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- W2092470507 abstract "Sedimentological, micropaleontological and seismic-profiling data elucidate the history of Tertiary sea-level movements around southern Africa. These new data show that landward movement of the sea began in early Paleocene time and continued into the early Eocene. The sea probably reached its maximum Paleocene height during the early Eocene, and is today represented by outcrops up to at least 204 m, and probably as high as 360 m, above modern sea level. A brief regressive pulse occurred during the middle Eocene, with renewed transgression in the late Eocene. A major regression followed, probably spanning all of Oligocene and early Miocene times. This regression exposed much of the continental shelf and is clearly represented on seismic-reflection profiles by a widespread unconformity. The major Neogene transgression began in the middle Miocene and probably reached its greatest extent in the late Miocene or early Pliocene. The overall middle Miocene to early Pliocene transgression was interrupted by a brie..." @default.
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- W2092470507 date "1981-01-01" @default.
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- W2092470507 title "Tertiary Sea-Level Movements around Southern Africa" @default.
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- W2092470507 doi "https://doi.org/10.1086/628565" @default.
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