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首页> 外文期刊>Stratigraphy >High-resolution stratigraphy of the Contrada Pesciarello borehole succession (SE Sicily): a lower Langhian reference section for the Mediterranean region
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High-resolution stratigraphy of the Contrada Pesciarello borehole succession (SE Sicily): a lower Langhian reference section for the Mediterranean region

机译:Contrada Pesciarello钻孔演替(西西里岛)的高分辨率地层:地中海地区的朗格下层参考剖面

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摘要

The results of a high-resolution multidisciplinary stratigraphic study of a lower Langhian succession, located in the Hyblean Plateau (SE Sicily, southern Italy), are here presented. The about 33m thick succession, which belongs to the "Ragusa Fm" (Auct.), has been recovered through a continuous coring sur-vey and highly-spaced sampling. A total amount of 281 samples has been collected at an average interval of about 12cm for the follow-ing analyses: quantitative calcareous nannofossil and planktonic foraminifer biostratigraphy, paleomagnetism. CaCO_3 content. The distribution pattern of biostratigraphically significant taxa was reconstructed and paleomagnetostratigraphic data provided temporal constrains. Cyclostratigraphic reconstruction and astrochronological calibration of the section are proposed, based on the available bio- and magnetostratigraphic data, combined with the fluctuations of the Calcium carbonate content. Our results demonstrate that the section entirely falls within the magnetozone C5Br and spans the interval from 15.163 to 15.968 Ma. High-resolution stratigraphic data for the early Langhian time interval, including a set of well established calcareous plankton events, are provided. Thus, the present section plays a strategic role as correlation tool among different coeval successions, in the frame-work of a wider project aiming at the definition of the Global Stratigraphic Section and Point of the Langhian Stage.
机译:本文介绍了位于Hyblean高原(意大利南部西西里岛)的较低Langhian演替的高分辨率多学科地层研究结果。通过连续的取心调查和高间隔采样,已回收了约33m厚的连续岩层,属于“ Ragusa Fm”(Auct。)。总共以平均间隔约12厘米收集了281个样品,用于以下分析:定量钙质纳米化石和浮游有孔虫生物地层学,古磁性。 CaCO_3含量。重建了具有生物地层学意义的分类单元的分布模式,古地层学数据提供了时间上的限制。根据现有的生物地层和磁地层数据,结合碳酸钙含量的波动,提出了该剖面的旋回地层重建和天文年代标定。我们的结果表明,该断面完全落在磁区C5Br内,跨度从15.163到15.968 Ma。提供了Langhian早期时间间隔的高分辨率地层数据,包括一组完善的钙质浮游生物事件。因此,在更广泛的项目框架中,本节在不同时期的演替中起着相关工具的战略作用,该项目旨在确定全球地层剖面和朗根期。

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