The age of the Middle Ordovician Winneshiek Shale: reply to a critical review by Lindskog & Young (2019) of a paper by Bergström et al . (2018a)

A recent review by Lindskog & Young (2019) of a paper published in Lethaia by Bergstrom et al. (2018a) contains many errors, misleading statements and unsupported opinions. Their review claims that we did not consider biostratigraphy in our efforts to chemostratigraphically date the Winneshiek Shale. That this is incorrect is shown by the fact that Liu et al. (2017), which contains a two-page review of all fossil evidence that has a bearing on the age of the Winneshiek Shale and was written by Bergstrom, was cited in Bergstrom et al. (2018a) and used extensively in our chemostratigraphical age assessment of the unit. Interestingly, recent research provides support for our conclusion regarding the age of the Winneshiek Shale, indicating that at least its upper part is coeval with the Nicholsonograptus fasciculatus Graptolite Zone and the Eoplacognathus pseudoplanus Conodont Zone. In constructing their arguments, Lindskog & Young (2019) provide no alternative interpretations or corrections of scientific value. (Less)

[1]  Seth A. Young,et al.  Dating of sedimentary rock intervals using visual comparison of carbon isotope records: a comment on the recent paper by Bergström et al . concerning the age of the Winneshiek Shale , 2019, Lethaia.

[2]  S. Bergström,et al.  δ 13 C Chemostratigraphy of the Ordovician‐Silurian Boundary Interval , 2018, Chemostratigraphy Across Major Chronological Boundaries.

[3]  B. Schmitz,et al.  High‐resolution δ13Corg chemostratigraphy links the Decorah impact structure and Winneshiek Konservat‐Lagerstätte to the Darriwilian (Middle Ordovician) global peak influx of meteorites , 2018 .

[4]  P. Ahlberg,et al.  Darriwilian (Middle Ordovician) chemostratigraphy linked to graptolite, conodont and trilobite biostratigraphy in the Fågelsång-3 drill core, Scania, Sweden , 2018 .

[5]  R. McKay,et al.  Exceptionally preserved conodont apparatuses with giant elements from the Middle Ordovician Winneshiek Konservat-Lagerstätte, Iowa, USA , 2017, Journal of Paleontology.

[6]  A. Lindskog,et al.  Refined Ordovician timescale reveals no link between asteroid breakup and biodiversification , 2017, Nature Communications.

[7]  T. Martma,et al.  Post-Hunnebergian Ordovician carbon isotope trend in Baltoscandia, its environmental implications and some similarities with that of Nevada , 2007 .

[8]  J. A. Rasmussen Conodont biostratigraphy and taxonomy of the Ordovician shelf margin deposits in the Scandinavian Caledonides , 2001, Fossils and Strata.

[9]  M. Boogaard Conodonts of the middle ordovician table head formation, Western Newfoundland , 1986 .

[10]  Wang Xiaofeng,et al.  Asteroid breakup linked to the Great Ordovician Biodiversification Event , 2008 .