TWO REMARKABLE FOSSIL INSECT LARVAE FROM BURMESE AMBER SUGGEST THE PRESENCE OF A TERMINAL FILUM IN THE DIRECT STEM LINEAGE OF DRAGONFLIES AND DAMSELFLIES (ODONATA)

IF 1.6 3区 地球科学 Q2 GEOLOGY Rivista Italiana Di Paleontologia E Stratigrafia Pub Date : 2020-01-08 DOI:10.13130/2039-4942/12720
M. Schädel, P. Müller, J. Haug
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引用次数: 8

Abstract

The fossil record of dragonfly relatives (Odonatoptera) dates back to the Carboniferous, yet knowledge about these extinct animals is meagre. For most of the species little is known except for the characteristics of the wing venation. As a result, it is difficult to include fossil larvae in a (wing character based) phylogenetic tree as the wing venation is not visible in most of the larval instars.             Two larval specimens from Cretaceous Burmese amber are in the focus of this study. The two specimens likely represent two subsequent early stage larval instars of the same individual. Not only is this an exceptional case to study ontogenetic processes in fossils – the larval instars are morphologically completely different from all known larvae of Odonata with respect to the posterior abdominal region. Therefore, besides the difficulties regarding the phylogenetic interpretation and though all Burmese amber odonatans are known from adults only, a new species – Arcanodraco filicauda n. sp. – is formally described.             Aside from likely representing a new species, the morphology of the posterior abdominal region is highly informative for reconstructing the character evolution within the lineage towards modern dragonflies and damselflies. A long median process in both of the fossils meets all criteria to be interpreted as a terminal filum (structure or derivative of tergite of abdominal segment 11, annulated in one of the specimens). Although the exact phylogenetic affinity of Arcanodraco filicauda n. sp. remains enigmatic, the presence of a larval terminal filum can be reconstructed for the ground pattern of Odonatoptera (including its direct stem lineage).
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从缅甸琥珀中发现的两种不同寻常的昆虫幼虫化石表明,在蜻蜓和豆娘的直接茎系中存在一种末端丝状物。
蜻蜓亲属(蜻蜓目)的化石记录可以追溯到石炭纪,但对这些灭绝动物的了解却很少。对于大多数物种来说,除了翅膀脉络的特征外,几乎一无所知。因此,很难将幼虫化石包括在(基于翅膀特征的)系统发育树中,因为在大多数幼虫龄期中都看不到翅膀脉络。白垩纪缅甸琥珀的两个幼虫标本是本研究的重点。这两个标本可能代表同一个体随后的两个早期幼虫龄。这不仅是研究化石个体发生过程的一个特例——在后腹部区域,幼虫龄在形态上与所有已知的蜻蜓幼虫完全不同。因此,除了系统发育解释方面的困难之外,尽管所有缅甸琥珀齿龙都只从成虫身上已知,但一个新物种——细尾龙——也被正式描述。除了可能代表一个新物种外,后腹部区域的形态对于重建现代蜻蜓和豆娘谱系中的特征进化具有重要信息意义。两个化石中的长中突都符合所有标准,可以被解释为终丝(腹部节段11的tergite的结构或衍生物,在其中一个标本中呈环状)。尽管Arcanodraco filicoda n.sp.的确切系统发育亲和力仍然是个谜,但幼虫末端丝的存在可以为齿翅目的地面模式(包括其直接茎系)重建。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
3.60
自引率
4.30%
发文量
28
审稿时长
>12 weeks
期刊介绍: The Rivista Italiana di Paleontologia e Stratigrafia was founded in 1895. It publishes original papers dealing with all fields of paleontology and of stratigraphy, from Italy and the Mediterranean to the Tethys, as well across the globe from China to North America.
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