scholarly journals Pleistocene Archaeology and Chronology of Putslaagte 8 (PL8) Rockshelter, Western Cape, South Africa

2015 ◽  
Vol 13 (1) ◽  
pp. 71-98 ◽  
Author(s):  
Alex Mackay ◽  
Zenobia Jacobs ◽  
Teresa E. Steele
Keyword(s):  
Late Pleistocene ◽  
Material Selection ◽  
Middle Stone Age ◽  
Western Cape ◽  
Stone Age ◽  
Before Present ◽  
Later Stone Age ◽  
Occupational Patterns ◽  
Chronological Sequence ◽  
Mis 5

We report on excavations of a small rock shelter — Putslaagte 8 (PL8) — located on the arid interior fringe of South Africa’s Fynbos biome. The shelter preserves a long sequence of Holocene and late Pleistocene occupation dating back beyond 75,000 years BP. This paper presents data on the technological, faunal and chronological sequence. Occupation is markedly pulsed and includes three late Pleistocene Later Stone Age (LSA) units (macrolithic, Robberg and early LSA), as well as several distinct Middle Stone Age (MSA) components from Marine Isotope Stage (MIS) 3–5. Pulsing may reflect the arid and possibly marginal environments in which the shelter is situated, and to that end some elements of the sequence contrast with occupational patterns towards the coast. Viewed in a regional setting PL8 suggests: 1) complementarity of resource movements between the coast and interior in terminal MIS 2; 2) distinctions in material selection, and possibly technology, between the coast and interior in earlier MIS 2; 3) an MSA lasting to at least 40,000 years before present; 4) a weak Howiesons Poort and post-Howiesons Poort in the interior; 5) possibly distinct periods of denticulate manufacture within the MIS 5 MSA; 6) highly localised patterns of material acquisition in the earlier MSA.

The Cyrenaican Prehistory Project 2012: the sixth season of excavations in the Haua Fteah cave

2013 ◽  
Vol 44 ◽  
pp. 113-125 ◽  
Author(s):  
Ryan Rabett ◽  
Lucy Farr ◽  
Evan Hill ◽  
Chris Hunt ◽  
Ross Lane ◽  
...  
Keyword(s):  
Seismic Event ◽  
Middle Stone Age ◽  
Arid Environments ◽  
Stone Age ◽  
Late Stone Age ◽  
Climatic Regime ◽  
Molluscan Fauna ◽  
Trench Area ◽  
Mis 5 ◽  
Deep Sounding

AbstractThe paper reports on the sixth season of fieldwork of the Cyrenaican Prehistory Project (CPP) undertaken in September 2012. As in the spring 2012 season, work focussed on the Haua Fteah cave and on studies of materials excavated in previous seasons, with no fieldwork undertaken elsewhere in the Gebel Akhdar. An important discovery, in a sounding excavated below the base of McBurney's 1955 Deep Sounding (Trench S), is of a rockfall or roof collapse conceivably dating to the cold climatic regime of Marine Isotope Stage (MIS) 6 (globally dated to c. 190–130 ka) but more likely the result of a seismic event within MIS 5 (globally dated to c. 130–80 ka). The sediments and associated molluscan fauna in Trench S and in Trench D, a trench being cut down the side of the Deep Sounding, indicate that this part of the cave was at least seasonally waterlogged during the accumulation, probably during MIS 5, of the ~6.5 m of sediment cut through by the Deep Sounding. Evidence for human frequentation of the cave in this period is more or less visible depending on how close the trench area was to standing water as it fluctuated through time. Trench M, the trench being cut down the side of McBurney's Middle Trench, has now reached the depth of the latest Middle Stone Age or Middle Palaeolithic (Levalloiso-Mousterian) industries. The preliminary indications from its excavation are that the transition from the Levalloiso-Mousterian to the blade-based Upper Palaeolithic or Late Stone Age Dabban industry was complex and perhaps protracted, at a time when the climate was oscillating between warm-stage stable environmental conditions and colder and more arid environments. The estimated age of the sediments, c. 50–40 ka, places these oscillations within the earlier part of MIS 3 (globally dated to 60–24 ka), when global climates experienced rapid fluctuations as part of an overall trend to increasing aridity and cold.

Changing Patterns in the Late Pleistocene/Early Holocene Prehistory of Southern Africa as Seen from the Nelson Bay Cave Stone Artifact Sequence

1978 ◽  
Vol 10 (1) ◽  
pp. 84-111 ◽  
Author(s):  
Janette Deacon
Keyword(s):  
Southern Africa ◽  
Sensu Stricto ◽  
Middle Stone Age ◽  
Stone Age ◽  
Faunal Remains ◽  
Later Stone Age ◽  
Large Numbers ◽  
Changing Patterns ◽  
Selection Of ◽  
Stone Artifact

The dating of the Stone Age sequence in southern Africa has been considerably revised over the last decade, and one of the anomalies which has resulted is that the Middle Stone Age, now dated to beyond 30,000 B.P., does not immediately precede the Later Stone Agesensu stricto. The excavation and analysis of occupation horizons dating between the most recent Middle Stone Age assemblages and the Holocene is therefore of particular interest. Nelson Bay Cave, situated on the southern coast of South Africa, contains deposits which partly fill the “gap” between the Middle and Later Stone Ages, and the occupation horizons dating between about 18,000 and 5000 years ago are described in this paper. Changes in the habitat in the vicinity of the site caused by sea-level and vegetation changes coincident with the amelioration of temperatures at the end of the Pleistocene are clearly marked in the faunal remains at the site. Largely correlated with the faunal changes (which includes the introduction of marine resources to the cave at about 12,000 B.P.) are changes in the stone artifact assemblages. Three industries are recognized in the sequence: the Robberg, characterized by microbladelets produced from bladelet cores and a few small scrapers and backed tools; the Albany, characterized by large scrapers and an absence of backed tools; and the Wilton, characterized by a variety of Formal Tools including relatively large numbers of small scrapers and backed tools. These changes in artifact-manufacturing traditions are interpreted as signaling adjustments to changing environmental conditions. An explanation for these adjustments is not sought in a simple cause-and-effect relationship between the environment and the cultural response; artifact changes are seen instead as the result of a twofold process, with the environment acting as an external stimulus to change, and the direction of the artifact change governed by the selection of a range of possibilities offered by the technology of the Later Stone Agesensu latothat was widespread in subequatorial Africa during the last 20,000 years.

scholarly journals Phytolith Palaeoenvironments at Mumba Rock Shelter

2021 ◽  
Vol 9 ◽  
Author(s):  
Julio Mercader ◽  
Siobhán Clarke ◽  
Makarius Itambu ◽  
Abdallah Mohamed ◽  
Musa Mwitondi ◽  
...  
Keyword(s):  
Statistical Analysis ◽  
East Africa ◽  
Late Pleistocene ◽  
Principal Components ◽  
Stone Age ◽  
Later Stone Age ◽  
Rock Shelter ◽  
Shelter Site ◽  
Northern Tanzania ◽  
Plant Habitat

The rock shelter site of Mumba in northern Tanzania plays a pivotal role in the overall study of the late Pleistocene archaeology of East Africa with an emphasis on the Middle to Later Stone Age transition. We used phytolith analysis to reconstruct general plant habitat physiognomy around the site from the onset of the late Pleistocene to recent times, tallying 4246 individual phytoliths from 19 archaeological samples. Statistical analysis explored phytolith richness, diversity, dominance, and evenness, along with principal components to compare phytolith distributions over the site’s sequence with known plant habitats today. Generally, the phytolith record of Mumba signifies paleoenvironments with analogs in the Somalia – Masai bushland and grassland, as well as Zambezian woodlands.

scholarly journals Human social organization during the Late Pleistocene: Beyond the nomadic-egalitarian model

2021 ◽  
Author(s):  
Manvir Singh ◽  
Luke Glowacki
Keyword(s):  
Resource Management ◽  
Social Organization ◽  
Late Pleistocene ◽  
Large Scale ◽  
Middle Stone Age ◽  
Small Scale ◽  
Stone Age ◽  
Human History ◽  
Hunter Gatherers ◽  
Social Variation

Many researchers assume that until 10-12,000 years ago, humans lived in small, mobile, relatively egalitarian bands composed mostly of kin. This “nomadic-egalitarian model” informs evolutionary explanations of behavior and our understanding of how contemporary societies differ from those of our evolutionary past. Here, we synthesize research challenging this model and propose an alternative, the diverse histories model, to replace it. We outline the limitations of using recent foragers as models of Late Pleistocene societies and the considerable social variation among foragers commonly considered small-scale, mobile, and egalitarian. We review ethnographic and archaeological findings covering 34 world regions showing that non-agricultural peoples often live in groups that are more sedentary, unequal, large, politically stratified, and capable of large-scale cooperation and resource management than is normally assumed. These characteristics are not restricted to extant Holocene hunter-gatherers but, as suggested by archaeological findings from 27 Middle Stone Age sites, likely characterized societies throughout the Late Pleistocene (until c. 130 ka), if not earlier. These findings have implications for how we understand human psychological adaptations and the broad trajectory of human history.

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