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• W2557136411 abstract "The Aptian stage represents a pivotal transition of the Cretaceous climate of the Earth but a comprehensive picture of the climate conditions is still unavailable due to the fragmentary paleotemperature records of the mid-late Aptian interval, especially in the Central Segment of South Atlantic region In this region extensive and thick salt sequence severely limiting the applicability of traditionally used paleotemperature proxies. In this paper, we present new quantitative sea surface temperatures from Congo Basin, during the late Aptian based on homogenization temperatures (Th) of fluid inclusions of halite. Homogenization temperatures concentrated at 25–35 °C are consistent with previous climate model results and represent the prevailing sea surface temperatures in the Congo Basin. The derived maximum sea surface temperature is 46.5 °C and much higher than existing paleotemperature records for the late Aptian, apparently representing local hot climate conditions. However, it is comparable with temperature records from many ancient and modern evaporitic basins where potash deposits also largely developed as seen in the Congo Basin. Significant cooling by about 5 °C was identified by both maximum (ThMax) and average (ThAverage) homogenization temperatures of halite during the late Aptian. A comparison of our results with records from other places leads to the conclusion that the observed declining sea surface temperatures of the Congo Basin represent the regional response to global climate cooling in the late Aptian. However, the amplitude, short-term oscillation pattern and worldwide correlation of this cooling is still difficult to assess due to often imprecise and poorly resolved age data, emphasizing the need of better constraint chronologies. Homogenization temperatures of halite fluid inclusions demonstrate the potential of the method to reliably track environmental and climatic changes of the past, especially in evaporitic settings of the Phanerozoic where other climate proxies are often not available." @default.
• W2557136411 created "2016-11-30" @default.
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• W2557136411 date "2017-03-01" @default.
• W2557136411 modified "2023-10-06" @default.
• W2557136411 title "Halite fluid inclusions and the late Aptian sea surface temperatures of the Congo Basin, northern South Atlantic Ocean" @default.
• W2557136411 cites W1963600555 @default.
• W2557136411 cites W1964648065 @default.
• W2557136411 cites W1971346015 @default.
• W2557136411 cites W1974537329 @default.
• W2557136411 cites W1978601024 @default.
• W2557136411 cites W1980709190 @default.
• W2557136411 cites W1984491575 @default.
• W2557136411 cites W1984974891 @default.
• W2557136411 cites W1985005684 @default.
• W2557136411 cites W1985260036 @default.
• W2557136411 cites W1987593072 @default.
• W2557136411 cites W1992266206 @default.
• W2557136411 cites W1993931487 @default.
• W2557136411 cites W1994639338 @default.
• W2557136411 cites W1998995868 @default.
• W2557136411 cites W2000252225 @default.
• W2557136411 cites W2002912225 @default.
• W2557136411 cites W2002998726 @default.
• W2557136411 cites W2004089187 @default.
• W2557136411 cites W2009934659 @default.
• W2557136411 cites W2010470144 @default.
• W2557136411 cites W2010819782 @default.
• W2557136411 cites W2012911259 @default.
• W2557136411 cites W2013458907 @default.
• W2557136411 cites W2013474973 @default.
• W2557136411 cites W2017255556 @default.
• W2557136411 cites W2019265572 @default.
• W2557136411 cites W2022097854 @default.
• W2557136411 cites W2029562728 @default.
• W2557136411 cites W2031547060 @default.
• W2557136411 cites W2046473714 @default.
• W2557136411 cites W2048644880 @default.
• W2557136411 cites W2050209614 @default.
• W2557136411 cites W2056212443 @default.
• W2557136411 cites W2056321513 @default.
• W2557136411 cites W2057199251 @default.
• W2557136411 cites W2058540279 @default.
• W2557136411 cites W2065375137 @default.
• W2557136411 cites W2065663218 @default.
• W2557136411 cites W2066770188 @default.
• W2557136411 cites W2067475292 @default.
• W2557136411 cites W2069299766 @default.
• W2557136411 cites W2075151349 @default.
• W2557136411 cites W2077053821 @default.
• W2557136411 cites W2082221791 @default.
• W2557136411 cites W2085333510 @default.
• W2557136411 cites W2085413519 @default.
• W2557136411 cites W2086474951 @default.
• W2557136411 cites W2088149005 @default.
• W2557136411 cites W2088179139 @default.
• W2557136411 cites W2090406412 @default.
• W2557136411 cites W2097820932 @default.
• W2557136411 cites W2098861869 @default.
• W2557136411 cites W2100233611 @default.
• W2557136411 cites W2106660898 @default.
• W2557136411 cites W2106685483 @default.
• W2557136411 cites W2107190049 @default.
• W2557136411 cites W2111211903 @default.
• W2557136411 cites W2114537558 @default.
• W2557136411 cites W2118432836 @default.
• W2557136411 cites W2120121502 @default.
• W2557136411 cites W2121514587 @default.
• W2557136411 cites W2121839724 @default.
• W2557136411 cites W2122586043 @default.
• W2557136411 cites W2123643570 @default.
• W2557136411 cites W2132529834 @default.
• W2557136411 cites W2133734728 @default.
• W2557136411 cites W2149695970 @default.
• W2557136411 cites W2151199706 @default.
• W2557136411 cites W2161715964 @default.
• W2557136411 cites W2164984370 @default.
• W2557136411 cites W2168003741 @default.
• W2557136411 cites W2168184269 @default.
• W2557136411 cites W2169757325 @default.
• W2557136411 cites W2171240692 @default.
• W2557136411 cites W2316455897 @default.
• W2557136411 cites W2323276389 @default.
• W2557136411 cites W2324446441 @default.
• W2557136411 cites W2332341125 @default.
• W2557136411 cites W4231010605 @default.
• W2557136411 doi "https://doi.org/10.1016/j.cretres.2016.11.008" @default.
• W2557136411 hasPublicationYear "2017" @default.
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