Human occupation, slash-burning and vegetation response from the final Pleistocene to the middle Holocene, Daling River basin, NE China

2020 ◽  
Vol 275 ◽  
pp. 104158
Author(s):  
Qingjiang Yang ◽  
Xinying Zhou ◽  
Chao Zhao ◽  
Qiang Gao ◽  
Junchi Liu ◽  
...  
2015 ◽  
Vol 363 ◽  
pp. 43-54 ◽  
Author(s):  
Ruth Dickau ◽  
Francisco Javier Aceituno ◽  
Nicolás Loaiza ◽  
Carlos López ◽  
Martha Cano ◽  
...  

Author(s):  
А. V. Tetenkin ◽  
◽  
V. М. Vetrov ◽  
Е. I. Demonterova ◽  
G. V. Pashkova ◽  
...  

Antiquity ◽  
2008 ◽  
Vol 82 (317) ◽  
pp. 560-570 ◽  
Author(s):  
César A. Méndez M. ◽  
Omar R. Reyes B.

How early did steppe dwellers penetrate the forests? The authors compare and contrast settlement on the steppe, in the forest and on the steep sea coast of western Patagonia, finding that the steppe is occupied first, from 11400 calendar years BP. But around 2800 calendar years BP settlements enter the forest almost simultaneously for a brief period along the length of the Cisnes river valley. Within a few centuries the experiment appears to be abandoned, and the focus of prehistoric peoples returns to the steppe.


Radiocarbon ◽  
2005 ◽  
Vol 47 (3) ◽  
pp. 383-394 ◽  
Author(s):  
Roberta Hall ◽  
Loren G Davis ◽  
Samuel Willis ◽  
Matthew Fillmore

Radiocarbon dates together with geoarchaeological, soil, and lithic analyses are presented to describe archaeological site 35-CS-9 in Bandon Ocean Wayside State Park, Oregon, northwestern USA. One of the few Oregon middle-Holocene coastal sites that includes sediments and artifacts dating to the early Holocene and possibly to the late Pleistocene, it was recorded in 1951 and surface surveyed by archaeologists in 1975, 1986, and 1991, but its depth and antiquity were not tested. In February 2002, we studied the site's stratigraphy and sediments and described 8 strata from the aeolian surface to bedrock at 350 cm depth. Soil samples taken from a cut bank for texture classification, particle size analysis, pH, carbon content, and chemical analysis suggested that the site represented a complete history of Holocene deposits. Excavation of 2 test units in August 2002 uncovered substantial lithic and charcoal remains that confirm a protracted middle-Holocene occupation and suggest that human occupation began in the early Holocene. Charcoal recovered at 235–245 cm dated to 11,000 14C BP, and the deepest lithic artifact was recovered in a level at 215–225 cm. Whether the human occupation was continuous throughout the Holocene, and whether it began in the early Holocene or in the late Pleistocene, can only be determined with further excavations.


AMERTA ◽  
2020 ◽  
Vol 37 (2) ◽  
pp. 71-92
Author(s):  
Citra Iqliyah Darojah ◽  
Anggraeni Anggraeni

Abstract, Researches at Karama River Basin sites have been conducted for years which gave indication of intensive human occupation during Prehistoric period. Hence, it is necessary to reveal and to understand the reason behind this human occupation based on the correlation between morphology, site characteristics, and site distributions. Scientific method was applied to obtain data from the field and to conduct spatial analysis. Disturbance caused by erosion and morphologic changes led to archaeological data transformation and also affected physical environment of archaeological sites. However, that kind of disturbance did not reduce the the importance of physical environment as spatial analysis data. Spatial analysis of sites along the main stem of Karama River both in downstream region and upstream region indicates occupation landscape characteristics. These characteristics can be seen from the location of the occupation which was close to waterway alluvial morphology (hilltop, hill terrace, and river terrace), at relatively flat surface area, and along the riverside or river confluence. There are two highlighted factors from landscape characteristics to support human occupation: accessibility and protection. Accessibility means there is no difficulties to access natural resources and there is possible access to secure interaction between communities. Protection means the location is relatively safe or less affected by both natural and human hazards. Those factors were probably the main reasons to choose Karama River Basin for human settlement.Abstrak, Penelitian situs di kawasan Daerah Aliran Sungai (DAS) Karama, Sulawesi Barat, telah dilakukan selama bertahun-tahun dan menghasilkan indikasi aktivitas hunian yang intensif pada masa Prasejarah. Dengan demikian, perlu diupayakan mencari alasan di balik penghunian manusia di DAS Karama berdasarkan korelasi antara morfologi, karakteristik situs, dan distribusi situs. Metode saintifik diterapkan untuk mendapatkan data dari lapangan dan melakukan analisis spasial. Perubahan morfologi lokasi situs dan erosi di kawasan DAS Karama menyebabkan transformasi data arkeologi serta memengaruhi lingkungan fisik lokasi situs. Meskipun demikian, pengaruh tersebut tidak lantas mengurangi pentingnya komponen fisik lokasi situs sebagai data analisis spasial. Analisis korelasi data dari situs, baik di sepanjang aliran utama Sungai Karama di kawasan muara maupun di kawasan pedalaman, mengindikasikan karakteristik lanskap hunian. Karakteristik tersebut menunjukkan lokasi hunian berada pada morfologi aluvial sungai (puncak bukit, teras bukit, dan teras sungai), berada pada topografi lahan yang relatif datar dan berlokasi di tepi aliran utama sungai atau di tepi pertemuan sungai (confluence). Ada dua faktor utama yang mendukung kawasan DAS Karama sebagai lokasi hunian, yakni aksesibilitas dan keamanan. Faktor aksesibilitas meliputi kemudahan akses terhadap sumber daya alam dan akses yang memungkinkan terjadinya interaksi antarkomunitas. Faktor keamanan menunjukkan bahwa lokasi situs relatif terlindungi dari ancaman bencana alam dan manusia. Kedua faktor tersebut kemungkinan besar menjadi alasan utama manusia memilih kawasan DAS Karama sebagai lokasi hunian.


2019 ◽  
Vol 33 (3) ◽  
pp. 14
Author(s):  
Alessandra Mendes Carvalho Vasconcelos ◽  
Alexandre Christófaro Silva ◽  
Marcelo Fagundes ◽  
Matheus Kuchenbecker ◽  
Valdinêy Amaral Leite

Este artigo tem como objetivo apresentar uma síntese das intervenções realizadas no Complexo Arqueológico Três Fronteiras, uma área que até o momento apresentou um total de 16 abrigos sob rocha quartzítica, todos com marcas evidentes de ocupação humana. A área está localizada na Serra do Espinhaço Meridional, mais precisamente em sua face leste (Serra Negra), nordeste de Minas Gerais, na bacia do Araçuaí, municípios de Felício dos Santos e de Senador Modestino Gonçalves. O abrigo no 7 foi escavado por uma equipe multidisciplinar com a intenção de obter datas e repertório cultural para posteriores análises e discussões com os resultados de outros sítios regionais escavados. Logo, o sítio Três Fronteiras no 7 obteve data de 4100 ± 30 anos AP. situando sua ocupação durante o Holoceno Médio, resultado comum para outros abrigos locais. TRÊS FRONTEIRAS ARCHAEOLOGICAL SITE No 7: A Shelter of The Mid-Holocene in the Araçuaí River Basin, Minas GeraisABSTRACTThe objective of this article is to summarize the interventions so far carried out within the Três Fronteiras Archaeological Complex, composed by 16 quartzite rock shelters with outstanding evidences of human occupation. The area is located in the eastern border of the southern Espinhaço range (Serra Negra), in which is drained by the Araçuaí river basin, in the municipalities of Felício dos Santos and Senador Modestino Gonçalves, Minas Gerais. The shelter no 7 was excavated by a multidisciplinary team with the intention of obtaining ages and material culture for further analysis and comparison with other archaeological sites. The oldest evidence of occupation within the site was dated in 4100 ± 30 yr BP. (Mid Holocene), which is coherent with the chronologies found in other sites.keywords: Espinhaço Meridional Range; Mid-Holocene; Três Fronteiras; Landscapes; Paleoenvironment.


2015 ◽  
Vol 32 (3) ◽  
pp. 465-503 ◽  
Author(s):  
Pierre M. Vermeersch ◽  
Veerle Linseele ◽  
Elena Marinova ◽  
Wim Van Neer ◽  
Jan Moeyersons ◽  
...  

Radiocarbon ◽  
2018 ◽  
Vol 60 (2) ◽  
pp. 367-382 ◽  
Author(s):  
Loukas Barton ◽  
Scott Shirar ◽  
James W Jordan

ABSTRACTThe Alaska Peninsula is a landscape defined by volcanic, tectonic, and glacial processes, and life throughout is conditioned on the interactions among them. During the middle Holocene (ca. 4100–3600 yr ago), intense caldera-forming eruptions of the Aniakchak and Veniaminof volcanoes changed the shape of the central portion of the Peninsula dramatically, and had significant and perhaps devastating impacts on both terrestrial and marine biota. Here we evaluate the severity of these impacts by tracking human settlement patterns using 75 unique radiocarbon (14C) age determinations on buried cultural features from the central Alaska Peninsula. Coastal regions were re-colonized within a few hundred years while river systems most proximate to the volcanoes were uninhabited for up to 1500 years following the most severe eruptions. Patterns of human settlement may also document previously unrecorded landscape change throughout the region, and further contribute to our understanding of post-volcanic ecological succession.


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