**Acknowledgements**

**Figure 9.** A shallow-marine peritidal succession measured in core of Ebbutt D-50 well (southern Mackenzie Corridor): (A) Striplog showing lack of well log response at multiple paleosols. (B–D) Polished and etched core face with details of paleosol at 600.25 m; (B) box view with pedogenic claystone-to-calcrete at 600.25–602.0 m (1969.3–1975.0 ft) and intense alteration down to at least 603.5 m (1980.0 ft); black arrow points at hydrothermal dolostone vein. (C) Top of paleosol profile composed of multiphase clayey calcrete; (D) float breccia at 600.9 m with residual clasts of marine limestone (*cl*).

118 Seismic and Sequence Stratigraphy and Integrated Stratigraphy - New Insights and Contributions

Sticky marks are ED-XRF reading points.

This work is a contribution to the Mackenzie and Western Arctic projects of the Geomapping for Energy and Minerals Program (GEM-2) and IGCP-652 "Reading geologic time in Paleozoic sedimentary rocks: the need for an integrated stratigraphy." Cordial thanks are due to the volume editor and reviewer Gemma Aiello, GSC reviewer Keith Dewing, and my better half Darya Baranova who worked through text and literature formatting. Colleagues of GSC Milovan Fustic and John W. Shimeld are greatly thanked for contributing figures. This is the NRCan Lands and Minerals Sector contribution # 20170095.
