Cyanobacterial Lineage with a Worldwide Distribution Hidden by a Dinoflagellate Host

Total Page:16

File Type:pdf, Size:1020Kb

Cyanobacterial Lineage with a Worldwide Distribution Hidden by a Dinoflagellate Host Single-cell genomics unveiled a cryptic cyanobacterial lineage with a worldwide distribution hidden by a dinoflagellate host Takuro Nakayamaa,1, Mami Nomurab,2, Yoshihito Takanoc, Goro Tanifujid, Kogiku Shibab, Kazuo Inabab, Yuji Inagakie, and Masakado Kawataa aGraduate School of Life Sciences, Tohoku University, Sendai 980-8578, Japan; bShimoda Marine Research Center, University of Tsukuba, Shimoda 415-0025, Japan; cFaculty of Science and Technology, Kochi University, Nankoku 783-8502, Japan; dDepartment of Zoology, National Museum of Nature and Science, Tsukuba 305-0005, Japan; and eCenter for Computational Sciences, University of Tsukuba, Tsukuba 305-8577, Japan Edited by David M. Karl, University of Hawaii at Manoa, Honolulu, HI, and approved May 24, 2019 (received for review February 13, 2019) Cyanobacteria are one of the most important contributors to revealed that this cyanobacterial lineage symbiotically interacts oceanic primary production and survive in a wide range of marine with a lineage of unicellular photosynthetic eukaryotes (14–17). habitats. Much effort has been made to understand their ecological This symbiosis is thought to trace back to at least the Late features, diversity, and evolution, based mainly on data from free- Cretaceous Period (18). Whole-genome sequencing of UCYN- living cyanobacterial species. In addition, symbiosis has emerged as A showed that the cyanobacterial lineage has greatly reduced an important lifestyle of oceanic microbes and increasing knowl- its metabolic capacities for photosynthesis and has been spe- edge of cyanobacteria in symbiotic relationships with unicellular cialized for nitrogen fixation, thus furthering current un- eukaryotes suggests their significance in understanding the global derstanding of marine cyanobacteria (16, 19). While detailed oceanic ecosystem. However, detailed characteristics of these genetic features of some symbiotic cyanobacteria have been cyanobacteria remain poorly described. To gain better insight into reported aside from UCYN-A (20–22), those of most cyano- marine cyanobacteria in symbiosis, we sequenced the genome of cyanobacteria collected from a cell of a pelagic dinoflagellate that bacterial symbionts remain unknown. These poorly understood ECOLOGY is known to host cyanobacterial symbionts within a specialized symbiotic species potentially have biodiversity, which is im- chamber. Phylogenetic analyses using the genome sequence revealed portant to an understanding of cyanobacteria as a whole. that the cyanobacterium represents an underdescribed lineage within Pelagic heterotrophic dinoflagellates of the genus Ornitho- an extensively studied, ecologically important group of marine cercus have long been known to host cyanobacteria as symbionts cyanobacteria. Metagenomic analyses demonstrated that this cyano- (Fig. 1). Ornithocercus species cells are surrounded by a cellulosic bacterial lineage is globally distributed and strictly coexists with its covering known as the thecal plate, and crown-shaped extensions host dinoflagellates, suggesting that the intimate symbiotic associa- tion allowed the cyanobacteria to escape from previous metagenomic Significance studies. Furthermore, a comparative analysis of the protein repertoire with related species indicated that the lineage has independently un- Cyanobacteria are an important component of marine micro- Prochloro- dergone reductive genome evolution to a similar extent as bial ecology, and thus their biodiversity has been extensively coccus , which has the most reduced genomes among free-living studied. Here, through whole-genome sequencing, we discov- cyanobacteria. Discovery of this cyanobacterial lineage, hidden by ered that a marine cyanobacterium in a symbiotic association its symbiotic lifestyle, provides crucial insights into the diversity, with a unicellular eukaryote (OmCyn) represents a previously ecology, and evolution of marine cyanobacteria and suggests the under-described lineage within an ecologically important cya- existence of other undiscovered cryptic cyanobacterial lineages. nobacterial group. Our metagenomic analyses showed that the cyanobacterium OmCyn thrives in global oceans, further sug- cyanobacteria | dinoflagellate | symbiosis | single-cell genomics | gesting the existence of other cryptic cyanobacterial lineages metagenomics that have been overlooked because of their symbiotic lifestyle. Via comparison with genomes of free-living relatives, the yanobacteria are one of the most successful groups of OmCyn genome was shown to have a reductive nature, which Coxygen-producing photoautotrophs occupying a broad range apparently resulted from intimate association with the host. of habitats on earth. Organisms in this group are highly ubiqui- Together, our results expand current understanding of the bi- tous in marine environments and play a vital role in oceanic ology of cyanobacteria and marine microbial ecology. biogeochemical cycles, with their metabolic abilities including photosynthesis and nitrogen fixation (1–3). To obtain a better Author contributions: T.N., M.N., Y.T., and Y.I. designed research; T.N., M.N., G.T., K.S., and K.I. performed research; T.N. analyzed data; and T.N., M.N., Y.T., G.T., K.S., K.I., Y.I., understanding of marine microbial ecology, the biodiversity and and M.K. wrote the paper. ecological features of marine cyanobacteria have been actively The authors declare no conflict of interest. explored (4–8). Previous studies based on environmental DNA and cultivated strains have revealed that marine cyanobacteria This article is a PNAS Direct Submission. display broad genetic diversity and have evolved by adapting to Published under the PNAS license. various ecological niches (9–11). Data deposition: The data reported in this paper are available from the DNA Data Bank of Japan (http://www.ddbj.nig.ac.jp/), NCBI GenBank database (https://www.ncbi.nlm.nih. Other than free-living species, which have been extensively gov/genbank), and the European Molecular Biology Laboratory (https://www.embl.de/) studied, cyanobacterial species have symbiotic relationships with DNA database under BioProject accession number PRJDB7787. various organisms (12, 13). Recent developments in DNA-sequencing 1To whom correspondence may be addressed. Email: [email protected]. technologies have revealed the genetic characteristics of one group 2Present address: Graduate School of Human and Environmental Studies, Kyoto Univer- of symbiotic cyanobacteria. Unicellular cyanobacteria group A sity, Kyoto 606-8501, Japan. (UCYN-A; also known as Candidatus Atelocyanobacterium tha- This article contains supporting information online at www.pnas.org/lookup/suppl/doi:10. lassa) is a recently recognized, ecologically important cyano- 1073/pnas.1902538116/-/DCSupplemental. bacterial group in the marine environment. Recent studies have www.pnas.org/cgi/doi/10.1073/pnas.1902538116 PNAS Latest Articles | 1of6 Downloaded by guest on September 26, 2021 of the thecal plate form an extracellular chamber per cell (SI phylogenetic relationship between OmCyn and the marine Appendix, Fig. S1). A number of coccoid cyanobacteria reside in picocyanobacteria (SI Appendix, Fig. S3). The OmCyn sequence the specialized chamber (Fig. 1 and SI Appendix, Fig. S1); these made a monophyletic clade along with previously reported se- extracellular symbionts are also called phaeosomes (12, 23). quences. Most of those were a part of diverse 16S rDNA se- Despite the existence of phaeosomes being first recorded over quences directly amplified from dinoflagellate cells with 100 y ago (23), there is no laboratory culture or any report of cyanobacterial symbionts that are akin to O. magnificus (24). successful cultivation of the symbiont and detailed characteristics Biodiversity within the picocyanobacterial clade has been ex- of the cyanobacteria surviving in these chambers remain poorly tensively studied, as these cyanobacterial species numerically understood. Here, we sequenced the genome of the cyanobacteria dominate global oceans (7, 25). However, we detected no strong isolated from the dinoflagellate Ornithocercus magnificus (Fig. 1) phylogenetic affinity between the clade of cyanobacterial se- using single-cell genomics technology. Analyses based on the ge- quences from dinoflagellates, including OmCyn, and previously nome sequence revealed that the cyanobacterium represents an explicitly described marine picocyanobacterial lineages (7) based underdescribed lineage of a cyanobacterial clade, of which bio- on traditional phylogenetic markers for this group—namely, 16S diversity has been extensively studied and which has independently rDNA (SI Appendix, Fig. S3) and the internal transcribed spacer undergone reductive genome evolution. Analyses using meta- (ITS; SI Appendix, Fig. S4). The two trees showed different genomic data from the Tara Oceans Expedition further suggest phylogenetic positions of the clade comprising the cyanobacterial worldwide distribution of this cyanobacterial lineage and the po- sequences from dinoflagellates: The ITS tree suggested the clade tential existence of other undiscovered symbiotic cyanobacterial is basal to a well-defined Synechococcus clade, known as Syn- lineages. echococcus subcluster 5.1 (7), while the 16S rDNA tree placed the clade as sister to one of the clades within Synechococcus Results and Discussion subcluster 5.1, named clade V. Nevertheless, since both back- Genome Sequence and Phylogenetic Analyses of Cyanobacteria bones of the two trees did not receive high
Recommended publications
  • Anoxygenic Photosynthesis in Photolithotrophic Sulfur Bacteria and Their Role in Detoxication of Hydrogen Sulfide
    antioxidants Review Anoxygenic Photosynthesis in Photolithotrophic Sulfur Bacteria and Their Role in Detoxication of Hydrogen Sulfide Ivan Kushkevych 1,* , Veronika Bosáková 1,2 , Monika Vítˇezová 1 and Simon K.-M. R. Rittmann 3,* 1 Department of Experimental Biology, Faculty of Science, Masaryk University, 62500 Brno, Czech Republic; [email protected] (V.B.); [email protected] (M.V.) 2 Department of Biology, Faculty of Medicine, Masaryk University, 62500 Brno, Czech Republic 3 Archaea Physiology & Biotechnology Group, Department of Functional and Evolutionary Ecology, Universität Wien, 1090 Vienna, Austria * Correspondence: [email protected] (I.K.); [email protected] (S.K.-M.R.R.); Tel.: +420-549-495-315 (I.K.); +431-427-776-513 (S.K.-M.R.R.) Abstract: Hydrogen sulfide is a toxic compound that can affect various groups of water microorgan- isms. Photolithotrophic sulfur bacteria including Chromatiaceae and Chlorobiaceae are able to convert inorganic substrate (hydrogen sulfide and carbon dioxide) into organic matter deriving energy from photosynthesis. This process takes place in the absence of molecular oxygen and is referred to as anoxygenic photosynthesis, in which exogenous electron donors are needed. These donors may be reduced sulfur compounds such as hydrogen sulfide. This paper deals with the description of this metabolic process, representatives of the above-mentioned families, and discusses the possibility using anoxygenic phototrophic microorganisms for the detoxification of toxic hydrogen sulfide. Moreover, their general characteristics, morphology, metabolism, and taxonomy are described as Citation: Kushkevych, I.; Bosáková, well as the conditions for isolation and cultivation of these microorganisms will be presented. V.; Vítˇezová,M.; Rittmann, S.K.-M.R.
    [Show full text]
  • Limits of Life on Earth Some Archaea and Bacteria
    Limits of life on Earth Thermophiles Temperatures up to ~55C are common, but T > 55C is Some archaea and bacteria (extremophiles) can live in associated usually with geothermal features (hot springs, environments that we would consider inhospitable to volcanic activity etc) life (heat, cold, acidity, high pressure etc) Thermophiles are organisms that can successfully live Distinguish between growth and survival: many organisms can survive intervals of harsh conditions but could not at high temperatures live permanently in such conditions (e.g. seeds, spores) Best studied extremophiles: may be relevant to the Interest: origin of life. Very hot environments tolerable for life do not seem to exist elsewhere in the Solar System • analogs for extraterrestrial environments • `extreme’ conditions may have been more common on the early Earth - origin of life? • some unusual environments (e.g. subterranean) are very widespread Extraterrestrial Life: Spring 2008 Extraterrestrial Life: Spring 2008 Grand Prismatic Spring, Yellowstone National Park Hydrothermal vents: high pressure in the deep ocean allows liquid water Colors on the edge of the at T >> 100C spring are caused by different colonies of thermophilic Vents emit superheated water (300C or cyanobacteria and algae more) that is rich in minerals Hottest water is lifeless, but `cooler’ ~50 species of such thermophiles - mostly archae with some margins support array of thermophiles: cyanobacteria and anaerobic photosynthetic bacteria oxidize sulphur, manganese, grow on methane + carbon monoxide etc… Sulfolobus: optimum T ~ 80C, minimum 60C, maximum 90C, also prefer a moderately acidic pH. Live by oxidizing sulfur Known examples can grow (i.e. multiply) at temperatures which is abundant near hot springs.
    [Show full text]
  • 182-188 Enhanced Chlorophyll a and Primary Production in the Northern
    Author version: Mar. Biol. Res., vol.8; 2012; 182-188 Enhanced chlorophyll a and primary production in the northern Arabian Sea during the spring intermonsoon due to green Noctiluca (N. scintillans) bloom N. V. Madhua,*, R. Jyothibabua, P. A. Maheswaranb, K. A. Jayaraja, C.T. Achuthankuttya aNational Institute of Oceanography, Regional Centre, Kochi -18, India bNaval Physical Oceanographic Laboratory, Kochi - 21, India Abstract The surface waters of the northeastern Arabian Sea sustained relatively high chlorophyll a (av. 0.81 ± 0.80 mgm-3) and primary production (av. 29.5 ± 23.6 mgC m-3d-1) during the early spring intermonsoon 2000. This was caused primarily by a thick patch of algal bloom spread over a vast area between 17° to 21°N and 66 to 70°E. Satellite images showed exceptionally high concentration of chlorophyll a in the bloom areas, representing the annually occurring ‘spring blooms’ during February-March. The causative organism of the bloom was the dinoflagellate, Noctiluca scintillans Macartney (synonym Noctiluca miliaris Suriray, Dinophyceae: Noctilucidea), symbiotically associated with an autotrophic prasinophyte Pedinomonas noctilucae. The symbiosis between N. scintillans and P. noctilucae is likely responsible for their explosive growth (av. 3 million cells L-1) over an extensive area making the northeastern Arabian Sea highly productive (av. 607 ± 338 mg Cm-3d-1) even during an oligotrophic period such as spring intermonsoon. Key words: - Chlorophyll a; Algal bloom; Noctiluca scintillans, Pedinomonas noctilucae; Spring intermonsoon *Email of the corresponding author - [email protected] 2 Introduction The Arabian Sea (AS hereafter) is one of the most productive regions in the Indian Ocean (Madhupratap et al., 1996), exhibiting a bimodal temperature cycles annually, with lows during winter (northeast monsoon - NEM) and summer (southwest monsoon - SWM) seasons.
    [Show full text]
  • Check List 15 (5): 951–963
    15 5 ANNOTATED LIST OF SPECIES Check List 15 (5): 951–963 https://doi.org/10.15560/15.5.951 Dinoflagellates in tropical estuarine waters from the Maraú River, Camamu Bay, northeastern Brazil Caio Ceza da Silva Nunes1, Sylvia Maria Moreira Susini-Ribeiro1, 2, Kaoli Pereira Cavalcante3 1 Mestrado em Sistemas Aquáticos Tropicais, Universidade Estadual de Santa Cruz, Rodovia Jorge Amado, km 16, Salobrinho, 45662090 Ilhéus, BA, Brazil. 2 Universidade Estadual de Santa Cruz, Rodovia Jorge Amado, km 16, Salobrinho, 45662090 Ilhéus, BA, Brazil. 3 Universidade Estadual Vale do Acaraú, Avenida da Universidade, 850, Campus da Betânia, Betânia, 62040370, Sobral, CE, Brazil. Corresponding author: Caio Ceza da Silva Nunes, [email protected] Abstract Dinoflagellates display great diversity in tropical regions and play an important role in the complex microbial food webs of marine and brackish environments. The goal of this study is to identify planktonic dinoflagellates and their distribution in the estuary of the Maraú River, Camamu Bay, state of Bahia, in a region with increasing use of shellfish farming. Samples were carried out monthly from August 2006 to July 2007 at four stations along the estuary. Plankton was sampled with a 20 μm mesh net. We identified 20 dinoflagellate species. The greatest species richness was ob- served in the genera Protoperidinium (five spp.), Tripos (four spp.), and Prorocentrum (three spp.). Based on literature, six species were classified as potentially harmful: Akashiwo sanguinea, Dinophysis caudata, Gonyaulax spinifera, Prorocentrum micans, Scrippsiella cf. acuminata, and Tripos furca. Protoperidinium venustum was recorded for the first time in coastal waters of Bahia. Keywords Brackish water, Dinophyta, distribution, potentially harmful species, taxonomy.
    [Show full text]
  • Genomics Reveals Alga-Associated Cyanobacteria Hiding in Plain Sight COMMENTARY John M
    COMMENTARY Genomics reveals alga-associated cyanobacteria hiding in plain sight COMMENTARY John M. Archibalda,b,1 Cyanobacteria occupy a special place in the pantheon of prokaryotic life. It is in the ancestors of these ubiquitous microbes that oxygenic photosynthesis first evolved more than 2 billion y ago (1), and it is from endosymbiotic cyanobacteria that the plastids (chloro- plasts) of plants and algae are derived (2). Modern-day cyanobacteria are diverse in form and function; they in- clude coccoid marine picoplankton such as Prochloro- coccus (3), freshwater biofilm-forming genera [e.g., Gloeomargarita (4)], and filamentous taxa capable of fix- ing nitrogen [e.g., Nostoc (5)]. In PNAS, Nakayama et al. (6) add an exciting chapter to the story of cyanobacterial diversity. The authors describe the genome sequence of a cyanobacterium living ectosymbiotically on an eye- catching dinoflagellate named Ornithocercus magnifi- cus. Their results provide insight into the nature of an enigmatic symbiotic relationship and reveal the exis- tence of a cryptic, globally distributed cyanobacterial lineage that has until now gone unappreciated. Ornithocercus is indeed magnificent, even by di- Fig. 1. Light micrograph of an Ornithocercus noflagellate standards. The surface of this heterotro- dinoflagellate. The ectosymbiotic OmCyn cyanobacteria phic marine protist is decorated with crown-shaped, are visible within an extracellular chamber on the cellulosic outcroppings that extend from the cell body “upper” crown of the cell. Image courtesy of Takuro Nakayama (Tohoku University, Sendai, Japan). in different directions (Fig. 1) (7). The “upper” crown forms an extracellular chamber in which autofluores- cent cyanobacteria reside, and microscopic evidence genome of the organism, which they dubbed “OmCyn.” suggests that the bacteria can be vertically transmitted In a preliminary phylogenetic analysis of the 16S ribo- from mother to daughter chambers during host cell somal RNA (rRNA) gene, OmCyn was found to branch division (8).
    [Show full text]
  • De Rijk, L?, Caers, A,, Van De Peer, Y. & De Wachter, R. 1998. Database
    BLANCHARD & HICKS-THE APICOMPLEXAN PLASTID 375 De Rijk, l?, Caers, A,, Van de Peer, Y. & De Wachter, R. 1998. Database gorad, L. & Vasil, I. K. (ed.), Cell Culture and Somatic Cell Genetics on the structure of large ribosomal subunit RNA. Nucl. Acids. Rex, of Plants, Vol7A: The molecular biology of plastids. Academic Press, 26: 183- 186. San Diego. p. 5-53. Deveraux, J., Haeberli, l? & Smithies, 0. 1984. A comprehensive set of Palmer, J. D. & Delwiche, C. E 1996. Second-hand chloroplasts and sequence analysis programs for the VAX. Nucl. Acids. Rex, 12:387-395. the case of the disappearing nucleus. Proc. Natl. Acad. Sci. USA, 93: Eaga, N. & Lang-Unnasch, N. 1995. Phylogeny of the large extrachro- 7432-7435. mosomal DNA of organisms in the phylum Apicomplexa. J. Euk. Popadic, A,, Rusch, D., Peterson, M., Rogers, B. T. & Kaufman, T. C. Microbiol,, 42:679-684. 1996. Origin of the arthropod mandible. Nature, 380:395. Fichera, M. E. & Roos, D. S. 1997. A plastid organelle as a drug target Preiser, l?, Williamson, D. H. & Wilson, R. J. M. 1995. Transfer-RNA in apicomplexan parasites. Nature, 390:407-409. genes transcribed from the plastid-like DNA of Plasmodium falci- Gardner, M. J., Williamson, D. H. & Wilson, R. J. M. 1991. A circular parum. Nucl. Acids Res., 23:4329-4336. DNA in malaria parasites encodes an RNA polymerase like that of Reith. M. & Munholland, J. 1993. A high-resolution gene map of the prokaryotes and chloroplasts. Mol. Biochem. Parasitiol., 44: 1 15-123. chloroplast genome of the red alga Porphyra purpurea. Plant Cell, Gardner, M.
    [Show full text]
  • PROTISTS Shore and the Waves Are Large, Often the Largest of a Storm Event, and with a Long Period
    (seas), and these waves can mobilize boulders. During this phase of the storm the rapid changes in current direction caused by these large, short-period waves generate high accelerative forces, and it is these forces that ultimately can move even large boulders. Traditionally, most rocky-intertidal ecological stud- ies have been conducted on rocky platforms where the substrate is composed of stable basement rock. Projec- tiles tend to be uncommon in these types of habitats, and damage from projectiles is usually light. Perhaps for this reason the role of projectiles in intertidal ecology has received little attention. Boulder-fi eld intertidal zones are as common as, if not more common than, rock plat- forms. In boulder fi elds, projectiles are abundant, and the evidence of damage due to projectiles is obvious. Here projectiles may be one of the most important defi ning physical forces in the habitat. SEE ALSO THE FOLLOWING ARTICLES Geology, Coastal / Habitat Alteration / Hydrodynamic Forces / Wave Exposure FURTHER READING Carstens. T. 1968. Wave forces on boundaries and submerged bodies. Sarsia FIGURE 6 The intertidal zone on the north side of Cape Blanco, 34: 37–60. Oregon. The large, smooth boulders are made of serpentine, while Dayton, P. K. 1971. Competition, disturbance, and community organi- the surrounding rock from which the intertidal platform is formed zation: the provision and subsequent utilization of space in a rocky is sandstone. The smooth boulders are from a source outside the intertidal community. Ecological Monographs 45: 137–159. intertidal zone and were carried into the intertidal zone by waves. Levin, S. A., and R.
    [Show full text]
  • Mixotrophic Protists Among Marine Ciliates and Dinoflagellates: Distribution, Physiology and Ecology
    FACULTY OF SCIENCE UNIVERSITY OF COPENHAGEN PhD thesis Woraporn Tarangkoon Mixotrophic Protists among Marine Ciliates and Dinoflagellates: Distribution, Physiology and Ecology Academic advisor: Associate Professor Per Juel Hansen Submitted: 29/04/10 Contents List of publications 3 Preface 4 Summary 6 Sammenfating (Danish summary) 8 สรุป (Thai summary) 10 The sections and objectives of the thesis 12 Introduction 14 1) Mixotrophy among marine planktonic protists 14 1.1) The role of light, food concentration and nutrients for 17 the growth of marine mixotrophic planktonic protists 1.2) Importance of marine mixotrophic protists in the 20 planktonic food web 2) Marine symbiont-bearing dinoflagellates 24 2.1) Occurrence of symbionts in the order Dinophysiales 24 2.2) The spatial distribution of symbiont-bearing dinoflagellates in 27 marine waters 2.3) The role of symbionts and phagotrophy in dinoflagellates with symbionts 28 3) Symbiosis and mixotrophy in the marine ciliate genus Mesodinium 30 3.1) Occurrence of symbiosis in Mesodinium spp. 30 3.2) The distribution of marine Mesodinium spp. 30 3.3) The role of symbionts and phagotrophy in marine Mesodinium rubrum 33 and Mesodinium pulex Conclusion and future perspectives 36 References 38 Paper I Paper II Paper III Appendix-Paper IV Appendix-I Lists of publications The thesis consists of the following papers, referred to in the synthesis by their roman numerals. Co-author statements are attached to the thesis (Appendix-I). Paper I Tarangkoon W, Hansen G Hansen PJ (2010) Spatial distribution of symbiont-bearing dinoflagellates in the Indian Ocean in relation to oceanographic regimes. Aquat Microb Ecol 58:197-213.
    [Show full text]
  • 21 Pathogens of Harmful Microalgae
    21 Pathogens of Harmful Microalgae RS. Salomon and I. Imai 2L1 Introduction Pathogens are any organisms that cause disease to other living organisms. Parasitism is an interspecific interaction where one species (the parasite) spends the whole or part of its life on or inside cells and tissues of another living organism (the host), from where it derives most of its food. Parasites that cause disease to their hosts are, by definition, pathogens. Although infection of metazoans by other metazoans and protists are the more fre quently studied, there are interactions where both host and parasite are sin gle-celled organisms. Here we describe such interactions involving microal gae as hosts. The aim of this chapter is to review the current status of research on pathogens of harmful microalgae and present future perspec tives within the field. Pathogens with the ability to impair and kill micro algae include viruses, bacteria, fungi and a number of protists (see reviews by Elbrachter and Schnepf 1998; Brussaard 2004; Park et al. 2004; Mayali and Azam 2004; Ibelings et al. 2004). Valuable information exists from non-harm ful microalgal hosts, and these studies will be referred to throughout the text. Nevertheless, emphasis is given to cases where hosts are recognizable harmful microalgae. 21.2 Viruses Viruses and virus-like particles (VLPs) have been found in more than 50 species of eukaryotic microalgae, and several of them have been isolated in laboratory cultures (Brussaard 2004; Nagasaki et al. 2005). These viruses are diverse both in size and genome type, and some of them infect harmful algal bloom (HAB)-causing species (Table 21.1).
    [Show full text]
  • Algae and Cyanobacteria in Coastal and Estuarine Waters
    CHAPTER 7 Algae and cyanobacteria in coastal and estuarine waters n coastal and estuarine waters, algae range from single-celled forms to the seaweeds. ICyanobacteria are organisms with some characteristics of bacteria and some of algae. They are similar in size to the unicellular algae and, unlike other bacteria, contain blue-green or green pigments and are able to perform photosynthesis; thus, they are also termed blue-green algae. Algal blooms in the sea have occurred throughout recorded history but have been increasing during recent decades (Anderson, 1989; Smayda, 1989a; Hallegraeff, 1993). In several areas (e.g., the Baltic and North seas, the Adriatic Sea, Japanese coastal waters and the Gulf of Mexico), algal blooms are a recurring phe- nomenon. The increased frequency of occurrence has accompanied nutrient enrich- ment of coastal waters on a global scale (Smayda, 1989b). Blooms of non-toxic phytoplankton species and mass occurrences of macro-algae can affect the amenity value of recreational waters due to reduced transparency, dis- coloured water and scum formation. Furthermore, bloom degradation can be accom- panied by unpleasant odours, resulting in aesthetic problems (see chapter 9). Several human diseases have been reported to be associated with many toxic species of dinoflagellates, diatoms, nanoflagellates and cyanobacteria that occur in the marine environment (CDC, 1997). The effects of these algae on humans are due to some of their constituents, principally algal toxins. Marine algal toxins become a problem primarily because they may concentrate in shellfish and fish that are subsequently eaten by humans (CDR, 1991; Lehane, 2000), causing syndromes known as para- lytic shellfish poisoning (PSP), diarrhetic shellfish poisoning (DSP), amnesic shellfish poisoning (ASP), neurotoxic shellfish poisoning (NSP) and ciguatera fish poisoning (CFP).
    [Show full text]
  • The Unicellular and Colonial Organisms Prokaryotic And
    The Unicellular and Colonial Organisms Prokaryotic and Eukaryotic Cells As you know, the building blocks of life are cells. Prokaryotic cells are those cells that do NOT have a nucleus. They mostly include bacteria and archaea. These cells do not have membrane-bound organelles. Eukaryotic cells are those that have a true nucleus. That would include plant, animal, algae, and fungal cells. As you can see, to the left, eukaryotic cells are typically larger than prokaryotic cells. Today in lab, we will look at examples of both prokaryotic and eukaryotic unicellular organisms that are commonly found in pond water. When examining pond water under a microscope… The unpigmented, moving microbes will usually be protozoans. Greenish or golden-brown organisms will typically be algae. Microorganisms that are blue-green will be cyanobacteria. As you can see below, living things are divided into 3 domains based upon shared characteristics. Domain Eukarya is further divided into 4 Kingdoms. Domain Kingdom Cell type Organization Nutrition Organisms Absorb, Unicellular-small; Prokaryotic Photsyn., Archaeacteria Archaea Archaebacteria Lacking peptidoglycan Chemosyn. Unicellular-small; Absorb, Bacteria, Prokaryotic Peptidoglycan in cell Photsyn., Bacteria Eubacteria Cyanobacteria wall Chemosyn. Ingestion, Eukaryotic Unicellular or colonial Protozoa, Algae Protista Photosynthesis Fungi, yeast, Fungi Eukaryotic Multicellular Absorption Eukarya molds Plantae Eukaryotic Multicellular Photosynthesis Plants Animalia Eukaryotic Multicellular Ingestion Animals Prokaryotic Organisms – the archaea, non-photosynthetic bacteria, and cyanobacteria Archaea - Microorganisms that resemble bacteria, but are different from them in certain aspects. Archaea cell walls do not include the macromolecule peptidoglycan, which is always found in the cell walls of bacteria. Archaea usually live in extreme, often very hot or salty environments, such as hot mineral springs or deep-sea hydrothermal vents.
    [Show full text]
  • About Cyanobacteria BACKGROUND Cyanobacteria Are Single-Celled Organisms That Live in Fresh, Brackish, and Marine Water
    About Cyanobacteria BACKGROUND Cyanobacteria are single-celled organisms that live in fresh, brackish, and marine water. They use sunlight to make their own food. In warm, nutrient-rich environments, microscopic cyanobacteria can grow quickly, creating blooms that spread across the water’s surface and may become visible. Because of the color, texture, and location of these blooms, the common name for cyanobacteria is blue-green algae. However, cyanobacteria are related more closely to bacteria than to algae. Cyanobacteria are found worldwide, from Brazil to China, Australia to the United States. In warmer climates, these organisms can grow year-round. Scientists have called cyanobacteria the origin of plants, and have credited cyanobacteria with providing nitrogen fertilizer for rice and beans. But blooms of cyanobacteria are not always helpful. When these blooms become harmful to the environment, animals, and humans, scientists call them cyanobacterial harmful algal blooms (CyanoHABs). Freshwater CyanoHABs can use up the oxygen and block the sunlight that other organisms need to live. They also can produce powerful toxins that affect the brain and liver of animals and humans. Because of concerns about CyanoHABs, which can grow in drinking water and recreational water, the U.S. Environmental Protection Agency (EPA) has added cyanobacteria to its Drinking Water Contaminant Candidate List. This list identifies organisms and toxins that EPA considers to be priorities for investigation. ASSESSING THE IMPACT ON PUBLIC HEALTH Reports of poisonings associated with CyanoHABs date back to the late 1800s. Anecdotal evidence and data from laboratory animal research suggest that cyanobacterial toxins can cause a range of adverse human health effects, yet few studies have explored the links between CyanoHABs and human health.
    [Show full text]