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- W2317164516 abstract "A global carbon cycle model covering the Late Jurassic Period to Recent (150–0 Ma) with subaerial metamorphism and continental and oceanic hot spot volcanism was constructed. The model's results indicate that the OAE1a and Valanginian OAE (OAE: oceanic anoxic event) in the Cretaceous Period are related to increased atmospheric CO2 level due to hot spot volcanism. Furthermore, the model results based on high-resolution geochemical records demonstrate that decreases in CO2 associated with the termination of the OAE1a, OAE2, and perhaps the Valanginian OAE are attributable to a large amount of organic carbon burial. Moreover, the model results indicate that enhanced continental weathering and carbonate precipitation contributed to the decrease in atmospheric CO2 during the OAE1a period. A comparison of the model results with proxy estimates of atmospheric CO2 indicates that CO2 degassings from the lithosphere and mantle, including those from subaerial metamorphism, partly contributed to high levels of atmospheric CO2 in the middle Cretaceous and the Eocene, but they are not sufficiently decisive to account for the suggested CO2 levels by the proxies. Differences in estimated CO2 between the model and the proxies in the middle Cretaceous can be explained by a complex evolution of the terrestrial plants from gymnosperms to angiosperms, and/or continental weathering assisted by arbuscular mycorrhizal and ectomycorrhizal fungi and a fluctuation of the climate sensitivity, which would have dynamically changed on geological time scales, whereas an increase in non-CO2 greenhouse gases could explain the CO2 difference in the Eocene warming." @default.
- W2317164516 created "2016-06-24" @default.
- W2317164516 creator A5057007152 @default.
- W2317164516 date "2016-07-01" @default.
- W2317164516 modified "2023-10-10" @default.
- W2317164516 title "Atmospheric carbon dioxide and climate change since the Late Jurassic (150Ma) derived from a global carbon cycle model" @default.
- W2317164516 cites W1504149159 @default.
- W2317164516 cites W1530286044 @default.
- W2317164516 cites W1611275020 @default.
- W2317164516 cites W1617554277 @default.
- W2317164516 cites W1633310309 @default.
- W2317164516 cites W1894009859 @default.
- W2317164516 cites W1966555934 @default.
- W2317164516 cites W1968838468 @default.
- W2317164516 cites W1969955164 @default.
- W2317164516 cites W1970354719 @default.
- W2317164516 cites W1973562437 @default.
- W2317164516 cites W1975350563 @default.
- W2317164516 cites W1981383339 @default.
- W2317164516 cites W1984357207 @default.
- W2317164516 cites W1985005684 @default.
- W2317164516 cites W1994607471 @default.
- W2317164516 cites W1999120548 @default.
- W2317164516 cites W2000241625 @default.
- W2317164516 cites W2002758589 @default.
- W2317164516 cites W2004464215 @default.
- W2317164516 cites W2008677458 @default.
- W2317164516 cites W2011963573 @default.
- W2317164516 cites W2013164736 @default.
- W2317164516 cites W2014949335 @default.
- W2317164516 cites W2015479092 @default.
- W2317164516 cites W2018535712 @default.
- W2317164516 cites W2019086155 @default.
- W2317164516 cites W2019640126 @default.
- W2317164516 cites W2022597252 @default.
- W2317164516 cites W2022778758 @default.
- W2317164516 cites W2023606819 @default.
- W2317164516 cites W2028095175 @default.
- W2317164516 cites W2028217507 @default.
- W2317164516 cites W2030169181 @default.
- W2317164516 cites W2031313070 @default.
- W2317164516 cites W2043643933 @default.
- W2317164516 cites W2049548531 @default.
- W2317164516 cites W2051772753 @default.
- W2317164516 cites W2054164658 @default.
- W2317164516 cites W2055442076 @default.
- W2317164516 cites W2059131953 @default.
- W2317164516 cites W2063574244 @default.
- W2317164516 cites W2068684133 @default.
- W2317164516 cites W2070283082 @default.
- W2317164516 cites W2071345686 @default.
- W2317164516 cites W2073788854 @default.
- W2317164516 cites W2077685934 @default.
- W2317164516 cites W2077877492 @default.
- W2317164516 cites W2078788152 @default.
- W2317164516 cites W2079852953 @default.
- W2317164516 cites W2084626014 @default.
- W2317164516 cites W2085311334 @default.
- W2317164516 cites W2089746913 @default.
- W2317164516 cites W2092206858 @default.
- W2317164516 cites W2099709537 @default.
- W2317164516 cites W2100732417 @default.
- W2317164516 cites W2106660898 @default.
- W2317164516 cites W2106670836 @default.
- W2317164516 cites W2111036301 @default.
- W2317164516 cites W2113285139 @default.
- W2317164516 cites W2114549590 @default.
- W2317164516 cites W2116562977 @default.
- W2317164516 cites W2116564966 @default.
- W2317164516 cites W2118419715 @default.
- W2317164516 cites W2130377704 @default.
- W2317164516 cites W2134577629 @default.
- W2317164516 cites W2143037254 @default.
- W2317164516 cites W2146200079 @default.
- W2317164516 cites W2147587805 @default.
- W2317164516 cites W2151285347 @default.
- W2317164516 cites W2154073704 @default.
- W2317164516 cites W2159123610 @default.
- W2317164516 cites W2171817134 @default.
- W2317164516 cites W2319127417 @default.
- W2317164516 cites W2328366459 @default.
- W2317164516 cites W2334349158 @default.
- W2317164516 cites W2953347398 @default.
- W2317164516 cites W4213170094 @default.
- W2317164516 cites W4245300726 @default.
- W2317164516 doi "https://doi.org/10.1016/j.palaeo.2016.04.002" @default.
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