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首页> 外文期刊>Journal of Asian earth sciences >Permian fusulinid biostratigraphy of the Baoshan Block in western Yunnan, China with constraints on paleogeography and paleoclimate
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Permian fusulinid biostratigraphy of the Baoshan Block in western Yunnan, China with constraints on paleogeography and paleoclimate

机译:云南西部宝山地块二叠纪融合地层生物地层,古地理和古气候限制

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Newly obtained fossil materials together with published data enable a review on the Permian fusulinids of the Gondwana-derived Baoshan Block in western Yunnan, China. The Baoshan Block yields rather impoverish Sakmarian-Yakhtashian fusulinids with just Eoparafusulina and Pseudofusulina in its northern and southern parts. These fusulinids biogeographically demonstrate the feature of peri-Gondwana province and signify a temperate-water condition. Further coniparison suggests the Baoshan Block was located distant from the tropical region and even with higher latitude than Central Iran and Central Pamir during the Sakmarian-Yakhtashian. In contrast, Murgabian-Midian fusulinids are more diversified. In the southern Baoshan Block, the Schwagerina assemblage, the Eopolydiexodina assemblage, the Sumatrina assemblage and the Verbeekina assemblage could be recognized in the Xiaoxinzhai area, and the Yangchienia Nankinella assemblage and the Chusenella-Rugosofusulina assemblage in the Bawei area, in ascending order. Contemporaneously, the Neofusulinella assemblage occurs in the northern and the Eopolydiexodina assemblage in the southwestern Baoshan Block respectively. These Murgabian Midian fusulinids show affinity of western Tethyan province and suggest a warm-water environment. Interestingly, the Midian Verbeekina assemblage is characterized by relatively low diversity and rather abundance of just one genus. Such compositional feature most likely signifies warm but still not optimal sea-surface water for the diversification of fusulinids. Also taking into account of the presence of Verbeekinids and Neoschwagerinids and the moderate total diversity, the Middle Permian fusulinids indicate that the Baoshan Block, during the Murgabian Midian, was probably located between equatorial region with warm water to the north and the majority of Sibumasu areas lacking Verbeekinids and Neoschwagerinids with temperate water to the south. (C) 2014 Elsevier Ltd. All rights reserved.
机译:最新获得的化石材料以及已发表的数据使我们能够对云南西部冈瓦纳衍生的宝山区块的二叠纪融合藻类进行回顾。宝山地块的北部和南部地区仅产生了Eoparafusulina和Pseudofusulina,因而生产了相当贫瘠的Sakmarian-Yakhtashian fusulinids。这些岩藻糖在生物地理学上显示了冈瓦纳周边地区的特征,并表明有温带水的条件。进一步的比较表明,宝山地块位于远离热带地区,甚至在萨克马期—雅克塔希期期间比伊朗中部和帕米尔中部地区纬度更高。相比之下,murgabian-midian fusulinids更加多样化。在宝山南段,在小新寨地区可以识别出Schwagerina组合,Eopolydiexododina组合,Sumatrina组合和Verbeekina组合,在Bawei阶地可以识别到Yangchienia Nankinella组合和Chusenella-Rugosofusulina组合。同时,新镰刀菌组合发生在北部,宝山地块的西南部出现了聚双螺旋藻组合。这些Murgabian Midian的融合蛋白显示出与特提斯省西部的亲和力,并暗示了温暖的水环境。有趣的是,Midiian Verbeekina组合的特征是相对较低的多样性和相当丰富的一个属。这种成分特征很可能意味着温暖的海面水,但对于岩藻素类的多样化仍然不是最佳的。还考虑到Verbeekinids和Neoschwagerinids的存在以及适度的总多样性,中二叠纪融合藻表明,在Murgabian Midian时期的宝山地块可能位于赤道地区与北部的温水之间,以及大部分Sibumasu地区在南部缺乏温带水的Verbeekinids和Neoschwagerinids。 (C)2014 Elsevier Ltd.保留所有权利。

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