Retallack 2011 Devonian tetrapod erratum

[untitled]
Source: The Journal of Geology, Vol. 119, No. 5 (September 2011), pp. 557-558
Published by: The University of Chicago Press
Stable URL: http://www.jstor.org/stable/10.1086/661255 .
Accessed: 19/10/2011 11:56
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E R R AT U M
In the article “Woodland Hypothesis for Devonian Tetrapod Evolution,” by Gregory J. Retallack (Journal
of Geology 119:235–258), the bottom portion of figure 10 was cut off. Here is the complete figure 10 and
its caption.
Figure 10. Summary of habitats of Devonian and Mississippian terrestrial and aquatic tetrapods, prototetrapods, and
lobefin fish. Marine, lacustrine, and river channel habitats are inferred from associated fossils and sedimentary facies,
but soil habitats are interpreted from paleosols in broad categories of alluvial soil (e.g., Farwell, Gleasonton, Renovo
pedotypes), swamp soil (e.g., Sproul pedotype), and woodland soil (Hyner, Richard pedotypes; Retallack et al. 2009).
Skeletal restoration sources include the following: Eusthenopteron foordi (Clack 2002), Tiktaalik rosae (Daeschler et
al. 2006), Ichthyostega stensioi (Clack 2006), Acanthostega gunnari (Clack 2006), Tulerpeton curtum (Lebedev 1990),
Pederpes finneyae (Clack and Finney 2005), Lethiscus stocki (Wellstead 1982), Eldeceeon rolfei (Smithson 1994),
Greererpeton burkemorani (Godfrey 1989), and Dendrerpeton acadianum (Holmes et al. 1998).
[The Journal of Geology, 2011, volume 119, p. 557] 䉷 2011 by The University of Chicago.
All rights reserved. 0022-1376/2011/11905-0010$15.00. DOI: 10.1086/661255
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