Open AccessMiocene evolution of atmospheric carbon dioxide
Author(s) -
Pagani Mark,
Arthur Michael A.,
Freeman Katherine H.
Publication year - 1999
Publication title -
paleoceanography
Language(s) - English
Resource type - Journals
eISSN - 1944-9186
pISSN - 0883-8305
DOI - 10.1029/1999pa900006
Subject(s) - geology , foraminifera , paleontology , late miocene , holocene climatic optimum , carbon dioxide , middle miocene disruption , oceanography , carbon dioxide in earth's atmosphere , antarctic ice sheet , carbon cycle , total organic carbon , glacial period , plankton , climate change , sea ice , cryosphere , ecosystem , benthic zone , structural basin , ecology , biology
Changes in p CO 2 or 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 Miocene p CO 2 from ε p values 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 highest p CO 2 occurred during the latest Oligocene (∼350 ppmv) but decreased rapidly at ∼25 Ma. The early and middle Miocene was characterized by low p CO 2 (260–190 ppmv). Lower intervals of p CO 2 correspond to inferred organic carbon burial events and glacial episodes with the lowest concentrations occurring during the middle Miocene. There is no evidence for either high p CO 2 during the late early Miocene climatic optimum or a sharp p CO 2 decrease associated with EAIS growth. Paradoxically, p CO 2 increased following EAIS growth and obtained preindustrial levels by ∼10 Ma. Although we emphasize an oceanographic control on Miocene climate, low p CO 2 could have primed the climate system to respond sensitively to changes in heat and vapor transport.