LDR   01553nam^^22003253a^4500
001        FI15060941_00001
005        20171020111127.0
006        m^^^^^o^^d^^^^^^^^
007        cr^^n^---ma^mp
008        150618n^^^^^^^^xx^||||^o^^^^^|||^u^eng^d
245 00 |a Influence of Sea-Level Oscillations During Highstands on Pleistocene Carbonate Shoals (Year 2) |h [electronic resource].
260        |c 2013.
506        |a 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.
520 2    |a 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.
533        |a Electronic reproduction. |c Florida International University, |d 2015. |f (dpSobek) |n Mode of access: World Wide Web. |n System requirements: Internet connectivity; Web browser software.
650        |a Climate Change.
650        |a Sea Level.
650        |a Oolite.
651        |a Miami (Fla.).
700        |a Caglar H. Usdun.
700        |a Gregor P. Eberli.
700        |a Donald F. McNeill.
830    0 |a dpSobek.
830    0 |a Sea Level Rise.
830    0 |a Florida Documents Collection.
830    0 |a South Florida Collection.
852        |a dpSobek |c Sea Level Rise
856 40 |u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15060941/00001 |y Click here for full text
992 04 |a http://dpanther.fiu.edu/sobek/content/FI/15/06/09/41/00001/Usdun et al_2013_Influence of Sea-Level Oscellations During Hightstands on Pleistocene Carbonatethm.
997        |a Sea Level Rise


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