Managing the human impact on the natural environment: patterns and processes

1993 ◽  
Vol 13 (3) ◽  
pp. 285
Author(s):  
Martin Cahn
2004 ◽  
Vol 39 (3) ◽  
pp. 148-156 ◽  
Author(s):  
S.J. Gale ◽  
R.J. Haworth ◽  
D.E. Cook ◽  
N.J. Williams

2011 ◽  
Vol 19 (4) ◽  
pp. 337-355
Author(s):  
Annik Dubied Losa ◽  
Claudine Burton-Jeangros

AbstractNowadays, relationships between nonhuman animals and humans are debated, often in relation to issues associated with the risks they represent for each other. On the one hand, new diseases and accidents indicate that animals are not as innocuous as they were long thought; on the other hand, the now questioned human impact on the natural environment is considered a risk for animals. This research analyzed these contrasting images of animals in the Swiss information media. Of the five main animal figures identified over the last 30 years, this paper focuses on the Undesirable Animal and the Victim Animal. These two figures have existed throughout the observed period; in contrast to Victim Animals, however, who appear fairly infrequently, Undesirable Animals have become more and more common in the last decade, usually in relation to a specific issue (such as the avian flu). This suggests that the media more often convey the dominant anthropocentric relationship to animals, reflecting a preoccupation with the protection of humans against dangerous animals, whereas the protection of animals from humans is considered less important. Recent controversies demonstrate, however, that the frontier between “us” and “them” is regularly renegotiated.


2007 ◽  
Vol 29 (-1) ◽  
pp. 1-21 ◽  
Author(s):  
Krystyna Bałaga

Changes in the Natural Environment Recorded in the Sediments of the Karaśne Lake-Mire Complex (Lublin Polesie, E Poland)This article presents results of multidisciplinary research which has been carried out in order to determine changes in the vegetation cover as well as changes in the structure of the Karaśne lake-mire complex in the Late Glacial and Holocene. In addition, human impact on the formation of the vegetation cover and the bio- and chronostratigraphy of the Late Glacial sediments is discussed.


Iraq ◽  
2015 ◽  
Vol 77 ◽  
pp. 9-39 ◽  
Author(s):  
Daniele Morandi Bonacossi ◽  
Marco Iamoni

This paper presents a preliminary report on the first two seasons of work by The Land of Nineveh Archaeological Project (LoNAP) of Udine University that aims to understand the formation and transformation of the cultural and natural landscape of northern Mesopotamia, (embracing large parts of the governorates of Ninawa and Dohuk) from the Palaeolithic to the Islamic period. Its purpose is to comprehend patterns of settlement, land use and management, based on a regional archaeological surface survey and excavation. These objectives are closely tied to the geoarcheological and bioarchaeological reconstruction of the ancient natural environment and its evolution as a result of global climatic fluctuations and human impact.


2021 ◽  
Vol 66 (3) ◽  
pp. 89-103
Author(s):  
Piotr Szwarczewski

The Mozgawa area, located in the Ponidzie Pińczowskie Region (SE part of the Nida River Basin), is a very good example of response of the natural environment to the progressive human impact. The research conducted there indicates that before the appearance of the first Neolithic farmers, the relief of the area was different to the modern one. Constant and intensive agricultural use of the loess plateau and the adjacent slopes (started in the Neolithic period some 5890±100 BP) led to the filling of the valley bottoms and local depressions with deluvial deposits, the thickness of which reaches up to 12 m. The deposition of these sediments and elevation of the surface level in the subordinate areas resulted in the creation of the Mozgawka River channel since the begining of the Roman Period. Formerly it was impossible (as it was within the depression) and the runoff was only through the karst system. Since that moment it has also started the accumulation of the alluvial fan, the progradation of which leads to the pushing of the Nida River channel towards the East.


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