The Radiocarbon Searcher

 

Date: OxA-618

Age BP
 
OxA-618 (5970 ±100)
Site
 
2B Occupation to 3B Occupation ( / Great Britain and Ireland / Great Britain and Ireland )
Stored in
 
Latitude
 
51.8784
Longitude
 
-5.2920
Contact
 
M Farley & R Wilson (Bucks Co Museum)
     
     
Period
 
Late Mesolithic to Early Neolithic transition
     
     
References
 
Archaeometry, 28, 1986, 211
     
Comments
 
CL Tufa with soils, animal bones, and flint-knapping Bone, id as Bos, vertebral spine, from F602, 52-318 at Misbourne Viaduct, Gerrard's Cross, Buckinghamshire, England. Subm M Farley & R Wilson. Comment (subm): (MF): The dates in general confirm the observed stratigraphic sequence and indicate that the tufa was forming from the later Meso into the later Neolithic. Two dates give problems: OxA-620 was expected to be contemporary with OxA-601 and OxA-619, but could be a downward intrusion due to rabbit activity. The early date of the red deer vertebra OxA-621 seems unlikely both on grounds of stratigraphy and because it appears to articulate with bone in the late Meso horizon. The early presence of red deer cannot be ruled out (cf Gough's Cave).
     





























Help
Databases
Contact Info