RECONSTRUCTION OF THE MULTIELEMENT APPARATUS OF THE CONODONT GLADIGONDOLELLA TETHYDIS (HUCKRIEDE) USING MULTIVARIATE STATISTICAL ANALYSIS; IMPLICATIONS FOR TAXONOMY, STRATIGRAPHY, AND EVOLUTION

IF 1.6 3区 地球科学 Q2 GEOLOGY
M. L. Golding, Ali M. Kiliç
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Abstract

The multielement apparatus of the Spathian (late Early Triassic) to Carnian (early Late Triassic) conodont Gladigondolella tethydis (Huckriede, 1958) is reconstructed here using multivariate statistical analysis to determine the co-occurrence of elements previously assigned to the Gl. tethydis apparatus by other authors. Disagreements on the apparatus composition of Gl. tethydis have focussed around whether or not the species contained two pairs of P2 elements, or only one pair. Some reconstructions consider elements referred to Cratognathodus as belonging to the multielement apparatus of Gladigondolella, whereas other workers consider these elements to belong to their own multielement apparatus. In the absence of fused clusters or bedding plane assemblages, multivariate statistical analysis of isolated elements provides the best method for constraining apparatus composition. Examination of collections from the Anisian (early Middle Triassic) of China and Romania, together with published occurrences from the Anisian and Carnian from around the world, has allowed the development of a database for both abundance and presence/absence of elements assigned to the Gladigondolella tethydis apparatus. Bray-Curtis indices for abundance data and Jaccard indices for presence/absence data both demonstrate that Cratognathodus elements occur as frequently with other elements belonging to the Gladigondolella tethydis apparatus as those elements do with each other. This lends support to the hypothesis that Cratognathodus elements also belong to the Gladigondolella tethydis apparatus. Therefore, the Gladigondolella tethydis apparatus proposed herein consists of the following elements: Gladigondolella tethydis (P1); Cratognathodus sp. (P2a): Ozarkodina saginata (Huckriede, 1958) (P2b); Roundya lautissima (Huckriede, 1958) (S0); Lonchodina spengleri (Huckriede, 1958) (S1); an enantiognathid element (S2); Hindeodella petrae-viridis (Huckriede, 1958) (S3); Hindeodella multihamata (Huckriede, 1958) (S4); and Lonchodina venusta (Huckriede, 1958) (M). Several of the elements assigned to the apparatus exhibit morphological variability, including the P1 element of Gladigondolella tethydis.
利用多元统计分析重建锥齿动物 gladigondolella tethydis (huckriede) 的多元素装置;对分类学、地层学和进化的影响
本文利用多元统计分析重建了斯帕提(早三叠世晚期)至卡尼(晚三叠世早期)锥齿动物 Gladigondolella tethydis(Huckriede,1958 年)的多元素器,以确定其他作者之前分配给 Gl.关于 Gl. tethydis 装置组成的分歧主要集中在该物种是否包含两对 P2 元素,还是只有一对。一些重建工作认为 Cratognathodus 的元素属于 Gladigondolella 的多元素器,而其他工作者则认为这些元素属于它们自己的多元素器。在没有融合群或层位面组合的情况下,对孤立元素进行多元统计分析是确定器的组成的最佳方法。通过对中国和罗马尼亚阿尼夏纪(早中三叠世)的采集物以及世界各地已发表的阿尼夏纪和卡尼夏纪的发现进行研究,我们建立了一个数据库,其中包括归属于 Gladigondolella tethydis 装置的元素的丰度和存在/不存在情况。丰度数据的 Bray-Curtis 指数和存在/不存在数据的 Jaccard 指数都表明,Cratognathodus 元素与属于 Gladigondolella tethydis 装置的其他元素的出现频率,与这些元素之间的出现频率一样高。这为 Cratognathodus 元素也属于 Gladigondolella tethydis 装置的假设提供了支持。因此,本文提出的 Gladigondolella tethydis 装置由以下元素组成:Gladigondolella tethydis(P1);Cratognathodus sp.(P2a):Ozarkodina saginata (Huckriede, 1958) (P2b);Roundya lautissima (Huckriede, 1958) (S0);Lonchodina spengleri (Huckriede, 1958) (S1);一个对映体元件 (S2);Hindeodella petrae-viridis (Huckriede, 1958) (S3);Hindeodella multihamata (Huckriede, 1958) (S4);以及 Lonchodina venusta (Huckriede, 1958) (M)。分配给该装置的几个元素表现出形态上的可变性,包括 Gladigondolella tethydis 的 P1 元素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
3.60
自引率
4.30%
发文量
28
审稿时长
>12 weeks
期刊介绍: The Rivista Italiana di Paleontologia e Stratigrafia was founded in 1895. It publishes original papers dealing with all fields of paleontology and of stratigraphy, from Italy and the Mediterranean to the Tethys, as well across the globe from China to North America.
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