Abstract

This chapter summarizes the main conclusions in this Memoir. Included is a comparison of the Arabian Intrashelf Basin events to the Haq (2017) revision of the Jurassic sea level curve. One conclusion is that the Mid- to Late Jurassic Arabian Intrashelf Basin, with its stable tectonic setting during deposition, extensive present-day outcrops and subsurface well and seismic control, may be an ideal place to evaluate global changes during its time span. The last part of this chapter lists and discusses topics and questions raised within this Memoir which warrant further evaluation.