Midterm 1 Flashcards
What is a reef?
A living community of bottom-dwelling (benthic) and swimming organisms, which centers on corals, oysters, worms and other cementing organisms
-organisms bind, secrete and precipitate CaCO3 in place, resulting in a 3D structure
What are stony corals?
-colonial organisms composed of hundreds of individuals, called polyps
-building up reef structures “framework builders”
-reef building corals are “hermatypic” - stony corals
What are morphological classifications of hermatypic corals?
-branching corals (fast growth)
-table or foliose corals (fast growth)
-massive corals (slow growth)
Accretion and erosion
Accretion: build up, primary production of calcium carbonate, and the creating of 3D structure
Erosion: mechanical or biotic agents, bioeroders
Accretion>erosion
Epilithic vs endolithic organisms
Epilithic: Organisms outside of the reef that contribute to its erosion (parrotfish)
Endolithic: organisms inside the reef that contribute to its erosion (mollusks, sponges)
Limiting factors for corals (abiotic conditions)
-temperature (narrow range)
-light/depth
-salinity (narrow range)
-sedimentation
-emergence into air
-Wave forcing
Temperature (limiting factor)
Higher temps cause bleaching
-lower temperature corals grow slowly and are outcompeted
Light (limiting factor)
-species specific, depends on zooxanthellae and coral species
-hermatypic species aren’t generally found below 50m
-light determines growth and zonation patterns (deep vs shallow)
Photosynthetically active radiation (PAR)
-solar radiation that photosynthetic organisms are able to use in the process of photosynthesis
-photons at shorter wavelengths are more energetic, so they can be damaging to cells and tissues
-photons at longer wavelengths don’t carry enough energy to allow for photosynthesis
Sedimentation (limiting factor)
-fine sediments interfere with coral respiration and feeding
-nutrients with sediments can cause algal blooms
-turbidity can affect photosynthesis and coral distributions
-increased turbidity = decrease in coral health
How do corals deal with sediments?
-mucus entanglement
-ciliary action
-tentacular manipulation
-pulsed inflation
Where are coral reefs located?
-limited to the tropics
-generally located in the Caribbean and Indo-Pacific and Coral Triangle (cradle of diversity)
due to the sediments in the Amazon river, there is no little development of corals
Fringing reef
Margin between land and sea
-low in diversity
-increased wave action
-very harsh environment
Patch reef
In between fringing reefs and barrier reefs
-located in the lagoon
-low wave action, not very harsh environmental conditions
Barrier reef
-separated from land by lagoon
-high diversity because its influenced diversity brought by open ocean waves
How do atoll reefs form?
-atoll reefs form from the subsidence of volcanic islands
-starts as fringing reef->barrier reef->atoll reef
-as the volcano sinks, corals grow vertically
How did the Great Barrier Reef form?
-used to be a mountain range and as the sea level lowered, the corals grew vertically
Horizontal/vertical distribution of a general reef
-seagrass (nurseries)
-reef flat (harsh, tidally limited, species poor)
-reef crest (barrier reef, very energetic, species poor)
-fore reef
Patch reefs in lagoons
-high points of underlying rock allows for corals to settle away from sand
-can be numerous and support diverse communities of corals and fish
Spurs and grooves -shallow fore reef
-alternating ridges and sand channels perpendicular to the shore
-formed by incoming waves/erosion or coral growth
Higher vs lower fore reef
Higher: high energy/light, branching corals, competition
Lower: less energy/light, massive/foliose corals, sedimentation
Epidermis/ectodermis
Includes oral region covering mouth and tentacles
Gastrodermis
-Digestion and absorption of nutrients, zoozanthellae
-folds into the coelenteron
Mesoglea
Gelatinous connective tissue
Mesenteries
Folds of gastrodermis and mesoglea