The Great Rann of Kachchh, a vast expanse of salt desert in Western India is a unique hostile ecosystem posing an extreme environment to life forms due to high salt content, hyper-axid climate, seasonal water logging ...The Great Rann of Kachchh, a vast expanse of salt desert in Western India is a unique hostile ecosystem posing an extreme environment to life forms due to high salt content, hyper-axid climate, seasonal water logging and extremes of temperature. In the virtual absence of natural vegetation, soils and sediments of Rann of Kachchh axe microbially dominated ecosystems. In the present study microbial activity and the diversity of cultivated heterotrophic bacteria were investigated in the sediments collected along a 5-m exposed section at Khadir Island in the Great Rann of Kachchh. Microbial activity （as an index of sediment enzymes） was found to be high in the middle of the section （200-280 cm）. Dehydrogenase （DHA）, substrate-induced DHA and alkaline phosphatase activities revealed the oligotrophic nature of the basal portion （320-480 cm）. Abundant bacterial isolates obtained from different depths were found to be clustered in 12 different phylogenetic groups by amplified ribosomal DNA restriction analysis. 16S rRNA gene sequencing revealed the dominant bacterial ribotypes to be affiliated to Firmicutes （Families Bacillaceae and Staphyloeoccaeeae） and Aetinobaeteria （Family Brevibaeteriaceae） with minor contribution of Proteobacteria （Families Phyllobacteriaeeae and Bartonellaceae）, pointing their endurance and adaptability to environmental stresses. Statistical analysis indicated that sediment organic carbon, salinity, total available nitrogen and total available phosphorous are most likely critical determinants of microbial activity in the Khadir Island sediments.展开更多
The present study is based on the field observations and geochemical analyses of flood sediments to ascertain the nature and causes of destruction in the Mandakini and Alaknanda river valleys during June 2013.The stud...The present study is based on the field observations and geochemical analyses of flood sediments to ascertain the nature and causes of destruction in the Mandakini and Alaknanda river valleys during June 2013.The study suggests that the sediments were contributed from two major sources:the moraines and alluvial fans located in the Trans and Higher Himalaya;and the landslides in the Higher and Lesser Himalaya.Although the flood was the result of a high intensity rainfall event.展开更多
基金Supported by the Department of Science and Technology(DST),Government of India(Nos.SR/S4/ES-21/Baroda Window/P3 andSR/S4/ES-21/Kachchh Window/P1)
文摘The Great Rann of Kachchh, a vast expanse of salt desert in Western India is a unique hostile ecosystem posing an extreme environment to life forms due to high salt content, hyper-axid climate, seasonal water logging and extremes of temperature. In the virtual absence of natural vegetation, soils and sediments of Rann of Kachchh axe microbially dominated ecosystems. In the present study microbial activity and the diversity of cultivated heterotrophic bacteria were investigated in the sediments collected along a 5-m exposed section at Khadir Island in the Great Rann of Kachchh. Microbial activity （as an index of sediment enzymes） was found to be high in the middle of the section （200-280 cm）. Dehydrogenase （DHA）, substrate-induced DHA and alkaline phosphatase activities revealed the oligotrophic nature of the basal portion （320-480 cm）. Abundant bacterial isolates obtained from different depths were found to be clustered in 12 different phylogenetic groups by amplified ribosomal DNA restriction analysis. 16S rRNA gene sequencing revealed the dominant bacterial ribotypes to be affiliated to Firmicutes （Families Bacillaceae and Staphyloeoccaeeae） and Aetinobaeteria （Family Brevibaeteriaceae） with minor contribution of Proteobacteria （Families Phyllobacteriaeeae and Bartonellaceae）, pointing their endurance and adaptability to environmental stresses. Statistical analysis indicated that sediment organic carbon, salinity, total available nitrogen and total available phosphorous are most likely critical determinants of microbial activity in the Khadir Island sediments.
文摘The present study is based on the field observations and geochemical analyses of flood sediments to ascertain the nature and causes of destruction in the Mandakini and Alaknanda river valleys during June 2013.The study suggests that the sediments were contributed from two major sources:the moraines and alluvial fans located in the Trans and Higher Himalaya;and the landslides in the Higher and Lesser Himalaya.Although the flood was the result of a high intensity rainfall event.
