Final answer:
The correct sequence of orogenies for the geologic events related to brachiopods is Sonoma, Sevier, Nevadan, and then Laramide.
Step-by-step explanation:
The correct sequence of orogenies in relation to brachiopods and related geologic events is important to understand the evolution of mountain ranges and the geological history of different regions. The orogenies of interest, namely the Nevadan, Sonoma, Sevier, and Laramide, were major mountain-building events that occurred in the western part of North America. Among them, the Sonoma Orogeny was first, followed by the Sevier Orogeny, the Nevadan Orogeny, and finally, the Laramide Orogeny. To clarify, the correct sequence is Sonoma, Sevier, Nevadan, Laramide, which aligns with the geologic records of the events leading to the formation and uplift of mountain ranges over time.
The correct sequence of orogenies for brachiopods is Sonoma, Nevadan, Sevier, and Laramide.
During the Sonoma orogeny, which occurred in the late Triassic and early Jurassic, brachiopods were present. This was followed by the Nevadan orogeny in the late Jurassic to early Cretaceous, then the Sevier orogeny in the late Cretaceous, and finally the Laramide orogeny in the late Cretaceous to early Cenozoic.