Sea Level and Reefs in Hawaii. Reefs 30 0 N and 30 0 S, shallow sunlight seas.

Slides:



Advertisements
Similar presentations
Carbonate sediment supply on oceanic islands: A model and its applications Jodi N. Harney Charles H. Fletcher University of Hawaii Dept. of Geology and.
Advertisements

The Great Barrier Reef Reef Formation Age, Reef Building Processes and Current Reef Situation.
Holocene Reef Accretion, Southwest Molokai, Hawaii Mary Engels.
Chapter 14 Part 2 Coral Reefs Other Reef Builders Conditions for Reef Growth Coral Reproduction Kinds of Reefs.
-in reality, few reefs are dominated solely by corals, hence the term “coral” reef is often a misnomer. -corals are largest, most showy, obvious, easiest.
SEDIMENTS & SEDIMENTARY ROCKS
Chapter 8 – FROM SEDIMENT INTO SEDIMENTARY ROCK
Sedimentary rocks Geology 103. Making sediment Weathering = rock breakdown into smaller rock, or minerals, or chemicals Sediment = result of weathering.
Shallow Marine Carbonate
Introduction to Oceanography Physical Oceanography -Coastlines 2-
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.
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.
Marginal Marine and Open-Shelf Environments
Reef Architecture and Zones. Reef Architecture -Structure of a ‘Typical’ Caribbean Reef (Goreau)
1 EES 450: Sedimentary Geology CARBONATE MATRIX Matrix in a carbonate sediment consists of very fine grained carbonate material filling the interstices.
Coral Reefs – What is a coral reef? Habitat forming scleractinians Different types of reef – Symbiosis – Biogeography Controls on Biogeography – The value.
Coral Reefs Oasis of the Sea Coral Reefs.
Coral Reefs Warm, shallow, tropical ocean waters Warm, shallow, tropical ocean waters “Rainforest of the Sea” “Rainforest of the Sea” High production High.
Notes: Coral Reef.  Characteristics  Coral reefs are massive biological communities and geologic structures.  Made of Calcium carbonate  Corals –
Reefs Kinds of buildups Geographic distribution Reef requirements Community: diversity, environmental mediators, species of great affect The Sensitive.
Site establishment and baseline activities report of RARE sites
Coral Reefs. “Coral” is general term for several different types of cnidarians (phylum Cnidaria) that produce calcium carbonate skeletons (CaCO 3, a.k.a.
Cambridge Marine Science AS Level
Coral Reef Watch – In-situ Observations (Pacific).
PROF. ABDULKADER M. ABED UNIVERSITY OF JORDAN 20/11 CARBONATE DEPOSITIONAL ENVIRONMENTS Abdulkader M. Abed University of Jordan
Republic of Yemen Prepared By: Mr. Gamal Abdullah Nasser Coral Reefs in Yemen.

Coral Reef Zonation. Disclaimer The terms used to identify different reef zones are not based upon a uniform agreement among reef scientists. There are.
Lecture 1 Reef Types and Formation. Bonaire. N.A.
Geology of Central America. Earth 65 Million Years Ago.
Reefs Formation and Growth II. REEF CEMENTERS Encrusting Coraline Algae Encrusting Corals.
Sediments and Sedimentary Rocks © Houghton Mifflin 1998; N. Lindsley-Griffin, LAYERED ROCKS, PARIS CANYON, ARIZONA Geology Today Barbara W. Murck.
By Dustin Price , Nathan Blackmon , Josh Crawford , and Osmond Curtis
16. Sediment Transport in the Ocean Basins – In Development William Wilcock OCEAN/ESS
Sediments... are unconsolidated particulate materials that either precipitate from or are depo- sited by a fluid (e.g., water, wind); provide information.
Sedimentary Rocks Chemical Sedimentary Rocks Limestone Limestone Chert – Silica Chert – Silica Evaporites Evaporites Organic Rocks Organic Rocks Coal Coal.
Global distribution of coral reefs
Types of Corals Types of Reefs
“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.
Chemical Mechanisms of Disease Resistance in Hawai’ian Corals Deborah Gochfeld 1, Greta Aeby 2, Jesse Miller 1 1 National Institute of Undersea Science.
Description of Waves The simplest way of looking at waves is the concept of a wave as a harmonic oscillation. It can then be described by its: period.
Giant Avalanches and Mega-tsunami (not). N coast of E. Moloka‘i.
Chapter 7 Aquatic Ecosystems Environmental Science Spring 2011.
What Lies Beneath. Pre Solar Nebula—4.6 Billion yrs ago.
Coral reefs.
Coral Reef Habitat. Reef Zones of the Coral Reef Habitat Reef Lagoon Beach Beaches are found along the shores of all Hawaiian islands. Most of Hawaii’s.
The Sea Floor. Origin of the Ocean Water vapor released during degassing of early earth –volcanism Salt from chemical weathering.
Continental Margins and Ocean Basins. Continental Margins Three Main Divisions  Continental shelf  Continental slope  Continental rise.
Reef Carbonates.
Carbonate Sedimentation Processes. The shallow marine “carbonate factory” differs from siliciclastic sedimentation in several fundamental ways: 1.Clastics.
Carbonates The other white meat….. Processes that affect compositionally controlled marine facies 1.Influx of terrigenous sediment 2.Rate of organic productivity.
Lesson 2: Wonders of coral Become an ocean explorer (ages 11-14)
GEOL 332 LECTURE 18 TODAYS MATERIAL:
 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 
Cool-Water Carbonates. Iceberg rainout Muddy limestone Dropstone Polar carbonates associated with ice sheets and icebergs Lower Permian, Tasmania.
Coral Bleaching Chrissy Covington October 14, 2004 Introduction to Coastal Management Dr. Hosier & Dr. Cleary.
Figure Figure CO 14 Figure 14.1 Dinoflagellates (single-celled algae): symbionts in corals (zooxanthellae) live inside the cells of corals.
Coral Reefs part 2 for website. Sand islands form (sand cays)
Biodiversity is the way in which plants and animals co-exist in the ecosystem. Coral Reefs form some of the most productive ecosystems. They provide shelter.
Tropical Marine Biology
Conditions necessary for reef development
By: Martin Arcibal and Teddy Lagrosa
Proceedings of the Yorkshire Geological Society
Coral reefs.
Atlantic Ocean Habitat
Giant Avalanches and Mega-tsunami (not)
Chapter 14 Coral Reefs.
Presentation transcript:

Sea Level and Reefs in Hawaii

Reefs

30 0 N and 30 0 S, shallow sunlight seas

Reef Types Barrier Reefs Fringing Reefs Atolls Patch Reefs

Reef Evolution

Methods Drilling Ecosystem surveys Dating (C 14 & U-series) Carbonate petrography

Holocene reef and dune Leahi reef and dune Waimanalo reef and dune Waianae reef None recognized ? Kaena Stand ? Carbonate System of Oahu

Ecosystem surveys Rotary cores

Ecosystem surveys

Wireline Drilling the Island Shelf

Large, bottom shearing swell events govern the geologic record

Low energy ~5-20 m Porites compressa branching Moderate energy ~2-8 m Porites lobata massive High energy ~0-2 m Porites lobata encrusting Shallow, high energy ~0-5 m Porolithon sp. High energy ~2-10 m Pocillopora meandrina stout branching Shallow, high energy ~0-10 m Montipora sp.

LONO HARBOR HALE O LONO SITE: -High wave exposure -Sparse coral cover -Shore parallel ridge and runnel morphology HIKAUHI SITE -Medium wave exposure -Abundant coral cover -Shore normal spur and groove morphology HIKAUHI SITE HALE O LONO SITE High bed shear

Modern Ecosystem Investigations: Results Modified from Storlazzi et al. (in press) Study Sites

Modern Ecosystem Investigations: Results Modified from Storlazzi et al. (in press)

Typical facies Branching coral framestone Encrusting coral-algal bindstone Mixed skeletal rubble Massive coral framestone Unconsolidated floatstone High energy Moderate energy Low energy

Typical facies Rudstone BindstoneGrainstoneFramestoneWackestone

Bindstone (algal pavement) Angular silt to pebble clasts (coral and algal) encrusted and bound by coralline algae, encrusting foraminifers and bryozoans; Extensive micritization of skeletal grains; Microcrystalline Mg- Calcite fills inter- and intraparticle pores

Framestone (reef framework) Intraskeletal pores lined by aragonitic accicular cement; Pores filled by peloidal Mg- calcite grading out to silt- sized skeletal debris; Thick crusts of coralline algae, encrusting foraminifers (Homotrema, Planorbulina?), bryozoans and serpulids