Fossil wood from the upper Miocene Mpesida Beds at Cheparain (Baringo District, Kenya): Botanical affinities and palaeoenvironmental implications
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We discovered fossil wood in place in the Upper Miocene layers in Kenya.

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We studied anatomically the fossil wood and identified them partly.

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The cambial activity of all the fossil wood reveals a past seasonal climate.

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The discovered palaeoflora is potentially close to the extant flora found in the Tana River valley in Eastern Kenya.

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The present environment of the Tugen Hills is cooler than the paleoenvironment of the fossil site due to the Hills uplift.

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