Chapter 6 Marine Microbes Karleskint Turner Small Today

Chapter 6 Marine Microbes Karleskint Turner Small

Today: • You have your chapter 4 Quiz. • All phones must be in the basket. • When you are finished, please pick up one of the national geographic articles. • I will place questions on the board for you to answer. • Please answer the questions on a separate sheet of paper and turn them in.

Article Questions: • • • 1) What did the “fantastic hot spot for life” turn out to be? 2) What did they consist of? 3) How were they discovered? 4) What makes the dead sea saltier than other oceans? 5) What did preliminary samples of the craters show? 6) Why do you think there were different bacteria on the bottom of the rocks? • 7) Why are the bacteria found in the Dead sea special compared to other bacteria? • 8) What makes the Dead Sea difficult to study? How do they get around this obstacle?

Key Concepts • Microbial life in the sea is extremely diverse, including members of all three domains of life as well as viruses. • Marine virology is an emerging field of study, due to recognition of the critical role that viruses may play in population control of other microbes, in nutrient cycling, and in marine pathology.

Key Concepts • Photosynthetic and chemosynthetic bacteria and archaeons are important primary producers in marine ecosystems. • Heterotrophic bacteria, archaeons, and fungi play essential roles in recycling nutrients in the marine environment.

Key Concepts • Marine eukaryotic microbes are primary producers, decomposers, and consumers, and some contribute significantly to the accumulation of deep-sea sediments. • Populations of several kinds of photosynthetic marine microbes may form harmful blooms that affect other marine and maritime organisms directly and indirectly.

Marine Viruses • Virology—the study of viruses • Viruses are diverse and are more abundant than any other organism in the sea • Have significance for marine food webs, population biology and diseases of marine organisms • Viruses of marine eukaryotic hosts first reported in the 1970 s • Reliable counts of marine viruses made in the 1980 s

Viral Characteristics • Most authorities do not consider them to be alive • Viruses consist of bits of DNA or RNA surrounded by protein • Have no metabolism, and rely entirely on host organism for energy, material and organelles to reproduce themselves • Viral replication must occur within a host cell • Origin of viruses: two hypotheses – highly reduced prokaryotic parasites – renegade genes • Viruses infect all groups of living organisms, but may be specialized

Viral Characteristics • Viral structure – virus particle is called a virion when outside the host cell – virion composed of a nucleic acid core surrounded by a coat of protein called a capsid (together called a nucleocapsid) – may have a protective envelope, a membrane derived from the host’s nuclear or cell membrane

Viral Characteristics • Viral structure (con’t) – viral shapes: • icosahedral viruses—capsid with 20 triangular faces composed of protein subunits • helical viruses—protein subunits of the capsid spiral around the central core of nucleic acid • binal viruses—those with icosahedral heads and helical tails – some virions have filaments and other parts used to attach to and infect the host cell

Viral Characteristics • Viral life cycles – lytic cycle—a rapid cycle of infection, replication of viral nucleic acids and proteins, assembly of virions, and release of virions by lysis (rupture) of the cell – lysogenic cycle—the viral nucleic acid is inserted into the host genome and may reside there through multiple cell divisions before becoming lytic

Lytic Cycle Infection Replication Lysis Lysogenic Cycle Stepped Art Fig. 6 -3, p. 128

Biodiversity and Distribution of Marine Viruses • 10 times more abundant than marine prokaryotes, may reach 1010 virons per liter of seawater, 1013 per kilogram of sediment • Estimated 100 to 10, 000 genotypes • Most planktonic viruses are icosahdral or binal bacteriophages (“bacteria eaters”) with lytic life cycles • Sediment viruses are typically helical and lysogenic

Ecology of Marine Viruses • Viruses kill host cells, and thus control populations of bacteria and other microbes in plankton communities • Viruses also responsible for chronic infection and mass mortality of populations of marine animals • Bacterial lysis can alter biogeochemical cycles and planktonic food webs • Viral populations are probably controlled by several biotic and abiotic factors – e. g. alteration by light, adsorption onto suspended particles, ingestion by microbes, failure to attach to appropriate host cell

Marine Bacteria • General characteristics – simple, prokaryotic organization: no nuclei or membrane-bound organelles, few genes, nonliving cell wall – reproduce asexually by binary fission – many shapes and sizes • bacillus—rod shape • coccus—spherical shape

Aerobic respiration Oxygen CONSUMERS Zooplankton Animals Aerobic respiration Consumed by Die DECOMPOSERS PRIMARY PRODUCERS Photosynthesizers Cyanobacteria Phytoplankton Multicellular algae Plants Chemosynthetic bacteria Consumed by Wastes Die Aerobic bacteria and fungi Consumed by Anaerobic bacteria Aerobic metabolism Fermentation Nutrients released Nitrogen Sulfur Phosphorus Carbon dioxide Stepped Art Fig. 6 -6, p. 131

Nutritional Types • Cyanobacteria (blue-green bacteria) – photosynthetic bacteria which are found in environments high in dissolved oxygen, and produce free oxygen – store excess photosynthetic products as cyanophycean starch and oils – primary photosynthetic pigments are chlorophyll a and chlorophyll b – accessory pigments include carotenoids and phycobilins

Light energy Carbon dioxide (CO 2) Water (H 2 O) Carbohydrates (CH 2 O)x Oxygen (O 2) Carbohydrates (CH 2 O)x Sulfate (SO 42–) (a) Cyanobacteria – Free oxygen produced Light energy Carbon dioxide (CO 2) Hydrogen sulfide (H 2 S) (b) Purple and green bacteria – No free oxygen produced Stepped Art Fig. 6 -8, p. 132

Nutritional Types (Cyanobacteria) • Cyanobacteria (con’t) – chromatic adaptation—response of pigment composition to the quality of light in the sea – may exist as single cells or form dense mats held together by mucilage • form associates called stromatolites—a coral-like mound of microbes that trap sediment and precipitate minerals in shallow tropical seas

Nutritional Types • Other photosynthetic bacteria – anaerobic green and purple sulfur and nonsulfur bacteria do not produce oxygen – the primary photosynthetic pigments are bacteriochlorophylls – sulfur bacteria are obligate anaerobes (tolerating no oxygen) – non-sulfur bacteria are facultative anaerobes (respiring when in low oxygen or in the dark and photosynthesizing anaerobically when in the presence of light)

Nutritional Types • Chemosynthetic bacteria – use energy derived from chemical reactions that involve substances such as ammonium ion, sulfides and elemental sulfur, nitrites, hydrogen, and ferrous ion – chemosynthesis is less efficient than photosynthesis, so rates of cell growth and division are slower – found around hydrothermal vents and some shallower habitats where needed materials are available in abundance

Chemosynthetic bacteria (in animal tissues, in water, and on rocks) Carbon dioxide (CO 2) Produce Water (H 2 O) Carbohydrates Hydrogen sulfide (H 2 S) Animal community Carbon dioxide (CO 2) Hydrogen sulfide (H 2 S) Elemental sulfur (S) Carbon dioxide (CO 2) Stepped Art Magma (molten rock) Fig. 6 -10, p. 134

Nutritional Types • Heterotrophic bacteria – decomposers that obtain energy and materials from organic matter in their surroundings – return many chemicals to the marine environment through respiration and fermentation – populate the surface of organic particles suspended in the water by secreting mucilage (glue-like substance)

Nutritional Types (Heterotrophic Bacteria) • Heterotrophic bacteria – association of heterotrophic bacteria with particles in the water column aids with: • consolidation: adjacent particles adhere • lithification: formation of mineral cement between particles • sedimentation: settling of particles – marine snow: large, cobweb-like drifting structures formed by mucus secreted by many kinds of plankton, where particles may accumulate

Nitrogen Fixation and Nitrification • Nitrogen fixation: process that converts molecular nitrogen dissolved in seawater to ammonium ion – major process that adds new usable nitrogen to the sea – only some cyanobacteria and a few archaeons with nitrogenase (enzyme) are capable of fixing nitrogen

Nitrogen Fixation and Nitrification • Nitrification: process of bacterial conversion of ammonium (NH 4+) to nitrite (NO 2 -) and nitrate (NO 3 -) ions – bacterial nitrification converts ammonium into a form of nitrogen usable by other primary producers (autotrophs)

NITRIFICATION NITROGEN FIXATION Dissolved nitrogen (N 2) Animal wastes recycled by microorganisms Nitrogen-fixing bacteria, cyanobacteria Ammonia (NH 3) +Hydrogen (H 2) Ammonium (NH 4+) 2 N Bacteria +Oxygen (O 2) +Hydrogen (H 2) Nitrite (NO 2–) Ammonia (NH 3) Bacteria +Oxygen (O 2) Nitrate (NO 3–) Microorganisms Marine plants Phytoplankton Algae Stepped Art Fig. 6 -11, p. 135

Symbiotic Bacteria • Many bacteria have evolved symbiotic relationships with a variety of marine organisms • Endosymbiotic theory – mitochondria, plastids & hydrogenosomes evolved as symbionts within other cells • Chemosynthetic bacteria live within tube worms and clams • Some deep-sea or nocturnal animals host helpful bioluminescent bacteria – photophores – embedded in the ink sacs of squid

Archaea • General characteristics – small (0. 1 to 15 micrometers) – prokaryotic – adapted to extreme environmental conditions: high and low temperatures, high salinities, low p. H, and high pressure – formerly considered bacteria – differences from bacteria • cell walls lack special sugar-amino acid compounds in bacterial cell walls • cell membranes contain different lipids, which help stabilize them under extreme conditions

Archaea • Nutritional Types – archaea includes photosynthesizers, chemosynthesizers and heterotrophs – most are methanogens: anaerobic organisms that metabolize organic matter for energy, producing methane as a waste product – halobacteria (photosynthetic), thrive at high salinities, trap light using bacteriorhodopsins, purple proteins

Archaea • Hyperthermophiles – organisms that can survive at temperatures exceeding 100 o C, such as near deep-sea vents – Potential for biomedical and industrial application

Eukarya • Eukarya includes all organisms with eukaryotic cells • Examples: – plants – animals – fungi – algae – single-celled animal-like protozoa

Fungi • History of marine mycology – marine fungi first discovered in 1849 – marine fungi’s ecological role is difficult to evaluate; biomass needs to be quantified – important in marine ecosystems as decomposers, prey, pathogens and symbionts

Fungi • General features of fungi – eukaryotes with cell walls of chitin – many are unicellular yeasts – filamentous fungi grow into long, multi-cellular filaments called hyphae that can branch to produce a tangled mass called a mycelium – heterotrohic decomposers that recycle organic material • can digest lignin (major component of wood)

Fungi • General features of fungi (con’t) – store energy as glycogen – kingdom Fungi is divided into 4 phyla: • • Chytridiomycota (motile cells) Zygomycota (e. g. black bread mold) Basidiomycota (club fungi, e. g. mushrooms) Ascomycota (sac fungi) – in the sea, ascomycotes are the most diverse and abundant fungi

Fungi • Ecology and physiology of marine fungi – can be either obligately marine, requiring ocean or brakish water or facultatively marine (primarily of terrestrial or fresh water origin) – salinity is toxic to fungi, so they must devote energy to removing sodium – most marine fungi live on wood from land – some live on grass in salt marshes – others live on algae, mangroves or sand – fungi decompose the chitinous remains of dead crustaceans in open sea plankton communities

Reproduction of Marine Fungi • Marine yeasts reproduce asexually by budding—mitosis that produces daughter cells of unequal size • Filamentous marine fungi reproduce asexually by production of conidiospores on the tips of hyphae • Filamentous marine ascomycotes can reproduce sexually by forming a fruiting body called an ascocarp, a structure which produces ascospores

Maritime Lichens • Lichens: mutualistic associations between a fungus and an alga – fungi are usually ascomycotes – algae are usually green or blue-green bacteria • The fungus provides attachment, general structure, minerals, moisture • The alga produces organic matter through photosynthesis

Stramenophiles • A diverse group of eukaryotic organisms unified by the nature of their cells’ 2 flagella • The special flagella – 1 flagellum is a simple form, usually with a light-sensing body at the base; senses light – 2 nd bears many mastigonemes (hair-like filaments) with a thickened base and a branching tip along the shaft; used for swimming

Stramenophiles • Heterokont: refers to the different form of the 2 flagella • Ochrophytes: photosynthetic type that are usually golden brown – e. g. diatoms, silicoflagellates and brown algae

Diatoms • Extremely diverse and distinct members of marine phytoplankton • Diatom structure – frustule—a two-part, box-shaped organic cell wall impregnated with silica – valve—one half of a frustule; 1 valve is larger and fits over the other like a box lid – 2 basic diatom shapes: • radially symmetrical valves (generally planktonic) • bilaterally symmetrical valves (generally benthic)

Diatoms • Locomotion in diatoms – some benthic diatoms move slowly by mucilage secretion from pores and grooves • Reproduction in diatoms – asexual reproduction by fission • each daughter cell gets 1 valve, and has to grow a 2 nd, smaller one to complete frustule • auxospore—daughter cell which casts off the small valve, increases in size, and secretes a new frustule of normal size (occurs when cell size reaches 50% of maximum)

Asexual Reproduction Sexual Reproduction New cell Frustule formation Growth of the cell (auxospore) Zygote Gamete from another Mitosis Gametes formed Cells’ division continues until cells become too small to divide Gametes released Stepped Art Fig. 6 -19, p. 144

Diatoms • Diatomaceous sediments – frustules of dead diatoms sink and collect on the seafloor to form siliceous oozes – accumulations form sedimentary rock – these deposits, called diatomaceous earth, are mined for use as filtering material, a mild abrasive, and for soundproofing and insulation products – nutrient reserves, stored as lipids, accumulate in siliceous oozes accounting for most of the worlds petroleum reserves

Other Ochrophytes • Silicoflagellates – abundant in cold marine waters – basket-shaped external skeletons of silica which the cell wraps around – cell wraps around skeleton which appears internal

Other Ochrophytes • Pelagophyceans – e. g. bloom-forming alga Aureococcus anophagefferens (non-toxic, coastal) responsible for “brown tides” – can block light from sea grasses or clog filterfeeding structures of molluscs

Labyrinthomorphs • Spindle-shaped, mucous secreting osmotrophic cells • Labyrinthulids – e. g. Labyrinthula zosterae, causes devastating eelgrass wasting disease • Thraustochytrids – planktonic and benthic decomposers – some are pathogens of shellfish – used to produce dietary supplements: oils extracted from some species are high in polyunsaturated omega 3 fatty acid docosahexaenoic acid (DHA)

Haptophytes • Photosynthetic organisms with 2 simple flagella both used for locomotion • Have haptonema: a unique structure arising from the cell surface between the 2 flagella, captures food • Most are coccolithophores with a surface coating of disc-shaped scales (coliths) of calcium carbonate – remains form calcereous oozes

Haptophytes • Account for up to 40% of carbonate production in modern seas • High reflectance of chalky coccolithophores and their production of dimethyl sulfide may have impact on global climate change

Alveolates • Recent re-grouping of several kinds of marine microbes • Have membranous sacs (alveoli) beneath their cell membranes – pellicle: term for the cell surface if the combination of cell membrane and alveoli is complex (distinct from cell wall) • Examples: – dinoflagellates – ciliates – apicomplexans (strictly parasitic)

Alveolates • Dinoflagellates – globular, unicellular (sometimes colonial) with 2 flagella – dinosporin: a unique chemical associated with the cellulose plates within the alveoli of dinoflagellates – Most are planktonic, some are benthic and others parasitic, also can be bioluminescent – Bioluminescent Bay, Puerto Rico

Alveolates (Dinoflagellates) • Dinoflagellate structure – heterokont flagella – simple flagellum encircles the cell in the cingulum (a horizontal groove) and produces a spinning motion – longer flagellum with hair-like filaments trails down the sulcus (a longitudinal groove) and imparts most of the forward motion to the cell – unarmored dinoflagellates have few or no cellulose plates in the pellicle; armored dinoflagellates have multiple layers of them – number, size and shapes of plates are used to identify different species

Alveolates (Dinoflagellates) • Dinoflagellate nutrition – photosynthetic ones have chlorophylls a and c, beta-carotene and peridinin (a xanthophyll which imparts a golden-brown color) – mixotrophic photosynthetic ones supplement photosynthesis by osmotrophy (absorbing nutrients) or phagotrophy (engulfing nutrients) • Reproduction in dinoflagellates – asexual reproduction by fission – sexual reproduction by fusion and meiosis – often have dormant stages (cyst formation)

Alveolates (Dinoflagellates) • Ecological roles of dinoflagellates – major component of phytoplankton – some are parasites of copepods (crustaceans) – zooxanthellae: species lacking flagella which are symbionts of jellyfish, corals and molluscs – photosynthetic zooxanthellae provide food for hosts – hosts provide carbon dioxide, other nutrients, and shelter

Alveolates (Dinoflagellates) • Harmful Algal Blooms (HABs) – occur when photosynthetic dinoflagellates undergo a population explosion – colors the water red, orange or brown – dinoflagellates that cause HABs produce toxins • paralytic shellfish poisoning (PSP) occurs in humans who consume shellfish contaminated with these toxins • toxins cannot be destroyed by cooking – oxygen content of the water may be reduced to deadly levels as bacteria decompose animals killed by dinoflagellate toxins

Alveolates • Ciliates – protozoans that bear cilia for locomotion and for gathering food • membranelles—tufts or long rows of fused adjacent cilia • cytostome—an organelle serving as a permanent site for phagocytosis of food – planktonic and benthic – major links in marine food chains – form symbiotic and parasitic relationships – reproduce asexually by binary fission and sexually by conjugation (nuclei transfer)

Alveolates (Ciliates) • Types of marine ciliates – scuticociliates (have a dense and uniform distribution of cilia on their body) – oligotrichs (have few cilia) – tintinnids (usually lack body cilia and secrete an organic, loosely fitting shell, the lorica) • Ecological roles of marine ciliates – most are heterotrophs; some harbor autotrophic symbionts or chloroplasts – link hetero- and autotrophic blue-green bacteria to higher levels in the food chain

Choanoflagellates • Phylum of marine and freshwater flagellated cells that are more closely related to animals than any other group of one-celled microbes • Unicellular or colonial – colonies may be stalked or embedded in a gelatinous mass – cell often surrounded by a lorica of siliceous rods; flagellum is surrounded by a funnel-shaped collar of microvilli • Highly efficient consumers of bacteria

Amoeboid Protozoans • All have an organelle called a pseudopod—an extension of the cell surface that can change shape and is used for locomotion (benthic species) and food capture (benthic and pelagic) • Are hererotrophs consuming bacteria and other small organisms • Most have a test—an externally secreted organic membrane often covered with foreign particles or strengthened by mineral secretions

Amoeboid Protozoans • Two major phyla: – foraminiferans (abundant, diverse) – actinopods, which include: • radiolarians (predominant type) • acantharians • heliozoans

Amoeboid Protozoans • Foraminiferans (forams) – have branched pseudopods that form reticulopods (elaborate, net-like structures) used to: • snare prey • crawl (benthic) • reduce sinking rate (pelagic) – consume bacteria and diatoms – some harbor symbiotic green and red algae and zooxanthellae

Amoeboid Protozoans (Foraminiferans) • Foraminiferan test – elaborate, multi-chambered tests of calcium carbonate – globigerina ooze: sediments of dead planktonic forams, largely Globigerina • Foraminiferans and zooxanthellae – zooxanthellae live symbiotically within the cytoplasm of many forams from nutrient-poor waters – photosynthetic zooxanthellae use foram waste products (e. g. CO 2, ammonia) as nutrients

Amoeboid Protozoans • Radiolarians – named for long, needle-like pseudopods • central nuclear region is surrounded by a capsule—an external organic membrane • pseudopods pass through pores in the capsule and form a region called the calymma • pseudopods capture food and slow sinking – radiolarian oozes form from the internal siliceous skeleton of dead radiolarians – live in the photic zone and capture phyto- and zooplankton, sometimes copepods – larger radiolarians prey on copepods and other planktonic crustaceans