EvGeo
Geological Evolution of a Habitable Planet
Giovanni Muttoni - The State University of Milan
2022/2023 lessons in Room BS (Teams 1g3gn4r)
LECTURES (* are mandatory)
Part 0. Introduction
Class discussion on the basic requirements for simple life and complex life.
Introductory icebreaker lecture: how many Earths?
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Part I. Setting the scene: the first half billion years. Formation of a wet rocky planet
Halliday, A. N. (2006), The origin of the Earth-What's new?, Elements, 2(4), 205-210.
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Part II. Liquid water: origin
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Part III. Liquid water: maintenance. The long-term carbon cycle
Without the radiative forcing supplied by CO2 and the other noncondensing greenhouse gases, the terrestrial greenhouse would collapse, plunging the global climate into an icebound Earth state.
Zonal climate, plate tectonics & Earth's thermostat *
WHY DO WE NEED A CO2 OUTPUT? *
Climate sensitivity calculator
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The role of planetary albedo
The building of polar ice has the effect to amplificate – through enhanced planetary albedo – global cooling resulting from the reduction of greenhouse gases via CO2 weathering consumption of mafic rocks in the tropical humid belt.
Kent, D.V., Muttoni, G. Latitudinal land–sea distributions and global surface albedo since the Cretaceous. Palaeogeography, Palaeoclimatology, Palaeoecology 585, 110718, 2022.
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Part IV. Liquid water: climate extremes
...expectations are that the silicate weathering thermostat would always be operative at the high temperature end and act to limit global overheating. However, at times when continental drift focused the weathering-prone landmasses in the pCO2-insensitive equatorial belt, the low range of the thermostat could become decoupled from global climate, allowing Earth to descend into glacial modes of varying severity.
Hoffman, P. F., A. J. Kaufman, G. P. Halverson, and D. P. Schrag (1998), A Neoproterozoic snowball earth, science, 281(5381), 1342-1346.
Hoffman, P. F., and D. P. Schrag (2002), The snowball Earth hypothesis: testing the limits of global change, Terra nova, 14(3), 129-155.
Documentary 'Snowball Earth'
From the Early Eocene Climatic Optimum to the Neogene Ice Age *
Kent, D. V., and G. Muttoni (2008), Equatorial convergence of India and early Cenozoic climate trends, Proceedings of the National Academy of Sciences, 105(42), 16065-16070.
Kent, D. V., and G. Muttoni (2013), Modulation of Late Cretaceous and Cenozoic climate by variable drawdown of atmospheric pCO 2 from weathering of basaltic provinces on continents drifting through the equatorial humid belt, Climate of the Past, 9(2), 525-546.
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Part V. Oxygen
Kump, L. R. (2008), The rise of atmospheric oxygen, Nature, 451(7176), 277.
Shields-Zhou, G., and L. Och (2011), The case for a Neoproterozoic oxygenation event: geochemical evidence and biological consequences, GSA Today, 21(3), 4-11.
LECTURES
Part VI. Earth's magnetic shield
Magnetic shielding of atmosphere *
Tarduno, J. A., R. D. Cottrell, W. J. Davis, F. Nimmo, and R. K. Bono (2015), A Hadean to Paleoarchean geodynamo recorded by single zircon crystals, Science, 349(6247), 521-524.
Tarduno, J. A., E. G. Blackman, and E. E. Mamajek (2014), Detecting the oldest geodynamo and attendant shielding from the solar wind: Implications for habitability, Physics of the Earth and Planetary Interiors, 233, 68-87.
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Part VII. From simple to complex life
Knoll, A. H. (2014), Paleobiological perspectives on early eukaryotic evolution, Cold Spring Harbor Perspectives in Biology, 6(1), a016121.
Students' presentations
(see Students page, top left)
Brasier, M., and J. Antcliffe (2004), Decoding the Ediacaran enigma, Science, 305(5687), 1115-1117.
Xiao, S., and M. Laflamme (2009), On the eve of animal radiation: phylogeny, ecology and evolution of the Ediacara biota, Trends in Ecology & Evolution, 24(1), 31-40.
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Part VIII. Evolution of life: the role of catastrophism
The punctuated equilibrium theory of Gould and Eldredge,1993
Jay Gould, S., and N. Eldredge (1993), Punctuated equilibrium comes of age, Nature, 366(6452), 223.
Case Study #1: The P/T boundary *
Lane, N. (2007), Reading the book of death, Nature, 448(7150), 122-125.
Docu 'The day Earth nearly ended'
Case Study #2: The K/T boundary *
Richards+ (see also lecture below)
Pierazzo, E., and N. Artemieva (2012), Local and global environmental effects of impacts on Earth, Elements, 8(1), 55-60.
LECTURES
Part IX. The last two million years: how humans conquered planet Earth
When did we become 'human'? the evolution of Homo in Africa (lecture to come).
Ice Ages & First hominin colonization of Europe
Muttoni, G., G. Scardia, and D. V. Kent (2018), Early hominins in Europe: The Galerian migration hypothesis, Quaternary Science Reviews, 180, 1-29.
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Part X. Final discussion: from microbes to space missions
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RESOURCES & NEWS
NASA TV