hymecromone and 7-amino-4-methylcoumarin

The aim of this work was to highlight a considerable and broad problem in UGT1A10 activity assessment that has led to underestimation of its role in intestinal glucuronidation of drugs and other xenobiotics. The reason appears to be poor activity of the commercial UGT1A10 that is used by many laboratories, and here we have tested it by comparison with our recombinant His-tagged UGT1A10 (designated as UGT1A10-H), both expressed in insect cells. The glucuronidation rates of morphine, estradiol, estrone, SN-38, diclofenac, 4-methylumbelliferone, 7-amino-4-methylcoumarin, N-(3-carboxypropyl)-4-hydroxy-1,8-naphthalimide, and bavachinin were assayed. The results revealed that the activity of commercial UGT1A10 was low, very low, and in the cases of morphine, estrone, 7-methyl-4-aminocoumarin, and bavachinin it was below the detection limit. On the other hand, under the same conditions, UGT1A10-H exhibited high glucuronidation rates toward all these compounds. Moreover, using estradiol, morphine, and estrone, in the presence and absence of suitable inhibitors, nilotinib or atractylenolide I, it was demonstrated that UGT1A10-H, but not the commercial UGT1A10, provides a good tool to study the role of native UGT1A10 in the human intestine. The results also suggest that much of the data in the literature on UGT1A10 activity may have to be re-evaluated.

Topics: Animals; Blotting, Western; Camptothecin; Chromatography, High Pressure Liquid; Coumarins; Diclofenac; Estradiol; Estrone; Flavonoids; Glucuronosyltransferase; Humans; Hymecromone; Intestinal Mucosa; Irinotecan; Kinetics; Microsomes, Liver

Hydrolytic exoenzymes as indicators of metabolically active bacteria were investigated in four consecutive sapropel layers collected from bathyal sediments of the eastern Mediterranean Sea. For comparison, the organic carbon-poor layers between the sapropels, sediment from the anoxic Urania basin, and sediments of intertidal mud flats of the German Wadden Sea were also analyzed. The sapropel layers contained up to 1.5. 10(8) bacterial cells cm(-3), whereas cell numbers in the intermediate layers were lower by a factor of 10. In sapropels, the determination of exoenzyme activity with fluorescently labeled substrate analogues was impaired by the strong adsorption of up to 97% of the enzymatically liberated fluorophores (4-methylumbelliferone [MUF] and 7-amino-4-methylcoumarin [MCA]) to the sediment particles. Because all established methods for the extraction of adsorbed fluorophores proved to be inadequate for sapropel sediments, we introduce a correction method which is based on the measurement of equilibrium adsorption isotherms for both compounds. Using this new approach, high activities of aminopeptidase and alkaline phosphatase were detected even in a 124,000-year-old sapropel layer, whereas the activity of beta-glucosidase was low in all layers. So far, it had been assumed that the organic matter which constitutes the sapropels is highly refractory. The high potential activities of bacterial exoenzymes indicate that bacteria in Mediterranean sapropels are metabolically active and utilize part of the subfossil kerogen. Since a high adsorption capacity was determined not only for the low-molecular-weight compounds MUF and MCA but also for DNA, the extraordinarily strong adsorption of structurally different substrates to the sapropel matrix appears to be the major reason for the long-term preservation of biodegradable carbon in this environment.

Topics: Alkaline Phosphatase; Aminopeptidases; Bacteria; beta-Glucosidase; Colony Count, Microbial; Coumarins; Fluorescent Dyes; Fossils; Geologic Sediments; Hymecromone; Kinetics; Mediterranean Sea; Seawater; Water Microbiology