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Bibliografia publikacji pracowników
Państwowej Szkoły Wyższej w Białej Podlaskiej

Baza tworzona przez Bibliotekę Akademii Bialskiej im. Jana Pawła II.


Zapytanie: GEOCHEMISTRY
Liczba odnalezionych rekordów: 2



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Nr opisu:
Autorzy: , , Vol. 68 2587-585X OTHER 20232541-96682022/202310.21638/spbu07.2023.206Zbucki, Łukaszalluvial soilFINAL_PUBLISHEDDespite their great importance, Holocene-Late Pleistocene sediments are poorly studied in the valleys of rivers in the Krasnoyarsk forest-steppe territory. We present the first detailed study of the geochemical composition of the first floodplain terrace sediments in the valley of the Berezovka River, and the continuous accumulation that occurred at the Late Pleistocene-Holocene (from 20833 ą 519 cal yr BP). This is of great fundamental importance and is the basis for further studies on the influence of anthropogenic activities on the natural environment in the Krasnoyarsk agglomeration. The sediments were covered by modern alluvial dark-humus hydrometamorphosed soil. Macromorphological studies and investigation of the humus content have revealed a well-developed process of humus formation and humus accumulation, a gley process. The measured contents of some elements (U, Pr, Rb, V, Bi, Cd, As, Th, Ga, Co, and Sm) exceeded the respective Clarke values for the Earth's crust. The distribution of most elements and their accumulation in the Middle-Late Holocene (from to 5477-4985 to 1241-803 cal yr BP) in the middle of the sediment profile is explained by the high content of mud and clay minerals. Based on the coefficients of radial migration, we established that most of the studied elements were introduced into the sediments during high water levels and floods. The values of palaeomarkers indicate a change in climatic conditions in the Late Pleistocene and Holocene from dry and cold to more humid and warm, and from arid and cold (in the Early Holocene) to modern climatic conditions, respectively.Berezovka Riverfloodplain terraceforest-steppegeochemistryholocenelate pleist.
Tytuł czasopisma:
Charakterystyka formalna:
Charakterystyka merytoryczna:
Język publikacji:
Wskaźnik Impact Factor ISI: studies and investigation of the humus content have revealed a well-developed process of humus formation and humus accumulation, a gley process. The measured contents of some elements (U, Pr, Rb, V, Bi, Cd, As, Th, Ga, Co, and Sm) exceeded the respective Clarke values for the Earth's crust. The distribution of most elements and their accumulation in the Middle-Late Holocene (from to 5477-4985 to 1241-803 cal yr BP) in the middle of the sediment profile is explained by the high content of mud and clay minerals. Based on the coefficients of radial migration, we established that most of the studied elements were introduced into the sediments during high water levels and floods. The values of palaeomarkers indicate a change in climatic conditions in the Late Pleistocene and Holocene from dry and cold to more humid and warm, and from arid and cold (in the Early Holocene) to modern climatic conditions, respectively.^aBerezovka River^afloodplain terrace^aforest-steppe^ageochemistry^aholocene^alate pleistocene^aradiocarbon dating^asediments
Praca recenzowana
Słowa kluczowe ang.: and investigation of the humus content have revealed a well-developed process of humus formation and humus accumulation, a gley process. The measured contents of some elements (U, Pr, Rb, V, Bi, Cd, As, Th, Ga, Co, and Sm) exceeded the respective Clarke values for the Earth's crust. The distribution of most elements and their accumulation in the Middle-Late Holocene (from to 5477-4985 to 1241-803 cal yr BP) in the middle of the sediment profile is explained by the high content of mud and clay minerals. Based on the coefficients of radial migration, we established that most of the studied elements were introduced into the sediments during high water levels and floods. The values of palaeomarkers indicate a change in climatic conditions in the Late Pleistocene and Holocene from dry and cold to more humid and warm, and from arid and cold (in the Early Holocene) to modern climatic conditions, respectively.^aBerezovka River^afloodplain terrace^aforest-steppe^ageochemistry^aholocene^alate pleistocene^aradiocarbon dating^asediments
Słowa kluczowe ang.: ; ; ;

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Nr opisu: n impact recorded in lake environment (Charzykowskie Lake, N Poland) during the last 6,200 ye00000464230000000325AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGhttps://geojournals.pgi.gov.pl/agp/article/view/33881100^a0001-5709^bQ^e2300-1887^fA^hABC^iX^jXY^kQ000213^a003^b003^c2023-10-03, 13:59^d2023-10-03, 13:59^e3121018880^f3121018880^aHuman impact recorded in lake environment (Charzykowskie Lake, N Poland) during the last 6,200 years^aActa Geologica Polonica^a2023^bVol. 73^cno. 3^dp. 467--478^a0001-5709^a2022/2023^a10.24425/agp.2023.145612^aZbucki, Łukasz^cy^ageochemistry^aFINAL_PUBLISHED^bOTHER^cAT_PUBLICATION^eOPEN_JOURNAL^aBased on geochemical and biological investigations of a 6-m-long sediment core, a reconstruction of the environmental conditions in Charzykowskie Lake (northern Poland) is presented. The analyzed sediments consist of fine calcareous detritus gyttja interbedded by lake marl. The results of palynological analysis document the vegetation development around and in the studied lake and confirm the middle and late Holocene age of the sedimentation of the deposits. The identification of 22 taxa of subfossil Cladocera shows the biodiversity of the fauna and reflects the changes in the trophic and water level. The concentrations of various chemical elements suggest the origin of the sediments. Geochemical, including isotope, and biological data, made it possible to reconstruct the environmental conditions, as well as traces of human influence over the last ca. 6,200 years. Four stages of human impact have been documented by the pollen data. The first traces of human groups in the vicinity of Charzykowskie Lake are preserved in sediments from about 4,000 years ago. The human activity is poorly recorded in the Cladocera and in the geochemical compositions of the lake sediments, probably due to the size and depth of the lake and its isolation.^aholocene^ahuman impact^alake sediments^aPoland^asubfossil cladocera
Autorzy: , .
Tytuł czasopisma:
Charakterystyka merytoryczna:
Język publikacji: , oland) during the last 6,200 ye00000464230000000325AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGhttps://geojournals.pgi.gov.pl/agp/article/view/33881100^a0001-5709^bQ^e2300-1887^fA^hABC^iX^jXY^kQ000213^a003^b003^c2023-10-03, 13:59^d2023-10-03, 13:59^e3121018880^f3121018880^aHuman impact recorded in lake environment (Charzykowskie Lake, N Poland) during the last 6,200 years^aActa Geologica Polonica^a2023^bVol. 73^cno. 3^dp. 467--478^a0001-5709^a2022/2023^a10.24425/agp.2023.145612^aZbucki, Łukasz^cy^ageochemistry^aFINAL_PUBLISHED^bOTHER^cAT_PUBLICATION^eOPEN_JOURNAL^aBased on geochemical and biological investigations of a 6-m-long sediment core, a reconstruction of the environmental conditions in Charzykowskie Lake (northern Poland) is presented. The analyzed sediments consist of fine calcareous detritus gyttja interbedded by lake marl. The results of palynological analysis document the vegetation development around and in the studied lake and confirm the middle and late Holocene age of the sedimentation of the deposits. The identification of 22 taxa of subfossil Cladocera shows the biodiversity of the fauna and reflects the changes in the trophic and water level. The concentrations of various chemical elements suggest the origin of the sediments. Geochemical, including isotope, and biological data, made it possible to reconstruct the environmental conditions, as well as traces of human influence over the last ca. 6,200 years. Four stages of human impact have been documented by the pollen data. The first traces of human groups in the vicinity of Charzykowskie Lake are preserved in sediments from about 4,000 years ago. The human activity is poorly recorded in the Cladocera and in the geochemical compositions of the lake sediments, probably due to the size and depth of the lake and its isolation.^aholocene^ahuman impact^alake sediments^aPoland^asubfossil cladocera
Wskaźnik Impact Factor ISI:
Punktacja ministerstwa:
Praca recenzowana
Słowa kluczowe ang.: ; ;

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