Two homogeneous new peptidoglycans were obtained from Lycium barbarum L. Theywere found to be effective ingredients capable of resining lipid peroxidation. The componentsand linkages of the two homogeneous polysacchar...Two homogeneous new peptidoglycans were obtained from Lycium barbarum L. Theywere found to be effective ingredients capable of resining lipid peroxidation. The componentsand linkages of the two homogeneous polysaccharides were studied by means of complete acidhydrolysis, periodate oxidation. Smith degradation enzyme hydrolysis, IR, GC and aminoacid analysis. Homogeneous polysaccharide LBPC2 was found to be a β(1→4)(1→6) peptidoglycanwith MW of 1.2×104, composed of Xyl, Rha. Man in a molar ratio of8.8:2.3;1, LBPC4 was foundto be a a(1→4)(1→6) peptidoglycan with MW of 1.0×104, composed of glucans.展开更多
THE hydrothermal activity area investigated is located at the middle of the trough (126°50′—127°30′E; 27°20′—27°50′N). Some surface sediment samples and core samples were collected, with othe...THE hydrothermal activity area investigated is located at the middle of the trough (126°50′—127°30′E; 27°20′—27°50′N). Some surface sediment samples and core samples were collected, with other samples from non-hydrothermal activity area (128°20′—129°10′E; 30°30′—31°40′N) in the north of the trough for comparison. Analyses for elements and展开更多
文摘Two homogeneous new peptidoglycans were obtained from Lycium barbarum L. Theywere found to be effective ingredients capable of resining lipid peroxidation. The componentsand linkages of the two homogeneous polysaccharides were studied by means of complete acidhydrolysis, periodate oxidation. Smith degradation enzyme hydrolysis, IR, GC and aminoacid analysis. Homogeneous polysaccharide LBPC2 was found to be a β(1→4)(1→6) peptidoglycanwith MW of 1.2×104, composed of Xyl, Rha. Man in a molar ratio of8.8:2.3;1, LBPC4 was foundto be a a(1→4)(1→6) peptidoglycan with MW of 1.0×104, composed of glucans.
文摘THE hydrothermal activity area investigated is located at the middle of the trough (126°50′—127°30′E; 27°20′—27°50′N). Some surface sediment samples and core samples were collected, with other samples from non-hydrothermal activity area (128°20′—129°10′E; 30°30′—31°40′N) in the north of the trough for comparison. Analyses for elements and
