喀山-米甸(晚二叠世)西太平洋腕足动物群的古生物地理学

G.R. Shi, N.W. Archbold
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引用次数: 25

摘要

采用聚类分析、非度量多维标度、主坐标分析和最小生成树等方法,对16个动物区系站(根据采样和研究经验从19个初步编制的动物区系中选取)129属的有无发生数据进行了数据矩阵分析。揭示了三个核心动物群,并将其解释为代表三个生物省。它们是韦尔科利马省,包括科利马山脉、韦尔乔延山脉、扎贝加尔东部和蒙古北部;日本的华夏省、中国北部和南部以及印度支那地块;以及澳大利亚东部和新西兰的澳大利亚省。本文以阿塞连-塔斯图阶、白根之年-早昆古里阶和喀山-米阶三个离散时间片为基础,总结了西太平洋二叠纪海洋地方性的总体演化模式。并试图从板块构造、海侵/海退和气候改善的角度来解释西太平洋二叠纪海洋地域性的显著变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Palaeobiogeography of Kazanian-Midian (Late Permian) western Pacific Brachiopod faunas

A data matrix of the presence/absence occurrence data of 129 genera from 16 faunal stations (selected from 19 initially compiled faunal stations on the basis of sampling and study adequacies) is analysed by cluster analysis, nonmetric multidimensional scaling, principal coordinate analysis and minimum spanning tree. Three core faunal groups are revealed and interpreted as representing three biotic provinces. They are the Verkolyma Province embracing the Kolyma Massif, Verchoyan Mountains, east Zabaikal and northern Mongolia; the Cathaysian Province of Japan, northern and southern China and the Indo-China block; and the Austrazean Province of eastern Australia and New Zealand. The overall evolving pattern of Permian marine provincialism of the western Pacific is summarized from our previous, as well as current studies, on the basis of three discrete time slices: Asselian-Tastubian, Baigendzhinian-Early Kungurian and Kazanian-Midian. An attempt is also made to explain the marked change of marine provinciality during the Permian in the western Pacific in the context of plate tectonics, transgression/regression and climatic amelioration.

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