首页> 外文期刊>Paleontology Journal >Revision of the Messinian-Early Zanclean Sediments from ODP Hole 953C (Canary Island Archipelago, North-Eastern Atlantic): Biostratigraphy, Cyclostratigraphy, and Astronomical Tuning
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Revision of the Messinian-Early Zanclean Sediments from ODP Hole 953C (Canary Island Archipelago, North-Eastern Atlantic): Biostratigraphy, Cyclostratigraphy, and Astronomical Tuning

机译:修改ODP 953C洞(加那利群岛,东北大西洋)的墨西拿早期Zanclean沉积物:生物地层学,旋回地层学和天文调整

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A quantitative study was performed on calcareous plankton of the Messinian-early Zanclean succession recovered at ODP Leg 157 Hole 953C (Canary Island Archipelago, North-Eastern Atlantic). This revision allowed to recognize some events typically recorded in the Mediterranean region, highlighting affinities between the Mediterranean and North Atlantic Ocean, in the considered time interval. The presence of such events in an open-ocean succession provides the possibility to substantially improve the biostratigraphic resolution and supplies useful correlation tools between the Mediterranean and oceanic areas. Moreover, to unravel cyclical patterns of deposition and given that the investigated succession shows no evident lithological pattern, cyclostratigraphic analyses have been based on abundance fluctuations ofGlobigerinoides-Orbulinagroup, neogloboquadrinids, and warm-water versus cool-water species ratio. As a result, forty-three precession-controlled cycles have been recognized spanning from 6.457 Ma to 4.799 Ma.
机译:对在ODP腿157孔953C(加那利群岛,东北大西洋)发现的墨西尼早Zanclean演替阶段的钙质浮游生物进行了定量研究。该修订版允许识别通常记录在地中海地区的一些事件,突出了在所考虑的时间间隔内地中海与北大西洋之间的亲和力。此类事件在开放海洋的演替中的存在提供了大大改善生物地层分辨率的可能性,并提供了地中海和海洋区域之间的有用的相关工具。此外,为了揭露沉积的周期性模式,并且鉴于所研究的演替没有显示出明显的岩性模式,旋回地层分析是基于球墨角藻类-奥布林纳群,新球藻类,以及温水与冷水物种比率的丰度波动进行的。结果,已经识别出43个旋进控制的周期,范围从6.457 Ma到4.799 Ma。

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