作者: S. E. Trumbore , W. S. Broecker , R. F. Anderson , Y. Lao , H. J. Hofmann
DOI:
关键词: Seawater 、 Boundary (topology) 、 Oceanography 、 Geology 、 Scavenging 、 Deposition (chemistry) 、 Holocene sediments 、 Pacific ocean
摘要: Measurements of U, Th, Pa-231, and Be-10 concentrations were conducted in Holocene sediments from several sites representing open-ocean ocean-margin environments the Pacific Ocean. The results show that boundary scavenging plays a major role removal Pacific. Deposition is more than an order magnitude greater at margin deep central sites, while Pa-231 4- to 5-fold sites. factors controling Pa Be are discussed.