Palaeoproductivity evolution in the centre of the western Pacific warm pool during the last 250 ka
Article first published online: 16 MAY 2011
Copyright © 2011 John Wiley & Sons, Ltd.
Journal of Quaternary Science
Volume 26, Issue 5, pages 478–484, July 2011
How to Cite
Li, T., Zhao, J., Nan, Q., Sun, R. and Yu, X. (2011), Palaeoproductivity evolution in the centre of the western Pacific warm pool during the last 250 ka. J. Quaternary Sci., 26: 478–484. doi: 10.1002/jqs.1471
- Issue published online: 24 JUN 2011
- Article first published online: 16 MAY 2011
- Manuscript Accepted: 2 NOV 2010
- Manuscript Revised: 26 SEP 2010
- Manuscript Received: 26 JUL 2008
- Earth's orbital period;
- western Pacific warm pool
To reconstruct the palaeoproductivity evolution history of the centre of the western Pacific warm pool (WPWP) over the last 250 ka, multi-proxies were analysed in sediment core WP7 recovered from the Ontong–Java Plateau. Palaeoproductivity evolution at the centre of the WPWP during the last 250 ka is closely related to glacial–interglacial cycles and the insolation controlled by precession. The glacial higher primary productivity relative to the interglacial conditions could have resulted from both thermocline shoaling associated with persistent El Niňo-like conditions and the increased influx of dust resulting from intensified winter monsoon together with important changes in the thermocline. The minimum primary productivity values during the last three terminations could be resulted from deglacial thermocline deepening and intensified stratification associated with persistent La Niña-like conditions, and the concurrent Neogloboquadrina dutertrei δ13C minimum events probably reflect the chemical signatures of Subantarctic Mode Water and Antarctic Intermediate Water. In addition, primary productivity values are also controlled by the thermocline variations resulting from El Niño/La Niña-Southern Oscillation processes responding to precession forcing, and lead the δ18O by about 4 ka. The 33.1 ka, 19 ka and “half-precession” periods are prominent in the palaeoproductivity records. Copyright © 2011 John Wiley & Sons, Ltd.