Articles | Volume 18, issue 2
https://doi.org/10.5194/bg-18-707-2021
© Author(s) 2021. 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-18-707-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
29 Jan 2021
Research article |
| 29 Jan 2021
| 29 Jan 2021
The patterns of elemental concentration (Ca, Na, Sr, Mg, Mn, Ba, Cu, Pb, V, Y, U and Cd) in shells of invertebrates representing different CaCO3 polymorphs: a case study from the brackish Gulf of Gdańsk (the Baltic Sea)
Anna Piwoni-Piórewicz
CORRESPONDING AUTHOR
Institute of Oceanology, Polish Academy of Sciences, Sopot, 81-712,
Poland
Stanislav Strekopytov
Imaging and Analysis Centre, Natural History Museum, London, SW7 5BD,
United Kingdom
current address: National Measurement Laboratory, LGC Limited,
Teddington, TW11 0LY, United Kingdom
Emma Humphreys-Williams
Imaging and Analysis Centre, Natural History Museum, London, SW7 5BD,
United Kingdom
Piotr Kukliński
Institute of Oceanology, Polish Academy of Sciences, Sopot, 81-712,
Poland
Department of Life Sciences, Natural History Museum, London, SW7 5BD,
United Kingdom
Related subject area
Biogeochemistry: Biomineralization
Upper-ocean flux of biogenic calcite produced by the Arctic planktonic foraminifera Neogloboquadrina pachyderma
Do bacterial viruses affect framboid-like mineral formation?
Calcification response of reef corals to seasonal upwelling in the northern Arabian Sea (Masirah Island, Oman)
Growth rate rather than temperature affects the B∕Ca ratio in the calcareous red alga Lithothamnion corallioides
Heavy metal uptake of nearshore benthic foraminifera during multi-metal culturing experiments
A stable ultrastructural pattern despite variable cell size in Lithothamnion corallioides
Decoupling salinity and carbonate chemistry: low calcium ion concentration rather than salinity limits calcification in Baltic Sea mussels
Technical note: A universal method for measuring the thickness of microscopic calcite crystals, based on bidirectional circular polarization
Carbonic anhydrase is involved in calcification by the benthic foraminifer Amphistegina lessonii
Distribution of chlorine and fluorine in benthic foraminifera
Rare earth elements in oyster shells: provenance discrimination and potential vital effects
Determining how biotic and abiotic variables affect the shell condition and parameters of Heliconoides inflatus pteropods from a sediment trap in the Cariaco Basin
Intercomparison of four methods to estimate coral calcification under various environmental conditions
Technical note: The silicon isotopic composition of choanoflagellates: implications for a mechanistic understanding of isotopic fractionation during biosilicification
Insights into architecture, growth dynamics, and biomineralization from pulsed Sr-labelled Katelysia rhytiphora shells (Mollusca, Bivalvia)
Subaqueous speleothems (Hells Bells) formed by the interplay of pelagic redoxcline biogeochemistry and specific hydraulic conditions in the El Zapote sinkhole, Yucatán Peninsula, Mexico
Kinetics of calcite precipitation by ureolytic bacteria under aerobic and anaerobic conditions
Coupled calcium and inorganic carbon uptake suggested by magnesium and sulfur incorporation in foraminiferal calcite
Planktonic foraminiferal spine versus shell carbonate Na incorporation in relation to salinity
Precipitation of calcium carbonate mineral induced by viral lysis of cyanobacteria: evidence from laboratory experiments
Mineral formation induced by cable bacteria performing long-distance electron transport in marine sediments
Variation in brachiopod microstructure and isotope geochemistry under low-pH–ocean acidification conditions
Weaving of biomineralization framework in rotaliid foraminifera: implications for paleoceanographic proxies
Marine and freshwater micropearls: biomineralization producing strontium-rich amorphous calcium carbonate inclusions is widespread in the genus Tetraselmis (Chlorophyta)
Carbon and nitrogen turnover in the Arctic deep sea: in situ benthic community response to diatom and coccolithophorid phytodetritus
Technical note: A refinement of coccolith separation methods: measuring the sinking characteristics of coccoliths
Improving the strength of sandy soils via ureolytic CaCO3 solidification by Sporosarcina ureae
Impact of salinity on element incorporation in two benthic foraminiferal species with contrasting magnesium contents
Calcification in a marginal sea – influence of seawater [Ca2+] and carbonate chemistry on bivalve shell formation
Effect of temperature rise and ocean acidification on growth of calcifying tubeworm shells (Spirorbis spirorbis): an in situ benthocosm approach
Phosphorus limitation and heat stress decrease calcification in Emiliania huxleyi
Anatomical structure overrides temperature controls on magnesium uptake – calcification in the Arctic/subarctic coralline algae Leptophytum laeve and Kvaleya epilaeve (Rhodophyta; Corallinales)
Coral calcifying fluid aragonite saturation states derived from Raman spectroscopy
Impact of trace metal concentrations on coccolithophore growth and morphology: laboratory simulations of Cretaceous stress
Ba incorporation in benthic foraminifera
Size-dependent response of foraminiferal calcification to seawater carbonate chemistry
Technical note: an economical apparatus for the observation and harvest of mineral precipitation experiments with light microscopy
Physiology regulates the relationship between coccosphere geometry and growth phase in coccolithophores
Trends in element incorporation in hyaline and porcelaneous foraminifera as a function of pCO2
Decoupled carbonate chemistry controls on the incorporation of boron into Orbulina universa
Mineralogical response of the Mediterranean crustose coralline alga Lithophyllum cabiochae to near-future ocean acidification and warming
Temperature affects the morphology and calcification of Emiliania huxleyi strains
Skeletal mineralogy of coral recruits under high temperature and pCO2
Direct uptake of organically derived carbon by grass roots and allocation in leaves and phytoliths: 13C labeling evidence
pH up-regulation as a potential mechanism for the cold-water coral Lophelia pertusa to sustain growth in aragonite undersaturated conditions
Iron encrustations on filamentous algae colonized by Gallionella-related bacteria in a metal-polluted freshwater stream
Ocean acidification does not affect magnesium composition or dolomite formation in living crustose coralline algae, Porolithon onkodes in an experimental system
Reconsidering the role of carbonate ion concentration in calcification by marine organisms
Impact of seawater carbonate chemistry on the calcification of marine bivalves
Impact of seawater [Ca2+] on the calcification and calciteMg / Ca of Amphistegina lessonii
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.
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
Jörn Thomsen, Kirti Ramesh, Trystan Sanders, Markus Bleich, and Frank Melzner
Biogeosciences, 15, 1469–1482, https://doi.org/10.5194/bg-15-1469-2018, https://doi.org/10.5194/bg-15-1469-2018, 2018
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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.
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.
Rosie M. Sheward, Alex J. Poulton, Samantha J. Gibbs, Chris J. Daniels, and Paul R. Bown
Biogeosciences, 14, 1493–1509, https://doi.org/10.5194/bg-14-1493-2017, https://doi.org/10.5194/bg-14-1493-2017, 2017
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Our culture experiments on modern Coccolithophores find that physiology regulates shifts in the geometry of their carbonate shells (coccospheres) between growth phases. This provides a tool to access growth information in modern and past populations. Directly comparing modern species with fossil coccospheres derives a new proxy for investigating the physiology that underpins phytoplankton responses to environmental change through geological time.
Inge van Dijk, Lennart J. de Nooijer, and Gert-Jan Reichart
Biogeosciences, 14, 497–510, https://doi.org/10.5194/bg-14-497-2017, https://doi.org/10.5194/bg-14-497-2017, 2017
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Culturing foraminifera under controlled pCO2 conditions shows that incorporation of certain elements (Zn, Ba) into foraminiferal shells is impacted by the inorganic carbonate system. Modeling the chemical speciation of these elements suggests that incorporation is determined by the availability of free ions. Furthermore, analyzing and comparing trends in element incorporation in hyaline and porcelaneous species may provide constrains on the differences between their calcification strategies.
Ella L. Howes, Karina Kaczmarek, Markus Raitzsch, Antje Mewes, Nienke Bijma, Ingo Horn, Sambuddha Misra, Jean-Pierre Gattuso, and Jelle Bijma
Biogeosciences, 14, 415–430, https://doi.org/10.5194/bg-14-415-2017, https://doi.org/10.5194/bg-14-415-2017, 2017
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To calculate the seawater carbonate system, proxies for 2 out of 7 parameters are required. The boron isotopic composition of foraminifera shells can be used as a proxy for pH and it has been suggested that B / Ca ratios may act as a proxy for carbonate ion concentration. However, differentiating between the effects of pH and [CO32−] is problematic, as they co-vary in natural systems. To deconvolve the effects, we conducted culture experiments with the planktonic foraminifer Orbulina universa.
Merinda C. Nash, Sophie Martin, and Jean-Pierre Gattuso
Biogeosciences, 13, 5937–5945, https://doi.org/10.5194/bg-13-5937-2016, https://doi.org/10.5194/bg-13-5937-2016, 2016
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We carried out a 1-year experiment on coralline algae to test how higher CO2 and temperature might change the mineral composition of the algal skeleton. We expected there to be a decline in magnesium with CO2 and an increase with temperature. We found that CO2 did not change the mineral composition, but higher temperature increased the amount of magnesium.
Anaid Rosas-Navarro, Gerald Langer, and Patrizia Ziveri
Biogeosciences, 13, 2913–2926, https://doi.org/10.5194/bg-13-2913-2016, https://doi.org/10.5194/bg-13-2913-2016, 2016
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The global warming debate has sparked an unprecedented interest in temperature effects on coccolithophores. We show that sub-optimal growth temperatures lead to an increase in malformed coccoliths in a strain-specific fashion and the inorganic / organic carbon has a minimum at optimum growth temperature. Global warming might cause a decline in coccoliths' inorganic carbon contribution to the "rain ratio", as well as improved fitness in some genotypes by reducing coccolith malformation.
T. Foster and P. L. Clode
Biogeosciences, 13, 1717–1722, https://doi.org/10.5194/bg-13-1717-2016, https://doi.org/10.5194/bg-13-1717-2016, 2016
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In recent years much research has focussed on whether corals will be able to build their skeletons under predicted ocean acidification. One strategy corals may employ is changing the mineralogy of their skeletons from aragonite to the less soluble polymorph of calcium carbonate; calcite. Here we show that newly settled coral recruits are unable to produce calcite in their skeletons under near-future elevations in pCO2, which may leave them more vulnerable to ocean acidification.
Anne Alexandre, Jérôme Balesdent, Patrick Cazevieille, Claire Chevassus-Rosset, Patrick Signoret, Jean-Charles Mazur, Araks Harutyunyan, Emmanuel Doelsch, Isabelle Basile-Doelsch, Hélène Miche, and Guaciara M. Santos
Biogeosciences, 13, 1693–1703, https://doi.org/10.5194/bg-13-1693-2016, https://doi.org/10.5194/bg-13-1693-2016, 2016
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This 13C labeling experiment demonstrates that carbon can be absorbed by the roots, translocated in the plant, and ultimately fixed in organic compounds subject to occlusion in silica particles that form inside plant cells (phytoliths). Plausible forms of carbon absorbed, translocated, and fixed in phytoliths are assessed. Implications for our understanding of the C cycle at the plant-soil-atmosphere interface are discussed.
M. Wall, F. Ragazzola, L. C. Foster, A. Form, and D. N. Schmidt
Biogeosciences, 12, 6869–6880, https://doi.org/10.5194/bg-12-6869-2015, https://doi.org/10.5194/bg-12-6869-2015, 2015
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We investigated the ability of cold-water corals to deal with changes in ocean pH. We uniquely combined morphological assessment with boron isotope analysis to determine if changes in growth are related to changes in control of calcification pH. We found that the cold-water coral Lophelia pertusa can maintain the skeletal morphology, growth patterns as well as internal calcification pH. This has important implications for their future occurrence and explains their cosmopolitan distribution.
J. F. Mori, T. R. Neu, S. Lu, M. Händel, K. U. Totsche, and K. Küsel
Biogeosciences, 12, 5277–5289, https://doi.org/10.5194/bg-12-5277-2015, https://doi.org/10.5194/bg-12-5277-2015, 2015
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We studied filamentous macroscopic algae growing in metal-rich stream water that leaked from a former uranium-mining district. These algae were encrusted with Fe-deposits that were associated with microbes, mainly Gallionella-related Fe-oxidizing bacteria, and extracellular polymeric substances. Algae with a lower number of chloroplasts often exhibited discontinuous series of precipitates, likely due to the intercalary growth of algae which allowed them to avoid detrimental encrustation.
M. C. Nash, S. Uthicke, A. P. Negri, and N. E. Cantin
Biogeosciences, 12, 5247–5260, https://doi.org/10.5194/bg-12-5247-2015, https://doi.org/10.5194/bg-12-5247-2015, 2015
L. T. Bach
Biogeosciences, 12, 4939–4951, https://doi.org/10.5194/bg-12-4939-2015, https://doi.org/10.5194/bg-12-4939-2015, 2015
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Calcification by marine organisms reacts to changing seawater carbonate chemistry, but it is unclear which components of the carbonate system drive the observed response. This study uncovers proportionalities between different carbonate chemistry parameters. These enable us to understand why calcification often correlates well with carbonate ion concentration, and they imply that net CaCO3 formation in high latitudes is not more vulnerable to ocean acidification than formation in low latitudes.
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
A. Mewes, G. Langer, S. Thoms, G. Nehrke, G.-J. Reichart, L. J. de Nooijer, and J. Bijma
Biogeosciences, 12, 2153–2162, https://doi.org/10.5194/bg-12-2153-2015, https://doi.org/10.5194/bg-12-2153-2015, 2015
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A culture study with the benthic foraminifer Amphistegina lessonii was conducted at varying seawater [Ca2+] and constant [Mg2+]. Results showed optimum growth rates and test thickness at ambient seawater Mg/Ca and a calcite Mg/Ca which is controlled by the relative seawater ratio. Results support the conceptual biomineralization model by Nehrke et al. (2013); however, our refined flux-based model suggests transmembrane transport fractionation that is slightly weaker than expected.
Cited articles
Allison, N., Finch, A. A., Sutton, S. R., and Newville, M.: Strontium
heterogeneity and speciation in coral aragonite: implications for the
strontium paleothermometer, Geochim. Cosmochim. Ac., 65, 2669–2676,
https://doi.org/10.1016/S0016-7037(01)00628-7, 2001.
Ashraf, M. P., Meenakumari, B., and Thomas, S. N.: Seasonal variation of
metal concentration in barnacles (Balanus spp.) of Cochin estuary, south-west coast of India, Fish. Technol., 44, 73–84, 2007.
Azizi, G., Akodad, M., Baghour, M., Layachi, M., and Moumen, A.: The use of
Mytilus spp. mussels as bioindicators of heavy metal pollution in the coastal environment, a review, J. Mater. Environ. Sci., 9, 1170–1181,
2018.
Balthasar, U. and Cusack, M.: Aragonite-calcite seas – quantifying the gray
area, Geology, 43, 99–102, https://doi.org/10.1130/G36293.1, 2015.
Barker, S., Greaves, M., and Elderfield, H.: A study of cleaning procedures
used for foraminiferal Mg∕Ca paleothermometry, Geochem. Geophy. Geosys., 4, 8407, https://doi.org/10.1029/2003GC000559, 2003.
Blanchard, S. C. and Chasteen, N. D.: Determination of manganese (II) in powdered barnacle shells by electron paramagnetic resonance, Anal. Chim. Acta, 82, 113–119, https://doi.org/10.1016/S0003-2670(01)82209-1, 1976.
Behrends, B., Hertweck, G., Liebezeit, G., and Goodfriend, G.: Earliest
Holocene occurrence of the soft-shell clam, Mya arenaria, in the Greifswalder Bodden, southern Baltic, Mar. Geol., 216, 79–82,
https://doi.org/10.1016/j.margeo.2005.01.002, 2005.
Beldowski, J., Löffler, A., Schneider, B., and Joensuu, L.: Distribution
and biogeochemical control of total CO2 and total alkalinity in the
Baltic Sea, J. Mar. Syst., 81, 252–259,
https://doi.org/10.1016/j.jmarsys.2009.12.020, 2010.
Bellotto, V. R. and Miekeley, N.: Trace metals in mussel shells and
corresponding soft tissue samples: a validation experiment for the use of
Perna perna shells in pollution monitoring, Anal. Bioanal. Chem., 389, 769–776, https://doi.org/10.1007/s00216-007-1420-y, 2007.
Bendell-Young, L. I., Thomas, C. A., and Stecko, J. P.: Contrasting the
geochemistry of oxic sediments across ecosystems: a synthesis, Appl.
Geochem., 17, 1563–1582, 2002.
Bentov, S. and Erez, J.: Novel observations on biomineralization processes
in foraminifera and implications for Mg∕Ca ratio in the shells, Geology, 33, 841, https://doi.org/10.1130/G21800.1, 2005.
Blackmore, G. and Wang, W. X.: Uptake and efflux of Cd and Zn by the green
mussel Perna viridis after metal preexposure, Environ. Sci. Technol., 36, 989–995, https://doi.org/10.1021/es0155534, 2002.
Bornhold, B. D. and Milliman, J. D.: Generic and environmental control of
carbonate mineralogy in serpulid (Polychaete) tubes, J. Geol., 81, 363–373,
https://doi.org/10.1086/627876, 1973.
Bourget, E.: Barnacle shells: composition, structure and growth, in:
Barnacle Biology, edited by: Southward, A. J. and Balkema, A. A., Rotterdam, the Netherlands, https://doi.org/10.1201/9781315138053-14, 267–285, 1987.
Bourget, F.: Environmental and structural control of trace elements in
barnacle shells, Mar. Biol., 28, 27–36, https://doi.org/10.1007/BF00389114,
1974.
Brannon, A. C. and Rao, K. R.: Barium, strontium and calcium levels in the
exoskeleton, hepatopancreas and abdominal muscle of the grass shrimp,
Palaemonetes pugio: relation to molting and exposure to barite, Comp. Biochem. Phys. A, 63, 261–274, https://doi.org/10.1016/0300-9629(79)90158-0, 1979.
Bulnheim, H. P. and Gosling, E.: Population genetic structure of mussels
from the Baltic Sea, Helgoländer Meeresunters., 42, 113–129,
https://doi.org/10.1007/BF02364207, 1988.
Cai, W. J., Hu, X., Huang, W. J., Jiang, L. Q., Wang, Y., Peng, T. H., and
Zhang, X.: Alkalinity distribution in the western North Atlantic Ocean
margins, J. Geophys. Res., 115, C08014,
https://doi.org/10.1029/2009JC005482, 2010.
Carpenter, J. and Kyger, C.: Sr∕Mg ratios of modern marine calcite:
empirical indicators of ocean chemistry and precipitation rate, Geochim.
Cosmochim. Ac., 56, 1837–1849, https://doi.org/10.1016/0016-7037(92)90314-9, 1992.
Carré, M., Bentaleb, I., Bruguier, O., Ordinola, E., Barrett, N. T., and
Fontugne, M.: Calcification rate influence on trace element concentrations
in aragonitic bivalve shells: evidences and mechanisms, Geochim. Cosmochim.
Acta, 70, 4906–4920, https://doi.org/10.1016/j.gca.2006.07.019, 2006.
Catsiki, V. A., Katsilieri, C., and Gialamas, V.: Chromium distribution in
benthic species from a gulf receiving tannery wastes (Gulf of Geras –
Lesbos island, Greece), Sci. Total Environ., 145, 173–185,
https://doi.org/10.1016/0048-9697(94)90308-5, 1994.
Cohen, A. L. and McConnaughey, T. A.: Geochemical perspectives on coral
mineralization, Rev. Mineral. Geochem., 354, 151–187,
https://doi.org/10.2113/0540151, 2003.
Cubadda, F., Superiore, I., Conti, M. E., Cubadda, F., Enrique, M., and
Campanella, L.: Size-dependent concentrations of trace metals in four
Mediterranean gastropods, Chemosphere, 45, 561–569,
https://doi.org/10.1016/S0045-6535(01)00013-3, 2001.
Cusack, M. and Freer, A.: Biomineralization: elemental and organic influence
in carbonate systems, Chem. Rev., 108, 4433–4454,
https://doi.org/10.1021/cr078270o, 2008.
Cyberski, J., Grześ, M., Gurty-Korycka, M., Nachlik, E., and Kundziewicz,
W. W.: History of floods on the river Vistula, Hydrol. Sci. J., 51,
799–817, https://doi.org/10.1623/hysj.51.5.799, 2006.
Dalbeck, P.: Crystallography, Stable Isotope and Trace Element Analysis of
Mytilus edulis Shells in the Context of Ontogeny, PhD thesis, University of Glasgow, UK, 235 pp., 2008.
Davis, K. J., Dove, P. M., and De Yoreo, J. J.: The role of Mg2+ as an
impurity in calcite growth, Science, 290, 1134–1138,
https://doi.org/10.1126/science.290.5494.1134, 2000.
de Boer, R. B.: Stability of Mg-Ca carbonates, Geochim. Cosmochim. Ac., 41,
265–270, https://doi.org/10.1016/0016-7037(77)90234-4, 1977.
De Choudens-Sanchez, V. and Gonzalez, L. A.: Calcite and aragonite
precipitation under controlled instantaneous supersaturation: elucidating
the role of CaCO3 saturation state and Mg∕Ca ratio on calcium carbonate polymorphism, J. Sediment. Res., 79, 363–376,
https://doi.org/10.2110/jsr.2009.043, 2009.
De Nooijer, L. J., Spero, H. J., Erez, J., Bijma, J., and Reichart, G. J.:
Biomineralization in perforate foraminifera, Earth-Sci. Rev., 135,
48–58, https://doi.org/10.1016/j.earscirev.2014.03.013, 2014.
Dickson, J. A. D.: Echinoderm skeletal preservation; calcite-aragonite seas
and the Mg∕Ca ratio of Phanerozoic oceans, J. Sediment. Res., 74, 355–365, https://doi.org/10.1306/112203740355, 2004.
Dodd, J. R. and Crisp, E. L.: Non-linear variation with salinity of Sr∕Ca and Mg∕Ca ratios in water and aragonitic bivalve shells and implications for paleosalinity studies, Paleogeogr. Paleocl., 38, 45–56,
1982.
Dove, P. M.: The rise of skeletal biominerals, Elements, 6, 37–42,
https://doi.org/10.2113/gselements.6.1.37, 2010.
Elder, J. F. and Collins, J.: Freshwater molluscs as indicators of
bioavailability and toxicity of metals in surface-water systems, in: Reviews
of Environmental Contamination and Toxicology, vol. 122, edited by: Ware,
G. W., Springer, New York, USA, 37–69,
https://doi.org/10.1007/978-1-4612-3198-1_2, 1991.
Elderfield, H. and Ganssen, G.: Past temperature and δ18O of
surface ocean waters inferred from foraminiferal Mg∕Ca ratios, Nature, 405, 442–445, https://doi.org/10.1038/35013033, 2000.
Findlater, G., Shelton, A., Rolin, T., and Andrews, J.: Sodium and strontium
in mollusc shells: preservation, palaeosalinity and palaeotemperature of the
Middle Pleistocene of eastern England, P. Geologist. Assoc., 125, 14–19,
https://doi.org/10.1016/j.pgeola.2013.10.005, 2014.
Findlay, H. S., Tyrrell, T., Bellerby, R. G. J., Merico, A., and Skjelvan, I.: Carbon and nutrient mixed layer dynamics in the Norwegian Sea, Biogeosciences, 5, 1395–1410, https://doi.org/10.5194/bg-5-1395-2008, 2008.
Freitas, P., Clarke, L. J., Kennedy, H., Richardson, C., and Abrantes, F.:
Mg/Ca, Sr/Ca, and stable-isotope (δ18O and δ13C)
ratio profiles from the fan mussel Pinna nobilis: seasonal records and temperature relationships, Geochem. Geophy. Geosy., 6, Q04D14,
https://doi.org/10.1029/2004GC000872, 2005.
Freitas, P. S., Clarke, L. J., Kennedy, H., Richardson, C. A., and Abrantes,
F.: Environmental and biological controls on elemental (Mg∕Ca, Sr∕Ca and Mn∕Ca) ratios in shells of the king scallop Pecten maximus, Geochim. Cosmochim. Ac., 70,
5119–5133, https://doi.org/10.1016/j.gca.2006.07.029, 2006.
Friel, D. D. and Tsien, R. W.: Voltage-gated calcium channels: direct
observation of the anomalous mole fraction effect at the single-channel
level, P. Natl. Acad. Sci. USA, 86, 5207–5211,
https://doi.org/10.1073/pnas.86.13.5207, 1989.
Fritioff, A., Kautsky, L., and Greger, M.: Influence of temperature and
salinity on heavy metal uptake by submersed plants, Environ. Pollut., 133,
265–274, https://doi.org/10.1016/j.envpol.2004.05.036, 2005.
Gaffey, S. J.: Water in skeletal carbonates, J. Sediment. Res., 58,
397–414, 1998.
Gillikin, D. P.: Geochemisry of Marine Bivalve Shells: the Potential for
Paleoenvironmental Reconstruction, PhD thesis, Vrije Universiteit Brussel,
Belgium, 258 pp., 2005.
Gillikin, D. P., Dehairs, F., Baeyens, W., Navez, J., Lorrain, A., and
Andre, L.: Inter- and intra-annual variations of Pb∕Ca ratios in clam shells
(Mercenaria mercenaria): a record of anthropogenic lead pollution?, Mar. Pollut. Bull., 50, 1530–1540, https://doi.org/10.1016/j.marpolbul.2005.06.020, 2005a.
Gillikin, D. P., Lorrain, A., Navez, J., Taylor, J. W., Andre, L., Keppens,
E., Baeyens, W., and Dehairs, F.: Strong biological controls on Sr∕Ca ratios in aragonitic marine bivalve shells, Geochem. Geophy. Geosy., 6, Q05009, https://doi.org/10.1029/2004GC000874, 2005b.
Gillikin, D. P., Dehairs, F., Lorrain, A., Steenmans, D., Baeyens, W., and
André, L.: Barium uptake into the shells of the common mussel (Mytilus edulis) and the
potential for estuarine paleo-chemistry reconstruction, Geochim. Cosmochim.
Ac., 70, 395–407, https://doi.org/10.1016/j.gca.2005.09.015, 2006.
Glasby, G. P. and Szefer, P.: Marine pollution in Gdansk Bay, Puck Bay and
the Vistula Lagoon, Poland: an overview, Sci. Total Environ., 212, 49–57,
https://doi.org/10.1016/S0048-9697(97)00333-1, 1998.
Glasby, G. P., Szefer, P., Geldon, J., and Warzocha, J.: Heavy-metal
pollution of sediments from Szczecin Lagoon and the Gdansk Basin, Poland,
Sci. Total Environ., 330, 249–269,
https://doi.org/10.1016/j.scitotenv.2004.04.004, 2004.
Gofas, S.: Mytilus trossulus Gould, 1850, MolluscaBase, available at: http://www.marinespecies.org/aphia.php?p=taxdetails&id=140482 (last access: 26 January 2021), 2004.
Góral, M., Szefer, P., Ciesielski, T., and Warzocha, J.: Distribution
and relationships of trace metals in the isopod Saduria entomon and adjacent bottom sediments in the southern Baltic, J. Environ. Monit., 11, 1875–1882, https://doi.org/10.1039/b900366e, 2009.
Gordon, C., Carr, R., and Larson, R.: Influence of environmental factors on
the sodium and manganese content of barnacle shells, Limnol. Oceanogr., 15,
461–466, 1970.
Heinemann, A., Fietzke, J., Eisenhauer, A., and Zumholz, K.: Modification of
Ca isotope and trace metal composition of the major matrices involved in
shell formation of Mytilus edulis, Geochem. Geophy. Geosy., 9, Q01006, https://doi.org/10.1029/2007GC001777, 2008.
Heinemann, A., Hiebenthal, C., Fietzke, J., Eisenhauer, A., and Wahl, M.:
Disentangling the biological and environmental control of M. edulis shell chemistry, Geochem. Geophy. Geosy., 12, Q03009,
https://doi.org/10.1029/2010GC003340, 2011.
Hiddink, J. G., Marijnissen, S. A., Troost, K., and Wolff, W. J.: Predation
on 0-group and older year classes of the bivalve Macoma balthica: interaction of size selection and intertidal distribution of epibenthic predators, J. Exp. Mar. Bio. Ecol., 269, 223–248, https://doi.org/10.1016/S0022-0981(02)00002-3, 2002.
Holcomb, M., DeCarlo, T. M., Schoepf, V., Dissard, D., Tanaka, K., and
McCulloch, M.: Cleaning and pre-treatment procedures for biogenic and
synthetic calcium carbonate powders for determination of elemental and boron
isotopic compositions, Chem. Geol., 398, 11–21,
https://doi.org/10.1016/j.chemgeo.2015.01.019, 2015.
Iglikowska, A., Beldowski, J., Chelchowski, M., Chierici, M., Kedra, M.,
Przytarska, J., Sowa, A., and Kukliński, P.: Chemical composition of two
mineralogically contrasting Arctic bivalves' shells and their relationships
to environmental variables, Mar. Pollut. Bull., 114, 903–916,
https://doi.org/10.1016/j.marpolbul.2016.10.071, 2016.
Iglikowska, A., Ronowicz, M., Humphreys-Williams, E., and Kukliński, P.:
Trace element accumulation in the shell of the Arctic cirriped Balanus balanus, Hydrobiologia, 818, 43–56, https://doi.org/10.1007/s10750-018-3564-5, 2018.
Imai, N., Terashima, S., Itoh, S., and Ando, A.: Compilation of analytical
data on nine GSJ geochemical reference samples, “Sedimentary rock series”,
Geostand. Newsl., 20, 165–216,
https://doi.org/10.1111/j.1751-908X.1996.tb00184.x, 1996.
Inoue, M., Nohara, M., Okai, T., Suzuki, A., and Kawahata, H.:
Concentrations of trace elements in carbonate reference materials Coral
JCp-1 and Giant Clam JCt-1 by inductively coupled plasma-mass spectrometry,
Geostand. Geoanal. Res., 28, 411–416,
https://doi.org/10.1111/j.1751-908X.2004.tb00759.x, 2004.
Janssen, H. H. and Scholtz, N.: Uptake and cellular distribution of cadmium
in Mytilus edulis, Mar. Biol., 55, 133–141, https://doi.org/10.1007/BF00397309, 1979.
Jelnes, J. E., Petersen, G. H., and Russell, P. C.: Isoenzyme taxonomy
applied on four species of Cardium from Danish and British waters with a short description of the distribution of the species (Bivalvia), Ophelia, 9, 15–19, https://doi.org/10.1080/00785326.1971.10430087, 1971.
Kawahata, H., Fujita, K., Iguchi, A., Inoue, M., Iwasaki, S., Kuroyanagi,
A., Maeda, A., Manaka, T., Moriya, K., Takagi, H., Toyofuku, T., Yoshimura,
T., and Suzuki, A.: Perspective on the response of marine calcifiers to
global warming and ocean acidification – behavior of corals and
foraminifera in a high CO2 world “hot house”, Prog. Earth Planet.
Sci., 6, 5, https://doi.org/10.1186/s40645-018-0239-9, 2019.
Kerckhof, F.: Barnacles (Cirripedia, Balanomorpha) in Belgian waters, an
overview of the species and recent evolutions, with emphasis on exotic
species, Bull. Inst. Roy. Sci. Nat. Belg., Biol., 72, 93–104, 2002.
Khim, B., Krantz, D. E., Cooper, L. W., and Grebmeie, J. M.: Seasonal
discharge of estuarine freshwater to the western Chukchi Sea shelf
identified in stable isotope profiles of mollusk shells, J. Geophys. Res.-Ocean., 108, 3300, https://doi.org/10.1029/2003JC001816, 2003.
Kim, G., Alleman, L. Y., and Church, T. M.: Accumulation records of
radionuclides and trace metals in two contrasting Delaware salt marshes,
Mar. Chem., 87, 87–96, https://doi.org/10.1016/j.marchem.2004.02.002, 2004.
Klein, R. T., Lohmann, K. C., and Thayer, C. W.: Sr∕Ca and 13C ∕ 12C
ratios in skeletal calcite of Mytilus trossulus: covariation with metabolic rate, salinity,
and carbon isotopic composition of seawater, Geochim. Cosmochim. Ac., 60,
4207–4221, https://doi.org/10.1016/S0016-7037(96)00232-3,
1996.
Kruk-Dowgiałło, L. and Szaniawska, A.: Gulf of Gdańsk and Puck Bay,
in: Ecology of Baltic Coastal Waters, edited by: Schiewer, U., Springer,
Berlin, Heidelberg, Germany, 139–165,
https://doi.org/10.1007/978-3-540-73524-3_7, 2008.
Kuklinski, P. and Taylor, P. D.: Mineralogy of Arctic bryozoan skeletons in
a global context, Facies, 55, 489–500,
https://doi.org/10.1007/s10347-009-0179-3, 2009.
Larsson, J., Lind, E. E., Corell, H., Grahn, M., Smolarz, K., and Lönn,
M.: Regional genetic differentiation in the blue mussel from the Baltic Sea
area, Estuar. Coast. Shelf Sci., 195, 98–109,
https://doi.org/10.1016/j.ecss.2016.06.016, 2017.
Lauringson, V., Kotta, J., Orav-Kotta, H., and Kaljurand, K.: Diet of
mussels Mytilus trossulus and Dreissena polymorpha in a brackish nontidal environment, Mar. Ecol., 35,
56–66, https://doi.org/10.1111/maec.12120, 2014.
Lazareth, C. E., Vander Putten, E., André, L., and Dehairs, F.:
High-resolution trace element profiles in shells of the mangrove bivalve
Isognomon ephippium: a record of environmental spatio-temporal variations?, Estuar. Coast. Shelf Sci., 57, 1103–1114, https://doi.org/10.1016/S0272-7714(03)00013-1,
2003.
Lécuyer, C. and O'Neil, J. R.: Stable isotope compositions of fluid
inclusions in biogenic carbonates, Geochim. Cosmochim. Ac., 58, 353–363,
https://doi.org/10.1016/0016-7037(94)90469-3, 1994.
Lee, B. G., Wallace, W. G., and Luoma, S. N.: Uptake and loss kinetics of
Cd, Cr and Zn in the bivalves Potamocorbula amurensis and Macoma balthica: effects of size and salinity, Mar.
Ecol. Prog. Ser., 175, 177–189, https://doi.org/10.3354/meps175177, 1998.
Lee, J. and Morse, J. W.: Influences of alkalinity and pCO2 on
CaCO3 nucleation from estimated Cretaceous composition seawater
representative of “calcite seas”, Geology, 38, 115–118,
https://doi.org/10.1130/G30537.1, 2010.
Lingard, S. M., Evans, R. D., and Bourgoin, B. P.: Method for the estimation
of organic-bound and crystal-bound metal concentrations in bivalve shells,
Bull. Environ. Contam. Toxicol., 48, 179–184,
https://doi.org/10.1007/BF00194369, 1992.
Lorens, R. B., Bender, M. L., and Island, R.: The impact of solution
chemistry on Mytilus edulis calcite and aragonite, Geochim. Cosmochim. Ac., 44,
1265–1278, https://doi.org/10.1016/0016-7037(80)90087-3, 1980.
Lowenstam, H. A. and Weiner, S.: On Biomineralization, Oxford University
Press, New York, 1989.
Loxton, J., Kuklinski, P., Barnes, D., Najorka, J., Spencer Jones, M., and
Porter, J.: Variability of Mg-calcite in Antarctic bryozoan skeletons across
spatial scales, Mar. Ecol.-Prog. Ser., 507, 169–180,
https://doi.org/10.3354/meps10826, 2014.
Loxton, J., Najorka, J., Humphreys-Williams, E., Kuklinski, P., Smith, A.
M., Porter, J. S., and Spencer Jones, M.: The forgotten variable: impact of
cleaning on the skeletal composition of a marine invertebrate, Chem. Geol.,
474, 45–57, https://doi.org/10.1016/j.chemgeo.2017.10.022, 2017.
Luoma, S. N. and Rainbow, P. S.: Why is metal bioaccumulation so variable? Biodynamics as a unifying concept, Environ. Sci. Technol., 39, 1921–1931, https://doi.org/10.1021/es048947e, 2005.
Luoma, S. N. and Rainbow, P. S.: Metal Contamination in Aquatic
Environments: Science and Lateral Management, Cambridge University Press,
Cambridge, 2008.
Mannella, G., Zanchetta, G., Regattieri, E., Perchiazzi, N., Drysdale, R.
N., Giaccio, B., Leng, M. J., and Wagneret, B.: Effects of organic removal
techniques prior to carbonate stable isotope analysis of lacustrine marls: a
case study from palaeo-lake Fucino (central Italy), Rapid Commun. Mass
Sp., 34, e8623, https://doi.org/10.1002/rcm.8623, 2020.
Marchitto, T. M., Jones, G. A., Goodfriend, G. A., and Christopher, R. W.:
Precise temporal correlation of Holocene mollusk shells using
sclerochronology, Quaternary Res., 53, 236–246,
https://doi.org/10.1006/qres.1999.2107, 2000.
Marin, F. and Luquet, G.: Molluscan shell proteins, Compt. Rend. Palevol, 3,
469–492, https://doi.org/10.1016/j.crpv.2004.07.009, 2004.
Martincic, D., Kwokal, Z., Peharec, Z., Margus, D., and Branica, M.:
Distribution of Zn, Pb, Cd and Cu between seawater and transplanted mussels
(Mytilus galloprovincialis), Sci. Total Environ., 119, 211–230,
https://doi.org/10.1016/0048-9697(92)90265-T, 1992.
Milliman, J. D.: Recent Sedimentary Carbonates. Part 1. Marine Carbonates,
Springer, Berlin, Heidelberg, Germany, 1974.
Mititelu, M., Ioniṭă, C., Ioniṭă, E., Neacşu, S. M., Amzoiu, E., Averis,
L. M. E., and Moroşan, E.: Detection of heavy metals from molluscs
shells, Ann. Univ. Craiova – Agric., Montanology, Cadastre Ser., 44,
163–166, 2014.
Morse, J. W., Wang, Q., and Tsio, M. Y.: Influences of temperature and Mg : Ca
ratio on CaCO3 precipitates from seawater, Geology, 25, 85–87,
https://doi.org/10.1130/0091-7613(1997)025<0085:IOTAMC>2.3.CO;2, 1997.
Morse, J. W., Arvidson, R. S., and Lüttge, A.: Calcium carbonate
formation and dissolution, Chem. Rev., 107, 342–381,
https://doi.org/10.1016/0166-445X(82)90002-9, 2007.
Newman, M. C. and Unger, M. A.: Uptake, biotransformation, detoxification,
elimination, and accumulation, in: Fundamentals of Ecotoxicology, 2nd Edn.,
CRC Press, Boca Raton, Florida, USA, 53–73, 2003.
Pierscieniak, K., Grzymala, J., Wolowicz, M., Pierścieniak, K., Grzymała, J., and Wołowicz, M.: Differences in reproduction and condition of
Macoma balthica and Mytilus trossulus in the Gulf of Gdansk (southern Baltic Sea) under anthropogenic
influences, Oceanol. Hydrobiol. Stud., 39, 17–32,
https://doi.org/10.2478/v10009-010-0054-0, 2010.
Pilkey, O. H. and Harris, R. C.: The effect of intertidal environment on the
composition of calcareous skeletal material, Limnol. Oceanogr., 11,
381–385, https://doi.org/10.4319/lo.1966.11.3.0381, 1966.
Piwoni-Piórewicz, A., Kukliński, P., Strekopytov, S.,
Humphreys-Williams, E., Najorka, J., and Iglikowska, A.: Size effect on the
mineralogy and chemistry of Mytilus trossulus shells from the southern Baltic Sea: implications for environmental monitoring, Environ. Monit. Assess., 189, 197, https://doi.org/10.1007/s10661-017-5901-y, 2017.
Pokroy, B., Fitch, A. N., Marin, F., Kapon, M., Adir, N., and Zolotoyabko,
E.: Anisotropic lattice distortions in biogenic calcite induced by
intra-crystalline organic molecules, J. Struct. Biol., 155, 96–103,
https://doi.org/10.1016/j.jsb.2006.03.008, 2006.
Ponnurangam, A., Bau, M., Brenner, M., and Koschinsky, A.: Mussel shells of Mytilus edulis as bioarchives of the distribution of rare earth elements and yttrium in seawater and the potential impact of pH and temperature on their partitioning behavior, Biogeosciences, 13, 751–760, https://doi.org/10.5194/bg-13-751-2016, 2016.
Ponnurangam, A. E.: Trace Elements in Mussel Shells as Potential Tools for
Environmental Reconstructions, PhD thesis, Jacobs University, Bremen,
Germany, 154 pp., 2018.
Poulain, C., Gillikin, D. P., Thébault, J., Munaron, J. M., Bohn, M.,
Robert, R., Paulet, Y. M., and Lorrain, A.: An evaluation of Mg∕Ca, Sr∕Ca,
and Ba∕Ca ratios as environmental proxies in aragonite bivalve shells, Chem.
Geol., 396, 42–50, https://doi.org/10.1016/j.chemgeo.2014.12.019, 2015.
Price, G. D. and Pearce, N. J. G.: Biomonitoring of pollution by
Cerastoderma edule from the British Isles: a laser ablation ICP-MS study, Mar. Pollut. Bull., 34, 1025–1031, https://doi.org/10.1016/S0025-326X(97)00098-2, 1997.
Protasowicki, M., Dural, M., and Jaremek, J.: Trace metals in the shells of
blue mussels (Mytilus edulis) from the Poland coast of Baltic Sea, Environ. Monit. Assess., 141, 329–337, https://doi.org/10.1007/s10661-007-9899-4, 2008.
Pruszak, Z., van Ninh, P., Szmytkiewicz, M., Hung, N. M., and Ostrowski, R.:
Hydrology and morphology of two river mouth regions (temperate Vistula delta
and subtropical Red River delta), Oceanologia, 47, 365–385, 2005.
Pruysers, P. A., de Lange, G. J., and Middelburg, J. J.: Geochemistry of
eastern Mediterranean sediments: primary sediment composition and diagenetic
alterations, Mar. Geol., 100, 137–154,
https://doi.org/10.1016/0025-3227(91)90230-2, 1991.
Puente, X., Villares, R., Carral, E., and Carballeira, A.: Nacreous shell of
Mytilus galloprovincialis as a biomonitor of heavy metal pollution in Galiza (NW Spain), Sci. Total Environ., 183, 205–211, https://doi.org/10.1016/0048-9697(96)05066-8, 1996.
Rainbow, P. S.: Physiology, physicochemistry and metal uptake – A crustacean perspective, Mar. Pollut. Bull., 31, 55–59, https://doi.org/10.1016/0025-326X(95)00005-8, 1995.
Rainbow, P. S.: Phylogeny of trace metal accumulation in crustaceans, in:
Metal Metabolism in Aquatic Environments, edited by: Langston, W. J. and
Bebianno, M. J., Springer, Dordrecht, The Netherlands, 285–319,
https://doi.org/10.1007/978-1-4757-2761-6_9, 1998.
Rainbow, P. S.: Trace metal concentrations in aquatic invertebrates: why and
so what?, Environ. Pollut., 120, 497–507,
https://doi.org/10.1016/S0269-7491(02)00238-5, 2002.
Rainbow, P. S. and Phillips, D. J. H.: Cosmopolitan biomonitors of trace
metals, Mar. Pollut. Bull., 26, 593–601,
https://doi.org/10.1016/0025-326X(93)90497-8, 1993.
Rainbow, P. S. and Wang, W.: Comparative assimilation of Cd, Cr, Se, and Zn
by the barnacle, Mar. Ecol.-Prog. Ser., 218, 239–248,
https://doi.org/10.3354/meps218239, 2001.
Rainbow, P. S., Amiard-Triquet, C., Amiard, J. C., Smith, B. D., Best, S.
L., Nassiri, Y., and Langston, W. J.: Trace metal uptake rates in
crustaceans (amphipods and crabs) from coastal sites in NW Europe
differentially enriched with trace metals, Mar. Ecol.-Prog. Ser., 183,
189–203, https://doi.org/10.3354/meps183189, 1999.
Rainbow, P. S., Wolowicz, M., Fialkowski, W., Smith, B. D., and Sokolowski,
A.: Biomonitoring of trace metals in the Gulf of Gdansk, using mussels
(Mytilus trossulus) and barnacles (Balanus improvisus), Water Res., 34, 1823–1829,
https://doi.org/10.1016/S0043-1354(99)00345-0, 2000.
Rainbow, P. S., Fialkowski, W., Sokolowski, A., Smith, B. D., and Wolowicz,
M.: Geographical and seasonal variation of trace metal bioavailabilities in
the Gulf of Gdansk, Baltic Sea using mussels (Mytilus trossulus) and barnacles (Balanus improvisus) as biomonitors, Mar. Biol., 144, 271–286, https://doi.org/10.1007/s00227-003-1197-2, 2004.
Raman, S. and Kumar, R.: Construction and nanomechanical properties of the
exoskeleton of the barnacle, Amphibalanus reticulatus, J. Struct. Biol., 176, 360–369, https://doi.org/10.1016/j.jsb.2011.08.015, 2011.
R Core Team: R: A Language and Environment for Statistical Computing, R Foundation for Statistical Computing, Vienna, Austria, available at: https://www.R-project.org/, last access: 10 August 2019.
Reeder, R. J.: Crystal chemistry of the rhombohedral carbonates, Rev.
Mineral., 11, 1–47, 1983.
Ricardo, F., Génio, L., Costa Leal, M., Albuquerque, R., Queiroga, H.,
Rosa, R., and Calado, R.: Trace element fingerprinting of cockle
(Cerastoderma edule) shells can reveal harvesting location in adjacent areas, Sci. Rep.-UK, 5, 11932, https://doi.org/10.1038/srep11932, 2015.
Ritz, D. A., Swain, R., and Elliott, N. G.: Use of the mussel Mytilus edulis planulatus (Lamarck) in monitoring heavy metal levels in seawater, Mar. Freshw. Res., 33, 491–506,
https://doi.org/10.1071/MF9820491, 1982.
Rodland, D. L., Schöne, B. R., Helama, S., Nielsen, J. K., and Baier,
S.: A clockwork mollusc: ultradian rhythms in bivalve activity revealed by
digital photography, J. Exp. Mar. Bio. Ecol., 334, 316–323,
https://doi.org/10.1016/j.jembe.2006.02.012, 2006.
Roger, L. M., George, A. D., Shaw, J., Hart, R. D., Roberts, M., Becker, T., McDonald, B. J., and Evans, N. J.: Geochemical and microstructural characterisation of two species of cool-water bivalves (Fulvia tenuicostata and Soletellina biradiata) from Western Australia, Biogeosciences, 14, 1721–1737, https://doi.org/10.5194/bg-14-1721-2017, 2017.
Rončević, S., Svedružić, L. P., Smetiško, J., and
Medaković, D.: ICP-AES analysis of metal content in shell of mussel
Mytilus galloprovincialis from Croatian coastal waters, Int. J. Environ. Anal. Chem., 90, 620–632,
https://doi.org/10.1080/03067310903410956, 2010.
Rosenberg, G. D. and Hughes, W. W.: A metabolic model for the determination
of shell composition in the bivalve mollusc, Mytilus edulis, Lethaia, 24, 83–96, https://doi.org/10.1111/j.1502-3931.1991.tb01182.x, 1991.
Rosenberg, G. D., Hughes, W. W., Parker, D. L., and Ray, B. D.: The geometry
of bivalve shell chemistry and mantle metabolism, Am. Malacol. Bull., 16,
251–261, 2001.
Rosenheim, B. E., Swart, P. K., Thorrold, S. R., Willenz, P., Berry, L., and
Latkoczy, C.: High-resolution Sr∕Ca records in sclerosponges calibrated to temperature in situ, Geology, 32, 145–148,
https://doi.org/10.1130/G20117.1, 2004.
Rueda, J. L. and Smaal, A. C.: Variation of the physiological energetics of
the bivalve Spisula subtruncata (da Costa, 1778) within an annual cycle, J. Exp. Mar. Bio. Ecol., 301, 141–157, https://doi.org/10.1016/j.jembe.2003.09.018, 2004.
Saavedra, Y., Gonzalez, A., Fernandez, P., and Blanco, J.: The effect of
size on trace metal levels in raft cultivated mussels (Mytilus galloprovincialis), Sci. Total Environ., 318, 115–124, https://doi.org/10.1016/S0048-9697(03)00402-9, 2004.
Sartori, A. F. and Gofas, S.: Macoma balthica (Linnaeus, 1758), MolluscaBase, available at: http://www.marinespecies.org/aphia.php?p=taxdetails&id=141579 (last access: 26 January 2021), 2016.
Sather, W. A. and McCleskey, E. W.: Permeation and selectivity in calcium
channels, Annu. Rev. Physiol., 65, 133–159,
https://doi.org/10.1146/annurev.physiol.65.092101.142345, 2003.
Schöne, B. R., Zhang, Z., Jacob, D., Gillikin, D. P., Tütken, T.,
Garbe-Schönberg, D., McConnaughey, T., and Soldati, A.: Effect of
organic matrices on the determination of the trace element chemistry (Mg,
Sr, Mg∕Ca, Sr∕Ca) of aragonitic bivalve shells (Arctica islandica) – comparison of ICP-OES and LA-ICP-MS data, Geochem. J., 44, 23–37, https://doi.org/10.2343/geochemj.1.0045, 2010.
Schöne, B. R., Zhang, Z., Radermacher, P., Thébault, J., Jacob, D.
E., Nunn, E. V., and Maurer, A.: Sr∕Ca and Mg∕Ca ratios of ontogenetically
old, long-lived bivalve shells (Arctica islandica) and their function as paleotemperature proxies, Palaeogeogr. Palaeocl., 302, 52–64,
https://doi.org/10.1016/j.palaeo.2010.03.016, 2011.
Skinner, L. C. and Elderfield, H.: Constraining ecological and biological
bias in planktonic foraminiferal Mg∕Ca and δ18Occ: a multispecies approach to proxy calibration testing, Paleoceanography, 20, PA1015, https://doi.org/10.1029/2004PA001058, 2005.
Smith, A. M. and Girvan, E.: Understanding a bimineralic bryozoan: skeletal
structure and carbonate mineralogy of Odontionella cyclops (Foveolariidae: Cheilostomata: Bryozoa) in New Zealand, Palaeogeogr. Palaeocl., 289, 113–122, https://doi.org/10.1016/j.palaeo.2010.02.022, 2010.
Smith, A. M., Nelson, C. S., and Spencer, H. G.: Skeletal carbonate
mineralogy of New Zealand bryozoans, Mar. Geol., 151, 27–46,
https://doi.org/10.1016/S0025-3227(98)00055-3, 1998.
Smith, A. M., Key, M. M., and Gordon, D. P.: Skeletal mineralogy of
bryozoans: taxonomic and temporal patterns, Earth Sci. Rev., 78, 287–306,
https://doi.org/10.1016/j.earscirev.2006.06.001, 2006.
Sokolowski, A., Wolowicz, M., and Hummel, H.: Distribution of dissolved and
labile particulate trace metals in the overlying bottom water in the Vistula
River plume (southern Baltic Sea), Mar. Pollut. Bull., 42, 967–980, 2001.
Staniszewska, M., Nehring, I., and Mudrak-Cegiołka, S.: Changes of
concentrations and possibility of accumulation of bisphenol A and
alkylphenols, depending on biomass and composition, in zooplankton of the
southern Baltic (Gulf of Gdansk), Environ. Pollut., 213, 489–501,
https://doi.org/10.1016/j.envpol.2016.03.004, 2016.
Stanley, S. M.: Effects of global seawater chemistry on biomineralization:
past, present, and future, Chem. Rev., 108, 4483–4498,
https://doi.org/10.1021/cr800233u, 2008.
Stecher, H. A., Krantz, D. E., Lord, C. J., Luther, G. W., and Bock, K. W.:
Profiles of strontium and barium in Mercenaria mercenaria and Spisula solidissima shells, Geochim. Cosmochim. Acta,
60, 3445–3456, https://doi.org/10.1016/0016-7037(96)00179-2, 1996.
Strasser, M., Walensky, M., and Reise, K.: Juvenile–adult distribution of
the bivalve Mya arenaria on intertidal flats in the Wadden Sea: why are there so few year classes?, Helgol. Mar. Res., 33, 45–55,
https://doi.org/10.1007/PL00012137, 1999.
Strasser, C. A., Mullineaux, L. S., and Walther, B. D.: Growth rate and age
effects on Mya arenaria shell chemistry: implications for biogeochemical studies, J. Exp. Mar. Bio. Ecol., 355, 153–163,
https://doi.org/10.1016/j.jembe.2007.12.022, 2008.
Strekopytov, S. V., Uspenskaya, T. Yu., Vinogradova, E. L., and Dubinin, A.
V.: Geochemistry of early diagenesis of sediments of Kandalaksha Bay of the
White Sea, Geochem. Int., 43, 117–130, 2005.
Strelkov, P., Nikula, R., and Väinölä, R.: Macoma balthica in the White and Barents seas: properties of a widespread marine hybrid swarm (Mollusca: Bivalvia), Mol. Ecol., 16, 4110–4127,
https://doi.org/10.1111/j.1365-294X.2007.03463.x, 2007.
Sugawara, A. and Kato, T.: Aragonite CaCO3 thin-film formation by
cooperation of Mg2+ and organic polymer matrices, Chem. Commun., 6,
487–488, https://doi.org/10.1039/A909566G, 2000.
Sunagawa, I., Takahashi, Y., and Imai, H.: Strontium and aragonite-calcite
precipitation, J. Mineral. Petrol. Sci., 102, 174–181,
https://doi.org/10.2465/jmps.060327a, 2007.
Szefer, P.: Metal pollutants and radionuclides in the Baltic Sea – an
overview, Oceanologia, 44, 129–178, 2002.
Szefer, P. and Grembecka, M.: Chemometric assessment of chemical element
distribution in bottom sediments of the southern Baltic Sea including
Vistula and Szczecin lagoons – an overview, Polish J. Environ. Stud., 18,
25–34, 2009.
Szefer, P. and Szefer, K.: Occurrence of ten metals in Mytilus edulis L. and Cardium glaucum L. from the
Gdańsk Bay, Mar. Pollut. Bull., 16, 446–450,
https://doi.org/10.1016/0025-326X(85)90415-1, 1985.
Szefer, P., Kusak, A., Szefer, K., Jankowska, H., Wołowicz, M., and Ali,
A. A.: Distribution of selected metals in sediment cores of Puck Bay, Baltic
Sea, Mar. Pollut. Bull., 30, 615–618,
https://doi.org/10.1016/0025-326X(95)00079-3, 1995.
Szefer, P., Glasby, G. P., Kusak, A., Szefer, K., Jankowska, H., Wolowicz,
M., and Ali, A. A.: Evaluation of the anthropogenic influx of metallic
pollutants into Puck Bay, southern Baltic, Appl. Geochemistry, 13, 293–304,
https://doi.org/10.1016/S0883-2927(97)00098-X, 1998.
Szefer, P., Frelek, K., Szefer, K., Lee, C. B., Kim, B. S., Warzocha, J.,
Zdrojewska, I., and Ciesielski, T.: Distribution and relationships of trace
metals in soft tissue, byssus and shells of Mytilus edulis trossulus from the southern Baltic, Environ. Pollut., 120, 423–444,
https://doi.org/10.1016/S0269-7491(02)00111-2, 2002.
Szumiło-Pilarska, E., Grajewska, A., Falkowska, L., and Hajdrych, J.:
Species differences in total mercury concentration in gulls from the Gulf of
Gdansk (southern Baltic), J. Trace Elem. Med. Biol., 33, 100–109,
https://doi.org/10.1016/j.jtemb.2015.09.005, 2016.
Takesue, R. K. and van Geen, A.: Mg∕Ca, Sr∕Ca, and stable isotopes in modern and Holocene Protothaca staminea shells from a northern California coastal upwelling region,
Geochim. Cosmochim. Acta, 68, 3845–3861,
https://doi.org/10.1016/j.gca.2004.03.021, 2004.
Takesue, R. K., Bacon, C. R., and Thompson, J. K.: Influences of organic
matter and calcification rate on trace elements in aragonitic estuarine
bivalve shells, Geochim. Cosmochim. Acta, 72, 5431–5445,
https://doi.org/10.1016/j.gca.2008.09.003, 2008.
Taylor, J. D. and Reid, D. G.: Shell microstructure and mineralogy of the
Littorinidae: ecological and evolutionary significance, in: Progress in
Littorinid and Muricid Biology: Proceedings of the Second European Meeting
on Littorinid Biology, Tjärnö Marine Biological Laboratory, Sweden,
4–8 July 1988 (Developments in Hydrobiology, vol. 56), edited by:
Johannesson, K., Raffaelli, D. G., and Hannaford Ellis, C. J., Kluwer,
Dordrecht, the Netherlands, 199–215,
https://doi.org/10.1007/978-94-009-0563-4_16, 1990.
Taylor, P. D., James, N. P., Bone, Y., Kuklinski, P., and Kyser, T. K.:
Evolving mineralogy of cheilostome bryozoans, Palaios, 24, 440–452,
https://doi.org/10.2110/palo.2008.p08-124r, 2008.
Taylor, P. D., Kudryavtsev, U. A. B., and Schopf, J. W.: Calcite and
aragonite distributions in the skeletons of bimineralic bryozoans as
revealed by Raman spectroscopy, Invertebr. Biol., 127, 87–97,
https://doi.org/10.1111/j.1744-7410.2007.00106.x, 2014.
Tessier, A., Campbell, P. G. C., and Bisson, M.: Sequential extraction
procedure for the speciation of particulate trace metals, Anal. Chem., 51,
844–851, https://doi.org/10.1021/ac50043a017, 1979.
Thébault, J., Chauvaud, L., Helguen, L., Clavier, J., and Pe, C.: Barium
and molybdenum records in bivalve shells: geochemical proxies for
phytoplankton dynamics in coastal environments?, Limnol. Oceanogr., 54,
1002–1014, https://doi.org/10.4319/lo.2009.54.3.1002, 2009.
Thomas, C. A. and Bendell-Young, L. I.: Linking the sediment geochemistry of
an intertidal region to metal bioavailability in the deposit feeder Macoma balthica, Mar.
Ecol. Prog. Ser., 173, 197–213, https://doi.org/10.3354/meps173197, 1998.
Ullmann, C. V., Gale, A. S., Huggett, J., Wray, D., Frei, R., Korte, C.,
Broom-Fendley, S., Littler, K., and Hesselbo, S. P.: The geochemistry of
modern calcareous barnacle shells and applications for palaeoenvironmental
studies, Geochim. Cosmochim. Ac., 243, 149–168,
https://doi.org/10.1016/j.gca.2018.09.010, 2018.
Urban-Malinga, B., Warzocha, J., and Zalewski, M.: Effects of the invasive
polychaete Marenzelleria spp. on benthic processes and meiobenthos of a species-poor brackish system, J. Sea Res., 80, 25–34,
https://doi.org/10.1016/j.seares.2013.02.005, 2013.
Urey, H. C., Lowenstam, H. A., Epstein, S., and McKinney, C. R.: Measurement
of paleotemperatures and temperatures of the Upper Cretaceous of England,
Denmark, and the southeastern United States, Geol. Soc. Am. Bull., 62,
399–416, https://doi.org/10.1130/0016-7606(1951)62[399:MOPATO]2.0.CO;2,
1951.
Uścinowicz, S.: Geochemia osadów powierzchniowych Morza Bałtyckiego (Geochemistry of the Baltic Sea surface sediments), Państwowy Instytut Geologiczny – Państwowy Instytut
Badawczy (Polish Geological Institute – National Research Institute), Warsaw, Poland, 2011 (in Polish).
Vander Putten, E., Dehairs, F., Keppens, E., and Baeyens, W.: High
resolution distribution of trace elements in the calcite shell layer of
modern Mytilus edulis: environmental and biological controls, Geochim. Cosmochim. Ac., 64, 997–1011, https://doi.org/10.1016/S0016-7037(99)00380-4, 2000.
Waldbusser, G. G., Hales, B., and Haley, B. A.: Calcium carbonate saturation
state: on myths and this or that stories, ICES J. Mar. Sci., 73, 563–568,
https://doi.org/10.1093/icesjms/fsv174, 2016.
Walls, R. A., Ragland, P. C., and Crisp, E. L.: Experimental and natural
early diagenetic mobility of Sr and Mg in biogenic carbonates, Geochim.
Cosmochim. Acta, 41, 1731–1737, https://doi.org/10.1016/0016-7037(77)90204-6, 1977.
Wang, W. and Fisher, N. S.: Modeling the influence of body size on trace
element accumulation in the mussel Mytilus edulis, Mar. Ecol.-Prog. Ser., 161, 103–115, https://doi.org/10.3354/meps161103, 1997.
Wang, Y. and Xu, H.: Prediction of trace metal partitioning between minerals
and aqueous solutions: a linear free energy correlation approach, Geochim.
Cosmochim. Acta, 65, 1529–1543, https://doi.org/10.1016/S0016-7037(01)00551-8, 2001.
Warter, V., Erez, J., and Müller, W.: Environmental and physiological
controls on daily trace element incorporation in Tridacna crocea from combined laboratory
culturing and ultra-high resolution LA-ICP-MS analysis, Palaeogeogr.
Palaeocl., 496, 32–47, 2018.
Watson, D., Foster, P., and Walker, G.: Barnacle shells as biomonitoring
material, Mar. Pollut. Bull., 31, 111–115,
https://doi.org/10.1016/0025-326X(95)00021-E, 1995.
Watson, S. A., Peck, L. S., Tyler, P. A., Southgate, P. C., Tan, K. S., Day,
R. W., and Morley, S. A.: Marine invertebrate skeleton size varies with
latitude, temperature and carbonate saturation: implications for global
change and ocean acidification, Glob. Change Biol., 18, 3026–3038,
https://doi.org/10.1111/j.1365-2486.2012.02755.x, 2012.
Weidema, I. R.: Introduced Species in the Nordic Countries, Nordic
Council of Ministers, Copenhagen, Denmark, 2000.
Wenne, R., Bach, L., Zbawicka, M., Strand, J., and McDonald, J. H.: A first
report on coexistence and hybridization of Mytilus trossulus and M. edulis mussels in Greenland, Polar Biol., 39, 343–355, https://doi.org/10.1007/s00300-015-1785-x, 2016.
Wit, J. C., de Nooijer, L. J., Wolthers, M., and Reichart, G. J.: A novel salinity proxy based on Na incorporation into foraminiferal calcite, Biogeosciences, 10, 6375–6387, https://doi.org/10.5194/bg-10-6375-2013, 2013.
Wolowicz, M. and Goulletquer, P.: The shell organic content in the energy budget of Mytilus trossulus from the South Baltic, Haliotis, 28, 1–10, 1999.
Zhang, G., He, L. S., Wong, Y. H., Xu, Y., Zhang, Y., and Qian, P. Y.:
Chemical component and proteomic study of the Amphibalanus (= Balanus) amphitrite shell, Plos One, 10,
e0133866, https://doi.org/10.1371/journal.pone.0133866, 2015.
Zhao, L., Schöne, B. R., and Mertz-Kraus, R.: Delineating the role of
calcium in shell formation and elemental composition of Corbicula fluminea (Bivalvia), Hydrobiologia, 790, 259–272, https://doi.org/10.1007/s10750-016-3037-7,
2017.
Żmudziński, L.: Świat zwierzȩcy Bałtyku – atlas makrofauny (Animal World of the Baltic Sea: Atlas of Macrofauna), WSiP, Warsaw, Poland, 1990 (in Polish).
Short summary
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.
Calcifying organisms occur globally in almost every environment, and the process of...
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