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1 - Geological Time

The Court Jester on the Platform of Life

Published online by Cambridge University Press:  05 August 2014

John L. Brooke
Affiliation:
Ohio State University
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Summary

Human history begins with human evolution, and human evolution is grounded in biological evolution, and this is where we must begin. Equally fundamentally, the evolution of life on earth must be seen as inexorably interwoven with its context, the earth itself, and its history. Throughout this book, we explore these interconnections, and they should be spelled out here at the outset: human history is continuous with natural history, and nature indeed has a history.

The central facts of this history are threefold. First, life and the physical constituents of the earth and the sun – a continuum running from the fiery iron of the earth’s inner core out to beyond the reach of the solar wind – have been powerfully interconnected for billions of years. Second, this interaction has been complex and unstable over these billions of years; the earth has been a shifting and volatile platform for life. Third, this instability on a rough world has shaped the specific course that evolution has taken. All earthly life forms owe their very existence to a rough instability and a growing complexity that gives the planet its unique character.

This is an understanding of evolution and the planet earth that has its immediate roots in a wave of scientific advances that began in the 1960s and 1970s. During these decades, the prevailing gradualist orthodoxy gave way to a specific earth history of dramatic moments of interconnected environmental and evolutionary change. At the same time, the boundaries between scientific disciplines collapsed, as biologists, geologists, and atmospheric scientists began to work together as never before to unravel the complex story of the evolution of life and the history of its unique planetary platform, the earth itself. This chapter sketches the emerging synthesis that is developing from this intellectual revolution, but first we need to consider the revolution’s central elements.

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Publisher: Cambridge University Press
Print publication year: 2014

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References

Huxley, Julian, Evolution: The Modern Synthesis (London, 1942)
Dawkins, Richard, The Blind Watchmaker: Why the Evidence of Evolution Reveals a Universe without Design (New York, 1986; rev. ed., 1996)
Loper, David E., “Scorched Earth: How Heat from the Core Triggers Surface Upheaval,” The Sciences 30 (1990), 23Google Scholar
Eldridge, Niles, Reinventing Darwin: The Great Debate at the High Table of Evolutionary Theory (New York, 1995)
Hsü, Kenneth J., “Uniformitarianism vs. Catastrophism in the Extinction Debate,” in William Glen, The Mass-Extinction Debates: How Science Works in a Crisis (Stanford, CA, 1994), 217–29
Gould, Stephen Jay, “Is a New and General Theory of Evolution Emerging?Paleobiology 6/1 (1980), 119–30Google Scholar
–, The Structure of Evolutionary Theory (Cambridge, MA, 2002), 451–66, 535–6
Lovelock, James, Ages of Gaia: A Biography of Our Living Earth (New York, 1988), 9–10
Cox, Allan, ed., Plate Tectonics and Geomagnetic Reversals (San Francisco, CA, 1973)
Glen, William, The Road to Jaramillo: Critical Years of the Revolution in Earth Science (Stanford, CA, 1982), 1–3
Newell, Norman D., “Paleontological Gaps and Geochronology,” Journal of Paleontology. 36 (1962), 592–610Google Scholar
–, “Revolutions in the History of Life,” Geological Society of American Special Papers 89 (1967), 63–91
Benton, Michael J., “Scientific Methodologies in Collision: The History of the Study of the Extinction of the Dinosaurs,” Evolutionary Biology 24 (1990), 371–400Google Scholar
Raup, David M., “Taxonomic Diversity during the Phanerozoic,” Science 177 (1972), 1065–71Google Scholar
Schneider, Stephen H., “Debating Gaia,” Environment 32 (1990), 5–9, 29–32Google Scholar
Margulis, Lynn and Dolan, Michael F., Early Life: Evolution on the Precambrian Earth, second edition (Boston, MA, 2002)
Lovelock, James, The Vanishing Face of Gaia: A Final Warning (New York, 2009), 159–203
Eldridge, Niles and Gould, Stephen Jay, “Punctuated Equilibria: An Alternative to Phyletic Gradualism,” in Schopf, Thomas J. M., ed., Models in Paleobiology (San Francisco, CA, 1972), 82–115
Gould, Stephen Jay and Eldridge, Niles, “Punctuated Equilibria: The Tempo and Mode of Evolution Reconsidered,” Paleobiology 3 (1977), 115–51Google Scholar
Mayr, Ernst, Systematics and the Origin of Species (New York, 1942)
Mayr, Ernst, Animal Species and Evolution (Cambridge, MA, 1963)
Gould, , “The Evolution of Life on Earth,” in Life in the Universe: SA, A Special Issue (New York, 1995), 53–65
Vrba, Elizabeth S., “Turnover Pulses, The Red Queen, and Related Topics,” AJS 293 (1993), 414–52Google Scholar
Mass Turnover and Heterochrony Events in Response to Physical Change,” Paleobiology 31 (2005), 157–214
Dennett, Daniel C., Darwin’s Dangerous Idea: Evolution and the Meanings of Life (New York, 1995)
Vermeij, Geerat J., Nature: An Economic History (Princeton, NJ, 2004)
Valen, Leigh Van, “A New Evolutionary Law,” Evolutionary Theory 1 (1973), 1–30Google Scholar
Barnosky, Anthony D., “Distinguishing the Effects of the Red Queen and the Court Jester on Miocene Mammal Evolution in the Northern Rocky Mountains,” Journal of Vertebrate Paleontology 21 (2001), 172–85Google Scholar
Jablonski, David, “Biotic Interactions and Macroevolution: Extensions and Mismatches across Scales and Levels,” Evolution 62 (2008), 715–39Google Scholar
Finnegan, Seth et al., “The Red Queen Revisited: Reevaluating the Age Selectivity Phanerozoic Marine Genus Extinctions,” Paleobiology 34 (2008), 318–41Google Scholar
Benton, Michael J., “The Red Queen and the Court Jester: Species Diversity and the Role of Biotic and Abiotic Factors through Time,” Science 323 (2009), 728–32Google Scholar
Ezard, Thomas H. G. et al., “Interplay between Changing Climate and Species Ecology Drives Macroevolutionary Dynamics,” Science 332 (2011), 349–51Google Scholar
Venditti, Chris et al., “Phylogenies Reveal New Interpretations of Speciation and the Red Queen,” Nature 463 (2010), 349–52Google Scholar
Stanley, Steven M., “Rates of Evolution,” Paleobiology 11 (1985), 15–26Google Scholar
Brett, Carlton et al., “Coordinated Stasis: An Overview,” PPP 127 (1996), 1–20Google Scholar
DiMichele, W. A. et al., “Long-Term Stasis in Ecological Assemblages: Evidence from the Fossil Record,” Annual Review of Ecology, Evolution, and Systematics, 35 (2004), 285–322Google Scholar
Hairston, Nelson G. et al., “Rapid Evolution and the Convergence of Ecological and Evolutionary Time,” Ecology Letters 8 (2005), 1114–27Google Scholar
Handley, John C. et al., “Probability Models for Stasis and Change in Paleocommunity Structure,” Palaios 24 (2009), 638–49Google Scholar
Gould, , “Is a New and General Theory of Evolution Emerging?”, 119–30; “Darwinism and the Expansion of Evolutionary Theory,” Science 216 (1982), 380–7Google Scholar
Gould, Stephen J. and Vrba, Elizabeth S., “Exaptation – A Missing Term in the Science of Form,” Paleobiology 8 (1982), 4–15Google Scholar
Leiberman, Bruce S. and Vrba, Elizabeth S., “Stephen Jay Gould on Species Selection: 30 Years of Insight,” Paleobiology 312 (2005), 113–21Google Scholar
Gould, fired back with both barrels in “Darwinian Fundamentalism,” New York Review of Books, 44, June 12, 1997, 34–7Google Scholar
Evolution: The Pleasures of Pluralism,” New York Review of Books 44, June 26, 1997, 47–52
Reid, Robert G. B., Biological Emergences: Evolution by Natural Experiment (Cambridge, MA, 2007), esp. 75–94, 289–328, 401–36
Jablonka, Eva and Lamb, Marian J., Evolution in Four Dimensions: Genetic, Epigenetic, Behavioral, and Symbolic Variation in the History of Life (Cambridge, MA, 2005)
West-Eberhard, Mary-Jane, Developmental Plasticity and Evolution (New York, 2003)
Reid, Robert G. B., Evolutionary Theory: The Unfinished Synthesis (Beckenham, 1985)
Carey, Nessa, The Epigenetics Revolution: How Modern Biology is Rewriting Our Understanding of Genetics, Disease, and Inheritance (New York, 2012)
Ruden, Douglas M., “The (New) New Synthesis and Epigenetic Capacitors of Morphological Evolution,” NatGen 43 (2011), 88–9Google Scholar
Parsons, Peter A., “The Importance and Consequences of Stress in Living and Fossil Populations: From Life-History Variation to Evolutionary Change,” The American Naturalist 142, suppl. (1993), S5–S20.Google Scholar
Lindquist, Susan, “The Heat-Shock Response,” Annual Reviews in Biochemistry 55 (1986), 1151–91Google Scholar
Rutherford, Suzanne L. and Lindquist, Susan, “Hsp90 as a Capacitor for Morphological Evolution,” Nature 396 (1998), 336–42Google Scholar
Feder, M. E. and Hoffman, G. E., “Heat-Shock Proteins, Molecular Chaperones, and the Stress Response: Evolutionary and Ecological Physiology,” Annual Review of Physiology 61 (1999), 243–82Google Scholar
Queiltsch, Christine et al., “Hsp90 as a Capacitor for Phenotypic Variation,” Nature 417 (2002), 618–24Google Scholar
Jackson, Sophie E. et al., “Hsp90: From Structure to Phenotype,” Nature Structural & Molecular Biology 11 (2004), 1152–5Google Scholar
Reusch, Thorsten B. R. H. and Wood, Troy E., “Molecular Ecology of Global Change,” Molecular Ecology 16 (2007), 3973–92Google Scholar
Sørensen, Jesper G. and Loeschcke, Volker, “Studying Stress Responses in the Post-Genomic Era: Its Ecological and Evolutionary Role,” Journal of Bioscience 32 (2007), 447–56Google Scholar
Halfmann, Randal and Lindquist, Susan, “Epigenetics in the Extreme: Prions and the Inheritance of Environmentally Acquired Traits,” Science 330 (2010), 629–32Google Scholar
Jarosz, Daniel F. and Lindquist, Susan, “Hsp90 and Environmental Stress Transform the Adaptive Value of Natural Genetic Variation,” Science 330 (2010), 1820–4Google Scholar
Gangaraju, Vamsi K. et al., “Drosophila Piwi Functions in Hsp90-Mediated Suppression of Phenotypic Variation,” NatGen 43 (2011), 153–8Google Scholar
Yahara, Ichiro, “The Role of Hsp90 in Evolution,” Genes to Cells 4 (1999), 375–9Google Scholar
McLaren, Anne, “Too Late for the Midwife Toad: Stress, Variability and Hsp90,” Trends in Genetics 15 (1999), 169–71Google Scholar
Holmes, Bob, “Ready, Steady, Evolve,” New Scientist 175/2362 (Sept. 28, 2002), 28–31Google Scholar
Sørensen, Jesper G. et al., “The Evolutionary Ecological Role of Heat Shock Proteins,” Ecology Letters 6 (2003), 1025–37Google Scholar
Wray, Gregory A., “Punctuated Evolution of Embryos,” Science 267 (1995), 1115–16Google Scholar
Pagel, Mark, “Inferring the Historical Patterns of Biological Evolution,” Nature 401 (1999), 877–84Google Scholar
Barracough, Timothy G. and Savolainen, Vincent, “Evolutionary Rates and Species Diversity in Flowering Plants,” Evolution 55 (2001), 677–83Google Scholar
Webster, Andrea J. et al., “Molecular Phylogenies Link Rates of Evolution and Speciation,” Science 301 (2003), 478Google Scholar
Lande, R., “Adaptation to an Extraordinary Environment by Evolution of Phenotypic Plasticity and Genetic Assimilation,” Journal of Evolutionary Biology 22 (2009), 1435–46Google Scholar
McQuigan, Katrina and Sgrò, Sarla M., “Evolutionary Consequences of Cryptic Genetic Variation,” Trends in Ecology and Evolution 24 (2009), 305–11Google Scholar
Lindsay, J. F. and Brasier, M. D., “Did Global Tectonic Drive Early Biosphere Evolution? Carbon Isotope Records from 2.6 to 1.9 Ga Carbonates of Western Australian Basins,” Precambrian Research 114 (2002), 30Google Scholar
Sleep, N. H. et al., “Initiation of Clement Surface Conditions on the Earliest Earth,” PNAS 98 (2001), 3666–72Google Scholar
Cowen, R.An Early Cosmic Wallop for Life on Earth?Science News 158 (2000), 357Google Scholar
Moorbath, Stephen, “Dating Earliest Life,” Nature 434 (2005), 155Google Scholar
Knoll, Andrew H., Life on a Young Planet: The First Three Billion Years of Evolution on Earth (Princeton, NJ, 2003), 16–88
Ruddiman, William F., Earth’s Climate: Past and Future (New York, 2001), 87–102
Eriksson, Patrick G. et al., “Patterns of Sedimentation in the Precambrian,” SedGeol 176 (2005), 17–42Google Scholar
Condie, Kent C., “Episodic Continental Growth Models: Afterthoughts and Extensions,” Tectonophysics 322 (2000), 153–62Google Scholar
Loper, David E., “Mantle Plumes and Their Effects on the Earth’s Surface: A Review and Synthesis,” Dynamics of Atmospheres and Oceans 27 (1997), 35–54Google Scholar
Brandson, Alan D. and Walker, Richard J., “The Debate over Core-Mantle Interaction,” EPSL 232 (2005), 211–35Google Scholar
Muller, Richard A., “Avalanches at the Core-Mantle Boundary,” GRL 29 (2002), 41–1–41–4Google Scholar
Shirey, Steven B. and Richardson, Stephen H., “Start of the Wilson Cycle at 3 Ga Shown by Diamonds from Subcontinental Mantle,” Science 333 (2011), 434–6Google Scholar
Rogers, John J. W., “A History of Continents in the Past Three Billion Years,” JGeol 104 (1996), 91–107Google Scholar
Rogers, John J. W. and Santosh, M., “Supercontinents in Earth History,” Gondwana Research 6 (2003), 357–68Google Scholar
Eriksson, Patrick G. et al., eds., The Precambrian Earth: Tempo and Events (Amsterdam, 2004), 584
Goldblatt, Colin et al., “Bistability of Atmospheric Oxygen and the Great Oxidation,” Nature 443 (2006), 683–6Google Scholar
Kopp, Robert E. et al., “The Paleoproterozoic Snowball Earth: A Climate Disaster Triggered by the Evolution of Oxygen Photosynthesis,” PNAS 102 (2005), 11131–6Google Scholar
Kirschvink, Joseph L. et al., “Paleoproterozoic Snowball Earth: Extreme Climatic and Geochemical Global Change and its Biological Consequences,” PNAS 97 (2000), 1400–5Google Scholar
Marmais, David J. Des, “Isotopic Evolution of the Biogeochemical Carbon Cycle during the Proterozoic Eon,” Organic Geochemistry 27 (1997), 185–93Google Scholar
Brasier, M. D. and Lindsay, J. F., “A Billion Years of Environmental Stability and the Emergence of Eukaryotes: New Data from Northern Australia,” Geology 26 (1996), 555–8Google Scholar
Catling, David C. and Claire, Mark W., “How Earth’s Atmosphere Evolved to an Oxic State: A Status Report,” EPSL 237 (2005), 1–20Google Scholar
Albani, Abderrazak El et al., “Large Colonial Organisms with Coordinated Growth in Oxygenated Environments, 2.1 Gyr Ago,” Nature 466 (2010), 100–4Google Scholar
Shixing, Zhu and Huineng, Chen, “Megascopic Multicellular Organisms from the 1700-Million-Year-Old Tuanshnazi Formation in the Jixian Area, North China,” Science 270 (1995), 620–2Google Scholar
Wray, Gregory A. et al., “Molecular Evidence for Deep Precambrian Divergences among Metazoan Phyla,” Science 274 (1996), 568–73Google Scholar
Seilacher, Adolf et al., “Triploblastic Animals More than 1 Billion Years Ago: Trace Fossil Evidence from India,” Science 282 (1998), 80–2Google Scholar
Rasmussen, Birger et al., “Discoidal Impressions and Trace-like Fossils More Than 1200 Million Years Old,” Science 296 (2002), 1112–15Google Scholar
Levinton, Jeffrey et al., “Simulations of Evolutionary Radiations and their Application to Understanding the Probability of a Cambrian Explosion,” Journal of Paleontology 78 (2004), 31–8Google Scholar
Knauth, L. Paul and Kennedy, Martin J., “The Late Precambrian Greening of the Earth,” Nature 460 (2009), 728–32Google Scholar
Dalziel, Ian W. D., “Neoproterozoic-Paleozoic Geography and Tectonics: Review, Hypothesis, Environmental Speculation,” GSA Bulletin 109 (1997), 16–42Google Scholar
Kirschvink, Joseph L., “Late Proterozoic Low-Latitude Global Glaciation: The Snowball Earth,” in Schopf, J. W. and Klein, C., eds., The Proterozoic Biosphere (New York, 1992), 51–2
Hoffman, Paul et al., “A Neoproterozoic Snowball Earth,” Science 281 (1998), 1342–6Google Scholar
Evans, David A. D., “Stratigraphic, Geochronological, and Paleomagnetic Constraints upon the Neoproterozoic Climatic Paradox,” AJS 300 (2000), 347–433Google Scholar
Schrag, Daniel P. and Hoffman, Paul F., “Life, Geology, and Snowball Earth,” Nature 409 (2001), 306Google Scholar
Maruyama, S. and Santosh, M., “Models of Snowball Earth and Cambrian Explosion: Synopsis,” Gondwana Research 14 (2008), 22–32Google Scholar
Kerr, Richard A., “Snowball Earth Has Melted Back to a Profound Wintry Mix,” Science 327 (2010), 1186Google Scholar
Walker, Gabrielle, Snow Ball Earth: The Story of the Great Global Catastrophe That Spawned Life as We Know It (New York, 2003)
Lenton, Timothy M. and Watson, Andrew J., “Biotic Enhancement of Weathering, Atmospheric Oxygen, and Carbon dioxide in the Neoproterozoic,” GRL 31 (2004), L05202 (1–5)Google Scholar
Donnadieu, Yannick et al., “A ‘Snowball Earth’ Triggered by Continental Break-Up through Changes in Runoff,” Nature 428 (2004), 303–6Google Scholar
Prokoph, Andreas et al., “Time-Series Analysis of Large Igneous Provinces: 3500Ma to Present,” JGeol 112 (2004), 1–22Google Scholar
Butterfield, Nichols J., “Macroevolution and Macroecology through Deep Time,” Palaeontology 50 (2007), 41–55Google Scholar
Fischer, Alfred B., “Climatic Oscillations in the Biosphere,” in Nitecki, M. H., ed., Biotic Crises in Ecological and Evolutionary Time (New York, 1981), 103–31
Fischer, Alfred G., “The Two Phanerozoic Supercycles,” in Berggren, W. A. and Van Couvering, J. A., eds., Catastrophes in Earth History: The New Uniformitarianism (Princeton, NJ, 1984), 129–50
Nance, R. Damian et al., “Post-Archean Biogeochemical Cycles and Long-Term Episodicity in Tectonic Process,” Geology 14 (1986), 514–18Google Scholar
– “The Supercontinent Cycle,” SA 259 (July, 1988), 72–9
Murphy, J. Brendan and Nance, R. Damian, “Mountain Belts and the Supercontinent Cycle,” SA 266 (April 1992), 84–91Google Scholar
Veevers, John J., “Tectonic-Climatic Supercycles in the Billion-Year Plate-Tectonic Eon: Permian Pangean Icehouse Alternates with Cretaceous Dispersed-Continents Greenhouse,” SedGeol 68 (1990), 1–16Google Scholar
Frakes, Lawrence A. et al., Climate Modes of the Phanerozoic: The History of the Earth’s Climate over the Past 600 Million Years (Cambridge, 1992)
Rino, S. et al., “The Grenvillian and Pan-African Orogens: World’s Largest Orogenies through Geological Time, and Their Implications on the Origin of the Superplume,” Gondwana Research 14 (2008), 51–72Google Scholar
Ernst, R. E. et al., “Global Record of 1600–700 Ma Large Igneous Provinces (LIPs): Implications for the Reconstruction of the Proposed Nuna (Columbia) and Rodinia Supercontinents,” Precambrian Research 160 (2008), 159–78Google Scholar
Glikson, A. Y., “Milestones in the Evolution of the Atmosphere with Reference to Climate Change,” Australian Journal of Earth Sciences 55 (2005), 125–39, esp. 125–30Google Scholar
Islay, Ann E. and Abbot, Dallas H., “Implications of the Temporal Distribution of High-MG Magmas for Mantle Plume Volcanism through Time,” JGeol 110 (2002), 141–58Google Scholar
Rampino, Michael R. and Caldiera, Ken, “Major Episodes of Geological Change: Correlations, Time Structure and Possible Causes,” EPSL 114 (1993), 215–27Google Scholar
Courtillot, V. et al., “On the Causal Links between Flood Basalts and Continental Breakup,” EPSL 166 (1999), 177–95Google Scholar
Condie, Kent C., “The Supercontinent Cycle: Are there Two Patterns of Cyclicity?Journal of African Earth Sciences 35 (2002), 179–83Google Scholar
Hays, James D. and Pitman, Walter C., “Lithospheric Plate Motion, Sea Level Changes and Climatic and Ecological Consequences,” Nature 246 (1973), 18–22Google Scholar
Andel, Tjeerd H. Van, New Views on an Old Planet: A History of Global Change, second edition (New York, 1994), 175–251
Berner, Robert A., “GEOCARBSULF: A Combined Model for Phanerozoic Atmospheric O2 and CO2, Geochimica et Cosmochimica Acta 70 (2006), 5653–64Google Scholar
Inclusion of the Weathering of Volcanic Rocks in the GEOCARBSULF Model,” AJS 306 (2006), 295–302
Royer, Dana L. et al., “CO2 as a Primary Driver of Phanerozoic Climate,” GSA Today 14/3 (March 2004), 4–10Google Scholar
Bergman, Noam M. et al., “COPSE: A New Model of Biogeochemical Cycling over Phanerozoic Time,” AJS 304 (2004), 397–437Google Scholar
Beerling, D. J. and Royer, D. L., “Fossil Plants as Indicators of the Phanerozoic Global Carbon Cycle,” Annual Reviews of Earth and Planetary Sciences 30 (2001), 527–56Google Scholar
Rellaack, Gregory J., “A 300-Million-Year Record of Atmospheric Carbon Dioxide from Fossil Plant Cuticles,” Nature 411 (2001), 287–90Google Scholar
Veizer, Ján et al., “Evidence for Decoupling of Atmospheric CO2 and Global Climate during the Phanerozoic Eon,” Nature 408 (2000), 698–701Google Scholar
Rothman, Daniel H., “Atmospheric Carbon Dioxide Levels for the Last 500 Million Years,” PNAS 99 (2002), 4167–71Google Scholar
Rothman, Daniel H. et al., “Dynamics of the Neoproterozoic Carbon Cycle,” PNAS 100 (2003), 8128–9Google Scholar
Doney, Scott C. and Schimel, David S., “Carbon and Climate System Coupling on Timescales from the Precambrian to the Anthropocene,” Annual Reviews Environmental Resources 32 (2007), 31–66Google Scholar
Lowenstein, Tim K. et al., “Oscillations in Phanerozoic Seawater Chemistry: Evidence from Fluid Inclusions,” Science 294 (2001), 1086–8Google Scholar
Prokoph, Andreas and Veiser, Jan, “Trends, Cycles, and Nonstationaries in Isotope Signals of Phanerozoic Seawater,” Chemical Geology 161 (1999), 225–40Google Scholar
Prokoph, Andreas et al., “Phanerozoic Paleography, Paleoenvironment and Lithofacies Maps of the Circum-Atlantic Margins,” Marine and Petroleum Geology 20 (2003), 249–85Google Scholar
Wignall, Paul B., “Large Igneous Provinces and Mass Extinctions,” Earth-Science Reviews 53 (2001), 1–33, esp. 18–20, 24–6Google Scholar
Schaller, Morgan F. et al., “Atmospheric Pco2 Perturbations Associated with the Central Atlantic Magmatic Province,” Science 331 (2011), 1404–9Google Scholar
Hallam, Anthony and Wignall, Paul B., “Mass Extinctions and Sea-Level Changes,” Earth-Science Reviews 48 (1999), 217–50, esp. 238–42Google Scholar
Santosh, M. et al., “The Making and Breaking of Supercontinents: Some Speculations based on Superplumes, Super Downwelling, and the Role of the Tectosphere,” Gondwana Research 15 (2009), 324–41Google Scholar
Vermeij, Geerat J., Evolution and Escalation: An Ecological History of Life (Princeton, NJ, 1987)
Economics, Volcanoes, and Phanerozoic Revolutions,” Paleobiology 21 (1995), 125–52
Courtillot, V. and Gaudemer, Y., “Effects of Mass Extinctions on Biodiversity,” Nature 381 (1996), 146–8Google Scholar
Beerling, David J. and Berner, Robert A., “Feedbacks and the Coevolution of Plants and Atmospheric CO2,” PNAS 105 (2005), 1302–5Google Scholar
Retallack, Gregory J., “Early Forest Soils and Their Role in Devonian Global Change, Science 276 (1997), 583–5Google Scholar
Graham, J. B. et al., “Implications of the Late Paleozoic Oxygen Pulse for Physiology and Evolution,” Nature 375 (1995), 117–20Google Scholar
Ward, Peter D., Confirmation of Romer’s Gap as a Low Oxygen Interval Constraining the Timing of Initial Arthropod and Vertebrate Terrestrialization,” PNAS 103 (2006), 16816–22Google Scholar
Raup, David M. and Sepkoski, John J., “Mass Extinctions in the Marine Fossil Record,” Science 215 (1982), 1501–3Google Scholar
Periodicity of Extinctions in the Geological Past,” PNAS 81 (1984), 801–5
Alvarez, Luis W. et al., “Extraterrestrial Cause for the Cretaceous-Tertiary Extinction,” Science 208 (1980), 1095–108Google Scholar
Alvarez, Walter and Muller, Richard A., “Evidence from Crater Ages for Periodic Impacts in the Earth,” Nature (308 (1984), 718–20Google Scholar
Alvarez, Walter, “Toward a Theory of Impact Crises,” Eos 67 (1986), 649–58Google Scholar
Raup, David M., The Nemesis Affair: A Story of the Death of Dinosaurs and the Ways of Science (New York, 1999
Culler, Timothy S. et al., “Lunar Impact History from 40 Ar/39AR Dating of Glass Spherules,” Science 287 (2000), 1785–8Google Scholar
Glikson, Andrew, “Asteroid/Comet Impact Clusters, Flood Basalts and Mass Extinctions: Significance of Isotopic Age Overlaps,” EPSL 236 (2005), 933–7, at 935Google Scholar
Becker, L., “Benout: A Possible End-Permian Impact Crater Offshore of Northwestern Australia,” Science 304 (2004), 1469–76Google Scholar
Courtillot, Vincent, Evolutionary Catastrophes: The Science of Mass Extinction (New York, 1999)
Officer, Charles B. and Page, Jake, The Great Dinosaur Controversy (Reading, MA, 1996)
Sergeant, William A. S., “The ‘Great Extinction’ that Never Happened: The Demise of the Dinosaurs Considered,” Canadian Journal of Earth Science 38 (2001), 239–47Google Scholar
Morgan, J. Phipps et al., “Contemporaneous Mass Extinctions, Continental Flood Basalts, and ‘Impact Signals’: Are Mantle Plume-Induced Lithospheric Gas Explosions the Causal Link?EPSL 217 (2004), 263–84Google Scholar
Kelly, Simon, “The Geochronology of Large Igneous Provinces, Terrestrial Impact Craters, and Their Relationship to Mass Extinctions on Earth,” Journal of the Geological Society, London 164 (2007), 923–36Google Scholar
Wignall, Paul B. et al., “Volcanism, Mass Extinction, and Carbon Isotope Fluctuations in the Middle Permian of China,” Science 324 (2009), 1179–82Google Scholar
Alvarez, Walter concedes considerable ground in “Comparing the Evidence Relevant to Impact and Flood Basalts at Times of Major Mass Extinctions,” Astrobiology 3 (2003), 153–61Google Scholar
Hallam, Anthony and Wignall, Paul B., Mass Extinctions and Their Aftermath (New York, 1997)
Stigall, Alycia L., “Invasive Species and Biodiversity Crises: Testing the Link in the Late Devonian,” PLOS One 5 (2010), e15584Google Scholar
Isozaki, Yukio, “Integrated ‘Plume Winter’ Scenario for the Double-Phased Extinction during the Paleozoic-Mesozoic Transition: The G-LB and P-TB Events for a Panthalassian Perspective,” Journal of Asian Earth Sciences 36 (2009), 459–80Google Scholar
Keller, Gerta et al., “New Evidence Concerning the Age and Biotic Effects of the Chicxubub Impact in New Mexico,” Journal of the Geological Society, London 166 (2009), 393–411Google Scholar
Ruhl, Micha et al., “Atmospheric Carbon Injection Linked to End-Triassic Mass Extinction,” Science 333 (2011), 430–4Google Scholar
Isozaki, Yukio, “Illawarra Reversal: The Fingerprint of a Superplume that Triggered Pangean Breakup and the End-Guadalupian (Permian) Mass Extinction,” Gondwana Research 15 (2009), 421–32Google Scholar
Courtillot, Vincent and Olson, Peter, “Mantle Plumes Link Magnetic Superchrons to Phanerozoic Mass Depletion Events,” EPSL 260 (2007), 495–504Google Scholar
Dormy, Emmanuel and Le Mouël, Jean-Louis, “Geomagnetism and the Dynamo: Where Do We Stand?C. R. Physique 9 9 (2008), 711–20Google Scholar
Jones, Adrian P. et al., “Impact Induced Melting and the Development of Large Igneous Provinces,” EPSL 202 (2002), 551–61Google Scholar
Muller, Richard A. and Morris, Donal E., “Geomagnetic Reversals from Impacts on the Earth,” GRL 13 (1986), 177–1180Google Scholar
Reese, C. C. and Solomatov, V. S., “Early Martian Dynamo Generation due to Giant Impacts,” Icarus 207 (2010), 82–97Google Scholar
Abbott, Dallas and Islay, Ann E.similarly link impacts and plumes, suggesting that impacts regularly intensify plume activity, in “Extraterrestrial Influences on Mantle Plume Activity,” EPSL 205 (2002), 53–62Google Scholar
Shaw, Herbert R. in Craters, Cosmos, and Chronicles: A New Theory of Earth (Stanford, CA, 1994)
Kelley, Simon, “The Geochronology of Large Igneous Provinces, Terrestrial Impact Craters, and Their Relationship to Mass Extinctions on Earth,” Journal of the Geological Society 164 (2007), 923–36Google Scholar
Svensmark, Hendrik and Calder, Nigel, The Chilling Stars: A New Theory of Climate Change (Thriplow, Cambridge, 2007)
Courtillot, Vincent et al., “Are there Connections between the Earth’s Magnetic Field and Climate?EPSL 253 (2007), 328–39Google Scholar
Sahviv, Nir J., “The Spiral Structure of the Milky Way, Cosmic Rays, and Ice Age Epochs on Earth,” New Astronomy 8 (2003), 39–77Google Scholar
Shaviv, Nir J. and Veizer, Ján, “Celestial Driver of Phanerozoic Climate?GSA-Today 13 (2003), 4–10Google Scholar
Goncharov, G. N. and Orlov, V. V., “Global Repeating Events in the History of the Earth and the Motion of the Sun through the Galaxy,” Astronomy Reports 47 (2003), 925–33Google Scholar
Carslaw, K. S. et al., “Cosmic Rays, Clouds, and Climate,” Science 298 (2002), 1732–6Google Scholar
Gunderson, Lance H. and Holling, C. S., eds., Panarchy: Understanding Transformations in Human and Natural Systems (Washington, DC, 2002)

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  • Geological Time
  • John L. Brooke, Ohio State University
  • Book: Climate Change and the Course of Global History
  • Online publication: 05 August 2014
  • Chapter DOI: https://doi.org/10.1017/CBO9781139050814.003
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  • Geological Time
  • John L. Brooke, Ohio State University
  • Book: Climate Change and the Course of Global History
  • Online publication: 05 August 2014
  • Chapter DOI: https://doi.org/10.1017/CBO9781139050814.003
Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

  • Geological Time
  • John L. Brooke, Ohio State University
  • Book: Climate Change and the Course of Global History
  • Online publication: 05 August 2014
  • Chapter DOI: https://doi.org/10.1017/CBO9781139050814.003
Available formats
×