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首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >Dynamics of cyclic carbonate deposition and biotic recovery on platforms during the Famennian of Late Devonian in Guangxi, South China: Constraints from high-resolution cycle and sequence stratigraphy
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Dynamics of cyclic carbonate deposition and biotic recovery on platforms during the Famennian of Late Devonian in Guangxi, South China: Constraints from high-resolution cycle and sequence stratigraphy

机译:中国南方广西泥盆纪后期法门尼期的台地循环碳酸盐沉积和生物恢复动力学:高分辨率旋回和层序地层的制约

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摘要

To better understand the dynamics of platform carbonate deposition, evolution and biotic recovery during the Famennian, high-resolution cycle and sequence stratigraphic analyses were carried out upon three platform sections (one in ramp, and two in rimmed platforms), along with a biostratigraphically well-constrained basinal section, in Guangxi, South China. Four main fades and fourteen lithofacies are identified in the three isolated platforms; these are vertically arranged into decimetre- to metre-scale, shallowing-upward peritidal and subtidal cycles (or parasequces), in which the peritidal cycles predominate over the lower-middle Famennian. Six third order sequences (S1 to S6) are identified based on the cycle stacking patterns as illustrated by Fischer-plots and vertical facies changes; these sequences are temporally calibrated through correlation with basinal sequences constrained with conodont zonation, and match well the six main Famennian transgressive-regressive cycles (T1 to T6) in Euramerica and elsewhere, indicating a eustatic control. However, an opposite longer-term trend in accommodation change (S3 to S4) between platform interior and deeper open shelf-to-basin settings during the middle Famennian suggests a differential subsidence across the platform-basin section, likely driven by block tilting. Thus, both eustatic fluctuations and local tectonism had played an important role in platform development and evolution. After the Frasnian-Famennian biotic crisis, main marine benthos preferentially recovered in the normal marine niches on the nearshore open shelves, and radiated gradually into offshore restricted platforms. Brachiopods, notably rhychonellides, were the taxa recovering the earliest (S1) in the normal (or near normal) marine conditions, then echinoderms (S3), stromatoporoids (upper S3) and corals (S5) stepped in episodically. However, these benthos generally appeared later in the restricted platform interiors only as if the ecological conditions were improved well enough for their colonization. Therefore, the biotic recovery processes were diachronous: both taxonomically- and ecologically-specified. (C) 2015 Elsevier B.V. All rights reserved.
机译:为了更好地了解法门尼亚期地台碳酸盐沉积,演化和生物恢复的动力学,对三个平台段(一个在斜坡上,两个在有缘平台上)以及一个生物地层井进行了高分辨率循环和层序地层分析。约束的盆地剖面,中国南方的广西。在三个隔离的平台中识别出四个主要的淡变和十四个岩相。这些垂直排列成分米至米级的,浅的向上的潮汐和潮汐周期(或副潮差),其中,潮差周期在中下法门尼时期占主导地位。根据Fischer曲线和垂直相变所示的循环叠加模式,确定了六个三阶序列(S1至S6)。这些序列通过与牙形体分区限制的盆地序列的相关性在时间上进行了校准,并与欧亚大陆和其他地区的六个主要的Famennian海侵-海退循环(T1到T6)相匹配,表明该系统具有良好的控制性。然而,在法门尼中部,平台内部和较深的陆架到台盆设置之间的平台变化(S3至S4)的长期变化趋势相反,这表明整个台盆区段的沉降差异很大,这可能是由于块体倾斜引起的。因此,欣喜若狂的波动和局部构造都在平台的发展和演变中发挥了重要作用。在发生弗拉斯尼亚人-法门尼人生物危机之后,主要的海洋底栖动物优先在近岸开放架子的正常海洋生态位中恢复,并逐渐向近海受限平台辐射。腕足类动物,尤其是Rhychonellides,是在正常(或接近正常)海洋条件下最早恢复(S1)的类群,然后棘皮动物(S3),层间孔类(S3的上部)和珊瑚(S5)流行。但是,这些底栖动物通常仅在后来出现在受限的平台内部时,才好像生态条件已得到足够改善以适合其定殖一样。因此,生物恢复过程是历时的:既是生物分类学上的,又是生态学上指定的。 (C)2015 Elsevier B.V.保留所有权利。

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