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mar bio exam 5

QuestionAnswer
The continental shelf is the submerged edge of a continental plate.
The continental shelf extends from the low tide line to an area known as the shelf break.
The slope of the continental shelf is normally more gradual, whereas, the slope past the shelf break is normally very steep.
Estuaries are much more well developed in areas of the world where the continental shelf has a gradual slope and is very wide.
The depth of water at the shelf break varies greatly with an average depth of around 490 feet.
The width of the continental shelf varies greatly from 0.6 miles to 470 miles with an average of 48 miles.
A major portion of the fisheries global catch is caught over the continental shelf.
A wide variety of organisms can be found on/in the continental shelf. Some of the most common includes sponges, cnidarians, worms, molluscs, fish and echinoderms.
Temperature of the water over the continental shelf varies much more than the water in the deep sea (but less than in an estuary).
The temperature in a continental shelf fluctuates more because the water is shallower than in the deep sea and because waves and currents keep the water circulating
Water turbulence created by waves and currents keep the water column well mixed.This affects not only the temperature of the water, but also affects the nutrients available in the water.
Nutrients come from many sources, including: -Autotrophs -Decaying marine organic matter -Nutrients delivered from estuaries and terrestrial ecosystems via rivers
Soft-bottomed benthic- -Dominant bottom type on the continental shelf. -There are more species present in this area than in the adjoining intertidal, but the distribution is often patchy
Sessile types are rare int he Soft-bottom benthic due to lack of “hard substrate” for attachment (remember, limiting resources?)
Many tube-builders can assist with the stability of the soft bottom habitat
Many soft-bottom benthic species are deposit feeders (directly getting nutrients from the soft bottomed material) -Many other species are suspension feeders and filter nutrients directly from the water
Bioturbators (organisms that disturb bottom sediments) constantly “churn” the bottom This churning helps to oxygenate benthic soils
Bioturbators can include worms, mollucs, fish and even whales
Skates and stringrays as well as sperm whales are well known for their activity as bioturbators
Seagrass Beds -They are best developed in sheltered, shallow waters with good water clarity -There are over 50 known species
Due to narrow tolerances, species of seagrass bed normally prefer either cool waters OR tropical/subtropical waters, but not both
Seagrasses are often found in combination with algal species
The density of individual seagrass plants tend to be very thick (high biomass)
Thalassia (turtle grass): -is a common seagrass in tropical and subtropical areas -It is named turtle grass because it is often directly consumed by green sea turtles
Zostera or eelgrass prefers cooler, temperate waters It is mainly found in the Pacific and the North Atlantic
Hard-bottomed subtidal- -Less common -Often, it is the result of a submerged rocky shoreline
Rock formations attract a wide variety of organisms including many sessile types that cannot survive in soft bottomed communities
Oyster reefs, worm tubes and calcareous algae can all serve as hard-bottomed subtidal communities
One of the most important features of the rocky hard-bottomed community is the hiding places it provides for prey and predators alike
Kelp community- Kelps are brown algae that are restricted to cold waters in distribution
In addition to requiring cold water, kelps are very nutrient-needy
Laminaria is a species of kelp common in the North Atlantic, North Pacific and the Asiatic coast of the Pacific - large primary producers
Macrocystis: -is a large species of kelp that can grow heights of over 100 feet -forms thick forests that serve as a MAJOR ocean ecosystem in the areas where it is found
Sea urchins are by far the largest direct consumer of kelp
The soft body of the coral (polyp) is enclosed in a hard shell of calcium carbonate “skeleton” created by the coral (technically called theca).
Hermatypic corals- -Reef builders -Normally contain zooxanthellae, symbiotic photosynthetic dinoflagellates -Restricted in distribution by water temperature and water quality
Ahermatypic corals- -Do not build reefs -May not contain zooxanthellae -Not restricted by water temperature and water quality
Corals are groups of polyps inter-connected by thin layers of tissue
Grouped coral polyps share a nervous system and digestive connection – this is due to the fact that the entire colony came from one original polyp.
Each coral polyp continues to lay down new CaCO3 beneath the polyp body so the entire coral colony continues to grow upward
The zooxanthellae housed inside the coral produce organic matter through photosynthesis
If zooxanthellae are supplied with enough light, they can feed the coral completely
Coral possess nematocysts to sting potential prey that come within reach of the tentacles
Coral can also feed using extensions of the gut wall called mesenterial filaments These filaments secrete digestive enzymes.
The coral can extend the mesenterial filaments with its enzymes allowing the coral to feed and digest food outside the body
Conditions Required for Reef Growth -Hard Substrate -Light Optimal -Narrow temperature range -Narrow salinity range -Low sediment load in water -Low pollution -Narrow range of pH
Corals reproduce both sexually and asexually
Asexual reproduction in corals allows for the growth of buds from a single polyp
Sexual reproduction in coral results in the creation of a planula larvae that is able to ride on the water currents to a new environment
Light must be able to penetrate the water to the depth of a coral to allow the symbiotic zooxanthellae to photosynthesize
Corals are mostly found on continental shelves, near islands or on seamounts due to this light/depth dependency
Reef building (hermatypic) corals tolerate a narrow temperature range compared with most marine organisms
Corals can only reproduce and grow if water temperatures are over 68 degrees F
water temperatures above 86 degrees (or higher in some species) causes coral stress. This can lead to “bleaching,” an expulsion of zooxanthellae from the coral polyp.
Poor water quality, increased sediment in water column, wave stress or disease can also cause bleaching
Widespread bleaching often occurs as a result of events such as El Nino (increased water temps) and hurricanes
Corals normally do not exist near areas where rivers deliver large amounts of freshwater to the marine environment because of salinity requirement (35ppt)
Corals do not normally grow in areas where wave action is high This is due to the fact that heavy wave action results in the suspension of sediments in the water column
Taller, more branching coral tend to be more common in shallower areas of the reef due to intense competition for space and light
Flatter coral forms tend to be more common in deeper areas of the reef; this probably assists with capturing all possible light available.
Scleractinian corals are the main reef builders. Produce a calcerous skeleton. Most have zoooxanthellae.
Soft corals non reef builders. - Most have zooxanthellae , calerous sksleton.
Gorgonians sea fans and sea whips. Skeleton of protein.
Fringing Reefs -Simplest and most common form of reefs -tropical waters -These reefs develop as narrow strips along the shore -consist of an inner reef flat and an outer reef slope
Growth of fringing reefs are normally fairly high on the reef slope and especially at the reef crest
Coral growth is slower on the reef flat due to runoff from land which includes sediment, freshwater and pollution
Barrier Reefs grow along the shore or may be farther from shore. They are different from fringing reefs by the presence of a deep lagoon between the shore and the reef
Belize barrier reef is the 2nd largest barrier reef in the world
Waves often wash sediment onto the back reef slope or reef flat which causes reduced coral growth in this area
Enough sediment may accrue to form small islands on the reef. These islands are called keys in the US or cays elsewhere
Coral growth is normally the highest at the reef crest or just below the crest on the fore-reef slope
The Great Barrier Reef is considered the largest reef structure in the world with regards to total coral area. -The length of the reef systems exceeds 1200 miles
Atolls a circular reef structure surrounding a central lagoon
Sand cayes may be a part of the atoll structure
Atolls form when a volcanic island is formed -The coral begins as a fringing reef around the newly formed island -Eventually, the island disappears below the water’s surface, leaving only the outer band of coral surrounding a lagoon
Atolls possess a reef flat and inner and outer reef slopes
The two largest atolls are in the Maldives (Indian Ocean) and the Marshall Islands (Pacific)
Patch reefs relatively small, isolated coral reefs found between the shore and barrier reef
Cyanobacteria present on the reef are able to fix nitrogen which is then available to other reef inhabitants who feed on the cyanobacteria
Many coral reef inhabitants can deter predation by producing toxic or foul tasting chemicals – this is common in soft corals and sponges
Coralline algae as well as other organisms grow in an encrusting form that is difficult to feed upon (tissue layer is VERY thin)
Corals may feed directly or sting one another if they contact each other
Created by: awahay
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