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Parafurnishius, an Induan (Lower Triassic) conodont new genus from northeastern Sichuan Province, southwest China and its evolutionary implications

机译:产自中国西南部四川省东北部的印度产(三叠纪)牙形石新属Parafurnishius及其进化意义

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A fundamental aspect of taxonomy at the generic level, critical to understand Early Triassic conodont evolution, is the composition of the multielement apparatus. In this paper, we document a platform-bearing new conodont genus, Parafurnishius n. gen., as well as its multielement apparatus from the Griesbachian Feixianguan Formation (Lower Triassic) in Xuanhan County, northeastern Sichuan Province, southwest China. The new conodont genus is characterized by numerous robust and irregularly distributed conical denticles with variable platform morphology that has a possible affinity with the P-1 elements of Furnishius. These genera have apparatuses similar to those of Ellisonia and are classified with the family Ellisoniidae. The strong intraspecific variation of P-1 elements and the growth series within the entire sample population suggest that Parafurnishius may have evolved from the Griesbachian Isarcicella by developing random denticle positioning away from the platform centre, and then possibly evolved into younger Triassic Furnishius by developing a stable blade configuration. This preferred interpretation implies an ellisonid apparatus for Isarcicella. Alternatively, Parafurnishius may have evolved from Ellisonia and developed a homeomorphic P-1 element with Isarcicella. This new taxon has strong intraspecific variation of denticle growth orientation during the Early Triassic. (C) 2014 Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. All rights reserved.
机译:通用级别分类学的一个基本方面,对于理解早期三叠纪牙形石的演化至关重要,是多元素仪器的组成。在本文中,我们记录了一个带有平台的新牙形石属Parafurnishius n。 ,以及四川西南部宣汉县的格里斯巴赫飞仙关组(下三叠统)的多元素仪器。新牙形刺属的特征是具有许多坚固且不规则分布的圆锥形齿,这些齿形具有可变的平台形态,可能与Furnishius的P-1元素具有亲和力。这些属具有与Ellisonia相似的仪器,并按Ellisoniidae科分类。在整个样本种群中,P-1元素的强烈种内变异和生长系列表明,Parafurnishius可能是通过远离平台中心的随机齿根位置从格里斯巴赫Isarcicella进化而来,然后可能通过发育成一个更年轻的Triassic Furnishius稳定的刀片配置。这种优选的解释暗示了伊氏杆菌的一种椭球体装置。另外,Parafurnishius可能已经从埃里希尼亚(Ellisonia)进化而来,并与伊萨菌(Isarcicella)形成了同胚P-1元素。在三叠纪早期,这种新的分类单元在牙齿生长方向上具有强烈的种内变化。 (C)2014年Elsevier B.V.和中科院南京地质与古生物研究所。版权所有。

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