Mechanisms of Calcification in Coccolithophores

Total Page:16

File Type:pdf, Size:1020Kb

Mechanisms of Calcification in Coccolithophores UNIVERSITY OF SOUTHAMPTON FACULTY OF NATURAL AND ENVIRONMENTAL SCIENCES Ocean and Earth Sciences Mechanisms of Calcification in Coccolithophores Charlotte Elizabeth Walker Thesis for the degree of DOCTOR OF PHILOSOPHY MARCH 2018 UNIVERSITY OF SOUTHAMPTON ABSTRACT FACULTY OF NATURAL AND ENVIRONMENTAL SCIENCES Ocean and Earth Sciences Doctor of Philosophy MECHANISMS OF CALCIFICATION IN COCCOLITHOPHORES By Charlotte Elizabeth Walker Coccolithophores are unicellular marine algae characterised by the production of calcite coccoliths. As a result of their calcification they contribute significantly to global biogeochemical cycles. Comprehensive understanding of the mechanisms behind calcification remains elusive, due in part to the research focus on one species, Emiliania huxleyi; the most globally abundant of all coccolithophores. It is imperative to investigate calcification in other species to better understand this biogeochemically important process, especially as the ecological success of E. huxleyi may be due to certain physiological differences with other species. This study set out to explore differences between species in the mechanisms of calcification in three primary areas. Firstly, the physiological requirement for calcification remains poorly understood, particularly as non-calcifying strains of E. huxleyi grow normally in laboratory culture. This study identified a contrast in the requirement for calcification between E. huxleyi and the ecologically important Coccolithus braarudii. Calcification disruption had no negative impacts on E. huxleyi but resulted in major growth defects in C. braarudii demonstrating an obligate requirement for calcification in this species. Secondly, the previous identification of Si transporters in some coccolithophores was further investigated using a combination of physiological and expression studies to identify that Si plays a role in heterococcolith calcification during their diploid life stage. C. braarudii Si transporters were also found to be regulated in response to available Si and shown to be expressed in natural populations. Finally, coccolith associated polysaccharides (CAPs) are an integral component of the calcification mechanism known to modulate the precipitation of calcite. The data presented here show that extracellular CAPs differ in structure and composition between species and that they also play an important role in the organisation of the coccosphere, expanding upon their role and importance in calcification. These findings mark crucial physiological differences between coccolithophore species. The identification of a requirement for calcification in coccolithophores highlights the importance of maintaining a coccosphere. The requirement for Si in some species suggests major physiological differences between species which may influence their ecology. Consequently, these contrasting physiological characteristics may contribute to significant differences in the response of coccolithophores to future ocean conditions. i List of Contents 1. Introduction 1 1.1 Coccolithophore Introduction 2 1.2 Coccoliths and Calcification 3 1.3 The Evolution of Calcification 7 1.4 The Role of Calcification 11 1.5 Differences Between Species 13 1.6 Current Study 16 2. The Effect of Ge on Coccolithophores 19 2.1 Abstract 20 2.2 Introduction 21 2.3 Materials and Methods 26 2.3.1 Algal strains and culture conditions 26 2.3.2 Physiological Measurements 26 2.4 Results 28 2.4.1 Effect of Ge exposure on Coccolithus braarudii 28 2.4.2 The ratio of Ge/Si 32 2.4.3 Effect of Ge on Coccolithus pelagicus and Calcidiscus leptoporus 34 2.4.4 Effect of Ge on Emiliania huxleyi and Chrysotile carterae 36 2.5 Discussion 39 3. The requirement for Calcification Differs Between Ecologically 45 Important Coccolithophore Species 3.1 Abstract 46 3.2 Introduction 47 3.3 Materials and Methods 50 3.3.1 Algal strains and culture conditions 50 3.3.2 Cell growth and discarded coccoliths 50 3.3.3 Disruption of calcification 50 3.3.4 Measurements of photosynthesis 51 ii 3.3.5 Time-lapse microscopy 52 3.3.6 Fluorescence microscopy 52 3.3.7 Scanning electron microscopy 52 3.3.8 Immunofluorescence microscopy 53 3.4 Results 54 3.4.1 Disruption of calcification in C. braarudii 54 3.4.2 Disruption of calcification inhibits growth in C. braarudii 56 3.4.3 Low Si inhibits growth where coccosphere formation is disrupted 58 3.4.4 Disruption of calcification does not inhibit photosynthesis 60 3.4.5 The role of the coccosphere during cell division 61 3.4.6 Disruption of the coccosphere prevents separation following cell division 63 3.4.7 A polysaccharide-rich organic layer contributes to cell adhesions in the absence 67 of the coccosphere 3.5 Discussion 69 4. Molecular characterisation of Si transporters in Coccolithus 73 braarudii 4.1 Abstract 74 4.2 Introduction 75 4.3 Materials and Methods 79 4.3.1 Algal strains and culture conditions 79 4.3.2 SITL expression analysis 79 4.3.3 C. braarudii SITL expression in natural populations 82 4.4 Results 84 4.4.1 Uptake of [dSi] by coccolithophores 84 4.4.2 SITL expression during changing Si availability 85 4.4.3 SITL expression changes in response to life cycle stage 87 4.4.4 SITL expression in natural populations 88 4.5 Discussion 91 5. Investigating Coccolith Associated Polysaccharides 95 5.1 Abstract 96 5.2 Introduction 97 5.3 Materials and Methods 101 5.3.1 Algal strains and culture conditions 101 iii 5.3.2 Decalcification of coccolithophores 101 5.3.3 Staining and confocal microscopy 101 5.3.4 Electron microscopy 101 5.3.5 Coccolith preparation 102 5.3.6 Polysaccharide extractions 102 5.3.7 GC-MS preparation and analysis 102 5.4 Results 104 5.4.1 Localisation of extracellular polysaccharides using lectin FITC-conA 104 5.4.2 Localisation of extracellular polysaccharides using lectin FITC-WGA 107 5.4.3 Polysaccharide extraction and composition analysis 109 5.4.4 Production and role of extracellular polysaccharides in C. braarudii 111 5.5 Discussion 114 6. General Discussion 119 6.1 Introduction 120 6.2 Discussion the role of calcification 121 6.2.1 Importance of the coccosphere in C. braarudii 121 6.2.2 Calcification as a potential carbon concentrating mechanisms 122 6.3 Introducing Si as a new component to the calcification mechanism 123 6.4 The evolution of calcification 125 6.4.1 Holococcolith formation 125 6.4.2 Si transporters 127 6.4.3 Obligate requirement for calcification 127 6.5 Ecological Impacts 128 6.5.1 Environmental conditions at the time of coccolithophore evolution 128 6.5.2 Current coccolithophore ecology 129 6.5.3 Response to future ocean scenarios 131 6.6 Concluding remarks 132 Appendices 135 References 169 iv List of Tables and Figures 1. Introduction Figure 1.1 Coccolithophores 2 Figure 1.2 Schematic of coccolithophore calcification 5 Figure 1.3 Coccolithophore phylogeny 10 2. The Effect of Ge on Coccolithophores Figure 2.1 The structure and distribution of SITs and SITLs in coccolithophores 22 Figure 2.2 Effect of Ge on C. braarudii 29 Figure 2.3 Morphological effect of Ge on C. braarudii 30 Figure 2.4 Longer-term effects of Ge on C. braarudii 31 Figure 2.5 The effect of changing Ge/Si ratio on C. braarudii 33 Figure 2.6 The effect of Ge on C. pelagicus 35 Figure 2.7 The effect of Ge on C. leptoporus 36 Figure 2.8 The effect of Ge on E. huxleyi 37 Figure 2.9 The effect of Ge on C. carterae 37 Figure 2.10 The distribution of SIT/Ls in coccolithophores correlated with their 38 sensitivity Ge. 3. The requirement for Calcification Differs Between Ecologically Important Coccolithophore Species Figure 3.1 Disruption of calcification in C. braarudii 55 Figure 3.2 Disruption of calcification leads to a reduction in growth in C. braarudii 57 Figure 3.3 Disruption of calcification by limiting Si availability 59 Figure 3.4 Disruption of calcification with low Ca2+ does not inhibit photosynthetic 60 activity Figure 3.5 Rearrangement of the coccosphere during cell division 62 Figure 3.6 Immunofluorescence microscopy of tubulin in dividing cells 63 Figure 3.7 Paired cells accumulate in cells with disrupted calcification 64 Figure 3.8 Progressive disruption of the coccosphere in C. braarudii cells treated 66 with Ge v Figure 3.9 A structured polysaccharide layer is involved in organisation of the 68 coccosphere 4. The Molecular Characterisation of Si Transporters in Coccolithus braarudii Figure 4.1 The structure and distribution of SITs and SITLs in coccolithophores 76 Figure 4.2. Uptake of [dSi] by T. weissflogii, C. braarudii and E. huxleyi 84 Figure 4.3 The expression of SITLs in response to Si reduction 86 Figure 4.4 Expression of SITLs in response to Si replenishment 87 Figure 4.5 The expression of SITL, EFL and RPS1 genes in haploid C. braarudii 88 Figure 4.6 Expression of SITLs in natural coccolithophore populations 90 81 Table 4.1 Primer details for qPCR Table 4.2 Standard Curve Reaction Efficiencies 82 5. Investigating Coccolith Associated Polysaccharides Figure 5.1 Scanning electron microscopy images of coccolithophore species in 104 this study Figure 5.2 Polysaccharide layer found on the cell surface of decalcified 105 coccolithophores Figure 5.3 Polysaccharide layer associated with coccosphere 107 Figure 5.4 Wheat germ agglutinin staining in S. apsteinii 108 Figure 5.5 Differential localisation of lectin stains in S. apsteinii 109 Figure 5.6 Coccolith polysaccaride composition 111 Figure 5.7 The extracellular polysaccharide is associated with the coccoliths in C. 112 braarudii Figure 5.8 The localisation of coccolith associated polysaccharides 114 100 Table 5.1 Coccolith Associated Polysaccharide Extraction Fractions Table 5.2 Results of polysaccharide lectin staining in coccolithophores 106 vi 1. General Discussion Figure 6.1 Key Findings 120 Figure 6.2 Distribution of holococcoliths, Si-transporters and calcification state in 126 culture vii List of Appendices Appendix I: Chapter 2 Supplementary Information Durak et al.
Recommended publications
  • 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.
    [Show full text]
  • The State of the World's Aquatic Genetic Resources for Food and Agriculture 1
    2019 ISSN 2412-5474 THE STATE OF THE WORLD’S AQUATIC GENETIC RESOURCES FOR FOOD AND AGRICULTURE FAO COMMISSION ON GENETIC RESOURCES FOR FOOD AND AGRICULTURE ASSESSMENTS • 2019 FAO COMMISSION ON GENETIC RESOURCES FOR FOOD AND AGRICULTURE ASSESSMENTS • 2019 THE STATE OF THE WORLD’S AQUATIC GENETIC RESOURCES FOR FOOD AND AGRICULTURE COMMISSION ON GENETIC RESOURCES FOR FOOD AND AGRICULTURE FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS ROME 2019 Required citation: FAO. 2019. The State of the World’s Aquatic Genetic Resources for Food and Agriculture. FAO Commission on Genetic Resources for Food and Agriculture assessments. Rome. The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or products of manufacturers, whether or not these have been patented, does not imply that these have been endorsed or recommended by FAO in preference to others of a similar nature that are not mentioned. The views expressed in this information product are those of the author(s) and do not necessarily reflect the views or policies of FAO. ISBN 978-92-5-131608-5 © FAO, 2019 Some rights reserved. This work is available under a CC BY-NC-SA 3.0 IGO licence 2018 © FAO, XXXXXEN/1/05.18 Some rights reserved. This work is made available under the Creative Commons Attribution-NonCommercial- ShareAlike 3.0 IGO licence (CC BY-NC-SA 3.0 IGO; https://creativecommons.org/licenses/by-nc-sa/3.0/igo/ legalcode).
    [Show full text]
  • 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.
    [Show full text]
  • Diversity and Evolution of Protist Mitochondria: Introns, Gene Content and Genome Architecture
    Diversity and Evolution of Protist Mitochondria: Introns, Gene Content and Genome Architecture 著者 西村 祐貴 内容記述 この博士論文は内容の要約のみの公開(または一部 非公開)になっています year 2016 その他のタイトル プロティストミトコンドリアの多様性と進化:イン トロン、遺伝子組成、ゲノム構造 学位授与大学 筑波大学 (University of Tsukuba) 学位授与年度 2015 報告番号 12102甲第7737号 URL http://hdl.handle.net/2241/00144261 Diversity and Evolution of Protist Mitochondria: Introns, Gene Content and Genome Architecture A Dissertation Submitted to the Graduate School of Life and Environmental Sciences, the University of Tsukuba in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy in Science (Doctral Program in Biologial Sciences) Yuki NISHIMURA Table of Contents Abstract ........................................................................................................................... 1 Genes encoded in mitochondrial genomes of eukaryotes ..................................................... 3 Terminology .......................................................................................................................... 4 Chapter 1. General introduction ................................................................................ 5 The origin and evolution of mitochondria ............................................................................ 5 Mobile introns in mitochondrial genome .............................................................................. 6 The organisms which are lacking in mitochondrial genome data ........................................ 8 Chapter 2. Lateral transfers of mobile introns
    [Show full text]
  • Barthelonids Represent a Deep-Branching Metamonad Clade with Mitochondrion-Related Organelles Generating No
    bioRxiv preprint doi: https://doi.org/10.1101/805762; this version posted October 29, 2019. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 2 3 Barthelonids represent a deep-branching Metamonad clade with mitochondrion-related 4 organelles generating no ATP. 5 6 Euki Yazaki1*, Keitaro Kume2, Takashi Shiratori3, Yana Eglit 4,5,, Goro Tanifuji6, Ryo 7 Harada7, Alastair G.B. Simpson4,5, Ken-ichiro Ishida7,8, Tetsuo Hashimoto7,8 and Yuji 8 Inagaki7,9* 9 10 1Department of Biochemistry and Molecular Biology, Graduate School and Faculty of 11 Medicine, The University of Tokyo, Tokyo, Japan 12 2Faculty of Medicine, University of Tsukuba, Ibaraki, Japan 13 3Department of Marine Diversity, Japan Agency for Marine-Earth Science and Technology, 14 Yokosuka, Japan 15 4Department of Biology, Dalhousie University, Halifax, Nova Scotia, Canada 16 5Centre for Comparative Genomics and Evolutionary Bioinformatics, Dalhousie University, 17 Halifax, Nova Scotia, Canada 18 6Department of Zoology, National Museum of Nature and Science, Ibaraki, Japan 19 7Graduate School of Life and Environmental Sciences, University of Tsukuba, Tsukuba, 20 Ibaraki, Japan 21 8Faculty of Life and Environmental Sciences, University of Tsukuba, Ibaraki, Japan 22 9Center for Computational Sciences, University of Tsukuba, Tsukuba, Ibaraki, Japan 23 24 Running head: Phylogeny and putative MRO functions in a new metamonad clade. 25 26 *Correspondence addressed to Euki Yazaki, [email protected] and Yuji Inagaki, 27 [email protected] 1 bioRxiv preprint doi: https://doi.org/10.1101/805762; this version posted October 29, 2019.
    [Show full text]
  • Representative Diatom and Coccolithophore Species Exhibit Divergent Responses Throughout Simulated Upwelling Cycles
    bioRxiv preprint doi: https://doi.org/10.1101/2020.04.30.071480; this version posted May 1, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC 4.0 International license. Representative diatom and coccolithophore species exhibit divergent responses throughout simulated upwelling cycles Robert H. Lampe1,2, Gustavo Hernandez2, Yuan Yu Lin3, and Adrian Marchetti2, 1Integrative Oceanography Division, Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA, USA 2Department of Marine Sciences, University of North Carolina at Chapel Hill, Chapel Hill, NC, USA Phytoplankton communities in upwelling regions experience a ton blooms following upwelling (2, 5, 6). When upwelling wide range of light and nutrient conditions as a result of up- delivers cells and nutrients into well-lit surface waters, di- welling cycles. These cycles can begin with a bloom at the sur- atoms quickly respond to available nitrate and increase their face followed by cells sinking to depth when nutrients are de- nitrate uptake rates compared to other phytoplankton groups pleted. Cells can then be transported back to the surface with allowing them to bloom (7). This phenomenon may partially upwelled waters to seed another bloom. In spite of the physico- be explained by frontloading nitrate assimilation genes, i.e. chemical extremes associated with these cycles, diatoms consis- high expression before the upwelling event occurs, in addi- tently outcompete other phytoplankton when upwelling events occur. Here we simulated the conditions of a complete upwelling tion to diatom’s unique metabolic integration of nitrogen and cycle with a common diatom, Chaetoceros decipiens, and coccol- carbon metabolic pathways (6, 8).
    [Show full text]
  • Detection of Coccolithophore Blooms with Biogeochemical-Argo Floats L
    Detection of Coccolithophore Blooms With BioGeoChemical-Argo Floats L. Terrats, H. Claustre, M. Cornec, Alain Mangin, G. Neukermans To cite this version: L. Terrats, H. Claustre, M. Cornec, Alain Mangin, G. Neukermans. Detection of Coccolithophore Blooms With BioGeoChemical-Argo Floats. Geophysical Research Letters, American Geophysical Union, 2020, 47 (23), 10.1029/2020GL090559. hal-03099761 HAL Id: hal-03099761 https://hal.archives-ouvertes.fr/hal-03099761 Submitted on 6 Jan 2021 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. Distributed under a Creative Commons Attribution - NonCommercial| 4.0 International License RESEARCH LETTER Detection of Coccolithophore Blooms With 10.1029/2020GL090559 BioGeoChemical‐Argo Floats Key Points: L. Terrats1,2 , H. Claustre1 , M. Cornec1 , A. Mangin2, and G. Neukermans3,4 • We matched profiling float trajectories with ocean‐color 1Sorbonne Université, CNRS, Laboratoire d'Océanographie de Villefranche, LOV, Villefranche‐sur‐Mer, France, satellite observations of 2 ‐ 3 coccolithophore blooms ACRI ST, Sophia Antipolis, France, Biology Department, MarSens Research Group, Ghent University, Ghent, Belgium, • Two simple bio‐optical indices 4Flanders Marine Institute (VLIZ), InnovOcean site, Ostend, Belgium permitted successful identification of coccolithophore blooms from floats in the Southern Ocean Coccolithophores (calcifying phytoplankton) form extensive blooms in temperate and subpolar • Abstract A method for identifying ‐ coccolithophore blooms at the global oceans as evidenced from ocean color satellites.
    [Show full text]
  • Introns, Gene Content and Genome Architecture
    Diversity and Evolution of Protist Mitochondria: Introns, Gene Content and Genome Architecture A Dissertation Submitted to the Graduate School of Life and Environmental Sciences, the University of Tsukuba in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy in Science (Doctral Program in Biologial Sciences) Yuki NISHIMURA Table of Contents Abstract ........................................................................................................................... 1 Genes encoded in mitochondrial genomes of eukaryotes ..................................................... 3 Terminology .......................................................................................................................... 4 Chapter 1. General introduction ................................................................................ 5 The origin and evolution of mitochondria ............................................................................ 5 Mobile introns in mitochondrial genome .............................................................................. 6 The organisms which are lacking in mitochondrial genome data ........................................ 8 Chapter 2. Lateral transfers of mobile introns among distantly related mitochondrial genomes ................................................................................................ 11 Summary ................................................................................................................................ 11 2-1. Leucocryptos
    [Show full text]
  • Effects of Increased Pco2 and Temperature on the North Atlantic Spring Bloom. III. Dimethylsulfoniopropionate
    Vol. 388: 41–49, 2009 MARINE ECOLOGY PROGRESS SERIES Published August 19 doi: 10.3354/meps08135 Mar Ecol Prog Ser Effects of increased pCO2 and temperature on the North Atlantic spring bloom. III. Dimethylsulfoniopropionate Peter A. Lee1,*, Jamie R. Rudisill1, Aimee R. Neeley1, 7, Jennifer M. Maucher2, David A. Hutchins3, 8, Yuanyuan Feng3, 8, Clinton E. Hare3, Karine Leblanc3, 9,10, Julie M. Rose3,11, Steven W. Wilhelm4, Janet M. Rowe4, 5, Giacomo R. DiTullio1, 6 1Hollings Marine Laboratory, College of Charleston, 331 Fort Johnson Road, Charleston, South Carolina 29412, USA 2Center for Coastal Environmental Health and Biomolecular Research, National Oceanic and Atmospheric Administration, 219 Fort Johnson Road, Charleston, South Carolina 29412, USA 3College of Marine and Earth Studies, University of Delaware, 700 Pilottown Road, Lewes, Delaware 19958, USA 4Department of Microbiology, University of Tennessee, 1414 West Cumberland Ave, Knoxville, Tennessee 37996, USA 5Department of Plant Pathology, The University of Nebraska, 205 Morrison Center, Lincoln, Nebraska 68583, USA 6Grice Marine Laboratory, College of Charleston, 205 Fort Johnson Road, Charleston, South Carolina 29412, USA 7Present address: National Aeronautics and Space Administration, Calibration and Validation Office, 1450 S. Rolling Road, Suite 4.111, Halethorpe, Maryland 21227, USA 8Present address: Department of Biological Sciences, University of Southern California, 3616 Trousdale Parkway, Los Angeles, California 90089, USA 9Present address: Aix-Marseille Université, CNRS,
    [Show full text]
  • Surface Seawater Plankton Sampling for Coccolithophores Undertaken During IODP Expedition 359
    Betzler, C., Eberli, G.P., Alvarez Zarikian, C.A., and the Expedition 359 Scientists Proceedings of the International Ocean Discovery Program Volume 359 publications.iodp.org doi:10.14379/iodp.proc.359.111.2017 Contents 1 Abstract Data report: surface seawater plankton 1 Introduction sampling for coccolithophores undertaken 1 Materials and methods 3 Results 1 during IODP Expedition 359 5 Biogeography 6 Acknowledgments Jeremy R. Young, Santi Pratiwi, Xiang Su, and the Expedition 359 Scientists2 6 References 7 Appendix Keywords: International Ocean Discovery Program, IODP, JOIDES Resolution, Expedition 359, Indian Ocean transect, Maldives, coccolithophores Abstract Darwin, Australia, to the Maldives (Figure F1A). This transit pre- sented a valuable opportunity to sample the equatorial assemblages Data on extant coccolithophore assemblages from plankton to determine broad patterns of coccolithophore distribution and samples collected during International Ocean Discovery Program compare them with those recorded previously, notably by Kleijne et Expedition 359 to the Maldives is presented. Samples include 12 al. (1989). Sampling continued within the Maldives drilling area to collected during passage across the Indian Ocean from Darwin, (1) determine whether assemblages within the Maldives show evi- Australia, to the Maldives and 40 collected in the Maldives. Assem- dence of ecological restriction or modified assemblages related to blages were analyzed by light and scanning electron microscopy, the particular environment of the atoll chain, (2) investigate repro- and detailed assemblage data are presented. Comparison with pre- ducibility of assemblage data by repeat sampling within a limited vious data from the region suggests that there are consistent distinc- area over an extended period, and (3) investigate the potential of the tive aspects to Indian Ocean assemblages.
    [Show full text]
  • The Influence of Environmental Variability on the Biogeography of Coccolithophores and Diatoms in the Great Calcite Belt Helen E
    Biogeosciences Discuss., doi:10.5194/bg-2017-110, 2017 Manuscript under review for journal Biogeosciences Discussion started: 13 April 2017 c Author(s) 2017. CC-BY 3.0 License. The Influence of Environmental Variability on the Biogeography of Coccolithophores and Diatoms in the Great Calcite Belt Helen E. K. Smith1,2, Alex J. Poulton1,3, Rebecca Garley4, Jason Hopkins5, Laura C. Lubelczyk5, Dave T. Drapeau5, Sara Rauschenberg5, Ben S. Twining5, Nicholas R. Bates2,4, William M. Balch5 5 1National Oceanography Centre, European Way, Southampton, SO14 3ZH, U.K. 2School of Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton Waterfront Campus, European Way, Southampton, SO14 3ZH, U.K. 3Present address: The Lyell Centre, Heriot-Watt University, Edinburgh, EH14 7JG, U.K. 10 4Bermuda Institute of Ocean Sciences, 17 Biological Station, Ferry Reach, St. George's GE 01, Bermuda. 5Bigelow Laboratory for Ocean Sciences, 60 Bigelow Drive, P.O. Box 380, East Boothbay, Maine 04544, USA. Correspondence to: Helen E.K. Smith ([email protected]) Abstract. The Great Calcite Belt (GCB) of the Southern Ocean is a region of elevated summertime upper ocean calcite 15 concentration derived from coccolithophores, despite the region being known for its diatom predominance. The overlap of two major phytoplankton groups, coccolithophores and diatoms, in the dynamic frontal systems characteristic of this region, provides an ideal setting to study environmental influences on the distribution of different species within these taxonomic groups. Water samples for phytoplankton enumeration were collected from the upper 30 m during two cruises, the first to the South Atlantic sector (Jan-Feb 2011; 60o W-15o E and 36-60o S) and the second in the South Indian sector (Feb-Mar 2012; 20 40-120o E and 36-60o S).
    [Show full text]
  • Transcriptomic Response of the Toxic Prymnesiophyte Prymnesium Parvum
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Electronic Publication Information Center Harmful Algae 18 (2012) 1–15 Contents lists available at SciVerse ScienceDirect Harmful Algae jo urnal homepage: www.elsevier.com/locate/hal Transcriptomic response of the toxic prymnesiophyte Prymnesium parvum (N. Carter) to phosphorus and nitrogen starvation a, a,b,1 a,1 a c,d Sa´ra Beszteri *, Ines Yang , Nina Jaeckisch , Urban Tillmann , Stephan Frickenhaus , e a a Gernot Glo¨ckner , Allan Cembella , Uwe John a Department of Ecological Chemistry, Alfred Wegener Institute for Polar and Marine Research, Am Handelshafen 12, 27568 Bremerhaven, Germany b Institute of Medical Microbiology and Hospital Epidemiology, Hannover Medical School, Carl-Neuberg-Str. 1, 30625 Hannover, Germany c Computing centre/Bioinformatics, Alfred Wegener Institute for Polar and Marine Research, Am Handelshafen 12, 27568 Bremerhaven, Germany d Hochschule Bremerhaven, An der Karlstadt 8, 27568 Bremerhaven, Germany e Leibniz-Institute of Freshwater Ecology and Inland Fisheries, IGB, Mu¨ggelseedamm 301, D-12587 Berlin, Germany A R T I C L E I N F O A B S T R A C T Article history: The ichthyotoxic and mixotrophic prymnesiophyte Prymnesium parvum is known to produce dense Received 23 August 2011 virtually monospecific blooms in marine coastal, brackish, and inshore waters. Fish-killing Pyrmnesium Received in revised form 6 March 2012 blooms are often associated with macronutrient imbalanced conditions based upon shifts in ambient Accepted 6 March 2012 nitrogen (N):phosphorus (P) ratios. We therefore investigated nutrient-dependent cellular acclimation Available online 30 March 2012 mechanisms of this microalga based upon construction of a normalized expressed sequence tag (EST) library.
    [Show full text]