Calcification Patterns of the Coccolithophore Coccolithus Braarudii (Haptophyta), from the Late Quaternary to Present in the Southern Ocean
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The Crazy Calcium Cycle. Eduardo A. Espeso Department of Cellular And
The CRaZy calcium cycle. Eduardo A. Espeso Department of Cellular and Molecular Biology Centro de Investigaciones Biológicas, CSIC. Ramiro de Maeztu, 9. 28040-Madrid. Spain. Key words: Crz1, calcineurin signaling, calcium pump, calcium channel, P-type ATPase, magnesium homeostasis Summary. Calcium is an essential cation for a cell. This cation participates in the regulation of numerous processes in either prokaryote s or eukaryotes, from bacteria to humans. Saccharomyces cerevisiae has served as a model organism to understand calcium homeostasis and calcium-dependent signaling in fungi. In this chapter it will be reviewed known and predicted transport mechanisms that mediate calcium homeostasis in the yeast. How and when calcium enters the cell, how and where it is stored, when is reutilized, and finally secreted to the environment to close the cycle. As a second messenger, maintenance of a controlled free intracellular calcium concentration is important for mediating transcriptional regulation. Many environmental stimuli modify the concentration of cytoplasmic free calcium generating the "calcium signal". This is sensed and transduced through the calmodulin/calcineurin pathway to a transcription factor, named c alcineurin-r esponsive z inc finger, CRZ, also known as "crazy" , to mediate transcriptional regulation of a large number of genes of diverse pathways including a negative feedback regulation of the calcium homeostasis system. A model of calcium regulation in yeasts In higher eukaryotes entry of calcium in the cell starts concatenated signaling events some of them are of enormous importance in animals such as initiation of the heartbeat or the synapses between neurons. In the budding yeast calcium mediates adaptation to a variety of stimuli such as the presence of mating pheromones (Iida et al., 1990), a damage to endoplasmic reticulum (Bonilla and Cunningham, 2003), and different ambient stresses like salinity, alkaline pH or high osmolarity [reviewed in (Cunningham, 2005)]. -
Ecology of Oceanic Coccolithophores. I. Nutritional Preferences of the Two Stages in the Life Cycle of Coccolithus Braarudii and Calcidiscus Leptoporus
AQUATIC MICROBIAL ECOLOGY Vol. 44: 291–301, 2006 Published October 10 Aquat Microb Ecol Ecology of oceanic coccolithophores. I. Nutritional preferences of the two stages in the life cycle of Coccolithus braarudii and Calcidiscus leptoporus Aude Houdan, Ian Probert, Céline Zatylny, Benoît Véron*, Chantal Billard Laboratoire de Biologie et Biotechnologies Marines, Université de Caen Basse-Normandie, Esplanade de la Paix, 14032 Caen Cedex, France ABSTRACT: Coccolithus braarudii and Calcidiscus leptoporus are 2 coccolithophores (Prymnesio- phyceae: Haptophyta) known to possess a complex heteromorphic life cycle, with alternation between a motile holococcolith-bearing haploid stage and a non-motile heterococcolith-bearing diploid stage. The ecological implications of this type of life cycle in coccolithophores are currently poorly known. The nutritional preferences of each stage of both species, and their growth response to conditions of turbulence were investigated by varying their growth conditions. Of the different cul- ture media tested, only the synthetic seawater medium did not support the growth of both stages of C. braarudii and C. leptoporus. With natural seawater-based media, the growth rate of the haploid phase of both coccolithophores was stimulated by the addition of soil extract (K/2: 0.23 ± 0.02 d–1 and K/2 with soil extract 0.35 ± 0.01 d–1 for the C. braarudii haploid stage), while the diploid phase was not, indicating that the motile stage is capable of utilizing compounds present in soil extract or ingest- ing bacteria that are activated in enriched media. The addition of sodium acetate to the medium also stimulated the haploid phase of C. -
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. -
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. -
The Plankton Lifeform Extraction Tool: a Digital Tool to Increase The
Discussions https://doi.org/10.5194/essd-2021-171 Earth System Preprint. Discussion started: 21 July 2021 Science c Author(s) 2021. CC BY 4.0 License. Open Access Open Data The Plankton Lifeform Extraction Tool: A digital tool to increase the discoverability and usability of plankton time-series data Clare Ostle1*, Kevin Paxman1, Carolyn A. Graves2, Mathew Arnold1, Felipe Artigas3, Angus Atkinson4, Anaïs Aubert5, Malcolm Baptie6, Beth Bear7, Jacob Bedford8, Michael Best9, Eileen 5 Bresnan10, Rachel Brittain1, Derek Broughton1, Alexandre Budria5,11, Kathryn Cook12, Michelle Devlin7, George Graham1, Nick Halliday1, Pierre Hélaouët1, Marie Johansen13, David G. Johns1, Dan Lear1, Margarita Machairopoulou10, April McKinney14, Adam Mellor14, Alex Milligan7, Sophie Pitois7, Isabelle Rombouts5, Cordula Scherer15, Paul Tett16, Claire Widdicombe4, and Abigail McQuatters-Gollop8 1 10 The Marine Biological Association (MBA), The Laboratory, Citadel Hill, Plymouth, PL1 2PB, UK. 2 Centre for Environment Fisheries and Aquacu∑lture Science (Cefas), Weymouth, UK. 3 Université du Littoral Côte d’Opale, Université de Lille, CNRS UMR 8187 LOG, Laboratoire d’Océanologie et de Géosciences, Wimereux, France. 4 Plymouth Marine Laboratory, Prospect Place, Plymouth, PL1 3DH, UK. 5 15 Muséum National d’Histoire Naturelle (MNHN), CRESCO, 38 UMS Patrinat, Dinard, France. 6 Scottish Environment Protection Agency, Angus Smith Building, Maxim 6, Parklands Avenue, Eurocentral, Holytown, North Lanarkshire ML1 4WQ, UK. 7 Centre for Environment Fisheries and Aquaculture Science (Cefas), Lowestoft, UK. 8 Marine Conservation Research Group, University of Plymouth, Drake Circus, Plymouth, PL4 8AA, UK. 9 20 The Environment Agency, Kingfisher House, Goldhay Way, Peterborough, PE4 6HL, UK. 10 Marine Scotland Science, Marine Laboratory, 375 Victoria Road, Aberdeen, AB11 9DB, UK. -
The Calcium Cycle
Curriculum Units by Fellows of the Yale-New Haven Teachers Institute 1985 Volume VII: Skeletal Materials- Biomineralization The Calcium Cycle Curriculum Unit 85.07.08 by Bill Duesing INTRODUCTION This unit is designed to be part of the Ecology course which is taught by High School in the Community at the West Rock Nature Center for four hours a day during the last quarter of the school year, The present ecology course involves both theoretical and practical studies relating to the earth and how it works. We will trace calcium in the biosphere from its location in igneous rocks in the early history of the earth to its location in the skeletons of high school students at the Nature Center. In the process of studying the transport and deposition of calcium we have a vehicle which touches on many of the important concepts we are teaching and relates to some of the hands-on activities the students are involved in. Some of the connections between the calcium cycle and the Ecology course are: Geology: Many of the students have no idea of the age and history of the earth and the great changes which it has gone through. How the calcium stored in the rocks in northwestern Connecticut came to be there touches on much of this chemistry: Most of the students have had very little exposure to chemistry, yet it is important in the study of ecology. Using the study of calcium, some simple chemical principles can be introduced such as the fact that calcium is intimately associated with carbon dioxide (CO2), as the solid calcium carbonate (CaCO3), and therefore is involved with life and life forms. -
Integrative Taxonomy of the Pavlovophyceae (Haptophyta): a Reassessment
Protist, Vol. 162, 738–761, November 2011 http://www.elsevier.de/protis Published online date 28 June 2011 ORIGINAL PAPER Integrative Taxonomy of the Pavlovophyceae (Haptophyta): A Reassessment El Mahdi Bendifa,b,1, Ian Proberta,2, Annie Hervéc, Chantal Billardb, Didier Gouxd, Christophe Lelongb, Jean-Paul Cadoretc, and Benoît Vérona,b,3 aUniversité de Caen Basse-Normandie, Algobank-Caen, IFR 146, 14032 Caen, France bUniversité de Caen Basse-Normandie, UMR 100 PE2 M - IFREMER, 14032 Caen, France cIFREMER, Laboratoire de Physiologie et Biotechnologie des Algues, rue de l’Ile d’Yeu, BP21105, 44311 Nantes, France dUniversité de Caen Basse-Normandie, Centre de Microscopie Appliquée à la Biologie, IFR 146, 14032 Caen, France Submitted October 18, 2010; Accepted March 15, 2011 Monitoring Editor: Barry S. C. Leadbeater. The Pavlovophyceae (Haptophyta) contains four genera (Pavlova, Diacronema, Exanthemachrysis and Rebecca) and only thirteen characterised species, several of which are important in ecological and eco- nomic contexts. We have constructed molecular phylogenies inferred from sequencing of ribosomal gene markers with comprehensive coverage of the described diversity, using type strains when avail- able, together with additional cultured strains. The morphology and ultrastructure of 12 of the described species was also re-examined and the pigment signatures of many culture strains were determined. The molecular analysis revealed that sequences of all described species differed, although those of Pavlova gyrans and P. pinguis were nearly identical, these potentially forming a single cryptic species complex. Four well-delineated genetic clades were identified, one of which included species of both Pavlova and Diacronema. Unique combinations of morphological/ultrastructural characters were iden- tified for each of these clades. -
Calcium Isotopes in Scleractinian Fossil Corals Since the Mesozoic: Implications for Vital Effects and Biomineralization Through Time ∗ Anne M
Earth and Planetary Science Letters 444 (2016) 205–214 Contents lists available at ScienceDirect Earth and Planetary Science Letters www.elsevier.com/locate/epsl Calcium isotopes in scleractinian fossil corals since the Mesozoic: Implications for vital effects and biomineralization through time ∗ Anne M. Gothmann a, , Michael L. Bender a, Clara L. Blättler a, Peter K. Swart b, Sharmila J. Giri b, Jess F. Adkins c, Jarosław Stolarski d, John A. Higgins a a Princeton University, Department of Geosciences, Princeton, NJ, USA b University of Miami, Department of Marine Geosciences, Miami, FL, USA c California Institute of Technology, Division of Geological and Planetary Sciences, Pasadena, CA, USA d Institute of Paleobiology, Polish Academy of Sciences, Warsaw, Poland a r t i c l e i n f o a b s t r a c t 44/40 Article history: We present a Cenozoic record of δ Ca from well preserved scleractinian fossil corals, as well as fossil 44/40 Received 24 September 2015 coral δ Ca data from two time periods during the Mesozoic (84 and 160 Ma). To complement the Received in revised form 27 February 2016 coral data, we also extend existing bulk pelagic carbonate records back to ∼80 Ma. The same fossil Accepted 6 March 2016 corals used for this study were previously shown to be excellently preserved, and to be faithful archives Available online 7 April 2016 44/40 of past seawater Mg/Ca and Sr/Ca since ∼200 Ma (Gothmann et al., 2015). We find that the δ Ca Editor: H. Stoll compositions of bulk pelagic carbonates from ODP Site 807 (Ontong Java Plateau) and DSDP Site 516 (Rio 44/40 Keywords: Grande Rise) have not varied by more than ∼±0.20h over the last ∼80 Myr. -
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. -
A 15 Million-Year Long Record of Phenotypic Evolution in the Heavily Calcified Coccolithophore Helicosphaera and Its Biogeochemical Implications
A 15 million-year long record of phenotypic evolution in the heavily calcified coccolithophore Helicosphaera and its biogeochemical implications 5 Luka Šupraha1, a, Jorijntje Henderiks1, 2 1 Department of Earth Sciences, Uppsala University, Villavägen 16, SE-752 36 Uppsala, Sweden. 2 Centre for Ecological and Evolutionary Synthesis (CEES), Department of Biosciences, University of Oslo, P.O. Box 1066 Blindern, 0316 Oslo, Norway. a Present address: Section for Aquatic Biology and Toxicology (AQUA), Department of Biosciences, University of Oslo, P.O. 10 Box 1066 Blindern, 0316 Oslo, Norway Correspondence to: Luka Šupraha ([email protected]) Abstract. The biogeochemical impact of coccolithophores is defined by their overall abundance in the oceans, but also by a wide range in physiological traits such as cell size, degree of calcification and carbon production rates between different species. Species’ “sensitivity” to environmental forcing has been suggested to relate to their cellular PIC:POC ratio and other 15 physiological constraints. Understanding both the short and longer-term adaptive strategies of different coccolithophore lineages, and how these in turn shape the biogeochemical role of the group, is therefore crucial for modeling the ongoing changes in the global carbon cycle. Here we present data on the phenotypic evolution of a large and heavily-calcified genus Helicosphaera (order Zygodiscales) over the past 15 million years (Ma), at two deep-sea drill sites from the tropical Indian Ocean and temperate South Atlantic. The modern species Helicosphaera carteri, which displays eco-physiological adaptations 20 in modern strains, was used to benchmark the use of its coccolith morphology as a physiological proxy in the fossil record. -
On the Ultrastructure of Gephyrocapsa Oceanica (Haptophyta) Life Stages
Cryptogamie, Algologie, 2014, 35 (4): 379-388 © 2014 Adac. Tous droits réservés On the ultrastructure of Gephyrocapsa oceanica (Haptophyta) life stages El Mahdi BENDIFa* & Jeremy YOUNGb aMarine Biological Association of the UK, Plymouth, UK bDepartment of Earth Sciences, University College, London, UK Résumé – Gephyrocapsa oceanica est une espèce cosmopolite de coccolithophores appar- tenant à la famille des Noëlaerhabdaceae dans l’ordre des Isochrysidales. Exclusivement pélagique, G. oceanica est fréquemment retrouvée dans les océans modernes ainsi que dans les sédiments fossiles. Aussi, elle est apparentée à Emiliania huxleyi chez qui un cycle haplodiplobiontique a été décrit, avec un stade diploïde ou les cellules sont immobiles et ornées de coccolithes, qui alterne avec un stade haploïde ou les cellules sont mobiles et ornées d’écailles organiques. Alors que la cytologie et l’ultrastructure des autres membres des Noëlaerhabdaceae n’ont jamais été étudié, ces caractères peuvent être uniques au genre Emiliania ou communs à la famille. Dans cette étude, nous présentons pour la première fois l’ultrastructure des stades non-calcifiants mobiles et calcifiants immobile de G. oceanica. Nous n’avons pas retrouvé de différences ultrastructurales significatives entre ces deux morpho-espèces apparentées au niveau des stades diploïdes et haploïdes. Les similarités entre ces deux morpho-espèces démontrent une importante conservation des caractères cytologiques. Par ailleurs, nous avons discuté de la vraisemblance de ces résultats en rapport au contexte évolutif des Noelaerhabdaceae. Calcification / coccolithophores / Gephyrocapsa oceanica / cycle de vie / microscopie électronique à transmission / ultrastructure Abstract – Gephyrocapsa oceanica is a cosmopolitan bloom-forming coccolithophore species belonging to the haptophyte order Isochrysidales and family Noëlaerhabdaceae.