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首页> 外文期刊>Quaternary International >Comparison of speleothem fabrics and microstratigraphic stacking patterns in calcite stalagmites as indicators of paleoenvironmental change
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Comparison of speleothem fabrics and microstratigraphic stacking patterns in calcite stalagmites as indicators of paleoenvironmental change

机译:方解石笋石笋纤维和微地层堆积模式比较古环境变化指标

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摘要

In the necessary task of obtaining high-resolution paleoclimate series from speleothems, the characterization of their internal microstratigraphy is a useful tool for: a) improving geochronology, and b) reaching a more complete knowledge of the speleothem formation and evolution through time and thus obtaining additional paleoenvironmental information. However, the development of standardized methodologies for microstratigraphic characterization is a pending task. In this paper, two different approaches allow construction of microstratigraphic logs for three stalagmites retrieved from two different caves. The logs correspond to vertical variations in speleothem fabrics and in microstratigraphic stacking patterns. The "fabrics logs" essentially provide information about the drip rate (sometimes used as a precipitation proxy) and the regularity or irregularity of each drip in the short-term. The "microstratigraphic stacking patterns logs" can be interpreted to obtain information about the changes in drip rates in the mid-and long-term. The results show a broad correlation between both kinds of logs that supports their validity as paleoenvironmental proxies. Fabrics formed under relatively constant and regular drips (columnar compact, open and elongated) usually constitute aggradational or progradational microstratigraphic stacking patterns. On the other hand, retractional stacking patterns are usually related with fabrics precipitated under more irregular drips (dendritic and columnar microcrystalline). However, this relation is not rigid and the information obtained from the logs is not equivalent, but complementary. The combination of both logs allows reconstruction of the hydrological history for each drip site. As all the obtained information derives directly from the drip conditions, drip effects result to be very important and can, in some cases, overwhelm the paleoclimate information recorded in each stalagmite. (C) 2016 Elsevier Ltd and INQUA. All rights reserved.
机译:在必要的任务中,从蛇麻藻中获得高分辨率的古气候系列,对其内部微地层进行表征是一种有用的工具,可用于:a)改善地质年代学,以及b)更加全面地了解蛇麻藻的形成和演化知识,从而获得其他古环境信息。但是,用于微地层表征的标准化方法的开发是一项悬而未决的任务。在本文中,两种不同的方法可以为从两个不同的洞穴中取回的三个石笋构造显微地层测井。测井曲线对应于针叶纤维织物和微地层堆积模式的垂直变化。 “织物日志”实质上提供了有关滴速(有时用作降水的替代物)以及短期内每个滴的规律性或不规律性的信息。可以解释“微地层堆积模式测井”,以获得有关中长期滴注率变化的信息。结果表明,两种原木之间的广泛相关性支持它们作为古环境代理的有效性。在相对恒定且规则的滴落下形成的织物(柱状致密,开放和拉长)通常构成聚集或渐进的微地层堆积图案。另一方面,缩回堆积模式通常与在不规则滴落(树突状和柱状微晶)下沉淀的织物有关。但是,这种关系不是严格的,从日志中获得的信息不是等效的,而是互补的。两种测井的结合允许重建每个滴水点的水文历史。由于所有获得的信息直接来自于滴水条件,因此滴水效果非常重要,在某些情况下,可能会使记录在每个石笋中的古气候信息不堪重负。 (C)2016 Elsevier Ltd和INQUA。版权所有。

著录项

  • 来源
    《Quaternary International》 |2016年第ptaa期|74-85|共12页
  • 作者单位

    Univ Complutense Madrid, Dept Estratig, Fac CC Geol, Madrid 28040, Spain;

    Univ Complutense Madrid, Dept Estratig, Fac CC Geol, Madrid 28040, Spain|Inst Geociencias IGEO CSIC UCM, C Jose Antonio Novais 12, Madrid 28040, Spain;

    Univ Complutense Madrid, Dept Estratig, Fac CC Geol, Madrid 28040, Spain|Inst Geociencias IGEO CSIC UCM, C Jose Antonio Novais 12, Madrid 28040, Spain;

    CENIEH, Paseo Sierra Atapuerca S-N, Burgos 09002, Spain;

    CIEMAT, Dpto Medioambiente, Avda Complutense 22, Madrid 28040, Spain;

    Univ Complutense Madrid, Dept Estratig, Fac CC Geol, Madrid 28040, Spain|Inst Geociencias IGEO CSIC UCM, C Jose Antonio Novais 12, Madrid 28040, Spain;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Speleothem; Cave; Karst; Paleoclimate; Microstratigraphic log; Holocene;

    机译:ele石;洞穴;喀斯特;古气候;显微地层测井;全新世;

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