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Showing 1 to 4 of 4 for “"Panthalassa"”.

  1. Marine Deoxygenation Predates the End-Triassic Mass Extinction Within the Equatorial Panthalassa and its Influence on Marine Ecosystems Before the Biotic Crisis

    … water marine deposition in eastern equatorial Panthalassa, likely capturing regional oceanic redox trends. δ15N records from Grotto Creek show a pronounced positive excursion of +3‰ that initiates in the upper Norian, peaks near the Norian-Rhaetian boundary (NRB; ~208.5), and declines through …

    vt Repository record for Marine Deoxygenation Predates the End-Triassic Mass Extinction Within the Equatorial Panthalassa and its Influence on Marine Ecosystems Before the Biotic Crisis (opens in a new tab)

  2. Biogeochemical Cycling and Paleoenvironmental Reconstructions of the Toarcian Oceanic Anoxic Event from Western North America

    … which was deposited on the eastern margin of the Panthalassa Ocean. The Toarcian carbon isotope excursions (CIEs) in the WCSB confirm that these features are global phenomena. I have suggested a new driver for small-scale CIEs observed during the event: the release of wetland-derived methane …

    vt Repository record for Biogeochemical Cycling and Paleoenvironmental Reconstructions of the Toarcian Oceanic Anoxic Event from Western North America (opens in a new tab)

  3. The impact of global environmental changes on exceptional preservation, extinction, and recovery in the early Jurassic (late Pliensbachian-Toarcian)

    … different geographical locations (Tethys versus Panthalassa Oceans) and depositional settings (shallow water carbonates versus deeper water shales). Scanning Electron Microscopy (SEM) and Energy Dispersive X-Ray Spectroscopy (EDS) analyses showed phosphatization is the main preservation pathway …

    texas Repository record for The impact of global environmental changes on exceptional preservation, extinction, and recovery in the early Jurassic (late Pliensbachian-Toarcian) (opens in a new tab)

  4. New Constraints For Convergent Margin Plate Tectonic Reconstructions From Imaged And Predicted Mantle Structure

    Details of global plate models decrease back in geological time, such that approximately one-third of the Earth surface lacks sufficient plate tectonic constraints by the early Cenozoic ~50 Ma, increasing to >60% uncertainty by the Late Jurassic. The most significant global plate model …

    houston Repository record for New Constraints For Convergent Margin Plate Tectonic Reconstructions From Imaged And Predicted Mantle Structure (opens in a new tab)