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Atmosphere history

Peterson BJ, Fry B (1987) Stable isotopes in ecosystem studies. Ann Rev Ecol Syst 18 293-320 Petit JR, et al. (1999) Qimate and atmospheric history of the past 420000 years from the Vostok ice core, Antarctica. Nature 399 429 36... [Pg.263]

Tmdinger CM, Etheridge DM, Sturrock GA, Fraser PJ, Krummel PB, McCulloch A (2004) Atmospheric Histories of Halocarbons from Analysis of Antarctic Fim Air Methyl Bromide, Methyl Chloride, Chloroform, and Dichloromethane. J Geophys Res 109 D22310... [Pg.389]

Fisher, A.G., 1965. Fossils, early life and atmospheric history. Proc. Natl. Acad. Sci. USA, 53 1205-1215. [Pg.288]

Rehder G., Keir R. S., Suess E., and Rhein M. (1999) Methane in the northern Atlantic controlled by microbial oxidation and atmospheric history. Geophys. Res. Lett. 26, 587-590. [Pg.2002]

Petit J. R., Jouzel J., Raynaud D., Barkov N. 1., Barnola J.-M., Basile L, Bender M., Chapellaz J., Davis M., Pelaygue G., Delmotte M., Kotylakov V. M., Legrand M., Lipankov V. Y., Lorius C., Pepin L., Ritz C., Saltzman E., and Stlevenard M. (1999) Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica. Nature 399, 429-436. [Pg.2854]

Arvidson R. S., Mackenzie F. T., and Guidry M. W. (2000) Ocean/atmosphere history and carbonate precipitation rates a solution to the dolomite problem. In Marine Authigenesis from Global to Microbial, SEPM Spec. Publ. No. 65 (eds. C. R. Glenn, L. Prevot-Lucas, and J. Lucas), SEPM, Tulsa, pp. 1-5. [Pg.3864]

Rutten, M. G., 1966 Geologic data on atmospheric history. Conf. on Atmospheric Chem., Circulation and Aerosols. Visby, Abstract of papers 58-59. [Pg.192]

Figure 1 Atmospheric history of A C measured by M. Stuiver in tree rings covering ad 1511 to ac 1954. Most of the decrease over the iast hundred years is due to the addition of anthropogenic CO2 to the atmosphere during the industriai revoiution by the burning of fossii fueis. Figure 1 Atmospheric history of A C measured by M. Stuiver in tree rings covering ad 1511 to ac 1954. Most of the decrease over the iast hundred years is due to the addition of anthropogenic CO2 to the atmosphere during the industriai revoiution by the burning of fossii fueis.

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See also in sourсe #XX -- [ Pg.158 ]




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