FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2043270326> ?p ?o ?g. }

• W2043270326 endingPage "72" @default.
• W2043270326 startingPage "58" @default.
• W2043270326 abstract "On Grand Cayman, the unconformity bounded Units A to F in the Ironshore Formation represent repeated cycles of deposition and subaerial exposure that were associated with the dramatic oscillations in sea levels that characterized the Middle to Late Pleistocene. Montastrea annularis and Acropora palmata, the dominant corals found in Units A to F in the Rogers Wreck Point area and offshore George Town area, reflect these changes with their complex mosaics of marine (aragonite cements, bioerosion, internal sediments) and meteoric (calcitization of coral skeleton, dissolution) diagenetic features. The distribution of the diagenetic fabrics throughout this sequence, however, is not predictable. The randomness in the degree of skeletal calcitization is shown by the lack of systematic variation in calcitization from Units A to F, and the fact that the degree of skeletal calcification in M. annularis is higher than that in A. palmata in the Rogers Wreck Point area but less than in A. palmata in the George Town cores. The stable isotope compositions (δ13C, δ18O) of the corals from Units A to F plot along the same trend line with their positions on that trend reflecting the amount of meteoric diagenesis they have undergone. The variable styles and degrees of diagenesis evident in the corals from the Ironshore Formation reflect (1) the variable impact of intrinsic (e.g., skeletal architecture, porosity of coral) and extrinsic (e.g., sea level, climate) factors during each phase of diagenesis, and (2) temporal effects associated with the diagenetic overprinting that took place during each successive phase of diagenesis. This means that the diagenetic fabrics are not stratigraphically ordered and that it is impossible to correlate specific diagenetic phases with specific sea level lowstands or highstands." @default.
• W2043270326 created "2016-06-24" @default.
• W2043270326 creator A5046895582 @default.
• W2043270326 creator A5055360910 @default.
• W2043270326 date "2013-03-01" @default.
• W2043270326 modified "2023-10-16" @default.
• W2043270326 title "Temporal and spatial variations in the diagenetic fabrics and stable isotopes of Pleistocene corals from the Ironshore Formation of Grand Cayman, British West Indies" @default.
• W2043270326 cites W121857346 @default.
• W2043270326 cites W1507360251 @default.
• W2043270326 cites W1915797674 @default.
• W2043270326 cites W1964165210 @default.
• W2043270326 cites W1965355594 @default.
• W2043270326 cites W1967422998 @default.
• W2043270326 cites W1974400428 @default.
• W2043270326 cites W1975813038 @default.
• W2043270326 cites W1984607107 @default.
• W2043270326 cites W1994027801 @default.
• W2043270326 cites W1997110050 @default.
• W2043270326 cites W2002115922 @default.
• W2043270326 cites W2005768058 @default.
• W2043270326 cites W2006521535 @default.
• W2043270326 cites W2008205524 @default.
• W2043270326 cites W2012688130 @default.
• W2043270326 cites W2015950805 @default.
• W2043270326 cites W2020547979 @default.
• W2043270326 cites W2020610093 @default.
• W2043270326 cites W2027605790 @default.
• W2043270326 cites W2029285401 @default.
• W2043270326 cites W2031262675 @default.
• W2043270326 cites W2033667127 @default.
• W2043270326 cites W2037976105 @default.
• W2043270326 cites W2040967573 @default.
• W2043270326 cites W2042457374 @default.
• W2043270326 cites W2044094077 @default.
• W2043270326 cites W2045706691 @default.
• W2043270326 cites W2047428375 @default.
• W2043270326 cites W2048291047 @default.
• W2043270326 cites W2051973454 @default.
• W2043270326 cites W2055312078 @default.
• W2043270326 cites W2055929527 @default.
• W2043270326 cites W2059369040 @default.
• W2043270326 cites W2059723891 @default.
• W2043270326 cites W2081845564 @default.
• W2043270326 cites W2082388053 @default.
• W2043270326 cites W2082460606 @default.
• W2043270326 cites W2090942757 @default.
• W2043270326 cites W2093548232 @default.
• W2043270326 cites W2100889397 @default.
• W2043270326 cites W2106398178 @default.
• W2043270326 cites W2108042074 @default.
• W2043270326 cites W2110784760 @default.
• W2043270326 cites W2119464175 @default.
• W2043270326 cites W2120528048 @default.
• W2043270326 cites W2131740309 @default.
• W2043270326 cites W2139933207 @default.
• W2043270326 cites W2152247912 @default.
• W2043270326 cites W2156776444 @default.
• W2043270326 cites W2164445499 @default.
• W2043270326 cites W2168628209 @default.
• W2043270326 cites W2170060025 @default.
• W2043270326 cites W2331683539 @default.
• W2043270326 cites W2332757869 @default.
• W2043270326 cites W4238125377 @default.
• W2043270326 doi "https://doi.org/10.1016/j.sedgeo.2013.01.001" @default.
• W2043270326 hasPublicationYear "2013" @default.
• W2043270326 type Work @default.
• W2043270326 sameAs 2043270326 @default.
• W2043270326 citedByCount "17" @default.
• W2043270326 countsByYear W20432703262013 @default.
• W2043270326 countsByYear W20432703262014 @default.
• W2043270326 countsByYear W20432703262017 @default.
• W2043270326 countsByYear W20432703262019 @default.
• W2043270326 countsByYear W20432703262020 @default.
• W2043270326 countsByYear W20432703262021 @default.
• W2043270326 countsByYear W20432703262022 @default.
• W2043270326 countsByYear W20432703262023 @default.
• W2043270326 crossrefType "journal-article" @default.
• W2043270326 hasAuthorship W2043270326A5046895582 @default.
• W2043270326 hasAuthorship W2043270326A5055360910 @default.
• W2043270326 hasConcept C111368507 @default.
• W2043270326 hasConcept C127313418 @default.
• W2043270326 hasConcept C130452526 @default.
• W2043270326 hasConcept C151730666 @default.
• W2043270326 hasConcept C156137136 @default.
• W2043270326 hasConcept C2779866092 @default.
• W2043270326 hasConcept C2780191791 @default.
• W2043270326 hasConcept C77044568 @default.
• W2043270326 hasConcept C84983702 @default.
• W2043270326 hasConceptScore W2043270326C111368507 @default.
• W2043270326 hasConceptScore W2043270326C127313418 @default.
• W2043270326 hasConceptScore W2043270326C130452526 @default.
• W2043270326 hasConceptScore W2043270326C151730666 @default.
• W2043270326 hasConceptScore W2043270326C156137136 @default.
• W2043270326 hasConceptScore W2043270326C2779866092 @default.
• W2043270326 hasConceptScore W2043270326C2780191791 @default.
• W2043270326 hasConceptScore W2043270326C77044568 @default.
• W2043270326 hasConceptScore W2043270326C84983702 @default.
• W2043270326 hasLocation W20432703261 @default.

• next