Letter | Published:

Fossil evidence of the avian vocal organ from the Mesozoic

Nature volume 538, pages 502505 (27 October 2016) | Download Citation


From complex songs to simple honks, birds produce sounds using a unique vocal organ called the syrinx1,2. Located close to the heart at the tracheobronchial junction, vocal folds or membranes attached to modified mineralized rings vibrate to produce sound1,2,3,4,5,6,7. Syringeal components were not thought to commonly enter the fossil record6, and the few reported fossilized parts of the syrinx are geologically young8,9,10,11 (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 illustrated12. Data on the relationship between soft tissue structures and syringeal three-dimensional geometry are also exceptionally limited5. 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 labia5. 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.

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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.

Author information


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

    • Julia A. Clarke
    •  & Zhiheng Li
  2. Museum of Texas Tech University, Box 43191, Lubbock, Texas 79409, USA

    • Sankar Chatterjee
  3. Key Laboratory of Vertebrate Evolution and Human Origins, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China

    • Zhiheng Li
  4. Department of Physiology, Midwestern University, 19555 N 59th Avenue, Glendale, Arizona 85308, USA

    • Tobias Riede
  5. Conicet — Laboratorio de Anatomía Comparada y Evolución de los Vertebrados, Museo Argentino de Ciencias Naturales, Av. Ángel Gallardo 470, C1405DJR Buenos Aires, Argentina

    • Federico Agnolin
    • , Marcelo P. Isasi
    •  & Fernando E. Novas
  6. Fundación de Historia Natural “Félix de Azara”, Universidad Maimónides, Hidalgo 775, C1405BDB Buenos Aires, Argentina

    • Federico Agnolin
  7. Department of Biology, University of Utah, 257 South 1400 East, Salt Lake City, Utah 84112, USA

    • Franz Goller
  8. Laboratorio de Geologia Andina, CADIC-Conicet, B.Houssay 200, CP V9410CAB Ushuaia, Tierra del Fuego, Argentina

    • Daniel R. Martinioni
  9. Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Ciudad Autónoma de Buenos Aires, CP C1405DJR Buenos Aires, Argentina

    • Francisco J. Mussel


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D.R.M. and F.J.M. collected the fossil specimen and contributed geological data. M.P.I. and S.C. contributed to the fossil specimen preparation and study. T.R., F.G., Z.L. and J.A.C. designed the study of the syrinx and collected primary data. Z.L. designed the enhanced contrast CT protocol and collected extant CT data. J.A.C. discovered the fossil syrinx remains and designed the project with F.E.N., S.C., T.R. and F.G. J.A.C., Z.L., F.A., F.E.N., T.R., F.G. and S.C. conducted morphological study of the specimen.

Competing interests

The authors declare no competing financial interests.

Corresponding author

Correspondence to Julia A. Clarke.

Reviewer Information

Nature thanks P. O’Connor and the other anonymous reviewer(s) for their contribution to the peer review of this work.

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