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The diversity of teleost fishes during the terminal Cretaceous and the consequences of the K/Pg boundary extinction event – CORRIGENDUM

Published online by Cambridge University Press:  16 May 2024

Werner W. Schwarzhans Open the ORCID record for Werner W. Schwarzhans [Opens in a new window] ,
Giorgio Carnevale Open the ORCID record for Giorgio Carnevale [Opens in a new window]  and
Gary L. Stringer Open the ORCID record for Gary L. Stringer [Opens in a new window]

Abstract

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Information

Type
Corrigendum
Information
Netherlands Journal of Geosciences , Volume 103 , 2024 , e16
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution and reproduction, provided the original article is properly cited.
Copyright
© The Author(s), 2024. Published by Cambridge University Press on behalf of the Netherlands Journal of Geosciences Foundation

The authors would like to correct an error in figure 5. The correct figure is available below.

The authors apologise for the error.

Figure 5. Stratigraphical ranges of ophidiiform lineages across the Late Cretaceous and Paleocene. Skeletal reconstruction is Carnevale & Johnson (2015); drawings of extant fishes are from Markle & Olney (1990), Nielsen (1995), Böhlke & Robins (1959) and Schwarzhans et al. (2005); otoliths are from Schwarzhans (2003) and Schwarzhans & Stringer (2020) and ongoing research.

References

Schwarzhans, W.W., Carnevale, G. and Stringer, G.L. (2024) ‘The diversity of teleost fishes during the terminal Cretaceous and the consequences of the K/Pg boundary extinction event’, Netherlands Journal of Geosciences, 103, p. e5. doi: 10.1017/njg.2024.1.CrossRefGoogle Scholar
Figure 0

Figure 5. Stratigraphical ranges of ophidiiform lineages across the Late Cretaceous and Paleocene. Skeletal reconstruction is Carnevale & Johnson (2015); drawings of extant fishes are from Markle & Olney (1990), Nielsen (1995), Böhlke & Robins (1959) and Schwarzhans et al. (2005); otoliths are from Schwarzhans (2003) and Schwarzhans & Stringer (2020) and ongoing research.