36(7): 48-55. doi: 10.1007/s13131-016-1083-2
Citation: TAO Jing, MA Weiwei, ZHU Maoxu, LI Tie, YANG Rujun. Characterization of iron diagenesis in marine sediments using refined iron speciation and quantized iron(Ⅲ)-oxide reactivity: a case study in the Jiaozhou Bay, China[J]. Acta Oceanologica Sinica, 2017, 36(7): 48-55. doi: 10.1007/s13131-016-1083-2

Characterization of iron diagenesis in marine sediments using refined iron speciation and quantized iron(Ⅲ)-oxide reactivity: a case study in the Jiaozhou Bay, China

doi: 10.1007/s13131-016-1083-2
  • Received Date: 2016-04-21
  • Rev Recd Date: 2016-12-02
  • As a case study, refined iron (Fe) speciation and quantitative characterization of the reductive reactivity of Fe (Ⅲ) oxides are combined to investigate Fe diagenetic processes in a core sediment from the eutrophic Jiaozhou Bay. The results show that a combination of the two methods can trace Fe transformation in more detail and offer nuanced information on Fe diagenesis from multiple perspectives. This methodology may be used to enhance our understanding of the complex biogeochemical cycling of Fe and sulfur in other studies. Microbial iron reduction (MIR) plays an important role in Fe(Ⅲ) reduction over the upper sediments, while a chemical reduction by reaction with dissolved sulfide is the main process at a deeper (> 12 cm) layer. The most bioavailable amorphous Fe(Ⅲ) oxides [Fe(Ⅲ)am] are the main source of the MIR, followed by poorly crystalline Fe(Ⅲ) oxides [Fe(Ⅲ)pc)] and magnetite. Well crystalline Fe(Ⅲ) oxides [Fe (Ⅲ)wc] have barely participated in Fe diagenesis. The importance of the MIR over the upper layer may be a combined result of the high availability of highly reactive Fe oxides and low availability of labile organic matter, and the latter is also the ultimate factor limiting sulfate reduction and sulfide accumulation in the sediments. Microbially reducible Fe(Ⅲ) [MR-Fe(Ⅲ)], which is quantified by kinetics of Fe(Ⅱ)-oxide reduction, mainly consists of the most reactive Fe(Ⅲ)am and less reactive Fe(Ⅲ)pc. The bulk reactivity of the MR-Fe(Ⅲ) pool is equivalent to aged ferrihydrite, and shows down-core decrease due to preferential reduction of highly reactive phases of Fe oxides.
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  • Álvarez-Iglesias P, Rubio B. 2012. Early diagenesis of organic-matter-rich sediments in a ría environment: organic matter sources, pyrites morphology and limitation of pyritization at depth. Estuarine, Coastal and Shelf Science, 100: 113-123
    Amann R, Glöckner F O, Neef A. 1997. Modern methods in subsurface microbiology: in situ identification of microorganisms with nucleic acid probes. FEMS Microbiology Reviews, 20(3-4): 191-200
    Beckler J S, Kiriazi N, Rabouille C, et al. 2016. Importance of microbial iron reduction in deep sediments of river-dominated continental-margins. Marine Chemistry, 178: 22-34
    Berner R A. 1982. Burial of organic carbon and pyrite sulfur in the modern ocean: its geochemical and environmental significance. American Journal of Science, 282(4): 451-473
    Burton E D, Sullivan L A, Bush R T, et al. 2008. A simple and inexpensive chromium-reducible sulfur method for acid-sulfate soils. Applied Geochemistry, 23(9): 2759-2766
    Canfield D E, Berner R A. 1987. Dissolution and pyritization of magnetite in anoxie marine sediments. Geochimica et Cosmochimica Acta, 51(3): 645-659
    Canfield D E, Kristensen E, Thamdrup B. 2005. Aquatic Geomicrobiology. Amsterdam: Elsevier
    Chen Liangjin, Zhu Maoxu, Yang Guipeng, et al. 2013. Reductive reactivity of iron(Ⅲ) oxides in the East China Sea sediments: characterization by selective extraction and kinetic dissolution. PLoS One, 8(11): e80367
    Chen Keke, Zhu Maoxu, Yang Guipeng, et al. 2014. Spatial distribution of organic and pyritic sulfur in surface sediments of eutrophic Jiaozhou Bay, China: clues to anthropogenic impacts. Marine Pollution Bulletin, 88(1-2): 284-291
    Cline J D. 1969. Spectrophotometric determination of hydrogen sulfide in natural waters. Limnology and Oceanography, 14(3): 454-458
    Devereux R, Lehrter J C. 2015. Manganese, iron, and sulfur cycling in Louisiana continental shelf sediments. Continental Shelf Research, 99: 46-56
    Ge Can, Zhang Weiguo, Dong Chenyin, et al. 2015. Magnetic mineral diagenesis in the river-dominated inner shelf of the East China Sea, China. Journal of Geophysical Research: Solid Earth, 120(7): 4720-4733
    Goldhaber M B. 2003. Sulfur-rich sediment. In: Mackenzie F T, ed. Sediments, Diagenesis, and Sedimentary Rocks, Treatise on Geochemistry. Amsterdam: Elsevier, 257–288
    Hoehler T M, Alperin M J, Albert D B, et al. 1998. Thermodynamic control on hydrogen concentrations in anoxic sediments. Geochimica et Cosmochimica Acta, 62(10): 1745-1756
    Hyacinthe C, Bonneville S, van Cappellen P. 2006. Reactive iron(Ⅲ) in sediments: chemical versus microbial extractions. Geochimica et Cosmochimica Acta, 70(16): 4166-4180
    Hyacinthe C, van Cappellen P. 2004. An authigenic iron phosphate phase in estuarine sediments: composition, formation and chemical reactivity. Marine Chemistry, 91(1-4): 227-251
    Hyun J H, Kim S H, Mok J S, et al. 2013. Impacts of long-line aquaculture of Pacific oysters (Crassostrea gigas) on sulfate reduction and diffusive nutrient flux in the coastal sediments of Jinhae-Tongyeong, Korea. Marine Pollution Bulletin, 74(1): 187-198
    Jacobson M E. 1994. Chemical and biological mobilization of Fe(Ⅲ) in marsh sediments. Biogeochemistry, 25(1): 40-60
    Jensen M M, Thamdrup B, Rysgaard S, et al. 2003. Rates and regulation of microbial iron reduction in sediments of the Baltic-North Sea transition. Biogeochemistry, 65(3): 295-317
    Kallmeyer J, Ferdelman T G, Weber A, et al. 2004. A cold chromium distillation procedure for radiolabeled sulfide applied to sulfate reduction measurements. Limnology and Oceanography: Methods, 2(6): 171-180
    Konhauser K. 2006. Introduction to Geomicrobiology. Malden: Blackwell Publishing
    Koretsky C M, Moore C M, Lowe K L, et al. 2003. Seasonal oscillation of microbial iron and sulfate reduction in saltmarsh sediments (Sapelo Island, GA, USA). Biogeochemistry, 64(2): 179-203
    Koretsky C M, van Cappellen P, DiChristina T J, et al. 2005. Salt marsh pore water geochemistry does not correlate with microbial community structure. Estuarine, Coastal and Shelf Science, 62(1-2): 233-251
    Kostka J E, Luther Ⅲ G W. 1994. Partitioning and speciation of solid phase iron in saltmarsh sediments. Geochimica et Cosmochimica Acta, 58(7): 1701-1710
    Kraal P, Burton E D, Bush R T. 2013. Iron monosulfide accumulation and pyrite formation in eutrophic estuarine sediments. Geochimica et Cosmochimica Acta, 122: 75-88
    Kristensen E, Mangion P, Tang M, et al. 2011. Microbial carbon oxidation rates and pathways in sediments of two Tanzanian mangrove forests. Biogeochemistry, 103(1): 143-158
    Larsen O, Postma D. 2001. Kinetics of reductive bulk dissolution of lepidocrocite, ferrihydrite, and goethite. Geochimica et Cosmochimica Acta, 65(9): 1367-1379
    Lehtoranta J, Ekholm P, Pitkänen H. 2009. Coastal eutrophication thresholds: a matter of sediment microbial processes. Ambio, 38(6): 303-308
    Liu Sumei, Zhang Jing, Chen Hongtao, et al. 2005. Factors influencing nutrient dynamics in the eutrophic Jiaozhou Bay, North China. Progress in Oceanography, 66(1): 66-85
    Liu Sumei, Zhu Bingde, Zhang Jing, et al. 2010. Environmental change in Jiaozhou Bay recorded by nutrient components in sediments. Marine Pollution Bulletin, 60(9): 1591-1599
    Lovley D R. 1991. Dissimilatory Fe(Ⅲ) and Mn(IV) reduction. Microbiological Review, 55(2): 259-287
    Lovley D R, Phillips E J P. 1987. Rapid assay for microbially reducible ferric iron in aquatic sediments. Applied and Environmental Microbiology, 53(7): 1536-1540
    Luna G M, Manini E, Danovaro R. 2002. Large fraction of dead and inactive bacteria in coastal marine sediments: comparison of protocols for determination and ecological significance. Applied and Environmental Microbiology, 68(7): 3509-3513
    Luther Ⅲ G W. 1991. Pyrite synthesis via polysulfide compounds. Geochimica et Cosmochimica Acta, 55(10): 2839-2849
    März C, Poulton S W, Brumsack H J, et al. 2012. Climate-controlled variability of iron deposition in the central arctic ocean (southern Mendeleev Ridge) over the last 130 000 years. Chemical Geology, 330-331: 116-126
    Nickel M, Vandieken V, Brüchert V, et al. 2008. Microbial Mn(IV) and Fe(Ⅲ) reduction in northern Barents Sea sediments under different conditions of ice cover and organic carbon deposition. Deep-Sea Research: Part Ⅱ Topical Studies in Oceanography, 55(20-21): 2390-2398
    Postma D. 1993. The reactivity of iron oxides in sediments: a kinetic approach. Geochimica et Cosmochimica Acta, 57(21-22): 5027-5034
    Poulton S W, Canfield D E. 2005. Development of a sequential extraction procedure for iron: implications for iron partitioning in continentally derived particulates. Chemical Geology, 214(3-4): 209-221
    Pu Xiaoqiang, Zhong Shaojun, Liu Fei, et al. 2009. Restriction factors to sulfide formation in estuarine sediments of Licun River of Jiaozhou Bay. Geochimica (in Chinese), 38(4): 323-333
    Raiswell R, Canfield D E, Berner R A. 1994. A comparison of iron extraction methods for the determination of degree of pyritisation and the recognition of iron-limited pyrite formation. Chemical Geology, 111(1–4): 101-110
    Raiswell R, Canfield D E. 2012. The iron biogeochemical cycle past and present. Geochemical Prospectives, 1(1): 1-220
    Raiswell R, Vu H P, Brinza L, et al. 2010. The determination of labile Fe in ferrihydrite by ascorbic acid extraction: methodology, dissolution kinetics and loss of solubility with age and de-watering. Chemical Geology, 278(1-2): 70-79
    Rickard D T. 1975. Kinetics and mechanism of pyrite formation at low temperatures. American Journal of Science, 275(6): 636-652
    Rickard D. 2014. The sedimentary sulfur system: biogeochemistry and evolution through geologic time. In: Mackenzie F T, ed. Sediments, Diagenesis, and Sedimentary Rocks, Treatise on Geochemistry. 2nd ed. Amsterdam: Elsevier, 267–326
    Rickard D, Morse J W. 2005. Acid volatile sulfide (AVS). Marine Chemistry, 97(3-4): 141-197
    Rowan C J, Roberts A P, Broadbent T. 2009. Reductive diagenesis, magnetite dissolution, greigite growth and paleomagnetic smoothing in marine sediments: a new view. Earth and Planetary Science Letters, 277(1-2): 223-235
    Rysgaard S, Fossing H, Jensen M M. 2001. Organic matter degradation through oxygen respiration, denitrification, and manganese, iron, and sulfate reduction in marine sediments (the Kattegat and the Skagerrak). Ophelia, 55(2): 77
    Stookey L L. 1970. Ferrozine -A new spectrophotometric reagent for iron. Analytical Chemistry, 42(7): 779-781
    Thamdrup B. 2000. Bacterial manganese and iron reduction in aquatic sediments. In: Schink B, eds. Advances in Microbial Ecology. New York: Springer, 41–84
    Wang Yifeng, van Cappellen P. 1996. A multicomponent reactive transport model of early diagenesis: application to redox cycling in coastal marine sediments. Geochimica et Cosmochimica Acta, 60(16): 2993-3014
    Wijsman J W M, Herman P M J, Middelburg J J, et al. 2002. A model for early diagenetic processes in sediments of the continental shelf of the Black Sea. Estuarine, Coastal and Shelf Science, 54(3): 403-421
    Wu Yulin, Sun Song, Zhang Yongshan. 2005. Long-term change of environment and it’s influence on phytoplankton community structure in Jiaozhou Bay. Oceanologia et Limnologia Sinica (in Chinese), 36(6): 487-498
    Zhu Maoxu, Chen Liangjin, Yang Guipeng, et al. 2014b. Kinetic characterization on reductive reactivity of iron(Ⅲ) oxides in surface sediments of the East China Sea and the influence of repeated redox cycles: implications for microbial iron reduction. Applied Geochemistry, 42: 16-26
    Zhu Maoxu, Chen Liangjin, Yang Guipeng, et al. 2014a. Humic sulfur in eutrophic bay sediments: characterization by sulfur stable isotopes and K-edge XANES spectroscopy. Estuarine, Coastal and Shelf Science, 138: 121-129
    Zhu Maoxu, Huang Xiangli, Yang Guipeng, et al. 2015. Iron geochemistry in surface sediments of a temperate semi-enclosed bay, North China. Estuarine, Coastal and Shelf Science, 165: 25-35
    Zhu Maoxu, Liu Juan, Yang Guipeng, et al. 2012. Reactive iron and its buffering capacity towards dissolved sulfide in sediments of Jiaozhou Bay, China. Marine Environmental Research, 80: 46-55
    Zhu Maoxu, Shi Xiaoning, Yang Guipeng, et al. 2013. Formation and burial of pyrite and organic sulfur in mud sediments of the East China Sea inner shelf: constraints from solid-phase sulfur speciation and stable sulfur isotope. Continental Shelf Research, 54: 24-36
    Zimmerman A R, Canuel E A. 2000. A geochemical record of eutrophication and anoxia in Chesapeake Bay sediments: anthropogenic influence on organic matter composition. Marine Chemistry, 69(1-2): 117-137
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