Functions of Calcium-bound Phosphorus in Relation to Characteristics of Phosphorus Releasing Bacteria in Sediment of a Chinese Shallow Lake (Lake Wabu)

Sediment phosphorus (P) release accelerates lake eutrophication, while retention capacity and release potential of different P fractions, calcium-bound P (CaCO₃～P) in particular, still remains unclear. Fractionation and sorption behaviors of phosphorus were studied in sediment of a Chinese shallow lake (Lake Wabu) and two inflowing rivers from December 2011 to December 2012. Abundance of P releasing bacteria was analyzed, and their main species were isolated using a culture-dependent method and identified by their 16S rDNA sequences. CaCO₃～P release abilities of these bacteria were also tested. In sediments of both the lake and rivers studied, the rank order of the different P extracts was CaCO₃～P > iron-bound P > acid-soluble organic P > hot NaOH-extractable organic P. At the same time, CaCO₃～P content and equilibrium P concentration (EPC₀) values in river sediments were significantly higher than those in the lake. Additionally, EPC₀ changes non-monotonically with increasing CaCO₃～P content, forming a V-shaped curve, with the lowest EPC₀ at an intermediate CaCO₃～P content (around 180 mg kg^?1). Below this threshold, CaCO₃～P was a component strengthening P retention; moreover, CaCO₃～P became an active species responsible for P release. Noticeably, between the two parts divided by this threshold, the differences in abundance of inorganic phosphorus solubilizing bacteria (IPB) and organic phosphorus mineralizing bacteria (OPB) were insignificant and the dominant IPB species clustered together. By contrast, OPB was distinguished from each other, whose dominant species isolated from the part with higher CaCO₃～P content, namely Novosphingobium sp., exhibited a stronger ability to solubilize CaCO₃～P. Shortly, with lower content, CaCO₃～P tends to stabilize P in sediment; while with higher content or under eutrophic condition, it shifted into P source, with some OPB species becoming the main factors to drive its release.     

Phosphorus fractions and alkaline phosphatase activity in sediments of a large eutrophic Chinese lake (Lake Taihu)

Spatial, vertical, and seasonal variations in phosphorus fractions and in alkaline phosphatase activity (APA) were investigated in sediments in a large-shallow eutrophic Chinese lake (Lake Taihu) in 2003–2004. The phosphorus content was highest in the most seriously polluted lake area. Iron-bound phosphorus (Fe(OOH)～P) dominated (47% on average) among the phosphorus fractions determined according to Golterman (Hydrobiologia 335:87–95, 1996). Notably, organically-bound P comprised a further significant additional portion (acid-soluble + hot NaOH-extractable organic P = 25%), which was highest at the most polluted sites. The Fe(OOH)～P content was the lowest in spring (April, 2004), suggesting that degradation of organic matter led to the release of iron-bound phosphates. Sediment APA showed a significant positive relationship with both organically-bound P and Fe(OOH)～P. Consequently, organically-bound P is an important portion of the sediment phosphorus in Lake Taihu. It is mainly derived from freshly-settled autochthonous particles and from external discharges. Organically-bound P induces APA and may lead to the release of bioavailable phosphates from the organic sediments, thereby accelerating lake eutrophication.     

Extracellular phosphatase activity in sediments of the Breitenbach,a Central European mountain stream

Activity of extracellular phosphatases (phosphomonoesterases) was measured in sandy streambed sediments of the Breitenbach, a small unpolluted upland stream in Central Germany. Fluorigenic 4-methylumbelliferyl phosphate served as a model substrate. Experiments were conducted using sediment cores in a laboratory simulation of diffuse groundwater discharge through the stream bed, a natural process occurring in the Breitenbach as well as many other streams.Streambed sediments contained high levels of particulate phosphorus, but concentrations of dissolved phosphorus in the interstitial water were 3 to 4 orders of magnitude lower. These interstitial concentrations were similar to those in the stream and groundwater. Extracellular phosphatase activity was high in the streambed sediments. These enzymes probably contribute significantly to the flux of phosphorus in sediment by hydrolyzing phosphomonoesters, making free phosphate available to the sediment microorganisms.Factors influencing the kinetic parameters V _max (maximum activity) and apparent K _m (enzyme affinity) of phosphatase were discharge rates of water through the sediment, water quality (ground- or stream water), and substrate (phosphomonoesters) as well as dissolved ortho-phosphate concentrations. Enzymes are supposed to be effective at limiting substrate concentrations, where, in this study, changes in discharge rates had little influence on rates of hydrolysis. Higher V _max and lower K _m values were found during percolation of groundwater through the sediment cores, compared with stream water. This indicates that rates of hydrolysis were higher with groundwater, both at substrate limitation and at substrate saturation. This was probably a consequence of the lower levels of dissolved ortho-phosphate in the groundwater.     

Salinity-sensitive alkaline phosphatase activity in gills of the blue crab,Callinectes sapidus Rathbun

A levamisole-sensitive (K_i = 0.72 mM) alkaline phosphatase (pH optimum 9.1) and a levamisole-insensitive alkaline phosphatase (pH optimum 7.1) are present in gills of the blue crab Callinectes sapidus. Both enzymes are distinct from ouabain-sensitive ATPase. Specific activity for either phosphatase is greatest in the acinar tissue, which lines the branchial vessels. Histochemical localization of the enzymes confirmed this distribution. Activity of levamisole-sensitive alkaline phosphatase is affected by acclimation salinity. V_max of the levamisole-sensitive alkaline phosphatase is greater in high-salinity crabs than in low-salinity crabs; apparent K_m is not significantly different. The levamisole-sensitive alkaline phosphatase associated with the acinar tissue lining the branchial vessels may modulate the osmoregulatory response in blue crabs.     

Isolation and Characterization of Organic Phosphorus-Mineralizing Bacteria in Sediment of a Chinese Large Shallow Eutrophic Lake (Lake Taihu)

The organic phosphorus mineralizing bacteria (OPB) play an important role in phosphorus cycling in lake sediment, to which less attention has been paid. Monthly sediment samples in 2009 ending in October, together with the samples from different seasons (May, July, October, and December) in 2008, were collected at 6 sites in a Chinese large shallow eutrophic lake (Lake Taihu). The sediment OPB numbers ranged from 2.2 × 10⁶ to 1.79 × 10⁸ cells g^?1 (dry weight) at different sampling sites and in different seasons, with the average being 3.88 × 10⁷ cells g^?1 (dry weight). Its number was highest at the most polluted site and peaked in spring and summer, which can be explained by the enrichment of organic matter in sediment. Furthermore, there existed a significant positive relationship between the OPB numbers and alkaline phosphatase activities in the sediment. The 6 OPB strains isolated from the sediment were distinct in terms of their colony morphology on the yolk agar, biochemical characteristics and phosphorus release abilities. According to the 16S rDNA sequences, these OPB belong to Bacillus cereus, Stenotrophomonas maltophilia, Stenotrophomonas sp., Bacillus cereus, Xanthomonas sp., Pseudomonas sp. They were distinguished from the OPB species recorded in a Chinese small shallow eutrophic lake whose sediment organic content was remarkably higher. Taken together, organic matter shaped the OPB community not only quantitatively but also qualitatively, which in concert facilitated the enzymatic hydrolysis of organic phosphorus in lake sediment.     

Nutrient uptake and alkaline phosphatase (ec 3:1:3:1) activity of emiliania huxleyi (PRYMNESIOPHYCEAE) during growth under n and p limitation in continuous cultures

Emiliania huxleyi (strain L) expressed an exceptional P assimilation capability. Under P limitation, the minimum cell P content was 2.6 fmol P·cell^?1, and cell N remained constant at all growth rates at 100 fmol N·cell^?1. Both, calcification of cells and the induction of the phosphate uptake system were inversely correlated with growth rate. The highest (cellular P based) maximum phosphate uptake rate (V_max^P) was 1400 times (i.e. 8.9 h^?1) higher than the actual uptake rate. The affinity of the P‐uptake system (dV/dS) was 19.8 L·μmol^?1·h^?1 at μ = 0.14 d^?1. This is the highest value ever reported for a phytoplankton species. V_max and dV/dS for phosphate uptake were 48% and 15% lower in the dark than in the light at the lowest growth rates. The half‐saturation constant for growth was 1.1 nM. The coefficient for luxury phosphate uptake (Q_maxt/Q_min) was 31. Under P limitation, E. huxleyi expressed two different types of alkaline phosphatase (APase) enzyme kinetics. One type was synthesized constitutively and possessed a V_max and half‐saturation constant of 43 fmol MFP·cell^?1·h^?1 and 1.9 μM, respectively. The other, inducible type of APase expressed its highest activity at the lowest growth rates, with a V_max and half‐saturation constant of 190 fmol MFP·cell^?1·h^?1 and 12.2 μM, respectively. Both APase systems were located in a lipid membrane close to the cell wall. Under N‐limiting growth conditions, the minimum N quotum was 43 fmol N·cell^?1. The highest value for the cell N‐specific maximum nitrate uptake rate (V_max^N) was 0.075 h^?1; for the affinity of nitrate uptake, 0.37 L·μmol^?1·h^?1. The uptake rate of nitrate in the dark was 70% lower than in the light. N‐limited cells were smaller than P‐limited cells and contained 50% less organic and inorganic carbon. In comparison with other algae, E. huxleyi is a poor competitor for nitrate under N limitation. As a consequence of its high affinity for inorganic phosphate, and the presence of two different types of APase in terms of kinetics, E. huxleyi is expected to perform well in P‐controlled ecosystems.     

Changes in alkaline phosphatase activity and phosphate uptake in P-limited phytoplankton,induced by light intensity and spectral quality

Alkaline phosphatase activity and P uptake were determined in P-limited Dunaliella tertiolecta, Thalassiosira pseudonana, Phaeodactylum tricornumtum, and Prymnesium parvum grown under different light intensities and colors. Both intracellular and extracellular enzyme activities varied with the intensity and quality of light in a species-specific manner. The spectral composition of the light also affected P uptake kinetics. No correlation was found between enzyme activity and V_max both within a species and for pooled data for all four species, indicating that the change in uptake kinetics and enzyme activity was not related to P limitation, but induced by the light conditions. Changes in the optimum N:P ratio induced by light were also not related to P uptake kinetics or enzyme activity. These data suggest that light conditions may in themselves have profound effects on species competition for limiting nutrients. Furthermore, since both alkaline phosphatase activity and P uptake were influenced by the prevailing light conditions we suggest that these parameters be used cautiously when determining the P nutritional status of phytoplankton in nature.Address for reprint requests     

UV-sensitive P compounds: release mechanism, seasonal fluctuation and inhibitory effects on alkaline phosphatase activity in a shallow Chinese freshwater lake (Donghu Lake)

Filtrable phosphorus compounds in a shallow Chinese freshwater lake (Donghu Lake) were fractionated by Sephadex G-25 gel-filtration chromatography. Some portions of those compounds released soluble reactive phosphorus upon irradiation with low dose ultraviolet light. Catalase and a hydroxyl radical scavenger (mannitol) markedly prevented photosensitive phosphorus release. The observed effects may be explained by the action of oxidizing reagents such as hydroxyl radicals, produced in photochemical reactions between UV irradiation and humic substances in the water. There was a strong seasonality in UV-sensitive P (UVSP) release. Michaels constants (K _m) of total alkaline phosphatase in the lake water showed a direct positive relation to UVSP Plot of K _m against the UVSP/phosphomonoester ratio reveals a strong relationship between the two variables. These results suggest that in some situations UVSP may be a competitive inhibitor of alkaline phosphatase activity in the lake. The competitive inhibition of fractionated UVSP on alkaline phosphatase reagent (Sigma) apparently supports this hypothesis.     

Phosphorus speciation in Myall Lake sediment, NSW, Australia

The amount of phosphorus and its fractions in the sediment of Lake Myall, NSW, Australia, was assessed using a sequential extraction technique. Five sedimentary phosphorus reservoirs were measured, namely loosely sorbed phosphorus (NH₄Cl–P), iron associated phosphorus (BD–P), calcium bound phosphorus (HCl–P), metal oxide bound phosphorus (NaOH–P) and residual phosphorus (organic and refractory P, Res-P). Samples were taken from the deep and shallow sites of the lake. During the analysis, the average concentrations of each fraction of phosphorus was calculated. The results depicted that the total phosphorus (TP) content and chemically extractable phosphorus in both fine and coarse sediment fractions from the deep sites of the lake were significantly higher than those of the shallow sites, except for HCl–P extracted from the fine sediment fraction. Sediment TP was also strongly and positively correlated to sediment Fe. The phosphorus in the sediment mainly consisted of BD–P and Res-P, while NH₄Cl–P and HCl–P only contributed a minor part. The rank order of the different phosphorus extracts was similar for the two sites, namely Residual-P > BD–P > NaOH–P > HCl–P > NH₄Cl–P.     

Lake depth rather than fish planktivory determines cladoceran community structure in Faroese lakes – evidence from contemporary data and sediments

1. This study describes the environmental conditions and cladoceran community structure of 29 Faroese lakes with special focus on elucidating the impact of fish planktivory. In addition, long‐term changes in biological structure of the Faroese Lake Heygsvatn are investigated. 2. Present‐day species richness and community structure of cladocerans were identified from pelagial snapshot samples and from samples of surface sediment (0–1 cm). Multivariate statistical methods were applied to explore cladoceran species distribution relative to measured environmental variables. For Lake Heygsvatn, lake development was inferred by cladoceran‐based paleolimnological investigations of a ¹⁴C‐dated sediment core covering the last ca 5700 years. 3. The 29 study lakes were overall shallow, small‐sized, oligotrophic and dominated by brown trout (Salmo trutta). Cladoceran species richness was overall higher in the surface sediment samples than in the snapshot samples. 4. Fish abundance was found to be of only minor importance in shaping cladoceran community and body size structure, presumably because of predominance of the less efficient zooplanktivore brown trout. 5. Canonical correspondence analysis showed maximum lake depth (Z_max) to be the only significant variable in explaining the sedimentary cladoceran species (18 cladoceran taxa, two pelagic, 16 benthic) distribution. Multivariate regression trees revealed benthic taxa to dominate in lakes with Z_max < 4.8 m and pelagic taxa to dominate when Z_max was > 4.8 m. 6. Predictive models to infer Z_max were developed using variance weighted‐averaging procedures. These were subsequently applied to subfossil cladoceran assemblages identified from a ¹⁴C‐dated sediment core from Lake Heygsvatn and showed inferred Z_max to correspond well to the present‐day lake depth. A recent increase in inferred Z_max may, however, be an artefact induced by, for instance, eutrophication.     

Sediment resuspension effects on alkaline phosphatase activity

Sediment cores, including the associated lake water, were collected from a shallow hypereutrophic lake located in central Florida. Alkaline phosphatase activity (APA) was measured as an indicator of potential organic P mineralization. In both the sediment and water columns, APA was mainly associated with particulate matter; < 10% of APA was within the soluble phase. This suggests that for enzymatic hydrolysis to occur the hydrolyzable organic compounds must be in close proximity to the particle-bound enzyme complex. Both total P (TP) and APA decreased with depth in the sediment, whereas soluble reactive P increased in the 20–40 cm fraction. Resuspension of surficial sediments resulted in an immediate increase in APA, total suspended solids, TP, total Kjeldahl N, and total organic C within the overlying water column. However, these concentrations decreased rapidly following cessation of turbulence and settling of the sediments, emphasizing the close association of these parameters with the sediment.     

Kinetic properties, and location of nonspecific phosphomonoesterases in subcellular fractions of fasciola hepatica

Optimal activity was recorded at pH 4.5–5 and pH 9.0–9.5 and specific activity was seen to be 0.013 μmoles of p-nitrophenyl phosphate/min/mg protein at 37 C at pH 4.5 and 0.00169 μmoles at pH 9.0. The ratio of acid to alkaline phosphatase was 7.7:1.0. The K_m for acid phosphatase (EC 3.1.3.2) was 0.5 mM with a V_max of 0.0128 units/mg protein and 0.2mM for alkaline phosphatase (EC 3.1.3.1) with a V_max of 0.00175 units/mg protein. Acid phosphatase activity was optimal at 60 C and alkaline at 37 C. Linearity of enzyme activity was observed with time after the first 15 min of incubation and with homogenate concentration. KCN at 20 mM inhibited 82% of activity at pH 9.0 but also 91.5% activity at pH 4.5. NaF at 10^?2M inhibited 92% of activity at pH 4.5 but had no effect at pH 9.0. The two flukicides rafoxanide and nitroxynil at 20mM had little effect on activity at pH 9.0 and pH 4.5. Enzyme activity at pH 4.5 was found to be greatest in the microsomal fraction with high activity in the lysosomal and soluble fractions. Histochemically, alkaline phosphatase was restricted to the excretory system, vitellaria, and uterus while acid phosphatase was found in the integument and gastrodermis.     

The effect of a shift from macrophyte to phytoplankton dominance on phosphorus forms and burial in the sediments of a shallow hard-water lake

In shallow lakes, increasing phosphorus (P) loading has often been accompanied by a shift from a clear-water, macrophyte-dominated state to a turbid state featuring phytoplankton dominance. The effect of a regime shift on P burial and P fractions in lake sediments, however, is poorly understood. We used sediment cores from a eutrophic hard-water lake (Lake Gollinsee, Germany) that had undergone a regime shift (in approximately 1917) to investigate the effect on the accumulation rate of P and on changes in P forms. The cores were dated using Hg contents and radioisotopes (²¹⁰Pb, ¹³⁷Cs, and ²⁴¹Am). A combination of total organic carbon to total nitrogen ratios (TOC:TN), δ¹³TOC values, X-ray fluorescence calcium (Ca) counts, and sediment colour clearly distinguished sediment layers that were deposited during periods of macrophyte or phytoplankton dominance. The accumulation rate of total P (TP) in the sediments was 1.8 times higher after the regime shift and was associated with changes in the distribution of P fractions. The proportions of loosely-(NH₄Cl-extracted TP) and Ca-(HCl-extracted TP) bound P decreased significantly, whilst the proportions of biogenic P (NaOH-extracted NRP) and aluminium-bound P (NaOH-extracted SRP) increased significantly. A higher dry mass deposition rate, reduced burial of stable Ca-P complexes, and increased contents and proportions of the mobile iron-bound (BD-extracted TP) and biogenic P fractions in the near-surface sediment layers are assumed to have enhanced the internal cycling of P and hence to have helped to maintain a state of phytoplankton dominance.

     

Mobility of phosphorus fractions in the sediments of Lake Balaton

Sediment phosporus was studied by a combination of the fractionation procedure of Hieltjes & Lijklema and the isotopic dilution technique in a mesotrophic (Tihany) and a hypertrophic (Keszthely) basin of Lake Balaton.In the calcareous sediments the largest part of phosphorus was bound to calcium. Iron-bound and residual P showed higher concentrations at Keszthely than at Tihany. There was little loosely adsorbed P at both locations. Vertical differences in P fractions of the sediments were more pronounced at Keszthely than at Tihany. Exchangeability of the fractions decreased in the following sequence: iron-bound > loosely adsorbed > calcium-bound > residual. Phosphorus, particularly in the calcium-bound fraction, was more mobile at Keszthely, and its exchangeability decreased rapidly downwards at both stations. Four times more potentially mobile phosphorus has been accumulated by the upper sediment layer at Keszthely than at Tihany.     

Uptake of phosphate and inorganic nitrogen by a sediment-algal system in a subarctic lake

SUMMARY.

• 1 The uptake of phosphate and inorganic nitrogen by sediment and phytoplankton was studied under natural conditions (1977) and during lake fertilization with phosphorus and nitrogen (1978–79) in Lake Gunillajaure, a small, stratified, subarctic lake in northern Sweden. The experiments were performed in situ in plexiglass cylinders, to which additions of nutrients were made, and the uptake followed by consecutive sampling and analysis of the water phase.
• 2 Additions of HgCl₂ to the experimental vessels reduced the phosphate uptake to the sediment to less than 10% and it could therefore be concluded that the sediment uptake was mainly of biological nature.
• 3 Dark assimilation was 30–40% of that in light. Since light clearly stimulated the sediment uptake the epipelic algae were probably responsible.
• 4 The phosphate uptake to the sediment could be described by Michaelis-Menten kinetics and the calculated constants (V_max, ks) were very alike in 1977 and 1978 but appeared to have increased in 1979.
• 5 The sediment uptake of ammonium and nitrate was very slow indrcating that the epipelic algae were not nitrogen starved.
• 6 Even though the epipelic algae had a potential for efficient uptake of phosphorus, the phytoplankton took up 92–96% of the phosphate added to the lake on each fertilization occasion due to the relatively large water volume in the epilimnion in relation to the bottom area available for the epipelic algae.

     

Prokaryotic extracellular enzymatic activity in relation to biomass production and respiration in the meso- and bathypelagic waters of the (sub)tropical Atlantic

Prokaryotic extracellular enzymatic activity, abundance, heterotrophic production and respiration were determined in the meso- and bathypelagic (sub)tropical North Atlantic. While prokaryotic heterotrophic production (PHP) decreased from the lower euphotic layer to the bathypelagic waters by two orders of magnitude, prokaryotic abundance and cell-specific PHP decreased only by one order of magnitude. In contrast to cell-specific PHP, cell-specific extracellular enzymatic activity (alpha- and beta-glucosidase, leucine aminopeptidase, alkaline phosphatase) increased with depth as did cell-specific respiration rates. Cell-specific alkaline phosphatase activity increased from the intermediate water masses to the deep waters up to fivefold. Phosphate concentrations, however, varied only by a factor of two between the different water masses, indicating that phosphatase activity is not related to phosphate availability in the deep waters. Generally, cell-specific extracellular enzymatic activities were inversely related to cell-specific prokaryotic leucine incorporation. Thus, it is apparent that the utilization of deep ocean organic matter is linked to higher cell-specific extracellular enzymatic activity and respiration and lower cell-specific PHP than in surface waters.     

Oxygen Uptakes Adjusted for Body Composition in Normal‐Weight and Obese Adolescents

Objective: To test whether resting oxygen uptake (Vo₂), submaximal Vo₂, and maximal Vo₂ (Vo_2max) differs between obese adolescents (n = 18; BMI > 30) and a matched normal‐weight control group after adjustment for differences in fat‐free mass (FFM) and fat mass (FM). Research Methods and Procedures: FFM and FM were assessed by DXA. Resting Vo₂, submaximal Vo₂, and Vo_2max were measured by indirect calorimetry. Results: There was no difference in resting Vo₂ between groups after adjusting for FFM and FM. Submaximal Vo₂ did not differ between groups after adjusting for body weight. Percentage Vo_2max and NET Vo₂ (Vo_2max ? resting Vo₂) were significantly higher in the obese group during submaximal exercise, however not after adjusting for body weight. Vo_2max was not significantly different between groups after adjusting for FFM. Discussion: When body compositions are appropriately controlled for, resting Vo₂, submaximal Vo₂, and Vo_2max do not differ between obese and normal‐weight adolescents. These data suggested that the higher relative Vo₂ observed in obese adolescent subjects is due to their higher FM and not to an impaired Vo_2max even though they may be less physically active.     

Effect of iron on early changes in Escherichia coli-induced ascending pyelonephritis in rats

Uptake of d-glucose, l-lysine and l-proline and the kinetic parameters of alkaline phosphatase and γ-glutamyl-transpeptidase were evaluated in renal brush border membrane (BBM) vesicles prepared from control, pyelonephritic and iron-administered pyelonephritic rats. The uptake of d-glucose and amino acids and V_max of both the enzymes studied were found to be altered in pyelonephritic and iron-administered pyelonephritic rats, but changes appeared earlier and more severely in iron-administered infected animals than in other infected animals. These early physiological alterations were accompanied by higher bacterial colonisation in iron-administered rats.     

A comparative study of 5’nucleotidase and alkaline phosphatase in human placenta during development

Activities and a few properties of alkaline phosphatase and 5’-nucleotidase were compared in the developing human placenta. Both the enzymes were mostly membrane-bound and displayed similar developmental patterns with the highest activities at 24/26 weeks of the placenta. L-Phenylalanine, L-tryptophan and L-leucine were inhibitors of alkaline phosphatase, whereas they had no effect on the 5’-nucleotidase. Alkaline phosphatase from a late stage of gestation appeared to be almost heat-stable. An appreciable part of 5’-nucleotidase was also resistant to heat inactivation and this fraction varied with gestational age of the tissue. For both the enzymes, V_max changed without alteringK _m values with periods of gestation. Ca²⁺, Mg²⁺ and Mn²⁺ ions stimulated the alkaline phosphatase activity and Hg²⁺, Zn²⁺, Cu²⁺, Ni²⁺ were inhibitory. 5’-Nucleotidase was not activated by any of these cations. EDTA and Concanavalin A inhibited both the enzymes, although the extent of inhibition was different and also varied with gestation.     

Kinetic characterization of unspecific alkaline phosphatase at different villus sites of rat jejunum

Summary A quantitative histochemical method to determine the apparent Km and V _max values of rat intestinal unspecific alkaline phosphatase at different sites of the villi is described. Naphthol-As-Bi-phosphate (0.025–1.5 mM) is employed as substrate and Fast Blue B as coupling reagent, and the resulting azo-dye in the brush border membrane has an absorbance maximum at 550 nm. The ratio between the absorbance at 550 and 500 nm is constant as calculated from automatically recorded spectra at different intense dye deposits. Its absorbance is a linear function of incubation time up to 3 min and thickness of the slices up to 10 m both with medium (0.5 mM) and high (1.5 mM) substrate concentrations. Using the histochemical assay under comparable conditions in test tube experiments with homogenates of intestinal mucosa an app. Km of 0.26±0.081 mM (weighted regression analysis) and 0.28–0.084 mM (direct linear plotting) is determined, demonstrating an affinity to the histochemical substrate, which is about 10 times higher than for p-Nitro-phenyl-phosphate with the purified enzyme.The results obtained by scanning the total dye deposits along jejunal villi show considerable differences in enzymatic activity between single villi and an increase from the villus base up to the transition between medium and apical villus third. As well in the apical region as at the villus base saturation curves are obtained by determining the relationship between the absorbance and the substrate concentration under standard conditions (slice thickness 10 m, incubation time 3 min, 37°C, pH 8.3). Calculated by weighted regression analysis and direct linear plotting from the absorbance data of six female rats the medium app. kinetic data ±SD from the jejunal villi read as follows. Apical: Km=0.81±0.438 mM, V _max=3.99±1.217 absorbance units (A) and Km=0.87±0.428 mM, V _max=4.02±1.191 A, respectively. Basal: Km=0.82±0.261 mM, V _max=3.26±0.719 A and Km=0.77±0.184 mM, V _max=3.04±0.518 AU, respectively. As demonstrated by factorial analysis of variance only V _max is influenced by the villus position.Supported by the Deutsche Forschungsgemeinschaft GU 184/1