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Corrigendum

Corrigendum

This article refers to:
A correlation between the Large Igneous Provinces and mass extinctions: constraint on the end-Guadalupian mass extinction and the Emeishan LIP in South China, eastern Tethys

Tian, X., Shi, Z., Yin, G., Long, H., and Wang, K., 2016, A correlation between the Large Igneous Provinces and mass extinctions: constraint on the end-Guadalupian mass extinction and the Emeishan LIP in South China, eastern Tethys: International Geology Review, v. 58, no. 10, p. 1215-1233. http://dx.doi.org/10.1080/00206814.2016.1147384

The authors of the above article wish to advise that, when originally published online, contained errors. The corrected version is provided below. It has also been corrected in both final print and online versions of the article.

Figure 7. Carbon isotope evolutions of the GLB sections within the ELIP and its margin in South China. The coarse dark line represents carbon isotope composition of about 4‰ from the normal Tethyan seawater in the Permian, adopted from Veizer et al. (1986, 1999) and Korte et al. (2005). All isotope data are taken from Lai et al. (2008), Wignall et al. (2009a), Saitoh et al. (2013), Wang et al. (2004), and the Zaodu section.

Figure 7. Carbon isotope evolutions of the GLB sections within the ELIP and its margin in South China. The coarse dark line represents carbon isotope composition of about 4‰ from the normal Tethyan seawater in the Permian, adopted from Veizer et al. (1986, 1999) and Korte et al. (2005). All isotope data are taken from Lai et al. (2008), Wignall et al. (2009a), Saitoh et al. (2013), Wang et al. (2004), and the Zaodu section.

References

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