Abstract

The McCullough Peaks section of the Willwood Formation in the northern Bighorn Basin, Wyoming, has produced a rich fossil record of early Eocene mammals spanning much of the Wasatchian land-mammal age. The Wasatchian is an especially significant period in mammalian evolution since it marks the first appearance of several modern orders of mammals including Perissodactyla, Artiodactyla, and true Primates. Magnetostratigraphic analysis of paleosol horizons in the McCullough Peaks region is used to correlate Wasatchian land-mammal zones to the geomagnetic polarity time scale. A total of 135 paleomagnetic samples were analyzed from 37 levels in a 1480 m section that ranges from Wasatchian zone Wa-0 (earliest Sandcouleean subage) to the base of zone Wa-7 (earliest Lostcabinian subage). Progressive thermal demagnetization of samples from red (B type) and mottled red/gray (AB type) soil horizons provides the most reliable results. The characteristic magnetization is carried by hematite with unblocking temperature...

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