Geochemistry of coral from Papua New Guinea as a proxy for ENSO ocean-atmosphere interactions in the Pacific Warm Pool

被引:22
作者
Ayliffe, LK
Bird, MI
Gagan, MK
Isdale, PJ
Scott-Gagan, H
Parker, B
Griffin, D
Nongkas, M
McCulloch, MT
机构
[1] Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT 0200, Australia
[2] Australian Inst Marine Sci, Townsville, Qld 4810, Australia
[3] CSIRO, Div Marine Res, Hobart, Tas 7000, Australia
[4] Univ Papua New Guinea, Dept Geol, Pt Moresby, Papua N Guinea
基金
澳大利亚研究理事会;
关键词
Porites; Sr/Ca; oxygen isotopes; UV fluorescence; ENSO; Asian-Australian monsoon; Pacific Warm Pool; Papua New Guinea;
D O I
10.1016/j.csr.2004.07.013
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
A Porites sp. coral growing offshore from the Sepik and Ramu Rivers in equatorial northern Papua New Guinea has yielded an accurate 20-year history (1977-1996) of sea surface temperature (SST), river discharge, and wind-induced mixing of the upper water column. Depressions in average SSTs of about 0.5-1.0degreesC (indicated by coral Sr/Ca) and markedly diminished freshwater runoff to the coastal ocean (indicated by coral delta(18)O, delta(13)C and UV fluorescence) are evident during the El Ni (n) over tildeo - Southern Oscillation (ENSO) events of 1982-1983, 1987 and 1991-1993. The perturbations recorded by the coral are in good agreement with changes in instrumental SST and river discharge/precipitation records, which are known to be diagnostic of the response of the Pacific Warm Pool ocean-atmosphere system to El Ni (n) over tildeo. Consideration of coastal ocean dynamics indicates that the establishment of northwest monsoon winds promotes mixing of near-surface waters to greater depths in the first quarter of most years, making the coral record sensitive to changes in the Asian-Australian monsoon cycle. Sudden cooling of SSTs by similar to1degreesC following westerly wind episodes, as indicated by the coral Sr/Ca, is consistent with greater mixing in the upper water column at these times. Furthermore, the coral UV fluorescence and oxygen isotope data indicate minimal contribution of river runoff to surface ocean waters at the beginning of most years, during the time of maximum discharge. This abrupt shift in flood-plume behaviour appears to reflect the duration and magnitude of northwest monsoon winds, which tend to disperse flood plume waters to a greater extent in the water column when wind-mixing is enhanced. Our results suggest that a multi-proxy geochemical approach to the production of long coral records should provide comprehensive reconstructions of tropical paleoclimate processes operating on interannual timescales. (C) 2004 Elsevier Ltd. All rights reserved.
引用
收藏
页码:2343 / 2356
页数:14
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