Answer: The Pacific Ocean
Explanation: The Pacific Ocean is the largest and deepest of Earth's oceanic divisions and it extends from the Arctic Ocean in the north to the Southern Ocean in the south and it is bounded by the continents of Asia and Australia in the west and the Americas in the east.
It has the largest division of the World Ocean and it covers about 46% of Earth's water surface and about one-third of its total surface area, making it larger than all of Earth's land area combined.
There are about 25,000 islands in the Pacific Ocean and the Islands are of four basic types: continental islands, high islands, coral reefs and uplifted coral platforms.
The Pacific is almost surrounded by subduction zones which makes it more complex to study its history.
The two important processes involved in lithification of sedimentary rocks are compaction and cementation.
Fresh sediment is usually loose material filled with open spaces or pores filled with air or water. Lithification serves to reduce this pore space and replace it with solid mineral material. The main processes involved in lithification are compaction and cementation.
Compaction compresses the sediment to a smaller volume by packing the sediment particles more tightly, removing water from the pore spaces, or by reducing the pressure at the sediment particle contact points. Cementation involves filling the pore spaces with solid minerals that are either deposited from solution or allow particles of existing sediment to grow into the pores.
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I would say these would be transform boundaries where the tectonic energy appears to be transformed from one plate to another such as off the coast of Guatemala so it is not a simple process of subduction,.
The Pleistocene often colloquially referred to as the Ice Age) is the geological epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the world's most recent period of repeated glaciations. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology.