152 130 Years of Research in the Turkana Basin, Kenya: Insights into Earth, Climate, and Life in Eastern Africa
Tuesday, 24 September 2024
8:00 AM - 12:00 PM
Ballroom A&B
STRATIGRAPHIC EVOLUTION OF THE TURKANA BASIN, EASTERN AFRICA
Paper number: 152-3
Program: Technical Sessions
Time: 8:40 AM – 9:00 AM
Authors
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Robert G. RaynoldsDenver Museum of Nature & Science, Denver, CO
Abstract
Basin fill includes some seven km of rift-related volcanics (basalts, phonolites, rhyolites) along with a diverse array of sedimentary strata reflecting lacustrine and fluvial depositional systems. CARS strata are composed of coarse alluvial deposits in a non-volcanic rift setting. EARS accumulation is dominated by early rift volcanic strata, which in late Oligocene through Miocene times are punctuated by thick lacustrine packages (Lokichar Basin) and scattered fluvial sequences that preserve important vertebrate fossil assemblages. The modern configuration of the basin developed in early Pliocene times, and hosted a complex fluvio-lacustrine system that persists to the present day. The latter is notable for abundant distal silicic tephra providing markers for correlation and age control. Legacy and on-going geologic mapping, outcrop and subsurface investigations provide a detailed record of the spatial and temporal dynamics in this long-lived archive of geologic history.
Geological Society of America Abstracts with Programs. Vol. 56, No. 5
doi: 10.1130/abs/2024AM-402242
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