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Marine Habitats
• What is a marine habitat?
• Where do we find (different) marine habitats?
• Water quality parameters that effect life?
• Who lives there (marine organisms and their necessary adaptations)?
• Marine Ecology (intro.)
• The benthic environment is divided by depth into the: – intertidal (littoral) zone
– subtidal (sublittoral) zone
– Epi, Meso, Bathyal & Abyssal zone(s)
– (other) hadal zone
• The pelagic environment is divided broadly into the: – neritic zone
– oceanic zone
• More specifically into the:– Epipelagic zone
– Mesopelagic zone
– Bathypelagic zone
– Abyssalpelagic zone
– hadalpelagic zone
•There are two major marine provinces: –the benthic (bottom)
–the pelagic (water column)
• PELAGIC ZONES: “water column”
(1) Oceanic – beyond shelf break
(2) Neritic – area that lies over shelf
Then this is divided vertically by depth:
(1) Epipelagic: shallowest (w/ lots of light)
(2) Mesopelagic: below (minimal light, no primary production, “twilight zone”)
(3) Bathypelagic, Abyssopelagic, Hadopelagic: at bottom (no light, “deep sea environment”)
ORGANISMS THAT LIVE IN PELAGIC ZONE ARE IN WATER COLUMN ONLY = PLANKTON and NEKTON
Each zone is different
• Light• Temperature• Salinity• Other: Turbidity/Water Clarity/Sedimentation, Dissolved
Gases (such as Carbon Dioxide), pH (ocean acidification), Pressure etc.
These are considered “Water Quality” parameters (as they effect the quality of the seawater that serves as “home” for so many marine organisms)
What does this mean to MARINE LIFE?
• Light effects WHERE plants and animals can live.
• Temperature effects WHERE plants and animals can live.
• Salinity effects WHERE plants and animals can live.
• …WATER QUALITY PARAMETERS determine the “health” of the environment marine organisms live in.
• The ocean can also be divided into zones based upon depth of light penetration.
– The photic zone is the depth where light is sufficient for photosynthesis.
– The dysphotic zone is where illumination is too weak for photosynthesis.
– The aphotic zone receives no light from the surface because it is all absorbed by the water above.
• In the dysphotic zone, seasonal effects are minimal – conditions tend to be uniform most of the year.
• The aphotic zone is permanently dark and cold.– It contains many unique midwater fishes.
Fnft: Midwater Fishes
• Light penetration is different, based on:
– Levels of photosynthesis/primary production.
– Water quality/sedimentation/turbidity
– Location: proximity to shoreline.
• In turbid coastal waters light rarely penetrates deeper than 20m.– The water appears
yellow to green because particles reflect these wavelengths.
Fnft: Yangtze River
Light Penetration
• Dictates how a species can grow
• Picture 1 is “shallow” subtidal coral – notice “raised” edges
• Picture 2, much deeper down, shows a coral that is FLATTENED (like a solar panel!) to “catch” as much light as possible in deeper waters
• This is SPECIES ADAPTATION!
Properties of Seawater
Light and Temperature in the Sea
• The range of biologically important temperatures at the
Earth’s surface.
• Fnft: Earth's sea surface temperatures obtained from two weeks of satellite infrared observations July 1984. Temperatures are color coded, with red being warmest and decreasing
through oranges, yellows, greens, blues, and black.
Properties of Seawater
Light and Temperature in the Sea
Image courtesy MODIS Ocean Group, NASA GSFC, and the University of Miami
• Temperature can control aspects of an organism’s life:– distribution
– degree of activity
– Reproduction
Barnacles
Properties of SeawaterLight and
Temperature in the Sea:
Our Planetary Greenhouse
• Pattern of atmospheric CO2 increase
over five decades. The slight annual variations are due to seasonal CO 2 uptake and release by land plants.
Reproduced from Robert A. Rohde.
• Other water quality parameters(these are certainly associated with light and
temperature)-- Salinity-- Dissolved Gases (pH/ocean acidification, carbon dioxide etc.)
+ Summary of all together included
Properties of Seawater
Geographic variations of surface ocean salinities, expressed in parts per thousand (‰).
• Ocean Salinity
Properties of Seawater
Dissolved Gases and Acid-Base
Buffering
• The pH scale, showing the concentration of H+ ions at each pH value. Note that the concentration scale is exponential.
Pressure
• Water is heavier than air
• Pressure changes ( a lot!) w/ increased water depth
• 1 atm. of pressure = sea level (on land) but in ocean each 10 m of depth (33’) you add another atm. of pressure
Combined…
• These give us a “3 layered” (stratified) ocean (based on depth) and specific areas for our unique marine habitats to exist.
• Coral Reefs don’t grow in the Arctic (why?) and Mangrove Forests aren’t found in the Arctic (why?)
• Everything has a “place!”
What grows where?
Image courtesy MODIS Ocean Group, NASA GSFC, and the University of Miami
Temperate vs. Tropical vs. Arctic Marine Habitats; examples include: Coral Reefs, Kelp Forests, Polar Seas, SAV Beds,Estuaries, Mangrove Forests etc.
Marine organisms can also be classified by lifestyle
• Plankton float in the water and have no ability to propel themselves against a current.– They can be divided into:
• phytoplankton (plants) • zooplankton (animals)
• Nekton are active swimmers and include:– fish,– Reptiles– mammals– birds
Plankton - Larvae
• Nekton have the ability to swim against currents.– They can actively search for a hospitable environment.
– Many fish school, which is another form of patchiness.
School of Fish
Major pelagic sediments in the ocean are red clay and biogenic oozes.
“Marine Snow”
Foraminifera
Diatoms
• Benthic organisms live:– on the bottom
(epifauna)
– within the bottom sediments (infauna)
• Some organisms cross from one lifestyle to another during their life, for example being planktonic early in life and benthic later.
Flounder, a bottom fish
• The water column is shallow in the sublittoral zone.
• Bottom energy is a function of:– wave energy
– tidal current
• Bottom energy at the sea bed diminishes as distance from shore increases.
Benthic zone properties/sedimentation
• The sea floor can be divided into high energy environments and low energy environments.
Figure 13-5a• Bottom energy affects organisms by:
–moving sediment around
–creating an unstable substrate
–controlling sediment size
• Physical factors regulate the number, type and distribution of benthic organisms.
– The two major benthic communities based upon substrate are:
• Soft-bottom communities are typified by unconsolidated sand and mud substrates. Sandy areas harbor filter feeders whereas deposit feeders dwell in muddy regions (e.g. estuaries/beaches).
• Hard-bottom communities are typified by rock and gravel substrates. Seaweeds occur here and the animals tend to be filter feeders, grazers, and predators (e.g. Coral Reefs and Kelp Forests).
©Ablestock.com
If you’re not benthic you’re…
• PELAGIC!
• A “Pelagic community” is a community of organisms that live suspended in the water column…they either float (plankton) or swim (nekton).
• This is different than those that live on shore, on the bottom (etc.)
• Top predators in the open ocean are:– Mackerel
– Squid
– Jellyfish
– Tuna
– Porpoise
– Shark
– Humans
Squid
Tuna
Shark
Jellyfish
Pelagic