Fish otoliths from the basal Oligocene Viborg Formation in Denmark

IF 1.2 4区 地球科学 Q2 Earth and Planetary Sciences
W. Schwarzhans, Kent A. Nielsen, Kai Ingemann Schnetler
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引用次数: 0

Abstract

The Viborg Formation is the lowest part of the early Oligocene in Denmark and represents the upper part of nannoplankton zone NP21. Here we describe a small assemblage of otoliths from the Viborg Formation obtained from five localities that yielded 88 specimens of nine species. The composition of the otolith-based f ish species is transitional between the terminal Eocene (Priabonian) faunas from the Latdorf Formation of northern Germany and its equivalents and the middle and upper Rupelian. The Viborg otolith association witnessed the first arrivals of the subsequently dominant Gadidae (Trisopterus elegans) and the migration of certain species of the merlucciid genus Palaeogadus from the Eastern Paratethys through the Polish gateway. Furthermore, the otoliths from the Viborg Formation f ill an important gap in the previous knowledge of late Eocene and early Oligocene otolith associations in the North Sea Basin and thus facilitate some refinement of their biostratigraphic usage.
丹麦基底渐新世维堡地层的鱼类耳石
维堡地层(Viborg Formation)是丹麦早渐新世的最低层,代表了NP21纳氏浮游生物区的上部。在这里,我们描述了从维堡地层的五个地点获得的少量耳石,这些耳石产生了 9 个物种的 88 个标本。以耳石为基础的物种组成是德国北部拉多夫地层(Latdorf Formation)的始新世末期(普里阿本纪)动物群及其等同物与中上鲁佩尔纪动物群之间的过渡。维堡耳石群见证了后来占主导地位的鳕形目(Trisopterus elegans)的首次到来,以及鲻形目 Palaeogadus 属的某些物种从东帕拉特提斯通过波兰门户的迁移。此外,来自维堡地层的耳石填补了以往对北海盆地晚始新世和早渐新世耳石组合认识的一个重要空白,从而有助于完善其生物地层学用途。
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来源期刊
Bulletin of the Geological Society of Denmark
Bulletin of the Geological Society of Denmark GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
2.80
自引率
16.70%
发文量
28
审稿时长
>12 weeks
期刊介绍: The Bulletin publishes contributions of international interest in all fields of geological sciences on results of new work on material from Denmark, the Faroes and Greenland. Contributions based on other material may also be submitted to the Bulletin if the subject is of relevance for the geology of the area of primary interest.
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