Changes and Continuities of Hunting Practices from the Late Pleistocene to the Late Holocene Among Nomadic Societies of the Patagonian Plateaus

2021 ◽  
pp. 259-291
Author(s):  
Laura Miotti ◽  
Laura Marchionni ◽  
Darío Hermo ◽  
Enrique Terranova ◽  
Lucía Magnin ◽  
...  
Keyword(s):  
Late Pleistocene ◽  
Late Holocene

Microlithic occurrences associated with sediments dated to terminal Pleistocene-late Holocene in the central Narmada basin, Madhya Pradesh, India

2021 ◽  
pp. SP515-2020-216
Author(s):  
Nupur Tiwari ◽  
P. Morthekai ◽  
K. Krishnan ◽  
Parth R. Chauhan
Keyword(s):  
Sri Lanka ◽  
South Asia ◽  
Late Pleistocene ◽  
Iron Age ◽  
Late Holocene ◽  
Indian Subcontinent ◽  
Central India ◽  
Madhya Pradesh ◽  
Doctoral Research ◽  
Terminal Pleistocene

AbstractThe earliest occurrence of microliths in South Asia dates back to the Late Pleistocene at Mehtakheri (45 ka) and Dhaba (48 ka) in Central India, Jwalapuram 9 in Southern India (38 ka), Kana and Mahadebbara in Northeastern India (42-25 ka) and Batadomba-Lena (35-36 ka) and Fa Hien Lena (48 ka) in Sri Lanka. Microlithic technology is distributed across the entire Indian Subcontinent and chronologically continues up to the Iron Age and Early Historic periods. This paper discusses new data acquired from the first author's doctoral research in the two districts of Madhya Pradesh (Hoshangabad and Sehore), which fall within the central part of the Narmada Basin in central India. We present here the preliminary dates from key areas of distribution to understand the geo-chronological contexts of microliths at Pilikarar, Morpani, and Gurla-Sukkarwada. Initial dates from these respective occurrences range between 12.5 ka and 2.3 ka.

A Good Place to Live: Plants and People at the Santa Elina Rock Shelter (Central Brazil) from Late Pleistocene to the Holocene

2020 ◽  
Vol 31 (2) ◽  
pp. 273-291
Author(s):  
Rita Scheel-Ybert ◽  
Caroline Bachelet
Keyword(s):  
Late Pleistocene ◽  
Late Holocene ◽  
Vegetation Changes ◽  
Vegetation Types ◽  
Rock Shelter ◽  
Good Place ◽  
Central Brazil ◽  
Cultural Preference ◽  
Vegetation And Climate ◽  
Over Time

The Santa Elina rock shelter (Central Brazil) was recurrently occupied from the Late Pleistocene to the Late Holocene. We compare sets of previously published anthracological analyses with new data to reconstruct the landscape, vegetation, and climate over the several thousand years of occupation, providing information on firewood management from about 27,000 to about 1500 cal BP. Laboratory analyses followed standard anthracological procedures. We identified 34 botanical families and 84 genera in a sample of almost 5,000 charcoal pieces. The Leguminosae family dominates the assemblage, followed by Anacardiaceae, Bignoniaceae, Rubiaceae, Euphorbiaceae, and Sapotaceae. The area surrounding the shelter was forested throughout the studied period. The local landscape was formed, as it is today, by a mosaic of vegetation types that include forest formations and open cerrado. Some regional vegetation changes may have occurred over time. Our data corroborate the practice of opportunistic firewood gathering in all periods of site occupation, despite a possible cultural preference for some taxa. The very long occupation of Santa Elina may be due not only to its attractiveness as a rock shelter but also to the continuously forested vegetation around it. It was a good place to live.

Late Pleistocene and Late Holocene Lake Highstands in the Pyramid Lake Subbasin of Lake Lahontan, Nevada, USA

2005 ◽  
Vol 64 (2) ◽  
pp. 257-263 ◽  
Author(s):  
Richard W. Briggs ◽  
Steven G. Wesnousky ◽  
Kenneth D. Adams
Keyword(s):  
Sierra Nevada ◽  
Late Pleistocene ◽  
Late Holocene ◽  
Large Lakes ◽  
Western Basin ◽  
Radiocarbon Dates ◽  
Beach Ridges ◽  
Climate Proxy ◽  
Pyramid Lake ◽  
Proxy Records

AbstractShoreline geomorphology, shoreline stratigraphy, and radiocarbon dates of organic material incorporated in constructional beach ridges record large lakes during the late Pleistocene and late Holocene in the Pyramid Lake subbasin of Lake Lahontan, Nevada, USA. During the late Holocene, a transgression began at or after 3595 ± 35 14C yr B.P. and continued, perhaps in pulses, through 2635 ± 40 14C yr B.P., resulting in a lake as high as 1199 m. During the latest Pleistocene and overlapping with the earliest part of the Younger Dryas interval, a lake stood at approximately 1212 m at 10,820 ± 35 14C yr B.P. and a geomorphically and stratigraphically distinct suite of constructional shorelines associated with this lake can be traced to 1230 m. These two lake highstands correspond to periods of elevated regional wetness in the western Basin and Range that are not clearly represented in existing northern Sierra Nevada climate proxy records.

Age and paleoclimatic significance of late Holocene lakes in the Carson Sink, NV, USA

2003 ◽  
Vol 60 (3) ◽  
pp. 294-306 ◽  
Author(s):  
Kenneth D. Adams
Keyword(s):  
United States ◽  
Tree Ring ◽  
Great Basin ◽  
Late Pleistocene ◽  
Lake Level ◽  
Late Holocene ◽  
Western United States ◽  
Long Period ◽  
Paleoclimatic Significance ◽  
Original Interpretation

AbstractNew dating in the Carson Sink at the termini of the Humboldt and Carson rivers in the Great Basin of the western United States indicates that lakes reached elevations of 1204 and 1198 m between 915 and 652 and between 1519 and 1308 cal yr B.P., respectively. These dates confirm Morrison's original interpretation (Lake Lahontan: Geology of the Southern Carson Desert, Professional Paper 40, U.S. Geol. Survey, 1964) that these shorelines are late Holocene features, rather than late Pleistocene as interpreted by later researchers. Paleohydrologic modeling suggests that discharge into the Carson Sink must have been increased by a factor of about four, and maintained for decades, to account for the 1204-m lake stand. The hydrologic effects of diversions of the Walker River to the Carson Sink were probably not sufficient, by themselves, to account for the late Holocene lake-level rises. The decadal-long period of increased runoff represented by the 1204-m lake is also reflected in other lake records and in tree ring records from the western United States.

scholarly journals Vertebrate community on an ice-age Caribbean island

2015 ◽  
Vol 112 (44) ◽  
pp. E5963-E5971 ◽  
Author(s):  
David W. Steadman ◽  
Nancy A. Albury ◽  
Brian Kakuk ◽  
Jim I. Mead ◽  
J. Angel Soto-Centeno ◽  
...  
Keyword(s):  
Sea Level ◽  
Late Pleistocene ◽  
Late Holocene ◽  
Ice Age ◽  
Caribbean Island ◽  
The Bahamas ◽  
Broadleaf Forest ◽  
The Past ◽  
Scuba Divers ◽  
Moist Habitat

We report 95 vertebrate taxa (13 fishes, 11 reptiles, 63 birds, 8 mammals) from late Pleistocene bone deposits in Sawmill Sink, Abaco, The Bahamas. The >5,000 fossils were recovered by scuba divers on ledges at depths of 27–35 m below sea level. Of the 95 species, 39 (41%) no longer occur on Abaco (4 reptiles, 31 birds, 4 mammals). We estimate that 17 of the 39 losses (all of them birds) are linked to changes during the Pleistocene–Holocene Transition (PHT) (∼15–9 ka) in climate (becoming more warm and moist), habitat (expansion of broadleaf forest at the expense of pine woodland), sea level (rising from −80 m to nearly modern levels), and island area (receding from ∼17,000 km2 to 1,214 km2). The remaining 22 losses likely are related to the presence of humans on Abaco for the past 1,000 y. Thus, the late Holocene arrival of people probably depleted more populations than the dramatic physical and biological changes associated with the PHT.

scholarly journals Industri Alat Mikrolit di Situs Balang Metti: Teknologi Toala Akhir dan Kontak Budaya di Dataran Tinggi Sulawesi Selatan

AMERTA ◽  
2017 ◽  
Vol 35 (2) ◽  
pp. 93
Author(s):  
Suryatman Suryatman ◽  
Budianto Hakim ◽  
Afdalah Harris
Keyword(s):  
Early Modern ◽  
Research Methods ◽  
Late Pleistocene ◽  
Late Holocene ◽  
Raw Material ◽  
Cultural Contact ◽  
South Sulawesi ◽  
Material Sources ◽  
Early Modern Humans ◽  
Out Of Africa

Abstract. The Microlith Tool Industry at Balang Metti Site: Late Toalean Technology and Cultural Contact in the Highlands of South Sulawesi.The presence and distribution of microlith tools in Africa, Europe, and Asia have often been debated by prehistorians. The technology was brought by Early Modern Humans out of Africa to some areas of Europe and Asia during the Late Pleistocene. In South Sulawesi, it exists from the Middle to Late Holocene and is classed as part of the ‘Toalean’ culture. Excavations at Balang Metti site revealed a layer of microlith tools representing an industry that occurred for no more than 3,500 years ago. This is remarkable as the site is located in the highlands, whereas all previously known Toalean occupation sites are dispersed throughout the lowlands of South Sulawesi. The purpose of our research is to explain this microlith technology, especially the implication of its cultural contact, which occurred up to the highlands. Research methods done by classified, counted, and measured all lithic artefacts from excavation. The results show that the early stages of flaking (reduction) occurred not only in the cave but also out of the site, possibly close to the raw material sources. Abstrak.Kehadiran dan persebaran alat mikrolit di Afrika, Eropa, dan Asia telah diperdebatkan oleh kalangan peneliti prasejarah. Peralatan tersebut dibawa oleh manusia modern awal keluar dari Afrika ke beberapa wilayah Eropa dan Asia pada akhir Pleistosen. Di Sulawesi Selatan peralatan ini baru muncul pada pertengahan hingga akhir Holosen dan digolongkan sebagai bagian dari budaya Toalean. Penggalian di Situs Balang Metti menunjukkan lapisan budaya industri alat mikrolit berumur tidak lebih dari 3.500 tahun. Permasalahannya adalah situs tersebut berada di wilayah dataran tinggi, yang sebelumnya situs-situs hunian Toalean hanya ditemukan tersebar di wilayah dataran rendah Sulawesi Selatan. Penelitian ini bertujuan untuk menjelaskan teknologi alat mikrolit dan implikasi kontak budaya yang terjadi hingga di dataran tinggi Sulawesi Selatan. Metode penelitian dilakukan dengan mengklasifikasi, menghitung, dan mengukur semua artefak batu dari penggalian. Hasil penelitian menunjukkan bahwa proses penyerpihan tidak hanya dilakukan di dalam gua, tetapi juga di luar gua yang mungkin tidak jauh dari lokasi pengambilan bahan.

scholarly journals Teknologi Litik di Situs Talimbue, Sulawesi Tenggara: Teknologi Berlanjut dari Masa Pleistosen Akhir Hingga Holosen.

AMERTA ◽  
2016 ◽  
Vol 34 (2) ◽  
pp. 81
Author(s):  
Suryatman Suryatman ◽  
Sue O’ Connor ◽  
David Bulbeck ◽  
Ben Marwick ◽  
Adhi Agus Oktaviana ◽  
...  
Keyword(s):  
Late Pleistocene ◽  
Quantitative Estimate ◽  
Late Holocene ◽  
Lithic Technology ◽  
Terminal Pleistocene ◽  
New Perspective

Abstract.  The  Lithic  Technology  at  Talimbue  Site,  Southeast  Sulawesi:  Continuing  Technology from Late Pleistocene up to Holocene Periods. The Talimbue site at Southeast Sulawesi is packed with  lithic  and  these  offer  a  new  perspective  on  the  lithic  technology  of  Sulawesi.  The  absence  of information  on  the  prehistoric  lithic  technology  of  Southeast  Sulawesi  is  a  factor  of  interest  that makes  research  on  knowledge  of  the  Talimbue  site  necessary.  Lithic  artefacts  were  manufactured from  the  terminal  Pleistocene  to  the  Late  Holocene.  This  research  will  disentangle  the  details  of the lithic technology at the Talimbue Site. The analyzed flaked stone artefacts fall into 3 categories, which are retouched flakes, debitage and cores. For its part, debitage was classified into 3 categories, which are complete flakes, broken flakes and debris. The retouch index was also measured so as to provide a quantitative estimate of the level of retouch intensity of the retouched flakes. The results of  the  analysis  indicate  changes  in  the  stone  flake  technology  during  the  period  of  occupation  of the Talimbue Site. The change of technology occurs because the process of adaptation caused by a change of environment. Abstrak. Temuan  litik  yang  sangat  padat  di  Situs  Talimbue  di  Sulawesi  Tenggara  menunjukkan sebuah persepektif baru dalam kajian teknologi litik di Sulawesi. Kekosongan informasi teknologi litik masa prasejarah di wilayah Sulawesi Tenggara adalah hal yang menarik dikaji dalam penelitian di Situs Talimbue. Artefak litik digunakan dari masa Pleistosen Akhir hingga masa Holosen Akhir. Penelitian ini akan menguraikan secara detail bagaimana teknologi litik di Situs Talimbue. Artefak batu diserpih yang dianalisis menjadi 3 kategori, yaitu serpih diretus, serpihan dan batu inti. Serpihan kemudian  diklasifikasi  menjadi  3  kategori,  yaitu  serpih  utuh,  serpih  rusak  dan  tatal.  Pengukuran indeks retus juga dilakukan bertujuan untuk mengestimasi secara kuantitatif tingkat intensitas retus terhadap serpih yang telah diretus. Hasil penelitian menunjukkan perubahan teknologi artefak batu diserpih terjadi selama masa hunian di Situs Talimbue. Perubahan teknologi terjadi karena adanya proses adaptasi yang disebabkan oleh perubahan lingkungan.

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