Gene/Protein Disease Symptom Drug Enzyme Compound
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Query: EC:3.2.1.26 (invertase)
 4,927 document(s) hit in 31,850,051 MEDLINE articles (0.00 seconds)

1. The disaccharidase activities of the small intestines of American alligators (Alligator mississippiensis) were studied in epithelial scrapes and brush-border membrane preparations. 2. Maltase, isomaltase and trehalase activities were found. Activities of these enzymes were higher in the proximal small intestine and decreased distally. 3. Disaccharidase activities were enriched 12-15 times in brush-border membrane preparations, compared with mucosa/enterocyte crude homogenates and were co-enriched with the brush-border membrane marker alkaline phosphatase. 3. The pH optima were: maltase 6.5; isomaltase 5.6; and trehalase 5.8. The Q10 of maltase, the most active enzyme, was equal to 1.82. 4. In reptiles, as in mammals, disaccharidase activities may be correlated with feeding habits. The co-occurrence of sucrase and isomaltase may not be a common feature of vertebrates.
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PMID:Intestinal brush border membrane-bound disaccharidases of the American alligator, Alligator mississippiensis. 306 78

In order to investigate the soil microbial respiration under different temperature conditions and its relationship to soil dissolved organic carbon ( DOC) and invertase, an indoor incubation experiment was performed. The soil samples used for the experiment were taken from Laoshan, Zijinshan, and Baohuashan. The responses of soil microbial respiration to the increasing temperature were studied. The soil DOC content and invertase activity were also measured at the end of incubation. Results showed that relationships between cumulative microbial respiration of different soils and soil temperature could be explained by exponential functions, which had P values lower than 0.001. The coefficient of temperature sensitivity (Q10 value) varied from 1.762 to 1.895. The Q10 value of cumulative microbial respiration decreased with the increase of soil temperature for all soils. The Q10 value of microbial respiration on 27 days after incubation was close to that of 1 day after incubation, indicating that the temperature sensitivity of recalcitrant organic carbon may be similar to that of labile organic carbon. For all soils, a highly significant ( P = 0.003 ) linear relationship between cumulative soil microbial respiration and soil DOC content could be observed. Soil DOC content could explain 31.6% variances of cumulative soil microbial respiration. For the individual soil and all soils, the relationship between cumulative soil microbial respiration and invertase activity could be explained by a highly significant (P < 0.01) linear regression function, which suggested that invertase was a good indicator of the magnitude of soil microbial respiration.
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PMID:[Soil Microbial Respiration Under Different Soil Temperature Conditions and Its Relationship to Soil Dissolved Organic Carbon and Invertase]. 2616 32