scholarly journals Last Interglacial Iberian Neandertals as fisher-hunter-gatherers

Science ◽  
2020 ◽  
Vol 367 (6485) ◽  
pp. eaaz7943 ◽  
Author(s):  
J. Zilhão ◽  
D. E. Angelucci ◽  
M. Araújo Igreja ◽  
L. J. Arnold ◽  
E. Badal ◽  
...  
Keyword(s):  
Marine Invertebrates ◽  
Middle Stone Age ◽  
Stone Age ◽  
Resource Exploitation ◽  
Last Interglacial ◽  
Hunter Gatherers ◽  
Marine Birds ◽  
Old World ◽  
Coastal Resource ◽  
Marine Food

Marine food–reliant subsistence systems such as those in the African Middle Stone Age (MSA) were not thought to exist in Europe until the much later Mesolithic. Whether this apparent lag reflects taphonomic biases or behavioral distinctions between archaic and modern humans remains much debated. Figueira Brava cave, in the Arrábida range (Portugal), provides an exceptionally well preserved record of Neandertal coastal resource exploitation on a comparable scale to the MSA and dated to ~86 to 106 thousand years ago. The breadth of the subsistence base—pine nuts, marine invertebrates, fish, marine birds and mammals, tortoises, waterfowl, and hoofed game—exceeds that of regional early Holocene sites. Fisher-hunter-gatherer economies are not the preserve of anatomically modern people; by the Last Interglacial, they were in place across the Old World in the appropriate settings.

The Cyrenaican Prehistory Project 2009: the third season of investigations of the Haua Fteah cave and its landscape, and further results from the 2007–2008 fieldwork

2009 ◽  
Vol 40 ◽  
pp. 55-94 ◽  
Author(s):  
Graeme Barker ◽  
Annita Antoniadou ◽  
Huw Barton ◽  
Ian Brooks ◽  
Ian Candy ◽  
...  
Keyword(s):  
Middle Stone Age ◽  
Stone Age ◽  
Glacial Cycle ◽  
Last Interglacial ◽  
Stratigraphic Sequence ◽  
Hunter Gatherers ◽  
The Third ◽  
Late Stone Age ◽  
Southern Side ◽  
Deep Sounding

AbstractThe paper reports on the third (2009) season of fieldwork of the Cyrenaican Prehistory Project, and on further results from the analysis of materials collected in the previous (2007 and 2008) fieldwork. Sediments in a 14 m-deep core drilled beside the McBurney trench provide an invaluable overview of the overall stratigraphic sequence, including at depths reached by the 1950s Deep Sounding but not yet investigated by the present project. Sampling of newly-exposed faces of the original excavation trench for dating (14C, ESR, OSL, U-series) and palaeoenvirommental indicators continued. Excavation was begun of sediments assigned to the early Holocene Libyco-Capsian (McBurney's Layer X), and of Pre-Aurignacian layers beside the top of the Deep Sounding. The Libyco-Capsian layers are particularly prolific in lithic debris, shells, and animal bones; preliminary analysis of the lithics suggests a development from Typical to Upper Capsian within the layers excavated in 2009. Geoarchaeological survey along the littoral to the west and east of the Haua Fteah identified complex sequences spanning most of the last interglacial-glacial cycle. Geoarchaeological survey south of the Haua Fteah characterized the major landforms of the Gebel Akhdar mountain and of the pre-desert and desert-edge zones further south, with Late Stone Age (Upper Palaeolithic and Epipalaeolithic) material being found especially on the southern side of the Gebel Akhdar, and Middle Stone Age (Middle Palaeolithic) material in the pre-desert and desert regions. The first suite of 14C dates (from charcoal samples taken in 2007) indicates the use of the Haua Fteah by Oranian hunter-gatherers during the Last Glacial Maximum and in the succeeding millennia, but not in the Younger Dryas cold/dry phase (c. 11,000–10,000 cal. BC), with Libyco-Capsian occupation resuming soon after the beginning of the Holocene c. 9000 cal. BC, suggesting that the cave, and perhaps the Gebel Akhdar in general, have a complex history as refugia for human settlement during the Pleistocene.

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.

On the issues related to the discoid cores

2017 ◽  
Vol 17 (1) ◽  
pp. 174-178
Author(s):  
Youcheng Chen ◽  
Tongli Qu
Keyword(s):  
Middle Stone Age ◽  
Middle Pleistocene ◽  
Middle Paleolithic ◽  
Stone Age ◽  
The West ◽  
Upper Pleistocene ◽  
Old World ◽  
Insight Into

AbstractThe discoid core and the Levallois core are important symbols of the Middle Paleolithic Age in the west of the Old World. The two types of artifacts show not only technical relationships but also differences. The discoid core can be classified into two sub-types, namely the unifacial and the bifacial classes. In China, discoid cores may have appeared in the upper Middle Pleistocene, and prevailed in the lower and middle Upper Pleistocene, which corresponded to the middle Paleolithic Age in Europe and to the Middle Stone Age in Africa. The discovery and study of discoid cores provide significant insight into the culture of the Middle Paleolithic Age in China.

Paleolithic Hunter-Gatherers of Nubia

2021 ◽  
pp. 79-100
Author(s):  
Mirosław Masojć
Keyword(s):  
Middle Stone Age ◽  
Upper Paleolithic ◽  
Early Pleistocene ◽  
Middle Pleistocene ◽  
Nile Valley ◽  
Stone Age ◽  
Human Settlement ◽  
Hunter Gatherers ◽  
Lower Paleolithic ◽  
Upper Egypt

The chapter is devoted to the earliest human settlement in Nubia, which took place in the Pleistocene, with numerous references to neighboring areas, especially Upper Egypt. Paleolithic groups of humans probably appeared in Nubia in the Early Pleistocene, but well-documented sites—connected with Lower Paleolithic-Acheulean complex industries—are dated only to Middle Pleistocene (MIS 9-7). Some of the oldest Middle Stone Age (MSA) assemblages in Africa were discovered in Nubia (ca. 220 ka, MIS 7). Numerous MSA sites (ca. 220–40 ka, MIS 7-3) with predominating Levallois technology are situated within the Nile valley and the neighboring deserts, mainly in oases. The onset of Upper Paleolithic (ca. 40–20 ka, MIS 3-2) blade technology was recorded together with the oldest mining. Late Paleolithic groups of humans (20–11 ka, MIS 2), characterized by considerable diversity in the hyper-arid period, lived only in the Nile valley. Local examples of rock paintings come from that period. Pleistocene human remains from Nubia are extremely rare; they all represent H. sapiens. Cemeteries with numerous burials, some of which display evidence of violence, were also discovered in this area.

Between the Mediterranean and the Sahara: geoarchaeological reconnaissance in the Jebel Gharbi, Libya

Antiquity ◽  
2006 ◽  
Vol 80 (309) ◽  
pp. 567-582 ◽  
Author(s):  
Barbara E. Barich ◽  
Elena A.A. Garcea ◽  
Carlo Giraudi
Keyword(s):  
Middle Stone Age ◽  
Early Holocene ◽  
Stone Age ◽  
Later Stone Age ◽  
Hunter Gatherers ◽  
Human Presence ◽  
North West ◽  
The Mediterranean ◽  
Jebel Gharbi

Intensive survey and three sample sections at Jebel Gharbi in north-west Libya offer a new dated sequence of the environment, and the human presence within it, from the Middle Stone Age to the early Holocene. Hunter-gatherers were continuously active, including during the hitherto elusive Later Stone Age.

scholarly journals Ancient genomes from southern Africa pushes modern human divergence beyond 260,000 years ago

2017 ◽  
Author(s):  
Carina M. Schlebusch ◽  
Helena Malmström ◽  
Torsten Günther ◽  
Per Sjödin ◽  
Alexandra Coutinho ◽  
...  
Keyword(s):  
Genome Sequence ◽  
Southern Africa ◽  
Hot Spot ◽  
Middle Stone Age ◽  
Sub Saharan Africa ◽  
Genetic Admixture ◽  
Population Divergence ◽  
Stone Age ◽  
Modern Humans ◽  
Hunter Gatherers

ABSTRACTSouthern Africa is consistently placed as one of the potential regions for the evolution of Homo sapiens. To examine the region’s human prehistory prior to the arrival of migrants from East and West Africa or Eurasia in the last 1,700 years, we generated and analyzed genome sequence data from seven ancient individuals from KwaZulu-Natal, South Africa. Three Stone Age hunter-gatherers date to ~2,000 years ago, and we show that they were related to current-day southern San groups such as the Karretjie People. Four Iron Age farmers (300–500 years old) have genetic signatures similar to present day Bantu-speakers. The genome sequence (13x coverage) of a juvenile boy from Ballito Bay, who lived ~2,000 years ago, demonstrates that southern African Stone Age hunter-gatherers were not impacted by recent admixture; however, we estimate that all modern-day Khoekhoe and San groups have been influenced by 9–22% genetic admixture from East African/Eurasian pastoralist groups arriving >1,000 years ago, including the Ju|‘hoansi San, previously thought to have very low levels of admixture. Using traditional and new approaches, we estimate the population divergence time between the Ballito Bay boy and other groups to beyond 260,000 years ago. These estimates dramatically increases the deepest divergence amongst modern humans, coincide with the onset of the Middle Stone Age in sub-Saharan Africa, and coincide with anatomical developments of archaic humans into modern humans as represented in the local fossil record. Cumulatively, cross-disciplinary records increasingly point to southern Africa as a potential (not necessarily exclusive) ‘hot spot’ for the evolution of our species.

scholarly journals Early, intensive marine resource exploitation by Middle Stone Age humans at Ysterfontein 1 rockshelter, South Africa

2021 ◽  
Vol 118 (16) ◽  
pp. e2020042118
Author(s):  
Elizabeth M. Niespolo ◽  
Warren D. Sharp ◽  
Graham Avery ◽  
Todd E. Dawson
Keyword(s):  
South Africa ◽  
Local Environment ◽  
Modern Human ◽  
Middle Stone Age ◽  
Human Populations ◽  
Western Cape ◽  
Stone Age ◽  
Resource Exploitation ◽  
Shell Midden ◽  
Coastal Adaptation

Modern human behavioral innovations from the Middle Stone Age (MSA) include the earliest indicators of full coastal adaptation evidenced by shell middens, yet many MSA middens remain poorly dated. We apply 230Th/U burial dating to ostrich eggshells (OES) from Ysterfontein 1 (YFT1, Western Cape, South Africa), a stratified MSA shell midden. 230Th/U burial ages of YFT1 OES are relatively precise (median ± 2.7%), consistent with other age constraints, and preserve stratigraphic principles. Bayesian age–depth modeling indicates YFT1 was deposited between 119.9 to 113.1 thousand years ago (ka) (95% CI of model ages), and the entire 3.8 m thick midden may have accumulated within ∼2,300 y. Stable carbon, nitrogen, and oxygen isotopes of OES indicate that during occupation the local environment was dominated by C3 vegetation and was initially significantly wetter than at present but became drier and cooler with time. Integrating archaeological evidence with OES 230Th/U ages and stable isotopes shows the following: 1) YFT1 is the oldest shell midden known, providing minimum constraints on full coastal adaptation by ∼120 ka; 2) despite rapid sea-level drop and other climatic changes during occupation, relative shellfish proportions and sizes remain similar, suggesting adaptive foraging along a changing coastline; 3) the YFT1 lithic technocomplex is similar to other west coast assemblages but distinct from potentially synchronous industries along the southern African coast, suggesting human populations were fragmented between seasonal rainfall zones; and 4) accumulation rates (up to 1.8 m/ka) are much higher than previously observed for dated, stratified MSA middens, implying more intense site occupation akin to Later Stone Age middens.

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