Articles | Volume 9, issue 11
https://doi.org/10.5194/bg-9-4589-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-9-4589-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
20 Nov 2012
Research article |
| 20 Nov 2012
Light and temperature effects on δ11B and B / Ca ratios of the zooxanthellate coral Acropora sp.: results from culturing experiments
D. Dissard
Laboratoire des Sciences du Climat et de l'Environnement, UMR8212, UVSQ-CNRS-CEA, LSCE/IPSL, Av. de la Terrasse, 91198 Gif sur Yvette, France
School of Earth and Environment, The University of Western Australia, 35 Stirling Highway Crawley WA 6009, Perth, Australia
E. Douville
Laboratoire des Sciences du Climat et de l'Environnement, UMR8212, UVSQ-CNRS-CEA, LSCE/IPSL, Av. de la Terrasse, 91198 Gif sur Yvette, France
S. Reynaud
Centre Scientifique de Monaco, Avenue Saint-Martin, MC 98000, Monaco
A. Juillet-Leclerc
Laboratoire des Sciences du Climat et de l'Environnement, UMR8212, UVSQ-CNRS-CEA, LSCE/IPSL, Av. de la Terrasse, 91198 Gif sur Yvette, France
P. Montagna
Institute of Marine Sciences – National Research Council, ISMAR-CNR, Via Gobetti 101 40129 Bologna, Italy
P. Louvat
Institut de Physique du Globe de Paris, Sorbonne Paris Cité, Université Paris-Diderot, UMR7154, CNRS, 1 rue Jussieu, 75238 Paris, France
M. McCulloch
School of Earth and Environment, The University of Western Australia, 35 Stirling Highway Crawley WA 6009, Perth, Australia
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David J. Harning, Brooke Holman, Lineke Woelders, Anne E. Jennings, and Julio Sepúlveda
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Jessica G. M. Crumpton-Banks, Thomas Tanner, Ivan Hernández Almeida, James W. B. Rae, and Heather Stoll
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Theresa M. King and Brad E. Rosenheim
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Revised manuscript accepted for BG
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Pablo Forjanes, María Simonet Roda, Martina Greiner, Erika Griesshaber, Nelson A. Lagos, Sabino Veintemillas-Verdaguer, José Manuel Astilleros, Lurdes Fernández-Díaz, and Wolfgang W. Schmahl
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Aragonitic skeletons are employed to decipher past climate dynamics and environmental change. Unfortunately, the information that these skeletons keep can be destroyed during diagenesis. In this work, we study the first changes undergone by aragonitic skeletons upon hydrothermal alteration. We observe that major changes occur from the very beginning of the alteration, even without mineralogical changes. These results have major implications for the use of these archives to understand the past.
Inga Labuhn, Franziska Tell, Ulrich von Grafenstein, Dan Hammarlund, Henning Kuhnert, and Bénédicte Minster
Biogeosciences, 19, 2759–2777, https://doi.org/10.5194/bg-19-2759-2022, https://doi.org/10.5194/bg-19-2759-2022, 2022
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This study presents the isotopic composition of recent biogenic carbonates from several lacustrine species which calcify during different times of the year. The authors demonstrate that when biological offsets are corrected, the dominant cause of differences between species is the seasonal variation in temperature-dependent fractionation of oxygen isotopes. Consequently, such carbonates from lake sediments can provide proxy records of seasonal water temperature changes in the past.
Gerard J. M. Versteegh, Karin A. F. Zonneveld, Jens Hefter, Oscar E. Romero, Gerhard Fischer, and Gesine Mollenhauer
Biogeosciences, 19, 1587–1610, https://doi.org/10.5194/bg-19-1587-2022, https://doi.org/10.5194/bg-19-1587-2022, 2022
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A 5-year record of long-chain mid-chain diol export flux and composition is presented with a 1- to 3-week resolution sediment trap CBeu (in the NW African upwelling). All environmental parameters as well as the diol composition are dominated by the seasonal cycle, albeit with different phase relations for temperature and upwelling. Most diol-based proxies are dominated by upwelling. The long-chain diol index reflects temperatures of the oligotrophic summer sea surface.
Johannes Hepp, Christoph Mayr, Kazimierz Rozanski, Imke Kathrin Schäfer, Mario Tuthorn, Bruno Glaser, Dieter Juchelka, Willibald Stichler, Roland Zech, and Michael Zech
Biogeosciences, 18, 5363–5380, https://doi.org/10.5194/bg-18-5363-2021, https://doi.org/10.5194/bg-18-5363-2021, 2021
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Deriving more quantitative climate information like relative air humidity is one of the key challenges in paleostudies. Often only qualitative reconstructions can be done when single-biomarker-isotope data are derived from a climate archive. However, the coupling of hemicellulose-derived sugar with leaf-wax-derived n-alkane isotope results has the potential to overcome this limitation and allow a quantitative relative air humidity reconstruction.
Angelica Feurdean
Biogeosciences, 18, 3805–3821, https://doi.org/10.5194/bg-18-3805-2021, https://doi.org/10.5194/bg-18-3805-2021, 2021
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This study characterized the diversity of laboratory-produced charcoal morphological features of various fuel types from Siberia at different temperatures. The results obtained improve the attribution of charcoal particles to fuel types and fire characteristics. This work also provides recommendations for the application of this information to refine the past wildfire history.
Martin Tetard, Laetitia Licari, Ekaterina Ovsepyan, Kazuyo Tachikawa, and Luc Beaufort
Biogeosciences, 18, 2827–2841, https://doi.org/10.5194/bg-18-2827-2021, https://doi.org/10.5194/bg-18-2827-2021, 2021
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Oxygen minimum zones are oceanic regions almost devoid of dissolved oxygen and are currently expanding due to global warming. Investigation of their past behaviour will allow better understanding of these areas and better prediction of their future evolution. A new method to estimate past [O2] was developed based on morphometric measurements of benthic foraminifera. This method and two other approaches based on foraminifera assemblages and porosity were calibrated using 45 core tops worldwide.
Maximiliano Rodríguez and Christelle Not
Biogeosciences, 18, 1987–2001, https://doi.org/10.5194/bg-18-1987-2021, https://doi.org/10.5194/bg-18-1987-2021, 2021
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Mg/Ca in calcium carbonate shells of marine organisms such as foraminifera and ostracods has been used as a proxy to reconstruct water temperature. Here we provide new Mg/Ca–temperature calibrations for two shallow marine species of ostracods. We show that the water temperature in spring produces the best calibrations, which suggests the potential use of ostracod shells to reconstruct this parameter at a seasonal scale.
Hongrui Zhang, Chuanlian Liu, Luz María Mejía, and Heather Stoll
Biogeosciences, 18, 1909–1916, https://doi.org/10.5194/bg-18-1909-2021, https://doi.org/10.5194/bg-18-1909-2021, 2021
Delphine Dissard, Gert Jan Reichart, Christophe Menkes, Morgan Mangeas, Stephan Frickenhaus, and Jelle Bijma
Biogeosciences, 18, 423–439, https://doi.org/10.5194/bg-18-423-2021, https://doi.org/10.5194/bg-18-423-2021, 2021
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Results from a data set acquired from living foraminifera T. sacculifer collected from surface waters are presented, allowing us to establish a new Mg/Ca–Sr/Ca–temperature equation improving temperature reconstructions. When combining equations, δ18Ow can be reconstructed with a precision of ± 0.5 ‰, while successive reconstructions involving Mg/Ca and δ18Oc preclude salinity reconstruction with a precision better than ± 1.69. A new direct linear fit to reconstruct salinity could be established.
Feng Wang, Dominique Arseneault, Étienne Boucher, Shulong Yu, Steeven Ouellet, Gwenaëlle Chaillou, Ann Delwaide, and Lily Wang
Biogeosciences, 17, 4559–4570, https://doi.org/10.5194/bg-17-4559-2020, https://doi.org/10.5194/bg-17-4559-2020, 2020
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Wood stain is challenging the use of the blue intensity technique for dendroclimatic reconstructions. Using stained subfossil trees from eastern Canadian lakes, we compared chemical destaining approaches with the
delta bluemathematical correction of blue intensity data. Although no chemical treatment was completely efficient, the delta blue method is unaffected by the staining problem and thus is promising for climate reconstructions based on lake subfossil material.
Dulcinea V. Groff, David G. Williams, and Jacquelyn L. Gill
Biogeosciences, 17, 4545–4557, https://doi.org/10.5194/bg-17-4545-2020, https://doi.org/10.5194/bg-17-4545-2020, 2020
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Tussock grasses that grow along coastlines of the Falkland Islands are slow to decay and build up thick peat layers over thousands of years. Grass fragments found in ancient peat can be used to reconstruct past climate because grasses can preserve a record of growing conditions in their leaves. We found that modern living tussock grasses in the Falkland Islands reliably record temperature and humidity in their leaves, and the peat they form can be used to understand past climate change.
Maxence Guillermic, Sambuddha Misra, Robert Eagle, Alexandra Villa, Fengming Chang, and Aradhna Tripati
Biogeosciences, 17, 3487–3510, https://doi.org/10.5194/bg-17-3487-2020, https://doi.org/10.5194/bg-17-3487-2020, 2020
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Boron isotope ratios (δ11B) of foraminifera are a promising proxy for seawater pH and can be used to constrain pCO2. In this study, we derived calibrations for new foraminiferal taxa which extend the application of the boron isotope proxy. We discuss the origin of different δ11B signatures in species and also discuss the potential of using multispecies δ11B analyses to constrain vertical pH and pCO2 gradients in ancient water columns to shed light on biogeochemical carbon cycling in the past.
Zeynep Erdem, Joachim Schönfeld, Anthony E. Rathburn, Maria-Elena Pérez, Jorge Cardich, and Nicolaas Glock
Biogeosciences, 17, 3165–3182, https://doi.org/10.5194/bg-17-3165-2020, https://doi.org/10.5194/bg-17-3165-2020, 2020
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Recent observations from today’s oceans revealed that oxygen concentrations are decreasing, and oxygen minimum zones are expanding together with current climate change. With the aim of understanding past climatic events and their relationship with oxygen content, we looked at the fossils, called benthic foraminifera, preserved in the sediment archives from the Peruvian margin and quantified the bottom-water oxygen content for the last 22 000 years.
Hannah K. Donald, Gavin L. Foster, Nico Fröhberg, George E. A. Swann, Alex J. Poulton, C. Mark Moore, and Matthew P. Humphreys
Biogeosciences, 17, 2825–2837, https://doi.org/10.5194/bg-17-2825-2020, https://doi.org/10.5194/bg-17-2825-2020, 2020
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The boron isotope pH proxy is increasingly being used to reconstruct ocean pH in the past. Here we detail a novel analytical methodology for measuring the boron isotopic composition (δ11B) of diatom opal and apply this to the study of the diatom Thalassiosira weissflogii grown in culture over a range of pH. To our knowledge this is the first study of its kind and provides unique insights into the way in which diatoms incorporate boron and their potential as archives of palaeoclimate records.
Eleonora Fossile, Maria Pia Nardelli, Arbia Jouini, Bruno Lansard, Antonio Pusceddu, Davide Moccia, Elisabeth Michel, Olivier Péron, Hélène Howa, and Meryem Mojtahid
Biogeosciences, 17, 1933–1953, https://doi.org/10.5194/bg-17-1933-2020, https://doi.org/10.5194/bg-17-1933-2020, 2020
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This study focuses on benthic foraminiferal distribution in an Arctic fjord characterised by continuous sea ice production during winter and the consequent cascading of salty and corrosive waters (brine) to the seabed. The inner fjord is dominated by calcareous species (C). In the central deep basins, where brines are persistent, calcareous foraminifera are dissolved and agglutinated (A) dominate. The high A/C ratio is suggested as a proxy for brine persistence and sea ice production.
Johannes Hepp, Imke Kathrin Schäfer, Verena Lanny, Jörg Franke, Marcel Bliedtner, Kazimierz Rozanski, Bruno Glaser, Michael Zech, Timothy Ian Eglinton, and Roland Zech
Biogeosciences, 17, 741–756, https://doi.org/10.5194/bg-17-741-2020, https://doi.org/10.5194/bg-17-741-2020, 2020
Julian Struck, Marcel Bliedtner, Paul Strobel, Jens Schumacher, Enkhtuya Bazarradnaa, and Roland Zech
Biogeosciences, 17, 567–580, https://doi.org/10.5194/bg-17-567-2020, https://doi.org/10.5194/bg-17-567-2020, 2020
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We present leaf wax n-alkanes and their compound-specific (CS) δ13C isotopes from semi-arid and/or arid Mongolia to test their potential for paleoenvironmental reconstructions. Plants and topsoils were analysed and checked for climatic control. Chain-length variations are distinct between grasses and Caragana, which are not biased by climate. However CS δ13C is strongly correlated to climate, so n-alkanes and their CS δ13C show great potential for paleoenvironmental reconstruction in Mongolia.
Elena Lo Giudice Cappelli, Jessica Louise Clarke, Craig Smeaton, Keith Davidson, and William Edward Newns Austin
Biogeosciences, 16, 4183–4199, https://doi.org/10.5194/bg-16-4183-2019, https://doi.org/10.5194/bg-16-4183-2019, 2019
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Fjords are known sinks of organic carbon (OC); however, little is known about the long-term fate of the OC stored in these sediments. The reason for this knowledge gap is the post-depositional degradation of OC. This study uses benthic foraminifera (microorganisms with calcite shells) to discriminate between post-depositional OC degradation and actual OC burial and accumulation in fjordic sediments, as foraminifera would only preserve the latter information in their assemblage composition.
Sara K. E. Goulden, Naohiko Ohkouchi, Katherine H. Freeman, Yoshito Chikaraishi, Nanako O. Ogawa, Hisami Suga, Oliver Chadwick, and Benjamin Z. Houlton
Biogeosciences, 16, 3869–3882, https://doi.org/10.5194/bg-16-3869-2019, https://doi.org/10.5194/bg-16-3869-2019, 2019
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We investigate whether soil organic compounds preserve information about nitrogen availability to plants. We isolate chlorophyll degradation products in leaves, litter, and soil and explore possible species and climate effects on preservation and interpretation. We find that compound-specific nitrogen isotope measurements in soil have potential as a new tool to reconstruct changes in nitrogen cycling on a landscape over time, avoiding issues that have limited other proxies.
Nicolai Schleinkofer, Jacek Raddatz, André Freiwald, David Evans, Lydia Beuck, Andres Rüggeberg, and Volker Liebetrau
Biogeosciences, 16, 3565–3582, https://doi.org/10.5194/bg-16-3565-2019, https://doi.org/10.5194/bg-16-3565-2019, 2019
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In this study we tried to correlate Na / Ca ratios from cold-water corals with environmental parameters such as salinity, temperature and pH. We do not observe a correlation between Na / Ca ratios and seawater salinity, but we do observe a strong correlation with temperature. Na / Ca data from warm-water corals (Porites spp.) and bivalves (Mytilus edulis) support this correlation, indicating that similar controls on the incorporation of sodium exist in these aragonitic organisms.
Mattia Greco, Lukas Jonkers, Kerstin Kretschmer, Jelle Bijma, and Michal Kucera
Biogeosciences, 16, 3425–3437, https://doi.org/10.5194/bg-16-3425-2019, https://doi.org/10.5194/bg-16-3425-2019, 2019
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To be able to interpret the paleoecological signal contained in N. pachyderma's shells, its habitat depth must be known. Our investigation on 104 density profiles of this species from the Arctic and North Atlantic shows that specimens reside closer to the surface when sea-ice and/or surface chlorophyll concentrations are high. This is in contrast with previous investigations that pointed at the position of the deep chlorophyll maximum as the main driver of N. pachyderma vertical distribution.
Anna Mikis, Katharine R. Hendry, Jennifer Pike, Daniela N. Schmidt, Kirsty M. Edgar, Victoria Peck, Frank J. C. Peeters, Melanie J. Leng, Michael P. Meredith, Chloe L. C. Jones, Sharon Stammerjohn, and Hugh Ducklow
Biogeosciences, 16, 3267–3282, https://doi.org/10.5194/bg-16-3267-2019, https://doi.org/10.5194/bg-16-3267-2019, 2019
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Antarctic marine calcifying organisms are threatened by regional climate change and ocean acidification. Future projections of regional carbonate production are challenging due to the lack of historical data combined with complex climate variability. We present a 6-year record of flux, morphology and geochemistry of an Antarctic planktonic foraminifera, which shows that their growth is most sensitive to sea ice dynamics and is linked with the El Niño–Southern Oscillation.
Eunmi Park, Jens Hefter, Gerhard Fischer, Morten Hvitfeldt Iversen, Simon Ramondenc, Eva-Maria Nöthig, and Gesine Mollenhauer
Biogeosciences, 16, 2247–2268, https://doi.org/10.5194/bg-16-2247-2019, https://doi.org/10.5194/bg-16-2247-2019, 2019
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We analyzed GDGT-based proxy temperatures in the polar oceans. In the eastern Fram Strait (79° N), the nutrient distribution may determine the depth habit of Thaumarchaeota and thus the proxy temperature. In the Antarctic Polar Front (50° S), the contribution of Euryarchaeota or the nonlinear correlation between the proxy values and temperatures may cause the warm biases of the proxy temperatures relative to SSTs.
Marijke W. de Bar, Jenny E. Ullgren, Robert C. Thunnell, Stuart G. Wakeham, Geert-Jan A. Brummer, Jan-Berend W. Stuut, Jaap S. Sinninghe Damsté, and Stefan Schouten
Biogeosciences, 16, 1705–1727, https://doi.org/10.5194/bg-16-1705-2019, https://doi.org/10.5194/bg-16-1705-2019, 2019
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We analyzed sediment traps from the Cariaco Basin, the tropical Atlantic and the Mozambique Channel to evaluate seasonal imprints in the concentrations and fluxes of long-chain diols (LDIs), in addition to the long-chain diol index proxy (sea surface temperature proxy) and the diol index (upwelling indicator). Despite significant degradation, LDI-derived temperatures were very similar for the sediment traps and seafloor sediments, and corresponded to annual mean sea surface temperatures.
Jens Zinke, Juan P. D'Olivo, Christoph J. Gey, Malcolm T. McCulloch, J. Henrich Bruggemann, Janice M. Lough, and Mireille M. M. Guillaume
Biogeosciences, 16, 695–712, https://doi.org/10.5194/bg-16-695-2019, https://doi.org/10.5194/bg-16-695-2019, 2019
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Here we report seasonally resolved sea surface temperature (SST) reconstructions for the southern Mozambique Channel in the SW Indian Ocean, a region located along the thermohaline ocean surface circulation route, based on multi-trace-element temperature proxy records preserved in two Porites sp. coral cores for the past 42 years. Particularly, we show the suitability of both separate and combined Sr / Ca and Li / Mg proxies for improved multielement SST reconstructions.
Hilde Pracht, Brett Metcalfe, and Frank J. C. Peeters
Biogeosciences, 16, 643–661, https://doi.org/10.5194/bg-16-643-2019, https://doi.org/10.5194/bg-16-643-2019, 2019
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In palaeoceanography the shells of single-celled foraminifera are routinely used as proxies to reconstruct the temperature, salinity and circulation of the ocean in the past. Traditionally a number of specimens were pooled for a single stable isotope measurement; however, technical advances now mean that a single shell or chamber of a shell can be measured individually. Three different hypotheses regarding foraminiferal biology and ecology were tested using this approach.
Anna Jentzen, Dirk Nürnberg, Ed C. Hathorne, and Joachim Schönfeld
Biogeosciences, 15, 7077–7095, https://doi.org/10.5194/bg-15-7077-2018, https://doi.org/10.5194/bg-15-7077-2018, 2018
Shauna Ní Fhlaithearta, Christophe Fontanier, Frans Jorissen, Aurélia Mouret, Adriana Dueñas-Bohórquez, Pierre Anschutz, Mattias B. Fricker, Detlef Günther, Gert J. de Lange, and Gert-Jan Reichart
Biogeosciences, 15, 6315–6328, https://doi.org/10.5194/bg-15-6315-2018, https://doi.org/10.5194/bg-15-6315-2018, 2018
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This study looks at how foraminifera interact with their geochemical environment in the seabed. We focus on the incorporation of the trace metal manganese (Mn), with the aim of developing a tool to reconstruct past pore water profiles. Manganese concentrations in foraminifera are investigated relative to their ecological preferences and geochemical environment. This study demonstrates that Mn in foraminiferal tests is a promising tool to reconstruct oxygen conditions in the seabed.
Siobhan Williams, Walter Adey, Jochen Halfar, Andreas Kronz, Patrick Gagnon, David Bélanger, and Merinda Nash
Biogeosciences, 15, 5745–5759, https://doi.org/10.5194/bg-15-5745-2018, https://doi.org/10.5194/bg-15-5745-2018, 2018
Robert Frei, Cora Paulukat, Sylvie Bruggmann, and Robert M. Klaebe
Biogeosciences, 15, 4905–4922, https://doi.org/10.5194/bg-15-4905-2018, https://doi.org/10.5194/bg-15-4905-2018, 2018
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The reconstruction of paleo-redox conditions of seawater has the potential to link to climatic changes on land and therefore to contribute to our understanding of past climate change. The redox-sensitive chromium isotope system is applied to marine calcifiers in order to characterize isotope offsets that result from vital processes during calcification processes and which can be eventually used in fossil equivalents to reconstruct past seawater compositions.
Thomas M. DeCarlo, Michael Holcomb, and Malcolm T. McCulloch
Biogeosciences, 15, 2819–2834, https://doi.org/10.5194/bg-15-2819-2018, https://doi.org/10.5194/bg-15-2819-2018, 2018
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Understanding the mechanisms of coral calcification is limited by the isolation of the calcifying environment. The boron systematics (B / Ca and δ11B) of aragonite have recently been developed as a proxy for the carbonate chemistry of the calcifying fluid, but a variety of approaches have been utilized. We assess the available experimental B / Ca partitioning data and present a computer code for deriving calcifying fluid carbonate chemistry from the boron systematics of coral skeletons.
Manuel Bringué, Robert C. Thunell, Vera Pospelova, James L. Pinckney, Oscar E. Romero, and Eric J. Tappa
Biogeosciences, 15, 2325–2348, https://doi.org/10.5194/bg-15-2325-2018, https://doi.org/10.5194/bg-15-2325-2018, 2018
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We document 2.5 yr of dinoflagellate cyst production in the Cariaco Basin using a sediment trap record. Each species' production pattern is interpreted in the context of the physico-chemical (e.g., temperature, nutrients) and biological (other planktonic groups) environment. Most species respond positively to upwelling, but seem to be negatively impacted by an El Niño event with a 1-year lag. This work helps understanding dinoflagellate ecology and interpreting fossil assemblages in sediments.
Gabriella M. Weiss, Eva Y. Pfannerstill, Stefan Schouten, Jaap S. Sinninghe Damsté, and Marcel T. J. van der Meer
Biogeosciences, 14, 5693–5704, https://doi.org/10.5194/bg-14-5693-2017, https://doi.org/10.5194/bg-14-5693-2017, 2017
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Algal-derived compounds allow us to make assumptions about environmental conditions in the past. In order to better understand how organisms record environmental conditions, we grew microscopic marine algae at different light intensities, salinities, and alkalinities in a temperature-controlled environment. We determined how these environmental parameters affected specific algal-derived compounds, especially their relative deuterium content, which seems to be mainly affected by salinity.
S. Nemiah Ladd, Nathalie Dubois, and Carsten J. Schubert
Biogeosciences, 14, 3979–3994, https://doi.org/10.5194/bg-14-3979-2017, https://doi.org/10.5194/bg-14-3979-2017, 2017
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Hydrogen isotopes of lipids provide valuable information about microbial activity, climate, and environmental stress. We show that heavy hydrogen in fatty acids declines from spring to summer in a nutrient-rich and a nutrient-poor lake and that the effect is nearly 3 times as big in the former. This effect is likely a combination of increased biomass from algae, warmer temperatures, and higher algal growth rates.
Karoliina A. Koho, Lennart J. de Nooijer, Christophe Fontanier, Takashi Toyofuku, Kazumasa Oguri, Hiroshi Kitazato, and Gert-Jan Reichart
Biogeosciences, 14, 3067–3082, https://doi.org/10.5194/bg-14-3067-2017, https://doi.org/10.5194/bg-14-3067-2017, 2017
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Here we report Mn / Ca ratios in living benthic foraminifera from the NE Japan margin. The results show that the Mn incorporation directly reflects the environment where the foraminifera calcify. Foraminifera that live deeper in sediment, under greater redox stress, generally incorporate more Mn into their carbonate skeletons. As such, foraminifera living close to the Mn reduction zone in sediment appear promising tools for paleoceanographic reconstructions of sedimentary redox conditions.
Stefania Milano, Gernot Nehrke, Alan D. Wanamaker Jr., Irene Ballesta-Artero, Thomas Brey, and Bernd R. Schöne
Biogeosciences, 14, 1577–1591, https://doi.org/10.5194/bg-14-1577-2017, https://doi.org/10.5194/bg-14-1577-2017, 2017
Diana Zúñiga, Celia Santos, María Froján, Emilia Salgueiro, Marta M. Rufino, Francisco De la Granda, Francisco G. Figueiras, Carmen G. Castro, and Fátima Abrantes
Biogeosciences, 14, 1165–1179, https://doi.org/10.5194/bg-14-1165-2017, https://doi.org/10.5194/bg-14-1165-2017, 2017
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Diatoms are one of the most important primary producers in highly productive coastal regions. Their silicified valves are susceptible to escape from the upper water column and be preserved in the sediment record, and thus are frequently used to reconstruct environmental conditions in the past from sediment cores. Here, we assess how water column diatom’s community in the NW Iberian coastal upwelling system is seasonally transferred from the surface to the seafloor sediments.
Andreia Rebotim, Antje H. L. Voelker, Lukas Jonkers, Joanna J. Waniek, Helge Meggers, Ralf Schiebel, Igaratza Fraile, Michael Schulz, and Michal Kucera
Biogeosciences, 14, 827–859, https://doi.org/10.5194/bg-14-827-2017, https://doi.org/10.5194/bg-14-827-2017, 2017
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Planktonic foraminifera species depth habitat remains poorly constrained and the existing conceptual models are not sufficiently tested by observational data. Here we present a synthesis of living planktonic foraminifera abundance data in the subtropical eastern North Atlantic from vertical plankton tows. We also test potential environmental factors influencing the species depth habitat and investigate yearly or lunar migration cycles. These findings may impact paleoceanographic studies.
Clemens Vinzenz Ullmann and Philip A. E. Pogge von Strandmann
Biogeosciences, 14, 89–97, https://doi.org/10.5194/bg-14-89-2017, https://doi.org/10.5194/bg-14-89-2017, 2017
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This study documents how much control growth rate has on the chemical composition of fossil shell material. Using a series of chemical analyses of the fossil hard part of a belemnite, an extinct marine predator, a clear connection between the rate of calcite formation and its magnesium and strontium contents was found. These findings provide further insight into biomineralization processes and help better understand chemical signatures of fossils as proxies for palaeoenvironmental conditions.
Cited articles
Al-Horani, F. A., Al-Moghrabi, S. M., and de Beer, D.: Microsensor study of photosynthesis and calcification in the scleractinian coral, Galaxea fascicularis: active internal carbon cycle, J. Exp. Mar. Biol. Ecol., 288, 1–15, 2003.
Allemand, D., Ferrier-Pages, C., Furla, P., Houlbreque, F., Puverel, S., Reynaud, S., Tambutte, E., Tambutte, S., and Zoccola, D.: Biomineralisation in reef-building corals: from molecular mechanisms to environmental control, C. R. Palevol, 3, 453–467, 2004.
Allen, K. A., Honisch, B., Eggins, S. M., Yu, J. M., Spero, H. J., and Elderfield, H.: Controls on boron incorporation in cultured tests of the planktic foraminifer Orbulina universa, Earth Planet. Sci. Lett., 309, 291–301, 2011.
Allison, N., and Finch, A. A.: $\delta ^{(11)}$B, Sr, Mg and B in a modern Porites coral: the relationship between calcification site pH and skeletal chemistry, Geochim. Cosmochim. Ac., 74, 1790–1800, 2010.
Al-Moghrabi, S. M., Allemand, D., and Jaubert, J.: Valine uptake by the scleractinian coral Galaxea fascicularis: characterization and effect of light and nutritional status., J. Comp. Physiol. B, 163, 355–362, 1993.
Al-Moghrabi, S. M., Al-Horani, F. A., and de Beer, D.: Calcification by the scleractinian coral Galaxea fascicularis: direct measurements on calicoblastic layer using micro-sensors, in: 8th Int. Symp. on Biomineralization, 45, 2001.
Barnes, D. J., and Chalker, B. E.: Calcification and photosynthesis in reef-building corals and algae, in: Coral Reefs, edited by: Z. Dubinsky, Amsterdam, Elsevier, 109–131, 1990.
Bourdin, C., Douville, E., and Genty, D.: Alkaline-earth metal and rare-earth element incorporation control by ionic radius and growth rate on a stalagmite from the Chauvet Cave, Southeastern France, Chem. Geol., 290, 1–11, 2011.
Caldeira, K., and Wickett, M. E.: Ocean model predictions of chemistry changes from carbon dioxide emissions to the atmosphere and ocean, J. Geophys. Res.-Oceans, 110, C09S04, https://doi.org/10.1029/2004JC002671, 2003.
Caldeira, K., and Wickett, M. E.: Anthropogenic carbon and ocean pH, Nature, 425, 365–365, 2005.
Chalker, B. E. and Taylor, D. L.: Light-enhanced calcification, and role of oxidative phosphorylation in calcification of coral Acropora cervicornis, P. Roy. Soc. Lond. B Bio., 190, 323–331, 1975.
Chalker, B. E. and Barnes, D. J.: Gamma-densitometry for the measurement of skeletal density, Coral Reefs, 9, 11–23, 1990.
Cohen, A. L. and McConnaughey, T. A.: Geochemical perspectives on coral mineralization, 151–187, in: Dove PMDJJWS, edited by: Biomineralization, Vol. 54, 2003.
Cohen, A. L. and Thorrold, S. R.: Recovery of temperature records from slow-growing corals by fine scale sampling of skeletons, Geophys. Res. Lett., 34, L17706, https://doi.org/10.1029/2007GL030967, 2007.
Coles, S. L., and Jokiel, P. L.: Synergistic effects of temperature salinity, and light on hermatypic corals Montipora verrucosa, Mar. Biol., 49, 187–195, 1977.
Coles, S. L., and Jokiel, P. L.: Effects of temperature on photosynthesis and respiration in hermatypic corals, Mar. Biol., 43, 209–216, 1978.
Corrège, T.: Sea surface temperature and salinity reconstruction from coral geochemical tracers, Palaeogeogr. Palaeocl., 232, 408–428, 2006.
Davies, P. S.: Short-term growth measurements of corals using an accurate buoyant weighing technique, Mar. Biol., 101, 389–395, 1989.
DeLong, K. L., Quinn, T. M., and Taylor, F. W.: Reconstructing twentieth-century sea surface temperature variability in the southwest Pacific: A replication study using multiple coral Sr/Ca records from New Caledonia, Paleoceanography, 22, PA4212, https://doi.org/10.1029/2007PA001444, 2007.
Dickson, A. G.: Thermodynamics of the dissociation of boric acid in synthetic seawater from 273.15 to 318.15 K., Deep-Sea Res., 37, 755–766, 1990.
DOE: Handbook of methods for the analysis of the various parameters of the carbon dioxide system in sea-water, Version 2, edited by: Dickson, A. G. and Goyet, C., ORNL/CDIAC-74, 1994.
Douville, E., Paterne, M., Cabioch, G., Louvat, P., Gaillardet, J., Juillet-Leclerc, A., and Ayliffe, L.: Abrupt sea surface pH change at the end of the Younger Dryas in the central sub-equatorial Pacific inferred from boron isotope abundance in corals (Porites), Biogeosciences, 7, 2445–2459, https://doi.org/10.5194/bg-7-2445-2010, 2010.
Dubinsky, Z., Falkowski, P. G., and Sharf, D.: Aspects of adaptation of hermatypic orals and their endosymbiotic zooxanthellae to light, Bull. Inst. Oceanogr. Fish., 9, 124–134, 1983.
Fallon, S. J., McCulloch, M. T., van Woesik, R., and Sinclair, D. J.: Corals at their latitudinal limits: laser ablation trace element systematics in Porites from Shirigai Bay, Japan, Earth Planet. Sci. Lett., 172, 221–238, 1999.
Fallon, S. J., McCulloch, M. T., and Alibert, C.: Examining water temperature proxies in Porites corals from the Great Barrier Reef: a cross-shelf comparison, Coral Reefs, 22, 389–404, 2003.
Foster, G. L.: Seawater pH, pCO2 and CO$_{3}^{2-}$ variations in the Caribbean Sea over the last 130 kyr: A boron isotope and B/Ca study of planktic foraminifera, Earth Planet. Sci. Lett., 271, 254–266, 2008.
Foster, G. L., Pogge von Strandmann, P. A. E., and Rae, J. W. B.: Boron and Magnesium Isotopic Composition of Seawater, Geochem. Geophy. Geosy., 11, 1–10, 2010.
Furla, P., Benazet-Tambutte, S., Jaubert, J., and Allemand, D.: Functional polarity of the tentacle of the sea anemone Anemonia viridis: role in inorganic carbon acquisition, Am. J. Physiol.-Reg. I., 274, R303–R310, 1998.
Gattuso, J. P. and Hansson, L.: Ocean acidification, edited by: Gattuso, J.-P. and Hansson, L., Oxford university press, 352 pp., 2011.
Gattuso, J. P., Allemand, D., and Frankignoulle, M.: Photosynthesis and calcification at cellular, organismal and community levels in coral reefs: A review on interactions and control by carbonate chemistry., Am. Zool., 39, 160–183, 1999.
Goodkin, N. F., Hughen, K. A., and Cohen, A. L.: A multicoral calibration method to approximate a universal equation relating Sr/Ca and growth rate to sea surface temperature, Paleoceanography, 22, PA1214, https://doi.org/10.1029/2006PA001312, 2007.
Goreau, T. F.: The physiology of skeleton formation in corals. 1. A method for measuring the rate of calcium deposition by corals under different conditions, Biol. Bull., 116, 59–75, 1959.
Griffith, P. C., Cubit, J. D., Adey, W. H., and Norris, J. N.: Computer-automated flow respirometry: metabolism measurements on a Caribbean reef and in a microcosm, Limnol. Oceanogr., 32, 442–451, 1987.
Harding, D. J., Arden, J. W., Rickaby, R. E. M.: A method for precise analysis of trace element/calcium ratios in carbonate samples using quadrupole inductively coupled plasma mass spectrometry, Geochem. Geophy. Geosy., 7, Q06003, https://doi.org/10.1029/2005GC001093, 2006.
Hart, S. R. and Cohen, A. L.: An ion probe study of annual cycles of Sr/Ca and other trace elements in corals, Geochim. Cosmochim. Ac., 60, 3075–3084, 1996.
Hemming, N. G. and Hanson, G. N.: Boron isotopic composition and concentration in modern marine carbonates, Geochim. Cosmochim. Ac., 56, 537–543, 1992.
Hendry, K. R., Rickaby, R. E. M., Meredith, M. P., and Elderfield, H.: Controls on stable isotope and trace metal uptake in Neogloboquadrina pachyderma (sinistral) from an Antarctic sea-ice environment, Earth Planet. Sci. Lett., 278, 67–77, 2009.
Herfort, L., Thake, B., and Taubner, I.: Bicarbonate stimulation of calcification and photosynthesis in two hermatypic corals, J. Phycology, 44, 91–98, 2008.
Hershey, J. P., Fernandez, M., Milne, P. J., and Millero, F. J.: The ionization of boric acid in NaCl, Na-Ca-Cl and Na-Mg-Cl solutions at 25 °C., Geochim. Cosmochim. Ac., 50, 143–148, 1986.
Hönisch, B., Hemming, N. G., Grottoli, A. G., Amat, A., Hanson, G. N., and Buma, J.: Assessing scleractinian corals as recorders for paleo-pH: Empirical calibration and vital effects, Geochim. Cosmochim. Ac., 68, 3675–3685, 2004.
Hönisch, B., Hemming, N. G., and Loose, B.: Comment on "A critical evaluation of the boron isotope-pH proxy: The accuracy of ancient ocean pH estimates", edited by: Pagani, M., Lemarchand, D., Spivack, A. and Gaillardet, J., Geochim. Cosmochim. Ac., 71, 1636–1641, 2007.
Hönisch, B., Bickert, T., and Hemming, N. G.: Modern and Pleistocene boron isotope composition of the benthic foraminifer Cibicidoides wuellerstorfi, Earth Planet. Sci. Lett., 272, 309–318, 2008.
Hönisch, B., Hemming, N. G., Archer, D., Siddall, M., and McManus, J. F.: Atmospheric Carbon Dioxide Concentration Across the Mid-Pleistocene Transition, Science, 324, 1551–1554, 2009.
Iglesias-Prieto, R. and Trench, R. K.: Acclimation and adaptation to irradiance in symbiotic dinoflagellates. II. Response of chlorophyll-protein complexes to different photon-flux densities, Mar. Biol., 130, 23 pp., 1997.
Jacques, T. G., Marshall, N., and Pilson, M. E. Q.: Experimental ecology of the temperate scleractinian coral Astrangia danae, 2. Effect of temperature, light-intensity and synbiosis with zooxanthellae on metabolic-rate and calcification, Mar. Biol., 76, 135–148, 1983.
Jokiel, P. L., and Coles, S. L.: Effects of temperature on mortality and growth of Hawaiian reef corals, Mar. Biol., 43, 201–208, 1977.
Jokiel, P. L., Maragos, J. E., and Franzisket, L: Coral growth: buoyant weight technique, in: Stoddart, D. R. and Johannes, R. E., Coral reefs, Research Methods, UNESCO monographs on oceanographic methodology, Paris, 529–542, 1978.
Juillet-Leclerc, A., Reynaud, S., Dissard, D., Tisserant, G., and Ferrier-Pagès, C.: Sr/Ca and Mg/Ca are indicators of the calcification rate of zooxanthellate scleractinian corals, Geochim. Cosmochim. Ac., submitted, 2012.
Kajiwara, K., Nagai, A., Ueno, S., and Yokochi, H.: Examination of the effect of temperature, light intensity and zooxanthellae concentration on calcification and photosynthesis of scleractinian coral Acropora pulchra, J. Sch. Mar. Sci., Tech Tokai Univ., 40, 95–103, 1995.
Kitano, Y., Okumura, M., and Idogaki, M.: Coprecipitation of Borate-Boron with Calcium-carbonate, Geochem. J., 12, 183–189, 1978.
Klochko, K., Kaufman, A. J., Yao, W. S., Byrne, R. H., and Tossell, J. A.: Experimental measurement of boron isotope fractionation in seawater, Earth Planet. Sci. Lett., 248, 276–285, 2006.
Klochko, K., Cody, G. D., Tossell, J. A., Dera, P., and Kaufman, A. J.: Re-evaluating boron speciation in biogenic calcite and aragonite using (11)B MAS NMR, Geochim. Cosmochim. Ac., 73, 1890–1900, 2009.
Krief, S., Hendy, E. J., Fine, M., Yam, R., Meibom, A, Foster, G. L., and Shemesh, A.: Physiological and isotopic responses of scleractinian corals to ocean acidification, Geochim. Cosmochim. Ac., 74, 4988–5001, 2010.
Kuhl, M., Cohen, Y., Dalsgaard, T., Jorgensen, B. B., and Revsbech, N. P.: Microenvironment and photosynthesis of zooxanthellae in scleractinian corals studied with microsensors for O2, pH and light, Mar. Ecol.-Progr. S., 117, 159–172, 1995.
Louvat, P., Bouchez, J., and Paris, G.: MC-ICP-MS Isotope measurements with direct injection nebulisation (d-DIHEN): optimisation and application to Boron in seawater and carbonate samples, Geostand. Geoanal. Res., 35, 75–88, 2011.
McCulloch, M., Trotter, J., Montagna, P., Falter, J., Dunbar, R., Freiwald, A., Försterra, G., López Correa, M., Maier, C., Rüggeberg, A., Taviani, M., and Thresher, R.: Boron Isotope Systematics of Cold-water Scleractinian Corals: Internal pH Up-regulation and Response to Ocean Acidification, Geochem. Cosmochim. Ac., in press, 2012.
Montagna, P., McCulloch, M., Mazzoli, C., Silenzi, S., and Odorico, R.: The non-tropical coral Cladocora caespitosa as the new climate archive for the Mediterranean: high-resolution (similar to weekly) trace element systematics, Quaternary Sci. Rev., 26, 441–462, 2007.
Moya, A., Tambutte, S., Tambutte, E., Zoccola, D., Caminiti, N., and Allemand, D.: Study of calcification during a daily cycle of the coral Stylophora pistillata: implications for 'light-enhanced calcification', J. Exp. Biol., 209, 3413–3419, 2006.
Okai, T., Suzuki, A., Terashima, S., Inoue, M., Nohara, M., Kawahata H., and Imai, N.: Collaborative analysis of GSJ/AIST geochemical reference materials JCp-1 (Coral) and JCt-1 (Giant Clam). Chikyukagaku, Geochemistry, 38, 281–286, 2004.
Palmer, M. R. and Pearson, P. N.: A 23 000-Year record of surface water pH and pCO2 in the Western Equatorial Pacific, Ocean Science, 300, 480–482, 2003.
Pelejero, C., Calvo, E., McCulloch, M. T., Marshall, J. F., Gagan, M. K., Lough, J. M., and Opdyke, B. N.: Preindustrial to modern interdecadal variability in coral reef pH, Science, 309, 2204–2207, 2005.
Quinn, T. M., and Sampson, D. E.: A multiproxy approach to reconstructing sea surface conditions using coral skeleton geochemistry, Paleoceanography, 17, 2002.
Reynaud, S., Ferrier-Pages, C., Sambrotto, S. R., Juillet-Leclerc, A., Jaubert, J., and Gattuso J.-P.: Effect of feeding on the carbon and oxygen isotopic composition in the tissues and skeleton of the zooxanthellae coral Stylophora pistillata, Mar. Ecol.-Progr. S., 238, 81–89, 2002.
Reynaud, S., Ferrier-Pages, C., Boisson, F., Allemand, D., and Fairbanks, R. G.: Effect of light and temperature on calcification and strontium uptake in the scleractinian coral Acropora verweyi, Mar. Ecol.-Progr. S., 279, 105–112, 2004.
Reynaud, S., Leclercq, N., Romaine-Lioud, S., Ferrier-Pages, C., Jaubert, J., and Gattuso, J. P.: Interacting effects of CO2 partial pressure and temperature on photosynthesis and calcification in a scleractinian coral, Global Change Biol., 9, 1660–1668, 2003.
Reynaud, S., Ferrier-Pages, C., Meibom, A., Mostefaoui, S., Mortlock, R., Fairbanks, R., and Allemand, D.: Light and temperature effects on Sr/Ca and Mg/Ca ratios in the scleractinian coral Acropora sp., Geochim. Cosmochim. Ac., 71, 354–362, 2007.
Reynaud-Vaganay, S., Gattuso, J. P., Cuif, J. P., Jaubert, J., and Juillet-Leclerc, A.: A novel culture technique for scleractinian corals: application to investigate changes in skeletal δ18O as a function of temperature, Mar. Ecol.-Progr. S., 180, 121–130, 1999.
Reynaud-Vaganay, S., Juillet-Leclerc, A., Jaubert, J., and Gattuso, J. P.: Effect of light on skeletal d13C and d18O, and interaction with photosynthesis, respiration and calcification in two zooxanthellate scleractinian corals, Palaeogeogr. Palaeocl., 175, 393–404, 2001.
Rodolfo-Metalpa, R., Peirano, A., Houlbreque, F., Abbate, M., and Ferrier-Pages, C.: Effects of temperature, light and heterotrophy on the growth rate and budding of the temperate coral Cladocora caespitosa, Coral Reefs, 27, 17–25, 2008.
Rodolfo-Metalpa, R., Martin, S., Ferrier-Pagès, C., and Gattuso, J.-P.: Response of the temperate coral Cladocora caespitosa to mid- and long-term exposure to pCO2 and temperature levels projected for the year 2100 AD, Biogeosciences, 7, 289–300, https://doi.org/10.5194/bg-7-289-2010, 2010.
Rollion-Bard, C., Blamart, D., Trebosc, J., Tricot, G., Mussi, A., and Cuif, J. P.: Boron isotopes as pH proxy: A new look at boron speciation in deep-sea corals using $^{(11)}$B MAS NMR and EELS, Geochim. Cosmochim. Ac., 75, 1003–1012, 2011.
Roy, R. N., Roy, L. N., Vogel, K. M., Moore, C. P., Pearson, T., Good, C. E., and Miller, F. J.: Thermodynamics of the dissociation of boric acid in seawater, Mar. Chem., 44, 243–248, 1993.
Shirai, K., Kawashima, T., Sowa, K., Watanabe, T., Nakaniori, T., Takahata, N., Arnakawa, H., and Sano, Y.: Minor and trace element incorporation into branching coral Acropora nobilis skeleton, Geochim. Cosmochim. Ac., 72, 5386–5400, 2008.
Sinclair, D. J., Kinsley, L. P. J., and McCulloch, M. T.: High resolution analysis of trace elements in corals by laser ablation ICP-MS, Geochim. Cosmochim. Ac., 62, 1889–1901, 1998.
Spivack, A. J., You, C. F., and Smith, H. J.: Foraminiferal boron isotope ratios as a proxy for surface ocean pH over the past 21-Myr, Nature, 363, 149–151, 1993.
Tambutté, S., Holcomb, M., Ferrier-Pages, C., Reynaud, S., Tambutte, E., Zoccola, D., and Allemand, D.: Coral biomineralization: From the gene to the environment, J. Exp. Mar. Biol. Ecol., 408, 58–78, 2011.
Tripati, A. K., Roberts, C. D., and Eagle, R. A.: Coupling of CO2 and Ice Sheet Stability Over Major Climate Transitions of the Last 20 Million Years, Science, 326, 1394–1397, 2009.
Trotter, J., Montagna, P., McCulloch, M., Silenzi, S., Reynaud, S., Mortimer, G., Martin, S., Ferrier-Pagès, C., Gattuso, J.-P., and Rodolfo-Metalpa, R.: Quantifying the pH 'vital effect' in the temperate zooxanthellate coral Cladocora caespitosa: Validation of the boron seawater pH proxy, Earth Planet. Sci. Lett., 303, 163–173, 2011.
Vengosh, A., Kolodny, Y., Starinsky, A., Chivas, A. R., and McCulloch, M. T.: Coprecipitation and isotopic fractionation of boron in modern biogenic carbonates, Geochim. Cosmochim. Ac., 55, 2901–2910, 1991.
Venn, A., Tambutte, E., Holcomb, M., Allemand, D., and Tambutte, S.: Live Tissue Imaging Shows Reef Corals Elevate pH under Their Calcifying Tissue Relative to Seawater, Plos One, 6, e200013, https://doi.org/10.1371/journal.pone.0020013, 2011.
Wei, G. J., McCulloch, M. T., Mortimer, G., Deng, W. F., and Xie, L. H.: Evidence for ocean acidification in the Great Barrier Reef of Australia, Geochim. Cosmochim. Ac., 73, 2332–2346, 2009.
Yu, J. M. and Elderfield, H.: Benthic foraminiferal B/Ca ratios reflect deep water carbonate saturation state, Earth Planet. Sci. Lett., 258, 73–86, 2007.
Yu, J. M., Elderfield, H., and Hönisch, B.: B/Ca in planktonic foraminifera as a proxy for surface seawater pH, Paleoceanography, 22, PA2202, https://doi.org/10.1029/2006PA001347, 2007.
Yu, J. M., Foster, G. L., Elderfield, H., Broecker, W. S., and Clark, E.: An evaluation of benthic foraminiferal B/Ca and $\delta ^{(11)}$B for deep ocean carbonate ion and pH reconstructions, Earth Plane. Sci. Lett., 293, 114–120, 2010.
Zeebe, R. E.: Stable boron isotope fractionation between dissolved B(OH)3 and B(OH)4-, Geochim. Cosmochim. Ac., 69, 2753–2766, 2005.
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