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Pacific microplate and the Pangea supercontinent in the Early to Middle Jurassic

¹ Institut de Géologie et Paléontologie, Université de Lausanne, Bâtiment des Facultés des Sciences Humaines 2, 1015 Lausanne, Switzerland
² Graduate School of Oceanography, University of Rhode Island, Narragansett, Rhode Island 02882, USA

New biostratigraphic data based on radiolarians recovered from deep within the oceanic crustal section of Ocean Drilling Program Hole 801C in the western Pacific, along with existing radiometric information, date this oceanic crust as late Bajocian–early Bathonian (170–165 Ma). The overlying basal sediments at Hole 801C are essentially identical in age (middle Bathonian, 164–162 Ma) to the basal sediments at Deep Sea Drilling Program Hole 534A in the central Atlantic. We estimate the time of formation of the Pacific plate as 175–170 Ma and the time of initial separation of the Pangea supercontinent in the central Atlantic as 190–180 Ma. We also identify a time of extensive subduction-zone magmatism (175–159 Ma) at the eastern and western edges of Pangea. We suggest that the initial plate separation of Pangea increased subduction rates at its outer margins and altered the plate boundaries in the Pacific superocean, leading to formation of the Pacific plate.

Key Words: Jurassic • Ocean Drilling Program • ocean crust • Pacific plate • Pangea • Radiolaria

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