Coccolithophore Calcification, Life-Cycle Dynamics and Diversity Response to a Warming and Acidifying Mediterranean Sea
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Overcalcified Forms of the Coccolithophore Emiliania Huxleyi in High CO2 Waters Are Not Pre-Adapted to Ocean Acidification
Biogeosciences Discuss., https://doi.org/10.5194/bg-2017-303 Manuscript under review for journal Biogeosciences Discussion started: 6 September 2017 c Author(s) 2017. CC BY 4.0 License. Overcalcified forms of the coccolithophore Emiliania huxleyi in high CO2 waters are not pre-adapted to ocean acidification. Peter von Dassow1,2,3*, Francisco Díaz-Rosas1,2, El Mahdi Bendif4, Juan-Diego Gaitán-Espitia5, Daniella Mella-Flores1, Sebastian Rokitta6, Uwe John6, and Rodrigo Torres7,8 5 1 Facultad de Ciencias Biológicas, Pontificia Universidad Católica de Chile, Santiago, Chile. 2 Instituto Milenio de Oceanografía de Chile. 3 UMI 3614, Evolutionary Biology and Ecology of Algae, CNRS-UPMC Sorbonne Universités, PUCCh, UACH. 4 Department of Plant Sciences, University of Oxford, OX1 3RB Oxford, UK. 5 CSIRO Oceans and Atmosphere, GPO Box 1538, Hobart 7001, TAS, Australia. 10 6 Marine Biogeosciences | PhytoChange Alfred Wegener Institute – Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany. 7 Centro de Investigación en Ecosistemas de la Patagonia (CIEP), Coyhaique, Chile. 8 Centro de Investigación: Dinámica de Ecosistemas marinos de Altas Latitudes (IDEAL), Punta Arenas, Chile. Correspondence to: Peter von Dassow ([email protected]) 15 Abstract. Marine multicellular organisms inhabiting waters with natural high fluctuations in pH appear more tolerant to acidification than conspecifics occurring in nearby stable waters, suggesting that environments of fluctuating pH hold genetic reservoirs for adaptation of key groups to ocean acidification (OA). The abundant and cosmopolitan calcifying phytoplankton Emiliania huxleyi exhibits a range of morphotypes with varying degrees of coccolith mineralization. We show that E. huxleyi populations in the naturally acidified upwelling waters of the Eastern South Pacific, where pH drops below 20 7.8 as is predicted for the global surface ocean by the year 2100, are dominated by exceptionally overcalcified morphotypes whose distal coccolith shield can be almost solid calcite. -
University of Oklahoma
UNIVERSITY OF OKLAHOMA GRADUATE COLLEGE MACRONUTRIENTS SHAPE MICROBIAL COMMUNITIES, GENE EXPRESSION AND PROTEIN EVOLUTION A DISSERTATION SUBMITTED TO THE GRADUATE FACULTY in partial fulfillment of the requirements for the Degree of DOCTOR OF PHILOSOPHY By JOSHUA THOMAS COOPER Norman, Oklahoma 2017 MACRONUTRIENTS SHAPE MICROBIAL COMMUNITIES, GENE EXPRESSION AND PROTEIN EVOLUTION A DISSERTATION APPROVED FOR THE DEPARTMENT OF MICROBIOLOGY AND PLANT BIOLOGY BY ______________________________ Dr. Boris Wawrik, Chair ______________________________ Dr. J. Phil Gibson ______________________________ Dr. Anne K. Dunn ______________________________ Dr. John Paul Masly ______________________________ Dr. K. David Hambright ii © Copyright by JOSHUA THOMAS COOPER 2017 All Rights Reserved. iii Acknowledgments I would like to thank my two advisors Dr. Boris Wawrik and Dr. J. Phil Gibson for helping me become a better scientist and better educator. I would also like to thank my committee members Dr. Anne K. Dunn, Dr. K. David Hambright, and Dr. J.P. Masly for providing valuable inputs that lead me to carefully consider my research questions. I would also like to thank Dr. J.P. Masly for the opportunity to coauthor a book chapter on the speciation of diatoms. It is still such a privilege that you believed in me and my crazy diatom ideas to form a concise chapter in addition to learn your style of writing has been a benefit to my professional development. I’m also thankful for my first undergraduate research mentor, Dr. Miriam Steinitz-Kannan, now retired from Northern Kentucky University, who was the first to show the amazing wonders of pond scum. Who knew that studying diatoms and algae as an undergraduate would lead me all the way to a Ph.D. -
Phytoplankton As Key Mediators of the Biological Carbon Pump: Their Responses to a Changing Climate
sustainability Review Phytoplankton as Key Mediators of the Biological Carbon Pump: Their Responses to a Changing Climate Samarpita Basu * ID and Katherine R. M. Mackey Earth System Science, University of California Irvine, Irvine, CA 92697, USA; [email protected] * Correspondence: [email protected] Received: 7 January 2018; Accepted: 12 March 2018; Published: 19 March 2018 Abstract: The world’s oceans are a major sink for atmospheric carbon dioxide (CO2). The biological carbon pump plays a vital role in the net transfer of CO2 from the atmosphere to the oceans and then to the sediments, subsequently maintaining atmospheric CO2 at significantly lower levels than would be the case if it did not exist. The efficiency of the biological pump is a function of phytoplankton physiology and community structure, which are in turn governed by the physical and chemical conditions of the ocean. However, only a few studies have focused on the importance of phytoplankton community structure to the biological pump. Because global change is expected to influence carbon and nutrient availability, temperature and light (via stratification), an improved understanding of how phytoplankton community size structure will respond in the future is required to gain insight into the biological pump and the ability of the ocean to act as a long-term sink for atmospheric CO2. This review article aims to explore the potential impacts of predicted changes in global temperature and the carbonate system on phytoplankton cell size, species and elemental composition, so as to shed light on the ability of the biological pump to sequester carbon in the future ocean. -
An Explanation for the 18O Excess in Noelaerhabdaceae Coccolith Calcite
Available online at www.sciencedirect.com ScienceDirect Geochimica et Cosmochimica Acta 189 (2016) 132–142 www.elsevier.com/locate/gca An explanation for the 18O excess in Noelaerhabdaceae coccolith calcite M. Hermoso a,⇑, F. Minoletti b,c, G. Aloisi d,e, M. Bonifacie f, H.L.O. McClelland a,1, N. Labourdette b,c, P. Renforth g, C. Chaduteau f, R.E.M. Rickaby a a University of Oxford – Department of Earth Sciences, South Parks Road, Oxford OX1 3AN, United Kingdom b Sorbonne Universite´s, UPMC Universite´ Paris 06 – Institut de Sciences de la Terre de Paris (ISTeP), 4 Place Jussieu, 75252 Paris Cedex 05, France c CNRS – UMR 7193 ISTeP, 4 Place Jussieu, 75252 Paris Cedex 05, France d Sorbonne Universite´s, UPMC Universite´ Paris 06 – UMR 7159 LOCEAN, 4 Place Jussieu, 75005 Paris, France e CNRS – UMR 7159 LOCEAN, 4 Place Jussieu, 75005 Paris, France f Institut de Physique du Globe de Paris, Sorbonne Paris Cite´, Universite´ Paris-Diderot, UMR CNRS 7154, 1 rue Jussieu, 75238 Paris Cedex, France g Cardiff University – School of Earth and Ocean Sciences, Parks Place, Cardiff CF10 3AT, United Kingdom Received 10 November 2015; accepted in revised form 11 June 2016; available online 18 June 2016 Abstract Coccoliths have dominated the sedimentary archive in the pelagic environment since the Jurassic. The biominerals pro- duced by the coccolithophores are ideally placed to infer sea surface temperatures from their oxygen isotopic composition, as calcification in this photosynthetic algal group only occurs in the sunlit surface waters. In the present study, we dissect the isotopic mechanisms contributing to the ‘‘vital effect”, which overprints the oceanic temperatures recorded in coccolith calcite. -
Biology and Systematics of Heterokont and Haptophyte Algae1
American Journal of Botany 91(10): 1508±1522. 2004. BIOLOGY AND SYSTEMATICS OF HETEROKONT AND HAPTOPHYTE ALGAE1 ROBERT A. ANDERSEN Bigelow Laboratory for Ocean Sciences, P.O. Box 475, West Boothbay Harbor, Maine 04575 USA In this paper, I review what is currently known of phylogenetic relationships of heterokont and haptophyte algae. Heterokont algae are a monophyletic group that is classi®ed into 17 classes and represents a diverse group of marine, freshwater, and terrestrial algae. Classes are distinguished by morphology, chloroplast pigments, ultrastructural features, and gene sequence data. Electron microscopy and molecular biology have contributed signi®cantly to our understanding of their evolutionary relationships, but even today class relationships are poorly understood. Haptophyte algae are a second monophyletic group that consists of two classes of predominately marine phytoplankton. The closest relatives of the haptophytes are currently unknown, but recent evidence indicates they may be part of a large assemblage (chromalveolates) that includes heterokont algae and other stramenopiles, alveolates, and cryptophytes. Heter- okont and haptophyte algae are important primary producers in aquatic habitats, and they are probably the primary carbon source for petroleum products (crude oil, natural gas). Key words: chromalveolate; chromist; chromophyte; ¯agella; phylogeny; stramenopile; tree of life. Heterokont algae are a monophyletic group that includes all (Phaeophyceae) by Linnaeus (1753), and shortly thereafter, photosynthetic organisms with tripartite tubular hairs on the microscopic chrysophytes (currently 5 Oikomonas, Anthophy- mature ¯agellum (discussed later; also see Wetherbee et al., sa) were described by MuÈller (1773, 1786). The history of 1988, for de®nitions of mature and immature ¯agella), as well heterokont algae was recently discussed in detail (Andersen, as some nonphotosynthetic relatives and some that have sec- 2004), and four distinct periods were identi®ed. -
Reduced Calcification of Marine Plankton in Response to Increased
letters to nature Acknowledgements representatives of the coccolithophorids, Emiliania huxleyi and This research was sponsored by the EPSRC. T.W.F. ®rst suggested the electrochemical Gephyrocapsa oceanica, are both bloom-forming and have a deoxidation of titanium metal. G.Z.C. was the ®rst to observe that it was possible to reduce world-wide distribution. G. oceanica is the dominant coccolitho- thick layers of oxide on titanium metal using molten salt electrochemistry. D.J.F. suggested phorid in neritic environments of tropical waters9, whereas the experiment, which was carried out by G.Z.C., on the reduction of the solid titanium dioxide pellets. M. S. P. Shaffer took the original SEM image of Fig. 4a. E. huxleyi, one of the most prominent producers of calcium carbonate in the world ocean10, forms extensive blooms covering Correspondence and requests for materials should be addressed to D. J. F. large areas in temperate and subpolar latitudes9,11. (e-mail: [email protected]). The response of these two species to CO2-related changes in seawater carbonate chemistry was examined under controlled ................................................................. pH Reduced calci®cation 8.4 8.2 8.1 8.0 7.9 7.8 PCO2 (p.p.m.v.) of marine plankton in response 200 400 600 800 a 10 to increased atmospheric CO2 ) 8 –1 Ulf Riebesell *, Ingrid Zondervan*, BjoÈrn Rost*, Philippe D. Tortell², d –1 Richard E. Zeebe*³ & FrancËois M. M. Morel² 6 * Alfred Wegener Institute for Polar and Marine Research, P.O. Box 120161, 4 D-27515 Bremerhaven, Germany mol C cell –13 ² Department of Geosciences & Department of Ecology and Evolutionary Biology, POC production Princeton University, Princeton, New Jersey 08544, USA (10 2 ³ Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York 10964, USA 0 ............................................................................................................................................. -
Coccolithophore Distribution in the Mediterranean Sea and Relate A
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Ocean Sci. Discuss., 11, 613–653, 2014 Open Access www.ocean-sci-discuss.net/11/613/2014/ Ocean Science OSD doi:10.5194/osd-11-613-2014 Discussions © Author(s) 2014. CC Attribution 3.0 License. 11, 613–653, 2014 This discussion paper is/has been under review for the journal Ocean Science (OS). Coccolithophore Please refer to the corresponding final paper in OS if available. distribution in the Mediterranean Sea Is coccolithophore distribution in the A. M. Oviedo et al. Mediterranean Sea related to seawater carbonate chemistry? Title Page Abstract Introduction A. M. Oviedo1, P. Ziveri1,2, M. Álvarez3, and T. Tanhua4 Conclusions References 1Institute of Environmental Science and Technology (ICTA), Universitat Autonoma de Barcelona (UAB), 08193 Bellaterra, Spain Tables Figures 2Earth & Climate Cluster, Department of Earth Sciences, FALW, Vrije Universiteit Amsterdam, FALW, HV1081 Amsterdam, the Netherlands J I 3IEO – Instituto Espanol de Oceanografia, Apd. 130, A Coruna, 15001, Spain 4GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel, Marine Biogeochemistry, J I Duesternbrooker Weg 20, 24105 Kiel, Germany Back Close Received: 31 December 2013 – Accepted: 15 January 2014 – Published: 20 February 2014 Full Screen / Esc Correspondence to: A. M. Oviedo ([email protected]) Published by Copernicus Publications on behalf of the European Geosciences Union. Printer-friendly Version Interactive Discussion 613 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract OSD The Mediterranean Sea is considered a “hot-spot” for climate change, being char- acterized by oligotrophic to ultra-oligotrophic waters and rapidly changing carbonate 11, 613–653, 2014 chemistry. Coccolithophores are considered a dominant phytoplankton group in these 5 waters. -
The Coccolithophore Family Calciosoleniaceae with Report of A
The coccolithophore family Calciosoleniaceae with report of a new species: Calciosolenia subtropicus from the southern Indian Ocean Shramik Patil, Rahul Mohan, Syed Jafar, Sahina Gazi, Pallavi Choudhari, Xavier Crosta To cite this version: Shramik Patil, Rahul Mohan, Syed Jafar, Sahina Gazi, Pallavi Choudhari, et al.. The coccolithophore family Calciosoleniaceae with report of a new species: Calciosolenia subtropicus from the southern Indian Ocean. Micropaleontology, Micropaleontology Press, 2019. hal-02323185 HAL Id: hal-02323185 https://hal.archives-ouvertes.fr/hal-02323185 Submitted on 22 Oct 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. The coccolithophore family Calciosoleniaceae with report of a new species: Calciosolenia subtropicus from the southern Indian Ocean Shramik Patil1, Rahul Mohan1, Syed A. Jafar2, Sahina Gazi1, Pallavi Choudhari1 and Xavier Crosta3 1National Centre for Polar and Ocean Research (NCPOR), Headland Sada, Vasco-da-Gama, Goa-403804, India email: [email protected] 2Flat 5-B, Whispering Meadows, Haralur Road, Bangalore-560 102, India 3UMR-CNRS 5805 EPOC, Université de Bordeaux, Allée Geoffroy Saint Hilaire, 33615 Pessac Cedex, France ABSTRACT: The families Calciosoleniaceae, Syracosphaeraceae and Rhabdosphaeraceae belong to the order Syracosphaerales and constitute a significant component of extant coccolithophore species, sharing similar ultrastructural bauplans. -
Stromatolites Below the Photic Zone in the Northern Arabian Sea Formed by Calcifying Chemotrophic Microbial Mats
Stromatolites below the photic zone in the northern Arabian Sea formed by calcifying chemotrophic microbial mats Tobias Himmler1*, Daniel Smrzka2, Jennifer Zwicker2, Sabine Kasten3,4, Russell S. Shapiro5, Gerhard Bohrmann1, and Jörn Peckmann2,6 1MARUM–Zentrum für Marine Umweltwissenschaften und Fachbereich Geowissenschaften, Universität Bremen, 28334 Bremen, Germany 2Department für Geodynamik und Sedimentologie, Erdwissenschaftliches Zentrum, Universität Wien, 1090 Wien, Austria 3Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, 27570 Bremerhaven, Germany 4Fachbereich Geowissenschaften, Universität Bremen, 28359 Bremen, Germany 5Geological and Environmental Sciences Department, California State University–Chico, Chico, California 95929, USA 6Institut für Geologie, Centrum für Erdsystemforschung und Nachhaltigkeit, Universität Hamburg, 20146 Hamburg, Germany − − + 2− + ABSTRACT reduction: HS + NO3 + H + H2O → SO4 + NH4 (cf. Fossing et al., 1995; Chemosynthesis increases alkalinity and facilitates stromatolite Otte et al., 1999). The effect of this process, referred to as nitrate-driven growth at methane seeps in 731 m water depth within the oxygen sulfide oxidation (ND-SO), is amplified when it takes place near hotspots minimum zone (OMZ) in the northern Arabian Sea. Microbial fab- of SD-AOM (Siegert et al., 2013). Therefore, it has been hypothesized rics, including mineralized filament bundles resembling the sulfide- that fossilization of sulfide-oxidizing bacteria may occur during seep- oxidizing bacterium Thioploca, mineralized extracellular polymeric carbonate formation (Bailey et al., 2009). Yet, seep carbonates resulting substances, and fossilized rod-shaped and filamentous cells, all pre- from the putative interaction of sulfide-oxidizing bacteria with the SD- served in 13C-depleted authigenic carbonate, suggest that biofilm cal- AOM consortium have, to the best of our knowledge, only been recognized cification resulted from nitrate-driven sulfide oxidation (ND-SO) and in ancient seep deposits (Peckmann et al., 2004). -
Is Coccolithophore Distribution in the Mediterranean Sea Related to Seawater Carbonate Chemistry? A
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Ocean Sci. Discuss., 11, 613–653, 2014 Open Access www.ocean-sci-discuss.net/11/613/2014/ Ocean Science doi:10.5194/osd-11-613-2014 Discussions © Author(s) 2014. CC Attribution 3.0 License. This discussion paper is/has been under review for the journal Ocean Science (OS). Please refer to the corresponding final paper in OS if available. Is coccolithophore distribution in the Mediterranean Sea related to seawater carbonate chemistry? A. M. Oviedo1, P. Ziveri1,2, M. Álvarez3, and T. Tanhua4 1Institute of Environmental Science and Technology (ICTA), Universitat Autonoma de Barcelona (UAB), 08193 Bellaterra, Spain 2Earth & Climate Cluster, Department of Earth Sciences, FALW, Vrije Universiteit Amsterdam, FALW, HV1081 Amsterdam, the Netherlands 3IEO – Instituto Espanol de Oceanografia, Apd. 130, A Coruna, 15001, Spain 4GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel, Marine Biogeochemistry, Duesternbrooker Weg 20, 24105 Kiel, Germany Received: 31 December 2013 – Accepted: 15 January 2014 – Published: 20 February 2014 Correspondence to: A. M. Oviedo ([email protected]) Published by Copernicus Publications on behalf of the European Geosciences Union. 613 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract The Mediterranean Sea is considered a “hot-spot” for climate change, being char- acterized by oligotrophic to ultra-oligotrophic waters and rapidly changing carbonate chemistry. Coccolithophores are considered a dominant phytoplankton group in these 5 waters. As a marine calcifying organism they are expected to respond to the ongo- ing changes in seawater CO2 systems parameters. However, very few studies have covered the entire Mediterranean physiochemical gradients from the Strait of Gibral- tar to the Eastern Mediterranean Levantine Basin. -
Observations on Syracosphaera Rhombica Sp. Nov
Disponible en ligne sur ScienceDirect www.sciencedirect.com Revue de micropaléontologie 59 (2016) 233–237 Coccolithophores in modern oceans Observations on Syracosphaera rhombica sp. nov. Observations sur Syracosphaera rhombica sp. nov. a b c,∗ Harald Andruleit , Aisha Ejura Agbali , Richard W. Jordan a Bundesanstalt für Geowissenschaften und Rohstoffe (BGR), Stilleweg 2, 30655 Hannover, Germany b Earth, Ocean and Atmospheric Science, Florida State University, P.O. Box 3064520, Tallahassee, FL 32306-4520, USA c Department of Earth & Environmental Sciences, Faculty of Science, Yamagata University, 1-4-12 Kojirakawa-machi, Yamagata 990-8560, Japan Abstract A spherical coccosphere and two collapsed coccospheres composed of monomorphic rhombic coccoliths were encountered in 2005 in the Java upwelling system of the SE Indian Ocean, while a further two specimens with elongate coccospheres were recently found in the Gulf of Mexico. All of the specimens were collected from the lower photic zone (75–160 m). The coccoliths possess a proximal flange, a slightly flared wall with a serrated distal margin, and a relatively plain central area structure comprised only of overlapping laths. The taxon appears to be an undescribed species of the Syracosphaera nodosa group, so we describe it herein as Syracosphaera rhombica sp. nov. © 2016 Published by Elsevier Masson SAS. Keywords: Coccolithophorid; Gulf of Mexico; Indian Ocean; Lower photic zone; Syracosphaera Résumé Une coccosphère sphérique (ainsi que deux coccosphères effondrées) composée de coccolithes rhombiques monomorphiques a été rencontrée en 2005 dans le système de remontée d’eaux profondes de Java dans l’océan Indien du Sud-Est, tandis que deux autres spécimens avec coccosphères allongées ont été récemment trouvées dans le golfe du Mexique. -
Phytobase: a Global Synthesis of Open-Ocean Phytoplankton Occurrences
Research Collection Journal Article PhytoBase: A global synthesis of open-ocean phytoplankton occurrences Author(s): Righetti, Damiano; Vogt, Meike; Zimmermann, Niklaus E.; Guiry, Michael D.; Gruber, Nicolas Publication Date: 2020 Permanent Link: https://doi.org/10.3929/ethz-b-000414680 Originally published in: Earth System Science Data 12(2), http://doi.org/10.5194/essd-12-907-2020 Rights / License: Creative Commons Attribution 4.0 International This page was generated automatically upon download from the ETH Zurich Research Collection. For more information please consult the Terms of use. ETH Library Earth Syst. Sci. Data, 12, 907–933, 2020 https://doi.org/10.5194/essd-12-907-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. PhytoBase: A global synthesis of open-ocean phytoplankton occurrences Damiano Righetti1, Meike Vogt1, Niklaus E. Zimmermann2, Michael D. Guiry3, and Nicolas Gruber1 1Environmental Physics, Institute of Biogeochemistry and Pollutant Dynamics, ETH Zürich, Universitätstrasse 16, 8092 Zürich, Switzerland 2Dynamic Macroecology, Landscape Dynamics, Swiss Federal Research Institute WSL, 8903 Birmensdorf, Switzerland 3AlgaeBase, Ryan Institute, NUI, Galway, University Road, Galway H91 TK33, Ireland Correspondence: Damiano Righetti ([email protected]) Received: 3 September 2019 – Discussion started: 14 October 2019 Revised: 24 February 2020 – Accepted: 11 March 2020 – Published: 24 April 2020 Abstract. Marine phytoplankton are responsible for half of the global net primary production and perform mul- tiple other ecological functions and services of the global ocean. These photosynthetic organisms comprise more than 4300 marine species, but their biogeographic patterns and the resulting species diversity are poorly known, mostly owing to severe data limitations.