Sea level, carbonate mineralogy, and early diagenesis controlled δ¹³C records in Upper Ordovician carbonates

Keyphrases

• Ordovician Carbonate 100%
• Upper Ordovician 100%
• Marine Diagenesis 100%
• Early Diagenesis 100%
• Carbonate Mineralogy 100%
• Earth History 66%
• Anticosti Island 66%
• Hirnantian 66%
• Isotopic Carbon 66%
• Carbon Isotope Excursion 66%
• Great Basin 66%
• Shallow-water Carbonates 66%
• Global Ocean 66%
• Canada 33%
• Major Components 33%
• Utah 33%
• Geochemical Data 33%
• Aragonite 33%
• Mineralogy 33%
• Lateral Gradient 33%
• Nevada 33%
• Sedimentary Rocks 33%
• Carbon Isotopes 33%
• Postglacial 33%
• Geochemical Proxies 33%
• Ocean Chemistry 33%
• Carbonate Platform 33%
• Isotope Ratio 33%
• Ramp Setting 33%
• Carbonate Strata 33%
• Inner Ramp 33%
• Calcium Isotopes 33%
• Element Geochemistry 33%
• Paleoenvironmental Changes 33%
• Sea-level Change 33%
• Glaciation 33%
• Shallow Water Environment 33%
• Sea-level Lowstand 33%
• Flooding 33%
• Stratigraphic Variability 33%
• Pre-Jurassic 33%

Earth and Planetary Sciences

• Ordovician 100%
• Diagenesis 100%
• Sea Level 100%
• Mineralogy 100%
• Shallow Water 75%
• Hirnantian 50%
• Geochemistry 50%
• Global Ocean 50%
• United States of America 25%
• Canada 25%
• Postglacial 25%
• Utah 25%
• Sedimentary Rock 25%
• Isotope Ratios 25%
• Sea Level Change 25%
• Carbonate Platform 25%
• Carbon Isotope Ratio 25%
• Nevada 25%
• Aragonite 25%
• Marine Chemistry 25%
• Water Environment 25%
• Limestone 25%