Kenya National Museums Lukenya Hill Hominid 1 (KNM-LH 1) is a
Homo sapiens partial calvaria from site GvJm-22 at Lukenya Hill, Kenya, associated with Later Stone Age (LSA) archaeological deposits. KNM-LH 1 is securely dated to the Late Pleistocene, and samples a time and region important for understanding the origins of modern human diversity. A revised chronology based on 26 accelerator mass spectrometry radiocarbon dates on ostrich eggshells indicates an age range of 23,576–22,887 y B.P. for KNM-LH 1, confirming prior attribution to the Last Glacial Maximum. Additional dates extend the maximum age for archaeological deposits at GvJm-22 to >46,000 y B.P. (>46 kya). These dates are consistent with new analyses identifying both Middle Stone Age and LSA lithic technologies at the site, making GvJm-22 a rare eastern African record of major human behavioral shifts during the Late Pleistocene. Comparative morphometric analyses of the KNM-LH 1 cranium document the temporal and spatial complexity of early modern human morphological variability. Features of cranial shape distinguish KNM-LH 1 and other Middle and Late Pleistocene African fossils from crania of recent Africans and samples from Holocene LSA and European Upper Paleolithic sites.For Late Pleistocene African populations of modern humans, the constellation of behavioral changes encapsulated in the transition from the Middle Stone Age (MSA) to the Later Stone Age (LSA) ∼70–20 kya represents a series of some of the most pronounced changes in the archaeological record before the adoption of domesticated animals and plants and the use of ceramics for cooking and storage. It is among LSA sites that the strongest parallels with ethnographic and historic foragers are observed. Typical archaeological signatures include lithic technologies focused on the production of microliths (small flakes, blades, and bladelets with one edge blunted or “backed”) from bipolar, single-, and opposed-platform cores; an increased use of ground-stone tools; and implements made of wood and bone. These new technologies occur with the appearance of material correlates of social identity and networks of long-distance exchange, including ostrich eggshell (OES) beads, ochre, and nonlocal stone raw material, as well as increased dietary breadth, all consistent with larger, more dense, or more interconnected populations (
1–
9).This same interval of ∼70–20 kya witnessed a number of human dispersals across Africa, with eastern Africa host to one or more candidate populations for the expansion of
Homo sapiens out of Africa (
10–
15). However, the eastern African hominin fossil record for this interval is extremely sparse and poorly dated, and it consists largely of isolated teeth or highly fragmentary crania and postcrania (
16–
18). Here, we reassess the age and context of the Kenya National Museums Lukenya Hill Hominid 1 (KNM-LH 1) partial calvaria from site GvJm-22 at Lukenya Hill, Kenya, the only eastern African fossil hominin from a Last Glacial Maximum [LGM; 19–26.4 kya (
19)] LSA archaeological context. We construct a revised accelerator mass spectrometry (AMS) radiocarbon chronology built on 26 new dates on OES fragments. The revised chronology confirms the LGM age of KNM-LH 1 and expands the maximum age of the site to beyond the limits of the radiocarbon method. Increased radiometric age is consistent with new technological analyses that demonstrate previously unrecognized MSA elements that indicate assemblages spanning the MSA/LSA transition from deposits underlying KNM-LH 1. Morphometric analyses using a robust comparative dataset demonstrate the variability among African Late Pleistocene hominins, including candidate populations for out-of-Africa dispersals. They indicate that KNM-LH 1 is distinct from (
i) modern Africans, (
ii)
H. sapiens from Holocene LSA sites, and (
iii) European Upper Paleolithic modern humans, suggesting that it may sample a now extinct lineage.
相似文献