I 'liked' this part concerning the early Holocene silty (retransported loess or “muck”) Ready Bullion Formation:
It contains none of the many extinct Pleistocene forms such as bison, horse, and mammoth present in the underlying Goldstream Formation. The only vertebrate remains the writer collected from this formation are well-preserved perennially frozen moose coprolites.
So, according to the 1975 USGS report, there was a (at least) local extinction event some time before 10,000 years ago.
The 2017 paper included this about the Wisconsinian Goldstream Formation:
The remarkable preservation of vertebrate and plant remains within the mucks, however, is in stark contrast to the physical disruption and damage affecting much of this material. Much of the skeletal remains from Alaska and Yukon were disarticulated and broken prior to freezing (Fig. 3a), and the rare preserved carcasses were often mangled and torn apart. Such dismemberment has been attributed to predators and scavengers, but these explanations raise questions including why the carcasses’ remaining fat and flesh had not been consumed. In addition, the fine-grained character of the mucks differs markedly from that of the more massive logs, megafaunal bones and tusks enclosed within it.
...
In view of this new evidence [not copied here], the mucks and their well-preserved but highly disrupted and damaged vertebrate and botanical remains are reinterpreted in part as blast deposits that resulted from several episodes of airbursts and ground/ice impacts within the northern hemisphere during Late Pleistocene time (~46–11 ka B.P.)
The Wisconsinian glaciation itself could be a reasonable cause of 'an extinction event', but this paper is all about catastrophic events.