TY - JOUR
T1 - Use of red ochre by early Neandertals
AU - Roebroeks, W.
AU - Sier, M.J.
AU - Kellberg Nielsen, T.
AU - De Loecker, D.
AU - Parés, J.
AU - Arps, C.E.S.
AU - Mücher, H.J.
PY - 2012
Y1 - 2012
N2 - The use of manganese and iron oxides by late Neandertals is well
documented in Europe, especially for the period 60–40 kya. Such
finds often have been interpreted as pigments even though their
exact function is largely unknown. Here we report significantly
older iron oxide finds that constitute the earliest documented
use of red ochre by Neandertals. These finds were small concentrates
of red material retrieved during excavations at Maastricht-
Belvédère, The Netherlands. The excavations exposed a series of
well-preserved flint artifact (and occasionally bone) scatters,
formed in a river valley setting during a late Middle Pleistocene
full interglacial period. Samples of the reddish material were submitted
to various forms of analyses to study their physical properties.
All analyses identified the red material as hematite. This is
a nonlocal material that was imported to the site, possibly over
dozens of kilometers. Identification of the Maastricht-Belvédère
finds as hematite pushes the use of red ochre by (early) Neandertals
back in time significantly, to minimally 200–250 kya (i.e., to the same
time range as the early ochre use in the African record)
AB - The use of manganese and iron oxides by late Neandertals is well
documented in Europe, especially for the period 60–40 kya. Such
finds often have been interpreted as pigments even though their
exact function is largely unknown. Here we report significantly
older iron oxide finds that constitute the earliest documented
use of red ochre by Neandertals. These finds were small concentrates
of red material retrieved during excavations at Maastricht-
Belvédère, The Netherlands. The excavations exposed a series of
well-preserved flint artifact (and occasionally bone) scatters,
formed in a river valley setting during a late Middle Pleistocene
full interglacial period. Samples of the reddish material were submitted
to various forms of analyses to study their physical properties.
All analyses identified the red material as hematite. This is
a nonlocal material that was imported to the site, possibly over
dozens of kilometers. Identification of the Maastricht-Belvédère
finds as hematite pushes the use of red ochre by (early) Neandertals
back in time significantly, to minimally 200–250 kya (i.e., to the same
time range as the early ochre use in the African record)
U2 - 10.1073/pnas.1112261109
DO - 10.1073/pnas.1112261109
M3 - Article
SN - 0027-8424
VL - 109
SP - 1889
EP - 1894
JO - Proceedings of the National Academy of Sciences of the United States of America
JF - Proceedings of the National Academy of Sciences of the United States of America
IS - 6
ER -