Articles | Volume 15, issue 20
https://doi.org/10.5194/bg-15-6329-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-15-6329-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
26 Oct 2018
Research article |
| 26 Oct 2018
| 26 Oct 2018
Vivianite formation in methane-rich deep-sea sediments from the South China Sea
Jiarui Liu
State Key Laboratory of Biogeology and Environment Geology, College
of Marine Science and Technology, School of Earth Sciences, China University
of Geosciences, Wuhan, 430074, China
Gareth Izon
Department of Earth,
Atmospheric and Planetary Sciences, Massachusetts Institute of Technology,
Cambridge, MA 02139, USA
Jiasheng Wang
CORRESPONDING AUTHOR
State Key Laboratory of Biogeology and Environment Geology, College
of Marine Science and Technology, School of Earth Sciences, China University
of Geosciences, Wuhan, 430074, China
Gilad Antler
Department of Geological and Environmental Sciences, Ben-Gurion
University of the Negev, Beersheba, 84105, Israel
The
Interuniversity Institute for Marine Sciences, Eilat, 88103, Israel
Department of Earth
Sciences, University of Cambridge, Cambridge, CB2 3EQ, UK
Zhou Wang
State Key Laboratory of Biogeology and Environment Geology, College
of Marine Science and Technology, School of Earth Sciences, China University
of Geosciences, Wuhan, 430074, China
Jie Zhao
State Key Laboratory of Biogeology and Environment Geology, College
of Marine Science and Technology, School of Earth Sciences, China University
of Geosciences, Wuhan, 430074, China
Matthias Egger
The Ocean Cleanup Foundation, Rotterdam, 3014 JH, the Netherlands
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Wytze K. Lenstra, Matthias Egger, Niels A. G. M. van Helmond, Emma Kritzberg, Daniel J. Conley, and Caroline P. Slomp
Biogeosciences, 15, 6979–6996, https://doi.org/10.5194/bg-15-6979-2018, https://doi.org/10.5194/bg-15-6979-2018, 2018
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We show that burial rates of phosphorus (P) in an estuary in the northern Baltic Sea are very high. We demonstrate that at high sedimentation rates, P retention in the sediment is related to the formation of vivianite. With a reactive transport model, we assess the sensitivity of sedimentary vivianite formation. We suggest that enrichments of iron and P in the sediment are linked to periods of enhanced riverine input of Fe, which subsequently strongly enhances P burial in coastal sediments.
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Gerard J. M. Versteegh, Andrea Koschinsky, Thomas Kuhn, Inken Preuss, and Sabine Kasten
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Annika Fiskal, Eva Anthamatten, Longhui Deng, Xingguo Han, Lorenzo Lagostina, Anja Michel, Rong Zhu, Nathalie Dubois, Carsten J. Schubert, Stefano M. Bernasconi, and Mark A. Lever
Biogeosciences, 18, 4369–4388, https://doi.org/10.5194/bg-18-4369-2021, https://doi.org/10.5194/bg-18-4369-2021, 2021
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Astrid Hylén, Sebastiaan J. van de Velde, Mikhail Kononets, Mingyue Luo, Elin Almroth-Rosell, and Per O. J. Hall
Biogeosciences, 18, 2981–3004, https://doi.org/10.5194/bg-18-2981-2021, https://doi.org/10.5194/bg-18-2981-2021, 2021
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Sediments in oxygen-depleted ocean areas release high amounts of phosphorus, feeding algae that consume oxygen upon degradation, leading to further phosphorus release. Oxygenation is thought to trap phosphorus in the sediment and break this feedback. We studied the sediment phosphorus cycle in a previously anoxic area after an inflow of oxic water. Surprisingly, the sediment phosphorus release increased, showing that feedbacks between phosphorus release and oxygen depletion can be hard to break.
Sebastiaan J. van de Velde, Rebecca K. James, Ine Callebaut, Silvia Hidalgo-Martinez, and Filip J. R. Meysman
Biogeosciences, 18, 1451–1461, https://doi.org/10.5194/bg-18-1451-2021, https://doi.org/10.5194/bg-18-1451-2021, 2021
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Some 540 Myr ago, animal life evolved in the ocean. Previous research suggested that when these early animals started inhabiting the seafloor, they retained phosphorus in the seafloor, thereby limiting photosynthesis in the ocean. We studied salt marsh sediments with and without animals and found that their impact on phosphorus retention is limited, which implies that their impact on the global environment might have been less drastic than previously assumed.
Martijn Hermans, Nils Risgaard-Petersen, Filip J. R. Meysman, and Caroline P. Slomp
Biogeosciences, 17, 5919–5938, https://doi.org/10.5194/bg-17-5919-2020, https://doi.org/10.5194/bg-17-5919-2020, 2020
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This paper demonstrates that the recently discovered cable bacteria are capable of using a mineral, known as siderite, as a source for the formation of iron oxides. This work also demonstrates that the activity of cable bacteria can lead to a distinct subsurface layer in the sediment that can be used as a marker for their activity.
Torben Windirsch, Guido Grosse, Mathias Ulrich, Lutz Schirrmeister, Alexander N. Fedorov, Pavel Y. Konstantinov, Matthias Fuchs, Loeka L. Jongejans, Juliane Wolter, Thomas Opel, and Jens Strauss
Biogeosciences, 17, 3797–3814, https://doi.org/10.5194/bg-17-3797-2020, https://doi.org/10.5194/bg-17-3797-2020, 2020
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To extend the knowledge on circumpolar deep permafrost carbon storage, we examined two deep permafrost deposit types (Yedoma and alas) in central Yakutia. We found little but partially undecomposed organic carbon as a result of largely changing sedimentation processes. The carbon stock of the examined Yedoma deposits is about 50 % lower than the general Yedoma domain mean, implying a very hetererogeneous Yedoma composition, while the alas is approximately 80 % below the thermokarst deposit mean.
Anna Plass, Christian Schlosser, Stefan Sommer, Andrew W. Dale, Eric P. Achterberg, and Florian Scholz
Biogeosciences, 17, 3685–3704, https://doi.org/10.5194/bg-17-3685-2020, https://doi.org/10.5194/bg-17-3685-2020, 2020
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We compare the cycling of Fe and Cd in sulfidic sediments of the Peruvian oxygen minimum zone. Due to the contrasting solubility of their sulfide minerals, the sedimentary Fe release and Cd burial fluxes covary with spatial and temporal distributions of H2S. Depending on the solubility of their sulfide minerals, sedimentary trace metal fluxes will respond differently to ocean deoxygenation/expansion of H2S concentrations, which may change trace metal stoichiometry of upwelling water masses.
Biqing Zhu, Manuel Kübler, Melanie Ridoli, Daniel Breitenstein, and Martin H. Schroth
Biogeosciences, 17, 3613–3630, https://doi.org/10.5194/bg-17-3613-2020, https://doi.org/10.5194/bg-17-3613-2020, 2020
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We provide evidence that the greenhouse gas methane (CH4) is enclosed in calcareous glacier-forefield sediments across Switzerland. Geochemical analyses confirmed that this ancient CH4 has its origin in the calcareous parent bedrock. Our estimate of the total quantity of CH4 enclosed in sediments across Switzerland indicates a large CH4 mass (~105 t CH4). We produced evidence that CH4 is stable in its enclosed state, but additional experiments are needed to elucidate its long-term fate.
Matteo Puglini, Victor Brovkin, Pierre Regnier, and Sandra Arndt
Biogeosciences, 17, 3247–3275, https://doi.org/10.5194/bg-17-3247-2020, https://doi.org/10.5194/bg-17-3247-2020, 2020
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A reaction-transport model to assess the potential non-turbulent methane flux from the East Siberian Arctic sediments to water columns is applied here. We show that anaerobic oxidation of methane (AOM) is an efficient filter except for high values of sedimentation rate and advective flow, which enable considerable non-turbulent steady-state methane fluxes. Significant transient methane fluxes can also occur during the building-up phase of the AOM-performing biomass microbial community.
Kyle Delwiche, Junyao Gu, Harold Hemond, and Sarah P. Preheim
Biogeosciences, 17, 3135–3147, https://doi.org/10.5194/bg-17-3135-2020, https://doi.org/10.5194/bg-17-3135-2020, 2020
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In this study, we investigate whether bubbles transport sediments containing arsenic and cyanobacteria from the bottom to the top of a polluted lake. We measured arsenic and cyanobacteria from bubble traps in the lake and from an experimental bubble column in the laboratory. We found that bubble transport was not an important source of arsenic in the surface waters but that bubbles could transport enough cyanobacteria to the surface to exacerbate harmful algal blooms.
Nathaniel Kemnitz, William M. Berelson, Douglas E. Hammond, Laura Morine, Maria Figueroa, Timothy W. Lyons, Simon Scharf, Nick Rollins, Elizabeth Petsios, Sydnie Lemieux, and Tina Treude
Biogeosciences, 17, 2381–2396, https://doi.org/10.5194/bg-17-2381-2020, https://doi.org/10.5194/bg-17-2381-2020, 2020
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Our paper shows how sedimentation in a very low oxygen setting provides a unique record of environmental change. We look at the past 250 years through the filter of sediment accumulation via radioisotope dating and other physical and chemical analyses of these sediments. We conclude, remarkably, that there has been very little change in net sediment mass accumulation through the past 100–150 years, yet just prior to 1900 CE, sediments were accumulating at 50 %–70 % of today's rate.
Dario Fussmann, Avril Jean Elisabeth von Hoyningen-Huene, Andreas Reimer, Dominik Schneider, Hana Babková, Robert Peticzka, Andreas Maier, Gernot Arp, Rolf Daniel, and Patrick Meister
Biogeosciences, 17, 2085–2106, https://doi.org/10.5194/bg-17-2085-2020, https://doi.org/10.5194/bg-17-2085-2020, 2020
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Dolomite (CaMg(CO3)2) is supersaturated in many aquatic settings (e.g., seawater) on modern Earth but does not precipitate directly from the fluid, a fact known as the dolomite problem. The widely acknowledged concept of dolomite precipitation involves microbial extracellular polymeric substances (EPSs) and anoxic conditions as important drivers. In contrast, results from Lake Neusiedl support an alternative concept of Ca–Mg carbonate precipitation under aerobic and alkaline conditions.
Aurèle Vuillemin, André Friese, Richard Wirth, Jan A. Schuessler, Anja M. Schleicher, Helga Kemnitz, Andreas Lücke, Kohen W. Bauer, Sulung Nomosatryo, Friedhelm von Blanckenburg, Rachel Simister, Luis G. Ordoñez, Daniel Ariztegui, Cynthia Henny, James M. Russell, Satria Bijaksana, Hendrik Vogel, Sean A. Crowe, Jens Kallmeyer, and the Towuti Drilling Project
Science team
Biogeosciences, 17, 1955–1973, https://doi.org/10.5194/bg-17-1955-2020, https://doi.org/10.5194/bg-17-1955-2020, 2020
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Ferruginous lakes experience restricted primary production due to phosphorus trapping by ferric iron oxides under oxic conditions. We report the presence of large crystals of vivianite, a ferrous iron phosphate, in sediments from Lake Towuti, Indonesia. We address processes of P retention linked to diagenesis of iron phases. Vivianite crystals had light Fe2+ isotope signatures and contained mineral inclusions consistent with antecedent processes of microbial sulfate and iron reduction.
Sonja Geilert, Patricia Grasse, Kristin Doering, Klaus Wallmann, Claudia Ehlert, Florian Scholz, Martin Frank, Mark Schmidt, and Christian Hensen
Biogeosciences, 17, 1745–1763, https://doi.org/10.5194/bg-17-1745-2020, https://doi.org/10.5194/bg-17-1745-2020, 2020
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Marine silicate weathering is a key process of the marine silica cycle; however, its controlling processes are not well understood. In the Guaymas Basin, silicate weathering has been studied under markedly differing ambient conditions. Environmental settings like redox conditions or terrigenous input of reactive silicates appear to be major factors controlling marine silicate weathering. These factors need to be taken into account in future oceanic mass balances of Si and in modeling studies.
Jessica B. Volz, Laura Haffert, Matthias Haeckel, Andrea Koschinsky, and Sabine Kasten
Biogeosciences, 17, 1113–1131, https://doi.org/10.5194/bg-17-1113-2020, https://doi.org/10.5194/bg-17-1113-2020, 2020
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Potential future deep-sea mining of polymetallic nodules at the seafloor is expected to severely harm the marine environment. However, the consequences on deep-sea ecosystems are still poorly understood. This study on surface sediments from man-made disturbance tracks in the Pacific Ocean shows that due to the removal of the uppermost sediment layer and thereby the loss of organic matter, the geochemical system in the sediments is disturbed for millennia before reaching a new equilibrium.
Ralf Conrad, Melanie Klose, and Alex Enrich-Prast
Biogeosciences, 17, 1063–1069, https://doi.org/10.5194/bg-17-1063-2020, https://doi.org/10.5194/bg-17-1063-2020, 2020
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Lake sediments release the greenhouse gas CH4. Acetate is an important precursor. Although Amazonian lake sediments all contained acetate-consuming methanogens, measurement of the turnover of labeled acetate showed that some sediments converted acetate not to CH4 plus CO2, as expected, but only to CO2. Our results indicate the operation of acetate-oxidizing microorganisms couples the oxidation process to syntrophic methanogenic partners and/or to the reduction of organic compounds.
Jens Rassmann, Eryn M. Eitel, Bruno Lansard, Cécile Cathalot, Christophe Brandily, Martial Taillefert, and Christophe Rabouille
Biogeosciences, 17, 13–33, https://doi.org/10.5194/bg-17-13-2020, https://doi.org/10.5194/bg-17-13-2020, 2020
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In this paper, we use a large set of measurements made using in situ and lab techniques to elucidate the cause of dissolved inorganic carbon fluxes in sediments from the Rhône delta and its companion compound alkalinity, which carries the absorption capacity of coastal waters with respect to atmospheric CO2. We show that sediment processes (sulfate reduction, FeS precipitation and accumulation) are crucial in generating the alkalinity fluxes observed in this study by in situ incubation chambers.
Sophie A. L. Paul, Matthias Haeckel, Michael Bau, Rajina Bajracharya, and Andrea Koschinsky
Biogeosciences, 16, 4829–4849, https://doi.org/10.5194/bg-16-4829-2019, https://doi.org/10.5194/bg-16-4829-2019, 2019
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We studied the upper 10 m of deep-sea sediments, including pore water, in the Peru Basin to understand small-scale variability of trace metals. Our results show high spatial variability related to topographical variations, which in turn impact organic matter contents, degradation processes, and trace metal cycling. Another interesting finding was the influence of dissolving buried nodules on the surrounding sediment and trace metal cycling.
Sarah Paradis, Antonio Pusceddu, Pere Masqué, Pere Puig, Davide Moccia, Tommaso Russo, and Claudio Lo Iacono
Biogeosciences, 16, 4307–4320, https://doi.org/10.5194/bg-16-4307-2019, https://doi.org/10.5194/bg-16-4307-2019, 2019
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Chronic deep bottom trawling in the Gulf of Castellammare (SW Mediterranean) erodes large volumes of sediment, exposing over-century-old sediment depleted in organic matter. Nevertheless, the arrival of fresh and nutritious sediment recovers superficial organic matter in trawling grounds and leads to high turnover rates, partially and temporarily mitigating the impacts of bottom trawling. However, this deposition is ephemeral and it will be swiftly eroded by the passage of the next trawler.
Zhichao Zhou, Bo Liang, Li-Ying Wang, Jin-Feng Liu, Bo-Zhong Mu, Hojae Shim, and Ji-Dong Gu
Biogeosciences, 16, 4229–4241, https://doi.org/10.5194/bg-16-4229-2019, https://doi.org/10.5194/bg-16-4229-2019, 2019
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This study shows a core bacterial microbiome with a small proportion of shared operational taxonomic units of common sequences among all oil reservoirs. Dominant methanogenesis shifts from the hydrogenotrophic pathway in water phase to the acetoclastic pathway in the oil phase at high temperatures, but the opposite is true at low temperatures. There are also major functional metabolism differences between the two phases for amino acids, hydrocarbons, and carbohydrates.
Annika Fiskal, Longhui Deng, Anja Michel, Philip Eickenbusch, Xingguo Han, Lorenzo Lagostina, Rong Zhu, Michael Sander, Martin H. Schroth, Stefano M. Bernasconi, Nathalie Dubois, and Mark A. Lever
Biogeosciences, 16, 3725–3746, https://doi.org/10.5194/bg-16-3725-2019, https://doi.org/10.5194/bg-16-3725-2019, 2019
Hanni Vigderovich, Lewen Liang, Barak Herut, Fengping Wang, Eyal Wurgaft, Maxim Rubin-Blum, and Orit Sivan
Biogeosciences, 16, 3165–3181, https://doi.org/10.5194/bg-16-3165-2019, https://doi.org/10.5194/bg-16-3165-2019, 2019
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Microbial iron reduction participates in important biogeochemical cycles. In the last decade iron reduction has been observed in many aquatic sediments below its classical zone, in the methane production zone, suggesting a link between the two cycles. Here we present evidence for microbial iron reduction in the methanogenic depth of the oligotrophic SE Mediterranean continental shelf using mainly geochemical and microbial sedimentary profiles and suggest possible mechanisms for this process.
Haoyi Yao, Wei-Li Hong, Giuliana Panieri, Simone Sauer, Marta E. Torres, Moritz F. Lehmann, Friederike Gründger, and Helge Niemann
Biogeosciences, 16, 2221–2232, https://doi.org/10.5194/bg-16-2221-2019, https://doi.org/10.5194/bg-16-2221-2019, 2019
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How methane is transported in the sediment is important for the microbial community living on methane. Here we report an observation of a mini-fracture that facilitates the advective gas transport of methane in the sediment, compared to the diffusive fluid transport without a fracture. We found contrasting bio-geochemical signals in these different transport modes. This finding can help to fill the gap in the fracture network system in modulating methane dynamics in surface sediments.
Laura A. Casella, Sixin He, Erika Griesshaber, Lourdes Fernández-Díaz, Martina Greiner, Elizabeth M. Harper, Daniel J. Jackson, Andreas Ziegler, Vasileios Mavromatis, Martin Dietzel, Anton Eisenhauer, Sabino Veintemillas-Verdaguer, Uwe Brand, and Wolfgang W. Schmahl
Biogeosciences, 15, 7451–7484, https://doi.org/10.5194/bg-15-7451-2018, https://doi.org/10.5194/bg-15-7451-2018, 2018
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Biogenic carbonates record past environmental conditions. Fossil shell chemistry and microstructure change as metastable biogenic carbonates are replaced by inorganic calcite. Simulated diagenetic alteration at 175 °C of different shell microstructures showed that (nacreous) shell aragonite and calcite were partially replaced by coarse inorganic calcite crystals due to dissolution–reprecipitation reactions. EBSD maps allowed for qualitative assessment of the degree of diagenetic overprint.
Wytze K. Lenstra, Matthias Egger, Niels A. G. M. van Helmond, Emma Kritzberg, Daniel J. Conley, and Caroline P. Slomp
Biogeosciences, 15, 6979–6996, https://doi.org/10.5194/bg-15-6979-2018, https://doi.org/10.5194/bg-15-6979-2018, 2018
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We show that burial rates of phosphorus (P) in an estuary in the northern Baltic Sea are very high. We demonstrate that at high sedimentation rates, P retention in the sediment is related to the formation of vivianite. With a reactive transport model, we assess the sensitivity of sedimentary vivianite formation. We suggest that enrichments of iron and P in the sediment are linked to periods of enhanced riverine input of Fe, which subsequently strongly enhances P burial in coastal sediments.
Marc A. Besseling, Ellen C. Hopmans, R. Christine Boschman, Jaap S. Sinninghe Damsté, and Laura Villanueva
Biogeosciences, 15, 4047–4064, https://doi.org/10.5194/bg-15-4047-2018, https://doi.org/10.5194/bg-15-4047-2018, 2018
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Benthic archaea comprise a significant part of the total prokaryotic biomass in marine sediments. Here, we compared the archaeal diversity and intact polar lipid (IPL) composition in both surface and subsurface sediments with different oxygen regimes in the Arabian Sea oxygen minimum zone. The oxygenated sediments were dominated by Thaumarchaeota and IPL-GDGT-0. The anoxic sediment contained highly diverse archaeal communities and high relative abundances of IPL-GDGT-1 to -4.
Georgina Robinson, Thomas MacTavish, Candida Savage, Gary S. Caldwell, Clifford L. W. Jones, Trevor Probyn, Bradley D. Eyre, and Selina M. Stead
Biogeosciences, 15, 1863–1878, https://doi.org/10.5194/bg-15-1863-2018, https://doi.org/10.5194/bg-15-1863-2018, 2018
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This study examined the effect of adding carbon to a sediment-based effluent treatment system to treat nitrogen-rich aquaculture waste. The research was conducted in incubation chambers to measure the exchange of gases and nutrients across the sediment–water interface and examine changes in the sediment microbial community. Adding carbon increased the amount of nitrogen retained in the treatment system, thereby reducing the levels of nitrogen needing to be discharged to the environment.
Daniele Brigolin, Christophe Rabouille, Bruno Bombled, Silvia Colla, Salvatrice Vizzini, Roberto Pastres, and Fabio Pranovi
Biogeosciences, 15, 1347–1366, https://doi.org/10.5194/bg-15-1347-2018, https://doi.org/10.5194/bg-15-1347-2018, 2018
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We present the result of a study carried out in the north-western Adriatic Sea by combining two different types of models with field sampling. A mussel farm was taken as a local source of perturbation to the natural flux of particulate organic carbon to the sediment. Differences in fluxes were primarily associated with mussel physiological conditions. Although restricted, these changes in particulate organic carbon fluxes induced visible effects on sediment biogeochemistry.
Volker Brüchert, Lisa Bröder, Joanna E. Sawicka, Tommaso Tesi, Samantha P. Joye, Xiaole Sun, Igor P. Semiletov, and Vladimir A. Samarkin
Biogeosciences, 15, 471–490, https://doi.org/10.5194/bg-15-471-2018, https://doi.org/10.5194/bg-15-471-2018, 2018
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We determined the aerobic and anaerobic degradation rates of land- and marine-derived organic material in East Siberian shelf sediment. Marine plankton-derived organic carbon was the main source for the oxic dissolved carbon dioxide production, whereas terrestrial organic material significantly contributed to the production of carbon dioxide under anoxic conditions. Our direct degradation rate measurements provide new constraints for the present-day Arctic marine carbon budget.
Jack J. Middelburg
Biogeosciences, 15, 413–427, https://doi.org/10.5194/bg-15-413-2018, https://doi.org/10.5194/bg-15-413-2018, 2018
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Organic carbon processing at the seafloor is studied by geologists to better understand the sedimentary record, by biogeochemists to quantify burial and respiration, by organic geochemists to elucidate compositional changes, and by ecologists to follow carbon transfers within food webs. These disciplinary approaches have their strengths and weaknesses. This award talk provides a synthesis, highlights the role of animals in sediment carbon processing and presents some new concepts.
Craig Smeaton, William E. N. Austin, Althea L. Davies, Agnes Baltzer, John A. Howe, and John M. Baxter
Biogeosciences, 14, 5663–5674, https://doi.org/10.5194/bg-14-5663-2017, https://doi.org/10.5194/bg-14-5663-2017, 2017
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Fjord sediments are recognised as hotspots for the burial and long-term storage of carbon. In this study, we use the Scottish fjords as a natural laboratory. Using geophysical and geochemical analysis in combination with upscaling techniques, we have generated the first full national sedimentary C inventory for a fjordic system. The results indicate that the Scottish fjords on a like-for-like basis are more effective as C stores than their terrestrial counterparts, including Scottish peatlands.
Perran Louis Miall Cook, Adam John Kessler, and Bradley David Eyre
Biogeosciences, 14, 4061–4069, https://doi.org/10.5194/bg-14-4061-2017, https://doi.org/10.5194/bg-14-4061-2017, 2017
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Nitrogen is the key nutrient that typically limits productivity in coastal waters. One of the key controls on the amount of bioavailable nitrogen is the process of denitrification, which converts nitrate (bioavailable) into nitrogen gas. Previous studies suggest high rates of denitrification may take place within carbonate sediments, and one explanation for this is that this process may take place within the sand grains. Here we show evidence to support this hypothesis.
Chris T. Parsons, Fereidoun Rezanezhad, David W. O'Connell, and Philippe Van Cappellen
Biogeosciences, 14, 3585–3602, https://doi.org/10.5194/bg-14-3585-2017, https://doi.org/10.5194/bg-14-3585-2017, 2017
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Phosphorus (P) has accumulated in sediments due to past human activities. The re-release of this P to water contributes to the growth of harmful algal blooms. Our research improves our mechanistic understanding of how P is partitioned between different chemical forms and between sediment and water under dynamic conditions. We demonstrate that P trapped within iron minerals may be less mobile during anoxic conditions than previously thought due to reversible changes to P forms within sediment.
Clint M. Miller, Gerald R. Dickens, Martin Jakobsson, Carina Johansson, Andrey Koshurnikov, Matt O'Regan, Francesco Muschitiello, Christian Stranne, and Carl-Magnus Mörth
Biogeosciences, 14, 2929–2953, https://doi.org/10.5194/bg-14-2929-2017, https://doi.org/10.5194/bg-14-2929-2017, 2017
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Continental slopes north of the East Siberian Sea are assumed to hold large amounts of methane. We present pore water chemistry from the 2014 SWERUS-C3 expedition. These are among the first results generated from this vast climatically sensitive region, and they imply that abundant methane, including gas hydrates, do not characterize the East Siberian Sea slope or rise. This contradicts previous modeling and discussions, which due to the lack of data are almost entirely based assumption.
Laura A. Casella, Erika Griesshaber, Xiaofei Yin, Andreas Ziegler, Vasileios Mavromatis, Dirk Müller, Ann-Christine Ritter, Dorothee Hippler, Elizabeth M. Harper, Martin Dietzel, Adrian Immenhauser, Bernd R. Schöne, Lucia Angiolini, and Wolfgang W. Schmahl
Biogeosciences, 14, 1461–1492, https://doi.org/10.5194/bg-14-1461-2017, https://doi.org/10.5194/bg-14-1461-2017, 2017
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Mollusc shells record past environments. Fossil shell chemistry and microstructure change as metastable biogenic aragonite transforms to stable geogenic calcite. We simulated this alteration of Arctica islandica shells by hydrothermal treatments. Below 175 °C the shell aragonite survived for weeks. At 175 °C the replacement of the original material starts after 4 days and yields submillimetre-sized calcites preserving the macroscopic morphology as well as the original internal micromorphology.
Jung-Ho Hyun, Sung-Han Kim, Jin-Sook Mok, Hyeyoun Cho, Tongsup Lee, Verona Vandieken, and Bo Thamdrup
Biogeosciences, 14, 941–958, https://doi.org/10.5194/bg-14-941-2017, https://doi.org/10.5194/bg-14-941-2017, 2017
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The surface sediments of the Ulleung Basin (UB) in the East Sea are characterized by high organic carbon contents (> 2.5 %, dry wt.) and very high concentrations of Mn oxides (> 200 μmol cm−3) and Fe oxides (up to 100 μmol cm−3). For the first time in deep offshore sediments on the Asian margin with water depth over 2000 m, we report that Mn reduction and Fe reduction were the dominant organic carbon (Corg) oxidation pathways, comprising 45 % and 20 % of total Corg oxidation, respectively.
Jens Rassmann, Bruno Lansard, Lara Pozzato, and Christophe Rabouille
Biogeosciences, 13, 5379–5394, https://doi.org/10.5194/bg-13-5379-2016, https://doi.org/10.5194/bg-13-5379-2016, 2016
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In situ O2 and pH measurements as well as determination of porewater concentrations of dissolved inorganic carbon, total alkalinity, sulfate and calcium have been measured in the sediments of the Rhône prodelta. Biogeochemical activity decreased with distance from the river mouth. Oxic processes decreased the carbonate saturation state (Ω) by lowering pH, whereas anaerobic organic matter degradation, dominated by sulfate reduction, was accompanied by increasing Ω and carbonate precipitation.
Matthias Egger, Peter Kraal, Tom Jilbert, Fatimah Sulu-Gambari, Célia J. Sapart, Thomas Röckmann, and Caroline P. Slomp
Biogeosciences, 13, 5333–5355, https://doi.org/10.5194/bg-13-5333-2016, https://doi.org/10.5194/bg-13-5333-2016, 2016
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By combining detailed geochemical analyses with diagenetic modeling, we provide new insights into how methane dynamics may strongly overprint burial records of iron, sulfur and phosphorus in marine systems subject to changes in organic matter loading or water column salinity. A better understanding of these processes will improve our ability to read ancient sediment records and thus to predict the potential consequences of global warming and human-enhanced inputs of nutrients to the ocean.
Cited articles
Algeo, T. J. and Ingall, E.: Sedimentary Corg:P ratios, paleocean
ventilation, and Phanerozoic atmospheric pO2, Palaeogeogr. Palaeocl., 256,
130–155, https://doi.org/10.1016/j.palaeo.2007.02.029, 2007.
Amonette, J. E. and Templeton, J. C.: Improvements to the quantitative assay
of nonrefractory minerals for Fe (II) and total Fe using 1,
10-phenanthroline, Clays Clay Miner., 46, 51–62,
https://doi.org/10.1346/CCMN.1998.0460106, 1998.
Amos, R., Bekins, B., Cozzarelli, I., Voytek, M., Kirshtein, J., Jones, E.,
and Blowes, D.: Evidence for iron-mediated anaerobic methane oxidation in a
crude oil-contaminated aquifer, Geobiology, 10, 506–517,
https://doi.org/10.1111/j.1472-4669.2012.00341.x, 2012.
Bar-Or, I., Elvert, M., Eckert, W., Kushmaro, A., Vigderovich, H., Zhu, Q.,
Ben-Dov, E., and Sivan, O.: Iron-Coupled Anaerobic Oxidation of Methane
Performed by a Mixed Bacterial-Archaeal Community Based on Poorly Reactive
Minerals, Environ. Sci. Technol., 51, 12293–12301,
https://doi.org/10.1021/acs.est.7b03126, 2017.
Beal, E. J., House, C. H., and Orphan, V. J.: Manganese-and iron-dependent
marine methane oxidation, Science, 325, 184–187, https://doi.org/10.1126/science.1169984,
2009.
Berner, R. A.: Thermodynamic stability of sedimentary iron sulfides, Am. J.
Sci., 265, 773–785, https://doi.org/10.2475/ajs.265.9.773, 1967.
Berner, R. A.: A new geochemical classification of sedimentary environments,
J. Sediment. Res., 51, 359–365,
https://doi.org/10.1306/212F7C7F-2B24-11D7-8648000102C1865D, 1981.
Borowski, W. S., Paull, C. K., and Ussler III, W.: Marine pore-water sulfate
profiles indicate in situ methane flux from underlying gas hydrate, Geology,
24, 655–658, https://doi.org/10.1130/0091-7613(1996)024<0655:MPWSPI>2.3.CO;2,
1996.
Borowski, W. S., Rodriguez, N. M., Paull, C. K., and Ussler III, W.: Are
34S-enriched authigenic sulfide minerals a proxy for elevated methane flux
and gas hydrates in the geologic record?, Mar. Pet. Geol., 43, 381–395,
https://doi.org/10.1016/j.marpetgeo.2012.12.009, 2013.
Burns, S.: Early diagenesis in Amazon fan sediments, in: Proc. ODP Sci.
Results, edited by: Flood, R. D., Piper, D. J. W., Klaus, A., and Peterson,
L. C., Texas, USA, 497–504, 1997.
Cai, C., Leu, A. O., Xie, G.-J., Guo, J., Feng, Y., Zhao, J.-X., Tyson, G.
W., Yuan, Z., and Hu, S.: A methanotrophic archaeon couples anaerobic
oxidation of methane to Fe(III) reduction, The ISME Journal, 12, 1929–1939,
https://doi.org/10.1038/s41396-018-0109-x, 2018.
Canfield, D. E.: Reactive iron in marine sediments, Geochim. Cosmochim. Ac.,
53, 619–632, https://doi.org/10.1016/0016-7037(89)90005-7, 1989.
Canfield, D. E., Raiswell, R., and Bottrell, S. H.: The reactivity of
sedimentary iron minerals toward sulfide, Am. J. Sci., 292, 659–683,
https://doi.org/10.2475/ajs.292.9.659, 1992.
Clemens, S. C., Kuhnt, W., LeVay, L. J., and the Expedition 353 Scientists:
Indian Monsoon Rainfall, Proceedings of the International Ocean Discovery
Program, 29 November 2014–29 January 2015, 353, College Station, Texas, USA,
https://doi.org/10.14379/iodp.proc.353.2016, 2016.
Crowe, S., Katsev, S., Leslie, K., Sturm, A., Magen, C., Nomosatryo, S.,
Pack, M., Kessler, J., Reeburgh, W., and Roberts, J.: The methane cycle in
ferruginous Lake Matano, Geobiology, 9, 61–78,
https://doi.org/10.1111/j.1472-4669.2010.00257.x, 2011.
Delaney, M.: Phosphorus accumulation in marine sediments and the oceanic
phosphorus cycle, Global Biogeochem. Cy., 12, 563–572,
https://doi.org/10.1029/98GB02263, 1998.
Dijkstra, N., Kraal, P., Kuypers, M. M., Schnetger, B., and Slomp, C. P.: Are
iron-phosphate minerals a sink for phosphorus in anoxic Black Sea sediments?,
PloS one, 9, e101139, https://doi.org/10.1371/journal.pone.0101139, 2014.
Dijkstra, N., Slomp, C. P., and Behrends, T.: Vivianite is a key sink for
phosphorus in sediments of the Landsort Deep, an intermittently anoxic deep
basin in the Baltic Sea, Chem. Geol., 438, 58–72,
https://doi.org/10.1016/j.chemgeo.2016.05.025, 2016.
Dijkstra, N., Hagens, M., Egger, M., and Slomp, C. P.: Post-depositional
formation of vivianite-type minerals alters sediment phosphorus records,
Biogeosciences, 15, 861–883, https://doi.org/10.5194/bg-15-861-2018, 2018a.
Dijkstra, N., Krupinski, N. B. Q., Yamane, M., Obrochta, S. P., Miyairi, Y.,
Yokoyama, Y., and Slomp, C. P.: Holocene refreshening and reoxygenation of a
Bothnian Sea estuary led to enhanced phosphorus burial, Estuar. Coast., 41,
139–157, https://doi.org/10.1007/s12237-017-0262-x, 2018b.
Egger, M., Jilbert, T., Behrends, T., Rivard, C., and Slomp, C. P.: Vivianite
is a major sink for phosphorus in methanogenic coastal surface sediments,
Geochim. Cosmochim. Ac., 169, 217–235, https://doi.org/10.1016/j.gca.2015.09.012, 2015a.
Egger, M., Rasigraf, O., Sapart, C. J., Jilbert, T., Jetten, M. S.,
Röckmann, T., van der Veen, C., Bândǎ, N., Kartal, B., and
Ettwig, K. F.: Iron-mediated anaerobic oxidation of methane in brackish
coastal sediments, Environ. Sci. Technol., 49, 277–283,
https://doi.org/10.1021/es503663z, 2015b.
Egger, M., Kraal, P., Jilbert, T., Sulu-Gambari, F., Sapart, C. J.,
Röckmann, T., and Slomp, C. P.: Anaerobic oxidation of methane alters
sediment records of sulfur, iron and phosphorus in the Black Sea,
Biogeosciences, 13, 5333–5355, https://doi.org/10.5194/bg-13-5333-2016,
2016.
Egger, M., Hagens, M., Sapart, C. J., Dijkstra, N., van Helmond, N. A.,
Mogollón, J. M., Risgaard-Petersen, N., van der Veen, C., Kasten, S., and
Riedinger, N.: Iron oxide reduction in methane-rich deep Baltic Sea
sediments, Geochim. Cosmochim. Ac., 207, 256–276,
https://doi.org/10.1016/j.gca.2017.03.019, 2017.
Egger, M., Riedinger, N., Mogollón, J. M., and Jørgensen, B. B.:
Global diffusive fluxes of methane in marine sediments, Nat. Geosci., 11,
421–425, https://doi.org/10.1038/s41561-018-0122-8, 2018.
Ettwig, K. F., Zhu, B., Speth, D., Keltjens, J. T., Jetten, M. S., and
Kartal, B.: Archaea catalyze iron-dependent anaerobic oxidation of methane,
P. Natl. Acad. Sci. USA, 113, 12792–12796, https://doi.org/10.1073/pnas.1609534113,
2016.
Fagel, N., Alleman, L., Granina, L., Hatert, F., Thamo-Bozso, E., Cloots, R.,
and André, L.: Vivianite formation and distribution in Lake Baikal
sediments, Global Planet. Change, 46, 315–336,
https://doi.org/10.1016/j.gloplacha.2004.09.022, 2005.
Feng, D. and Chen, D.: Authigenic carbonates from an active cold seep of the
northern South China Sea: new insights into fluid sources and past seepage
activity, Deep-Sea Res. Pt. II, 122, 74–83, https://doi.org/10.1016/j.dsr2.2015.02.003,
2015.
Feng, D., Cheng, M., Kiel, S., Qiu, J.-W., Yang, Q., Zhou, H., Peng, Y., and
Chen, D.: Using Bathymodiolus tissue stable carbon, nitrogen and sulfur
isotopes to infer biogeochemical process at a cold seep in the South China
Sea, Deep-Sea Res. Pt. I, 104, 52–59, https://doi.org/10.1016/j.dsr.2015.06.011, 2015.
Feng, D., Qiu, J.-W., Hu, Y., Peckmann, J., Guan, H., Tong, H., Chen, C.,
Chen, J., Gong, S., Li, N., and Chen, D.: Cold seep systems in the South
China Sea: An overview, J. Asian Earth Sci.,
https://doi.org/10.1016/j.jseaes.2018.09.021, online first, 2018.
Grizelj, A., Bakrač, K., Horvat, M., Avanić, R., and
Hećimović, I.: Occurrence of vivianite in alluvial Quaternary
sediments in the area of Sesvete (Zagreb, Croatia), Geol. Croat., 70, 41–52,
https://doi.org/10.4154/gc.2017.01, 2017.
Habicht, K. S., Gade, M., Thamdrup, B., Berg, P., and Canfield, D. E.:
Calibration of Sulfate Levels in the Archean Ocean, Science, 298, 2372–2374,
https://doi.org/10.1126/science.1078265, 2002.
Haese, R. R., Wallmann, K., Dahmke, A., Kretzmann, U., Müller, P. J., and
Schulz, H. D.: Iron species determination to investigate early diagenetic
reactivity in marine sediments, Geochim. Cosmochim. Ac., 61, 63–72,
https://doi.org/10.1016/S0016-7037(96)00312-2, 1997.
Han, X., Suess, E., Huang, Y., Wu, N., Bohrmann, G., Su, X., Eisenhauer, A.,
Rehder, G., and Fang, Y.: Jiulong methane reef: microbial mediation of seep
carbonates in the South China Sea, Mar. Geol., 249, 243–256,
https://doi.org/10.1016/j.margeo.2007.11.012, 2008.
Holmkvist, L., Ferdelman, T. G., and Jørgensen, B. B.: A cryptic sulfur
cycle driven by iron in the methane zone of marine sediment (Aarhus Bay,
Denmark), Geochim. Cosmochim. Ac., 75, 3581–3599,
https://doi.org/10.1016/j.gca.2011.03.033, 2011.
Holmkvist, L., Kamyshny Jr, A., Bruechert, V., Ferdelman, T. G., and
Jørgensen, B. B.: Sulfidization of lacustrine glacial clay upon Holocene
marine transgression (Arkona Basin, Baltic Sea), Geochim. Cosmochim. Ac.,
142, 75–94, https://doi.org/10.1016/j.gca.2014.07.030, 2014.
Hsu, H.-H., Liu, C.-S., Morita, S., Tu, S.-L., Lin, S., Machiyama, H., Azuma,
W., Ku, C.-Y., and Chen, S.-C.: Seismic imaging of the Formosa Ridge cold
seep site offshore of southwestern Taiwan, Mar. Geophys. Res., 1–13,
https://doi.org/10.1007/s11001-017-9339-y, 2017.
Hsu, T.-W., Jiang, W.-T., and Wang, Y.: Authigenesis of vivianite as
influenced by methane-induced sulfidization in cold-seep sediments off
southwestern Taiwan, J. Asian Earth Sci., 89, 88–97,
https://doi.org/10.1016/j.jseaes.2014.03.027, 2014.
Hu, Y., Feng, D., Liang, Q., Xia, Z., Chen, L., and Chen, D.: Impact of
anaerobic oxidation of methane on the geochemical cycle of redox-sensitive
elements at cold-seep sites of the northern South China Sea, Deep-Sea Res.
Pt. II, 122, 84-94, https://doi.org/10.1016/j.dsr2.2015.06.012, 2015.
Izon, G., Zerkle, A. L., Zhelezinskaia, I., Farquhar, J., Newton, R. J.,
Poulton, S. W., Eigenbrode, J. L., and Claire, M. W.: Multiple oscillations
in Neoarchaean atmospheric chemistry, Earth. Planet. Sc. Lett., 431,
264–273, https://doi.org/10.1016/j.epsl.2015.09.018, 2015.
Izon, G., Zerkle, A. L., Williford, K. H., Farquhar, J., Poulton, S. W., and
Claire, M. W.: Biological regulation of atmospheric chemistry en route to
planetary oxygenation, P. Natl. Acad. Sci. USA, 114, E2571–E2579,
https://doi.org/10.1073/pnas.1618798114, 2017.
Jensen, H. S., Mortensen, P. B., Andersen, F., Rasmussen, E., and Jensen, A.:
Phosphorus cycling in a coastal marine sediment, Aarhus Bay, Denmark, Limnol.
Oceanogr., 40, 908–917, https://doi.org/10.4319/lo.1995.40.5.0908, 1995.
Jørgensen, B. B., Böttcher, M. E., Lüschen, H., Neretin, L. N.,
and Volkov, I. I.: Anaerobic methane oxidation and a deep H2S sink generate
isotopically heavy sulfides in Black Sea sediments, Geochim. Cosmochim. Ac.,
68, 2095–2118, https://doi.org/10.1016/j.gca.2003.07.017, 2004.
Kagan, M. R. and McCreery, R. L.: Reduction of fluorescence interference in
Raman spectroscopy via analyte adsorption on graphitic carbon, Anal. Chem.,
66, 4159–4165, https://doi.org/10.1021/ac00095a008, 1994.
Kasten, S., Freudenthal, T., Gingele, F. X., and Schulz, H. D.: Simultaneous
formation of iron-rich layers at different redox boundaries in sediments of
the Amazon deep-sea fan, Geochim. Cosmochim. Ac., 62, 2253–2264,
https://doi.org/10.1016/S0016-7037(98)00093-3, 1998.
Kasting, J. F., Pavlov, A. A., and Siefert, J. L.: A Coupled
Ecosystem-Climate Model for Predicting the Methane Concentration in the
Archean Atmosphere, Origins Life Evol. Biosphere, 31, 271–285,
https://doi.org/10.1023/a:1010600401718, 2001.
Kennett, J. P., Cannariato, K. G., Hendy, I. L., and Behl, R. J.: Methane
Hydrates in Quaternary Climate Change: The Clathrate Gun Hypothesis, American
Geophysical Union, Washington, DC, USA, 2003.
Klein, C.: Some Precambrian banded iron-formations (BIFs) from around the
world: Their age, geologic setting, mineralogy, metamorphism, geochemistry,
and origins, Am. Mineral., 90, 1473–1499, https://doi.org/10.2138/am.2005.1871, 2005.
Knittel, K. and Boetius, A.: Anaerobic oxidation of methane: progress with an
unknown process, Annu. Rev. Microbiol., 63, 311–334,
https://doi.org/10.1146/annurev.micro.61.080706.093130, 2009.
Konhauser, K. O., Hamade, T., Raiswell, R., Morris, R. C., Ferris, F. G.,
Southam, G., and Canfield, D. E.: Could bacteria have formed the Precambrian
banded iron formations?, Geology, 30, 1079–1082,
https://doi.org/10.1130/0091-7613(2002)030<1079:CBHFTP>2.0.CO;2, 2002.
Kvenvolden, K. A.: Gas hydrates–geological perspective and global change,
Rev. Geophys., 31, 173–187, https://doi.org/10.1029/93RG00268 1993.
Lin, Q., Wang, J., Fu, S., Lu, H., Bu, Q., Lin, R., and Sun, F.: Elemental
sulfur in northern South China Sea sediments and its significance, Sci. China
Earth Sci., 58, 2271–2278, https://doi.org/10.1007/s11430-015-5182-7, 2015.
Lin, Q., Wang, J., Algeo, T. J., Sun, F., and Lin, R.: Enhanced framboidal
pyrite formation related to anaerobic oxidation of methane in the
sulfate-methane transition zone of the northern South China Sea, Mar. Geol.,
379, 100–108, https://doi.org/10.1016/j.margeo.2016.05.016, 2016.
Lin, R., Wang, J., Su, P., Lin, Q., Sun, F., and Yang, J.: Characteristics of
magnetic susceptibility of cored sediments and their implications for the
potential methane events in northern South China Sea, Acta Sedimentologica
Sinica, 35, 290–298, https://doi.org/10.14027/j.cnki.cjxb.2017.02.008, 2017.
Lin, Z., Sun, X., Peckmann, J., Lu, Y., Xu, L., Strauss, H., Zhou, H., Gong,
J., Lu, H., and Teichert, B. M. A.: How sulfate-driven anaerobic oxidation of
methane affects the sulfur isotopic composition of pyrite: A SIMS study from
the South China Sea, Chem. Geol., 440, 26–41,
https://doi.org/10.1016/j.chemgeo.2016.07.007, 2016.
Lin, Z., Sun, X., Strauss, H., Lu, Y., Gong, J., Xu, L., Lu, H., Teichert, B.
M., and Peckmann, J.: Multiple sulfur isotope constraints on sulfate-driven
anaerobic oxidation of methane: Evidence from authigenic pyrite in seepage
areas of the South China Sea, Geochim. Cosmochim. Ac., 211, 153–173,
https://doi.org/10.1016/j.gca.2017.05.015, 2017.
Liu, C.-S., Huang, I. L., and Teng, L. S.: Structural features off
southwestern Taiwan, Mar. Geol., 137, 305–319,
https://doi.org/10.1016/S0025-3227(96)00093-X, 1997.
Lovley, D. R.: Microbial Fe (III) reduction in subsurface environments, FEMS
Microbiol. Rev., 20, 305–313, https://doi.org/10.1111/j.1574-6976.1997.tb00316.x, 1997.
Lu, H., Liu, J., Chen, F., Cheng, S., and Liao, Z.: Shallow sulfate-methane
interface in northeastern South China Sea: An indicator of strong methane
seepage on seafloor, Mar Geol Quat Geol, 32, 93–98,
https://doi.org/10.3724/SP.J.1140.2012.01093, 2012.
Luo, G., Ono, S., Beukes, N. J., Wang, D. T., Xie, S., and Summons, R. E.:
Rapid oxygenation of Earth's atmosphere 2.33 billion years ago, Science
Advances, 2, e1600134, https://doi.org/10.1126/sciadv.1600134, 2016.
Lyons, T. W., Reinhard, C. T., and Planavsky, N. J.: The rise of oxygen in
Earth's early ocean and atmosphere, Nature, 506, 307–315,
https://doi.org/10.1038/nature13068, 2014.
März, C., Hoffmann, J., Bleil, U., De Lange, G., and Kasten, S.:
Diagenetic changes of magnetic and geochemical signals by anaerobic methane
oxidation in sediments of the Zambezi deep-sea fan (SW Indian Ocean), Mar.
Geol., 255, 118–130, https://doi.org/10.1016/j.margeo.2008.05.013, 2008a.
März, C., Poulton, S. W., Beckmann, B., Küster, K., Wagner, T., and
Kasten, S.: Redox sensitivity of P cycling during marine black shale
formation: Dynamics of sulfidic and anoxic, non-sulfidic bottom waters,
Geochim. Cosmochim. Ac., 72, 3703–3717, https://doi.org/10.1016/j.gca.2008.04.025,
2008b.
März, C., Riedinger, N., Sena, C., and Kasten, S.: Phosphorus dynamics
around the sulphate-methane transition in continental margin sediments:
Authigenic apatite and Fe(II) phosphates, Mar. Geol., 404, 84–96,
https://doi.org/10.1016/j.margeo.2018.07.010, 2018.
Maslin, M., Owen, M., Day, S., and Long, D.: Linking continental-slope
failures and climate change: Testing the clathrate gun hypothesis, Geology,
32, 53–56, https://doi.org/10.1130/G20114.1, 2004.
McDonnell, S., Max, M., Cherkis, N. E. A., and Czarnecki, M.:
Tectono-sedimentary controls on the likelihood of gas hydrate occurrence near
Taiwan, Mar. Pet. Geol., 17, 929–936, https://doi.org/10.1016/S0264-8172(00)00023-4,
2000.
McGlynn, S. E., Chadwick, G. L., Kempes, C. P., and Orphan, V. J.: Single
cell activity reveals direct electron transfer in methanotrophic consortia,
Nature, 526, 531–535, https://doi.org/10.1038/nature15512, 2015.
Morse, J. W.: Interactions of trace metals with authigenic sulfide minerals:
implications for their bioavailability, Mar. Chem., 46, 1–6,
https://doi.org/10.1016/0304-4203(94)90040-X, 1994.
Nakano, S.: Manganoan vivianite in the bottom sediments of Lake Biwa, Japan,
Mineral. J., 16, 96–107, https://doi.org/10.2465/minerj.16.96, 1992.
Nembrini, G., Capobianco, J., Viel, M., and Williams, A.: A Mössbauer and
chemical study of the formation of vivianite in sediments of Lago Maggiore
(Italy), Geochim. Cosmochim. Ac., 47, 1459–1464,
https://doi.org/10.1016/0016-7037(83)90304-6, 1983.
Norði, K. à., Thamdrup, B., and Schubert, C. J.: Anaerobic oxidation
of methane in an iron-rich Danish freshwater lake sediment, Limnol.
Oceanogr., 58, 546–554, https://doi.org/10.4319/lo.2013.58.2.0546, 2013.
Nriagu, J. O.: Stability of vivianite and ion-pair formation in the system
Ou, W.: Sedimentary organic geochemistry research of source rocks of the
potential gas hydrate-bearing areas in the northern South China Sea, PhD
thesis, Xiamen University, China, 2013.
Peckmann, J. and Thiel, V.: Carbon cycling at ancient methane–seeps, Chem.
Geol., 205, 443–467, https://doi.org/10.1016/j.chemgeo.2003.12.025, 2004.
Piriou, B. and Poullen, J.: Raman study of vivianite, J. Raman Spectrosc.,
15, 343–346, https://doi.org/10.1002/jrs.1250150510, 1984.
Porrenga, D. H.: Glauconite and chamosite as depth indicators in the marine
environment, Mar. Geol., 5, 495–501, https://doi.org/10.1016/0025-3227(67)90056-4, 1967.
Poulton, S. W.: Early phosphorus redigested, Nat. Geosci., 10, 75–76,
https://doi.org/10.1038/ngeo2884, 2017.
Poulton, S. W. and Canfield, D. E.: Development of a sequential extraction
procedure for iron: implications for iron partitioning in continentally
derived particulates, Chem. Geol., 214, 209–221,
https://doi.org/10.1016/j.chemgeo.2004.09.003, 2005.
Poulton, S. W. and Canfield, D. E.: Ferruginous Conditions: A Dominant
Feature of the Ocean through Earth's History, Elements, 7, 107–112,
https://doi.org/10.2113/gselements.7.2.107, 2011.
Poulton, S. W., Krom, M. D. and Raiswell, R.: A revised scheme for the
reactivity of iron (oxyhydr) oxide minerals towards dissolved sulfide,
Geochim. Cosmochim. Ac., 68, 3703–3715, https://doi.org/10.1016/j.gca.2004.03.012, 2004.
Raiswell, R., Canfield, D., and Berner, R.: A comparison of iron extraction
methods for the determination of degree of pyritisation and the recognition
of iron-limited pyrite formation, Chem. Geol., 111, 101–110,
https://doi.org/10.1016/0009-2541(94)90084-1, 1994.
Reed, D. C., Gustafsson, B. G., and Slomp, C. P.: Shelf-to-basin iron
shuttling enhances vivianite formation in deep Baltic Sea sediments, Earth.
Planet. Sc. Lett., 434, 241–251, https://doi.org/10.1016/j.epsl.2015.11.033, 2016.
Reinhard, C. T., Planavsky, N. J., Gill, B. C., Ozaki, K., Robbins, L. J.,
Lyons, T. W., Fischer, W. W., Wang, C., Cole, D. B., and Konhauser, K. O.:
Evolution of the global phosphorus cycle, Nature, 541, 386–389,
https://doi.org/10.1038/nature20772, 2017.
Riedinger, N., Formolo, M. J., Lyons, T. W., Henkel, S., Beck, A., and
Kasten, S.: An inorganic geochemical argument for coupled anaerobic oxidation
of methane and iron reduction in marine sediments, Geobiology, 12, 172–181,
https://doi.org/10.1111/gbi.12077, 2014.
Riedinger, N., Brunner, B., Krastel, S., Arnold, G. L., Wehrmann, L. M.,
Formolo, M. J., Beck, A., Bates, S. M., Henkel, S., and Kasten, S.: Sulfur
cycling in an iron oxide-dominated, dynamic marine depositional system: The
Argentine continental margin, Front. Earth Sci., 5, 33 pp.,
https://doi.org/10.3389/feart.2017.00033, 2017.
Rodgers, K. A.: Metavivianite and kerchenite: a review, Mineral. Mag., 50,
687–691, https://doi.org/10.1180/minmag.1986.050.358.16, 1986.
Rooze, J., Egger, M., Tsandev, I., and Slomp, C. P.: Iron-dependent anaerobic
oxidation of methane in coastal surface sediments: Potential controls and
impact, Limnol. Oceanogr., 61, S267–S282, https://doi.org/10.1002/lno.10275, 2016.
Rotaru, A.-E. and Thamdrup, B.: A new diet for methane oxidizers, Science,
351, 658–658, https://doi.org/10.1126/science.aaf0741, 2016.
Rothe, M., Frederichs, T., Eder, M., Kleeberg, A., and Hupfer, M.: Evidence
for vivianite formation and its contribution to long-term phosphorus
retention in a recent lake sediment: a novel analytical approach,
Biogeosciences, 11, 5169–5180, https://doi.org/10.5194/bg-11-5169-2014,
2014.
Rothe, M., Kleeberg, A., Grüneberg, B., Friese, K., Pérez-Mayo, M.,
and Hupfer, M.: Sedimentary sulphur: iron ratio indicates vivianite
occurrence: a study from two contrasting freshwater systems, Plos one, 10,
e0143737, https://doi.org/10.1371/journal.pone.0143737, 2015.
Rothe, M., Kleeberg, A., and Hupfer, M.: The occurrence, identification and
environmental relevance of vivianite in waterlogged soils and aquatic
sediments, Earth-Sci. Rev., 158, 51–64, https://doi.org/10.1016/j.earscirev.2016.04.008,
2016.
Ruppel, C. D. and Kessler, J. D.: The interaction of climate change and
methane hydrates, Rev. Geophys., 55, 126–168, https://doi.org/10.1002/2016RG000534,
2017.
Ruttenberg, K. C.: Development of a sequential extraction method for
different forms of phosphorus in marine sediments, Limnol. Oceanogr., 37,
1460–1482, https://doi.org/10.4319/lo.1992.37.7.1460, 1992.
Ruttenberg, K. C.: The Global Phosphorus Cycle, in: Treatise on Geochemistry,
2nd edn., edited by: Turekian, K. K., Elsevier, Oxford, 499–558, 2014.
Ruttenberg, K. C. and Berner, R. A.: Authigenic apatite formation and burial
in sediments from non-upwelling, continental margin environments, Geochim.
Cosmochim. Ac., 57, 991–1007, https://doi.org/10.1016/0016-7037(93)90035-U, 1993.
Sapota, T., Aldahan, A., and Al-Aasm, I. S.: Sedimentary facies and climate
control on formation of vivianite and siderite microconcretions in sediments
of Lake Baikal, Siberia, J. Paleolimnol., 36, 245–257,
https://doi.org/10.1007/s10933-006-9005-x, 2006.
Scheller, S., Yu, H., Chadwick, G. L., McGlynn, S. E., and Orphan, V. J.:
Artificial electron acceptors decouple archaeal methane oxidation from
sulfate reduction, Science, 351, 703–707, https://doi.org/10.1126/science.aad7154, 2016.
Schulz, H. D., Dahmke, A., Schinzel, U., Wallmann, K., and Zabel, M.: Early
diagenetic processes, fluxes, and reaction rates in sediments of the South
Atlantic, Geochim. Cosmochim. Ac., 58, 2041–2060,
https://doi.org/10.1016/0016-7037(94)90284-4, 1994.
Segarra, K. E., Comerford, C., Slaughter, J., and Joye, S. B.: Impact of
electron acceptor availability on the anaerobic oxidation of methane in
coastal freshwater and brackish wetland sediments, Geochim. Cosmochim. Ac.,
115, 15–30, https://doi.org/10.1016/j.gca.2013.03.029, 2013.
Severmann, S., Johnson, C. M., Beard, B. L., and McManus, J.: The effect of
early diagenesis on the Fe isotope compositions of porewaters and authigenic
minerals in continental margin sediments, Geochim. Cosmochim. Ac., 70,
2006–2022, https://doi.org/10.1016/j.gca.2006.01.007, 2006.
Sha, Z., Liang, J., Zhang, G., Yang, S., Lu, J., Zhang, Z., McConnell, D. R.,
and Humphrey, G.: A seepage gas hydrate system in northern South China Sea:
Seismic and well log interpretations, Mar. Geol., 366, 69–78,
https://doi.org/10.1016/j.margeo.2015.04.006, 2015.
Shi, C., Lei, H., Zhao, J., Zhang, J., and Han, C.: Vertical microbial
community structure characteristics of sediment in gas hydrate potential area
of northern South China Sea Jiulong Methane Reef, Acta Sedimentol. Sinica,
32, 1072–1082, 2014.
Sivan, O., Adler, M., Pearson, A., Gelman, F., Bar-Or, I., John, S. G., and
Eckert, W.: Geochemical evidence for iron-mediated anaerobic oxidation of
methane, Limnol. Oceanogr., 56, 1536–1544, https://doi.org/10.4319/lo.2011.56.4.1536,
2011.
Slomp, C. P., Epping, E. H., Helder, W., and Raaphorst, W. V.: A key role for
iron-bound phosphorus in authigenic apatite formation in North Atlantic
continental platform sediments, J. Mar. Res., 54, 1179–1205,
https://doi.org/10.1357/0022240963213745, 1996.
Slomp, C. P., Mort, H. P., Jilbert, T., Reed, D. C., Gustafsson, B. G., and
Wolthers, M.: Coupled dynamics of iron and phosphorus in sediments of an
oligotrophic coastal basin and the impact of anaerobic oxidation of methane,
PloS one, 8, e62386, https://doi.org/10.1371/journal.pone.0062386, 2013.
Suess, E., Huang, Y., Wu, N., Han, X., and Su, X.: South China Sea
continental margin: Geological methane budget and environmental effects of
methane emissions and gas hydrates, RV SONNE Cruise Report, Leibniz Institute
of Marine Sciences, Kiel, Germany, 154 pp., 2005.
Sundby, B., Gobeil, C., Silverberg, N., and Alfonso, M.: The phosphorus cycle
in coastal marine sediments, Limnol. Oceanogr., 37, 1129–1145,
https://doi.org/10.4319/lo.1992.37.6.1129, 1992.
Tenzer, R. and Gladkikh, V.: Assessment of density variations of marine
sediments with ocean and sediment depths, Sci. World J., 2014, 823296,
https://doi.org/10.1155/2014/823296, 2014.
Treude, T., Niggemann, J., Kallmeyer, J., Wintersteller, P., Schubert, C. J.,
Boetius, A., and Jørgensen, B. B.: Anaerobic oxidation of methane and
sulfate reduction along the Chilean continental margin, Geochim. Cosmochim.
Ac., 69, 2767–2779, https://doi.org/10.1016/j.gca.2005.01.002, 2005.
Treude, T., Krause, S., Maltby, J., Dale, A. W., Coffin, R., and Hamdan, L.
J.: Sulfate reduction and methane oxidation activity below the
sulfate-methane transition zone in Alaskan Beaufort Sea continental margin
sediments: Implications for deep sulfur cycling, Geochim. Cosmochim. Ac.,
144, 217–237, https://doi.org/10.1016/j.gca.2014.08.018, 2014.
Wallmann, K., Hennies, K., König, I., Petersen, W., and Knauth, H.-D.:
New procedure for determining reactive Fe(III) and Fe(II) minerals in
sediments, Limnol. Oceanogr., 38, 1803–1812, https://doi.org/10.4319/lo.1993.38.8.1803,
1993.
Wankel, S. D., Adams, M. M., Johnston, D. T., Hansel, C. M., Joye, S. B., and
Girguis, P. R.: Anaerobic methane oxidation in metalliferous hydrothermal
sediments: influence on carbon flux and decoupling from sulfate reduction,
Environ. Microbiol., 14, 2726–2740, https://doi.org/10.1111/j.1462-2920.2012.02825.x,
2012.
Wegener, G., Krukenberg, V., Riedel, D., Tegetmeyer, H. E., and Boetius, A.:
Intercellular wiring enables electron transfer between methanotrophic archaea
and bacteria, Nature, 526, 587–590, https://doi.org/10.1038/nature15733, 2015.
Yan, Z., Joshi, P., Gorski, C. A., and Ferry, J. G.: A biochemical framework
for anaerobic oxidation of methane driven by Fe (III)-dependent respiration,
Nat. Commun., 9, 1642, https://doi.org/10.1038/s41467-018-04097-9, 2018.
Ye, H., Yang, T., Zhu, G., Jiang, S., and Wu, L.: Pore water geochemistry in
shallow sediments from the northeastern continental slope of the South China
Sea, Mar. Pet. Geol., 75, 68–82, https://doi.org/10.1016/j.marpetgeo.2016.03.010, 2016.
Zhang, B., Wu, D., and Wu, N.: Characteristics of sedimentary geochemistry
and their responses to cold-seep activities in Dongsha, the northern South
China Sea, Mar. Geol. Front., 31, 14–27, 2015.
Zhang, B., Pan, M., Wu, D., and Wu, N.: Distribution and isotopic composition
of foraminifera at cold-seep Site 973-4 in the Dongsha area, northeastern
South China Sea, J. Asian Earth Sci., https://doi.org/10.1016/j.jseaes.2018.05.007,
online first, 2018.
Zhang, G., Liang, J., Lu, J., Yang, S., Zhang, M., Holland, M.,
Schultheiss, P., Su, X., Sha, Z., and Xu, H.: Geological features,
controlling factors and potential prospects of the gas hydrate occurrence in
the east part of the Pearl River Mouth Basin, South China Sea, Mar. Pet.
Geol., 67, 356–367, https://doi.org/10.1016/j.marpetgeo.2015.05.021, 2015.
Zhang, J., Lei, H., Ou, W., Yang, Y., Gong, C., and Shi, C.: Research of the
sulfate-methane transition zone (SMTZ) in sediments of 973-4 column in
continental slope of northern South China Sea, Nat. Gas Geosci., 25,
1811–1820, https://doi.org/10.11764/j.issn.1672-1926.2014.11.1811, 2014.
Zhang, J., Lei, H., Yang, M., Chen, Y., Kong, Y., and Lu, Y.: The
Interactions of P-S-Fe in sediment from the continental slope of northern
South China Sea and their implication for the sulfate – methane transition
zone, Earth Sci. Front., 25, 285–293, https://doi.org/10.13745/j.esf.sf.2018.2.2, 2018a.
Zhang, J., Lei, H., Chen, Y., Kong, Y., Kandasamy, S., Ou, W., and Cheng, W.:
Carbon and oxygen isotope composition of carbonate in bulk sediment in the
southwest Taiwan Basin, south China sea: Methane hydrate decomposition
history and its link to mud volcano eruption, Mar. Pet. Geol., 98, 687–696,
https://doi.org/10.1016/j.marpetgeo.2018.08.031, 2018b.
Zhang, Z., Li, C., Cheng, M., Algeo, T. J., Jin, C., Tang, F., and Huang, J.:
Evidence for Highly Complex Redox Conditions and Strong Water-Column
Stratification in an Early Cambrian Continental-Margin Sea, Geochem. Geophys.
Geosyst., 19, 2397–2410, https://doi.org/10.1029/2018GC007666, 2018.
Zhong, G., Cartigny, M. J., Kuang, Z., and Wang, L.: Cyclic steps along the
South Taiwan Shoal and West Penghu submarine canyons on the northeastern
continental slope of the South China Sea, GSA Bulletin, 127, 804–824,
https://doi.org/10.1130/B31003.1, 2015.
Zhuang, C., Chen, F., Cheng, S., Lu, H., Zhou, Y., and Liu, G.: Stable
isotopic characteristics and their influencing factors of benthic
foraminifera in the prospective gas hydrate area from the northern South
China Sea since the last glacial, Quaternary Sci., 35, 422–432,
https://doi.org/10.11928/j.issn.1001-7410.2015.02.17, 2015.
Short summary
Our work provides new insights into the biogeochemical cycling of iron, methane and phosphorus. We found that vivianite, an iron-phosphate mineral, is pervasive in methane-rich sediments, suggesting that iron reduction at depth is coupled to phosphorus and methane cycling on a much greater spatial scale than previously assumed. Acting as an important burial mechanism for iron and phosphorus, vivianite authigenesis may be an under-considered process in both modern and ancient settings alike.
Our work provides new insights into the biogeochemical cycling of iron, methane and phosphorus....
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