The Boxgrove tibia was discovered in 1993, associated with Middle Plei
stocene fauna, and Lower Palaeolithic archaeology. The sediments at Bo
xgrove were deposited during a temperate interglacial. episode and ens
uing cold stage. They thus represent a wide range of modes and environ
ments of deposition. Archaeological remains have been excavated from a
ll the major stratigraphic units, giving a continuity of occupation fo
r this part of southern England over a 10(4) year timescale, through m
arkedly changing climatic regimes. The stratigraphic, archaeological a
nd sedimentological contexts of the tibia are described, as well as it
s preservation and morphology. Measurements are given, with discussion
of reconstructed bone length, and stature estimates. Comparative meas
urements are provided for fossil and recent human samples: the large d
imensions of its diaphysis place the Boxgrove tibia near or beyond the
upper size limits of the comparative samples, but its reconstructed l
ength and estimated stature are less exceptional. The elevated robusti
city of the specimen indicates exceptional diaphyseal strength and/or
cold adapted body proportions paralleling those of the Neanderthals. D
isagreement about the taxonomy of Middle Pleistocene hominids and lack
of comparable fossil material make a specific assignment for the Boxg
rove tibia problematic. The tibia can only definitely be assigned to n
on-modern Homo sp., with possible further reference to Homo cf. heidel
bergensis (Schoetensack, 1908) on temporal and geographic grounds, if
the validity of that species is accepted. (C) 1998 Academic Press Limi
ted.