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AICE Marine Science Unit 5

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1 AICE Marine Science Unit 5
Coral Reefs & Lagoons AICE Marine Science Unit 5

2 What are corals? Invertebrate marine animal
A polyp that begins to form an exoskeleton CO2 & Ca in the water to make calcium carbonate (CaCO3) aka limestone Sessile – immobile Form colonies

3 Habitat Usually between 30O N & S latitudes Usually in Photic Zone
Clear, warm, tropical, shallow

4 Coral Reef Growth Needs
Lots of light (low to no turbidity) Depth between 0-20M (to deep = not enough light) Temperatures averaging 23°-25°C (70°-85°F) Most coral cannot survive below 16° C Must have Salinity between 34-37ppt Substrate is a limiting factor

5 Reef-building Corals (shallow):

6 Reef-building Corals:
Hermatypic Corals = reef-building/shallow Kingdom Animalia Phylum Cnidaria Class Anthozoa Subclass Zoantharia Order Scleractinia Primarily made up of small individual coral polyps Skeleton made up of calcium carbonate

7 Reef-building Corals:
Have a mutualistic symbiotic relationship with zooxanthellae Dinoflagellate that lives within their tissues Corals get energy & O2 & wastes removed Zooxanthellae gets products for photosynthesis& a “safe” home Fun Fact: Zooxanthellae is what gives coral its color!

8 Coral Polyps http://youtu.be/wbNeIn3vVKM

9 3 Coral Reef formations:
1 Fringing = Usually closest to shoreline (sometimes called finger reef); most common (like a skirt) Barrier = Separated from mainland by a lagoon Atoll = Ring of sand, coral, & land w/ central lagoon; oldest reef formation (sinking volcanic island) 2 3

10 Fringing

11 Barrier

12 Atolls Bikini Atoll Belize

13 Darwin-Dana-Daly Theory of Atoll Formation
Oceanic volcano emerges from sea & forms an island Reef-building corals build & surround island (fringing) Island sinks & lagoon forms between island & reef (barrier) Island disappears below sea, leaving ring of small islands w/ lagoon in center (atoll)

14 Darwin-Dana-Daly Theory
Coral atolls 1st proposed by Charles Darwin HMS Beagle (Nov – Apr 1836) Supported and modified by 2 geologists James Daly Reginald Dana

15 Darwin-Dana-Daly theory of coral atoll formation
1. Oceanic volcano emerges from sea surface and forms an island Colonized by reef-building corals

16 Darwin-Dana-Daly theory of coral atoll formation
2. Growth of corals forms a fringing reef around the island Fringing reef – coral structure attached to the mainland or continental islands Island begins to sink slowly Coral growth continues

17 Darwin-Dana-Daly theory of coral atoll formation
3. Island continues to sink Barrier reef forms with lagoon around reef and island Barrier reef - reef separated from a mainland or island shore by a deep channel or lagoon

18 Darwin-Dana-Daly theory of coral atoll formation
4. Island eventually disappears below sea surface Atoll - consists of a ring of small islands Shallow lagoon in center

19 Atoll Formation Fringing reef can take 10,000 years to form
Atolls up to 30 my Coral – tan and purple

20 Evidence Data from deep drilling on coral atolls
Bikini Atoll (Pacific Ocean) As depth of corals increased, age of corals also increased Fossil corals dated 50 myo and found 1200 m deep Grown on underlying volcanic rock Shallow corals found at deep depths!

21 Atoll Formation, an animation:
Thanks for animation NOAA

22 Stop Day 1


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