δ18O in the Tropical Conifer Agathis robusta Records ENSO-Related Precipitation Variations

被引:17
|
作者
Boysen, Bjorn M. M. [1 ]
Evans, Michael N. [2 ,3 ]
Baker, Patrick J. [4 ]
机构
[1] Dept Environm & Primary Resources, East Melbourne, Vic, Australia
[2] Univ Maryland, Dept Geol, College Pk, MD 20742 USA
[3] Univ Maryland, Earth Syst Sci Interdisciplinary Ctr, College Pk, MD 20742 USA
[4] Univ Melbourne, Melbourne Sch Land & Environm, Dept Forest & Ecosyst Sci, Melbourne, Vic 3010, Australia
来源
PLOS ONE | 2014年 / 9卷 / 07期
基金
澳大利亚研究理事会; 美国国家科学基金会;
关键词
OXYGEN-ISOTOPE RATIOS; KAURI TREE-RINGS; AUSTRALIS KAURI; STABLE-ISOTOPES; CLIMATE; CHRONOLOGIES; HISTORY; VARIABILITY; DELTA-C-13; HYDROGEN;
D O I
10.1371/journal.pone.0102336
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Long-lived trees from tropical Australasia are a potential source of information about internal variability of the El Nino-Southern Oscillation (ENSO), because they occur in a region where precipitation variability is closely associated with ENSO activity. We measured tree-ring width and oxygen isotopic composition (delta O-18) of alpha-cellulose from Agathis robusta (Queensland Kauri) samples collected in the Atherton Tablelands, Queensland, Australia. Standard ring-width chronologies yielded low internal consistency due to the frequent presence of false ring-like anatomical features. However, in a detailed examination of the most recent 15 years of growth (1995-2010), we found significant correlation between delta O-18 and local precipitation, the latter associated with ENSO activity. The results are consistent with process-based forward modeling of the oxygen isotopic composition of alpha-cellulose. The delta O-18 record also enabled us to confirm the presence of a false growth ring in one of the three samples in the composite record, and to determine that it occurred as a consequence of anomalously low rainfall in the middle of the 2004/5 rainy season. The combination of incremental growth and isotopic measures may be a powerful approach to development of long-term (150+ year) ENSO reconstructions from the terrestrial tropics of Australasia.
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页数:9
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