EGU25-21298, updated on 15 Mar 2025
https://doi.org/10.5194/egusphere-egu25-21298
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Monday, 28 Apr, 11:50–12:00 (CEST)
 
Room 0.15
Late Cenozoic Eastern African Aridification, Vegetation Change, and Behavioral Diversity from Enamel Isotopes
Daniel Green1,2, Kevin Uno1,2,3, and the Turkana Miocene Project Coauthors*
Daniel Green and Kevin Uno and the Turkana Miocene Project Coauthors
  • 1Department of Human Evolutionary Biology, Harvard University, Cambridge MA 02138, USA
  • 2Lamont-Doherty Earth Observatory and Climate School, Columbia University, Palisades NY 10964, USA
  • 3Department of Earth and Planetary Sciences, Harvard University, Cambridge MA 02138, USA
  • *A full list of authors appears at the end of the abstract

Eastern African geochemical and paleovegetation records hint at the presence of C4 photosynthesis in the Early Miocene (~21 Ma), long before the origin and diversification of hominins, and during a period of relative global climatic stability. Evidence of C4 proliferation and its impact on faunal behavior and ecosystem structure, however, is lacking from stable isotope records in mammalian tooth enamel, one of the most abundant and resilient archives of past diet and ecological change. We present novel and published enamel stable oxygen and carbon isotope records from 22 eastern African fossil assemblages; totaling 1252 specimens dating from 29 to 4 Ma. Oxygen isotope compositions indicate cooling and drying from the Oligocene into a hydrologically diverse Miocene, setting the stage for a shift to the consumption of C4 resources potentially as early as 13 Ma and in larger amounts beginning at 10 Ma. Faunal stable isotope variability within and between Early Miocene sites suggest that a C3-dominated eastern Africa nevertheless hosted varied hydrological regimes and animal behaviors across different sites. Taxa such as anthracotheres and giraffoids occupy consistently semi-aquatic or sub-canopy browsing niches. Primates, however, exhibit exceptional behavioral plasticity, with the large-bodied Early Miocene ape Afropithecus deriving most water from flowing surface sources at Buluk (Turkana Basin, Kenya) instead of from canopy vegetation as at other sites. The ecological and hydroclimate transformations from the Paleogene into the Neogene help explain how C3 landscapes became primed for Late Miocene C4 expansion and hosted behavioral diversity that shaped an emerging African savanna fauna, and the behavioral plasticity of our ancestors.

Turkana Miocene Project coauthors include: Eipa Aoron, Sneha Bapana, Catherine Beck, Paul Barrett, Mikael Fortelius, Craig Feibel, Aryeh Grossman, Greg Henkes, Ashley House, Francis Kirera, Martin Kirinya, Daeun Lee, Cynthia Liutkus-Pierce, Sam Lavin, Ellen R. Miller, Christopher Poulsen, Patricia Princehouse, John Rowan, Gabrielle Russo, William Sanders, Mae Saslaw, Ruth Tweedy, Linet Sankau, Natasha S. Vitek, and Indrė Žliobaitė.

Turkana Miocene Project Coauthors:

Eipa Aoron, Sneha Bapana, Catherine Beck, Paul Barrett, Mikael Fortelius, Craig Feibel, Aryeh Grossman, Greg Henkes, Ashley House, Francis Kirera, Martin Kirinya, Daeun Lee, Cynthia Liutkus-Pierce, Sam Lavin, Ellen R. Miller, Christopher Poulsen, Patricia Princehouse, John Rowan, Gabrielle Russo, William Sanders, Mae Saslaw, Ruth Tweedy, Linet Sankau, Natasha S. Vitek, and Indrė Žliobaitė.

How to cite: Green, D. and Uno, K. and the Turkana Miocene Project Coauthors: Late Cenozoic Eastern African Aridification, Vegetation Change, and Behavioral Diversity from Enamel Isotopes, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-21298, https://doi.org/10.5194/egusphere-egu25-21298, 2025.