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Schischcatella (Fenestrata, Bryozoa) from the Devonian of the Rhenish Massif, Germany

机译:来自德国Rhenish断层泥盆纪的Schischcatella(Fenestrata,Bryozoa)

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摘要

The Devonian fenestrate bryozoan, SchischcatellaWaschurova, 1964, possessed colonies in the form of low, erect bifoliate fronds that grew from an encrusting sheet-like base with autozooecia arranged in biserial, bifurcating rows. This growth habit is unique in fenestrates, which normally had unilaminate arborescent colonies. Originally, Schischcatella was described from the Lower Devonian of Tajikistan. This article describes a new species, S. heinorum sp. nov., from the Middle Devonian of the Eifel (western Rhenish Massif, Germany) with additional material from the Lower Devonian of the Kellerwald (eastern Rhenish Massif, Germany). External and internal morphologies of this bryozoan have been studied using abundant material. The growth habit of Schischcatella suggests a completely different pattern of feeding currents than that in the normal fenestrate colony. The outflow of the filtered water occurred only on edges of colonies between rami. In the absence of chimneys (areas of vertical water expelling), such a functional morphology may have restricted extension of the colony in a distal direction. The evolution of Schischcatella is apparently an example of paedomorphosis, the genus evolved from an unknown semicosciniid species by the early ontogenetic interruption of colony development and further changes in the mode of growth.
机译:泥盆纪有优势的苔藓动物,SchischcatellaWaschurova,1964,具有低直立的双叶状叶片的菌落,该叶状叶由盘绕的片状基部生长而成,自生动物排列成双分叉状。这种生长习性在通常具有单层状树状菌落的甲虫中是独特的。 Schischcatella最初是从塔吉克斯坦的下泥盆纪开始描述的。本文介绍了一个新物种,S。heinorum sp。十一月,来自埃菲尔中泥盆纪(德国莱茵河断层块),以及来自凯勒瓦德下泥盆纪(德国东部莱茵河断层块)的其他材料。已使用大量材料研究了这种苔藓虫的外部和内部形态。 Schischcatella的生长习性表明,与正常穿孔菌落中的摄食电流完全不同。过滤水的流出仅发生在拉米之间的菌落边缘。在没有烟囱(垂直水排出区域)的情况下,这种功能形态可能会限制菌落在远端方向上的延伸。 Schischcatella的进化显然是paedomorphosis的一个例子,该属通过殖民地发育的早期个体发育中断和生长方式的进一步改变而从未知的半球孢菌种进化而来。

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