chapter 14 part 2 coral reefs other reef builders conditions for reef growth coral reproduction...
TRANSCRIPT
Chapter 14Part 2
Coral Reefs
Other Reef BuildersConditions for Reef Growth
Coral ReproductionKinds of Reefs
Reef Builders
• Hermatypic corals• Coralline algae (Porolithon sp., Lithothamnion
sp.)• Halimeda sp.• Sponges• Foraminifera • Stromatolites
Coralline Algae• Porolithon sp., Lithothamnion sp.• Red algae that deposit CaCO3
• Hold reef together – keep it from washing away
• Algal ridge on outer edge of many reefs – protects reef from wave action
• Grow over and cement sediment that settle on corals
Halimeda sp.• Calcareous green alga• Deposits CaCO3 in tissues for support and to
deter predators• Remnants of Halimeda accumulate on reefs
and can be bound by encrusting organisms• Microcosm of diversity
www.turtles.org www.nceas.ucsb.edu
More Halimeda
Sponges• Bind sediments into place
www.johneasley.com
Foraminifera• Eukaryotic protists• CaCO3 shells
• Benthic, but a few are planktonic• Some have endosymbiotic algae• Bioindicator
www.proprofs.com
www.wikipedia.com
Stromatolites• Cycling of microbial communities (cyanobacteria)
and sediment• 3.5 billion years old (Earth is 4.5 billion yrs old!)• Not common today – Exuma, Bahamas• Rich source of fossil information
www.flickriver.com www.stromatolite.info
Highbourne CayExumas, Bahamas
Conditions for Reef Growth
• Hard bottom • Shallow water (< 50 m) with bright sunlight• Clear water• Warm water (> 20°C)
Coral Reproduction• Sexually– Egg + Sperm = Planula– Mostly hermaphroditic– Self fertilization (egg fertilized before released)– Broadcast spawners– What are advantages to mass spawning?
Coral Planula
G.Spencer
Coral Spawning
NOAA video BBC video
Coral Reproduction• Asexually– Fragmentation– Budding– Fission (esp. Fungiidae)
www.wikipedia.com
Budding
The distribution of coral reef communities p. 304
Bioerosion
• Erosion caused by living organisms• Who causes bioerosion?
fw.dpnr.gov.vi
www.coral.org
Bioerosion
• Epilithic organisms– Remain at surface of the calcareous substrate, where they
rasp, scrape, and/or etch the surface. – The majority of damage occurs during algal grazing. – Browsers consume plant material above the substrate – Grazers consume plant material down to, and sometimes
below, the surface of the substrate.• Grazers often consume quantities of coral skeleton as well as the
invertebrates associated with it and inflict much more damage than browsers. Neither grazers nor browsers usually have a great influence on strength of the greater coral structure (Kleemann 2001)
Bioerosion
Bioerosion• Endolithic organisms– Beneath the surface of the coral skeleton. – Bore for food or shelter. – Majority are suspension feeders
• Large borers, in particular polychaetes, are important in oxygenating the interior of coral structures to support smaller organisms.
• Internal bioeroding species degrade calcareous materials to fine textures
• External bioeroders generally erode to much coarser textures (Kleemann 2001)
Reef GrazersGrey angelfish and Blue tangs
Coral Reefs and Zonation3 main categories of reefs
1. Fringing – close to shore, high nutrients, high turbidity
2. Barrier – farther from shore, usually a lagoon between the reef and the shore
3. Atoll - Circular reef with central lagoon and possibly small islands formed on the reef.
Types of Coral Reefs: Fringing Reefs
• Simplest and most common• Rocky shorelines provide the best conditions for
fringing reefs
Upward growth of reef flats is limited by the tides. Figure 14.16
Barrier Reefs• Distinction between barrier and fringing reefs
sometimes unclear• Occur farther offshore• Presence of lagoons
Lady Musgrave Island Great Barrier Reef
Australia-trips.info
Spur and Groove formations• Debate about what causes it• Wind, waves, or both involved• Develop primarily on reef slopes that are
exposed to strong winds
Atolls
• Occur mostly in the Indo-West Pacific region• Practically no land around (no silt, little FW
runoff)• Spectacular coral growth and great water clarity
Atoll in Fiji
Atoll Formation
Typical Atoll Structure