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首页> 外文期刊>Geochemical Journal >High sensitivity measurements of nitrogen isotopic ratios in coral skeletons from Palau, western Pacific: Temporal resolution and seasonal variation of nitrogen sources
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High sensitivity measurements of nitrogen isotopic ratios in coral skeletons from Palau, western Pacific: Temporal resolution and seasonal variation of nitrogen sources

机译:西太平洋帕劳珊瑚骨骼中氮同位素比的高灵敏度测量:氮源的时间分辨率和季节变化

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摘要

By using a step-wise heating method in conjunction with static vacuum mass spectrometry, we have measuied at high temporal resolution (one month) the nitrogen isotopic ratio of a coral skeletal sample collected from Palau in the northern part of the Western Pacific, The <515N value from the 900°C combustion step varies significantly, from +l..l%o to +10.9%o for the estimated time period from July 1995 to January 1998, The higher values occurred during winter and the lower values in summer. The <518O and 513C values of the skeleton were also analyzed for the same period, using conventional methods. The ranges of <518O and <513C variations are from -6. Woo to -5.4%o and from -1.6%o to -0.9%o, respectively, which are significantly smaller than the <515N variation The <513C change is possibly attributable to kinetic isotope effects, as deduced from a negative correlation between the <513C value and mean sea surface temperature (SST) in the region. On the other hand, the <515N variation could be derived from seasonal change of the relative ratio of two components utilized by symbiotic algae: a 15N-depleted component from N2 fixation and 15N-enriched nitrate from the tropical oligotrophic open ocean.
机译:通过使用逐步加热方法与静态真空质谱联用,我们以较高的时间分辨率(一个月)测量了从西太平洋北部帕劳采集的珊瑚骨骼样品的氮同位素比。在1995年7月至1998年1月的估计时间段内,900°C燃烧步骤产生的515N值变化很大,从+ 1.l%o到+ 10.9%o。较高的值出现在冬季,而较低的值出现在夏季。使用常规方法,还分析了同期骨骼的<518O和513C值。 <518O和<513C变化范围是-6。 Woo分别为-5.4%o和-1.6%o至-0.9%o,显着小于<515N变化。<513C变化可能归因于动力学同位素效应,这是由< 513C值和该区域的平均海面温度(SST)。另一方面,<515N的变化可能源自共生藻类利用的两种组分相对比例的季节性变化:一种来自N2固定的15N贫化组分和来自热带贫营养性开放海洋的15N富集硝酸盐。

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