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1.
Abstract Growth-chamber cultivated Raphanus plants accumulate nitrate during their vegetative growth. After 25 days of growth at a constant supply to the roots of 1 mol m?3 (NO?3) in a balanced nutrient solution, the oldest leaves (eight-leaf stage) accumulated 2.5% NO?3-nitrogen (NO3-N) in their lamina, and almost 5% NO3-N in their petioles on a dry weight basis. This is equivalent to approximately 190 and 400 mol?3 m?3 concentration of NO?3 in the lamina and the petiole, respectively, as calculated on a total tissue water content basis. Measurements were made of root NO?3 uptake, NO?3 fluxes in the xylem, nitrate uptake by the mesophyll cells, and nitrate reduction as measured by an in vivo test. NO?3 uptake by roots and mesophyll cells was greater in the light than in the dark. The NO?3 concentration in the xylem fluid was constant with leaf age, but showed a distinct daily variation as a result of the independent fluxes of root uptake, transpiration and mesophyll uptake. NO?3 was reduced in the leaf at a higher rate in the light than in the dark. The reduction was inhibited at the high concentrations calculated to exist in the mesophyll vacuoles, but reduction continued at a low rate, even when there was no supply from the incubation medium. Sixty-four per cent of the NO?3 influx was turned into organic nitrogen, with the remaining NO?3 accumulating in both the light and the dark.  相似文献   
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ABSTRACT. Homogenates of trophozoites of Entamoeba histolytica were shown to bring about the total degradation of glycogen while purified phosphorylase of the same source alone yielded a limit dextrin as end product. An enzyme system capable of debranching the limit dextrin was obtained from the 40,000 g pellet by extraction in aqueous medium, purified by gel filtration on Fractogel TSK HW-55(F), and separated from phosphorylase by chromatography on Blue Sepharose CL-6B and aminobutyl Agarose. The glycogen-debranching system was purified 540-fold to a state of homogeneity by criterion of disc-gel electrophoresis. The purified enzyme was able to degrade glycogen-limit dextrin in the presence of phosphorylase and exhibited activities of both amylo-1,6-glucosidase (EC 3.2.1.33) and 4- α -glucanotransferase (EC 2.4.1.25). Although amylo-1,6-glucosidase released glucose from a glycogen-phosphorylase limit dextrin, transferase activity moved single glucose residues from the limit dextrin to 4-nitrophenyl- α -glucoside yielding successively 4-nitrophenyl- α -maltoside and 4-nitrophenyl- α -maltotrioside that could be detected by HPLC. Native glycogen-debranching system exhibited a relative molecular mass of Mr= 180,000 ± 10% by gel filtration and gel electrophoresis in both denaturing and nondenaturating conditions.  相似文献   
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A method was developed to produce radiolabeled 3-hydroxy-L-kynurenine by injection of [14C]-L-tryptophan into pupae of the heliconid butterfly, Heliconius charitonia, which was converted into [14C]-3-hydroxy-L-kynurenine and deposited as a wing pigment. Extractions of 3-hydroxykynurenine (3-OHK) with 60% methanol from wings yielded in 14.4 μg per mg dry weight. In extracts from yellow wing areas, 3-OHK represented 100% of detectable amino acids. Resulting specific radioactivity of [14C]-3-OHK was between 0.05 and 0.07 mCi/mmol when 0.5 μCi [14C]-tryptophan was injected into pupae 1 or 2 days before emergence of the butterfly. Incorporation of [14C]-3-OHK into wing ommochromes was studied in nymphalid butterflies, Araschnia levana and Precis coenia. After injection into pupae [I4C]-3-OHK as well as [14C]-tryptophan were specifically incorporated into red and red-brown wing scales as shown by autoradiography. The same incorporation occurred in isolated wings after incubation in Grace's medium containing [14C]-3-OHK. In Araschnia levana, [14C]-3-OHK offered to left wing pairs was incorporated into dihydroxanthommatin six times more effectively than [14C]-tryptophan offered to right wing pairs from the same specimen. Therefore, 3-OHK seems to be the ultimate precursor of wing ommatins.  相似文献   
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The Emsian? through early Eifelian Onondaga Limestone of the Appalachian Basin was deposited in a topographic basin and on the carbonate platform which surrounded the basin on the west, north, and northeast. Onondaga strata thin from the platform into the basin. Two sedimentary cycles are present in the sub-Tioga Onondaga of eastern North America. The Edgecliff-Amherstburg represents an interval of transgression, in which epeiric seas spread over much of eastern North America. During the Nedrow-Lucas regression, the interior of the carbonate platform became restricted, resulting in the deposition of evaporites. The Moorehouse-Anderdon transgression continued through the deposition of the Tioga Bentonite, followed by the pre-Speeds-Dundee regression from the craton. Early Eifelian Appalachian Basin Onondaga brachiopod communities, arranged from nearshore to offshore, include the Atrypid-Megakozlowskiella, Atrypid-Levenea, Chonetid, Atlanticocoelia, Ambocoeliid, and Truncalosia Communities. The Onondaga-age Eastern Americas Realm is divided into the Appohimchi Province in the Appalachian Basin and the Michigan Basin-Hudson Bay Lowland Province in the Midwest. The provincial assignment of the James Bay region of Ontario is uncertain; the Eastern Townships of Quebec are near the boundaries both of the two provinces of the Eastern Americas Realm, and of the Eastern Americas Realm and the Old World Realm, the latter realm being probably in the Canadian Maritime Provinces.  相似文献   
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