Understanding Earth's Deep Past Lessons for Our Climate Future (2011) / Chapter Skim
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References
References
Pages 149-178
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Scheckler, 1995. Late Devonian oceanic anoxic events and biotic crises: "Rooted" in the evolution of vascular land plants?
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Phanerozoic biodiversity mass extinctions. Annual Review of Earth and Planetary Sciences 34: 127-155.
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GEOCARBSULF: A combined model for Phanerozoic atmospheric O2 and CO2. Geochimica et Cosmochimica Acta 70: 5653-5664.
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Earth and Planetary Science Letters 230: 227-240. Cao, M., and Woodward, F.I., 1998.
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Climate-driven biotic change in the marine Permian of eastern Australia during the aftermath of the late Paleozoic Ice Age. Geological Society of America Abstracts with Programs 39: 354.
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Isotopic evidence for Fe cycling and repartitioning in ancient oxygen-deficient settings: Examples from black shales of the mid to late Devonian Appalachian basin. Earth and Planetary Science Letters 290: 244-253.
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Roberts, 2008. Strati graphic imprint of the late Palaeozoic Ice Age in eastern Australia: A record of alternat ing glacial and nonglacial climate regime.
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Evidence for rapid climate change in North America during the latest Paleocene Thermal Maximum: Oxygen isotope compositions of biogenic phosphate from the Bighorn Basin (Wyoming)
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Orbital chronology of Early Eocene hyperthermals from the Contessa Road section, central Italy. Earth and Planetary Science Letters 290: 192-200.
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Carbon-isotope record of the Early Jurassic (Toarcian) Oceanic Anoxic Event from fossil wood and marine carbonate (Lusitanian basin, Portugal)
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Middle-late Cretaceous climate of the southern high latitudes -- Stable isotopic evidence for minimal equator-to-pole thermal gradients. Geological Society of America Bulletin 107: 1164-1191.
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Erel, 2007. Nitrate reduction, sulfate reduc tion, and sedimentary iron isotope evolution during the Cenomanian-Turonian oceanic anoxic event.
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Astronomically tuned geomagnetic polarity time scale for the Late Triassic. Journal of Geophysical Research 104: 12831-12841.
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The impact of Miocene atmospheric carbon dioxide fluctuations on climate and the evolution of terrestrial ecosystems. Proceedings of the National Academy of Sciences USA 105: 449-453.
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Climate impact of Late Quaternary equatorial Pacific sea surface temperature variations. Science 289: 1719-1724.
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carbon isotope excursions: A comparison of their time scales, associated environmental change, causes and consequences. Journal of the Geological Society 165: 875-880.
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The δ44Ca temperature calibration on fossil and cultured Globigerinoides sacculifer: New tool for reconstruction of past sea surface temperatures. Geochemistry Geophysics Geosystems 1: 2000GC000091.
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Geological Society of America Special Papers 356: 505-522. Olsen, P.E., D.V.
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Hall, 2001. Warm tropical sea surface temperatures in the Late Cretaceous and Eocene epochs.
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High-precision U-Pb zircon age constraints on the Carboniferous-Permian bound ary in the southern Urals stratotype. Earth and Planetary Science Letters 256: 244-257.
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Effect of changes in δ18O con tent of the surface ocean on estimated sea surface temperatures in past warm climate. Paleoceanography 21: PA2023, 7 pp.
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. Earth and Planetary Science Letters 295: 262-276.
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Towards calibration of the TEX86 palaeothermometer for tropical sea surface temperatures in ancient green house worlds. Organic Geochemistry 38: 1537-1546.
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Moran, 2006. Subtropical Arctic Ocean temperatures during the Palaeocene/Eocene thermal maximum.
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High-resolution stable isotope records from the Upper Cretaceous rocks of Italy and Spain: Glacial episodes in a greenhouse planet? Geological Society of America Bulletin 112: 308-319.
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Modeling phosphorus cycling and carbon burial during Cretaceous Oceanic Anoxic Events. Earth and Planetary Science Letters 286: 71-79.
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Beckmann, 2004. Euxinia and primary production in Late Cretaceous eastern equatorial Atlantic surface waters fostered orbitally driven formation of marine black shales.
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Premoli-Silva, 2003. A transient rise in tropical sea surface temperature during the Paleocene-Eocene Thermal Maximum.
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An explanation of the effect of seawater carbonate concentration on foraminiferal oxygen isotopes. Geochimica et Cosmochimica Acta 63: 2001-2007.
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