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Though most material is from Late Pleistocene deposits unearthed by Storrs L. Olson, David B. Wingate and others in the Admirals Cave, the Wilkinson Quarry, and in the Walsingham Sink Cave in Hamilton Parish in Bermuda in 1981 there is one bone, a tarsometatarsus from a juvenile, which is from a Holocene layer in the Spittal Pond.
A prehistoric relative, Euphagus magnirostris, is known from Late Pleistocene fossils found in the famous tar seeps of Rancho La Brea, California.
A species of fossil duck from the Late Pleistocene of Vero Beach, Florida, was described as Querquedula floridana (a genus now included in Anas), but upon reexamination turned out to be a species closely related to the Hooded Merganser; it is now named Lophodytes floridanus, but the exact relationship between this bird and the modern species is unknown.
Pupilla loessica was first described by Czech biologist Vojen Ložek (1954) from late Pleistocene loess from Předmostí near Přerov (Moravia, Czech Republic).
All remains except one Early Pleistocene partial skeleton from the Leisey Shell Pit near Charlotte Harbor, Florida (which may represent a different species or a subspecies) date from the Late Pleistocene, with the youngest remains dating from the Pleistocene-Holocene boundary.
If Viator picis, also from the Late Pleistocene of Talara, does not belong to an entirely extinct lineage, it might belong to that group too; it seems too large to be closely related to the smallish Pied Lapwing.
Fossils of Alpine ibex date back to the late Pleistocene, when it and the Spanish ibex probably evolved from the extinct Pleistocene species Capra camburgensis.
Bonneville cutthroats are descended from cutthroat trout that once inhabited the Late Pleistocene-aged Lake Bonneville of Utah, eastern Nevada, and southern Idaho.
Fossils of Conus californicus have been recovered from the Late Pleistocene strata of Isla Vista, California.
Anthropologist Tom Dillehay dates the earliest hunter-gatherer cultures on the continent at almost 10,000 BC, during the late Pleistocene and early Holocene periods.
The Presumpscot formation is a late Pleistocene glacial deposit of predominantly submarine clays, located along the Maine and New Hampshire coast and inland along their major river valleys.