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Ecological continuity between Lower and Upper Bed II, Olduvai Gorge, Tanzania
Kris Kovarovic1, Rebecca Slepkov, Kieran P McNulty
1Department of Anthropology, Durham University, Dawson Building, South Road, Durham DH1 3LE, United Kingdom. kris.kovarovic@durham.ac.uk
Journal of Human Evolution
|April 10, 2013
Summary
Early hominin environments in Olduvai Gorge Bed II were primarily woodland habitats, with some marshy areas. Mammal fossil analysis reveals consistent woodland environments despite changes over time.
Area of Science:
- Paleoecology
- Paleontology
- Archaeology
Background:
- Olduvai Gorge Bed II sediments offer insights into early hominin environmental changes.
- Previous studies noted faunal community differences above and below the Lemuta Member tuff (~1.74 Ma).
- Hominin fossil density is lower in Bed II compared to Bed I, leading to less research.
Purpose of the Study:
- To investigate palaeoecological conditions during the transition between older and younger Bed II faunas.
- To analyze mammalian community ecological niche exploitation profiles and compare them to modern habitats.
- To assess environmental changes across the Lemuta Member disconformity in Olduvai Gorge.
Main Methods:
- Compilation of comprehensive species lists for older and younger Bed II faunas.
- Correspondence analysis of faunal assemblages to identify palaeoecological differences.
- Resampling of modern locality data with similar body mass profiles for discriminant analysis.
Main Results:
- Initial analysis indicated palaeoecological differences between pre- and post-Lemuta Member assemblages, neither representing forest habitats.
- After accounting for taphonomic body mass differences, ecological distinctions became less significant.
- Discriminant correspondence analyses suggest both fossil assemblages resemble modern woodland habitats, with Lower Bed II showing affinity to floodplain and marshy woodlands.
Conclusions:
- Woodland habitats were consistently important throughout Olduvai Gorge Bed II.
- Differences between older and younger Bed II faunas could originate from within a single modern habitat type.
- While increased aridity may have occurred post-Lemuta Member, woodland environments persisted.
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