Coral Reefs Warm, shallow, tropical ocean waters Warm, shallow, tropical ocean waters “Rainforest of the Sea” “Rainforest of the Sea” High production High.

Slides:



Advertisements
Similar presentations
Phylum Cnidaria: Jellies, anemones, corals and hydroids
Advertisements

THE CHEMISTRY OF CORAL BLEACHING. WHAT IS A CORAL? CORALS ARE MARINE INVERTEBRATES (ANIMALS) THEY CAN TAKE MANY SHAPES! THEY USUALLY LIVE IN COLONIES.
Chapter 15 Animals of the Benthic Environment
Symbiosis between Zooxanthellae & Corals By Mark Mergler.
What is coral? It’s a living organism! It is an invertebrate 2 different types:  Reef Building: Hermatypic  Solitary: Ahermatypic Coral is cousins to.
Introduction to Oceanography Physical Oceanography -Coastlines 2-
Part I Section 5.  Invertebrate marine animal  A polyp that begins to form an exoskeleton ◦ CO 2 & Ca in the water to make calcium carbonate (CaCO 3.
Coral Reefs. Introduction Calcium carbonate (CaCO 3 ) anyone?? Limestone is left over when animals grow and die. This carbon containing molecule is the.
Coral Reefs Oasis of the Sea Coral Reefs.
Introduction to Coral Reefs Coral reefs are amazing, natural wonders that live in the warm waters of the tropics, providing habitat for thousands of marine.
Notes: Coral Reef.  Characteristics  Coral reefs are massive biological communities and geologic structures.  Made of Calcium carbonate  Corals –
Coral Reefs.
Coral Reefs By: Alica Majercinova Geography 12.
-Gautam Sanka. What is a Coral? Coral is an animal in the phylum Cnidaria and class Anthozoa Coral exists in the ocean as polyps which are a form of life.
Coral Reefs. Facts about Coral Reefs Largest living thing on Earth Covers less than 1% of the Earth’s Surface Needs sunlight to grow.
Coral Reefs.
Coral Reefs and Human Activity Keerthi Potluri and Tina Stancheva Human Nature, Technology and the Environment April 15, 2003.
Chapter 14 Coral Reefs.
Coral Reefs. “Coral” is general term for several different types of cnidarians (phylum Cnidaria) that produce calcium carbonate skeletons (CaCO 3, a.k.a.
Coral Reef Formation By Kurose.
CORAL REEFS “Rainforests of the Oceans” By: Jaime Denny and Mary Wood.
Coral Reefs.
Cambridge Marine Science AS Level
© 2007 W.W. Norton & Company, Inc. Intro. to Ocean Sciences, 2 nd Ed.
Coral Reefs. Scleractinian corals Phyllum Cnidaria –Class Anthozoa Subclass Zoantharia –Order Scleractinia Only polyp phase (no medusae) Colonial organisms.
Coral Reefs. What is a coral reef? Ecosystem Community of living organisms Exist since millions of years The reefs that we see today had to grow for around.
By: David Anderson. Structure of a Coral Each coral is lined with multiple polyps which are individual animals that make up the coral. Each polyp has.
Coral Reefs Shipley Marine Bio Summit High School
Haley Sullivan, Mathilde Perez-Huet. Plasmodium Protists: apicomplexans Parasitic Release sporozoites into hosts Complex life cycles
“The Forests of the Sea” Fringe 1/6 th of the world’s coastlines Largest reef is the Great Barrier Reef in Australia (2000km or 1200mi) Member of the.
Kelly Lekan. Early Reefs First appearance of reefs around 570 million years ago. The first reefs formed were made of cyanobacteria. –Were found living.
Coral Reefs.  Calcium carbonate (CaCO 3 ) makes up coral reefs.  Limestone is left over when animals grow and die.  This carbon containing molecule.
Honors Marine Biology Module 11 Coral Reefs. Class Challenge The Best Joke.
Diversity and Distribution of coral reefs By Robyn and Taylor.
Chapter 7 Aquatic Ecosystems Environmental Science Spring 2011.
1. Coral Atoll 2. Fringing Reef 3. Barrier Reef. CORAL ATOLL Isolated ring shaped reef rising out of deep water.
Corals Rainforests of the ocean. What does this map show?
Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. Chapter 14 Lecture Slides.
Coral Reefs. Facts about Coral Reefs Largest living thing on Earth Covers less than 1% of the Earth’s Surface Needs sunlight to grow.
Coral Reefs Marine Biology Unit #9.
Coral Reefs. What is a Coral Reef? CaCO 3 from living things Reef builders –Corals –Algae –Sponges –Bryozoans –Shells.
WARNING THIS PRESENTATION CONTAINS CONTENTS AND INFORMATIONS STRICTLY FOR ADULTS ALSO.
 Invertebrate marine animal  A polyp that begins to form an exoskeleton ◦ CO 2 & Ca in the water to make calcium carbonate (CaCO 3 ) aka limestone 
Coral Reefs Coral reefs are similar to rain forests in that they are complex and diverse.
Coral Reefs By Laura Leyda and Jennifer EnglerBy Laura Leyda and Jennifer Engler.
Coral Reefs & Lagoons Part 2
Coral Reef Ecology Types of Coral Reefs Found in the Florida Keys Outer Bank Spur and Groove Reef Outer Bank Spur and Groove Reef –Found on the outer.
© 2014 Pearson Education, Inc. Chapter 15 Animals of the Benthic Environment Rocky and sandy shores Coral Reef Deep Sea.
Figure Figure CO 14 Figure 14.1 Dinoflagellates (single-celled algae): symbionts in corals (zooxanthellae) live inside the cells of corals.
Coral Reefs. Georgia’s Gray’s Reef Gray's Reef is not a coral reef. It is not built by living hard corals as tropical reefs are. Instead it is a consolidation.
 Cnidarians:  Animals in the phylum  Cnidaria  Radial symmetry  Tissue-level organization  Tentacles with nematocysts  Stinging cells  Life stages:
The majority of reef building corals are found within tropical and subtropical waters. These typically occur between 30 north and 30 south latitudes. The.
Coral Reefs part 2 for website. Sand islands form (sand cays)
Invertebrates Phylum Phylum Cnidaria Cnidaria. Class Cubozoa Some are among the most dangerous marine animals. Some are among the most dangerous marine.
CORAL REEFS.
Coral Reefs Outcome: To understand where coral reefs are distributed, examine the symbiotic relationships within coral reefs, compare/contrast the three.
Pg. 76 RTW: What is an advantage & disadvantage of clumped dispersion?
Coral Reefs.
Marine Habitats.
Chapter 14 Coral Reefs Copyright © 2016 McGraw-Hill Education. All rights reserved. No reproduction or distribution without the prior written consent of.
AICE Marine Science Unit 5
The individual coral polyps
8:29 REEF HABITATS Coral reefs are only found on western boundary currents where water is warm, shallow, and clear with good light. The coral reef is.
By: Martin Arcibal and Teddy Lagrosa
Coral Reef Degradation
Coral reefs.
Chapter 14 Coral Reefs.
Symbiosis between Zooxanthellae & Corals
…and the organisms that build them.
Coral reefs.
Presentation transcript:

Coral Reefs Warm, shallow, tropical ocean waters Warm, shallow, tropical ocean waters “Rainforest of the Sea” “Rainforest of the Sea” High production High production High organismal diversity High organismal diversity High structural diversity High structural diversity Provides food & shelter to many organisms Provides food & shelter to many organisms Provides natural products Provides natural products Source of many drugs and chemicals Source of many drugs and chemicals

Phylum? Phylum? Cnidaria Cnidaria Includes? Includes? jellyfish, sea anemones, corals jellyfish, sea anemones, corals Key shared characteristic? Key shared characteristic? Cnidocytes or “stinging cells” Cnidocytes or “stinging cells” Colony of polyps Colony of polyps Calcium carbonate skeleton Calcium carbonate skeleton Key players

Process Coral growth is slow… Coral growth is slow… ~ 1 cm / year ~ 1 cm / year Other organisms help Other organisms help Zooxanthellae Zooxanthellae single-celled algae single-celled algae See Fig. 14.1, Castro & Huber See Fig. 14.1, Castro & Huber symbiotic relationship symbiotic relationship Coralline algae Coralline algae Multicellular Multicellular Produces its own CaCO 3 skeleton Produces its own CaCO 3 skeleton Adds to reef and helps “glue” it together Adds to reef and helps “glue” it together

Types of Coral Reefs Fringing reefs Fringing reefs Shallow coastal waters Shallow coastal waters Vulnerable to sediment, freshwater runoff, & human disturbance Vulnerable to sediment, freshwater runoff, & human disturbance Reef flat Reef flat Wide & influenced by low tides Wide & influenced by low tides Reef slope Reef slope Dense with corals Dense with corals

Barrier reefs Barrier reefs Parallel the coast Parallel the coast Separated by lagoon Separated by lagoon Inner reef (back reef slope) protected Inner reef (back reef slope) protected Outer reef slope Outer reef slope Dense Dense Spur & Groove Spur & Groove Windward side Windward side Shock absorbers Shock absorbers

Atolls Circular reef left by subsiding island Circular reef left by subsiding island Windward side Windward side Lots of wind and waves Lots of wind and waves Tradewinds (30 0 to 0 0 ) Tradewinds (30 0 to 0 0 ) Spur & groove Spur & groove Coralline algae Coralline algae Leeward side Leeward side Sheltered Sheltered Begins as fringing Begins as fringing Volcanic island Volcanic island Island subsides Island subsides Creates barrier reef Creates barrier reef Subsiding continues Subsiding continues Ring left behind Ring left behind Atoll Atoll

Limitations of Coral Reefs Shallow water Shallow water Hard substrate Hard substrate Limited temperature range Limited temperature range ~20 – 32 Celsius (68 – 90 Fahrenheit) ~20 – 32 Celsius (68 – 90 Fahrenheit) Sensitive to lowered salinity Sensitive to lowered salinity Sensitive to human impacts Sensitive to human impacts Pollutants Pollutants Fuels, waste, sunscreen Fuels, waste, sunscreen Increased run-off from population growth Increased run-off from population growth eutrophication eutrophication Coral bleaching? Coral bleaching? Loss of zooxanthellae Loss of zooxanthellae Increased turbidity (sediments) Increased turbidity (sediments) Decreased salinity Decreased salinity Weather events Weather events Hurricanes Hurricanes Cyclones Cyclones