Stable isotope paleoecology of Late Pleistocene Middle Stone Age humans from the Lake Victoria basin, Kenya

Nicole D. Garrett, David L. Fox, Kieran P. McNulty, J. Tyler Faith, Daniel J. Peppe, Alex Van Plantinga, Christian A. Tryon

Research output: Contribution to journalArticlepeer-review

27 Scopus citations


Paleoanthropologists have long argued that environmental pressures played a key role in human evolution. However, our understanding of how these pressures mediated the behavioral and biological diversity of early modern humans and their migration patterns within and out of Africa is limited by a lack of archaeological evidence associated with detailed paleoenvironmental data. Here, we present the first stable isotopic data from paleosols and fauna associated with Middle Stone Age (MSA) sites in East Africa. Late Pleistocene (~100-45 ka, thousands of years ago) sediments on Rusinga and Mfangano Islands in eastern Lake Victoria (Kenya) preserve a taxonomically diverse, non-analog faunal community associated with MSA artifacts. We analyzed the stable carbon and oxygen isotope composition of paleosol carbonate and organic matter and fossil mammalian tooth enamel, including the first analyses for several extinct bovids such as Rusingoryx atopocranion, Damaliscus hypsodon, and an unnamed impala species. Both paleosol carbonate and organic matter data suggest that local habitats associated with human activities were primarily riverine woodland ecosystems. However, mammalian tooth enamel data indicate that most large-bodied mammals consumed a predominantly C4 diet, suggesting an extensive C4 grassland surrounding these riverine woodlands in the region at the time. These data are consistent with other lines of paleoenvironmental evidence that imply a substantially reduced Lake Victoria at this time, and demonstrate that C4 grasslands were significantly expanded into equatorial Africa compared with their present distribution, which could have facilitated dispersal of human populations and other biotic communities. Our results indicate that early populations of Homo sapiens from the Lake Victoria region exploited locally wooded and well-watered habitats within a larger grassland ecosystem.

Original languageEnglish (US)
Pages (from-to)1-14
Number of pages14
JournalJournal of Human Evolution
StatePublished - May 1 2015

Bibliographical note

Funding Information:
Research presented here was conducted under research permit NCST/5/002/R/576 issued to Tryon by the government of the Republic of Kenya and an Exploration and Excavation License issued by the National Museums of Kenya. Funding was provided by the National Science Foundation ( BCS-0841530 , BCS-1013199 , BCS-1013108 , and BCS-1013134 ), the National Geographic Society's Committee for Research and Exploration ( 8762-10 ), the Leakey Foundation , McKnight Foundation , the Geological Society of America , New York University , Baylor University , the University of Minnesota , and the University of Queensland . We thank Drs. Idle Farah and Emma Mbua for facilitating our research at the National Museums of Kenya, and the British Institute in eastern Africa and Rusinga Island Lodge for logistical and material support. We are grateful to the many individuals who helped us in the field and laboratory, including Mathew Macharwas, Jared Olelo, Stephen Longoria, Joshua Siembo, Julian Ogondo, Sheila Nightingale, Kirsten Jenkins, Andrew Haveles, and Maniko Solheid.

Publisher Copyright:
© 2014 Elsevier Ltd.


  • Human dispersal
  • Mfangano island
  • Paleoenvironment
  • Quaternary
  • Rusinga island


Dive into the research topics of 'Stable isotope paleoecology of Late Pleistocene Middle Stone Age humans from the Lake Victoria basin, Kenya'. Together they form a unique fingerprint.

Cite this