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Subduction Zones Seismic Activity Seismic Studies Seismology Earthquake Mechanics Seismic Monitoring Tectonic Plates Continental Drift Seismic Waves Seismic Phenomena Fault Lines Seismic Zones Earthquakes Nazca Plate Pacific Plate Tectonic Activity Volcanism Pacific Ring of Fire Continental Plates Volcanology Seismic Events Continental Separation Earth's History Indo-Australian Plate Earthquake Magnitude Himalayas Crust Formation Farallon Plate Mid-Atlantic Ridge Volcanic Activity Parkfield Section LLVPs Necessity for Life Debate on Early Earth Plate Tectonics Seismic Risk East African Rift System Magma Movement Seismic Risks Ring of Fire Rift Zones Tsunami Generation Tectonic Plates Interaction Climate Regulation Earth Cocos–North American plate convergence Cocos-Caribbean plate interaction Plate Boundaries Tectonic Theory Rift Systems Juan de Fuca Plate Cocos Plate Sunda Megathrust Subduction Processes Cocos-North America Plate Subduction African Plate Earth's Crust Cocos Plate subduction Earthquake Mechanisms Supercontinents Cocos–North American plate subduction Cocos–North American Plate Interaction Active Faults Cocos–North American plate interaction Seismic activity in Mexico Nazca–South American Plate Interaction
The finding suggests tectonic-driven volcanism from a vast Gondwana changed climate, raised sea level, fostered conditions that aided the Cambrian explosion.
