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The Ordovician sponge Palaeomanon cratera (Roemer, 1848) as an erratic on Gotland (Sweden)

机译:奥陶纪海绵Palaeomanon cratera(Roemer,1848)在哥得兰岛(瑞典)飘忽不定

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摘要

Recent cataloguing of collections of Late Ordovician erratic sponges from Gotland (Sweden) in Swedish museums has revealed the presence of Palaeomanon cratera (Roemer, 1848), previously known only from Silurian strata in Tennessee (USA) and the Northwest Territories (Canada). The species forms part of a rich sponge assemblage occurring on Gotland, representing one of three associations in north and northwest Europe, and originating from unknown source areas in Baltica. Palynomorphs extracted from adhering sediment document a Late Ordovician (Ashgill) age; thus, they are the oldest representatives of the species known to date. Naturally, this has implications for the palaeobiogeography of Palaeomanon, in relation to faunal exchange between Baltica and Laurentia; a possible migration from Baltica to Laurentia is discussed.
机译:瑞典博物馆最近对哥得兰岛(瑞典)的晚奥陶纪不定型海绵的收藏进行了分类,发现存在火山口古罗马纪古迹(Roemer,1848年),以前只有田纳西州(美国)和西北地区(加拿大)的志留纪地层才知道。该物种构成了哥得兰岛上丰富的海绵类组合的一部分,代表着北欧和西北欧洲的三个协会之一,起源于波罗的海的未知来源地区。从附着的沉积物中提取的古怪物记录了奥陶纪晚期(阿什吉尔)的年龄。因此,它们是迄今为止已知物种的最古老代表。自然地,这与波罗的海和劳伦西亚之间的动物区系交换有关,对古生物学的古生物地理有影响;讨论了从波罗的海到劳伦蒂亚的可能迁徙。

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