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Research Article| January 01, 1983 Increased productivity in the eastern equatorial Pacific during the last glacial maximum (19,000 to 14,000 yr B.P) Thomas F. Pedersen Thomas F. Pedersen 1Department of Oceanography, University of British Columbia, Vancouver, British Columbia V6T 1W5, Canada Search for other works by this author on: GSW Google Scholar Geology (1983) 11 (1): 16–19. https://doi.org/10.1130/0091-7613(1983)112.0.CO;2 Article history first online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Thomas F. Pedersen; Increased productivity in the eastern equatorial Pacific during the last glacial maximum (19,000 to 14,000 yr B.P). Geology 1983;; 11 (1): 16–19. doi: https://doi.org/10.1130/0091-7613(1983)112.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract A widespread pronounced enrichment in the organic carbon content occurs at shallow depths in eastern equatorial Pacific sediments. The Corg peak is shown by radiocarbon dating to be temporally coincident with the last (Stage 2 or Wisconsin) glacial maximum. In contrast, CaCO3 profiles show less overall variation, which appears to be partly a function of the location of the sediments relative to the lysocline. Consideration of the iodine:Corg ratio in the sediments rules out enhanced preservation as a cause of the Stage 2 organic carbon enrichment. The peak, instead, must have resulted from a significant increase in productivity during the glacial maximum. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
Thomas F. Pedersen (Sat,) studied this question.