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Relate the variations in altitude of oolitic grainstone shoals that were deposited during the last interglacial (MIS 5e) to oscillations in sea level during the last highstand.  Test the hypothesis that oscillations of sea level produce extensive lateral accretion of ooid shoals by examining the evolution of the Miami Oolite.

Title
Influence of Sea-Level Oscillations During Highstands on Pleistocene Carbonate Shoals (Year 2)
Contributor
Caglar H. Usdun
Gregor P. Eberli
Donald F. McNeill
Date
2013
System Control No.
FI15060941_00001
Subject
Climate Change
Sea Level
Oolite
Subject (Geographic)
Miami (Fla.)
Type
Text
Language
English
Holding Institution
Florida International University Libraries. Government Resources and Information Department
Owning Institution
Florida International University
Collection Information
Florida Documents Collection; South Florida Collection
Usage Statement
Please contact the owning institution for licensing and permissions. It is the user's responsibility to ensure use does not violate any third party rights.
Record Appears in
Florida International University Libraries > FIU Government Resources and Information Department > FIU Government Resources and Information Department
Florida International University Libraries > FIU Government Resources and Information Department > Florida Documents Collection
Florida International University Libraries > FIU Government Resources and Information Department > South Florida Collection
Florida International University > Sea Level Rise
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