首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Hawaiian imprint on dissolved Nd and Ra isotopes and rare earth elements in the central North Pacific: Local survey and seasonal variability
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Hawaiian imprint on dissolved Nd and Ra isotopes and rare earth elements in the central North Pacific: Local survey and seasonal variability

机译:夏威夷在北太平洋中部溶解的Nd和Ra同位素以及稀土元素上的印记:当地调查和季节性变化

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Dissolved neodymium isotopes (Nd-143/Nd-144, expressed as epsilon(Nd)) and rare earth elements (REEs) have the potential to trace the provenance of lithogenic material as well as water masses. The central North Pacific is poorly investigated with respect to its Nd isotope signature and REE cycling, and little is known about the contributions of volcanic islands, such as Hawaii, relative to dust input from Asian deserts to the surface water REE budgets. Here we present dissolved Nd isotope and REE data along with long-lived radium isotope activities from Hawaii Ocean Time-Series Station ALOHA and coastal waters from Oahu, sampled for a GEOTRACES process study in February 2011. The data are supplemented with seasonal samples from ALOHA. Our results show a clear influence of the Hawaiian Islands on the coastal ocean and surface waters at ALOHA during February, expressed by higher surface water Ra activities, radiogenic surface epsilon(Nd) (epsilon(Nd) = +1.4 to -1.0), and elevated Eu anomalies (Eu/Eu* >= 1.3). Seasonal cycles of Asian dust deposition most likely contribute to the seasonal epsilon(Nd) variability of surface waters at ALOHA, as suggested by more negative epsilon(Nd) and the lack of Eu anomalies in summer. Neodymium isotopes in the intermediate and deep water column at ALOHA trace typical North Pacific water masses, such as North Pacific Intermediate Water and North Pacific Deep Water. We suggest that a radiogenic epsilon(Nd) excursion in 1000-2000 m water depth, observed in various North Pacific profiles, is controlled by advection of a modified Upper Circumpolar Deep Water or North Equatorial Pacific Intermediate Water. We further present an updated average epsilon(Nd) signature of -3.5 +/- 0.5 for North Pacific Deep Water and show that REE patterns of deep waters at ALOHA are dominantly controlled by vertical processes. (C) 2016 Elsevier Ltd. All rights reserved.
机译:溶解的钕同位素(Nd-143 / Nd-144,表示为epsilon(Nd))和稀土元素(REEs)具有追踪成岩物质和水团起源的潜力。关于北太平洋中部的Nd同位素特征和REE循环研究不多,关于夏威夷等火山岛相对于亚洲沙漠尘埃输入地表水REE预算的贡献知之甚少。在这里,我们提供了溶解的Nd同位素和REE数据,以及夏威夷海洋时间序列站ALOHA和瓦胡岛的近海水域的长寿命镭同位素活动,这些数据在2011年2月进行了GEOTRACES过程研究。这些数据与ALOHA的季节性样本相辅相成。我们的结果表明,夏威夷群岛对2月份ALOHA的沿海海洋和地表水有明显影响,表现为地表水Ra活度较高,放射性地表ε(Nd)(epsilon(Nd)= +1.4至-1.0)和Eu异常升高(Eu / Eu *> = 1.3)。亚洲尘埃沉积的季节性周期最有可能导致ALOHA地表水的季节性ε(Nd)变异,这是由于负ε(Nd)较负和夏季缺乏Eu异常所表明的。 ALOHA中深水柱中的钕同位素可追踪典型的北太平洋水团,例如北太平洋中间水和北太平洋深水。我们建议在北太平洋各种剖面中观察到的在1000-2000 m水深处的放射性epsilon(Nd)偏移受改良的上极地极深水或北赤道太平洋中间水的平流控制。我们进一步提出了北太平洋深水的平均更新ε-(-Nd)签名为-3.5 +/- 0.5,并表明ALOHA深水的REE模式主要由垂直过程控制。 (C)2016 Elsevier Ltd.保留所有权利。

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