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Unravelling a Late Ordovician pentameride (Brachiopoda) hotspot from the Boda Limestone, Siljan district, central Sweden

机译:从瑞典中部Siljan区的Boda石灰石中解开奥陶纪晚期的pentameride(Brachiopoda)热点

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The correlation of the uppermost Boda Core Member of the Boda Limestone is reassessed and the beds assigned to the upper Katian. This is based on the identification of the brachiopod species Brevilamnulella kjerulfi (Kiaer) and Amphiplecia tardicostata Wright & Jaanusson from the highest beds in the unit. The former species is overwhelmingly abundant in the uppermost beds of the Boda Core Member in Osmundsberget quarry, forming an almost monospecific coquina. Also occurring in the coquina, is Clorilamnulella osmundsbergensis gen. et sp. nov., which ranges into the overlying Hirnantian Glisstjarn Formation. The new genus is here regarded as a transitional form between Brevilamnulella and Clorinda. The oldest occurrence of this latter genus is here revised and not found in rocks older than the Aeronian. Instead, previous Rhuddanian occurrences of ‘Clorinda’ are transferred to Clorilamnulella based on a dorsal cardinalia that differs from both that of Brevilamnulella, as well as that of Clorinda. Moreover, gigantic shells of a new species of Brevilamnulella, B. umbosulcata sp. nov, are described from the nearby Solberga quarry where the species occurs in great abundance in a local fossil pocket, that also is correlated with the upper Katian. These new virgianid and clorindoid occurrences, together with previously described occurrences of Holorhynchus and Costilamnulella, demonstrate that during the late Katian, the Boda Limestone was a virgianid hotspot crucial in the evolution of the earliest pentameroid family, the Virgianidae, as well as a possible early cradle for the evolution of the hitherto exclusively Silurian superfamily, the Clorindoidea.
机译:重新评估了Boda石灰岩的最高Boda核心成员的相关性,并将床分配给了上Katian。这是基于从该单元最高层中鉴定腕足动物Brevilamnulella kjerulfi(Kiaer)和Amphiplecia tardicostata Wright和Jaanusson的结果。在Osmundsberget采石场的Boda核心成员的最上层床中,前一种物种非常丰富,形成了几乎单种的喹诺酮。在coquina中也出现了Closirilamnulella osmundsbergensis gen。等。 11月,其范围包括上覆的Hirnantian Glisstjarn组。在这里,新属被认为是布氏杆菌和克林达之间的过渡形式。后一属的最古老发生在这里被修改,在比Aeronian年龄更大的岩石中找不到。取而代之的是,以前的罗丹科“ Clorinda”事件根据背侧心基转移到Clorilamnulella,而背心不同于Brevilamnulella和Clorinda。此外,巨大的壳的Brevilamnulella,B。umbosulcata sp。的新物种。 nov是从附近的Solberga采石场进行描述的,该物种在当地的化石袋中大量存在,而该化石也与上层Katian有关。这些新的virgianid和clorindoid的出现,以及先前描述的Holorhynchus和Costilmnulella的出现,表明在凯迪安晚期,Boda石灰石是一个virgianid热点,在最早的五倍体类,Virgianidae以及可能的早期进化中至关重要是迄今为止志留纪超家族Clorindoidea进化的摇篮。

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