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Coral Reefs

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Page 1: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

Coral Reefs

Page 2: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

Introduction

• Limestone is left over when animals grow and die.

• Calcium carbonate is the basis for coral formation.

• As we will see, coral production exhibits huge impacts on ecosystem diversity and success.

Page 3: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

Requirements for Reef Formation

• High Light Levels

• High Water Transparency

• Water Temperatures > 20°C (68°F)

• Hard Substrate for Attachment

• Good water circulation

Page 4: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

Coral :

• Hard (Stony, true) corals build the reef by extracting calcium carbonate from the ocean water.

• They create a home in which primary producers can live.

Page 5: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

What is Coral?? Animal, Vegetable, Mineral?

Coral are actually a special group of cnidarians, the same family as jellyfish!!

Page 6: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

Hermatypic vs. Non-Hermatypic Corals

• Hermatypic Corals (a) : Corals that form large colonies called reefs.

• Ahermatypic Corals (b) : Corals that are solitary or form small colonies (often lack zooxanthellae and do not help build reefs).

a. brain coral (Diploria) b. Mushroom coral (Fungia)

Page 7: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

Coral remain closely connected.

Zooxanthellae, single-celled photosyntheticalgae work within the coral to help feed itthrough photosynthesis.

As a result of this symbioticrelationship, many coralsdon’t need to seek food.

This added nutrition also helps corals to build reefsmuch faster!

microscopic view of zooxanthellae)microscopic view of zooxanthellae)

Page 8: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

Mutualism Between Corals and Zooxanthellae

• Coral Polyp-

– Provides a home for the zooxanthellae.

– Provides nitrates and phosphates.

– Gives off CO2.

– Zoox helps coral eat and get more sunlight

Page 9: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

Here is a good example of a live coral.

Page 10: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

Obviously, the one on the left needs help!!

Page 11: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

Coral take on many shapes!!

Page 12: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

Reefs grow when calciumcontaining sediments are deposited in spaces between coral.

As encrusting coraline algae “glues” the sediments together,new “live rock” is formed.

Page 13: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

Once this green algae dies, 95% of what remains will be sediment and real estate for new coral colonies.

Coral benefits from the death of other organisms.

Page 14: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

Coral exhibit limited range in growth patterns.

Page 15: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

Without proper light and temperature,coral dies (bleaches).

It only takes 1-2 degrees in some cases.

How does global warming effect this trend?

Page 16: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

From this…

Page 17: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

To this….

Temperature increases and competition from red algae have killed much of this coral reef.

Page 18: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

3 types of Coral Reefs

• Fringing reefs- The most common type of reef, grows seaward directly from the shore. They form borders along the shoreline and surrounding islands.

• Atoll reefs- form from fringing reefs built on a sunken volcanic island. Usually circular or oval in shape, with an open lagoon in the center.

• Barrier reefs- are similar to fringing reefs in that they also border a shoreline; however, instead of growing directly out from the shore, they are separated from land by an expanse of water. This creates a lagoon of open, often deep water between the reef and the shore.

Page 19: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

Fringing Reefs- Growth on reefs are often limited by tidal action.

Page 20: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

Disease is another major factor limiting growth. Here is an example of elkhorn coral (Acropora palmata) infested by “white band disease.”

Page 21: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

Barrier Reefs

Page 22: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

An excellent example of a Pacific barrier reef.

Page 23: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

The Great Barrier Reef

Page 24: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

Atoll Reefs: Volcanic Left-overs!

Page 25: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

Food Webs: Same concept, more complexity

Page 26: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

Coral Fights??

Yes!

Just like other animals competing for space, coral attack each other if they come into close contact.

Usually they just over grow one another, but some actually poison the others out!

Page 27: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

Soft corals are fast growers, making them excellent competitors.

Page 28: Coral Reefs. Introduction Limestone is left over when animals grow and die. Calcium carbonate is the basis for coral formation. As we will see, coral

Is there perfect harmony on reefs? Not really, most animals on reefs compete daily for everything, from food to mating opportunities.