Halite fluid inclusions and the late Aptian sea surface temperatures of the Congo Basin, northern South Atlantic Ocean
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文摘
The late Aptian paleotemperature records of Congo Basin are revealed by halite fluid inclusions homogenization temperature. The large-scale tachyhydrite and potash support the revealed high temperature in Congo Basin during the late Aptian. Significant cooling by about 5 °C in Congo Basin represents a region response to global climate cooling in the late Aptian.

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