Abstract
The Bering Sea consists of (a) an abyssal basin that apparently was isolated from the Pacific Ocean by the development of the Aleutian Ridge near the end of Cretaceous Period and (b) a large epicontinental shelf area that first became submerged near the middle of the Tertiary Period. We postulate that the sediment eroded from Alaska and Siberia during Cenozoic time. It (1) was trapped in subsiding basins on the Bering shelf and in abyssal basins during the Tertiary, (2) collected mostly in continental rise and abyssal plain deposits of the Bering Sea during periods of low sea level of the Pleistocene, and (3) has been transported generally northward from the Bering shelf through the Bering Strait into the Arctic Ocean during periods of high sea level in Pleistocene and Holocene time.
Filling of subsiding basins on the shelf apparently was dominated by continental sedimentation in the early Tertiary and by marine deposition in the later Tertiary. River diversions caused by Miocene uplift of the Alaskan Range appear to have more than doubled the drainage area of the Yukon River. This change established the Yukon as the dominant source of river sediments (~90%) reaching the Bering Sea and must have greatly accelerated sedimentation in the basins.
The Quaternary Period presumably has been a time of alternation between two modes of sedimentation. When sea level was glacio-eustatically lowered, the Yukon and other rivers extended their courses across the continental shelf and delivered most of their sediment to the abyssal basin; an incidental result was the cutting of some of the world’s largest submarine canyons. Occurrence of the thin Holocene marine deposits near the present Yukon delta, of mainly relict sediments in the northern Bering Sea north of St. Lawrence Island and of several meters of Holocene sediment in the Chukchi Sea, suggests that when sea level was high, currents evidently swept much of the sediment from the Yukon River northward through the Bering Strait to be deposited on the continental shelf of the Chukchi Sea.
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Nelson, C.H., Hopkins, D.M., Scholl, D.W. (1974). Tectonic Setting and Cenozoic Sedimentary History of the Bering Sea. In: Herman, Y. (eds) Marine Geology and Oceanography of the Arctic Seas. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-87411-6_4
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