Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Zbigniew Śnieszko"'
Publikováno v:
Water, Vol 13, Iss 6, p 777 (2021)
Beavers have lived in the territory of Poland since the beginning of the Holocene, as testified by bone remains found in archaeological sites of different ages. The area inhabited by these animals has experienced continuing transformations of terrain
Externí odkaz:
https://doaj.org/article/60ece586caa0405dbf19f07e639e212b
Autor:
Dominika Łuców, Mariusz Lamentowicz, Katarzyna Marcisz, Milena Obremska, Krzysztof Jażdżewski, Dariusz Brykała, Zbigniew Śnieszko, Sebastian Tyszkowski, Achim Brauer, Anna Pieńczewska, Elisabeth Dietze, Michał Słowiński, Florian Ott, Jan Barabach
Publikováno v:
Journal of Environmental Management
In recent decades, it has been observed that most forest fires in Europe were caused by people. Extreme droughts, which are more often prolonged, can increase the risk of forest fires, not only in southern Europe but also, in Central Europe. Nonethel
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3d218b256ae6df4a26824002fe33acc6
https://doi.org/10.1016/j.jenvman.2019.02.002
https://doi.org/10.1016/j.jenvman.2019.02.002
Publikováno v:
Quaternary International. 502:45-59
In the well-known settlement micro-region of the Malopolska Upland - known for extensive studies into the Neolithic agricultural anthropopressure - the authors have re-examined three selected Holocene soil-sediment sequences derived from soil erosion
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::72d4f858ac1d349bf2c82fb275f4a0cf
https://doi.org/10.1016/j.quaint.2018.09.018
https://doi.org/10.1016/j.quaint.2018.09.018
Loess areas used for agriculture are susceptible to soil erosion. The intensive process of soil erosion in Polish loess areas began with the onset of the Neolithic and has continued intermittently until today. This work presents the results of soil e
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::af0ec1a12777b3e28e73431f67fe33cb
http://hdl.handle.net/20.500.12128/11090
http://hdl.handle.net/20.500.12128/11090
Publikováno v:
Quaternary International. 374:189-197
Slopes used agriculturally at medium latitudes in European loess areas are modelled mainly by washing processes. The thickness of colluvium depends on the intensity of washing processes and the length of time of agricultural use, and it ranges from t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::21ae5d5079b13a3eb9d7a41e2f0987ad
https://doi.org/10.1016/j.quaint.2015.04.004
https://doi.org/10.1016/j.quaint.2015.04.004
Publikováno v:
SGEM International Multidisciplinary Scientific GeoConference EXPO Proceedings.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fc67e10efa798497c431fa272c3e6097
https://doi.org/10.5593/sgem2017/11/s01.066
https://doi.org/10.5593/sgem2017/11/s01.066
Publikováno v:
Quaternary International. 296:61-67
Although colluvium is a valuable record of past human impact, there is a lack of a precise method of age determination. The luminescence method could be used, but the basic difficulty is partial bleaching of quartz grains. In this study, colluviums f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::512a165f1a96b503b65807a7dc065878
https://doi.org/10.1016/j.quaint.2012.05.032
https://doi.org/10.1016/j.quaint.2012.05.032
Publikováno v:
Quaternary International. 240:44-51
At the end of the Pleistocene in Central-Eastern Europe, the accumulation of periglacial loess had already finished. From the end of loess accumulation to the establishment of grass cover and forest succession in this area, a phase of active modeling
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3ab7c327b55fbb75ac85c40bb963c13b
https://doi.org/10.1016/j.quaint.2011.02.005
https://doi.org/10.1016/j.quaint.2011.02.005
Publikováno v:
GEOCHR. 28:61-66
The Basis of the Study of the Age of the Holocene Diluvium on Loess Areas of Polish Highlands Large part of slope sediments (pediment) which are the effect of water induced soil erosion in the loess areas of Polish Uplands, has a close relationship w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e6789997ace336a2021f81a93d52a112
https://doi.org/10.2478/v10003-007-0022-1
https://doi.org/10.2478/v10003-007-0022-1