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首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >Uranium-series dating of fossil coral reefs: Extending the sea-level record beyond the last glacial cycle
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Uranium-series dating of fossil coral reefs: Extending the sea-level record beyond the last glacial cycle

机译:铀系列化石珊瑚礁定年:将海平面记录扩展到上一个冰川周期以外

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摘要

Absolutely dated records of past sea-level change are extremely important for understanding the advance and retreat of the large ice sheets. When combined with other complementary climate archives and climate models, such records offer the potential to gain an improved understanding of Earth's natural climate cycles, providing a firmer basis for assessing the role of anthropogenic effects, such as greenhouse gas emissions, in modifying climate. The U-series dating of fossil coral reefs has been widely utilized to provide absolutely dated records of past sea-level change and numerous observations now exist for the past 130,000 years spanning the last glacial cycle. Despite this, controversies still exist regarding the exact timing and character of sea-level events within this time interval, and extending the sea-level history further back in time on the basis of robust and independent age constraints for older fossil reefs remains very elusive. This is primarily due to a progressive loss in the resolution of the U-series chronometer as one goes further back in time, coupled to a lack of well-preserved, dateable coral in older fossil reefs. To overcome these limitations, the primary challenges are three-fold. First, new analytical protocols are required to improve the resolution of the U-series chronometer Enhanced analytical precision must be coupled to accuracy through continued refinement of the U-series decay constant determinations and via the implementation of rigorous inter-laboratory calibration exercises. Second, efforts should continue to be focussed on gaining an improved understanding of the mechanisms controlling open-system exchange of the U-series isotopes in fossil reef systems. This will allow the number of 'reliable' U-series observations to be extended. Third, alternative dateable archives of past sea-level change must continue to be emphasized to further complement the coral reef database. These limitations are discussed in the context of current developments that further advance the application of U-series chronology to older fossil reef systems formed prior to the last glacial cycle. (C) 2009 Elsevier B.V. All rights reserved.
机译:关于过去海平面变化的绝对日期记录对于了解大型冰原的进退极为重要。当与其他补充性气候档案和气候模型结合使用时,这些记录可能会更好地了解地球的自然气候周期,为评估人为影响(例如温室气体排放)在改变气候中的作用提供更坚实的基础。 U系列化石珊瑚礁的年代已被广泛用于提供过时的海平面变化的绝对日期记录,并且在过去的最后一个冰川周期的过去130,000年中,现在存在大量观测资料。尽管如此,在此时间间隔内关于海平面事件的确切时间和特征仍然存在争议,并且基于对较老化石礁的稳健和独立的年龄限制,将海平面历史进一步追溯到过去仍然很遥远。这主要是由于随着时间的流逝,U系列计时码表的分辨率逐渐下降,同时在较早的化石礁中缺少保存完好的可更新日期的珊瑚。为了克服这些限制,主要挑战是三方面。首先,需要新的分析方案来提高U系列天文钟的分辨率。必须通过不断完善U系列衰减常数的确定方法以及实施严格的实验室间校准工作,将分析精度与准确性相结合。其次,应该继续集中精力,更好地了解控制化石礁系统中U系列同位素的开放系统交换的机制。这将允许扩展“可靠” U系列观测的数量。第三,必须继续强调过去海平面变化的可替代日期的档案,以进一步补充珊瑚礁数据库。在当前发展的背景下讨论了这些局限性,这些发展进一步推动了U系列年代学在上一次冰川循环之前形成的较早的化石礁系统中的应用。 (C)2009 Elsevier B.V.保留所有权利。

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