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Hirnantian
Climate Change and the Selective Signature of the Late Ordovician Mass Extinction
(Silurian) Anoxic Palaeo-Depressions at the Western Margin of the Murzuq Basin (Southwest Libya), Based on Gamma-Ray Spectrometry in Surface Exposures
Palynology of the Middle Ordovician Hawaz Formation in the Murzuq Basin, South-West Libya
Polar Front Shift and Atmospheric CO During the Glacial Maximum of the Early Paleozoic Icehouse
Reconstruction of the Hirnantian (Late Ordovician) Palaeotopography in the Upper Yangtze Region Linna Zhang University of Chinese Academy of Sciences
A Sulfidic Driver for the End-Ordovician Mass Extinction
International Chronostratigraphic Chart
Estimating Dispersal and Evolutionary Dynamics in Diploporan Blastozoans (Echinodermata) Across the Great Ordovician Biodiversification Ve Ent
Terminal Ordovician Carbon Isotope Stratigraphy and Glacioeustatic Sea-Level Change Across Anticosti Island (Québec, Canada)
2009 Geologic Time Scale Cenozoic Mesozoic Paleozoic Precambrian Magnetic Magnetic Bdy
Ordovician Stratigraphy and Benthic Community Replacements in the Eastern Anti-Atlas, Morocco J
Type of the Paper (Article
Abrupt Global-Ocean Anoxia During the Late Ordovician–Early Silurian Detected Using Uranium Isotopes of Marine Carbonates
Cascading Trend of Early Paleozoic Marine Radiations Paused by Late Ordovician Extinctions
A Cenozoic-Style Scenario for the End-Ordovician Glaciation
Hirnantian (Latest Ordovician) Strata in the Heart of the Continent? Intriguing Results from Williston Basin, Manitoba M.W
Late Ordovician Mass Extinction Caused by Volcanism, Warming, and Anoxia, Not Cooling and Glaciation David P.G
Climate Change and the Selective Signature of the Late Ordovician Mass Extinction
Top View
Early Silurian Δ Corg Excursions in the Foreland Basin of Baltica, Both Familiar
Marine Redox Variability from Baltica During Extinction Events in the Latest Ordovician–Early Silurian T ⁎ Seth A
Supporting Information
Brenchley Et Al., 2001)
GEOLOGIC TIME SCALE V
Precession-Driven Climate Cycles and Time Scale Prior to the Hirnantian Glacial Maximum M
Carbon Isotope Chemostratigraphy and Sea
A Volcanic Trigger for the Late Ordovician Mass Extinction? Mercury Data from South China and Laurentia
Carbon Isotope Chemostratigraphy and Sea
Lower Silurian Stromatolites in Shallow-Marine Environments of the South
A Volcanic Trigger for the Late Ordovician Mass Extinction? Mercury Data from South China and Laurentia
GSSP) for the Base of the Hirnantian Stage (The Uppermost of the Ordovician System
Sea Level, Carbonate Mineralogy, and Early Diagenesis Controlled Δ13c Records in Upper Ordovician Carbonates David S
Ordovician News
2009 Geologic Time Scale Cenozoic Mesozoic Paleozoic Precambrian Magnetic Magnetic Bdy
Silurian) Strata in Southeastern Ohio by Christopher B
Hirnantian Isotope Carbon Excursion in Gorny Altai, Southwestern Siberia
Chitinozoan Biozonation in the Upper Katian and Hirnantian of the Welsh Basin, UK Challands, T