| Literature DB >> 24789039 |
Abstract
Neandertals are the best-studied of all extinct hominins, with a rich fossil record sampling hundreds of individuals, roughly dating from between 350,000 and 40,000 years ago. Their distinct fossil remains have been retrieved from Portugal in the west to the Altai area in central Asia in the east and from below the waters of the North Sea in the north to a series of caves in Israel in the south. Having thrived in Eurasia for more than 300,000 years, Neandertals vanished from the record around 40,000 years ago, when modern humans entered Europe. Modern humans are usually seen as superior in a wide range of domains, including weaponry and subsistence strategies, which would have led to the demise of Neandertals. This systematic review of the archaeological records of Neandertals and their modern human contemporaries finds no support for such interpretations, as the Neandertal archaeological record is not different enough to explain the demise in terms of inferiority in archaeologically visible domains. Instead, current genetic data suggest that complex processes of interbreeding and assimilation may have been responsible for the disappearance of the specific Neandertal morphology from the fossil record.Entities:
Mesh:
Year: 2014 PMID: 24789039 PMCID: PMC4005592 DOI: 10.1371/journal.pone.0096424
Source DB: PubMed Journal: PLoS One ISSN: 1932-6203 Impact factor: 3.240
Hypotheses for the demise of Neandertals (a).
| 1. AMH had “complex symbolic communication systems” and “fully syntactic language”, while Neandertals did not. |
| 2 Neandertals had limited capacity for innovations. |
| 3. Neandertals were less efficient hunters. |
| 4. Neandertal weaponry was inferior to AMH projectile technology. |
| 5. Neandertals had a narrow diet, unsuccessful in competition with AMH with their more diverse diets. |
| 6. The use of traps and snares to capture animals was the exclusive domain of AMH. |
| 7. AMH had larger social networks. |
| 8. The initial AMH populations entering Neandertal territory were significantly larger than regional Neandertal populations. |
| 9. Hafting by AMH required complex procedures indicative of modern cognition, while Neandertals hafting was a simple procedure using naturally available glues. |
| 10. Cold climate around 40 ka was a factor in Neandertal decline. |
| 11. Eruption of Mount Toba volcano at 75 ka played an indirect role in Neandertal extinction. |
(a) See Text S1 Hypotheses 1–11 for details.
Dates of technological phases in the late Middle Paleolithic of Europe and in the late Middle Stone Age of South Africa (a).
| Technological phases | Start (ka) | End (ka) |
|
| ||
| Blombos | ca.75.5 (OSL) | 67.8 (OSL) |
| Sibudu | 70.5±2.0 (OSL) | |
| Diepkloof | 109±10 (TL) | |
|
| ||
| Sibudu | 64.7±2.3 (OSL) | 61.7±2 (OSL) |
| Klasies River Main Site, Cave 1A | 64.1±2.6 (OSL) | 56±3 (TL) |
| Border Cave | 74±4 (ESR) | 60±3 (ESR) |
| Diepkloof | 105±10 (TL) | 52.5±5 (TL) |
|
| ||
| Klasies, Cave 1A | 60±5 (TL) | – |
| Klasies, Cave 1A | 57.9±5.3 (OSL) | – |
| Border Cave | 60±3 (ESR) | 44−42 (14 C cal BP) |
| Sibudu | 58.5±1.4 (OSL) | 38.6±1.9 (OSL) |
| Boomplaas | ca 56±6 (U-series) | 38−36 (14 C cal BP) |
| Klein Kliphuis | 57.8±2.4 (OSL) | 33.3±1.3 (OSL) |
| Rose Cottage | 56.0±2.3 (OSL) | – |
|
| ||
| Mousterian of Acheulian Tradition(six sites in SW France) | 70 | 40 |
| Quina Mousterian(six sites in SW France) | 73 | 40 |
| The | 80 | 50 |
(a) After [89], [91]–[92], [94], [96]–[105]. We have excluded assemblages with uncertain stratigraphy (Umhlatuzana, HP layers at Klein Kliphuis) or unpublished dates (Hollow Rock Shelter).
(b) The term Post-Howiesons Poort is equivalent to MSA III at Klasies River Main Site. It includes informal designations of the Sibudu sequence such as late MSA and final MSA. We have not included several TL and OSL dates for the HP and Post-HP of Rose Cottage because they are inconsistent or only informative for the middle part of the sequence [105]–[106]. The Post-HP OSL date reported here for Rose Cottage [89] is of layer LIN which is toward the base of the Post-HP sequence but above its oldest layer.
(c) The Middle Paleolithic technocomplexes are dated by TL, ESR, 14C (calibrated BP) and chronostratigraphy.