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Chapter 28 (B)
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These hyphae have cellulose cells walls and are analogous with
the hyphae of true fungi (with chitin cell walls).
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Unlike fungi, the diploid stage dominates in oomycotes and
they have biflagellated cells.
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These filamentous bodies have extensive surface area,
enhancing absorption of nutrients.
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In the Oomycota, the “egg fungi”, a relatively large egg cell
is fertilized by a smaller “sperm nucleus,”
forming a resistant zygote.
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Water molds are important decomposers, mainly in fresh
water.
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They form cottony masses on dead algae and
animals.
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Some water molds are parasitic, growing on the skin and gills
of injured fish.
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White rusts and downy mildews are parasites of terrestrial
plants.
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They are dispersed by windblown spores.
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One species of downy mildew threatened French vineyards in the
1870’s and another species causes late potato blight, which
contributed to the Irish famine in the 19th
century.
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The photosynthetic stramenopile taxa are known collectively as
the heterokont algae.
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“Hetero” refers to the two different types of
flagella.
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The plastids of these algae evolved by secondary
endosymbiosis.
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They have a three-membrane envelope and a small amount of
eukaryotic cytoplasm within the plastid.
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The probable ancestor was a red alga.
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The heterokont algae include diatoms, golden algae, and brown
algae.
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Diatoms
(Bacillariophyta) have unique glasslike walls composed of
hydrated silica embedded in an organic matrix.
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The wall is divided into two parts that overlap like a shoe
box and lid.
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Most of the year, diatoms reproduce asexually by mitosis with
each daughter cell receiving half of the cell wall and
regenerating a new second half.
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Some species form cysts as resistant stages.
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Sexual stages are not common, but sperm may be amoeboid or
flagellated, depending on species.
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Diatom are abundant members of both freshwater and marine
plankton.
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Diatoms store food reserves in a glucose polymer, laminarin,
and a few store food as oils.
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Massive accumulations of fossilized diatoms are major
constituents of diatomaceous earth.
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Golden algae (
Chrysophyta), named for the yellow and brown carotene
and xanthophyll pigments, are typically
biflagellated.
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Some species are mixotrophic and many live among freshwater
and marine plankton.
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While most are unicellular,
some are colonial.
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At high densities, they can form resistant cysts that remain
viable for decades.
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Brown algae
(Phaeophyta) are the largest and most complex
algae.
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Most brown algae are multicellular.
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Most species are marine.
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Brown algae are especially common along temperate coasts in
areas of cool water and adequate nutrients.
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They owe their characteristic brown or olive color to
accessory pigments in the plastids.
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Some brown algae have floats to raise the blades toward the
surface.
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Giant brown algae, known as kelps, form forests in deeper
water.
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The stipes of these plants
may be 60 m long.
Structural and biochemical adaptations help seaweeds
survive and reproduce at the ocean’s
margins
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The largest marine algae, including brown, red, and green
algae, are known collectively as seaweeds.
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Seaweeds have a complex multicellular anatomy, with some
differentiated tissues and organs that resemble those in
plants.
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These analogous features include the thallus or body of the
seaweed.
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The thallus typically consists of a rootlike holdfast and a
stemlike stipe, which supports leaflike photosynthetic
blades.
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Many seaweeds have biochemical adaptations for intertidal and
subtidal conditions.
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The cells walls, composed of cellulose and gel-forming
polysaccharides, help cushion the thalli against agitation by
waves.
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Many seaweeds are eaten by coastal people, including
Laminaria (“kombu” in Japan) and Porphyra
(Japanese “nori”) for sushi wraps.
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A variety of gelforming substances are extracted in commercial
operations.
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Algin from brown algae and agar and carageenan from red algae
are used as thickeners in food, lubricants in oil drilling, or
culture media in microbiology.
Some algae have life cycles with alternating
multicellular haploid and diploid
generations
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The multicellular brown, red, and green algae show complex
life cycles with alternation of multicellular haploid and
multicellular diploid forms.
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A similar alternation of generations evolved convergently in
the life cycle of plants.
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The life cycle of the brown alga Laminaria is an
example of alternation of generations.
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The diploid individual, the sporophyte, produces
haploid spores (zoospores) by meiosis.
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The haploid individual,the gametophyte, produces
gametes by mitosis that fuse to
form a diploid zygote.
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In Laminaria, the sporophyte and gametophyte are
structurally different, called
heteromorphic.
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In other algae, the alternating generations look alike
(isomorphic), but they differ in the number of
chromosomes.
Rhodophyta: Red algae lack flagella
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Unlike other eukaryotic algae, red algae have no
flagellated stages in their life cycle.
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The red coloration visible in many members is due to the
accessory pigment phycoerythrin.
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Coloration varies among species and depends on the depth which
they inhabit.
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The plastids of red algae evolved from primary endosymbiosis
of cyanobacteria.
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Some species lack pigmentation and are parasites on other red
algae.
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Red algae (Rhodophyta) are the most common seaweeds in the
warm coastal waters of tropical oceans.
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Others live in freshwater, still others in soils.
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Some red algae inhabit deeper waters than other photosynthetic
eukaryotes.
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Their photosynthetic pigments, especially phycobilins, allow
some species to absorb those wavelengths (blues and greens)
that penetrate down to deep water.
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One red algal species has been discovered off Bahamas at a
depth of over 260m.
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Most red algae are multicellular, with some reaching a size to
be called “seaweeds”.
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The thalli of many species are filamentous.
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The base of the thallus is usually differentiated into a
simple holdfast.
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The life cycles of red algae are especially
diverse.
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In the absence of flagella, fertilization depends entirely on
water currents to bring gametes together.
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Alternation of generation (isomorphic and especially
heteromorphic) is common in red algae.
Chlorophyta: Green algae and plants evolved from a
common photoautotrophic ancestor
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Green algae
(chlorophytes and charophyceans) are named for their
grass-green chloroplasts.
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These are similar in ultrastructure and pigment composition to
those of plants.
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The common ancestor of green algae and plants probably had
chloroplasts derived from cyanobacteria by primary
endosymbiosis.
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The charophyceans are especially closely related to land
plants.
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Most of the 7,000 species of chlorophytes live in
freshwater.
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Other species are marine, inhabit damp soil or snow, or live
symbiotically within other eukaryotes.
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Some chlorophytes live symbiotically with fungi to form
lichens, a mutualistic collective.
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Chlorophytes range in complexity, including:
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biflagellated unicells that resemble gametes and
zoospores
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colonial species and filamentous forms
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multicellular forms large enough to qualify as seaweeds.
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Large size and complexity in chlorophytes has evolved by three
different mechanisms:
(1) formation of colonies of individual cells
(Volvox)
(2) the repeated division of nuclei without cytoplasmic
division to form multinucleate filaments
(Caulerpa)
(3) formation of true multicellular forms by cell division and
cell differentiation (Ulva).
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Most green algae have both sexual and asexual reproductive
stages.
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Most sexual species have biflagellated gametes with cup-shaped
chloroplasts.
A diversity of protists use pseudopodia for movement
and feeding
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Three groups of protists use pseudopodia, cellular
extensions, to move and often to feed.
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Rhizopods (amoebas) are all unicellular and use
pseudopodia to move and to feed.
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Pseudopodium emerge from anywhere in the cell
surface.
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To move, an amoeba extends a pseudopod, anchors its tip, and
then streams more cytoplasm into the pseudopodium.
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Amoeboid movement is driven by changes in microtubules and
microfilaments in the cytoskeleton.
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Pseudopodia activity is not random but in fact directed toward
food.
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In some species pseudopodia extend out through openings in a
protein shell around the organism.
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Amoebas inhabit freshwater and marine environments
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They may also be abundant in soils.
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Most species are free-living heterotrophs.
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Some are important parasites.
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These include Entamoeba histolytica which causes
amoeboid dysentery in humans.
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These organisms spread via contaminated drinking water, food,
and eating utensils.
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Actinopod (heliozoans and radiolarians), “ray foot,” refers to
slender pseudopodia (axopodia) that radiate from the
body.
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Each axopodium is reinforced by a bundle of microtubules
covered by a thin layer of cytoplasm.
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Most actinopods are planktonic.
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The large surface area created by axopodia help them to float
and feed.
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Smaller protists and other microorganisms stick to the
axopodia and are phagocytized by the thin layer of
cytoplasm.
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Cytoplasmic streaming carries the engulfed prey into the main
part of the cell.
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Most heliozoans (“sun animals”) live in fresh
water.
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Their skeletons consist of unfused siliceous (glassy) or
chitinous plates.
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The term radiolarian refers to several groups of mostly
marine actinopods.
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In this group, the siliceous skeleton is fused into one
delicate piece.
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After death, these skeleton accumulate as an ooze that may be
hundreds of meters thick in some seafloor
locations.
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Foraminiferans, or forams, are almost all
marine.
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Most live in sand or attach to rocks or algae.
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Some are abundant in the plankton.
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Forams have multichambered, porous shells, consisting of
organic materials hardened with calcium carbonate.
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Pseudopodia extend through the pores for swimming, shell
formation, and feeding.
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Many forams form symbioses with algae.
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Over ninety percent of the described forams are
fossils.
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The calcareous skeletons of forams are important components of
marine sediments.
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Fossil forams are often used as chronological markers to
correlate the ages of sedimentary rocks from different parts
of the world.
Mycetozoa: Slime molds have structural adaptations and life
cycles that enhance their ecological roles as
decomposers
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Mycetozoa
(slime molds or “fungus animals”) are neither fungi nor
animals, but protists.
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Any resemblance to fungi is analogous, not homologous, for
their convergent role in the decomposition of leaf litter and
organic debris.
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Slime molds feed and move via pseudopodia, like amoeba, but
comparisons of protein sequences place slime molds relatively
close to the fungi and animals.
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The plasmodial slime molds (Myxogastrida) are brightly
pigmented, heterotrophic organisms.
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The feeding stage is an amoeboid mass, the plasmodium,
that may be several centimeters in diameter.
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The plasmodium is not multicellular, but a single mass of
cytoplasm with multiple nuclei.
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The diploid nuclei undergo synchronous mitotic divisions,
perhaps thousands at a time.
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Within the cytoplasm, cytoplasmic streaming distributes
nutrients and oxygen throughout the plasmodium.
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The plasmodium phagocytises food particles from moist soil,
leaf mulch, or rotting logs.
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If the habitat begins to dry or if food levels drop, the
plasmodium differentiates into stages that lead to sexual
reproduction.
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The cellular slime molds (Dictyostelida) straddle the
line between individuality and multicellularity.
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The feeding stage consists of solitary cells.
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When food is scarce, the cells form an aggregate (“slug”) that
functions as a unit.
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Each cell retains its identity in the aggregate.
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The dominant stage in a cellular slime mold is the haploid
stage.
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Aggregates of amoebas form fruiting bodies that produce spores
in asexual reproduction.
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Most cellular slime molds lack flagellated stages.
Multicellularity originated independently many
times
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The origin of unicellular eukaryotes permitted more structural
diversity than was possible for prokaryotes.
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This ignited an explosion of biological
diversification.
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The evolution of multicellular bodies and the possibility of
even greater structural diversity, triggered another wave of
diversification.
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