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首页> 外文期刊>Journal of Asian earth sciences >Aalenian-Early Bathonian (Middle Jurassic) radiolarian assemblages in the Tavas nappe within Lycian nappes in the western Taurides (SW Turkey): The first dating of carbonate platform drowning
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Aalenian-Early Bathonian (Middle Jurassic) radiolarian assemblages in the Tavas nappe within Lycian nappes in the western Taurides (SW Turkey): The first dating of carbonate platform drowning

机译:塔乌里德西部(西南土耳其)的利西亚河床内塔瓦斯河床中的亚伦-早巴东(中侏罗世)放射虫组合:碳酸盐台地溺水的第一次约会

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Stratigraphic sections (Kizilca and Kizilca North) in the Tavas nappe, western Taurides, Turkey records the event of carbonate platform drowning in the western Tethyan realm. Our detailed biostratigraphic study of radiolarians and other microfossils places the important temporal constraints on this event and indicates that drowning occured in the geochronological interval from Early Jurassic (Hettangian-Sinemurian) through to Middle Jurassic (early Bathonian). The basal part of the Kizilca section is represented by platform carbonates with abundant benthic foraminifera and algae of Hettangian-Sinemurian to Pliensbachian age. Toward the upper part of the section, the occurrence of brecciated limestones with some ammonites and belemnites reveals that the drowning event began in the Pliensbachian. The first radiolarian assemblages of early-middle to late Aalenian age were obtained from the overlying units characterized by pelagic limestones and chert alternation. Just after the subsidence of the platform, ribbon chert sedimentation began in the late Aalenian, as indicated by the radiolarians. Successively, early-late Bajocian and latest Bajocian-early Bathonian radiolarian assemblages were obtained from overlying chert with mudstone-silicified mudstones. Similar to that observed in the Kizilca section, the Kizilca North section include successively pelagic limestones, pelagic limestone-chert alternation and chert-mudstone alternation of late Aalenian to early-middle Bajocian age according to radiolarian biostratigraphy. All of these observations indicate that a continuous stratigraphy recorded the drowning event without a large gap from Hettangian-Sinemurian to early Bathonian in the Tavas nappe. This drowning event has close similarities with coeval events in other Tethyan realms in terms of mechanism, facies characteristics and fossil assemblages. Therefore, this study can aid correlation studies of the Tavas nappe with the Jurassic paleogeography worldwide. (C) 2014 Elsevier Ltd. All rights reserved.
机译:土耳其Taurides西部塔瓦斯纳普(Tavas nappe)地层剖面(Kizilca和Kizilca North)记录了在特提斯地区西部溺水的碳酸盐台地事件。我们对放射虫和其他微化石的详细生物地层学研究对这一事件施加了重要的时间约束,并表明溺水发生在从侏罗纪早期(Hettangian-Sinemurian)到侏罗纪中部(早期巴东期)的地质年代学期间。 Kizilca剖面的基部以台地碳酸盐为代表,碳酸盐具有丰富的底栖有孔虫和Hettangian-Sinemurian至Pliensbachian年龄的藻类。在该部分的上部,角砾岩灰岩中有一些炸药和甜菜碱的出现表明溺水事件始于普林斯巴赫河。从中上层石灰岩和石蚀变为特征的上覆单元中,获得了早于中晚期的第一个放射虫组合。平台沉降后,放射radio虫便指出,带状石的沉积开始于晚安的亚伦尼西亚。随后,从上覆的石与泥岩硅化泥岩中获得了早晚的巴约西亚人和最新的巴约西亚人至早的巴东人的放射虫组合。与基齐尔卡剖面观察到的情况相似,根据放射线虫生物地层学,基齐尔卡北剖面包括依次为上阿利安时代至巴乔奇早期至中早期的上层石灰岩,上层石灰岩-t石交替和and石-泥岩交替。所有这些观察结果表明,连续的地层学记录了溺水事件,在塔瓦斯(Tavas)推覆中,从Hettangian-Sinemurian到早期Bathonian没有很大的差距。在机制,相特征和化石组合方面,该溺水事件与特提斯其他地区的近代事件具有相似性。因此,这项研究可以帮助塔瓦斯推覆与全世界侏罗纪古地理的相关性研究。 (C)2014 Elsevier Ltd.保留所有权利。

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