Vero man refers to a set of fossilized human bones found near Vero (now Vero Beach), Florida, in 1915 and 1916. The human bones were found in association with those of animals. The question of whether humans were present in Florida (or anywhere in the Americas) during the Pleistocene was controversial at the time, and most archaeologists did not accept that the Vero fossils were that old. Recent studies show that the Vero human bones are from the Pleistocene, and are the largest collection of human remains from the Pleistocene found in North America.
Starting in late 1913 vertebrate fossils were uncovered during the construction of a drainage canal from the Indian River between Vero and Gifford. Samples of the fossils were sent by Isaac M. Weills and Frank Ayers to the state geologist of Florida, E. H. Sellards, who recognized the finds as animals. In 1915, 26 fossilized human bones and fragments were found in the banks of the canal. The following year Sellards conducted his own excavations at the site, recovering an engraved mammoth tusk and a bird bone with marks possibly made by humans. In a nearby location he recovered human bones from the stratum that contained Pleistocene fossils. Sellards also found chert flakes and bone tools, including what appears to be a broken stemmed Archaic projectile point, and near the surface found a few ceramic sherds.
Sellards first published his findings in 1916. He invited other scientists to visit the Vero site and investigate it themselves in October 1916 and in March 1917. Aleš Hrdlička, T. Wayland Vaughan, Oliver Perry Hay, George Grant MacCurdy and Rollin T. Chamberlin visited and examined the site. Sellards and Hays concluded that the human bones dated from the Pleistocene. Hrdlička, MacCurdy and Chamberlin argued that the human bones were much more recent, while Vaughan felt that more evidence was needed before making a decision. Hrdlička, the most prominent physical anthropologist in America at the time, was firmly convinced that humans had not arrived in America until well after the Pleistocene had ended.