How did rising sea levels change continental shelves during the Triassic?

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At the beginning of the Triassic Period, shallow seas were limited in distribution, having dwindled significantly following the mass extinction at the end of the Permian Period. However, as the Triassic progressed, increased plate tectonic activity and the onset of continental rifting contributed to a gradual rise in sea levels.123

This rise in sea level caused shallow continental shelf seas to become more extensive along the margins of the continents. These expanding shelf environments provided new habitats that were colonized for the first time by diverse groups, including large marine reptiles and modern-style reef-building corals.23