来自丹麦Fyn的Selandian(古新世中期)的新朱虫gundstrupensis sp.nov.(Polychaeta,Serpulidae)

IF 1.2 4区 地球科学 Q2 Earth and Planetary Sciences
T. Kočí, J. Milán, M. Jäger
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引用次数: 0

摘要

来自丹麦Fyn Gundstrup砾石坑的Kerteminde Marl组(Selandian,古新世中期)下部的一种新的serpulid物种Neo朱虫属gundstrupensis sp.nov.的管,代表了丹麦Selandian的第一批serpulid。在新蠕虫属(Oxfordian to Recent)中,新发现将最后一次有记录的密切相关的非正规细尾蛇亚群的出现从上大丹阶扩展到下塞拉兰阶。新朱粉虫的特征是直径缓慢增加,达到约5毫米,并具有小的、通常密集分布的环状条纹,偶尔合并成弱但从未强烈发育的环状外变异体。到目前为止,几乎所有发现的标本都附着在Ventriculites属的硅质海绵上。对新种管的形态、管壁的微观结构及其古生态学进行了讨论。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Neovermilia gundstrupensis sp. nov. (Polychaeta, Serpulidae) from the Selandian (middle Paleocene) of Fyn, Denmark
Tubes of a new serpulid species, Neovermilia gundstrupensis sp. nov., from the lower part of the Kerteminde Marl Formation (Selandian, middle Paleocene) of Gundstrup gravel pit, Fyn, Denmark, represent the first serpulids of this group from the Selandian of Denmark. Within the long-ranging genus Neovermilia (Oxfordian to Recent), the new finds extend the last recorded occurrence of an informal sub-group of closely related serpulids from the upper Danian to the lower Selandian. Neovermilia gundstrupensis is characterized by a tube increasing only slowly in diameter reaching up to approximately 5 mm and possessing small, often densely spaced annular striae occasionally merging into weakly but never strongly developed annular peristomes. Almost all specimens found so far are attached to siliceous sponges of the genus Ventriculites. The tube morphology of the new species and the microstructure of the tube wall, as well as its palaeoecology are discussed.
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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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