Articles | Volume 15, issue 5
https://doi.org/10.5194/bg-15-1469-2018
© 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-15-1469-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
09 Mar 2018
Research article |
| 09 Mar 2018
| 09 Mar 2018
Calcification in a marginal sea – influence of seawater [Ca2+] and carbonate chemistry on bivalve shell formation
Jörn Thomsen
CORRESPONDING AUTHOR
Marine Ecology, GEOMAR Helmholtz Centre for Ocean Research, Kiel,
Germany
Kirti Ramesh
Marine Ecology, GEOMAR Helmholtz Centre for Ocean Research, Kiel,
Germany
Institute of Physiology, Kiel University, 24098 Kiel, Germany
Trystan Sanders
Marine Ecology, GEOMAR Helmholtz Centre for Ocean Research, Kiel,
Germany
Markus Bleich
Institute of Physiology, Kiel University, 24098 Kiel, Germany
Frank Melzner
Marine Ecology, GEOMAR Helmholtz Centre for Ocean Research, Kiel,
Germany
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Trystan Sanders, Jörn Thomsen, Jens Daniel Müller, Gregor Rehder, and Frank Melzner
Biogeosciences, 18, 2573–2590, https://doi.org/10.5194/bg-18-2573-2021, https://doi.org/10.5194/bg-18-2573-2021, 2021
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The Baltic Sea is expected to experience a rapid drop in salinity and increases in acidity and warming in the next century. Calcifying mussels dominate Baltic Sea seafloor ecosystems yet are sensitive to changes in seawater chemistry. We combine laboratory experiments and a field study and show that a lack of calcium causes extremely slow growth rates in mussels at low salinities. Subsequently, climate change in the Baltic may have drastic ramifications for Baltic seafloor ecosystems.
J. Thomsen, K. Haynert, K. M. Wegner, and F. Melzner
Biogeosciences, 12, 4209–4220, https://doi.org/10.5194/bg-12-4209-2015, https://doi.org/10.5194/bg-12-4209-2015, 2015
K. Haynert, J. Schönfeld, R. Schiebel, B. Wilson, and J. Thomsen
Biogeosciences, 11, 1581–1597, https://doi.org/10.5194/bg-11-1581-2014, https://doi.org/10.5194/bg-11-1581-2014, 2014
Trystan Sanders, Jörn Thomsen, Jens Daniel Müller, Gregor Rehder, and Frank Melzner
Biogeosciences, 18, 2573–2590, https://doi.org/10.5194/bg-18-2573-2021, https://doi.org/10.5194/bg-18-2573-2021, 2021
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The Baltic Sea is expected to experience a rapid drop in salinity and increases in acidity and warming in the next century. Calcifying mussels dominate Baltic Sea seafloor ecosystems yet are sensitive to changes in seawater chemistry. We combine laboratory experiments and a field study and show that a lack of calcium causes extremely slow growth rates in mussels at low salinities. Subsequently, climate change in the Baltic may have drastic ramifications for Baltic seafloor ecosystems.
Carolin R. Löscher, Hermann W. Bange, Ruth A. Schmitz, Cameron M. Callbeck, Anja Engel, Helena Hauss, Torsten Kanzow, Rainer Kiko, Gaute Lavik, Alexandra Loginova, Frank Melzner, Judith Meyer, Sven C. Neulinger, Markus Pahlow, Ulf Riebesell, Harald Schunck, Sören Thomsen, and Hannes Wagner
Biogeosciences, 13, 3585–3606, https://doi.org/10.5194/bg-13-3585-2016, https://doi.org/10.5194/bg-13-3585-2016, 2016
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The ocean loses oxygen due to climate change. Addressing this issue in tropical ocean regions (off Peru and Mauritania), we aimed to understand the effects of oxygen depletion on various aspects of marine biogeochemistry, including primary production and export production, the nitrogen cycle, greenhouse gas production, organic matter fluxes and remineralization, and the role of zooplankton and viruses.
Rainer Kiko, Helena Hauss, Friedrich Buchholz, and Frank Melzner
Biogeosciences, 13, 2241–2255, https://doi.org/10.5194/bg-13-2241-2016, https://doi.org/10.5194/bg-13-2241-2016, 2016
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The diel vertical migration of zooplankton and nekton results in an active export of carbon and nitrogen from the oceans surface layer. In vast areas of the ocean the daytime distribution depth of migrating organisms corresponds to the core of an oxygen minimum zone (OMZ). We show that exposure to OMZ conditions can result in a strong depression of respiration and ammonium excretion in zooplankton, a fact that needs to be considered when calculating carbon and nitrogen fluxes in OMZ regions.
J. Thomsen, K. Haynert, K. M. Wegner, and F. Melzner
Biogeosciences, 12, 4209–4220, https://doi.org/10.5194/bg-12-4209-2015, https://doi.org/10.5194/bg-12-4209-2015, 2015
K. Haynert, J. Schönfeld, R. Schiebel, B. Wilson, and J. Thomsen
Biogeosciences, 11, 1581–1597, https://doi.org/10.5194/bg-11-1581-2014, https://doi.org/10.5194/bg-11-1581-2014, 2014
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Mollusk shells are valuable recorders of climate and environmental changes of the past down to a daily resolution. To explore this potential, we measured changes in the composition of shells of two types of bivalves recorded at the hourly scale: the king scallop Pecten maximus and giant clams (Tridacna) that engaged in photosymbiosis. We find that photosymbiosis produces more day–night fluctuation in shell chemistry but that most of the variation is not periodic, perhaps recording weather.
Kristian Spilling, Jonna Piiparinen, Eric P. Achterberg, Javier Arístegui, Lennart T. Bach, Maria T. Camarena-Gómez, Elisabeth von der Esch, Martin A. Fischer, Markel Gómez-Letona, Nauzet Hernández-Hernández, Judith Meyer, Ruth A. Schmitz, and Ulf Riebesell
Biogeosciences, 20, 1605–1619, https://doi.org/10.5194/bg-20-1605-2023, https://doi.org/10.5194/bg-20-1605-2023, 2023
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We carried out an enclosure experiment using surface water off Peru with different additions of oxygen minimum zone water. In this paper, we report on enzyme activity and provide data on the decomposition of organic matter. We found very high activity with respect to an enzyme breaking down protein, suggesting that this is important for nutrient recycling both at present and in the future ocean.
Thomas Letulle, Danièle Gaspard, Mathieu Daëron, Florent Arnaud-Godet, Arnauld Vinçon-Laugier, Guillaume Suan, and Christophe Lécuyer
Biogeosciences, 20, 1381–1403, https://doi.org/10.5194/bg-20-1381-2023, https://doi.org/10.5194/bg-20-1381-2023, 2023
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This paper studies the chemistry of modern marine shells called brachiopods. We investigate the relationship of the chemistry of these shells with sea temperatures to test and develop tools for estimating sea temperatures in the distant past. Our results confirm that two of the investigated chemical markers could be useful thermometers despite some second-order variability independent of temperature. The other chemical markers investigated, however, should not be used as a thermometer.
Franziska Tell, Lukas Jonkers, Julie Meilland, and Michal Kucera
Biogeosciences, 19, 4903–4927, https://doi.org/10.5194/bg-19-4903-2022, https://doi.org/10.5194/bg-19-4903-2022, 2022
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This study analyses the production of calcite shells formed by one of the main Arctic pelagic calcifiers, the foraminifera N. pachyderma. Using vertically resolved profiles of shell concentration, size and weight, we show that calcification occurs throughout the upper 300 m with an average production flux below the calcification zone of 8 mg CaCO3 m−2 d−1 representing 23 % of the total pelagic biogenic carbonate production. The production flux is attenuated in the twilight zone by dissolution.
Paweł Działak, Marcin D. Syczewski, Kamil Kornaus, Mirosław Słowakiewicz, Łukasz Zych, and Andrzej Borkowski
Biogeosciences, 19, 4533–4550, https://doi.org/10.5194/bg-19-4533-2022, https://doi.org/10.5194/bg-19-4533-2022, 2022
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Bacteriophages comprise one of the factors that may influence mineralization processes. The number of bacteriophages in the environment usually exceeds the number of bacteria by an order of magnitude. One of the more interesting processes is the formation of framboidal pyrite, and it is not entirely clear what processes determine its formation. Our studies indicate that some bacterial viruses may influence the formation of framboid-like or spherical structures.
Philipp M. Spreter, Markus Reuter, Regina Mertz-Kraus, Oliver Taylor, and Thomas C. Brachert
Biogeosciences, 19, 3559–3573, https://doi.org/10.5194/bg-19-3559-2022, https://doi.org/10.5194/bg-19-3559-2022, 2022
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We investigate the calcification rate of reef corals from an upwelling zone, where low seawater pH and high nutrient concentrations represent a recent analogue for the future ocean. Calcification rate of the corals largely relies on extension growth. Variable responses of extension growth to nutrients either compensate or exacerbate negative effects of weak skeletal thickening associated with low seawater pH – a mechanism that is critical for the persistence of coral reefs under global change.
Giulia Piazza, Valentina A. Bracchi, Antonio Langone, Agostino N. Meroni, and Daniela Basso
Biogeosciences, 19, 1047–1065, https://doi.org/10.5194/bg-19-1047-2022, https://doi.org/10.5194/bg-19-1047-2022, 2022
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The coralline alga Lithothamnion corallioides is widely distributed in the Mediterranean Sea and NE Atlantic Ocean, where it constitutes rhodolith beds, which are diversity-rich ecosystems on the seabed. The boron incorporated in the calcified thallus of coralline algae (B/Ca) can be used to trace past changes in seawater carbonate and pH. This paper suggests a non-negligible effect of algal growth rate on B/Ca, recommending caution in adopting this proxy for paleoenvironmental reconstructions.
Sarina Schmidt, Ed C. Hathorne, Joachim Schönfeld, and Dieter Garbe-Schönberg
Biogeosciences, 19, 629–664, https://doi.org/10.5194/bg-19-629-2022, https://doi.org/10.5194/bg-19-629-2022, 2022
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The study addresses the potential of marine shell-forming organisms as proxy carriers for heavy metal contamination in the environment. The aim is to investigate if the incorporation of heavy metals is a direct function of their concentration in seawater. Culturing experiments with a metal mixture were carried out over a wide concentration range. Our results show shell-forming organisms to be natural archives that enable the determination of metals in polluted and pristine environments.
Valentina Alice Bracchi, Giulia Piazza, and Daniela Basso
Biogeosciences, 18, 6061–6076, https://doi.org/10.5194/bg-18-6061-2021, https://doi.org/10.5194/bg-18-6061-2021, 2021
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Ultrastructures of Lithothamnion corallioides, a crustose coralline alga collected from the Atlantic and Mediterranean Sea at different depths, show high-Mg-calcite cell walls formed by crystals with a specific shape and orientation that are unaffected by different environmental conditions of the living sites. This suggests that the biomineralization process is biologically controlled in coralline algae and can have interesting applications in paleontology.
Trystan Sanders, Jörn Thomsen, Jens Daniel Müller, Gregor Rehder, and Frank Melzner
Biogeosciences, 18, 2573–2590, https://doi.org/10.5194/bg-18-2573-2021, https://doi.org/10.5194/bg-18-2573-2021, 2021
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The Baltic Sea is expected to experience a rapid drop in salinity and increases in acidity and warming in the next century. Calcifying mussels dominate Baltic Sea seafloor ecosystems yet are sensitive to changes in seawater chemistry. We combine laboratory experiments and a field study and show that a lack of calcium causes extremely slow growth rates in mussels at low salinities. Subsequently, climate change in the Baltic may have drastic ramifications for Baltic seafloor ecosystems.
Luc Beaufort, Yves Gally, Baptiste Suchéras-Marx, Patrick Ferrand, and Julien Duboisset
Biogeosciences, 18, 775–785, https://doi.org/10.5194/bg-18-775-2021, https://doi.org/10.5194/bg-18-775-2021, 2021
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The coccoliths are major contributors to the particulate inorganic carbon in the ocean. They are extremely difficult to weigh because they are too small to be manipulated. We propose a universal method to measure thickness and weight of fine calcite using polarizing microscopy that does not require fine-tuning of the light or a calibration process. This method named "bidirectional circular polarization" uses two images taken with two directions of a circular polarizer.
Anna Piwoni-Piórewicz, Stanislav Strekopytov, Emma Humphreys-Williams, and Piotr Kukliński
Biogeosciences, 18, 707–728, https://doi.org/10.5194/bg-18-707-2021, https://doi.org/10.5194/bg-18-707-2021, 2021
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Calcifying organisms occur globally in almost every environment, and the process of biomineralization is of great importance in the global carbon cycle and use of skeletons as environmental data archives. The composition of skeletons is very complex. It is determined by the mechanisms of biological control on biomineralization and the response of calcifying organisms to varying environmental drivers. Yet for trace elements, such as Cu, Pb and Cd, an impact of environmental factors is pronounced.
Siham de Goeyse, Alice E. Webb, Gert-Jan Reichart, and Lennart J. de Nooijer
Biogeosciences, 18, 393–401, https://doi.org/10.5194/bg-18-393-2021, https://doi.org/10.5194/bg-18-393-2021, 2021
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Foraminifera are calcifying organisms that play a role in the marine inorganic-carbon cycle and are widely used to reconstruct paleoclimates. However, the fundamental process by which they calcify remains essentially unknown. Here we use inhibitors to show that an enzyme is speeding up the conversion between bicarbonate and CO2. This helps the foraminifera acquire sufficient carbon for calcification and might aid their tolerance to elevated CO2 level.
Anne Roepert, Lubos Polerecky, Esmee Geerken, Gert-Jan Reichart, and Jack J. Middelburg
Biogeosciences, 17, 4727–4743, https://doi.org/10.5194/bg-17-4727-2020, https://doi.org/10.5194/bg-17-4727-2020, 2020
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We investigated, for the first time, the spatial distribution of chlorine and fluorine in the shell walls of four benthic foraminifera species: Ammonia tepida, Amphistegina lessonii, Archaias angulatus, and Sorites marginalis. Cross sections of specimens were imaged using nanoSIMS. The distribution of Cl and F was co-located with organics in the rotaliids and rather homogeneously distributed in miliolids. We suggest that the incorporation is governed by the biomineralization pathway.
Vincent Mouchi, Camille Godbillot, Vianney Forest, Alexey Ulianov, Franck Lartaud, Marc de Rafélis, Laurent Emmanuel, and Eric P. Verrecchia
Biogeosciences, 17, 2205–2217, https://doi.org/10.5194/bg-17-2205-2020, https://doi.org/10.5194/bg-17-2205-2020, 2020
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Rare earth elements (REEs) in coastal seawater are included in bivalve shells during growth, and a regional fingerprint can be defined for provenance and environmental monitoring studies. We present a large dataset of REE abundances from oysters from six locations in France. The cupped oyster can be discriminated from one locality to another, but this is not the case for the flat oyster. Therefore, provenance studies using bivalve shells based on REEs are not adapted for the flat oyster.
Rosie L. Oakes and Jocelyn A. Sessa
Biogeosciences, 17, 1975–1990, https://doi.org/10.5194/bg-17-1975-2020, https://doi.org/10.5194/bg-17-1975-2020, 2020
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Pteropods are a group of tiny swimming snails whose fragile shells put them at risk from ocean acidification. We investigated the factors influencing the thickness of pteropods shells in the Cariaco Basin, off Venezuela, which is unaffected by ocean acidification. We found that pteropods formed thicker shells when nutrient concentrations, an indicator of food availability, were highest, indicating that food may be an important factor in mitigating the effects of ocean acidification on pteropods.
Miguel Gómez Batista, Marc Metian, François Oberhänsli, Simon Pouil, Peter W. Swarzenski, Eric Tambutté, Jean-Pierre Gattuso, Carlos M. Alonso Hernández, and Frédéric Gazeau
Biogeosciences, 17, 887–899, https://doi.org/10.5194/bg-17-887-2020, https://doi.org/10.5194/bg-17-887-2020, 2020
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In this paper, we assessed four methods (total alkalinity anomaly, calcium anomaly, 45Ca incorporation, and 13C incorporation) to determine coral calcification of a reef-building coral. Under all conditions (light vs. dark incubations and ambient vs. lowered pH levels), calcification rates estimated using the alkalinity and calcium anomaly techniques as well as 45Ca incorporation were highly correlated, while significantly different results were obtained with the 13C incorporation technique.
Alan Marron, Lucie Cassarino, Jade Hatton, Paul Curnow, and Katharine R. Hendry
Biogeosciences, 16, 4805–4813, https://doi.org/10.5194/bg-16-4805-2019, https://doi.org/10.5194/bg-16-4805-2019, 2019
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Isotopic signatures of silica fossils can be used as archives of past oceanic silicon cycling, which is linked to marine carbon uptake. However, the biochemistry that lies behind such chemical fingerprints remains poorly understood. We present the first measurements of silicon isotopes in a group of protists closely related to animals, choanoflagellates. Our results highlight a taxonomic basis to silica isotope signatures, possibly via a shared transport pathway in choanoflagellates and animals.
Laura M. Otter, Oluwatoosin B. A. Agbaje, Matt R. Kilburn, Christoph Lenz, Hadrien Henry, Patrick Trimby, Peter Hoppe, and Dorrit E. Jacob
Biogeosciences, 16, 3439–3455, https://doi.org/10.5194/bg-16-3439-2019, https://doi.org/10.5194/bg-16-3439-2019, 2019
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This study uses strontium as a trace elemental marker in combination with high-resolution nano-analytical techniques to label the growth fronts of bivalves in controlled aquaculture conditions. The growing shells incorporate the labels and are used as
snapshotsvisualizing the growth processes across different shell architectures. These observations are combined with structural investigations across length scales and altogether allow for a detailed understanding of this shell.
Simon Michael Ritter, Margot Isenbeck-Schröter, Christian Scholz, Frank Keppler, Johannes Gescher, Lukas Klose, Nils Schorndorf, Jerónimo Avilés Olguín, Arturo González-González, and Wolfgang Stinnesbeck
Biogeosciences, 16, 2285–2305, https://doi.org/10.5194/bg-16-2285-2019, https://doi.org/10.5194/bg-16-2285-2019, 2019
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Unique and spectacular under water speleothems termed as Hells Bells were recently reported from sinkholes (cenotes) of the Yucatán Peninsula, Mexico. However, the mystery of their formation remained unresolved. Here, we present detailed geochemical analyses and delineate that the growth of Hells Bells results from a combination of biogeochemical processes and variable hydraulic conditions within the cenote.
Andrew C. Mitchell, Erika J. Espinosa-Ortiz, Stacy L. Parks, Adrienne J. Phillips, Alfred B. Cunningham, and Robin Gerlach
Biogeosciences, 16, 2147–2161, https://doi.org/10.5194/bg-16-2147-2019, https://doi.org/10.5194/bg-16-2147-2019, 2019
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Microbially induced carbonate mineral precipitation (MICP) is a natural process that is also being investigated for subsurface engineering applications including radionuclide immobilization and microfracture plugging. We demonstrate that rates of MICP from microbial urea hydrolysis (ureolysis) vary with different bacterial strains, but rates are similar in both oxygenated and oxygen-free conditions. Ureolysis MICP is therefore a viable biotechnology in the predominately oxygen-free subsurface.
Inge van Dijk, Christine Barras, Lennart Jan de Nooijer, Aurélia Mouret, Esmee Geerken, Shai Oron, and Gert-Jan Reichart
Biogeosciences, 16, 2115–2130, https://doi.org/10.5194/bg-16-2115-2019, https://doi.org/10.5194/bg-16-2115-2019, 2019
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Systematics in the incorporation of different elements in shells of marine organisms can be used to test calcification models and thus processes involved in precipitation of calcium carbonates. On different scales, we observe a covariation of sulfur and magnesium incorporation in shells of foraminifera, which provides insights into the mechanics behind shell formation. The observed patterns imply that all species of foraminifera actively take up calcium and carbon in a coupled process.
Eveline M. Mezger, Lennart J. de Nooijer, Jacqueline Bertlich, Jelle Bijma, Dirk Nürnberg, and Gert-Jan Reichart
Biogeosciences, 16, 1147–1165, https://doi.org/10.5194/bg-16-1147-2019, https://doi.org/10.5194/bg-16-1147-2019, 2019
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Seawater salinity is an important factor when trying to reconstruct past ocean conditions. Foraminifera, small organisms living in the sea, produce shells that incorporate more Na at higher salinities. The accuracy of reconstructions depends on the fundamental understanding involved in the incorporation and preservation of the original Na of the shell. In this study, we unravel the Na composition of different components of the shell and describe the relative contribution of these components.
Hengchao Xu, Xiaotong Peng, Shijie Bai, Kaiwen Ta, Shouye Yang, Shuangquan Liu, Ho Bin Jang, and Zixiao Guo
Biogeosciences, 16, 949–960, https://doi.org/10.5194/bg-16-949-2019, https://doi.org/10.5194/bg-16-949-2019, 2019
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Viruses have been acknowledged as important components of the marine system for the past 2 decades, but understanding of their role in the functioning of the geochemical cycle remains poor. Results show viral lysis of cyanobacteria can influence the carbonate equilibrium system remarkably and promotes the formation and precipitation of carbonate minerals. Amorphous calcium carbonate (ACC) and aragonite are evident in the lysate, implying that different precipitation processes have occurred.
Nicole M. J. Geerlings, Eva-Maria Zetsche, Silvia Hidalgo-Martinez, Jack J. Middelburg, and Filip J. R. Meysman
Biogeosciences, 16, 811–829, https://doi.org/10.5194/bg-16-811-2019, https://doi.org/10.5194/bg-16-811-2019, 2019
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Multicellular cable bacteria form long filaments that can reach lengths of several centimeters. They affect the chemistry and mineralogy of their surroundings and vice versa. How the surroundings affect the cable bacteria is investigated. They show three different types of biomineral formation: (1) a polymer containing phosphorus in their cells, (2) a sheath of clay surrounding the surface of the filament and (3) the encrustation of a filament via a solid phase containing iron and phosphorus.
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
Yukiko Nagai, Katsuyuki Uematsu, Chong Chen, Ryoji Wani, Jarosław Tyszka, and Takashi Toyofuku
Biogeosciences, 15, 6773–6789, https://doi.org/10.5194/bg-15-6773-2018, https://doi.org/10.5194/bg-15-6773-2018, 2018
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We interpret detailed SEM and time-lapse observations of the calcification process in living foraminifera, which we reveal to be directly linked to the construction mechanism of organic membranes where the calcium carbonate precipitation takes place. We show that these membranes are a highly perforated outline is first woven by skeletal pseudopodia and then later overlaid by a layer of membranous pseudopodia to close the gaps. The chemical composition is related to these structures.
Agathe Martignier, Montserrat Filella, Kilian Pollok, Michael Melkonian, Michael Bensimon, François Barja, Falko Langenhorst, Jean-Michel Jaquet, and Daniel Ariztegui
Biogeosciences, 15, 6591–6605, https://doi.org/10.5194/bg-15-6591-2018, https://doi.org/10.5194/bg-15-6591-2018, 2018
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The unicellular microalga Tetraselmis cordiformis (Chlorophyta) was recently discovered to form intracellular mineral inclusions, called micropearls, which had been previously overlooked. The present study shows that 10 Tetraselmis species out of the 12 tested share this biomineralization capacity, producing amorphous calcium carbonate inclusions often enriched in Sr. This novel biomineralization process can take place in marine, brackish or freshwater and is therefore a widespread phenomenon.
Ulrike Braeckman, Felix Janssen, Gaute Lavik, Marcus Elvert, Hannah Marchant, Caroline Buckner, Christina Bienhold, and Frank Wenzhöfer
Biogeosciences, 15, 6537–6557, https://doi.org/10.5194/bg-15-6537-2018, https://doi.org/10.5194/bg-15-6537-2018, 2018
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Global warming has altered Arctic phytoplankton communities, with unknown effects on deep-sea communities that depend strongly on food produced at the surface. We compared the responses of Arctic deep-sea benthos to input of phytodetritus from diatoms and coccolithophorids. Coccolithophorid carbon was 5× less recycled than diatom carbon. The utilization of the coccolithophorid carbon may be less efficient, so a shift from diatom to coccolithophorid blooms could entail a delay in carbon cycling.
Hongrui Zhang, Heather Stoll, Clara Bolton, Xiaobo Jin, and Chuanlian Liu
Biogeosciences, 15, 4759–4775, https://doi.org/10.5194/bg-15-4759-2018, https://doi.org/10.5194/bg-15-4759-2018, 2018
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The sinking speeds of coccoliths are relevant for laboratory methods to separate coccoliths for geochemical analysis. However, in the absence of estimates of coccolith settling velocity, previous implementations have depended mainly on time-consuming method development by trial and error. In this study, the sinking velocities of cocooliths were carefully measured for the first time. We also provide an estimation of coccolith sinking velocity by shape, which will make coccolith separation easier.
Justin Michael Whitaker, Sai Vanapalli, and Danielle Fortin
Biogeosciences, 15, 4367–4380, https://doi.org/10.5194/bg-15-4367-2018, https://doi.org/10.5194/bg-15-4367-2018, 2018
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Materials, like soils or cements, can require repair. This study used a new bacterium (Sporosarcina ureae) in a repair method called "microbially induced carbonate precipitation" (MICP). In three trials, benefits were shown: S. ureae could make a model sandy soil much stronger by MICP, in fact better than a lot of other bacteria. However, MICP-treated samples got weaker in three trials of acid rain. In conclusion, S. ureae in MICP repair shows promise when used in appropriate climates.
Esmee Geerken, Lennart Jan de Nooijer, Inge van Dijk, and Gert-Jan Reichart
Biogeosciences, 15, 2205–2218, https://doi.org/10.5194/bg-15-2205-2018, https://doi.org/10.5194/bg-15-2205-2018, 2018
Sha Ni, Isabelle Taubner, Florian Böhm, Vera Winde, and Michael E. Böttcher
Biogeosciences, 15, 1425–1445, https://doi.org/10.5194/bg-15-1425-2018, https://doi.org/10.5194/bg-15-1425-2018, 2018
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Spirorbis tube worms are common epibionts on brown algae in the Baltic Sea. We made experiments with Spirorbis in the
Kiel Outdoor Benthocosmsat CO2 and temperature conditions predicted for the year 2100. The worms were able to grow tubes even at CO2 levels favouring shell dissolution but did not survive at mean temperatures over 24° C. This indicates that Spirorbis worms will suffer from future excessive ocean warming and from ocean acidification fostering corrosion of their protective tubes.
Andrea C. Gerecht, Luka Šupraha, Gerald Langer, and Jorijntje Henderiks
Biogeosciences, 15, 833–845, https://doi.org/10.5194/bg-15-833-2018, https://doi.org/10.5194/bg-15-833-2018, 2018
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Calcifying phytoplankton play an import role in long-term CO2 removal from the atmosphere. We therefore studied the ability of a representative species to continue sequestrating CO2 under future climate conditions. We show that CO2 sequestration is negatively affected by both an increase in temperature and the resulting decrease in nutrient availability. This will impact the biogeochemical cycle of carbon and may have a positive feedback on rising CO2 levels.
Merinda C. Nash and Walter Adey
Biogeosciences, 15, 781–795, https://doi.org/10.5194/bg-15-781-2018, https://doi.org/10.5194/bg-15-781-2018, 2018
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Past seawater temperatures can be reconstructed using magnesium / calcium ratios of biogenic carbonates. As temperature increases, so does magnesium. Here we show that for these Arctic/subarctic coralline algae, anatomy is the first control on Mg / Ca, not temperature. When using coralline algae for temperature reconstruction, it is first necessary to check for anatomical influences on Mg / Ca.
Thomas M. DeCarlo, Juan P. D'Olivo, Taryn Foster, Michael Holcomb, Thomas Becker, and Malcolm T. McCulloch
Biogeosciences, 14, 5253–5269, https://doi.org/10.5194/bg-14-5253-2017, https://doi.org/10.5194/bg-14-5253-2017, 2017
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We present a new technique to quantify the chemical conditions under which corals build their skeletons by analysing them with lasers at a very fine resolution, down to 1/100th the width of a human hair. Our first applications to laboratory-cultured and wild corals demonstrates the complex interplay among seawater conditions (temperature and acidity), calcifying fluid chemistry, and bulk skeleton accretion, which will define the sensitivity of coral calcification to 21st century climate change.
Giulia Faucher, Linn Hoffmann, Lennart T. Bach, Cinzia Bottini, Elisabetta Erba, and Ulf Riebesell
Biogeosciences, 14, 3603–3613, https://doi.org/10.5194/bg-14-3603-2017, https://doi.org/10.5194/bg-14-3603-2017, 2017
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The main goal of this study was to understand if, similarly to the fossil record, high quantities of toxic metals induce coccolith dwarfism in coccolithophore species. We investigated, for the first time, the effects of trace metals on coccolithophore species other than E. huxleyi and on coccolith morphology and size. Our data show a species-specific sensitivity to trace metal concentration, allowing the recognition of the most-, intermediate- and least-tolerant taxa to trace metal enrichments.
Lennart J. de Nooijer, Anieke Brombacher, Antje Mewes, Gerald Langer, Gernot Nehrke, Jelle Bijma, and Gert-Jan Reichart
Biogeosciences, 14, 3387–3400, https://doi.org/10.5194/bg-14-3387-2017, https://doi.org/10.5194/bg-14-3387-2017, 2017
Michael J. Henehan, David Evans, Madison Shankle, Janet E. Burke, Gavin L. Foster, Eleni Anagnostou, Thomas B. Chalk, Joseph A. Stewart, Claudia H. S. Alt, Joseph Durrant, and Pincelli M. Hull
Biogeosciences, 14, 3287–3308, https://doi.org/10.5194/bg-14-3287-2017, https://doi.org/10.5194/bg-14-3287-2017, 2017
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It is still unclear whether foraminifera (calcifying plankton that play an important role in cycling carbon) will have difficulty in making their shells in more acidic oceans, with different studies often reporting apparently conflicting results. We used live lab cultures, mathematical models, and fossil measurements to test this question, and found low pH does reduce calcification. However, we find this response is likely size-dependent, which may have obscured this response in other studies.
Chris H. Crosby and Jake V. Bailey
Biogeosciences, 14, 2151–2154, https://doi.org/10.5194/bg-14-2151-2017, https://doi.org/10.5194/bg-14-2151-2017, 2017
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In the course of experiments exploring the formation of calcium phosphate minerals in a polymeric matrix, we developed a small-scale, reusable, and low-cost setup that allows microscopic observation over time for use in mineral precipitation experiments that use organic polymers as a matrix. The setup uniquely accommodates changes in solution chemistry during the course of an experiment and facilitates easy harvesting of the precipitates for subsequent analysis.
Cited articles
Bach, L. T.: Reconsidering the role of carbonate ion concentration in
calcification by marine organisms, Biogeosciences, 12, 4939–4951,
https://doi.org/10.5194/bg-12-4939-2015, 2015.
Barott, K. L., Perez, S. O., Linsmayer, L. B., and Tresguerres, M.:
Differential localization of ion transporters suggests distinct cellular
mechanisms for calcification and photosynthesis between two coral species,
Am. J. Physiol.-Reg. I., 309, R235–R246, 2015.
Barton, A., Hales, B., Waldbusser, G. G., Langdon, C., and Felly, R. A.: The
Pacific oyster Crassostrea gigas, shows negative correlation to
naturally elevated carbon dioxide levels: Implications for near-term ocean
acidification effects, Limnol. Oceanogr., 57, 698–710, 2012.
Beldowski, J., Löffler, A., and Joensuu, L.: Distribution and
biogeochemical control of total CO2 and total alkalinity in the Baltic
Sea, J. Marine Syst., 81, 252–259, 2010.
Blaustein, M. P. and Lederer, W. J.: Sodium/Calcium Exchange: Its
physiological implications, Physiol. Rev., 79, 763–854, 1999.
BSH: Hourly meteorological observations at Station Oder Bank 2000–2015,
Bundesamt für Seeschiffahrt und Hydrographie, Hamburg, 2000–2015.
Casties, I., Clemmensen, C., Melzner, F., and Thomsen, J.: Salinity
dependence of recruitment success of the sea star Asterias rubens in
the brackish western Baltic Sea, Helgoland Mar. Res., 69, 169–175, 2015.
Chalker, B. E.: Calcium transport during skeletogenesis in hermatypiccorals,
Comp. Biochem. Phys. A, 54, 455–459, 1976.
Cragg, S. M.: The adductor and retractor muscles of the veliger of
Pecten maximus (L.) (Bivalvia), J. Mollus. Stud., 51, 276–283,
1985.
Crenshaw, M. A.: The inorganic composition of molluscan extrapallial fluid,
Biol. Bull., 143, 506–512, 1972.
Cyronak, T., Schulz, K. G., and Jokiel, P. L.: The Omega myth: what really
drives lower calcification rates in an acidifying ocean, ICES J. Mar. Sci.,
73, 558–562, 2015.
De Beer, D., Kühl, M., Stambler, N., and Vaki, L.: A mirosensor study of
light enhanced Ca2+ uptake and photosynthesis in the reef-building
hematypic coral Favia sp., Mar. Ecol.-Prog. Ser., 194, 75–85, 2000.
Dickson, A. G.: Standard potential of the reaction – AgClS + 1/2
H2 = AgS + HClAq and the standard acidity constant of the ion HSO4 –
in synthetic sea-water from 273.15-K to 318.15-K, J. Chem. Thermodyn., 22,
113–127, 1990.
Dickson, A. G., Afghan, J. D., and Anderson, G. G.: Reference materials for
oceanic CO2 analysis: A method for the certification of total alkalinity,
Mar. Chem., 80, 185–197, 2003.
Enderlein, P. and Wahl, M.: Dominance of blue mussels versus
consumer-mediated enhancement of benthic diversity, J. Sea Res., 51,
145–155, 2004.
Falini, G., Albeck, S., Weiner, S., and Addadi, L.: Control of aragonite or
calcite polymorphism by mollusk shell macromolecules, Science, 271, 67–69,
1996.
Fassbender, A. J., Sabine, C. L., and Feifel, K. M.: Consideration of coastal
carbonate chemistry in understanding biological calcification, Geophys. Res.
Lett., 43, 4467–4476, 2016.
Frieder, C. A., Applebaum, S. L., Pan, T. C. F., Hedgecock, D., and Manahan,
D.: Metabolic cost of calcification in bivalve larvae under experimental
ocean acidification, ICES J. Mar. Sci., 74, 941–954, 2017.
Gazeau, F., Parker, L. M., Comeau, S., Gattuso, J. P., O`Connor, W. A.,
Martin, S., Pörtner, H. O., and Ross, P. M.: Impacts of ocean
acidification on marine shelled molluscs, Mar. Biol., 160, 2207–2245, 2013.
Gräwe, U., Freidland, R., and Burchard, H.: The future of the western
Baltic Sea: two possible scenarios, Ocean Dynam., 63, 901–921, 2013.
Gustafsson, E., Wällstedt, T., Humborg, C., Mörth, C. M., and
Gustafsson, B. G.: External total alkalinity loads versus internal
generation: The influence of nonriverine alkalinity sources in the Baltic
Sea, Global Biochem. Cy., 28, 1358–1370, 2014.
Haapala, J.: Upwelling and its influence on nutrient concentration in the
coastal area of the Hanko Peninsula, Entrance of the Gulf of Finland, Estuar.
Coast. Shelf S., 38, 507–521, 1994.
Haynert, K., Schönfeld, J., Schiebel, R., Wilson, B., and Thomsen, J.:
Response of benthic foraminifera to ocean acidification in their natural
sediment environment: a long-term culturing experiment, Biogeosciences, 11,
1581–1597, https://doi.org/10.5194/bg-11-1581-2014, 2014.
Heinemann, A., Fietzke, J., Melzner, F., Böhm, F., Thomsen, J.,
Garbe-Schönberg, D., and Eisenhauer, A.: Conditions of Mytilus edulis extracellular body fluids and shell composition in a pH-treatment
experiment: Acid-base status, trace elements and δ11B, Geochem.
Geophy. Geosy., 13, Q01005, https://doi.org/10.1029/2011GC003790, 2012.
Ip, Y. K. and Krishnaveni, P.: Incorporation of Strontium (90Sr2+)
into the skeleton of the hermatypic coral Galaxea fascicularis, J.
Exp. Zool., 258, 273–276, 1991.
Johannesson, K., Smolarz, K., Grahn, M., and Andre, C.: The Future of Baltic
Sea Populations: Local Extinction or Evolutionary Rescue?, AMBIO, 40,
179–190, 2011.
Juhna, T. and Klavins, M.: Water-quality changes in Latvian and Riga
1980–2000: Possibilities and Problems, AMBIO, 30, 306–314, 2001.
Kester, D. R., Duedall, I. W., Connors, D. N., and Pytkowicz, R. M.:
Preparation of artificial seawater, Limnol. Oceanogr., 12, 176–179, 1967.
Kniprath, E.: Larval development of the shell and the shell gland in
Mytilus (Bivalvia), Roux. Arch. Dev. Biol., 188, 201–204, 1980.
Kremling, K. and Wilhelm, G.: Recent increase of the calcium concentrations
in Baltic Sea waters, Mar. Pollut. Bull., 34, 763–767, 1997.
Kube, S., Gerber, A., Jansen, J. M., and Schiedek, D.: Patterns of organic
osmolytes in two marine bivalves, Macoma baltica, and
Mytilus spp., along their European distribution, Mar. Biol., 149,
1387–1396, 2006.
Larsson, J., Lind, E. E., Corell, H., Smolarz, K., and Lönn, M.:
Regional genetic differentiation in the blue mussel from the Baltic Sea,
Estuar. Coast. Shelf S., 295, 98–109, 2017.
Lucas, A. and Rangel, C.: Detection of the first larval feeding in
Crassostrea gigas using the epifluorescence microscope, Aquaculture,
30, 369–374, 1983.
Maar, M., Saurel, C., Landes, A., Dolmer, P., and Petersen, J. K.: Growth
potential of blue mussels (M. edulis) exposed to different
salinities evaluated by a Dynamic Energy Budget model, J. Marine Syst., 148,
48–55, 2015.
Maeda-Martinez, A. N.: The rates of calcium deposition in shells of molluscan
larvae, Comp. Biochem. Phys. A, 86, 21–28, 1987.
Malone, P. G. and Dodd, J. R.: Temperature and salinity effects on
calcification rate in Mytilus edulis and its paleoecological
implications, Limnol. Oceanogr., 12, 432–436, 1967.
Martin, G., Kotta, J., Möller, T., and Herkül, K.: Spatial
distribution of marine benthic habitats in the Estonian coastal sea,
northeastern Baltic Sea, Est. J. Ecol., 62, 165–191, 2013.
McConnaughey, T. A. and Gillikin, D. P.: Carbon isotopes in mollusk shell
carbonates, Geo-Mar. Lett., 28, 287–299, 2008.
Meier, H. E. M., Kjellström, E., and Graham, L. P.: Estimating
uncertainties of projected Baltic Sea salinity in the late 21st century,
Geophys. Res. Lett., 33, L15705, https://doi.org/10.1029/2006GL026488, 2006.
Melzner, F., Stange, P., Trübenbach, K., Thomsen, J., Casties, I.,
Panknin, U., Gorb, S., and Gutowska, M. A.: Food supply and seawater
pCO2 impact calcification and internal shell dissolution in the Blue
Mussel Mytilus edulis, PLOS ONE, 6, e24223, https://doi.org/10.1371/journal.pone.0024223, 2011.
Melzner, F., Thomsen, J., Koeve, W., Oschlies, A., Gutowska, M. A., Bange, H.
W., Hansen, H. P., and Körtzinger, A.: Future ocean acidification will be
amplified by hypoxia in coastal habitats, Mar. Biol., 160, 1875–1888, 2013.
Miller, A. W., Reynolds, A. C., Sobrino, C., and Riedel, G. F.: Shellfish
face uncertain future in high CO2 world: Influence of acidification on
oyster larvae calcification and growth in estuaries, PLOS ONE, 4, e5661,
https://doi.org/10.1371/journal.pone.0005661,
2009.
Millero, F.: The conductivity-density-salinity-chlorinity relationships for
estuarine water, Limnol. Oceanogr., 29, 1317–1321, 1984.
Mucci, A.: The solubility of calcite and aragonite in seawater at various
salinities, temperatures, and one atmosphere total pressure, Am. J. Sci., 28,
780–799, 1983.
Müller, J., Schneider, B., and Rehder, G.: Long-term alkalinity trends in
the Baltic Sea and implications for Co2-induced acidification, Limnol.
Oceanogr., 61, 1984–2002, 2016.
Myrberg, K. and Andrejev, O.: Main upwelling regions in the Baltic Sea – a
statistical analysis based on three-dimensional modelling, Boreal Environ.
Res., 8, 97–112, 2003.
Natochin, Y. V., Berger, V. Y., Khlebovich, V. V., Lavrova, E. A., and
Michailova, O. Y.: The participation of electrolytes in adaptation mechanisms
of intertidal molluscs' cells to altered salinity, Comp. Biochem. Phys. A,
63, 115–119, 1979.
Ohlson, M. and Anderson, L.: Recent investigation of total carbonate in the
Baltic Sea: changes from the past as a result of acid rain?, Mar. Chem., 30,
259–267, 1990.
Podbielski, I., Bock, C., Lenz, M., and Melzner, F.: Using the critical
salinity (Scrit) concept to predict invasion potential of the
anemone Diadumene lineata in the Baltic Sea, Mar. Biol., 163, 227,
https://doi.org/10.1007/s00227-016-2989-5,
2016.
Ries, J. B.: Review: geological and experimental evidence for secular
variation in seawater Mg ∕ Ca (calcite-aragonite seas) and its effects on
marine biological calcification, Biogeosciences, 7, 2795–2849,
https://doi.org/10.5194/bg-7-2795-2010, 2010.
Riisgard, H. U., Larsen, P. S., Turja, R., and Lundgreen, K.: Dwarfism of
blue mussels in the lower saline Baltic Sea – growth to the lower salinity
limit, Mar. Ecol.-Prog. Ser., 517, 181–192, 2014.
Roy, R. N., Roy, L. N., Vogel, K. M., Porter-Moore, C., Pearson, T., Good, C.
E., Millero, F. J., and Campbell, D.: The dissociation constants of carbonic
acid in seawater at salinities 5 to 45 and temperatures 0 to 45 ∘C,
Mar. Chem., 44, 249–267, 1993.
Saderne, V., Fietzek, P., and Herman, P. M. J.: Extreme variations of
pCO2 and pH in a macrophyte meadow of the Baltic Sea in summer: Evidence
of the effect of photosynthesis and local upwelling, PLOS ONE, 8, e62689,
https://doi.org/10.1371/journal.pone.0062689,
2013.
Schneider, B. and Kuss, J.: Past and present productivity of the Baltic Sea
inferred from pCO2 data, Cont. Shelf Res., 24, 1611–1622, 2004.
Silva, A. L. and Wright, S. H.: Short-term cell volume regulation in
Mytilus californianus gill, J. Exp. Biol., 194, 47–68, 1994.
Stuckas, H., Knobel, L., Schade, H., Breusing, C., Hinrichsen, H.-H., Bartel,
M., Langguth, K., and Melzner, F.: Combining hydrodynamic modelling with
genetics: Can passive larval drift shape the genetic structure of Baltic
Mytilus populations?, Mol. Ecol., 26, 2765–2782, 2017.
Stumpp, M., Hu, M., Casties, I., Saborowski, R., Bleich, M., Melzner, F., and
Dupont, S.: Digestion in sea urchin larvae impaired under ocean
acidification, Nat. Clim. Change, 3, 1044–1049, 2013.
Tambutte, E., Allemand, D., Mueller, E., and Jaubert, J.: A compartimental
approach to the mechanism of calcification in hermatypic corals, J. Exp.
Biol., 199, 1029–1041, 1996.
Thomsen, J., Gutowska, M. A., Saphörster, J., Heinemann, A.,
Trübenbach, K., Fietzke, J., Hiebenthal, C., Eisenhauer, A.,
Körtzinger, A., Wahl, M., and Melzner, F.: Calcifying invertebrates
succeed in a naturally CO2-rich coastal habitat but are threatened by high
levels of future acidification, Biogeosciences, 7, 3879–3891,
https://doi.org/10.5194/bg-7-3879-2010, 2010.
Thomsen, J., Haynert, K., Wegner, K. M., and Melzner, F.: Impact of seawater
carbonate chemistry on the calcification of marine bivalves, Biogeosciences,
12, 4209–4220, https://doi.org/10.5194/bg-12-4209-2015, 2015.
Thomsen, J., Stapp, L. S., Haynert, K., Schade, H., Danelli, M., Lannig, G.,
Wegner, K. M., and Melzner, F.: Naturally acidified habitat selects for ocean
acidification–tolerant mussels, Sci. Adv., 3, e1602411, https://doi.org/10.1126/sciadv.1602411,
2017a.
Thomsen, J., Ramesh, K., Sanders, T., Bleich, M., and Melzner, F.: Effects of
seawater calcium on calcification in mussel larvae, PANGAEA,
https://doi.org/10.1594/PANGAEA.871804, 2017b.
Waldbusser, G. G., Hales, B., Langdon, C. J., Haley, B. A., Schrader, P.,
Brunner, E. L., Gray, M. W., Miller, C. A., and Gimenez, I.: Saturation-state
sensitivity of marine bivalve larvae to ocean acidification, Nat. Clim.
Change, 5, 273–280, 2014.
Waldbusser, G. G., Hales, B., Langdon, C. J., Haley, B. A., Schrader, P.,
Brunner, E. L., Gray, M. W., Miller, C. A., Gimenez, I., and Hutchinson,
G.: Ocean acidification has multiple modes of action in bivalve larvae, PLOS
ONE, 10, e0128376, https://doi.org/10.1371/journal.pone.0128376, 2015.
Wang, X., Fan, W., Xie, L., and Zhang, R.: Molecular cloning and distribution
of a plasma membane calcium ATPase homolog from the pearl oyster
Pinctada fucata, Tsinghua Sci. Technol., 13, 439–446, 2008.
Westerbom, M., Kilpi, M., and Mustonen, O.: Blue mussels, Mytilus edulis, at the edge of the range: population structure, growth and biomass
along a salinity gradient in the north-eastern Baltic Sea, Mar. Biol., 140,
991–999, 2002.
Whitfield, A. K., Elliott, M., Basset, A., Blaber, S. J. M., and West, R. J.:
Paradigms in estuarine ecology – A review of the Remane diagram with a
suggested revised model for estuaries, Estuar. Coast. Shelf S., 97, 78–90,
2012.
Williams, E. K. and Hall, J. A.: Seasonal and geographic variability in
toxicant sensitivity of Mytilus galloprovinicialis, Australas. J.
Ecotox., 5, 1–10, 1999.
Willmer, P. G.: Sodium fluxes and exchange pumps: Further correlates of
osmotic conformity in the nerves of an estuarine bivalve (Mytilus edulis), J. Exp. Biol., 77, 207–223, 1978.
Wright, S. H., Moon, D. A., and Silva, A. L.: Intracellular Na+ and the
control of amino acid fluxes in the integumental epithelium of a marine
bivalve, J. Exp. Biol., 142, 293–310, 1989.
Zhao, L., Schöne, B. R., and Mertz-Kruas, R.: Delineating the role of
calcium in shell formation and elemental composition of Corbicula fluminea (Bivalvia), Hydrobiologica, 790, 259–270, 2016.
Short summary
The distribution of mussel in estuaries is limited but the mechanisms are not well understood. We document for the first time that reduced Ca2+ concentration in the low saline, brackish Baltic Sea affects the ability of mussel larvae to calcify the first larval shell. As complete formation of the shell is a prerequisite for successful development, impaired calcification during this sensitive life stage can have detrimental effects on the species' ability to colonize habitats.
The distribution of mussel in estuaries is limited but the mechanisms are not well understood....
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