Transcript Document
Opener
The
Microbial
World
Radiolarian shells
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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.
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Fig. 5.1
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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
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Retroviruses
Genetic information stored as RNA
Responsible for human diseases
HIV/AIDS
leukemia
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Lytic and Lysogenic viruses
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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
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Bacteriophages
Viruses that specifically target and
destroy bacteria.
Common in marine environments
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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
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Viral diseases
Shellfish
Fishes
Sea turtles
Marine mammals
Humans
oysters and mussels filter sewagecontaminated water.
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Prokaryotes
Smallest, structurally simplest living
organisms
oldest forms of life on earth
most chemical processes evolved
first in prokaryotes
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Prokaryotic cells
protective cell wall
plasma membrane immediately
inside cell wall
lack a nucleus
lack most membrane-bound
organelles
circular DNA
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Fig. 5.2
Cyclobacterium marinarus, a ringforming marine bacterium
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Fig. 5.3
The largest known
bacterium,
Thiomargarita
namibiensis, 0.75mm
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2 prokaryotic domains
Bacteria
and Archaea
Differences in:
• chemistry of cell walls
• cell membranes
• cellular machinery that makes proteins
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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
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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
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Bacteria as Decomposers
Grow in detritus (dead organic
matter)
break down waste products
release nutrients back into the
environment
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Cyanobacteria
formerly called blue-green algae
photosynthetic
pigments
chlorophyll a (like eukaryotes)
phycocyanin (blue)
phycoerythrin (red)
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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
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Fig. 5.4
stromatolites in the
Bahamas
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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
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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
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Fig. 5.5
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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
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Depth distribution of
bacteria and archaea in
the subtropical North
Pacific
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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
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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
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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
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Tab. 5.1
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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
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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
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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.
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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
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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
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Domoic acid
Some diatoms produce domoic acid
neurotoxin
contaminates fish or shellfish
fatal to marine mammals and humans
that eat contaminated organisms
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Fig. 5.6
Diatom cell
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Fig. 5.7
Diatom reproduction
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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
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Blooms
Rapid reproduction
Triggered by favorable
environmental conditions
nutrients and light
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Fig. 5.8
DINOFLAGELLATES
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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”
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Zooxanthellae
round, golden-brown dinoflagellates
live in association with animals
sponges
giant clams
sea anemones
Help provide organic matter to coral
for reef building
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Fig. 5.9
Silicoflagellate
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Fig. 5.10
Coccolithophorids,
Umbilicosphaera sibogae
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Protozoans
animal-like eukaryotes
unicellular
heterotrophic (ingest food)
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Foraminiferans
Phylum Granuloreticulosa
Marine protozoans
shell, or test, made of calcium
carbonate (CaCO3)
retractable pseudopodia
live on sea bottom, form
foraminiferous ooze
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Fig. 5.11
foraminiferans
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Fig. 5.12
radiolarians –
shells made of
glass
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Ciliates
Protozoans with hairlike cilia
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Fig. 5.13
Tintinnopsis
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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
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Fig. 5.14
Encrusting lichens form
a dark band.
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Japanese pufferfish, fugu
Do symbiotic bacteria produce tetrodotoxin?
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Bioluminscent dinoflagellates
Phosphorescent bay, Puerto Rico
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Tab. 5.2
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