This paper describes the biodiversity of cyanobacteria and microalgae of biological soil crusts(BSC)on bare substrates in different mountain vegetation types at the Northern Urals.In total,we identified 99 algal speci...This paper describes the biodiversity of cyanobacteria and microalgae of biological soil crusts(BSC)on bare substrates in different mountain vegetation types at the Northern Urals.In total,we identified 99 algal species from six divisions in all sampled sites.The species diversity and structure of BSC algal communities show a relationship with environmental factors(altitude,soil p H and humidity,and illumination).Taxonomic diversity of algae decreases along the altitude gradient from mountain meadow to mountain tundra.Algae and cyanobacteria species from six divisions were identified in meadow communities,five in mountain forests and four in mountain tundra.We observed a positive correlation between species diversity of phototrophic microorganisms and altitude in the forest communities,but a negative correlation in the tundra.The dominant complex of cyanobacterial and algal species in BSC was specific for each type of plant community and was reflective of the habitat conditions.The species diversity and morphological organization of the BSC algae thalli can be used as a criterion for the ongoing assessment of climatic changes in high latitudes and mountain regions.展开更多
The distribution and availability of phosphorus(P)fractions in restored cut slope soil aggregates,along altitude gradients,were analyzed.Samples were collected at 3009,3347,3654 and 3980 m of altitude.We examined soil...The distribution and availability of phosphorus(P)fractions in restored cut slope soil aggregates,along altitude gradients,were analyzed.Samples were collected at 3009,3347,3654 and 3980 m of altitude.We examined soil aggregates total phosphorus(TP),available phosphorus(AP)and phosphorus activation coefficient(PAC),and discovered that there was no significant difference in TP levels between all four altitudes samples(p>0.05).However,there was a significant difference in AP at 3009,3347 and 3980 m of altitude(p<0.05).At the altitudes of 3009,3347 and 3654 m,the AP accumulation in small size aggregates was more advantageous.Overall,PAC dropped steadily as soil aggregates sizes increased,as shown:PAC(3654 m)>PAC(3347 m)>PAC(3009 m)>PAC(3980 m).In all particle size soil aggregates,the distribution of the P fractions was as follows:total inorganic phosphorus(TPi)>total organic phosphorus(TPo)>residual phosphorus(R-P),at 3009,3347 and 3654 m,but a different registry was observed at 3980 m of altitude:TPo>TPi>R-P.Through correlation and multiple stepwise regression analysis,it was concluded that active NaHCO_(3)-Pi was the main AP source.It was also suggested that more attention should be given to the ratio of small particle size aggregates to increase soil AP storage.In order to improve the activation capacity and supply of soil P,along with promotion of the healthy development of soil ecosystem on slope land,it was suggest that inorganic P fertilizer and P activator could be added to soil at both low(3009 m)and high altitudes(3980 m).展开更多
Introduction:Soil is the major reservoir of organic carbon.There is a paucity of soil organic carbon(SOC)stock data of afroalpine and sub-afroalpine vegetation in Ethiopia.Hence,this study was conducted to estimate th...Introduction:Soil is the major reservoir of organic carbon.There is a paucity of soil organic carbon(SOC)stock data of afroalpine and sub-afroalpine vegetation in Ethiopia.Hence,this study was conducted to estimate the SOC stock and correlate it with soil physicochemical properties in Abune Yosef afroalpine and sub-afroalpine vegetation.Systematic sampling was employed to collect soil samples from upper 30 cm.Dry bulk density soil pH(1:2.5 water);organic carbon(Walkley and Black),and total nitrogen(Kjeldahl)were the methods used for soil analysis.Pearson correlation and linear regression analysis were performed in SPSS 24 statistical software.Results:The SOC stock of the study area was found to be 79.57 t C ha−1.Soil organic carbon stock showed statistically significant positive correlation with vegetation type(r=0.522,p<0.01),bulk density(r=0.62,p<0.01),total nitrogen(r=0.41,p<0.01),and altitude(r=0.468,p<0.01)and negative correlation with slope(r=−0.298,p<0.05).The present study revealed similar soil organic carbon stock(SOCS)with the Intergovernmental Panel on Climate Change(IPCC)default estimate for similar regions.Positive correlation of SOCS and altitude could be resulted from the variations in anthropogenic disturbances,temperature,and precipitation vegetation types.The negative correlation between SOCS and slope is the result from the predictably higher soil erosion at steeper slopes.Temporal livestock trampling increased the bulk density but never affected the SOCS to decline.Aspect did not show any significant relationship with SOCS due to either the under surveying of all aspects or similar solar radiation found in the study area.Moreover,gazing,aspect,and soil pH did not show statistically significant impact on SOCS.Conclusion:The SOCS of Abune Yosef afroalpine and sub-afroalpine vegetation is similar to the IPCC default estimate for similar regions.This is a great contribution both to the global and local terrestrial carbon sink.展开更多
基金supported by the Ministry of Education and Science of the Russian Federation project No.1021051101424-8-1.6.111.6.191.6.20。
文摘This paper describes the biodiversity of cyanobacteria and microalgae of biological soil crusts(BSC)on bare substrates in different mountain vegetation types at the Northern Urals.In total,we identified 99 algal species from six divisions in all sampled sites.The species diversity and structure of BSC algal communities show a relationship with environmental factors(altitude,soil p H and humidity,and illumination).Taxonomic diversity of algae decreases along the altitude gradient from mountain meadow to mountain tundra.Algae and cyanobacteria species from six divisions were identified in meadow communities,five in mountain forests and four in mountain tundra.We observed a positive correlation between species diversity of phototrophic microorganisms and altitude in the forest communities,but a negative correlation in the tundra.The dominant complex of cyanobacterial and algal species in BSC was specific for each type of plant community and was reflective of the habitat conditions.The species diversity and morphological organization of the BSC algae thalli can be used as a criterion for the ongoing assessment of climatic changes in high latitudes and mountain regions.
基金This work was supported by the National Natural Science Foundation of China(No.41971056)the National Key R&D Program of China(No.2017YFC0504903)。
文摘The distribution and availability of phosphorus(P)fractions in restored cut slope soil aggregates,along altitude gradients,were analyzed.Samples were collected at 3009,3347,3654 and 3980 m of altitude.We examined soil aggregates total phosphorus(TP),available phosphorus(AP)and phosphorus activation coefficient(PAC),and discovered that there was no significant difference in TP levels between all four altitudes samples(p>0.05).However,there was a significant difference in AP at 3009,3347 and 3980 m of altitude(p<0.05).At the altitudes of 3009,3347 and 3654 m,the AP accumulation in small size aggregates was more advantageous.Overall,PAC dropped steadily as soil aggregates sizes increased,as shown:PAC(3654 m)>PAC(3347 m)>PAC(3009 m)>PAC(3980 m).In all particle size soil aggregates,the distribution of the P fractions was as follows:total inorganic phosphorus(TPi)>total organic phosphorus(TPo)>residual phosphorus(R-P),at 3009,3347 and 3654 m,but a different registry was observed at 3980 m of altitude:TPo>TPi>R-P.Through correlation and multiple stepwise regression analysis,it was concluded that active NaHCO_(3)-Pi was the main AP source.It was also suggested that more attention should be given to the ratio of small particle size aggregates to increase soil AP storage.In order to improve the activation capacity and supply of soil P,along with promotion of the healthy development of soil ecosystem on slope land,it was suggest that inorganic P fertilizer and P activator could be added to soil at both low(3009 m)and high altitudes(3980 m).
文摘Introduction:Soil is the major reservoir of organic carbon.There is a paucity of soil organic carbon(SOC)stock data of afroalpine and sub-afroalpine vegetation in Ethiopia.Hence,this study was conducted to estimate the SOC stock and correlate it with soil physicochemical properties in Abune Yosef afroalpine and sub-afroalpine vegetation.Systematic sampling was employed to collect soil samples from upper 30 cm.Dry bulk density soil pH(1:2.5 water);organic carbon(Walkley and Black),and total nitrogen(Kjeldahl)were the methods used for soil analysis.Pearson correlation and linear regression analysis were performed in SPSS 24 statistical software.Results:The SOC stock of the study area was found to be 79.57 t C ha−1.Soil organic carbon stock showed statistically significant positive correlation with vegetation type(r=0.522,p<0.01),bulk density(r=0.62,p<0.01),total nitrogen(r=0.41,p<0.01),and altitude(r=0.468,p<0.01)and negative correlation with slope(r=−0.298,p<0.05).The present study revealed similar soil organic carbon stock(SOCS)with the Intergovernmental Panel on Climate Change(IPCC)default estimate for similar regions.Positive correlation of SOCS and altitude could be resulted from the variations in anthropogenic disturbances,temperature,and precipitation vegetation types.The negative correlation between SOCS and slope is the result from the predictably higher soil erosion at steeper slopes.Temporal livestock trampling increased the bulk density but never affected the SOCS to decline.Aspect did not show any significant relationship with SOCS due to either the under surveying of all aspects or similar solar radiation found in the study area.Moreover,gazing,aspect,and soil pH did not show statistically significant impact on SOCS.Conclusion:The SOCS of Abune Yosef afroalpine and sub-afroalpine vegetation is similar to the IPCC default estimate for similar regions.This is a great contribution both to the global and local terrestrial carbon sink.
