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中生代鸟类发声器官的化石证据。

Fossil evidence of the avian vocal organ from the Mesozoic.

机构信息

Department of Geological Sciences, University of Texas at Austin, Austin, Texas 78756, USA.

Museum of Texas Tech University, Box 43191, Lubbock, Texas 79409, USA.

出版信息

Nature. 2016 Oct 27;538(7626):502-505. doi: 10.1038/nature19852. Epub 2016 Oct 12.

Abstract

From complex songs to simple honks, birds produce sounds using a unique vocal organ called the syrinx. Located close to the heart at the tracheobronchial junction, vocal folds or membranes attached to modified mineralized rings vibrate to produce sound. Syringeal components were not thought to commonly enter the fossil record, and the few reported fossilized parts of the syrinx are geologically young (from the Pleistocene and Holocene (approximately 2.5 million years ago to the present)). The only known older syrinx is an Eocene specimen that was not described or illustrated. Data on the relationship between soft tissue structures and syringeal three-dimensional geometry are also exceptionally limited. Here we describe the first remains, to our knowledge, of a fossil syrinx from the Mesozoic Era, which are preserved in three dimensions in a specimen from the Late Cretaceous (approximately 66 to 69 million years ago) of Antarctica. With both cranial and postcranial remains, the new Vegavis iaai specimen is the most complete to be recovered from a part of the radiation of living birds (Aves). Enhanced-contrast X-ray computed tomography (CT) of syrinx structure in twelve extant non-passerine birds, as well as CT imaging of the Vegavis and Eocene syrinxes, informs both the reconstruction of ancestral states in birds and properties of the vocal organ in the extinct species. Fused rings in Vegavis form a well-mineralized pessulus, a derived neognath bird feature, proposed to anchor enlarged vocal folds or labia. Left-right bronchial asymmetry, as seen in Vegavis, is only known in extant birds with two sets of vocal fold sound sources. The new data show the fossilization potential of the avian vocal organ and beg the question why these remains have not been found in other dinosaurs. The lack of other Mesozoic tracheobronchial remains, and the poorly mineralized condition in archosaurian taxa without a syrinx, may indicate that a complex syrinx was a late arising feature in the evolution of birds, well after the origin of flight and respiratory innovations.

摘要

从复杂的歌曲到简单的鸣叫声,鸟类使用一种独特的发声器官——鸣管来产生声音。鸣管位于靠近心脏的气管支气管交界处,附着在改良的矿化环上的声韧带或膜会振动产生声音。人们认为鸣管的组成部分通常不会进入化石记录,而且少数报道的鸣管化石都是地质年轻的(来自更新世和全新世(大约 250 万年前到现在))。唯一已知的更古老的鸣管是一个未被描述或说明的始新世标本。关于软组织结构与鸣管三维几何形状之间关系的数据也非常有限。在这里,我们描述了第一个已知的中生代鸣管化石,它保存在南极晚白垩世(约 6600 万至 6900 万年前)的一个标本中,以三维形式保存。有了颅骨和后躯的遗骸,新的 Vegavis iaai 标本是从鸟类(Aves)辐射中回收的最完整的标本。对 12 种现存非雀形目鸟类的鸣管结构进行增强对比度的 X 射线计算机断层扫描(CT),以及对 Vegavis 和始新世鸣管的 CT 成像,既为鸟类祖先状态的重建提供了信息,也为灭绝物种的发声器官的特性提供了信息。Vegavis 中的融合环形成了一个矿化良好的 pessulus,这是一种衍生的新颌鸟类特征,据推测可以固定扩大的声韧带或阴唇。像 Vegavis 这样的左右支气管不对称,仅见于具有两组声源的现存鸟类中。新的数据显示了鸟类发声器官的化石潜力,并提出了一个问题,为什么这些遗骸在其他恐龙中没有被发现。其他中生代气管支气管遗骸的缺乏,以及没有鸣管的恐龙类爬行动物矿化程度差,可能表明复杂的鸣管是鸟类进化中一个较晚出现的特征,远在飞行和呼吸创新之后。

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