Sea Level and Reefs in Hawaii. Reefs 30 0 N and 30 0 S, shallow sunlight seas.
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Transcript of Sea Level and Reefs in Hawaii. Reefs 30 0 N and 30 0 S, shallow sunlight seas.
Sea Level and Reefs in Hawaii
Reefs
300 N and 300S, shallow sunlight seas
Reef Types
•Barrier Reefs•Fringing Reefs•Atolls•Patch Reefs
Reef Evolution
Methods
• Drilling
• Ecosystem surveys
• Dating (C14 & 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 shearingswell events governthe geologic record
Low energy~5-20 m
Porites compressabranching
Moderate energy~2-8 m
Porites lobatamassive
High energy~0-2 m
Porites lobataencrusting
Shallow, high energy~0-5 m
Porolithon sp.
High energy~2-10 m
Pocillopora meandrinastout 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 SITEHALE 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
Encrustingcoral-algalbindstone
Mixedskeletalrubble
Massivecoral
framestone
Unconsolidatedfloatstone
High energy Moderate energy Low energy
Typical facies
Rudstone Bindstone Grainstone Framestone Wackestone
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