Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Microbial biomass carbon and enzymes-degraders of carbohydrates in polar soils from the area of Livingston Island, Antarctica. / Malcheva, Boyka ; Nustorova, Maya ; Zhiyanski, Miglena ; Yaneva, Rositsa ; Abakumov, Evgeniy .
в: Soil Science Annual, Том 73, № 2, 156042, 25.10.2022.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - Microbial biomass carbon and enzymes-degraders of carbohydrates in polar soils from the area of Livingston Island, Antarctica
AU - Malcheva, Boyka
AU - Nustorova, Maya
AU - Zhiyanski, Miglena
AU - Yaneva, Rositsa
AU - Abakumov, Evgeniy
PY - 2022/10/25
Y1 - 2022/10/25
N2 - Polar soils under different vegetation cover from Livingston Island (Antarctica) were studied analyzing indicators of carbohydrates decomposition in soils: organic carbon, biomass carbon, total nitrogen, C:N ratio, cellulase, amylase, and invertase activity. The highest values of microbial biomass in soils were indicated for sites with vegetation cover while the lowest values in soils without vegetation, which correlate with the content of total organic carbon and the C:N ratio. The highest percentage of biomass carbon compared to the total organic biomass carbon is obtained for two sites with mosses, and the lowest in sites without vegetation, followed by the sites with lichens. Cellulase activity is highest in polar soils with moss cover. Amylase activity depends more strongly on the type of vegetation. The highest amylase activity is detected in soils under algae cover and the lowest in soils without vegetation. Invertase activity is limited by the extreme soil and climatic conditions of Antarctica. A very strong, positive correlation is found between total carbon and total nitrogen. The relationship between total carbon and the C:N ratio, as well as between biomass carbon and amylase activity, is moderate, and positive. The higher dependence of amylase activity from organic carbon with microbial origin correlates with higher values of the enzyme amylase compared to the enzyme cellulase. There is a strong (cellulase) and very strong (amylase) positive relationship between the activity of enzymes and the combination of factors: total carbon, total nitrogen, C: N ratio and biomass carbon.
AB - Polar soils under different vegetation cover from Livingston Island (Antarctica) were studied analyzing indicators of carbohydrates decomposition in soils: organic carbon, biomass carbon, total nitrogen, C:N ratio, cellulase, amylase, and invertase activity. The highest values of microbial biomass in soils were indicated for sites with vegetation cover while the lowest values in soils without vegetation, which correlate with the content of total organic carbon and the C:N ratio. The highest percentage of biomass carbon compared to the total organic biomass carbon is obtained for two sites with mosses, and the lowest in sites without vegetation, followed by the sites with lichens. Cellulase activity is highest in polar soils with moss cover. Amylase activity depends more strongly on the type of vegetation. The highest amylase activity is detected in soils under algae cover and the lowest in soils without vegetation. Invertase activity is limited by the extreme soil and climatic conditions of Antarctica. A very strong, positive correlation is found between total carbon and total nitrogen. The relationship between total carbon and the C:N ratio, as well as between biomass carbon and amylase activity, is moderate, and positive. The higher dependence of amylase activity from organic carbon with microbial origin correlates with higher values of the enzyme amylase compared to the enzyme cellulase. There is a strong (cellulase) and very strong (amylase) positive relationship between the activity of enzymes and the combination of factors: total carbon, total nitrogen, C: N ratio and biomass carbon.
KW - Polar soils
KW - Organic carbon
KW - Biomass carbon
KW - cellulase
KW - Amylase
KW - Invertase
U2 - 10.37501/soilsa/156042
DO - 10.37501/soilsa/156042
M3 - Article
VL - 73
JO - Soil Science Annual
JF - Soil Science Annual
SN - 2300-4967
IS - 2
M1 - 156042
ER -
ID: 101051861