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Ireviken event
Early Silurian Oceanic Episodes and Events
Revised Correlation of Silurian Provincial Series of North America with Global and Regional Chronostratigraphic Units 13 and D Ccarb Chemostratigraphy
Records of Carbon and Sulfur Cycling During the Silurian Ireviken Event in Gotland, Sweden
On the Causes of Mass Extinctions
Integrated Biostratigraphy of the Lower Silurian of the Aizpute-41 Core, Latvia
Greenhouse−Icehouse Transition in the Late Ordovician Marks a Step Change in Extinction Regime in the Marine Plankton
Paleozoic–Mesozoic Eustatic Changes and Mass Extinctions: New Insights from Event Interpretation
Type of the Paper (Article
Back Matter (PDF)
Cyclo and Chemostratigraphic Characteristics of the Middle Silurian in Gotland, Sweden M.C.M
View That Primary Carbon Isotope Signatures Have Been Preserved [Samtleben Et Al., 1996; Bickert Et Al., 1997; Cramer and Saltzman, 2005]
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
Cyclo and Chemostratigraphic Characteristics of the Middle Silurian in Gotland, Sweden
Extinction Events Ver2.Pub
Carbon Isotope Chemostratigraphy of the Late Silurian Lau Event, Gotland, Sweden
UNIVERSITY of CALIFORNIA RIVERSIDE Molecular Organic
Reconstructing the Environmental Conditions Around the Silurian Ireviken Event Using the Carbon Isotope Composition of Bulk and Palynomorph Organic Matter
Top View
Ludlow, Silurian) in Southern Laurentia – Preliminary Results
(Llandovery–Wenlock Boundary) Mass Extinction ∗ Seth A
Linking the Progressive Expansion of Reducing Conditions to a Stepwise Mass Extinction Event in the Late Silurian Oceans Chelsie N
Silurian and Ordovician Conodont Biostratigraphy of the Moose River Basin and Appalachian Basin
Metal-Induced Malformations in Early Palaeozoic Plankton Are Harbingers of Mass Extinction
Cyclo and Chemostratigraphic Characteristics of the Middle Silurian in Gotland, Sweden M.C.M
Silurian 13C Stratigraphy
Greenhouse−Icehouse Transition in the Late Ordovician Marks a Step Change in Extinction Regime in the Marine Plankton
(Silurian) Positive Carbon Isotope Excursion
Patterns of Conodont Extinction Selectivity During Ireviken Event (Lower Silurian), Example from Eastern Baltic Basin
Carbonate Platform Evolution and Conodont Stratigraphy During the Middle Silurian Mulde Event, Gotland, Sweden
Summary of East Gondwanan Conodont Data Through the Ireviken Event at Boree Creek