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Panthalassa

  • Timeline of Natural History

    Timeline of Natural History

  • Assembly, Configuration, and Break-Up History of Rodinia

    Assembly, Configuration, and Break-Up History of Rodinia

  • Proto-Adamastor Ocean Crust (920 Ma) Described in Brasiliano Orogen from Coetaneous Zircon and Tourmaline

    Proto-Adamastor Ocean Crust (920 Ma) Described in Brasiliano Orogen from Coetaneous Zircon and Tourmaline

  • Early Paleozoic Post-Breakup Magmatism Along the Cordilleran Margin of Western North America: New Zircon U-Pb Age And

    Early Paleozoic Post-Breakup Magmatism Along the Cordilleran Margin of Western North America: New Zircon U-Pb Age And

  • Dinosaurs.Pdf

    Dinosaurs.Pdf

  • Download File

    Download File

  • Elevated CO2 Degassing Rates Prevented the Return of Snowball Earth During the Phanerozoic

    Elevated CO2 Degassing Rates Prevented the Return of Snowball Earth During the Phanerozoic

  • Intra-Panthalassa Ocean Subduction Zones Revealed by Fossil Arcs and Mantle Structure D

    Intra-Panthalassa Ocean Subduction Zones Revealed by Fossil Arcs and Mantle Structure D

  • Earth's Tectonic History

    Earth's Tectonic History

  • The Paleozoic Minimum in 87Sr/86Sr Ratio in the Capitanian (Middle

    The Paleozoic Minimum in 87Sr/86Sr Ratio in the Capitanian (Middle

  • Permian World Brochure

    Permian World Brochure

  • Plate Driven Extension and Convergence Along the East Gondwana Active Margin: Late Silurian–Middle Devonian Tectonics of the L

    Plate Driven Extension and Convergence Along the East Gondwana Active Margin: Late Silurian–Middle Devonian Tectonics of the L

  • Panel 3: Phanerozoic (541 Ma to Now) © Walter Álvarez, 2019

    Panel 3: Phanerozoic (541 Ma to Now) © Walter Álvarez, 2019

  • Supercontinent Reconstruction the Palaeomagnetically Viable, Long

    Supercontinent Reconstruction the Palaeomagnetically Viable, Long

  • Different Triggers for the Two Pulses of Mass Extinction Across the Permian

    Different Triggers for the Two Pulses of Mass Extinction Across the Permian

  • Speculations on the Mechanisms for the Formation and Breakup of Supercontinents

    Speculations on the Mechanisms for the Formation and Breakup of Supercontinents

  • Late Paleozoic Glaciation and Ice Sheet

    Late Paleozoic Glaciation and Ice Sheet

  • EPSC 233: Earth and Life History

    EPSC 233: Earth and Life History

Top View
  • Selva Mariana Marroquín Higher Education
  • Paleoecological Successions from Shallow-Marine Depositional Environments in Upper Silurian Carbonate Rocks of Blair County, Pennsylvania
  • GSA TODAY North-Central, P
  • Dynamic Carboniferous Tropical Forests: New Views of Plant Function and Potential for Physiological Forcing of Climate
  • Permian Monsters: Life Before the Dinosaurs’
  • Molecular and Isotopic Evidence Reveals the End-Triassic Carbon Isotope Excursion Is Not from Massive Exogenous Light Carbon
  • Extending Full-Plate Tectonic Models Into Deep Time: Linking the Neoproterozoic and the Phanerozoic
  • Models of Rodinia Assembly and Fragmentation
  • Impact of 10-Myr Scale Monsoon Dynamics on Mesozoic Climate And
  • Distribution of Oceans and Continents
  • Extreme Eolian Delivery of Reactive Iron to Late Paleozoic Icehouse Seas
  • The Challenge of Reconstructing the Phanerozoic Sea Level and the Pacific Basin Tectonics
  • UNIT 13: the Icehouse–Hothouse of the Late Paleozoic Ice Age, Coal-Forming Environments, and Their Non-Analog Vegetation
  • Using Network Analysis to Trace the Evolution of Biogeography Through Geologic Time: a Case Study
  • Geological History of Earth
  • Cisuralian and Guadalupian Global Paleobiogeography of Fusulinids In
  • Earth Science Chapter 10
  • The Colonization of the Oceans by Calcifying Pelagic


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