Thomas Farm site: An ancient sinkhole with an associated cave system not unusual for N. Florida. It's within a calcareoussandstone and blue claystone. The fossils are from multiple horizons including a joint clay; a layer of clayballs, lime sand; a bed of limestone, boulders with gravel and lime sand matrix; and a laminated bluish clay. Most of the material is from the lime sand. The biochronology points to an early Hemingfordian origin through the presence of the ancient bear, Phoberocyon, the mustelid Leptarctus, the rhino Floridaceras, and Metatomarctus, a canid.[4] The Thomas Farm site is located on the Alachua Formation.
Toledo Bend site: A coarse palaeochannel fill; a conglomerate likely from an episode of violent flood mixing of materials. (Albright, 1999). Also recovered with several mammals including two other Tayassuidae (Marshochoerus, Hesperhys) three species of rhino, two species of horse, the Dinohyus, Daphoedon, and Nothokemas.
