期刊
GEOPHYSICAL RESEARCH LETTERS
卷 27, 期 1, 页码 133-136出版社
AMER GEOPHYSICAL UNION
DOI: 10.1029/1999GL002306
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Two sediment cores were investigated to study the regional climatic variability of the NW African upwelling over the-late Quaternary. Biomarker data and Sea Surface Temperatures (SSTs) predicted from alkenones at 25 degrees N and 21 degrees N-exhibited distinct features. The amplitude of the last deglaciation was estimated to 4.5 degrees C at 25 degrees N and 2-2.5 degrees C at 21 degrees N. At 25 degrees N, terrestrial and marine glacial inputs were higher than Holocene ones as a result of a strengthening of the trade winds:and intensification of oceanic production. In contrast, at 21 degrees N, warmer SSTs and lower organic carbon and alkenone productions during the last glacial suggest a regression of the upwelling and therefore a change of wind regime. Low glacial n-alkanols are consistent with the migration of the vegetation belt during the maximum of African aridity, while their decrease towards the core-top may be indicative of anthropogenic disturbances.
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