TY - JOUR
T1 - Geological and taphonomic context for the new hominin species Homo naledi from the Dinaledi Chamber, South Africa
AU - Dirks, Paul H.G.M.
AU - Berger, Lee R.
AU - Roberts, Eric M.
AU - Kramers, Jan D.
AU - Hawks, John
AU - Randolph-Quinney, Patrick S.
AU - Elliott, Marina
AU - Musiba, Charles M.
AU - Churchill, Steven E.
AU - de Ruiter, Darryl J.
AU - Schmid, Peter
AU - Backwell, Lucinda R.
AU - Belyanin, Georgy A.
AU - Boshoff, Pedro
AU - Hunter, K. Lindsay
AU - Feuerriegel, Elen M.
AU - Gurtov, Alia
AU - Harrison, James du G.
AU - Hunter, Rick
AU - Kruger, Ashley
AU - Morris, Hannah
AU - Makhubela, Tebogo V.
AU - Peixotto, Becca
AU - Tucker, Steven
N1 - Publisher Copyright:
© Dirks et al.
PY - 2015/9/10
Y1 - 2015/9/10
N2 - We describe the physical context of the Dinaledi Chamber within the Rising Star cave, South Africa, which contains the fossils of Homo naledi. Approximately 1550 specimens of hominin remains have been recovered from at least 15 individuals, representing a small portion of the total fossil content. Macro-vertebrate fossils are exclusively H. naledi, and occur within clay-rich sediments derived from in situ weathering, and exogenous clay and silt, which entered the chamber through fractures that prevented passage of coarser-grained material. The chamber was always in the dark zone, and not accessible to non-hominins. Bone taphonomy indicates that hominin individuals reached the chamber complete, with disarticulation occurring during/after deposition. Hominins accumulated over time as older laminated mudstone units and sediment along the cave floor were eroded. Preliminary evidence is consistent with deliberate body disposal in a single location, by a hominin species other than Homo sapiens, at an as-yet unknown date.
AB - We describe the physical context of the Dinaledi Chamber within the Rising Star cave, South Africa, which contains the fossils of Homo naledi. Approximately 1550 specimens of hominin remains have been recovered from at least 15 individuals, representing a small portion of the total fossil content. Macro-vertebrate fossils are exclusively H. naledi, and occur within clay-rich sediments derived from in situ weathering, and exogenous clay and silt, which entered the chamber through fractures that prevented passage of coarser-grained material. The chamber was always in the dark zone, and not accessible to non-hominins. Bone taphonomy indicates that hominin individuals reached the chamber complete, with disarticulation occurring during/after deposition. Hominins accumulated over time as older laminated mudstone units and sediment along the cave floor were eroded. Preliminary evidence is consistent with deliberate body disposal in a single location, by a hominin species other than Homo sapiens, at an as-yet unknown date.
UR - http://www.scopus.com/inward/record.url?scp=84942038949&partnerID=8YFLogxK
U2 - 10.7554/eLife.09561
DO - 10.7554/eLife.09561
M3 - Article
C2 - 26354289
AN - SCOPUS:84942038949
SN - 2050-084X
VL - 4
JO - eLife
JF - eLife
IS - September2015
M1 - e09561
ER -