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A 27,000 year record of Red Sea Outflow: Implication for timing of post‐glacial monsoon intensification
Author(s) -
Naqvi Wajih A.,
Fairbanks Richard G.
Publication year - 1996
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/96gl01030
Subject(s) - oceanography , monsoon , benthic zone , geology , foraminifera , climatology , outflow , dominance (genetics) , environmental science , biochemistry , chemistry , gene
We reconstruct here the history of the Red Sea Outflow (RSO) over the past 27,000 years from an AMS 14 C‐dated high‐resolution δ 13 C record of benthic foraminifera from the inner Gulf of Aden assuming the dominance of circulation over productivity in regulating benthic δ 13 C. The results reveal that, following a period of suppressed RSO due to shallow sill 24,000–18,000 yr BP, the Red Sea was vigorously flushed for ∼2,000 years before a major monsoon intensification caused the cessation of deep water formation from 15,500 to 7,300 yr BP. It appears that the monsoon intensification did lag behind insolation until 15,500 yr BP. Between 15,500 and the present, however, there was no lag in conflict with the previous reports, implying a negligible dampening effect of continental albedo during this period. However, since our analysis is confined to a single depth horizon and our record is sensitive to sea level, it has some limitations as an indicator of monsoon intensity.