What is a Reef ? What is a Reef ? Coral Reef Geology Wilson Ramirez.

Slides:



Advertisements
Similar presentations
Investigation 3 Earth History Grade 6
Advertisements

“How can scientists determine the age of rocks and fossils?”
Paleontology Lab II CNIDARIANS.
Deltaic Depositional Systems
Rocks Formed by Surface Processes
UNIT 8 Surface process Biology and Geology 3. Secondary Education SEDIMENTARY BASINS.
Sedimentary Rocks Sedimentary rock is formed by weathering and erosion
 A rock is a naturally occurring solid mixture of one or more minerals, or organic matter  Rocks are classified by how they are formed, their composition,
Carbonate Rocks Carbonate rocks - limestones composed of calcite (CaCO3) or dolostones composed of dolomite (CaMgCO3). Carbonate rocks - limestones composed.
Chapter 3, Section 4 Rocks From Reefs Monday, December 14, 2009 Pages
Section 4: Rocks from Reefs.  Structure of calcite (calcium carbonate - CaCO 3 ) skeletons built up by coral animals in warm, shallow ocean water.
Vocabulary Foldable XIV.  The preserved remains, trace, or imprint of an ancient organism.
What do these abiotic factors have in common? What is different about them?
Corals. Staghorn coral (Acropora Cervicornis) exoskeleton.
Reefs Kinds of buildups Geographic distribution Reef requirements Community: diversity, environmental mediators, species of great affect The Sensitive.
Coral Reef Formation By Kurose.
Lecture 1 Reef Types and Formation. Bonaire. N.A.
Reefs Formation and Growth II. REEF CEMENTERS Encrusting Coraline Algae Encrusting Corals.
Sponge Reefs M. Krautter, U. Stuttgart Sponge Reef Project, 1999
“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.
1 EES 450: Sedimentary Geology CARBONATES - Rocks with > 50% carbonate materials; most abundant biochemical/chemical rocks. - Make up 20-25% of the sedimentary.
EXPLORING THE EARTH.
Geology of Australia and New Zealand, HWS/UC Plate Tectonics.
The Early Paleozoic Fauna: Ordovician radiation of the Cambrian survivors EPSC233 Earth & Life History (Fall 2002)
The Early Paleozoic Fauna: earliest animal reef formers
Kelly Lekan. Early Reefs First appearance of reefs around 570 million years ago. The first reefs formed were made of cyanobacteria. –Were found living.
Section 2: Precambrian Time and the Paleozoic Era
Geology Unit: Sea level history
1. Geological Oceanography Ocean Topography. Two Sad Jokes Q: Why don't aliens eat clowns. A: Because they taste funny. Two snowmen are standing in a.
Sedimentary Rocks 2006 Prentice Hall Science Explorer- Earth Science Liz LaRosa 2009http://
THE ROCK CYCLE THE ROCK CYCLE IS A GROUP OF CHANGES IN WHICH: Igneous rock can change into sedimentary rock or into metamorphic rock Sedimentary rock.
Types of Rock.
Geological Time Geology 12. Uniformitarianism “The present is the key to the past”- the fundamental principle that underlies most of geology. Put simply,
Sedimentary Rocks Chapter 3 Section 3. Sedimentary  sedimentum Latin for ‘settling’ Rock formed from compressed or cemented layers (DEPOSITS) of sediment.
The major landforms of advancing (depositional) coastlines
NATURAL THREAT ON CORAL REEFS Done by: The Reef Avengers.
Reef Carbonates.
Coral Reefs Coral reefs are similar to rain forests in that they are complex and diverse.
S E D I M E N T A R Y R O C K.
Earth History Sandstone & Shale Formation. Basin An area of relative low elevation where water and sediments collect.
The majority of reef building corals are found within tropical and subtropical waters. These typically occur between 30 north and 30 south latitudes. The.
Precambrian Time and the Paleozoic Era
Earth Science Notes ROCK TYPES: Igneous Metamorphic Sedimentary.
Geoscientists gather and interpret data about the Earth and other planets. They use their knowledge to increase our understanding of Earth processes and.
Principles of Geology Mr. Halfen Jan
Scientific revolutions
AIM: Introduce you to scientific study of oceans and seas
Introduction of Oceanography
Section 2: Precambrian Time and the Paleozoic Era
Sedimentary Rocks 2006 Prentice Hall Science Explorer- Earth Science
F3 KI 1c.
Section 2: Precambrian Time and the Paleozoic Era
Unit 14: The Future of Humanity
Intro to Oceanography.
Relative Age Dating What is it?
Section 2: Precambrian Time and the Paleozoic Era
Warm-Up: Thurs 4/17 Write What You Know!
Rocks Rock.
Types of Rock.
Section 2: Precambrian Time and the Paleozoic Era
Harry Williams, Historical Geology
How Old is Old? Geologic Time.
What are the characteristics of the Earth’s major aquatic communities?
Types of Rock Sedimentary Rock
Statistics for research and ecology
Tropical Reefs: Coral/Algal
April 24th/25th Notes 12.c: Adaptations
Geological Evidence Part 2
The World of Earth Science
Presentation transcript:

What is a Reef ? What is a Reef ? Coral Reef Geology Wilson Ramirez

 Mariners  Can I hit my keel on it (i.e., shallow)  Biologists  Biologically abundant and diverse assemblage  Geologists  Biologically built  Wave resistant  Stands above its surroundings Perspective….what is a reef?

 Mariners  Can I hit my keel on it (i.e., shallow)  Biologists  Biologically abundant and diverse assemblage  Geologists  Biologically built  Wave resistant  Stands above its surroundings Perspective….what is a reef? Canning Basin, Australia (Devonian) Palau, Oceania

Canning Basin, Australia (Devonian) Isla de Mona, Puerto Rico

A Geologist’s Reef

Reef Definition “the vast majority of of ancient reef deposits are comprised not of in-place, interlocking framework, but rather are loose assemblages with reef-building organisms ‘floating’ in a matrix of reef-derived debris” Hubbard (1997, p. 43 )

Reef Definition Stanley (2001) “Growth of biological framework on modern shallow reefs is rapid….” “…it is counterbalanced by highly destructive (recycling) processes…”

 Constructed of material of biological origin  Rigid structure, owing to either interlocked and in place framework elements or of re­worked framework elements bound together by secondary encrustation or cementation  Stands topographically above the surrounding seascape and, therefore, exerts at least local control on oceanographic processes  The majority of the framework elements were formed in an environment similar to the one in which they were ultimately deposited “Reef” definition

Tucker & Wright

A Geologic Reef  Rigid, & wave resistant  Elevated - affect local oceanography  Near sea level?

Let’s put this into a geological perspective… The reef is "apparent" i.e., no topography actually occurred in the past

An oyster bank is not wave resistant, but in time a thick sequence could result from upward layered accumulation. Stratigraphic reef

Topography at the time of deposition

Fossil reef with in place structural elements – Acropora palmata Ecologic reef accumulation

BIOHERM A B Question: What differences will we see at A versus B?

BIOSTROME e.g., a coral”carpet” No significant topography A B Question: What differences will we see at A versus B?

Biostrome vs. Bioherm No Original Relief Relief During Deposition

Coral Growth How do we get rigid, elevated structures?  Construction  Corals  Other calcifiers  Destruction  Fish  Urchins  Borers  Encrustation  Cementation

Corals Grow Corals Grow Reefs Accrete (or build) Reefs Accrete (or build) Sediment production and redistribution