Sangmin Lee, G. Shi, B. Runnegar, J. B. Waterhouse
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引用次数: 0
Abstract
Abstract Elements of a high-latitude (∼60–70°S) and low-diversity early Kungurian (Cisuralian/Early Permian) brachiopod fauna have been sporadically reported from the sandstone-dominated Snapper Point Formation (SPF) in the southern Sydney Basin of southeastern Australia for more than a half-century, but a detailed description of this fauna is not yet available. In this paper we describe 12 brachiopod species and an indeterminate ingelarellid from the SPF, including one new species (Tasmanospirifer jervisbayensis sp. nov. Waterhouse & Lee). Though this brachiopod fauna is evidently associated with an interglacial stratigraphic interval, its taxonomic characteristics overall resemble those from stratigraphically bounding glacial intervals. This association is interpreted to indicate persistence and the strong endemic nature of the Permian Eastern Australian biogeographic province in high-latitude eastern Gondwana, regardless of glacial/interglacial climate states during the Cisuralian. Biostratigraphically, the SPF brachiopod fauna is divisible into two distinctive stratigraphic assemblages: the Notospirifer cf. triplicata–Simplicisulcus sp. Assemblage in the lower part of the formation and the Johndearia brevis–Sulciplica transversa Assemblage in the upper part, each distinguished by a set of unique species. Sangmin Lee [sangminlee76@gmail.com] and G. R. Shi [guang@uow.edu.au] School of Earth, Atmospheric and Life Sciences, University of Wollongong Faculty of Science Medicine and Health, Northfields Avenue, Wollongong, NSW 2522, Australia Bruce Runnegar [runnegar@ucla.edu] Earth, Planetary and Space Sciences, University of California, Los Angeles, Los Angeles, CA 90095-1567, USA J. B. Waterhouse [permia@xtra.co.nz] Oamaru, Oamaru, New Zealand.
半个多世纪以来,在澳大利亚东南部悉尼盆地南部以砂岩为主的鲷点组(Snapper Point Formation, SPF)中,零星报道了高纬度(~ 60-70°S)和低多样性的早昆古里亚(中晚二叠世/早二叠世)腕足动物区系的元素,但尚未得到详细的描述。本文描述了SPF中12种腕足动物和1种不确定的ingelarellid,包括1个新种(Tasmanospirifer jervisbayensis sp. 11 . Waterhouse & Lee)。虽然该腕足动物群明显与间冰期地层有关,但其分类特征总体上与地层学上的冰期界线相似。这种联系被解释为表明,无论在西苏拉纪的冰川/间冰期气候状态如何,在高纬度冈瓦纳东部的二叠纪东澳大利亚生物地理省的持久性和强烈的地方性。在生物地层学上,SPF腕足动物群可划分为两个独特的地层组合:位于地层下部的Notospirifer . cftriplicata - simplicisulcus sp.组合和位于地层上部的Johndearia brevis-Sulciplica transversa组合,每个组合都有一组独特的物种。李sangmin Lee [sangminlee76@gmail.com], Shi G. R. [guang@uow.edu.au]澳大利亚伍伦贡大学科学医学与健康学院地球、大气与生命科学学院Bruce Runnegar [runnegar@ucla.edu]美国加州大学洛杉矶分校地球、行星与空间科学学院,洛杉矶,CA 90095-1567 . J. B. Waterhouse [permia@xtra.co.nz] Oamaru, Oamaru,新西兰。