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Palaeontological Note

New material from the Ordovician of China indicates that Inocaulis is a graptolite

Pages 565-566 | Received 13 Dec 2012, Accepted 13 May 2013, Published online: 10 Jul 2013

References

  • Bouček, B., 1957. The dendroid graptolites of the Silurian of Bohemia. Rozpravy Ústředního ústavu geologického23, 1–294.
  • Bronn, H.G., 1849. Index Palaeontologicus B, Enumerator Palaeontologicus. E. Schweizerbart’sche, Stuttgart, 980 pp.
  • Grote, A.B. & Pitt, W.H., 1876. The discovery of a marine fucoid from the Water Lime Group. Bulletin of the Buffalo Society of Natural Sciences3, 88.
  • Hall, J., 1852. Palaeontology of New York, Volume II. Containing Descriptions of the Organic Remains of the Lower Middle Division of the New-York System (Equivalent in Part to the Middle Silurian Rocks of Europe). Geological Survey of New York, Albany . 362 pp.
  • Mierzejewski, P., 1986. Ultrastructure, taxonomy and affinities of some Ordovician and Silurian organic microfossils. Palaeontologia Polonica47, 129–220.
  • Mitchell, C.E., Melchin, M.J., Cameron, C.B. & Maletz, J., 2013. Phylogenetic analysis reveals that Rhabdopleura is an extant graptolite. Lethaia46, 34–56.
  • Zhang, Y.-D., Chen, X. & Goldman, D., 2007. Diversification patterns of Early and Mid Ordovician graptolites in South China. Geological Journal42, 315–337.

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