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- W4387466495 startingPage "717" @default.
- W4387466495 abstract "The central Kenya Rift around Lakes Baringo and Bogoria hosts a series of sedimentary formations that preserve evidence of past environmental change dating back to the Miocene. During that time lakes were created, developed, and ultimately destroyed by a combination of tectonic, volcanic and climatic controls. Flood lavas and central volcanoes gave rise to a variety of volcanic rocks, including basalts, phonolites, trachytes, trachyphonolites and airfall ash deposits. Saline and freshwater lakes, fluvial environments and pedogenic settings developed during deposition of the Miocene Tambach, Ngorora, Ngerngerwa and Lukeino formations as well as the Mpesida and Muruyur Beds. Deposits laid down in these settings also contributed to the Plio-Pleistocene Chemeron, Mabaget, Kapthurin, Chesowanja and Chemoigut formations; the Toluk, Kampi ya Samaki, Loiminange and Ilosowuani beds; and the Pleistocene Loboi Silts. Diatoms, sponge spicules, phytoliths, ostracods, pollen, charcoal, fossil fish, vertebrate remains, insect nests and stone tools are variously reported from these deposits. Sedimentary facies include diatomites, diatomaceous sediments, siliciclastic clay to conglomeratic deposits, zeolitic deposits, tufa, phosphorites, and tuffaceous units. Sedimentation in the Chemeron Formation has been linked to Milankovitch cycles. Palaeogeographic reconstructions provide a clear history of lake development through time although the lateral extent of some palaeolakes is uncertain." @default.
- W4387466495 created "2023-10-10" @default.
- W4387466495 creator A5056527653 @default.
- W4387466495 creator A5074754470 @default.
- W4387466495 date "2023-01-01" @default.
- W4387466495 modified "2023-10-11" @default.
- W4387466495 title "The Baringo-Bogoria Basin and Adjacent Parts of the Kenya Rift" @default.
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