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首页> 外文期刊>Geobios: Paleontologie, Stratigraphie, Paleoecologie >Leptomitid sponges from the Cambrian (Stage 4) Balang Fauna of Guizhou, China
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Leptomitid sponges from the Cambrian (Stage 4) Balang Fauna of Guizhou, China

机译:来自寒武纪的Leptomitid海绵(第4阶段)贵州巴兰·塞努纳

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摘要

New Cambrian sponge fossils can generate alternative interpretations of the phylogenetic and biogeographical history of early sponges. Recently, many sponge fossils have been discovered from the Stage 4 Balang Fauna of Guizhou, China; these sponges are dominated by protomonaxonids, some of which can provide reliable evidence for interpreting the above-mentioned history. The sponge fossils, having the basic skeletal architecture of leptomitids, are recognized here asJianhella obconica nov. gen., nov. sp., and Leptomitus teretiusculus Chen, Hou et Lu, 1989. The new taxon has a large obconical shape; it is characterized by a dominantly longitudinal skeleton consisting of isolated longitudinal and oblique monaxons, and apparently lacks transverse spicules. The obconical body form and unique skeleton show that Jianhella nov. gen. clearly differs from previously described leptomitids and suggest that it may represent an intermediate morphology between leptomitids and basal protomonaxonids. The occurrence of Jianhella nov. gen. from a single deposit and its absence elsewhere may indicate that it was a monospecific, endemic genus, but may also suggest that it was a rare genus, so far exemplified by its occurrence in a single site with very few specimens. Additional specimens with an elongated tubular shape and a skeleton consisting of bundled longitudinal monaxons and isolated transverse spicules closely fit the description and illustrations of Leptomitus teretiusculus from the Cambrian biotas of South China. According to the spicule morphology, the degree of spicule bundling and the skeletal architecture, there likely exists a deep node separating Jianhella nov. gen. from the earlier ancestral members of Leptomitus. Fossil evidence, together with previous studies, confirms that Leptomitus generally had a relatively long stratigraphic range (Cambrian Stage 3 to Drumian) and had an effectively cosmopolitan distribution during the early and middle Cambrian. (C) 2019 Elsevier Masson SAS. All rights reserved.
机译:新的寒武纪海绵化石可以产生早期海绵的系统发育和生物地理学史的替代解释。最近,许多海绵化石已从中国贵州的BALANG FAUNA阶段发现;这些海绵占据主导的原子蒙古蛋白,其中一些可以提供可靠的证据来解释上述历史。具有Leptomitids的基本骨骼建筑的海绵化石在这里被认为是asjianhella obconica 11月。 Gen。,11月。 SP。和Leptomitus Teretiusculus Chen,Hou et Lu,1989.新的分类群具有大的相互相互相互相互的形状;它的特征在于由分离的纵向和倾斜的Monaxons组成的主要纵向骨架,并且显然缺乏横向斑块。相互相互的身体形态和独特的骨架表明剑窝菌11月。 Gen。清楚地与先前描述的乳腺菌有关,并表明它可以代表瘦肿瘤和基底原素酸的中间形态。剑窝菌的发生11月。 Gen。从单一的沉积物中,其他地方的缺席可能表明它是一种单特异性,但也可能表明它是一种罕见的属,到目前为止其在一个具有很少的标本中的单一站点中的发生。具有细长管状形状的额外标本和由捆绑的纵向Monaxons和分离的横向斑块组成的骨架密切关注来自华南寒册生物群的Leptomitus Teretiusculus的描述和说明。根据分子形态,分子捆绑的程度和骨骼架构,很可能存在一个分隔剑窝菌的深度节点。 Gen。从瘦菌的早期祖先成员。化石证据与以前的研究一起证实,Leptomitus通常具有相对较长的地层范围(寒武纪3至鼓舞人员),并且在早期和中间寒武纪中有一个有效的国际化学分布。 (c)2019年Elsevier Masson SAS。版权所有。

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