Spatial variability of initial 230Th/232Th in modern Porites from the inshore region of the Great Barrier Reef

被引:53
作者
Clark, Tara R. [1 ]
Zhao, Jian-xin [1 ,2 ]
Feng, Yue-xing [2 ]
Done, Terry J. [3 ]
Jupiter, Stacy [4 ]
Lough, Janice [3 ]
Pandolfi, John M. [5 ]
机构
[1] Univ Queensland, Sch Earth Sci, Brisbane, Qld 4072, Australia
[2] Univ Queensland, Ctr Microscopy & Microanal, Radiogen Isotope Lab, Brisbane, Qld 4072, Australia
[3] Australian Inst Marine Sci, Townsville, Qld 4810, Australia
[4] Wildlife Conservat Soc, Fiji Country Program, Suva, Fiji
[5] Univ Queensland, ARC Ctr Excellence Coral Reef Studies, Sch Biol Sci, Ctr Marine Sci, Brisbane, Qld 4072, Australia
关键词
NINO SOUTHERN-OSCILLATION; CORAL-REEFS; AUSTRALIAN RAINFALL; DUST TRANSPORT; SERIES; SEDIMENT; SEA; LAGOON; QUEENSLAND; CLIMATE;
D O I
10.1016/j.gca.2011.11.032
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The main limiting factor in obtaining precise and accurate uranium-series (U-series) ages of corals that lived during the last few hundred years is the ability to constrain and correct for initial thorium-230 (Th-230(0)), which is proportionally much higher in younger samples. This is becoming particularly important in palaeoecological research where accurate chronologies, based on the Th-230 chronometer, are required to pinpoint changes in coral community structure and the timing of mortality events in recent time (e.g. since European settlement of northern Australia in the 1850s). In this study, thermal ionisation mass spectrometry (TIMS) U-series dating of 43 samples of known ages collected from living Porites spp. from the far northern, central and southern inshore regions of the Great Barrier Reef (GBR) was performed to spatially constrain initial Th-230/Th-232 (Th-230/Th-232(0)) variability. In these living Porites corals, the majority of Th-230/Th-232(0) values fell within error of the conservative bulk Earth Th-230/Th-232 atomic value of 4.3 +/- 4.3 x 10(-6) (2 sigma) generally assumed for Th-230(0) corrections where the primary source is terrestrially derived. However, the results of this study demonstrate that the accuracy of Th-230 ages can be further improved by using locally determined Th-230/Th-232(0) values for correction, supporting the conclusion made by Shen et al. (2008) for the Western Pacific. Despite samples being taken from regions adjacent to contrasting levels of land modification, no significant differences were found in Th-230/Th-232(0) between regions exposed to varying levels of sediment during river runoff events. Overall, 39 of the total 43 Th-230/Th-232(0) atomic values measured in samples from inshore reefs across the entire region show a normal distribution ranging from 3.5 +/- 1.1 to 8.1 +/- 1.1 x 10(-6), with a weighted mean of 5.76 +/- 0.34 x 10(-6) (2 sigma, MSWD = 8.1). Considering the scatter of the data, the weighted mean value with a more conservative assigned error of 25% (i.e. 5.8 perpendicular to 1.4 x 10(-6)) that encompasses the full variation of the 39 Th-230/Th-232(0) measurements is recommended as a more appropriate value for initial Th-230 corrections for U-series dating of most Porites samples from inshore regions of the GBR. This will result in significant improvement in both the precision and accuracy of the corrected Th-230 ages related to those based on the assumed bulk Earth Th-230/Th-232(0) value of 4.3 +/- 4.3 x 10(-6). However, several anomalously high Th-230/Th-232(0) values reaching up to 28.0 +/- 1.6 x 10(-6) occasionally found in some coral annual bands coinciding with El Nino years imply high Th-230/Th-232(0) sources and highlight the complexities of understanding Th-230/Th-232(0) variability. For U-series dating of young coral samples from such sites where anomalous Th-230/Th-232(0) values occur, we suggest replicate dating of multiple growth bands with known age difference to verify age accuracy. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:99 / 118
页数:20
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