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Warianty tytułu
Języki publikacji
Abstrakty
In the Solar System, the coming into existence of a peculiar, fully developed atmosphere on Earth was determined by the ‘Great Oxidation Event’ at the turn of the Proterozoic and Palaeozoic. Within about 600 million years, there were large changes in oxygen concentrations in this atmosphere, ranging from 15 to 35 per cent, having been determined by a combination of cosmic-climatic, tectonic-volcanic and biological phenomena. A particular environmental change occurred at the beginning of the 19th century, as a result of the overlap of the end of the natural Little Ice Age and the beginning of anthropogenic warming of the ‘industrial revolution’. According to the author, the rate of human impact on environmental changes is estimated at about 15 per cent. The appearance of mankind brought new changes in the natural environment, including the oxygen content of the air. The current scale of anthropogenic impact justifies the introduction of a new time slice in the planet’s history - the Anthropocene. The functioning of civilisation is conditioned by meeting energy needs, to be implemented by creating a system of energy generators, among which the heat of the Earth should be an important component. The energy generated from this inexhaustible and cost-free geo-resource should be seen as the most ecological among all currently used energy carriers.
Czasopismo
Rocznik
Tom
Strony
117--131
Opis fizyczny
Bibliogr. 48 poz.
Twórcy
autor
- Institute of Geology, Adam Mickiewicz University, Krygowski Street 12, 61-680 Poznań, Poland
Bibliografia
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- Jóźwiak, K., 2017. Zmienność stężeń gazów w powietrzu strefy aeracji środowiska naturalnego i przekształconego rolniczo [Variability of concentrations of gases in the air of the vadose zone in the natural and agriculturally converted environments]. Przegląd Geologiczny 65, 1075–1079 (in Polish with English summary).
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- Lyons, T.W., Reinhard, Ch.T. & Planavsky, N.J., 2014. Atmospheric oxygenation three billion years ago. Nature 506, 535–539.
- Łuszczyk, M., 2021. Spowolnienie wykorzystania zasobów naturalnych wyzwaniem współczesnej gospodarki. Nierówności Społeczne a Wzrost Gospodarczy 16, 423–434 (in Polish with English summary).
- Majewski, G. & Cichocka, D., 2012. Zmiany zawartości tlenu (O2) w powietrzu atmosferycznym aglomeracji warszawskiej w latach 2008–2009. Przegląd Naukowy – Inżyniernia i Kształtowanie Środowiska 56, 33–49 (in Polish with English summary).
- Martin, D., McKenna, H. & Livina, V., 2017. The human physiological impact of global deoxygenation. Journal of Physiological Sciences 67, 97–106.
- Michalski, J., 2003. Megalityczne zagadki [Megalithic puzzles]. Archeologia Żywa 1, 8–10 (in Polish).
- Milankovič, M., 1914. O pitanju astronomskih teorija lednih doba [On te problem of the astronomical theory of the Ice Ages]. [In:] Izvadak iz razprave. Priopćene u ‘Radu’, 204. Zagreb, pp. 140–150 (in Serbian).
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- Paulo, A. & Gałaś, A., 2011. Polska wyprawa naukowa do Peru [Polish scientific expedtion to Peru]. Przegląd Geologiczny 59, 58–68 (in Polish, with English summary).
- Reinhard, Ch.T., Planavsky, N.J., Gill, B.C., Ozaki, K., Robbins, L.J., Lyons, T.W., Fischer, W.W., Wang, Ch., Cole, D.B. & Konhauser, K.G., 2017. Evolution of the globar phosphorus cycle. Nature 541, 7637.
- Schmidt-Rohr, K., 2020. Oxygen is the high-energy molecule powering complex multicellular life. Fundamental corrections to traditional bioenergetics. ACS Omega 5, 2221–2233.
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- Shackleton, N.J. & Opdyke, N.D., 1973. Oxygen isotope and palaeomagnetic stratigraphy of equatorial Pacific core V28-238: oxygen isotope temperatures and ice volumes on a 105 and 106 year scale. Quaternary Research 3, 39–55.
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- Steinthorsdottir, M., Wolfarth, B., Kylander, M.E., Blaauw, M. & Reimer, P.J., 2013. Stomatal proxy record of CO2 concentrations from the last termination suggests an important role for CO2 at climate change transitions. Quaternary Science Reviews 68, 43–58.
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- Vinther, B.M., Buchardt, S.L., Clausen, H.B., Dahl-Jensen, D., Johnsen, S.J., Fisher, D.A., Koerner, R.M., Raynaud, D., Lipenkov, V., Andersen, K.K., Blunier, T., Rasmussen, S.O., Steffenson, J.P. & Svensson, A.M., 2009. Holocene thinning of the Greenland ice sheet. Nature 461, 385–388.
- Wagner, F., Aaby, B. & Visscher, H., 2002. Rapid atmospheric CO2 changes associated with the 8,200-years-B.P. cooling event. Proceedings of the National Academy of Sciences USA 99, 12011–12014.
- Waters, C.N., Williams, M., Zalasiewicz, J.,Turner, S.D., Barnosky, A.D., Head, M.J., Wing, S.L., Wagreich, Ch.M., Steffen, W., Summerhayes, C.P., Cundy, A.B., Zinke, J., Fiałkiewicz-Kozieł, R., Leinfelder, R., Haff, P.K., McNeill, J.R., Rose, N.L., Hajdas, I., McCarthy, F.M.G., Cearreta, A., Gałuszka, A., Syvitski, J., Han, Y., An, Z., Fairchild, J.J., Ivardosul, J. & Jeandel, C., 2022. Epochs, events and episodes: Marking the geological impact of humans. Earth-Science Reviews 234, 104171.
- Zahnle, K., Schaefer, L. & Fegley, B. 2010. Earth’s earliest atmospheres. [In:] Deamer, D. & Szostak, J.W. (Eds): Additional perspectives on the origins of life. Cold Spring Harbor Perspectives in Biology, 1–17 pp.
- Zalasiewicz, J., Williams, M., Haywood, A. & Ellis, M., 2011. The Anthropocene a new epoch of geological time? Phylosophical Transactions of the Royal Society. Mathematical, Physical and Engineering Sciences 369, 1938.
Uwagi
Opracowanie rekordu ze środków MNiSW, umowa nr SONP/SP/546092/2022 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2024).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-1ba05e25-0ca3-4f5e-9ec9-4f49c8857f8a