Extreme Diversity in Noncalcifying Haptophytes Explains a Major Pigment Paradox in Open Oceans
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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. -
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 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. -
Functional Group-Specific Traits Drive Phytoplankton Dynamics in the Oligotrophic Ocean
Functional group-specific traits drive phytoplankton dynamics in the oligotrophic ocean Harriet Alexandera,b, Mónica Roucoc, Sheean T. Haleyc, Samuel T. Wilsond, David M. Karld,1, and Sonya T. Dyhrmanc,1 aMIT–WHOI Joint Program in Oceanography/Applied Ocean Science and Engineering, Cambridge, MA 02139; bBiology Department, Woods Hole Oceanographic Institution, Woods Hole, MA 02543; cDepartment of Earth and Environmental Sciences, Lamont–Doherty Earth Observatory, Columbia University, Palisades, NY 10964; and dDaniel K. Inouye Center for Microbial Oceanography: Research and Education, Department of Oceanography, University of Hawaii, Honolulu, HI 96822 Contributed by David M. Karl, September 15, 2015 (sent for review June 29, 2015; reviewed by Kay D. Bidle and Adrian Marchetti) A diverse microbial assemblage in the ocean is responsible for Marine phytoplankton accounts for roughly half of global nearly half of global primary production. It has been hypothesized primary production (6). Although central to balancing global and experimentally demonstrated that nutrient loading can stimulate biogeochemical models of gross primary production (7), knowl- blooms of large eukaryotic phytoplankton in oligotrophic systems. edge of the biogeochemical drivers that govern the dynamics of Although central to balancing biogeochemical models, knowledge of these bloom-forming organisms in oligotrophic systems is lim- the metabolic traits that govern the dynamics of these bloom-forming ited. Nutrient environments are integral to the structuring of phytoplankton is limited. We used eukaryotic metatranscriptomic phytoplankton communities (8–10) and initiating blooms. Orig- techniques to identify the metabolic basis of functional group-specific inally thought to be a stable low-fluctuating habitat, long-term traits that may drive the shift between net heterotrophy and monitoring at Station ALOHA has demonstrated that within the autotrophy in the oligotrophic ocean. -
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. -
A Single Origin of the Peridinin- and Fucoxanthin- Containing Plastids in Dinoflagellates Through Tertiary Endosymbiosis
A single origin of the peridinin- and fucoxanthin- containing plastids in dinoflagellates through tertiary endosymbiosis Hwan Su Yoon, Jeremiah D. Hackett, and Debashish Bhattacharya† Department of Biological Sciences and Center for Comparative Genomics, University of Iowa, Iowa City, IA 85542-1324 Edited by Hewson Swift, University of Chicago, Chicago, IL, and approved June 26, 2002 (received for review April 18, 2002) The most widely distributed dinoflagellate plastid contains chlo- (as Gymnodinium breve), Karenia mikimotoi (as Gymnodinium rophyll c2 and peridinin as the major carotenoid. A second plastid mikimotoi), and Karlodinium micrum (as Gymnodinium galathea- type, found in taxa such as Karlodinium micrum and Karenia spp., num) (12) is surrounded by three membranes and contains ͞ ؉ ϩ Ј contains chlorophylls c1 c2 and 19 -hexanoyloxy-fucoxanthin chlorophylls c1 c2 and 19 -hexanoyloxy-fucoxanthin and or .(and͞or 19-butanoyloxy-fucoxanthin but lacks peridinin. Because 19Ј-butanoyloxy-fucoxanthin, but lacks peridinin (6, 13, 14 ؉ the presence of chlorophylls c1 c2 and fucoxanthin is typical of These taxa are believed to be monophyletic, and their plastid is haptophyte algae, the second plastid type is believed to have believed to have originated from a haptophyte alga through a originated from a haptophyte tertiary endosymbiosis in an ances- tertiary endosymbiosis in their common ancestor (15). Hapto- tral peridinin-containing dinoflagellate. This hypothesis has, how- phyte algae are primarily unicellular marine taxa that have ever, never been thoroughly tested in plastid trees that contain external body scales composed of calcium carbonate known as genes from both peridinin- and fucoxanthin-containing dinoflagel- coccoliths, two anterior flagella, and plastids surrounded by four lates. -
A Sea of Lilliputians
1 5/27/08 A Sea of Lilliputians by Marie-Pierre Aubry Department of Earth and Planetary Sciences Rutgers University 610 Taylor Road, Piscataway, New Jersey 08854-8066 and Department of Geology and Geophysics Woods Hole Oceanographic Institution Woods Hole Ma 02543 Fax: 732 445 3374, [email protected] Abstract Smaller size is generally seen as a negative response of organisms to stressful environmental conditions, associated with low diversity and species dominance. The mean size of the coccolithophorids decreased through the Neogene, leading to the prediction that their extant representatives are characterized by poor diversification and low specialization. The study of the (exo)coccospheres of selected taxa in the order Syracosphaerales negates this prediction, revealing that on the contrary some extant lineages are highly diversified and remarkably specialized. Whereas the general role of coccoliths remains indeterminate, this analysis suggests that some highly derived coccoliths may be modified for the collection of food particles, including picoplankton, thus implying that mixotrophy may characterize these lineages. In the extant coccolithophorids, species richness of genera is inversely correlated with the size of cells, definitive evidence that small size is part of a morphologic strategy rather than a sign of evolutionary failure. Because of their extreme minuteness, the extant nannoplankton can be well compared to Lilliputians, but the trend toward size decrease in Neogene lineages is not attributable to the Lilliput effect described by Urbanek (1993). 2 5/27/08 Key words: Extant coccolithophorids, Neogene, size, exococcospheres, functional morphology, mixotrophy. 1. Introduction Cope’s law, which in its broadest concept states that the size of organisms increases as lineages diversify, is generally regarded as prevalent among organisms despite a considerable debate as to its significance (e.g., Stanley, 1973, Gould, 1997, Jablonski, 1997, Alroy, 1998, Trammer, 2002). -
Nanoplankton Protists from the Western Mediterranean Sea. II. Cryptomonads (Cryptophyceae = Cryptomonadea)*
sm69n1047 4/3/05 20:30 Página 47 SCI. MAR., 69 (1): 47-74 SCIENTIA MARINA 2005 Nanoplankton protists from the western Mediterranean Sea. II. Cryptomonads (Cryptophyceae = Cryptomonadea)* GIANFRANCO NOVARINO Department of Zoology, The Natural History Museum, Cromwell Road, London SW7 5BD, U.K. E-mail: [email protected] SUMMARY: This paper is an electron microscopical account of cryptomonad flagellates (Cryptophyceae = Cryptomon- adea) in the plankton of the western Mediterranean Sea. Bottle samples collected during the spring-summer of 1998 in the Sea of Alboran and Barcelona coastal waters contained a total of eleven photosynthetic species: Chroomonas (sensu aucto- rum) sp., Cryptochloris sp., 3 species of Hemiselmis, 3 species of Plagioselmis including Plagioselmis nordica stat. nov/sp. nov., Rhinomonas reticulata (Lucas) Novarino, Teleaulax acuta (Butcher) Hill, and Teleaulax amphioxeia (Conrad) Hill. Identification was based largely on cell surface features, as revealed by scanning electron microscopy (SEM). Cells were either dispersed in the water-column or associated with suspended particulate matter (SPM). Plagioselmis prolonga was the most common species both in the water-column and in association with SPM, suggesting that it might be a key primary pro- ducer of carbon. Taxonomic keys are given based on SEM. Key words: Cryptomonadea, cryptomonads, Cryptophyceae, flagellates, nanoplankton, taxonomy, ultrastructure. RESUMEN: PROTISTAS NANOPLANCTÓNICOS DEL MAR MEDITERRANEO NOROCCIDENTAL II. CRYPTOMONADALES (CRYPTOPHY- CEAE = CRYPTOMONADEA). – Este estudio describe a los flagelados cryptomonadales (Cryptophyceae = Cryptomonadea) planctónicos del Mar Mediterraneo Noroccidental mediante microscopia electrónica. La muestras recogidas en botellas durante la primavera-verano de 1998 en el Mar de Alboran y en aguas costeras de Barcelona, contenian un total de 11 espe- cies fotosintéticas: Chroomonas (sensu auctorum) sp., Cryptochloris sp., 3 especies de Hemiselmis, 3 especies de Plagio- selmis incluyendo Plagioselmis nordica stat. -
Nuclear Genome Sequence of the Plastid-Lacking
Cenci et al. BMC Biology (2018) 16:137 https://doi.org/10.1186/s12915-018-0593-5 RESEARCH ARTICLE Open Access Nuclear genome sequence of the plastid- lacking cryptomonad Goniomonas avonlea provides insights into the evolution of secondary plastids Ugo Cenci1,2†, Shannon J. Sibbald1,2†, Bruce A. Curtis1,2, Ryoma Kamikawa3, Laura Eme1,2,11, Daniel Moog1,2,12, Bernard Henrissat4,5,6, Eric Maréchal7, Malika Chabi8, Christophe Djemiel8, Andrew J. Roger1,2,9, Eunsoo Kim10 and John M. Archibald1,2,9* Abstract Background: The evolution of photosynthesis has been a major driver in eukaryotic diversification. Eukaryotes have acquired plastids (chloroplasts) either directly via the engulfment and integration of a photosynthetic cyanobacterium (primary endosymbiosis) or indirectly by engulfing a photosynthetic eukaryote (secondary or tertiary endosymbiosis). The timing and frequency of secondary endosymbiosis during eukaryotic evolution is currently unclear but may be resolved in part by studying cryptomonads, a group of single-celled eukaryotes comprised of both photosynthetic and non-photosynthetic species. While cryptomonads such as Guillardia theta harbor a red algal-derived plastid of secondary endosymbiotic origin, members of the sister group Goniomonadea lack plastids. Here, we present the genome of Goniomonas avonlea—the first for any goniomonad—to address whether Goniomonadea are ancestrally non-photosynthetic or whether they lost a plastid secondarily. Results: We sequenced the nuclear and mitochondrial genomes of Goniomonas avonlea and carried out a comparative analysis of Go. avonlea, Gu. theta, and other cryptomonads. The Go. avonlea genome assembly is ~ 92 Mbp in size, with 33,470 predicted protein-coding genes. Interestingly, some metabolic pathways (e.g., fatty acid biosynthesis) predicted to occur in the plastid and periplastidal compartment of Gu. -
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. -
Calcareous Nannoplankton As a Tracer of the Marine Influence on the NW Coast of Portugal Over the Last 14 000 Years
J. Nannoplankton Res. 27 (2), 2005, pp.159-172 © 2005 International Nannoplankton Association 159 ISSN 1210-8049 Printed by Cambridge University Press, UK Calcareous nannoplankton as a tracer of the marine influence on the NW coast of Portugal over the last 14 000 years C. Guerreiro Centre of Geology, University of Lisbon, Building C6, 6.4.67, Campo Grande, 1749-016 Lisboa, Portugal; [email protected] M. Cachão Centre of Geology, University of Lisbon, Building C6, 6.4.67, Campo Grande, 1749-016 Lisboa, Portugal & Department of Geology, Faculty of Sciences, University of Lisbon, Building C6, 6.4.55, Campo Grande, 1749-016 Lisboa, Portugal T. Drago INIAP, IPIMAR, CRIPSUL, 8700-305 Olhão, Portugal Manuscript received 22nd March, 2005; revised manuscript accepted 19th August, 2005 Abstract A calcareous nannoplankton taphonomic and palaeoecological study was performed on cores from the Minho and Douro Estuaries (NW Portugal) and from the NW Portuguese middle continental shelf. Because certain nannoplankton species are taphonomically resistant to the highly energetic and aggressive conditions between the estuaries and the shelf, their sedimentary record acts as an oceanic tracer in such coastal domains. For the Late Quaternary, this allows interpretation of eustatic variation from the induced sequence of palaeoenvironmental changes. Palaeogeographically, the time-series pattern of nannofossil abundances in these coastal sediments is inter- preted as follows: (1) persistently high amounts of nannofossils (2x107 nannofossils/g) are related to marine envi- ronmental conditions, produced by post-glacial flooding of pre-existing valleys; (2) the gradual increase in intermit- tency of nannofossil abundances through time indicates a regressive trend, first due to recovery of the estuarine con- ditions, followed by a total absence of nannofossils, indicating evolution towards complete emersion either by flu- vial (Core CPF1) or barrier-beach sediments (Cores M1, M2, D1A and D1B). -
Continued Evolutionary Surprises Among Dinoflagellates
Commentary Continued evolutionary surprises among dinoflagellates Clifford W. Morden*†‡ and Alison R. Sherwood* *Department of Botany and †Hawaiian Evolutionary Biology Program, University of Hawaii, 3190 Maile Way, Honolulu, HI 96822 t is well established that chloroplasts in (also in green algae), fucoxanthin, chl c1 gene encoding the carbon assimilation Igreen and red algae are derived from a and c2 (also in stramenopiles and hapto- protein Rubisco, rbcL, has frequently primary endosymbiotic event between a phytes) and chl c1 and phycobilins (also in been used to examine deep phylogenetic cyanobacterium and a eukaryotic organ- cryptophytes), and are believed to be the relationships (12–14). However, recent ism Ϸ1 billion years ago (Fig. 1; refs. 1 and products of further endosymbioses with studies have demonstrated that there are 2). Although these two groups account for species from those groups (5–8). In this several problems associated with using many of the world’s photosynthetic spe- issue of PNAS, Yoon et al. (9) provide rbcL for this purpose. First, there appears cies, most other major taxonomic groups startling new evi- to have been ram- of photosynthetic organisms (strameno- dence that implicates pant horizontal piles—including diatoms, phaeophytes, dinoflagellate plas- gene transfer chrysophytes—and haptophytes) have tids containing fucox- Long-held theories suggested that among various al- plastids derived from a photosynthetic eu- anthin and chl c1 and primitive dinoflagellates were gal groups (14, c (derived from a 15). Reliance on karyote implying a secondary endosym- 2 heterotrophic and the addition biosis (1, 2). Still other groups, such as the haptophyte ancestor) such a gene to de- dinoflagellates, have more complicated as being ancestral to of a peridinin-containing plastid termine potential associations believed to be derived from those with peridinin.