Presented at SVP (Poster) 2017:
Vertebrate species richness change from the late Miocene to early Pliocene of Lothagam, Turkana Basin, Kenya
Turkana Basin in Kenya, Africa is home to many discoveries of both hominin and non-hominin fossils. To date, a myriad of isotopic analyses has been conducted to interpret the paleoenvironment of the region. These include stable carbon isotope analysis in fossil tooth enamel and fossil eggshell to determine diet, stable carbon isotope analyses in paleosols to determine the amount of C4 biomass in the paleoecosystem, and oxygen stable isotope analyses in fossil enamel and paleosols to determine precipitation patterns. The purpose of the present study is to ascertain if paleoenvironmental shifts from the late Miocene to early Pliocene are associated with changes in vertebrate (mammals, turtles, and crocodiles) diversity (taxonomic richness) at Lothagam site in the Turkana Basin. The upper Miocene is represented by the Lower and Upper members of the Nawata Formation, and the lower Pliocene is represented by the Apak and Kaiyumung members of the Nachukui Formation. Both formations consist of alternating sandstone and mudstone, representing a perennial fluvial system. The Lower and Upper Nawata members also show repeated volcanic activity. The Apak Member is separated from the Kaiyumung Member by a basalt layer and lacustrine strata that have been excluded due to lack of vertebrate fossils, except for fish. The fossils utilized in this study were all collected from fluvial deposits, but further details about collecting methods and deposits are not available. Thus, possible taphonomic differences among the faunas cannot be ruled out and could conceivably be affecting the analyses of species richness. To determine richness changes, I compiled specimen counts for terrestrial, semi-aquatic and aquatic fossil species for each member, excluding fish and birds. Rarefaction analysis from the Lower and Upper Nawata, Apak, and Kaiyumung Members shows a significant (p<0.05) decrease in species richness from the Apak to Kaiyumung Member. There is also a decrease from the Lower to Upper Nawata Member, but it is not statistically significant (p>0.05). Paleoenvironmental interpretations show a shift from C3 to C4 vegetation and a transition from browsing to grazing ungulates at the Miocene-Pliocene boundary. The general change of vegetation and a shift of ungulate abundance are plausible drivers for the decline in species richness. Further broad scale richness analyses in the Turkana Basin would be required to determine if regional climatic changes were driving the decrease of diversity observed in the early Pliocene or if the pattern was localized to Lothagam.
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Presented at SVP (Poster) and GSA (Oral Presentation) 2015:
A comprehensive study of key paleoenvironmental changes using major faunal turnovers focusing in the Turkana Basin, Kenya: A development of a new model to determine environmental change.
Lake Turkana in Kenya, Africa has been home to many discoveries that are critical for understanding human evolution. These include a Paranthropus bosei cranium, Homo ergaster type specimen, cranium and full skeleton, Homo rudolfensis cranium, Homo habilis cranium, Paranthropus aethiopicus cranium, Austrolopithecus anamensis mandible, Kenyanthropus platyops cranium, and hominin footprints. However, we have limited understanding of the factors that drove adaptations observed in hominins. To date, efforts to understand the environmental underpinning of these adaptations have been based mainly on isotopic analysis of paleosols, using carbon and strontium isotopes from paleosols and comparing carbon dioxide ratios taken from paleosols to modern day carbon dioxide ratios taken from soil. The environmental information that is extracted from these isotopic analyses is limited. The purpose of this study was to diagnose significant environmental transitions based directly on faunal turnover of aquatic/amphibious and fully terrestrial biotas in the middle-late Miocene to the Recent. By compiling and creating a comprehensive synthesis of previous research in the Turkana Basin, I was able to document faunal turnover and then determine environmental changes. Based on analysis of hippopotamids, equids, suids, elephantids, rhinocerotids, proboscideans, antelopes and primates, I was able to diagnose significant environmental changes at the late Miocene transitioning to early Pliocene. At this time, there was a change from lowland wooded tropical forests with alluvial grassland to a savannah grassland with riparian tropical rainforests. This compilation of environments from modern and recent faunal habitats is supported with previous isotope research, supporting this method of determining environmental change. By comparing the results gathered through this research against environmental changes gathered previously through isotope data, this research would begin to establish a new model of diagnosing environmental changes through fossil records alone.
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