TY - JOUR
T1 - Fossil evidence of the avian vocal organ from the Mesozoic
AU - Clarke, Julia A.
AU - Chatterjee, Sankar
AU - Li, Zhiheng
AU - Riede, Tobias
AU - Agnolin, Federico
AU - Goller, Franz
AU - Isasi, Marcelo P.
AU - Martinioni, Daniel R.
AU - Mussel, Francisco J.
AU - Novas, Fernando E.
N1 - Funding Information:
This project was funded by the Gordon and Betty Moore Foundation (grant GBMF4498; J.A.C., T.R. and F.G.), as well as the National Science Foundation (OPP ANT-1141820, OPP 0927341 and EAR 1355292; J.A.C.), C. Burke and the Agencia Nacional de Promoción Científica y Técnica (PICT 2010-066; F.E.N). The Instituto Antártico Argentino (IAA), G. M. Robles, W. J. Zinsmeister and especially C. A. Rinaldi, E. B. Olivero, and the Fuerza Aérea Argentina provided key support for fieldwork in 1993.
Publisher Copyright:
© 2016 Macmillan Publishers Limited, part of Springer Nature. All rights reserved.
PY - 2016
Y1 - 2016
N2 - 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.
AB - 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.
UR - http://www.scopus.com/inward/record.url?scp=84993940158&partnerID=8YFLogxK
U2 - 10.1038/nature19852
DO - 10.1038/nature19852
M3 - Article
C2 - 27732575
AN - SCOPUS:84993940158
SN - 0028-0836
VL - 538
SP - 502
EP - 505
JO - Nature
JF - Nature
IS - 7626
ER -