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Radiocarbon dating loess deposits in the Mississippi Valley using terrestrial gastropod shells (Polygyridae, Helicinidae, and Discidae)

机译:密西西比河谷的放射性碳年代黄土沉积 使用陆生腹足类壳(polygyridae,Helicinidae和Discidae)

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摘要

Small terrestrial gastropod shells (mainly Succineidae) have been used successfully to date late Quaternary loess deposits in Alaska and the Great Plains. However, Succineidae shells are less common in loess deposits in the Mississippi Valley compared to those of the Polygyridae, Helicinidae, and Discidae families. In this study, we conducted several tests to determine whether shells of these gastropods could provide reliable ages for loess deposits in the Mississippi Valley. Our results show that most of the taxa that we investigated incorporate small amounts (1–5%) of old carbon from limestone in their shells, meaning that they should yield ages that are accurate to within a few hundred years. In contrast, shells of the genus Mesodon (Mesodon elevatus and Mesodon zaletus) contain significant and variable amounts of old carbon, yielding ages that are up to a couple thousand 14C years too old. Although terrestrial gastropod shells have tremendous potential for 14C dating loess deposits throughout North America,weacknowledge that accuracy to within a few hundred years may not be sufficient for those interested in developing high-resolution loess chronologies. Even with this limitation, however, 14C dating of terrestrial gastropod shells present in Mississippi Valley loess deposits may prove useful for researchers interested in processes that took place over multi-millennial timescales or in differentiating stratigraphic units that have significantly different ages but similar physical and geochemical properties. The results presented here may also be useful to researchers studying loess deposits outside North America that contain similar gastropod taxa.
机译:在阿拉斯加和大平原,已经成功地使用了小型陆生腹足动物的贝壳(主要是琥珀科)来定殖晚第四纪的黄土沉积物。但是,与多头杜鹃科,螺旋科和盘状科的那些相比,在密西西比河谷的黄土沉积物中,丁二科的壳较少见。在这项研究中,我们进行了几次测试,以确定这些腹足动物的壳是否可以为密西西比河谷的黄土沉积提供可靠的年龄。我们的结果表明,我们研究的大多数分类单元的壳中都掺有少量(1-5%)的石灰石中的旧碳,这意味着它们的年龄应精确到几百年。相反,Mesodon属的壳(Mesodon elevatus和Mesodon zaletus)含有大量的可变化的旧碳,产生的年龄已经过了14C几千年。尽管陆生腹足动物的贝壳在整个北美具有14C年代黄土沉积的巨大潜力,但对于对发展高分辨率黄土年代感兴趣的人来说,数百年以内的准确性可能不足。然而,即使有这个限制,密西西比河谷黄土沉积物中存在的地面腹足动物壳的14 C年代定型可能仍对研究人员感兴趣,这些研究人员对经历了几千年时间尺度的过程或区分年龄明显不同但物理和地球化学相似的地层单位感兴趣属性。此处给出的结果对于研究北美以外含有类似腹足动物类群的黄土沉积物的研究人员也可能有用。

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