Abstract
Changes inpCO2or ocean circulation are generally invoked to explain warm early Miocene climates and a rapid East Antarctic ice sheet (EAIS) expansion in the middle Miocene. This study reconstructs late Oligocene to late MiocenepCO2from εpvalues based on carbon isotopic analyses of diunsaturated alkenones and planktonic foraminifera from Deep Sea Drilling Project sites 588 and 608 and Ocean Drilling Program site 730. Our results indicate that highestpCO2occurred during the latest Oligocene (∼350 ppmv) but decreased rapidly at ∼25 Ma. The early and middle Miocene was characterized by lowpCO2(260–190 ppmv). Lower intervals ofpCO2correspond to inferred organic carbon burial events and glacial episodes with the lowest concentrations occurring during the middle Miocene. There is no evidence for either highpCO2during the late early Miocene climatic optimum or a sharppCO2decrease associated with EAIS growth. Paradoxically,pCO2increased following EAIS growth and obtained preindustrial levels by ∼10 Ma. Although we emphasize an oceanographic control on Miocene climate, lowpCO2could have primed the climate system to respond sensitively to changes in heat and vapor transport.
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