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microbial loop process
phytoplankton die w/o being eaten → break down into dissolved org matter → eaten by bacteria
→ bacteria incorp into standard food chain if eaten by zooplankton who are eaten by something bigger
→ or bacteria cycled back into microbial loop if eaten by zooplankton who aren’t eaten + return to DOM pool
microbial loop
marine version of detrital food chain
can add productivity to marine food chain by inclusion of outside detritus
as much as ½ primary production channeled thru it
seasonal productivity: salt marsh grasses
grasses have seasonal growth + dieback pds depending on location
dead grasses (wrack) stay rooted + rot where they are
stored nutrients from summer in underground rhizomes + turnover of wrack nutrients → large growth each spring
seasonal productivity: phytoplankton in tropics
oligotrophic (low nutrients)
no seasonal bloom
year-round sunlight
always nutrient limited
seasonal productivity: phytoplankton in polar regions
bloom in summer when no light limitations
recedes in winter + fall due to onset of shorter days
seasonal productivity: phytoplankton in temperate regions (spring)
larger spring bloom
not light limited
thermocline forms, concentrating phytoplankton to surface waters, don’t get circulated to below comp depth daily
bloom dies due to nutrient limits from surface water depletion, no upwelling
seasonal productivity: phytoplankton in temperate regions (fall)
smaller fall bloom
fall storms kick up sedients + release nutrients by breaking thermocline + allowing mixing of deep water
bloom dies bc of light limitations + circulation of phytoplankton below comp depth
seasonal productivity: phytoplankton in temperate regions (summer + winter)
summer: no light limit but no nutrients left from spring, + added stratification
winter: light limit, but despite no thermocline, there is no bloom
geotaxis
to know whether to move up or down by sensing earth’s gravity
positive = w/gravity (down)
negative = vice versa
phototaxis
sensitivity to light
positive = towards light (up)
negative = vice versa
barotaxis
hydrostatic pressure
increases w/incoming tides bc water depth increases → more pressure
role of adults
time, season, location, tide, depth of spawning + release of eggs, + buoyancy of eggs
→ determine transport for first few days of development before larvae are big enough to act on their own
selective tidal stream transport (STST)
relies on combo of larval behavior + oceanographic processes to transport larvae much farther than they could swim on their own
factors of selective tidal stream transport (STST)
oceanographic processes
tides: ebb, flood, slack water, zero net movement up/down estuary
vertical estuarine strat
boundary layer effect
old settlement model
random larval settlement
site-specific mortality determines final distribution
new settlement model
active habitat selection based on larval behavior + settlement cues
new model: larval behavior
free-swimming larvae alternate photonegative + photopositive to test bottom (crawling, turning, flexing abdomen) for suitable cues
leave if surface is clean (uncolonized) or crowded
new model: settlement cues
chem/microfloral cues indicating suitable habitat
presence of conspecifics
pits + grooves
avoidance of competition
bottom type: solid vs mud vs sand
passive deposition (microhydrodynamics)
larvae deposited on bottom as a function of their fall velocities, behavior, + bottom flow patterns
passive deposition: deposition
can determine where + when active habitat selection can take place
larvae transported by velocities above their swimming speeds deposited in bottom in areas of low flow, where their swimming + habitat selection behavior is effective
passive deposition: structure
any structure on bottom can create passive deposition of larvae bc currents + flow patterns are changed as they move around the structure
cyclical movement in vortexes around structure → increases sedimentation + passive deposition
interaction of flow + chem cues
flow can determine when a larvae has an opp to respond to a chem cue + when they don’t
still water: each chem cue can attract larvae
moving water: only the cues in low-flow/deposition areas can attract larvae
bottom-up regulation
community structure shaped by nutrient availability + consequent primary production
bottom-up regulation: seasonal photosynthetic blooms
blooms create seasonal oscillations in abundance of orgs at higher trophic levels
species + pops up the food chain rise one at a time one after the other, but with 10% less energy each time
bottom-up regulation: nutrient availability
increased nutrients → increased secondary production → increasing reproduction
top-down regulation
control of diversity + abundance in a community based on presence of consumers
direct effects of consumers limit success of orgs at lower trophic levels (ecological + evolutional)
ecological effects of top-down regulation
death: decreases prey pop size + less prey left to reproduce
limiting prey to refuges
indirect effects
ecological effects of top-down regulation: limiting prey to refuges
generally physiologically stressful places → more energy spent to survive → less energy left for reproduction → decreases pop size
top-down control: evolutionary time
consumers act as selective force for evolution of anti-predator defenses that promote coexistence of predator + prey
but metabolically expensive to make defenses
indirect effects of top-down control
effects other than spatial restriction of prey
trophic cascades
habitat modification
indirect effects of top-down control: trophic cascades
consumers limit their prey
releases lower trophic levels from predation
increases pop size of lower trophic levels
killifish - grass shrimp - anemone
gulls - urchins - algae
indirect effects of top-down control: habitat modification
modification of habitat by 1 consumer that trickles down to affect every other species that requires that habitat
urchins eat kelp, removing habitat species need for protection + primary production
zonation: physical stress
induced by env factors
terrestrial orgs: increased w/decreased elevation (towards water) bc increased salt, lower o2, lack of air, waterlogged sediment
marine orgs: increased w/increased elevation (towards shore) bc dessication, lack of water for respiration, thermal stress
zonation: biotic stress
competition, predation increase as physical strength decreases
terrestrial orgs: increases w/elevation (out of water)
marine: increases w/decreased elevation (into water)
positive interactions: facilitation
factor increasing success of a diff species → often leads to replacement of facilitator by species they helped
any action an org does that increases amt of env that meets niche requirements of another species
positive interactions: the facilitator
orgs that positively effect a neighboring org (measured by individual physio benefit or pop level effects
habitat amelioration
an org changes an abiotic factor that unintentionally helps a member of the same species/another species by making env less harsh for them
can allow for extension of range in stressful territory (can be facilitation)
ex low soil o2 counteracted by marsh grasses/mangroves oxygenating soil
habitat amelioration: physical stress + variation in neighbor interaction w/stress
amelioration more important the more stressful a habitat is
high stress levels = positive interactions
low stress levels = negative interaction (competition)
associational defenses
response to biotic stress (predation)
multiple species groupings (opportunistic or mutualistic, palatable orgs hiding among noxious prey)
tradeoff for loss of space/ideal conditions, increased competition
importance of habitat amelioration vs associational defenses
increasing physical stress + low consumer pressure = habitat amelioration more important
increasing consumer pressure + low env stress = assoc defense more important
ecosystem engineers
org that creates, significantly modifies, maintains, or destroys a habitat
also alters availability of env resources (light, nutrients, water flow, etc) for other species
estuary
semi-enclosed body of water in which fresh + saltwater mix
bar-built estuary
sandbars + barrier islands act as barrier btwn ocean + rivers behind the islands
ex: Pamlico Sound
fjord estuary
glacially carved U-shaped valley on coastline from mtns → sea
valleys flood at sea level rise
ex: coastal New Zealand
tectonic estuary
piece of land sinks, allows sea to flood area rather than sea level rising
ex: San Francisco Bay
coastal plain/drowned river valley estuary
sea invades river valleys + lowlands as sea level rises
ex: Chesapeake Bay