地球大気中の二酸化炭素 (Japanese Wikipedia)

Analysis of information sources in references of the Wikipedia article "地球大気中の二酸化炭素" in Japanese language version.

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T. Owen, R. D. Cess and V. Ramanathan (1979). “Enhanced CO₂ greenhouse to compensate for reduced solar luminosity on early Earth”. Nature 277: 640-642. doi:10.1038/277640a0.
Ken Caldeira and James F. Kasting (1992). “The life span of the biosphere revisited”. Nature 360 (6406): 721-723. doi:10.1038/360721a0. "They pointed out that, despite the current fossil-fuel induced increase in the atmospheric CO₂ concentration, the long-term trend should be in the opposite direction: as increased solar luminosity warms the Earth, silicate rocks should weather more readily, causing atmospheric CO₂ to decrease. In their model¹, atmospheric CO₂ falls below the critical level for C3 photosynthesis, 150 parts per million (p.p.m.), in only 100 Myr, and this is assumed to mark the demise of the biosphere as a whole."
Daniel R. Colman et al. (2017). “The deep, hot biosphere: Twenty-five years of retrospection”. Proceedings of the National Academy of Sciences 114 (27): 6895-6903. doi:10.1073/pnas.1701266114.
P. H. Barry et al. (2019). “Forearc carbon sink reduces long-term volatile recycling into the mantle”. Nature 568 (7753): 487. doi:10.1038/s41586-019-1131-5.

Ken Caldeira and James F. Kasting (1992). “The life span of the biosphere revisited”. Nature 360 (6406): 721-723. doi:10.1038/360721a0. "They pointed out that, despite the current fossil-fuel induced increase in the atmospheric CO₂ concentration, the long-term trend should be in the opposite direction: as increased solar luminosity warms the Earth, silicate rocks should weather more readily, causing atmospheric CO₂ to decrease. In their model¹, atmospheric CO₂ falls below the critical level for C3 photosynthesis, 150 parts per million (p.p.m.), in only 100 Myr, and this is assumed to mark the demise of the biosphere as a whole."