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• W2107190049 endingPage "2244" @default.
• W2107190049 startingPage "2215" @default.
• W2107190049 abstract "Depositional sequences capped by peritidal carbonates and breccias on the Aptian Adriatic carbonate platform, Croatia, were studied to evaluate evidence for glacioeustasy within an age framework constrained by carbon-isotope chemostratigraphy. Sequence Ad1 (17–60-m [56–197-ft] thick; uppermost Barremian–lower Aptian) is dominated by shallow subtidal parasequences. Sequence Ad2 (7–13-m [23–43-ft] thick; lower Aptian–lowermost upper Aptian) contains oceanic anoxic event (OAE) 1a, associated with lagoonal laminated carbonates. Sequence Ad3 (3–8-m [10–26-ft] thick) probably is lower upper Aptian and likely is separated by a major hiatus from sequence Ad4 (8–20-m [26–66-ft] thick; uppermost Aptian), which spans OAE1b. Both Ad2 and Ad3 are dominated by peritidal parasequences updip in the lower transgressive systems tract and upper highstand systems tract and by subtidal parasequences elsewhere, whereas sequence Ad4 is dominated by shallow subtidal parasequences. Low accommodation rates (4.0–6.0 cm [1.6–2.4 in.] in the earliest Aptian, decreasing to approximately 1.0 cm/k.y. [0.3 in./k.y.] later) promoted widespread breccia development during relative sea level falls, aided by tectonic warping. The sequence-capping breccias, eccentricity-dominated cyclicity, restriction of peritidal facies to late highstands, and coeval off-shelf oxygen-isotope records all suggest that sea level falls occurred during times of cooling and had a significant glacioeustatic component. These intermittent cooler periods and continental ice buildup punctuated the Aptian greenhouse climate." @default.
• W2107190049 created "2016-06-24" @default.
• W2107190049 creator A5026944996 @default.
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• W2107190049 date "2012-12-01" @default.
• W2107190049 modified "2023-10-16" @default.
• W2107190049 title "Sequence development influenced by intermittent cooling events in the Cretaceous Aptian greenhouse, Adriatic platform, Croatia" @default.
• W2107190049 cites W1493645101 @default.
• W2107190049 cites W1505957071 @default.
• W2107190049 cites W1533729466 @default.
• W2107190049 cites W1534297386 @default.
• W2107190049 cites W1552509298 @default.
• W2107190049 cites W1555646088 @default.
• W2107190049 cites W1583491481 @default.
• W2107190049 cites W1584354900 @default.
• W2107190049 cites W1604103721 @default.
• W2107190049 cites W1620496676 @default.
• W2107190049 cites W1630322587 @default.
• W2107190049 cites W1639686691 @default.
• W2107190049 cites W1748996452 @default.
• W2107190049 cites W1753926244 @default.
• W2107190049 cites W1807528795 @default.
• W2107190049 cites W1897585621 @default.
• W2107190049 cites W1965846255 @default.
• W2107190049 cites W1969072489 @default.
• W2107190049 cites W1984491575 @default.
• W2107190049 cites W1993844779 @default.
• W2107190049 cites W1995253200 @default.
• W2107190049 cites W1996116627 @default.
• W2107190049 cites W1998138507 @default.
• W2107190049 cites W1998995868 @default.
• W2107190049 cites W1999173650 @default.
• W2107190049 cites W2002998726 @default.
• W2107190049 cites W2007668228 @default.
• W2107190049 cites W2009022128 @default.
• W2107190049 cites W2011076039 @default.
• W2107190049 cites W2012948170 @default.
• W2107190049 cites W2013050239 @default.
• W2107190049 cites W2013446430 @default.
• W2107190049 cites W2014735478 @default.
• W2107190049 cites W2017195568 @default.
• W2107190049 cites W2020439806 @default.
• W2107190049 cites W2020594208 @default.
• W2107190049 cites W2022470696 @default.
• W2107190049 cites W2027622090 @default.
• W2107190049 cites W2027711078 @default.
• W2107190049 cites W2033708716 @default.
• W2107190049 cites W2034716029 @default.
• W2107190049 cites W2037509965 @default.
• W2107190049 cites W2039126607 @default.
• W2107190049 cites W2042921697 @default.
• W2107190049 cites W2046607507 @default.
• W2107190049 cites W2051657527 @default.
• W2107190049 cites W2053259135 @default.
• W2107190049 cites W2055336492 @default.
• W2107190049 cites W2055826656 @default.
• W2107190049 cites W2057199251 @default.
• W2107190049 cites W2058222931 @default.
• W2107190049 cites W2058540279 @default.
• W2107190049 cites W2058695708 @default.
• W2107190049 cites W2059131953 @default.
• W2107190049 cites W2061541155 @default.
• W2107190049 cites W2067785440 @default.
• W2107190049 cites W2069217550 @default.
• W2107190049 cites W2081033828 @default.
• W2107190049 cites W2081392172 @default.
• W2107190049 cites W2081582907 @default.
• W2107190049 cites W2086676264 @default.
• W2107190049 cites W2089962601 @default.
• W2107190049 cites W2091348587 @default.
• W2107190049 cites W2097798991 @default.
• W2107190049 cites W2103111091 @default.
• W2107190049 cites W2104754992 @default.
• W2107190049 cites W2105027613 @default.
• W2107190049 cites W2106559152 @default.
• W2107190049 cites W2107127140 @default.
• W2107190049 cites W2108570205 @default.
• W2107190049 cites W2108977787 @default.
• W2107190049 cites W2111775073 @default.
• W2107190049 cites W2113716498 @default.
• W2107190049 cites W2114251363 @default.
• W2107190049 cites W2114261226 @default.
• W2107190049 cites W2121737756 @default.
• W2107190049 cites W2125191778 @default.
• W2107190049 cites W2129709602 @default.
• W2107190049 cites W2137239952 @default.
• W2107190049 cites W2142602441 @default.
• W2107190049 cites W2149660572 @default.
• W2107190049 cites W2152668572 @default.
• W2107190049 cites W2155104238 @default.
• W2107190049 cites W2157358846 @default.
• W2107190049 cites W2160468719 @default.
• W2107190049 cites W2161537617 @default.
• W2107190049 cites W2164982181 @default.

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