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Macroalgal
and Periphyton Ecology
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Substrate:
macroalga and periphyton live attached and non-motile on substrate; substrates
can be rocks, corals, sand, other algae, aquatic animals
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Light
requirements for photosynthesis limits distribution
to shallow, coastal areas
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Macroalgal
production is important for coastal food webs
in terms of carbon fixation and as habitat for other animals and juvenile
fish; production of seaweed communities and kelp forrests is a high as
highest terrestrial primary production
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Only
10% of macroalgal biomass is directly grazed by
herbivores, 90% is made available to higher trophic levels by the detritus
food web
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In streams
and shallow lakes,
periphyton contributes more primary production than phytoplankton
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Eutrophication
can lead to overgrow of substrates and benthic communities by fast-growing
macroalgae such as the green alga Cladophora
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Community
shaping factors: herbivorous grazing, competition
for substrate and nutrients, pathogene attack, physico-chemical environment
The Physical Environment:
Tides
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Tides
:
periodical changes in the water level due to the gravitational influence
of the moon (and the sun)
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High
tides occur every 12 hrs 25 min = ½ lunar day !
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Sun and
Moon and Earth…
Gravitational
forces of sun and moon add at full and new moon to produce spring tides.
Gravitational forces of sun and moon compete at half moon to produce neap
tides.
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Lunar
tides occur twice a day (semidiurnal
tides), solar
tides once a day (diurnal tides)
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Depending
on the orbital position of sun and moon and ocean region, mixed tides occur.
The Littoral: Between
Water and Air
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Harsh
environment: loss of water at low tide; physical
forces of waves; variation in temperature; UV radiation; ice formation;
variation in salinity (rain exposure)
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Adaptation
of algae to life between water and air:
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Solid
attachement against wave action
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High
temperature and water loss tolerance (60-90% in some algae)
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Synchronized
release of gametes
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Cluster
formation
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Highly
flexible thalli or thick, rigid thalli
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Littoral
zonation: Tides set the boundaries for permanently,
periodically, and rarely submerged zones in the coastal ecosystem, the
littoral
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Eulittoral:
range between mean low water and mean high water, periodically submerged
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Supralittoral:
range above the mean high water, rarely submerged
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Sublittoral:
range below the mean low water, permanently submerged
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Zonatation
of macroalgae according to resistance to wave action, falling dry, light
requirements – specific for each coast and substrate
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Wave
action has positive and negative effects:
Positive
Effects
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Reduce shading by re-arranging
thalli
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Transport and mixing of nutrients
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Reduce thickness of boundary
layer (higher uptake of nutrients and faster growth)
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Remove sessile animals and other
competitors for habitat
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Dispersal of spores, gametes,
zygotes
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Negative
Effects
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Damage, destruction, removal
of thalli
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Removal of settling zygotes/germlings
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Expense of energy into strong
holdfast and thick, rigid thallus or calcification
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Destruction by ice floes during
winter in temperate and polar regions
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Light:
High light irradiance and UV irradiation can cause photoinhibition and
DNA damage; low light irradiance requires low-light adaptation by higher
pigment concentrations and adjusting thallus forms
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Light
and UV protection mechanisms involve inactive
photosystems, increase in accessory pigments, UV absorbants (mycosporin
like amino acids)
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Timing
of growth and reproduction is triggered by light signals (sensor pigments
cytochrome, phytochrome)
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Herbivory
Defense
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Macroalgal
herbivores are predominantly amphipods, copepods,
polychaetes, urchins, fish
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Chemical
defense by production of secondary metabolic
substances such as terpenes, alkaloids, halogenated (bromid) phenolics,
and many more
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One species
can produce multiple defense chemicals
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Structural
defense by spiny or calcified thalli
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Interaction
of defense mechanisms: in the green alga Halimeda,
cell division occurs at night (no visual predators), and young, less calcified
cells contain more defense chemicals than older, calcified cells
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Animals
(e.g. the amphipod Ampithoe) ingest algal defense chemicals to protect
themselves against grazers
The amphipod Ampithoe uses defense chemicals from the brown alga
Dictyota
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Energetic
cost: production on complex defense molecules
requires energy; defended species often grow slower than species without
defense chemicals; production of defense chemicals can be grazer-induced
or constitutive (continuous)
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Marine
Periphyton Turfs
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Periphyton
compete for habitat space
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Macroalgae
possess mechanisms to prevent overgrowth by periphyton, such as shedding
superficial cell layers or constant errosion of thallus tips
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Turf
development starts usually with diatom settlement, followed by cyanobacteria,
which eventually dominate most marine turfs
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epiphytic
cyanobacteria are a major source for nitrogen fixation
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Primary
production is high per unit biomass (in contrast to macroalgae)
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Grazing
pressure on epiphyton is higher than on macroalgae; grazing helps preserving
the turf by preventing dominance of larger forms and enhancing branching
by grazing on filament/thallus tips
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Freshwater
Periphyton
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Freshwater
periphyton comprises settlement on other algae/plants and microphytobenthos
(on rocks and sediments)
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Major
source of photosynthetic carbon fixation in shallow lakes and streams,
which do not provide a favorable environment for plankton
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Periphyton
traps nutrients from the water and transfers them to the sediment upon
death, thus preventing nutrient loss from wetlands and streams into lakes
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Freshwater
periphyton contains more bacteria and fungi than marine turfs, held together
by mucilage from algae and/or bacteria
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Metaphyton
describes loose masses of epiphyton broken from their substrate and floating
in the plankton
Grazing
losses are higher than in marine epiphyton
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