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Bryozoan borings in shells of Costa Rican miocene oysters

机译:哥斯达黎加中新世牡蛎壳中的苔藓虫钻孔

摘要

Borings of bryozoan colonies are rare fossils and hitherto unknown from Central America. Four different types of zoaria, belonging to Spathipora sp., Terebripora sp. A, Terebripora cf. falunica and Iramena sp., were recognized. They are developed on shells of Miocene oysters (Saccostrea sp. and Ostrea sp.) from shell - beds of the Venado-Formation (Northern Limon - San Carlos Basin, Costa Rica). The period of colonization and growth by bryozoans and/or a few other benthic invertebrates was probably a short - term event, followed by suffocation from accumlating sediment.
机译:苔藓虫菌落的钻孔是罕见的化石,迄今为止是中美洲迄今未知的。四种不同的zoaria,属于Spathipora sp。,Terebripora sp.。 A,Terebripora参见。 falunica和Iramena sp。被认可。它们是从中新世牡蛎壳(Saccostrea sp。和Ostrea sp。)的壳上发育而来的,这些壳是由Venado-Formation的床层(北里蒙-哥斯达黎加的圣卡洛斯盆地)形成的。苔藓虫和/或其他一些底栖无脊椎动物的定居和生长时期可能是短期事件,随后由于沉积物的堆积而窒息而死。

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