俄罗斯远东滨海南二叠纪腕足类:系统分类学、古地理和古海洋意义

G. Shi, Sangmin Lee, Galina V. Kotylar, Y. Zakharov
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引用次数: 1

摘要

长期以来,俄罗斯远东滨海南地区以其高度多样化的中二叠纪腕足动物群而闻名;然而,分类学和古生物地理学的重新评估是迟来的。本文描述了南滨海地区Barabash和Pilnikov剖面的两个腕足动物组合。Barabash剖面组合来自Barabashevka组下部,包括18种腕足类动物,与其他代表世界晚期的海洋动物群有关联。另外,Pilnikov剖面组合来自Pilnikov组,并产生与中昆古里亚(Irenian)一致的四种腕足动物。Barabash组合的古生物地理组成以冷水北寒带元素和古赤道暖水华夏省元素的明显混合以及具有反热带分布的属为特征。与日本海/东海相似的新近纪动物群比较表明,巴拉巴什剖面可能位于中蒙海道的东部,处于北温带暖流和冷水流的中纬度交汇处。石国荣* [guang@uow.edu.au],李尚民[sangminlee76@gmail.com],澳大利亚卧龙岗大学地球、大气与生命科学学院,澳大利亚新南威尔士州卧龙岗2522;Galina V. Kotlyar [galina_kotlyar@vsegei.ru], Karpinsky全俄地质研究所(VSEGEI), Srednii pr. 74, 199106俄罗斯圣彼得堡;Yuri D. Zakharov [yurizakh@mail.ru],俄罗斯科学院远东分院远东地质研究所,符拉迪沃斯托克,690022俄罗斯。
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Permian brachiopods from South Primorye, Far East Russia: systematics, palaeobiogeographical and palaeoceanographical implications
Abstract The South Primorye area of Far East Russia has long been recognized for its highly diverse mid-Permian brachiopod fauna; however, a taxonomic and palaeobiogeographical reassessment is overdue. This paper describes two brachiopod assemblages from the Barabash and Pilnikov section localities in South Primorye. The Barabash section assemblage was collected from the lower part of the Barabashevka Formation and includes 18 brachiopod species associated with other marine faunas indicative of the late Wordian. Alternatively, the Pilnikov section assemblage derives from the Pilnikov Formation and yields four brachiopod species consistent with the mid-Kungurian (Irenian). The palaeobiogeographical composition of the Barabash assemblage is distinguished by a conspicuous admixture of cool-water Boreal Realm elements and palaeoequatorial warm-water Cathaysian Province elements, together with genera that have antitropical distributions. Comparisons with analogous Neogene faunas from the Sea of Japan/East Sea suggest that the Barabash section might have been situated in the eastern part of the Sino-Mongolian seaway, which was located in an equivalent mid-latitude northern temperate confluence of warm- and cold-water ocean currents. G. R. Shi* [guang@uow.edu.au ] and Sangmin Lee [sangminlee76@gmail.com ], School of Earth, Atmospheric and Life Sciences, University of Wollongong, Northfields Ave, Wollongong, NSW 2522, Australia; Galina V. Kotlyar [galina_kotlyar@vsegei.ru ], Karpinsky All Russian Research Geological Institute (VSEGEI), Srednii pr. 74, St. Petersburg, 199106 Russia; Yuri D. Zakharov [ yurizakh@mail.ru ], Far East Geological Institute, Far East Branch, Russian Academy of Sciences, Vladivostok, 690022 Russia.
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