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High-resolution ~(14)C analyses of annually-banded coral skeletons from Ishigaki Island, Japan: implications for oceanography

机译:日本石垣岛一年生带状珊瑚骨架的高分辨率〜(14)C分析:对海洋学的影响

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摘要

We report high-resolution radiocarbon (Δ~(14)C) analyses of annually-banded coral skeletons (Ponies luted) from Ishigaki Island, the Ryukyus, Japan, for the years 1985-1993. Analyses were carried out using an accelerator mass spectrometer (AMS) system at the National Institute for Environmental Studies, Tandem accelerator for Environmental Research and Radiocarbon Analysis (NIES-TERRA). Results provide a Δ~(14)C time series showing significant seasonal and interannual variations superimposed on a long-term trend. Δ~(14)C has a range of 66 per thousand, from a minimum of 79 per thousand to a maximum of 145 per thousand. The amplitude of the seasonal variation is 15-40 per thousand with lower Δ~(14) values in summer, which may indicate monsoon-induced local upwelling. The long-term trend of Δ~(14) is equivalent to a decrease of ~ 30 per thousand for the 8 yr from 1985 to 1993. Most of this trend probably reflects the gradual diffusion of bomb-derived ~(14)C from the atmosphere to the deep ocean via air-sea gas exchange and vertical movement of water masses. These results and ongoing analyses contribute to understanding of the ocean environment and ocean-atmosphere interactions in the far western subtropical Pacific.
机译:我们报告了从高分辨率的放射性碳(Δ((14)C)分析从1985-1993年,日本琉球,日本石垣岛的每年带状珊瑚骨架(被诱捕的小马)。使用美国国家环境研究所的加速器质谱仪(AMS),环境研究和放射性碳分析的串联加速器(NIES-TERRA)进行了分析。结果提供了一个Δ〜(14)C时间序列,该序列显示出明显的季节性和年际变化叠加在长期趋势上。 Δ〜(14)C的范围是千分之66,从最低的千分之79至最高的千分之145。夏季的季节变化幅度为千分之十五至四十,夏季的Δ〜(14)值较低,这可能表明季风引起的局部上升。 Δ〜(14)的长期趋势相当于从1985年至1993年的8年中,每千人下降〜30。这种趋势大部分可能反映了炸弹衍生的〜(14)C逐渐扩散。通过海气交换和水团的垂直运动进入深海的大气。这些结果和正在进行的分析有助于人们了解远西亚热带太平洋的海洋环境和海洋-大气相互作用。

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