What drove late Holocene dust activity in central Asia, natural processes or human activity?

Author(s):  
Tao Zhang ◽  
Wenxia Han ◽  
Yongxiang Han ◽  
Shuang Lü ◽  
David Madsen ◽  
...  
1983 ◽  
Vol 48 (3) ◽  
pp. 553-572 ◽  
Author(s):  
Peter M. Bowers ◽  
Robson Bonnichsen ◽  
David M. Hoch

Time lapse studies of frost action effects on arctic and subarctic surficial archaeological sites have been conducted from 1973 to the present. Test plots of experimentally produced flakes were constructed in 1973 in the Tangle Lakes Region of the Central Alaska Range and subsequently remapped and photographed in 1974, 1976, and 1980. Similar test plots were laid out in the arctic foothills province of the Brooks Range. Observations made during the study period include: (1) flake displacements of as much as 20 cm/yr; (2) average minimum movement is 4 cm/yr; and (3) upslope movements were observed, suggesting that slope is not the primary factor in flake displacements. Frost heave, needle ice and, possibly, wind appear to be the dominant forces responsible for dispersals. It is argued that these and other natural processes can restructure the archaeological record into patterns that easily can be mistaken for those produced by human activity.


The Holocene ◽  
2021 ◽  
pp. 095968362110032
Author(s):  
Halinka Di Lorenzo ◽  
Pietro Aucelli ◽  
Giuseppe Corrado ◽  
Mario De Iorio ◽  
Marcello Schiattarella ◽  
...  

The Garigliano alluvial-coastal plain, at the Latium-Campania border (Italy), witnessed a long-lasting history of human-environment interactions, as demonstrated by the rich archaeological knowledge. With the aim of reconstructing the evolution of the landscape and its interaction with human activity during the last millennia, new pollen results from the coastal sector of the Garigliano Plain were compared with the available pollen data from other nearby sites. The use of pollen data from both the coastal and marine environment allowed integrating the local vegetation dynamics within a wider regional context spanning the last 8000 years. The new pollen data presented in this study derive from the analysis of a core, drilled in the coastal sector, which intercepted the lagoon-marshy environments that occurred in the plain as a response to the Holocene transgression and subsequent coastal progradation. Three radiocarbon ages indicate that the chronology of the analyzed core interval ranges from c. 7200 to c. 2000 cal yr BP. The whole data indicate that a dense forest cover characterized the landscape all along the Prehistoric period, when a few signs of human activity are recorded in the spectra, such as cereal crops, pasture activity and fires. The main environmental changes, forced by natural processes (coastal progradation) but probably enhanced by reclamation works, started from the Graeco-Roman period and led to the reduction of swampy areas that favoured the colonisation of the outer plain.


2018 ◽  
Vol 115 (21) ◽  
pp. E4735-E4736 ◽  
Author(s):  
Yannick Garcin ◽  
Pierre Deschamps ◽  
Guillemette Ménot ◽  
Geoffroy de Saulieu ◽  
Enno Schefuß ◽  
...  

2021 ◽  
Vol 273 ◽  
pp. 107235
Author(s):  
Lucas Dugerdil ◽  
Guillemette Ménot ◽  
Odile Peyron ◽  
Isabelle Jouffroy-Bapicot ◽  
Salomé Ansanay-Alex ◽  
...  

Erdkunde ◽  
2021 ◽  
Vol 75 (1) ◽  
pp. 15-30
Author(s):  
Witold Paweł Alexandrowicz

The presented study is dedicated to the assessment of the scope and degree of anthropopressure, and the dependence of its intensity on the characteristics and nature of micro-environments. The research was based on the subfossil remains of molluscs. Eleven profiles of Late Holocene sediments in the Dulówka valley near Cracow were subjected to malacological analysis. In the upper part of the valley, there are calcareous tufas containing rich molluscan assemblages with a large share of shade-loving species. In the lower part, malacofauna dominated by open-country snails occurs in fluvial sediments. Radiocarbon dating has shown that mollusc-bearing deposits represent the last 2,000 years. The diversity of ecological features of molluscan assemblages in different parts of the valley depends on the intensity of anthropopressure. In the upper part, natural forest communities have survived to the present day, and anthropopressure has only been marked to a limited extent. The lower section has undergone a major transformation, mainly due to deforestation and the development of agricultural areas. Unfavorable terrain conditions for the human economy should be considered the major cause of the low anthropopressure intensity in the upper part of the valley. The malacological analysis used in the study allowed showing a significant diversity of microhabitats within the valley and its uneven susceptibility to human interference in natural processes.


2019 ◽  
Vol 519 ◽  
pp. 144-155 ◽  
Author(s):  
Sayuri Naito ◽  
Nagayoshi Katsuta ◽  
Shin-ichi Kawakami ◽  
Yoshimitsu Koido ◽  
Hiroshi Shimono

2015 ◽  
Vol 26 (2) ◽  
pp. 375-389 ◽  
Author(s):  
Emily McClung de Tapia

AbstractPaleoenvironmental and geoarchaeological data generated over the past three decades for parts of the Basin of Mexico are little known among archaeologists working in the region. This paper summarizes and evaluates what is currently known about the prehistoric environment, landscape development, and human impact in the region. Archaeological evidence indicates that human activity became important in ecosystem evolution in the basin during the Middle-Late Holocene. Most traditional paleoenvironmental studies based on lake sediments, however, generalize results corresponding to this period simply asevidence for human impact. Essentially the same vegetation communities extant in the basin today appear to have been present during most of the Holocene, albeit with broader distributions and variability in secondary taxa. Recognizing potential contributions of archaeology to understanding human adaptation to climatic and ecosystemic change, past and present, should stimulate future research on paleoenvironment in the region.


2006 ◽  
Vol 25 (S1) ◽  
pp. 6-6
Author(s):  
Andrey V. Daryin ◽  
Ivan A. Kalugin ◽  
Lubov G. Smolyaninova ◽  
Konstantin V. Zolotarev ◽  
Elena G. Vologina ◽  
...  

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