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A synthesis of biostratigraphic, isotope-stratigraphic, and paleoenvironmental records from the Callovian (Middle Jurassic) carbonate succession of Saudi Arabia and its global implications
Coral-stromatoporoid reef, Middle Callovian warming, NE Gondwana, 0, Arabian Plate, Bayesian age-depth model, Integrated biostratigraphy, Carbon-isotope stratigraphy
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