The Oltulelei Formation of the southern Kenyan Rift Valley: A chronicle of rapid landscape transformation over the last 500 k.y.

Anna K. Behrensmeyer, Richard Potts, Alan Deino

Research output: Contribution to journalArticlepeer-review

13 Scopus citations

Abstract

The last half-million years of geological history of the East African Rift in southern Kenya is recorded by the Oltulelei Formation, which is newly described in this paper. Well-dated depositional cycles in this formation reveal how tectonics and climate shaped rift valley sedimentation, as well as the landscapes inhabited by human ancestors. The Oltulelei Formation (ca. 320 to ca. 36 ka) overlies the Olorgesailie Formation (1.2-0.5 Ma) on an erosional unconformity and is divided into three successive units, the Olkesiteti, Oltepesi, and Tinga Members. The stratotype for the formation is exposed in the Olorgesailie Basin, north and northwest of Mount Olorgesailie. The 40Ar/39Ar dates on interbedded tephras provide geochronological controls on the timing of three major depositional cycles. Lateral variability in the Oltulelei Formation shows that the Olorgesailie Basin and the northern Koora Graben formed three rift subbasins that were periodically connected and disconnected over the past 500 k.y. Erosional phases removed large volumes of sediment from the Olorgesailie Basin, requiring through-flowing drainage to a lower base level southwest and south of Mount Olorgesailie. Aggradational phases were primarily fluvial, with siliciclastic and volcaniclastic sediment filling valleys and burying dissected landscapes. Tufa, shallow lacustrine, and wetlands deposits also occur and indicate elevated water tables in fault-controlled sumps or blocked drainages. We propose that connections and disconnections between rift segments were driven by tectonic forces, primarily faulting of volcanic basement rocks and periodic influxes of volcanicsediment, combined with climatic conditions that enabled erosion and transport of large volumes of sediment into and out of the subbasins. The Oltulelei Formation preserves a record of a dynamic change in the physical landscape of the southern Kenya Rift, with major shifts in erosion versus deposition on time scales of 104-105 yr. This study provides new, well-calibrated information on sedimentation in active rift settings as well as an outcrop- based, three-dimensional, basin-scale geological history that can be integrated with emerging drill-core paleoclimate records from southern Kenya. The stratigraphic record preserved in the Oltulelei Formation advances understanding and poses new questions about how tectonics and climate shaped middle to late Pleistocene faunal turnover and the transition in southern Kenya from Acheulean to Middle Stone Age technology.

Original languageEnglish (US)
Pages (from-to)1474-1492
Number of pages19
JournalBulletin of the Geological Society of America
Volume130
Issue number9-10
DOIs
StatePublished - 2018

Bibliographical note

Funding Information:
Research reported here was supported by the Peter Buck Fund for Human Origins Research, the Ruth and Vernon Taylor Foundation, the National Science Foundation (NSF) HOMINID Program (BCS-0218511), and the NSF Archaeometry program (EAR-1322017). The Olorgesailie field work is a collaborative project by the National Museums of Kenya (NMK) and Smithsonian Institution. We especially thank M. Kibunjia, I.O. Farah, E. Mbua, F.K. Manthi, and M. Muungu of the NMK for their permissions and logistical support. We are indebted to all of our field crew for many different contributions to our research on the "post-Olorgesailie beds" over the past 15 yr, with special thanks to Muteti Nume for his contributions as excavation foreman and supervisor of the geological trenching operations. Behrensmeyer thanks Bill Keyser for calculating the weight of the Tinga Member boulder, the 2004-2005 Olorgesailie Field School participants for their enthusiastic mapping of Oltepesi Member paleochannels, Brian Grivna and LacCore for help with PsiCat, and Mary Parrish for advice and assistance with the figures. Potts thanks Jennifer Clark and Briana Pobiner for field logistics assistance. We offer a particular note of appreciation in memory of Glynn Isaac for his inspiring early work on the geology and archaeology of Olorgesailie. This is a publication of the Smithsonian's Human Origins Program.

Publisher Copyright:
© 2018 Geological Society of America.

Copyright:
Copyright 2018 Elsevier B.V., All rights reserved.

Continental Scientific Drilling Facility tags

  • ODP

Fingerprint

Dive into the research topics of 'The Oltulelei Formation of the southern Kenyan Rift Valley: A chronicle of rapid landscape transformation over the last 500 k.y.'. Together they form a unique fingerprint.

Cite this