一个泥盆纪四足动物的头骨碎片,具有独特的侧线形态,收藏于柏林自然博物馆

IF 1.4 4区 地球科学 Q3 Earth and Planetary Sciences
Florian Witzmann
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引用次数: 2

摘要

图中详细描述了来自拉脱维亚Ketleri的famenian晚期的一块真皮骨,由Oleg Lebedev鉴定为可能的四足动物后兽,并保存在柏林自然博物馆(Museum fnaturkunde Berlin)。它的四足动物身份是基于由多边形凹坑和径向排列的脊和沟组成的皮肤雕刻。这个雕塑类似于泥盆纪的四足动物,但却不像大多数泥盆纪后的形式那样规则。由于其前缘凹,侧线无分叉,骨化中心位于骨的背侧部分,因此可以将其指定为眶后骨。侧线(即眶下线的眶后支)在眶后腹侧形成一个开放的深沟,但在背侧部分被封闭在骨内,并通过孔打开到表面。这种后趾分支的形态在基生四足动物中是独特的。这块骨头可能属于四足动物Ventastega curonica Ahlberg et al., 1994,这是在Ketleri的同一地层中发现的,然而,由于该分类单元的后生物是未知的,所以不能肯定地说。(©2010 WILEY-VCH Verlag GmbH &KGaA公司,Weinheim)
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A skull fragment of a Devonian tetrapod with a unique lateral line morphology in the collection of the Museum für Naturkunde Berlin

A dermal bone from the late Famennian of Ketleri in Latvia, identified as a probable tetrapod postorbital by Oleg Lebedev and stored in the Museum für Naturkunde Berlin, is described in detail. Its tetrapod status is confirmed based on the dermal sculpture consisting of polygonal pits and radially aligned ridges and furrows. The sculpture resembles that of Devonian tetrapods but is nevertheless not as regular as in most post-Devonian forms. The bone can be designated as a postorbital because of its concave anterior margin, the lateral line that shows no bifurcation, and the ossification centre that is located in the dorsal portion of the bone. The lateral line (i.e., the postorbital branch of the infraorbital line) forms an open, deep sulcus in the ventral portion of the postorbital but is enclosed within the bone in the dorsal portion and opens through pores to the surface. This morphology of the postorbital branch is unique among basal tetrapods. The bone might belong to the tetrapod Ventastega curonica Ahlberg et al., 1994 that is known from the same strata at Ketleri, however, since the postorbital is unknown in this taxon, this cannot be stated with certainty. (© 2010 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim)

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来源期刊
Fossil Record
Fossil Record PALEONTOLOGY-
CiteScore
2.50
自引率
7.10%
发文量
18
审稿时长
>12 weeks
期刊介绍: Fossil Record (FR) is the palaeontological journal of the Museum für Naturkunde Berlin. This journal was founded in 1998 under the name Mitteilungen aus dem Museum für Naturkunde Berlin, Geowissenschaftliche Reihe and appears with two issues each year. Fossil Record publishes original papers in all areas of palaeontology including the taxonomy and systematics of fossil organisms, biostratigraphy, palaeoecology, and evolution. All taxonomic groups are treated, including invertebrates, microfossils, plants, and vertebrates.
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