in 



Florida in Association with Extinct Vertebrates. 11 



locality lias affected alike, although in a slightly varying degree, 

 all of the bones of the deposit. The fossil wood in this bed, on 

 the contrary, has apparently undergone but little change, hav- 

 ing merely become water soaked and softened. ISTo implements 

 have been taken in this part of the section, although a fragment 

 of bird bone and the tip of the tusk of a proboscidian taken in 

 place at the base of this bed, show markings which apparently 



Fig. 7. 



Fig. 7. Photograph of the bank showing the human remains in place 

 in bed no. 3 as shown in text-figure 2. The ulna lies at (1) ; the humerus 

 at ( 2 ) ; and the radius at ( 3 ) . The human bones, although found at 

 slightly different actual levels, lie at the same place in the section, at the 

 bottom of the alluvial bed. 



were made by tools. Charcoal is found in this as well as in 

 the later bed at this locality. 



Human Remains from Bed No. .8 of the General Section. 



In February, 1916, Mr. Ayers obtained a human right ulna 

 which, although not found in place, was recognized as having 

 been derived from the bank, since the degree of mineralization 

 was similar to that of the associated vertebrate fossils. The 

 skeleton from which this bone came, however, was not located 



