Transcript Document
Opener The Microbial World Radiolarian shells 1 Microorganisms The most abundant forms of marine life. Represented in all three biological domains. Bacteria, Archaea, Eukarya Smallest and structurally simplest Primary producers Organisms that manufacture organic matter from CO2, usually by photosynthesis. 2 Fig. 5.1 3 Viruses Not made up of a cell Short chain of genetic material (nucleic acid) Relatively few genes Protected by capsid, outer protein coat Parasites 20 to 200 nm in size 4 Retroviruses Genetic information stored as RNA Responsible for human diseases HIV/AIDS leukemia 5 Lytic and Lysogenic viruses 6 Lysogenic viruses Reproduce by inducing their nucleic acid to become part of the genome of the host cell. Genome then directs the production of new viruses. LYTIC VIRUSES infects cells,causing them to burst 7 Bacteriophages Viruses that specifically target and destroy bacteria. Common in marine environments 8 Viruses and algae Viruses infect phytoplankton Bursting releases DOM (dissolved organic matter) DOM not used by most organisms DOM is taken up by bacteria and microbes • in turn, they’re eaten by zooplankton • in turn, they’re eaten by larger zooplankton Bursting releases essential nutrients • used by primary producers 9 Viral diseases Shellfish Fishes Sea turtles Marine mammals Humans oysters and mussels filter sewagecontaminated water. 10 Prokaryotes Smallest, structurally simplest living organisms oldest forms of life on earth most chemical processes evolved first in prokaryotes 11 Prokaryotic cells protective cell wall plasma membrane immediately inside cell wall lack a nucleus lack most membrane-bound organelles circular DNA 12 Fig. 5.2 Cyclobacterium marinarus, a ringforming marine bacterium 13 Fig. 5.3 The largest known bacterium, Thiomargarita namibiensis, 0.75mm 14 2 prokaryotic domains Bacteria and Archaea Differences in: • chemistry of cell walls • cell membranes • cellular machinery that makes proteins 15 Bacteria Many shapes: spheres, rods, spirals, rings Rigid and strong cell walls Stiff or slimy covering protection or attachment Very small from about 0.1 to about 600 µm from just bigger than a virus, to nearly visible 16 Ubiquitous bacteria Bacteria are ubiquitous, that is, they occur EVERYWHERE in the ocean. all surfaces water column most abundant life form in the open ocean 300 m deep in buried sediment 17 Bacteria as Decomposers Grow in detritus (dead organic matter) break down waste products release nutrients back into the environment 18 Cyanobacteria formerly called blue-green algae photosynthetic pigments chlorophyll a (like eukaryotes) phycocyanin (blue) phycoerythrin (red) 19 cyanobacteria, continued role in accumulating O2 in the early atmosphere fossil stromatolites calcareous mounds (made of CaCO3) oldest are 3 billion years old still being formed Prochlorococcus – most abundant photosynthetic organism in the ocean 20 Fig. 5.4 stromatolites in the Bahamas 21 Types of cyanobacteria endolithic – burrow into calcareous rocks and coral skeletons Planktonic species rapidly multiply some “red tides” epiphytes live on algae endophytes live in algae lifeinfreshwaterorg.uk 22 Archaea, page 1 among simplest, most primitive Oldest fossils: 3.8 billions years old common in water column and sediments Important role in early evolution Spherical, spiral, rod shaped 23 Fig. 5.5 24 Archaea, page 2 some are “extremophiles” Deep water: high pressure (300-800 atm) hypersalinity high temperatures (70-80oC) • some up to 121oC extreme pH (acid and alkaline) some live symbiotically in sponges, seacucumbers, and fishes 25 Page 92 Depth distribution of bacteria and archaea in the subtropical North Pacific 26 Prokaryote metabolism metabolism –all the chemical reactions that take place in an organism autotrophs – organisms that can use energy to make their own organic compounds (primary producers) photoautotrophs – photosynthetic, contain chlorophyll and photosynthetic pigments to trap light energy Use CO2 to make organic compounds release O2 not the same process as in plants 27 Light energy without photosynthesis Light-mediated ATP synthesis energy from sunlight trapped in ATP proteorhodopsin, bacteriorhodopsin • pigment converts light energy to ATP • doesn’t use cholorphyll 28 Chemosynthesis Deriving energy from chemical compounds hydrogen sulfide (H2S) oxidation reactions • substrates: ammonium, nitrite, iron • oxidation reactions add oxygen or remove hydrogen forming higher energy bonds • chemical energy is stored in chemical bonds 29 Tab. 5.1 30 Heterotrophs obtain energy from organic matter by respiration in marine bacteria and archaea: mostly decomposers respiration in aerobic bacteria uses oxygen respiration in anaerobic bacteria does not use oxygen • anaerobic bacteria won’t grow in the presence of oxygen • anoxic (devoid of oxygen ) sediment is site of H2S producing bacteria 31 Nitrogen fixation conversion of gaseous nitrogen (N2) into ammonium(NH4+1) ammonium can be used as a nitrogen source for primary producers carried out by planktonic cyanobacteria 32 Protista simple eukaryotes unicellular or multicellular without specialized tissues formerly a kingdom relatively simple organization • distinguishes the protists from other eukaryotes, such as fungi, animals and plants. 33 34 Unicellular algae photosynthesis takes place in chloroplasts green, red, brown organelles layers of internal membranes with pigments “plants” • no flowers, leaves, stems, or roots • some swim with flagella 35 Diatoms Phylum Bacillariophyta unicellular (may aggregate into chains or stars) open water primary producers cell walls made of silica (SiO2) glassy shell called frustule golden brown chloroplasts • chlorophyll a and c, carotenoid pigments minute perforations 36 Domoic acid Some diatoms produce domoic acid neurotoxin contaminates fish or shellfish fatal to marine mammals and humans that eat contaminated organisms 37 Fig. 5.6 Diatom cell 38 Fig. 5.7 Diatom reproduction 39 Dead diatoms settle to the ocean floor form biogenous sediments • siliceous ooze • diatomaceous ooze • fossil deposits found inland make diatomaceous earth • used in pool filters • insulators • mild abrasives 40 Blooms Rapid reproduction Triggered by favorable environmental conditions nutrients and light 41 Fig. 5.8 DINOFLAGELLATES 42 Dinoflagellates Unicellular Planktonic Cell wall made of cellulose Most photosynthesize Some ingest food particles Crude eye (light sensitive pigment spot) One of the major causes of “red tide” 43 Zooxanthellae round, golden-brown dinoflagellates live in association with animals sponges giant clams sea anemones Help provide organic matter to coral for reef building 44 Fig. 5.9 Silicoflagellate 45 Fig. 5.10 Coccolithophorids, Umbilicosphaera sibogae 46 Protozoans animal-like eukaryotes unicellular heterotrophic (ingest food) 47 Foraminiferans Phylum Granuloreticulosa Marine protozoans shell, or test, made of calcium carbonate (CaCO3) retractable pseudopodia live on sea bottom, form foraminiferous ooze 48 Fig. 5.11 foraminiferans 49 Fig. 5.12 radiolarians – shells made of glass 50 Ciliates Protozoans with hairlike cilia 51 Fig. 5.13 Tintinnopsis 52 Fungi Eukaryotic molds and yeasts multicellular live symbiotically with algae to form lichen fungi support algae or cyanobacteria provide food from photosynthesis 1500 known marine species 53 Fig. 5.14 Encrusting lichens form a dark band. 54 Page 90 Japanese pufferfish, fugu Do symbiotic bacteria produce tetrodotoxin? 55 Page 96 Bioluminscent dinoflagellates Phosphorescent bay, Puerto Rico 56 Tab. 5.2 57