Articles | Volume 15, issue 24
https://doi.org/10.5194/bg-15-7451-2018
© 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-15-7451-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
21 Dec 2018
Research article |
| 21 Dec 2018
| 21 Dec 2018
Hydrothermal alteration of aragonitic biocarbonates: assessment of micro- and nanostructural dissolution–reprecipitation and constraints of diagenetic overprint from quantitative statistical grain-area analysis
Laura A. Casella
CORRESPONDING AUTHOR
Department of Earth and Environmental Sciences and GeoBioCenter,
Ludwig-Maximilians-Universität München, Munich, 80333, Germany
Sixin He
Department of Earth and Environmental Sciences and GeoBioCenter,
Ludwig-Maximilians-Universität München, Munich, 80333, Germany
Erika Griesshaber
Department of Earth and Environmental Sciences and GeoBioCenter,
Ludwig-Maximilians-Universität München, Munich, 80333, Germany
Lourdes Fernández-Díaz
Instituto de Geociencias, Universidad Complutense Madrid (UCM, CSIC),
Madrid, 28040, Spain
Martina Greiner
Department of Earth and Environmental Sciences and GeoBioCenter,
Ludwig-Maximilians-Universität München, Munich, 80333, Germany
Elizabeth M. Harper
Department of Earth Sciences, University of Cambridge, Cambridge, CB2 3EQ, UK
Daniel J. Jackson
Department of Geobiology, Georg-August University of Göttingen,
Göttingen, 37077, Germany
Andreas Ziegler
Central Facility for Electron Microscopy, University of Ulm, Ulm,
89081, Germany
Vasileios Mavromatis
Institute of Applied Geosciences, Graz University of Technology,
Rechbauerstr. 12, 8010 Graz, Austria
Martin Dietzel
Institute of Applied Geosciences, Graz University of Technology,
Rechbauerstr. 12, 8010 Graz, Austria
Anton Eisenhauer
GEOMAR-Helmholtz Centre for Ocean Research, Marine
Biogeochemistry/Marine Geosystems, Kiel, 24148, Germany
Sabino Veintemillas-Verdaguer
Instituto de Ciencia de Materiales de Madrid (ICMM, CSIC), 28049
Madrid, Spain
Uwe Brand
Department of Earth Sciences, Brock University, 1812 Sir Isaac Brock
Way, St. Catharines, Ontario, L2S 3A1, Canada
Wolfgang W. Schmahl
Department of Earth and Environmental Sciences and GeoBioCenter,
Ludwig-Maximilians-Universität München, Munich, 80333, Germany
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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.
Pablo Forjanes, María Simonet Roda, Martina Greiner, Erika Griesshaber, Nelson A. Lagos, Sabino Veintemillas-Verdaguer, José Manuel Astilleros, Lurdes Fernández-Díaz, and Wolfgang W. Schmahl
Biogeosciences, 19, 3791–3823, https://doi.org/10.5194/bg-19-3791-2022, https://doi.org/10.5194/bg-19-3791-2022, 2022
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Aragonitic skeletons are employed to decipher past climate dynamics and environmental change. Unfortunately, the information that these skeletons keep can be destroyed during diagenesis. In this work, we study the first changes undergone by aragonitic skeletons upon hydrothermal alteration. We observe that major changes occur from the very beginning of the alteration, even without mineralogical changes. These results have major implications for the use of these archives to understand the past.
Holly L. Taylor, Isaac J. Kell Duivestein, Juraj Farkas, Martin Dietzel, and Anthony Dosseto
Clim. Past, 15, 635–646, https://doi.org/10.5194/cp-15-635-2019, https://doi.org/10.5194/cp-15-635-2019, 2019
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Approximately 600 million years ago, major environmental changes set the course for the emergence of animal life. Lithium (Li) isotopes in calcium carbonates can be used as a proxy to understand changes in the palaeo-environment. We conducted experiments that allow us to use Li isotopes in dolostones to extend our understanding of palaeo-environmental changes deeper into the geological record, where other calcium carbonates archives are not present.
Facheng Ye, Hana Jurikova, Lucia Angiolini, Uwe Brand, Gaia Crippa, Daniela Henkel, Jürgen Laudien, Claas Hiebenthal, and Danijela Šmajgl
Biogeosciences, 16, 617–642, https://doi.org/10.5194/bg-16-617-2019, https://doi.org/10.5194/bg-16-617-2019, 2019
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
Short summary
Short summary
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.
N. Glock, V. Liebetrau, and A. Eisenhauer
Biogeosciences, 11, 7077–7095, https://doi.org/10.5194/bg-11-7077-2014, https://doi.org/10.5194/bg-11-7077-2014, 2014
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Our study explores the correlation of I/Ca ratios in four benthic foraminiferal species (three calcitic, one aragonitic) from the Peruvian OMZ with bottom water oxygenation ([O2]BW), and evaluates foraminiferal I/Ca ratios as a possible redox proxy. All species have a positive trend in the I/Ca ratios as a function of [O2]BW. Only for the aragonitic species Hoeglundina elegans is this trend not significant. The highest significance has been found for Uvigerina striata.
M. Dietzel, A. Leis, R. Abdalla, J. Savarino, S. Morin, M. E. Böttcher, and S. Köhler
Biogeosciences, 11, 3149–3161, https://doi.org/10.5194/bg-11-3149-2014, https://doi.org/10.5194/bg-11-3149-2014, 2014
J. Raddatz, A. Rüggeberg, S. Flögel, E. C. Hathorne, V. Liebetrau, A. Eisenhauer, and W.-Chr. Dullo
Biogeosciences, 11, 1863–1871, https://doi.org/10.5194/bg-11-1863-2014, https://doi.org/10.5194/bg-11-1863-2014, 2014
M. N. Müller, M. Lebrato, U. Riebesell, J. Barcelos e Ramos, K. G. Schulz, S. Blanco-Ameijeiras, S. Sett, A. Eisenhauer, and H. M. Stoll
Biogeosciences, 11, 1065–1075, https://doi.org/10.5194/bg-11-1065-2014, https://doi.org/10.5194/bg-11-1065-2014, 2014
N. Glock, J. Schönfeld, A. Eisenhauer, C. Hensen, J. Mallon, and S. Sommer
Biogeosciences, 10, 4767–4783, https://doi.org/10.5194/bg-10-4767-2013, https://doi.org/10.5194/bg-10-4767-2013, 2013
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Biogeosciences, 19, 763–776, https://doi.org/10.5194/bg-19-763-2022, https://doi.org/10.5194/bg-19-763-2022, 2022
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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
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Microbially produced methane can serve as a carbon source for freshwater macrofauna most likely through grazing on methane-oxidizing bacteria. This study investigates the contributions of different carbon sources to macrofaunal biomass. Our data suggest that the average contribution of methane-derived carbon is similar between different fauna but overall remains low. This is further supported by the low abundance of methane-cycling microorganisms.
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.
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.
Jiarui Liu, Gareth Izon, Jiasheng Wang, Gilad Antler, Zhou Wang, Jie Zhao, and Matthias Egger
Biogeosciences, 15, 6329–6348, https://doi.org/10.5194/bg-15-6329-2018, https://doi.org/10.5194/bg-15-6329-2018, 2018
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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.
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
Addadi, L., Joester, D., Nudelman, F., and Weiner, S.: Mollusk shell
formation: a source of new concepts for understanding biomineralization
processes, Chemistry, 12, 980–987, 2006.
Allison, N., Finch, A. A., Webster, J. M., and Clague, D. A.:
Palaeoenvironmental records from fossil corals: the effects of submarine
diagenesis on temperature and climate estimates, Geochim. Cosmochim. Ac.,
71, 4693–4703, 2007.
Altree-Williams, A., Pring, A., Ngothai, Y., and Brugger, J.: Textural and
compositional complexities resulting from coupled
dissolution-reprecipitation reactions in geomaterials, Earth-Sci. Rev., 150,
628–651, 2015.
Arvidson, R. S. and Morse, J. W.: Formation and diagenesis of carbonate
sediments, in: Treatise on
geochemistry, edited by: Holland H. D. and Turekian K. K., Elsevier, Oxford, 9, 61–101, 2014.
Barthelat, F. and Espinosa, H. D.: An experimental investigation of
deformation and fracture of nacre-mother of pearl, Exp. Mech., 47,
311–324, 2007.
Bathurst, R. G. C.: Carbonate Sediments and their Diagenesis, Elsevier,
Amsterdam, 1975.
Blanchon, P., Eisenhauer, A., Fietzke, J., and Liebetrau, V.: Rapid
sea-level rise and reef back-stepping at the close of the last interglacial
highstand, Nature, 458, 881–884, 2009.
Böhm, F., Gussone, N., Eisenhauer, A., Dullo, W.-C., Reynaud, S., and
Paytan, A.: Calcium isotope fractionation in modern scleractinian corals,
Geochim. Cosmochim. Ac., 70, 4452–4462, 2006.
Brand, U.: Aragonite-calcite transformation based on Pennsylvanian molluscs,
Geol. Soc. Am. Bull., 101, 377–390, 1989.
Brand, U.: Morphochemical and replacement diagenesis of biogenic carbonates,
Dev. Sedimentol., 51, 217–282, 1994.
Brand, U.: Carbon, oxygen and strontium isotopes in Paleozoic carbonate
components: an evaluation of original seawater-chemistry proxies, Chem.
Geol., 204, 23–44, 2004.
Brand, U. and Veizer, J.: Chemical diagenesis of a multicomponent
carbonate-system – 1: trace elements, J. Sed. Petrol., 50, 1219–1236, 1980.
Brand, U. and Veizer, J.: Chemical diagenesis of a multicomponent carbonate
system – 2: stable isotopes, J. Sed. Petrol., 51, 987–997, 1981.
Brown, W. H., Fyfe, W. S., and Turner, F. J.: Aragonite in California
glaucophane schists, and the kinetics of the aragonite-calcite
transformation, J. Petrol., 3, 566–582, 1962.
Butler, P. G., Richardson, C. A., Scourse, J. D., Witbaard, R., Schöne,
B. R., Fraser, N. M., Wanamaker Jr., A. D., Bryant, C. L., Harris, I., and
Robertson, I.: Accurate increment identification and the spatial extent of
the common signal in five Arctica islandica chronologies from the Fladen Ground, northern
North Sea, Paleoceanography, 24, PA2210, https://doi.org/10.1029/2008PA001715, 2009.
Butler, P. G., Wanamaker Jr., A. D., Scourse, J. D., Richardson, C. A., and
Reynolds, D. J.: Variability of marine climate on the North Icelandic Shelf
in a 1,357-year proxy archive based on growth increments in the bivalve
Arctica islandica, Palaeogeogr. Palaeocl., 373, 141–151, 2013.
Cardew, P. T. and Davey, R. J.: The kinetics of solvent-mediated phase
transformations, P. Roy. Soc. Lond. A, 398,
415–428, 1985.
Cartwright, J. H. E. and Checa, A. G.: The dynamics of nacre self-assembly,
J. R. Soc. Interface, 4, 491–504, 2007.
Casella, L. A., Griesshaber, E., Yin, X., Ziegler, A., Mavromatis, V., Müller, D.,
Ritter, A.-C., Hippler, D., Harper, E. M., Dietzel, M., Immenhauser, A., Schöne, B. R.,
Angiolini, L., and Schmahl, W. W.: Experimental diagenesis: insights into aragonite to
calcite transformation of Arctica islandica shells by hydrothermal
treatment, Biogeosciences, 14, 1461–1492, https://doi.org/10.5194/bg-14-1461-2017, 2017.
Casella, L. A., Griesshaber, E., Simonet Roda, M. d. M., Ziegler, A.,
Mavromatis, V., Henkel, D., Laudien, J., Häussermann, V., Neuser, R. D.,
Angiolini, L., Dietzel, M., Eisenhauer, A., Immenhauser, A., Brand, U., and
Schmahl, W. W.: Micro- and nanostrucures reflect the degree of diagenetic
alteration in modern and fossil brachiopod shell calcite: a multi-analytical
screening approach (CL, FE-SEM, AFM, EBSD), Palaeogeogr. Palaeocl., 502, 13–30, 2018a.
Casella, L. A., Simonet Roda, M. D. M., Angiolini, L., Ziegler, A., Schmahl,
W. W., Brand, U., and Griesshaber, E.: Archival biogenic micro- and
nanostructure data analysis: signatures of diagenetic systems, Data In
Brief, 19, 299–311, 2018b.
Checa, A. G., Okamoto, T., and Ramírez, J.: Organization pattern of
nacre in Pteriidae (Bivalvia: Mollusca) explained by crystal competition,
Proc. Biol. Sci., 273, 1329–1337, 2006.
Checa, A. G., Cartwright, J. H. E., and Willinger, M.-G.: The key role of
the surface membrane in why gastropod nacre grows in towers, P. Natl. Am.
Soc., 106, 38–43, 2009.
Checa, A. G., Cartwright, J. H. E., and Willinger, M.-G.: Mineral bridges in
nacre, J. Struct. Biol., 176, 330–339, 2011.
Checa, A. G., Pina, C. M., Osuna-Mascaró, A. J., Rodrígues-Navarro,
A. B., and Harper, E. M.: Crystalline organization of the fibrous prismatic
calcitic layer of the Mediterranean mussel Mytilus galloprovincialis, Eur. J. Mineral., 26, 495–505,
2014.
Cherns, L., Wheeley, J. R., and Wright, V. P.: Taphonomic windows and
molluscan preservation, Palaeogeogr. Palaeocl., 270,
220–229, 2008.
Cohen, A. L., Layne, G. D., and Hart, S. R.: Kinetic control of skeletal
Sr/Ca in a symbiotic coral: implications for the paleotemperature proxy,
Paleoceanography, 16, 20–26, 2001.
Crippa, G. and Raineri, G.: The genera Glycymeris, Aequipecten and Arctica,
and associated mollusk fauna of the Lower Pleistocene Arda River section
(Northern Italy), Riv. Ital. Paleontol. Stratigr., 121, 61–101, 2015.
Crippa, G., Angiolini, L., Bottini, C., Erba, E., Felletti, F. Frigerio, C.,
Hennissen, J. A., Leng, M. J., Petrizzo, M. R., Raffi, I., Raineri, G., and
Stephenson, M. H.: Seasonality fluctuations recorded in fossil bivalves
during the early Pleistocene: implications for climate change, Palaeogeogr.
Palaeocl., 446, 234–251, 2016.
Cuesta Mayorga, I., Astilleros, J. M., Fernández-Díaz, L., Morales,
J., Prieto, M., Roncal-Herrero, T., and Benning, L. G.: Epitactic
overgrowths of calcite (CaCO3) on anhydrite (CaSO4) cleavage
surfaces, Cryst. Growth Des., 18, 1666–1675, 2018.
Delanghe, D., Bard, E., and Hamelin, B.: New TIMS constraints on the
uranium-238 and uranium-234 in seawaters from the main ocean basins and the
Mediterranean Sea, Mar. Chem., 80, 79–93, 2002.
Elliot, M., deMenocalm, P. B., Linsley, B. K., and Howe, S. S.:
Environmental controls on the stable isotopic composition of Mercenaria mercenaria: potential
application to paleoenvironmental studies, Geochem. Geophys. Geosyst., 4,
1056, https://doi.org/10.1029/2002GC000425, 2003.
Etschmann, B., Brugger, J., Pearce, M. A., Ta, C., Brautigan, D., Jung, M.,
and Pring, A.: Grain boundaries as microreactors during reactive fluid flow:
experimental dolomitization of a calcite marble, Contrib. Mineral. Petrol.,
168, 1045, https://doi.org/10.1007/s00410-014-1045-z, 2014.
Fabritius, H., Walther, P., and Ziegler, A.: Architecture of the organic
matrix in the sternal CaCO3 deposits of Porcellio scaber (Crustacea, Isopoda), J.
Struct. Biol., 150, 190–199, 2005.
Fernández-Díaz, L., Pina, C. M., Astilleros, J. M., and
Sánchez-Pastor, N.: The carbonatation of gypsum: pathways and
pseudomorph formation, Am. Mineral., 94, 1223–1234, 2009.
Friedman, G. M.: Early diagenesis and lithification in carbonate sediments,
J. Sediment. Petrol., 34, 777–813, 1964.
Greiner, M., Férnandez-Díaz, L., Griesshaber, E., Zenkert, M. N.,
Yin, X., Ziegler, A., Veintemillas-Verdaguer, S., and Schmahl, W. W.:
Biomineral reactivity: the kinetics of the replacement reaction of
biological aragonite to apatite, Minerals, 8, 315, https://doi.org/10.3390/min8080315, 2018.
Gries, K., Kroger, R., Kubel, C., Schowalter, M., Fritz, M., and Rosenauer,
A.: Correlation of the orientation of stacked aragonite platelets in nacre
and their connection via mineral bridges, Ultramicroscopy, 109, 230–236,
2009.
Griesshaber, E., Schmahl, W. W., Ubhi, H. S., Huber, J., Nindiyasari, F.,
Maier, B., and Ziegler, A.: Homoepitaxial meso- and microscale crystal
co-orientation and organic matrix network structure in Mytilus edulis nacre and calcite,
Acta Biomater., 9, 9492–9502, 2013.
Griesshaber, E., Yin, X., Ziegler, A., Kelm, K., Checa, A., Eisenhauer, A.,
and Schmahl, W. W.: Patterns of mineral organization in carbonate biological
hard materials, in:
Highlights in Applied Mineralogy, edited by: Heuss-Aßbichler, S., Amthauer, G., and John, M., de Gruyter, Berlin, 2017.
Hahn, S., Rodolfo-Metalpa, R., Griesshaber, E., Schmahl, W. W., Buhl, D.,
Hall-Spencer, J. M., Baggini, C., Fehr, K. T., and Immenhauser, A.: Marine bivalve shell
geochemistry and ultrastructure from modern low pH environments: environmental
effect versus experimental bias, Biogeosciences, 9, 1897–1914, https://doi.org/10.5194/bg-9-1897-2012, 2012.
Hahn, S., Griesshaber, E., Schmahl, W. W., Neuser, R. D., Ritter, A.-C.,
Hoffmann, R., Buhl, D., Niedermayr, A., Geske, A., and Immenhauser, A.:
Exploring aberrant bivalve shell ultrastructure and geochemistry as proxies
for past sea water acidification, Sedimentology, 61, 1625–1658, 2014.
Hamelin, B., Bard, E., Zindler, A., and Fairbanks, R. G.:
234U/238U mass spectrometry of corals: how accurate is the U-Th
age of the last interglacial period?, Earth Planet. Sc. Lett., 106, 169–180,
1991.
Harper, E. M.: The fossil record of bivalve molluscs, in: The adequacy of the fossil record, edited by: Donovan S. K. and
Paul C. R. C., John Wiley and Sons,
Chichester, 243–267, 1998.
Heiss, G. A.: Coral reefs in the Red Sea: growth, production, and stable
isotopes, Geomar. Report, 32, 1–141, 1994.
Henderson, G. M., Cohen, A. S., and O'Nions, R. K.:
234U∕238U ratios and 230Th ages for Hateruma Atoll corals:
implications for coral diagenesis and seawater 234U∕238U ratios,
Earth Planet. Sc. Lett., 115, 65–73, 1993.
Hendry, J. P., Dirchfield, P. W., and Marshall, J. D.: Two-stage neomorphism
of Jurassic aragonitic bivalves: implications for early diagenesis, J.
Sediment. Res., A65, 214–224, 1995.
Hippler, D., Buhl, D., Witbaard, R., and Immenhauser, A.: Towards a better
understanding of magnesium-isotope ratios, Geochim. Cosmochim. Ac., 73,
6134–6146, 2009.
Hover, V. C., Walter, L. M., and Peacor, D. R.: Early marine diagenesis of
biogenic aragonite and Mg-calcite: new constraints from high-resolution STEM
and AEM analyses of modern platform carbonates, Chem. Geol., 175, 221–248,
2001.
Immenhauser, A., Schöne, B. R., Hoffmann, R., and Niedermayr, A.:
Mollusc and brachiopod skeletal hard parts: intricate archives of their
marine environment, Sedimentology, 63, 1–59, 2015.
Jackson, A. P., Vincent, J. F. V., and Turner, R. M.: The mechanical design
of nacre, P. Roy. Soc. B, 234, 415–440, 1988.
James, N. P., Bone, Y., and Kyser, K. T.: Where has all the aragonite gone?
Mineralogy of Holocene neritic cool-water carbonates, Southern Australia, J.
Sediment. Res., 75, 454–463, 2005.
Jarosch, D. and Heger, G.: Neutron diffraction refinement of the crystal
structure of aragonite, Tscher. Miner. Petrog., 35, 127–131, 1986.
Jonas, L., John, T., King, H. E., Geisler, T., and Putnis, A.: The role of
grain boundaries and transient porosity in rocks as fluid pathways for
reaction front propagation, Earth Planet. Sc. Lett., 386, 64–74, 2014.
Jonas, L., Müller, T., Dohmen, R., Baumgartner, L., and Putlitz, B.:
Transport-controlled hydrothermal replacement of calcite by Mg-carbonates,
Geology, 43, 779–782, 2015.
Karney, G. B., Butler, P. G., Speller, S., Scourse, J. D., Richardson, C.
A., Schröder, M., Highes, G. M., Czernuszka, J. T., and Grovenor, C. R.
M.: Characterizing the microstructure of Arctica islandica shells using NanoSIMS and EBSD,
Geochem. Geophys. Geosyst., 13, 1–14, 2012.
Kidwell, S. M.: Shell composition has no net impact on large-scale
evolutionary patterns in mollusks, Science, 307, 914–917, 2005.
Korte, C., Kozur, H. W., and Veizer, J.: δ13C and δ18O
values of Triassic brachiopods and carbonate rocks as proxies for
coeval seawater and palaeotemperature, Palaeogeogr. Palaeocl.,
226, 287–306, 2005.
Krause-Nehring, J., Brey, T., and Thorrold, S. R.: Centennial records of
lead contamination in northern Atlantic bivalves (Arctica islandica), Mar. Pollut. Bull.,
64, 233–240, 2012.
Ku, T. C. W., Walter, L. M., Coleman, M. L., Blake, R. E., and Martini, A.
M.: Coupling between sulfur recycling and syndepositional carbonate
dissolution: evidence from oxygen and sulfur isotope composition of pore
water sulfate, South Florida Platform, U. S. A., Geochim. Cosmochim. Ac.,
63, 2529–2546, 1999.
Land, L. S.: Diagenesis of skeletal carbonates, J. Sediment. Res., 37,
914–930, 1967.
Levi-Kalisman, Y., Falini, G., Addadi, L., and Weiner, S.: Structure of the
nacreous organic matrix of a bivalve mollusk shell examined in the hydrated
state using Cryo-TEM, J. Struct. Biol., 135, 8–17, 2001.
Li, X., Xu, Z.-H., and Wang, R.: In situ observation of nanograin rotation
and deformation in nacre, Nano Lett., 6, 2301–2304, 2006.
Maliva, R. G., Missimer, T. M., and Dickson, J. A. D.: Skeletal aragonite
neomorphism in Plio-Pleistocene sandy limestones and sandstones, Holloywood,
Florida, U.S.A., Sediment. Geol., 136, 147–154, 2000.
Marchitto, T. M., Jones, G. A., Goodfriend, G. A., and Weidman, C. R.:
Precise temporal correlation of Holocene mollusk shells using
sclerochronology, Quat. Res., 53, 236–246, 2000.
Marin, F. and Luquet, G.: Molluscan shell proteins, C. R. Palevol., 3,
469–492, 2004.
Markgraf, S. A. and Reeder, R. J.: High-temperature structure refinements of
calcite and magnesite, Am. Mineral., 70, 590–600, 1985.
Martin, G. D., Wilkinson, B. H., and Lohmann, K. C.: The role of skeletal
porosity in aragonite neomorphism – Strombus and Montastrea from the Pleistocene Key Largo
Limestone, Florida, J. Sediment. Petrol., 56, 194–203, 1986.
Mayer, G.: Rigid biological systems as models for synthetic composites,
Science, 298, 1144–1147, 2005.
McGregor, H. V. and Gagan, M. K.: Diagenesis and geochemistry of Porites corals
from Papua New Guinea: implications for paleoclimate reconstruction,
Geochim. Cosmochim. Ac., 67, 2147–2156, 2002.
Meibom, A., Mostefaoui, S., Cuif, J.-P., Dauphin, Y., Houlbreque, F.,
Dunbar, R., and Constantz, B.: Biological forcing controls the chemistry of
reef-building coral skeleton, Geophys. Res. Lett., 34, L02601, https://doi.org/10.1029/2006GL028657, 2007.
Metzler, R. A., Abrecht, M., Olabisi, R. M., Ariosa, D., Johnson, C. J.,
Frazer, B. H., Coppersmith, S. N., and Gilbert, P. U. P. A.: Architecture of
columnar nacre, and implications for its formation mechanism, Phys. Rev.
Lett., 98, 268102, https://doi.org/10.1103/PhysRevLett.98.268102, 2007.
Morton, B.: The biology and functional morphology of Arctica islandica (Bivalvia:
Arcticidae): a gerontophilic living fossil, Mar. Biol. Res., 7, 540–553,
2011.
Nindiyasari, F., Ziegler, A., Griesshaber, E., Fernández-Díaz, L.,
Huber, J., Walther, P., and Schmahl, W. W.: Effect of hydrogel
matrices on calcite crystal growth morphology, aggregate formation, and
co-orientation in biomimetic experiments and biomineralization environments,
Cryst. Growth Des., 15, 2667–2685, 2015.
Patterson, W. P. and Walter, L. M.: Sydepositional diagenesis of modern
platform carbonates: evidence from isotopic and minor element data, Geology,
22, 127–130, 1994.
Perdikouri, C., Kasioptas, A., Geisler, T., Schmidt, B. C., and Putnis, A.:
Experimental study of the aragonite to calcite transition in aqueous
solution, Geochim. Cosmochim. Ac., 75, 6211–6224, 2011.
Perdikouri, C., Piazolo, S., Kasioptas, A., Schmidt, B. C., and Putnis, A.:
Hydrothermal replacement of aragonite by calcite: interplay between
replacement, fracturing and growth, Eur. J. Mineral., 25, 123–136, 2013.
Pollok, K., Putnis, C. V., and Putnis, A.: Mineral replacement reactions in
solid solution-aqueous solution systems: volume changes, reactions paths and
end-points using the example of model salt systems, Am. J. Sci., 311,
211–236, 2011.
Putnis, A.: Mineral replacement reactions: from macroscopic observations to
microscopic mechanisms, Mineral. Mag., 66, 689–708, 2002.
Putnis, A.: Mineral replacement reactions, Rev. Mineral. Geochem., 70,
87–124, 2009.
Qian, G., Brugger, J., Skinner, W. M., Chen, G., and Pring, A.: An
experimental study of the mechanism of the replacement of magnetite by
pyrite up to 300 °C, Geochim. Cosmochim. Ac., 74, 5610–5630,
2010.
Raffi, S.: The significance of marine boreal molluscs in the Early
Pleistocene faunas of the Mediterranean area, Palaeogeogr. Palaeocl., 52, 267–289, 1986.
Randle, V. and Engler, O.: Introduction to texture analysis, CRC Press,
Amsterdam, 2000.
Rashid, R., Eisenhauer, A., Stocchi, P., Fietzke, J., Rüggeberg, A., and
Dullo, W.-C.: Constraining mid to late Holocene relative sea level change
in the southern equatorial Pacific Ocean relative to the Society Islands,
French Polynesia, Geochem. Geophy. Geosy., 15, 2601–2615, 2014.
Regenberg, M., Nürnberg, D., Schönfeld, J., and Reichart, G.-J.:
Early diagenetic overprint in Caribbean sediment cores and its effect
on the geochemical composition of planktonic foraminifera, Biogeosciences, 4, 957–973, https://doi.org/10.5194/bg-4-957-2007, 2007.
Richardson, C. A.: Molluscs as archives of environmental change, Oceanogr.
Mar. Biol., 39, 103–164, 2001.
Ridgway, I. D., Richardson, C. A., and Austad, S. N.: Maximum shell size,
growth rate, and maturation age correlate with longevity in bivalve
molluscs, J. Gerontol. A Biol. Sci. Med. Sci., 66, 183–190, 2011.
Ritter, A.-C., Mavromatis, V., Dietzel, M., Wiethoff, F., Griesshaber, E.,
Casella, L. A., Schmahl, W. W., Koelen, J., Neuser, R. D., Leis, A., Buhl, D., Niedermayr, A., Bernasconi, S. M., and
Immenhauser, A.: Exploring the impact of diagenesis on (isotope)geochemical
and microstructural alteration features in biogenic aragonite,
Sedimentology, 64, 1354–1380, 2017.
Rodríguez-Carvajal, J.: Recent developments of the program FULLPROF,
Commission on Powder Diffraction (IUCr), Newsletter, 26, 12–19, 2001.
Roncal-Herrero, T., Astilleros, J. M., Bots, P., Diego, J., Blanco, R.,
Prieto, M., Benning, L. G., and Fernández-Díaz, L.: Reaction
pathways and textural aspects of the replacement of anhydrite by calcite at
25 °C, Am. Mineral., 120, 1270–1278, 2017.
Rüggeberg, A., Fietzke, J., Liebetrau, V., Eisenhauer, A., Dullo, W.-C.,
and Freiwald, A.: Stable strontium isotopes (δ88∕86Sr) in
cold-water corals – a new proxy for reconstruction of intermediate ocean
water temperatures, Earth Planet. Sc. Lett., 269, 570–575, 2008.
Ruíz-Agudo, E., Putnis, C. V., and Putnis, A.: Coupled dissolution and
precipitation at mineral-fluid interfaces, Chem. Geol., 383, 132–146, 2014.
Sandberg, P. A. and Hudson, J. D.: Aragonite relic preservation in Jurassic
calcite-replaced bivalves, Sedimentology, 30, 879–892, 1983.
Schmahl, W. W., Griesshaber, E., Kelm, K., Goetz, A., Jordan, G., Ball, A.,
Xu, D., Merkel, C., and Brand, U.: Hierarchical structure of marine shell
biomaterials: biomechanical functionalization of calcite by brachiopods, Z.
Kristallogr., 227, 793–804, 2012.
Schmidt, N. H. and Olesen, N. O.: Computer-aided determination of
crystal-lattice orientation from electron channeling patterns in the SEM,
Can. Mineral., 27, 15–22, 1989.
Schöne, B. R.: Arctica islandica (Bivalvia): a unique paleoenvironmental archive of the
northern North Atlantic Ocean, Global Planet. Change, 111, 199–225, 2013.
Schöne, B. R. and Surge, D. M.: Bivalve sclerochronology and
geochemistry, in: Treatise on invertebrate Paleontology
(Part N Revised), edited by: Selden, P. A., Treatise Online, 46, 1–24, 2012.
Schöne, B. R., Freyre Castro, A. D., Fiebig, J., Houk, S. D., Oschmann,
W., and Kröncke, I.: Sea surface water temperatures over the period
1884–1983 reconstructed from oxygen isotope ratios of a bivalve mollusk
shell (Arctica islandica, southern North Sea), Palaeogeogr. Palaeocl., 212,
215–232, 2004.
Schöne, B. R., Houk, S. D., Freyre Castro, A. D., Fiebig, J.,
Kröncke, I., Dreyer, W., Gosselck, F., and Oschmann, W.: Daily growth
rates in shells of Arctica islandica: assessing subseasonal environmental controls on a
long-lived bivalve mollusc, Palaios, 20, 78–92, 2005a.
Schöne, B. R., Pfeiffer, M., Pohlmann, T., and Siegismund, F.: A
seasonally resolved bottom-water temperature record for the period as
1866–2002 based on shells of Arctica islandica (Mollusca, North Sea), Int. J. Climatol., 25,
947–962, 2005b.
Sorauf, J. E.: Biomineralization, structure and diagenesis of the
coelenterate skeleton, Acta Palaeont. Polonica, 25, 237–343, 1980.
Stirling, C. H., Esat, T. M., McCulloch, M. T., and Lambeck, K.:
High-precision U-series of corals from Western Australia and implications
for the timing and duration of the Last Interglacial, Earth Planet. Sc.
Lett., 135, 115–130, 1995.
Strahl, J., Dringen, R., Schmidt, M. M., Hardenberg, S., and Abele, D.:
Metabolic and physiological responses in tissues of the longlived bivalve
Arctica islandica to oxygen deficiency, Comp. Biochem. Physiol. A, 158, 513–519, 2011.
Swart, P. K.: The geochemistry of carbonate diagenesis: the past, present
and future, Sedimentology, 62, 1233–1304, 2015.
Tomiak, P. J., Andersen, M. B., Hendy, E. J., Potter, E. K., Johnson, K. G.,
and Penkman, K. E. H.: The role of skeletal micro-architecture in diagenesis
and dating of Acropora palmata, Geochim. Cosmochim. Ac., 183, 153–175, 2016.
Ullmann, C. V. and Korte, C.: Diagenetic alteration in low-Mg calcite from
macrofossils: a review, Geol. Quart., 59, 3–20, 2015.
Wanamaker Jr., A. D., Kreutz, K. J., Schöne, B. R., Pettigrew, N.,
Borns, H. W., Introne, D. S., Belknap, D., Maasch, K. A., and Feindel, S.:
Coupled North Atlantic slope water forcing on Gulf of Maine temperatures
over the past millennium, Clim. Dynam., 31, 183–194, 2008.
Wanamaker Jr., A. D., Kreutz, K. J., Schöne, B. R., and Introne, D. S.:
Gulf of Main shells reveal changes in seawater temperature seasonality
during the Medieval Climate Anomaly and the Little Ice Age, Palaeogeogr.
Palaeocl., 302, 43–51, 2011.
Wardlaw, N., Oldershaw, A., and Stout, M.: Transformation of aragonite to
calcite in a marine gastropod, Can. J. Earth Sci., 15, 1861–1866, 1978.
Wright, V. P., Cherns, L., and Hodges, P.: Missing molluscs: field testing
taphonomic loss in the Mesozoic through early largescale aragonite
dissolution, Geology, 31, 211–214, 2003.
Xia, F., Brugger, J. I., Chen, G., Ngothai, Y., O'Neill, B., Putnis, A., and
Pring, A.: Mechanism and kinetics of pseudomorphic mineral replacement
reactions: a case study of the replacement of pentlandite by violarite,
Geochim. Cosmochim. Ac. 73, 1945–1969, 2009a.
Xia, F., Brugger, J. I., Ngothai, Y., O'Neill, B., Chen, G., and Pring, A.:
Three-dimensional ordered arrays of zeolite nanocrystals with uniform size
and orientation by a pseudomorphic coupled dissolution-reprecipitation
replacement route, Cryst. Growth Des., 9, 4902–4906, 2009b.
Zazzo, A., Lécuyer, C., Sheppard, S. M., Grandjean, P., and Mariotti,
A.: Diagenesis and the reconstruction of paleoenvironments: a method to
restore original δ18O values of carbonate and phosphate from
fossil tooth enamel, Geochim. Cosmochim. Ac., 68, 2245–2258, 2004.
Short summary
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.
Biogenic carbonates record past environmental conditions. Fossil shell chemistry and...
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