Trehalose synthesis from maltose by a thermostable trehalose synthase from Thermus caldophilus

Purified trehalose synthase from Thermus caldophilus GK24 produced 18–86% trehalose from 10 mM–1 M maltose. The enzyme also catalyzed the conversion of ,-trehalose into maltose but did not act on other disaccharides. The yield of trehalose from maltose by this enzyme increased 30% more at 40°C than at 80°C and was independent of the substrate concentration. The maximum yield of ,-trehalose from 10 mM maltose reached 86% at 40°C. In addition, ,-trehalose was also formed from maltose or ,-trehalose at 3.5% yield at 80°C. © Rapid Science Ltd. 1998     

Emission of gaseous nitrogen oxides from an extensively managed grassland in NE Bavaria, Germany.

We analysed the stable isotope composition of emitted N₂O in a one-year field experiment (June 1998 to April 1999) in unfertilized controls, and after adding nitrogen by applying slurry or mineral N (calcium ammonium nitrate). Emitted N₂O was analysed every 2–4 weeks, with additional daily sampling for 10 days after each fertilizer application. In supplementary soil incubations, the isotopic composition of N₂O was measured under defined conditions, favouring either denitrification or nitrification. Soil incubated for 48 h under conditions favouring nitrification emitted very little N₂O (0.024 mol g_dw ^–1) and still produced N₂O from denitrification. Under denitrifying incubation conditions, much more N₂O was formed (0.91 mol g_dw ^–1 after 48 h). The isotope ratios of N₂O emitted from denitrification stabilized at ¹⁵N = –40.8 ± 5.7 and ¹⁸O = 2.7 ± 6.3. In the field experiment, the N₂O isotope data showed no clear seasonal trends or treatment effects. Annual means weighted by time and emission rate were ¹⁵N = –8.6 and ¹⁸O = 34.7 after slurry application, ¹⁵N = –4.6 and ¹⁸O = 24.0 after mineral fertilizer application and ¹⁵N = –6.4 and ¹⁸O = 35.6 in the control plots, respectively. So, in all treatments the emitted N₂O was ¹⁵N-depleted compared to ambient air N₂O (¹⁵N = 11.4 ± 11.6, ¹⁸O = 36.9 ± 10.7). Isotope analyses of the emitted N₂O under field conditions per se allowed no unequivocal identification of the main N₂O producing process. However, additional data on soil conditions and from laboratory experiments point to denitrification as the predominant N₂O source. We concluded (1) that the isotope ratios of N₂O emitted from the field soil were not only influenced by the source processes, but also by microbial reduction of N₂O to N₂ and (2) that N₂O emission rates had to exceed 3.4 mol N₂O m^–2 h^–1 to obtain reliable N₂O isotope data.     

Oligonucleotide formation catalyzed by divalent metal ions. The uniqueness of the ribosyl system

Summary Polymerization of various nucleoside-5-phosphorimidazolides has been conducted in neutral aqueous solution using divalent metal ions as catalysts. Oligonucleotide formation took place from each of the ribonucleoside-5-phosphorimidazolides, ImpC, ImpU, ImpA, ImpG, and ImpI. The yields and distributions of the resulting oligonucleotides varied depending on the difference of the nucleic acid base and the metal ions used. The catalytic effect of divalent metal ions on the formation of oligocytidylates occurred in the following order: Pb²⁺>Zn²⁺>Co²⁺, Mn²⁺>Cd²⁺>Cu²⁺>Ni²⁺>Ca²⁺, Mg²⁺, none >Hg²⁺. The order changes slightly for other types of oligoribonucleotide formation. Oligoribonucleotides up to hexamers were obtained in 35–55% overall yield, when Pb²⁺ ion was used as a catalyst. Zn²⁺ ions yielded oligoribonucleotides up to tetramers in 10–20% overall yield. The resulting oligonucleotides contained mainly 2–5 internucleotide linkages.Little or no oligonucleotide was obtained from nucleoside-5-phosphorimidazolides modified in the sugars, Imp(3-dA), Imp(2-dA), Imp(Ara), Imp(Aris), and Imp(Nep). The results indicate that a ribosyl system is required for the metal ion-catalyzed synthesis of oligonucleotides. Abbreviations. EDTA, ethylenediaminetetraacetic acid; Versenol,N-hydroxyethylethylenediaminetriacetic acid; Tris, tris-(hydroxymethyl)aminomethane; pN (N is A, C, G, U, I, 3-dA, 2-dA, AraA, Aris, or Nep), nucleoside-5-phosphate; Np, nucleoside-2(3)-phosphate; I, inosine; 3-dA, 3-deoxyadenosine; 2-dA, 2-deoxyadenosine; AraA, arabinosyladenine; Aris, aristeromycin; Nep, neplanocin A; ImpN, nucleoside-5-phosphorimidazolide; NppN, P₁,P₂-dinucleoside-5,5-pyrophosphate; (pN)_n (n=2, 3, ...), oligomers of pN, numbers given between a nucleoside and a phosphate indicate the type of internucleotide linkage, e.g., pC₂ p₅C is 5-phosphorylcytidyl-(2–5)-cytidine; , cyclic dimers of pN; BAP, bacterial alkaline phosphatase; N.Pl, nuclease Pl; VPDase, venom phosphodiesterase; HPLC, high pressure liquid chromatography     

Seasonal variation of denitrification rate in Lake Suwa sediment

The seasonal variation of denitrification rate in sediments in the central station of Lake Suwa, Japan, was estimated by the acetylene-inhibition technique from March 20 to December 10, 1994. The denitrification rate ranged from 0 to 1800µmolNm^–2day^–1 and showed a distinct seasonal trend, i.e., relatively high rates in spring and winter, and low or negligible rates in summer. The denitrification rate was well correlated with NO^–₃ concentration in overlying water, suggesting that NO^–₃ in overlying water was the primary controlling factor for denitrification. The annual rate of denitrification was 0.15molNm^–2year^–1. Denitrification removed 5% of the annual nitrogen load from the lake, and this fraction was relatively small compared to the values reported for a variety of aquatic environments. In Lake Suwa, NO^–₃ in the water column was depleted during summer, and this suppressed effective removal of nitrogen from the lake by denitrification.     

Foam behavior of biological media

Summary The surface tension and foaminess of (a) unlimited, (b) substrate limited, and (c) oxygen transfer limited growth media of Hansenula polymorpha were measured using methanol, ethanol or glucose as a substrate.The time dependence of can be described by the Avrami-Überreiter relationship: log (2.3 log V)=n log t+log b, where V = (_O – _eq/(_t – _eq, and _O, _t and _eq are at t_M=0, t_M=t and t_M (equilibrium value).The constants n and b are functions of the fermentation time t_F as long as the growth is unlimited but they are constant in the state of limited growth. With glucose substrate, the foaminess can be presented as a definite function of the time, t_DG, which is necessary to attain _eq. With alcohol as a substrate no definite (t_DG) function was found.Symbols b constant in Eq. (1) - n constant in Eq. (1) - S substrate concentration - T temperature - t_M time h (measured from the beginning of the determination of the surface tension ) - t_F cultivation time h (measured from the time of inoculation) - t_DG time (min) necessary to attain the equilibrium surface tension ) - X dry biomass concentration (gl^–1) - V (_O – _eq)/(_t – _eq) - V_S equilibrium volume of the foam (cm³) - V_G volumetric gas flow rate during the estimation of (cm³ s^–1) - vvm volumetric gas flow rate with regard to the volume of the medium (min^–1) - w_SG superficial gas velocity (cm s^–1) - _m maximum specific growth rate (h^–1) - V_S/V_G foaminess (s) - surface tension, mMm^–1 (milli Newton m^–1) - _O at t_M=0 - _eq equilibrium surface tension ( at t_M) - _t at t_M=t - HP probes from Hansenula polymorpha cultivation - NLG non limited growth - OTLG oxygen transfer limited growth - SLG substrate limited growth     

α-Globin gene deletions associated with αAand αG Philadelphiagenes in an Algerian family that includes two Hb G homozygotes

Summary An Algerian family with a high degree of consanguinity and including two homozygotes for Hb-G Philadelphia is presented. Whether homozygotes or heterozygotes, all subjects displayed microcytosis (with various degrees of poikilocytosis) and a moderately depressed -globin chain synthesis. Hb H and Heinz bodies were absent. DNA mapping revealed the presence of 3.7 kb deletion resulting from the rightward type of recombination event between ₂ and ₁ genes on both the ^A/and the ^G chromosomes. Such data indicate that the –^A/ and –^G/ haplotypes are involved and suggest that the –^G/ haplotype, which is very rare in Algeria, has an African Black origin. In subjects with genotype (–^A/–^G/) or (–^G/–^G/), the output of the remaining genes is sufficiently high to avoid the appearance of Hb H. This situation contrasts with that reported in an Algerian patient, who had a (–^A/–^A/) genotype but who was producing Hb H (Whitelaw et al. 1980). The data collected from this family suggest that the –^A/ haplotypes are heterogeneous in Algerians.     

C-Terminal exchange between Gα o and Gα i3 proteins differently modulates α2A-adrenoceptor activation

Chimeric G proteins, obtained by exchanging their C-terminal portion for that of a G protein from an unrelated class, drive the receptor selectivity to that corresponding to the introduced G protein domain. The _2A-adrenoceptor (_2AAR), which yielded an efficacious and weak [³⁵S]GTPS binding response by respectively G _o and G _i3 protein, was investigated in CHO-K1 cells co-expressing chimeric G proteins for which the six last C-terminal amino acids between G _o and G _i3 proteins, and reciprocally, were permuted. Activation of the chimeric G _{o / i3} protein was highly efficient whereas the G _{i3 / o} protein yielded a weak stimulation. These [³⁵S]GTPS binding responses were not different from their parental wild-type G _o and G _i3 proteins. Similar results were obtained with an _2AAR carrying a facilitating Thr³⁷³Lys mutation in a putative G protein interaction domain. These data indicate that the six terminal G _o protein amino acids do not constitute a major _2AAR interaction domain for G protein activation.     

Partitioning and separation of α-lactalbumin and β-lactoglobulin in polyethylene glycol/ammonium sulphate aqueous two-phase systems

The partition behaviour of -lactalbumin (la) and -lactoglobulin (lg) on PEG/(NH₄)₂SO₄ system was studied. For purified proteins, a partition coefficient of 12.8 for la and 0.34 for lg, with mass recovery yields of 96.7% for la in the upper phase and 83.8% for lg in the lower phase was obtained, in 18% (w/w) PEG 900/14% (w/w) (NH₄)₂SO₄ system, at pH 7. PEG/(NH₄)₂SO₄ system was an economical alternative for the recovery and separation of the two proteins in cheese whey, allowing a 50% reduction in costs. An efficient and inexpensive separation of both proteins in cheese whey could be achieved, by using 16% (w/w) PEG 900/15% (w/w) (NH₄)₂SO₄, at pH 7.5.     

Pioneer and late stage tropical rainforest tree species (French Guiana) growing under common conditions differ in leaf gas exchange regulation,carbon isotope discrimination and leaf water potential

Leaf gas exchange rates, predawn _wp and daily minimum _wm leaf water potentials were measured during a wet-to-dry season transition in pioneer (Jacaranda copaia, Goupia glabra andCarapa guianensis) and late stage rainforest tree species (Dicorynia guianensis andEperua falcata) growing in common conditions in artificial stands in French Guiana. Carbon isotope discrimination () was assessed by measuring the stable carbon isotope composition of the cellulose fraction of wood cores. The values were 2.7 higher in the pioneer species than in the late stage species. The calculated time integratedC _i values derived from the values averaged 281 mol mol^–1 in the pioneers and 240 mol mol^–1 in the late stage species. The corresponding time-integrated values of intrinsinc water-use efficiency [ratio CO₂ assimilation rate (A)/leaf conductance (g)] ranged from 37 to 47 mmol mol^–1 in the pioneers and the values were 64 and 74 mmol mol^–1 for the two late stage species. The high values were associated—at least inJ. copaia—with high maximumg values and with high plant intrinsinc specific hydraulic conductance [Cg/(_wm–_wp], which could reflect a high competitive ability for water and nutrient uptake in the absence of soil drought in the pioneers. A further clear discriminating trait of the pioneer species was the very sensitive stomatal response to drought in the soil, which might be associated with a high vulnerability to cavitation in these species. From a methodological point of view, the results show the relevance of for distinguishing ecophysiological functional types among rainforest trees.     

Travelling waves and dominance of ESS's

We consider a simple two strategy game in which each pure strategy is an evolutionarily stable strategy (ESS). Under the usual dynamical equations, the large-time behaviour of the system will depend upon the initial conditions and the pay-off matrix. If spatial effects are included to give a reaction-diffusion system, we prove that travelling wavefronts can occur which in effect replace one ESS by another. The strength or dominance of each ESS which decides the winner in a precisely defined sense is determined by its pay-off and by its diffusion rate. Good strategies have large pay-offs and small diffusion rates.     

Identification of a GDP-Fuc:Galβ1–3GalNAc-R (Fuc to Gal)α1–2 fucosyltransferase and a GDP-Fuc:Galβ1–4GlcNAc (Fuc to GlcNAc)α1–3 fucosyltransferase in connective tissue of the snailLymnaea stagnalis

Connective tissue of the freshwater pulmonateLymnaea stagnalis was shown to contain fucosyltransferase activity capable of transferring fucose from GDP-Fuc in 1–2 linkage to terminal Gal of type 3 (Gal1–3GalNAc) acceptors, and in 1–3 linkage to GlcNAc of type 2 (Gal1–4GlcNAc) acceptors. The 1–2 fucosyltransferase was active with Gal1–3GalNAc1-OCH₂CH=CH₂ (K _m=12 mM,V _max=1.3 mU ml^–1) and Gal1–3GalNAc (K _m=20 mM,V _max=2.1 mU ml^–1), whereas the 1–3 fucosyltransferase was active with Gal1–4GlcNAc (K _m=23 mM,V _max=1.1 mU ml^–1). The products formed from Gal1–3GalNAc1-OCH₂CH=CH₂ and Gal1–4GlcNAc were purified by high performance liquid chromatography, and identified by 500 MHz¹H-NMR spectroscopy and methylation analysis to be Fuc1–2Gal1–3GalNAc1-OCH₂CH=CH₂ and Gal1–4(Fuc1–3)GlcNAc, respectively. Competition experiments suggest that the two fucosyltransferase activities are due to two distinct enzymes.Abbreviations 2Fuc-T 1–2 fucosyltransferase - 3Fuc-T 1–3 fucosyltransferase - MeO-3Man 3-O-methyl-D-mannose - MeO-3Gal 3-O-methyl-D-galactose     

One-pot enzymatic synthesis of the Galα1→3Galβ1→4GlcNAc sequence within situ UDP-Gal regeneration

The trisaccharide Gal13Gal14GlcNAc1O-(CH₂)₈COOCH₃ was enzymatically synthesized, within situ UDP-Gal regeneration. By combination in one pot of only four enzymes, namely, sucrose synthase, UDP-Glc 4-epimerase, UDP-Gal:GlcNAc 4-galactosyltransferase and UDP-Gal:Gal14GlcNAc 3-galactosyltransferase, Gal13Gal14GlcNAc1O-(CH₂)₈COOCH₃ was formed in a 2.2 µmol ml^–1 yield starting from the acceptor GlcNAc1O-(CH₂)₈COOCH₃. This is an efficient and convenient method for the synthesis of the Gal13Gal14GlcNAc epitope which plays an important role in various biological and immunological processes.     

Phylogeny and evolutionary rates of G protein α subunit genes

Summary Rooted phylogenetic trees for a total of 34 genes encoding the stimulatory (s), inhibitory (i), transducin (t), G_x (x), G_z (z), G₁₁ (11), G₁₂ (12), G₁₃ (13), G₁₆ (16), G_q (q), and other (o) G protein a subunits have been constructed. The analysis shows that the G₁₂ (12 and 13), G_q (11, 16, and q), and G_s (s genes) groups form one cluster, and the G_x (x and z genes), G_i (i genes), G_t (t1 and t2), and G_o (o genes) groups form another cluster. During mammalian evolution, the rates of synonymous substitutions for these genes were estimated to be between 1.77 × 10^–9/site/year and 5.63 × 10^–9/site/year, whereas those of nonsynonymous substitutions were between 0.008 × 10^–9/site/year and 0.067 × 10^–9/site/year. These evolutionary rates are similar to those for histone genes, suggesting equally important biological functions of the G protein a subunits. Offprint requests to: S. Yokoyama     

Characteristics of βA chromosome haplotypes in Japanese

DNA polymorphism patterns linked to the ^A-globin gene were analyzed in healthy Japanese using four different restriction endonucleases. The chromosomes with the ^A-globin gene were mapped through an evaluation of the presence of seven different restriction sites (HincII 5 to ; HindIII in ^G and ^A; HincII in, and 3 to, ₁; AvaII in ; Bam-HI 3 to ). Among 36 chromosomes analyzed, 20 chromosomes had a haplotype of [+–––––+]. Among 55 individuals examined, 7 possessed a homozygous haplotye of [+–––––+]. All Japanese with the ^AT-globin gene had a subhaplotype of [–++–+] 5 to the -globin gene. Their major haplotypes were [–++–+–+] and [–++–++–]. It was expected that the presence of the ^AT-globin gene in Japanese may be deduced from subhaplotypes 5 to the -globin gene.     

Carbon dioxide and water vapor exchange over a <Emphasis Type="Italic">Miscanthus</Emphasis>-type grassland: Effects of development of the canopy

The eddy correlation technique was employed to measure net ecosystem carbon dioxide (CO₂) (NEE) and water vapor exchange (LE) over a C3/C4 co-occurring wet temperate Miscanthus-type grassland in the Kanto plain of Japan in the 1999 growing season. The maximal mean canopy height and maximal leaf area index were 1.0m and 5.5, respectively. The daily maximal LE was approximately 540Wm^–2. The maximum value of daily accumulative LE was 16.3MJday^–1. Daily variation of the decoupling factor () suggests that in the morning LE decoupled with the atmosphere, and the available energy was the major driving force for LE, whereas in the afternoon LE coupled strongly with the atmosphere, and the atmospheric evaporative demand played a critical role in LE. The decline in (from 0.8 to 0.5) with the growing season demonstrates that LE decoupled from the atmosphere in the later growth season. The peak NEE value was 57.4µmolCO₂m^–2s^–1 (the positive value signifies the canopy carbon gain was from the air). The maximal daily integrated NEE was 1.06molCO₂m^–2day^–1 observed during the peak growth stage. A rectangular hyperbolic model was used to describe the relation between daytime NEE and incident photosynthetic photon flux density (PPFD). The net ecosystem CO₂ was not light-saturated up to a PPFD level of 2000µmol m^–2s^–1. The initial slope estimated with the NEE–PPFD response model was approximately 0.042molCO₂mol^–1photon on average. The canopy light compensation point ranged from 210 to 430µmolm^–2s^–1 with an average of approximately 310µmolm^–2s^–1. Both the initial slope and the canopy light compensation point decreased as the canopy senesced. The switch in dominance from C3 to C4 plants played an important role in the canopy fluxes.     

Spatial and temporal variation in soil CO2 efflux in an old-growth neotropical rain forest, La Selva, Costa Rica

Our objectives were to quantify and compare soil CO₂ efflux of two dominant soil types in an old-growth neotropical rain forest in the Atlantic zone of Costa Rica, and to evaluate the control of environmental factors on CO₂ release. We measured soil CO₂ efflux from eight permanent soil chambers on six Oxisol sites. Three sites were developed on old river terraces (old alluvium) and the other three were developed on old lava flows (residual). At the same time we measured soil CO₂ concentrations, soil water content and soil temperature at various depths in 6 soil shafts (3 m deep). Between old alluvium sites, the two-year average CO₂ flux rates ranged from 117.3 to 128.9 mg C m^–2 h^–1. Significantly higher soil CO₂ flux occurred on the residual sites (141.1 to 184.2 mg C m^–2 h^–1). Spatial differences in CO₂ efflux were related to fine root biomass, soil carbon and phosphorus concentration but also to soil water content. Spatial variability in CO₂ storage was high and the amount of CO₂ stored in the upper and lower soil profile was different between old alluvial and residual sites. The major factor identified for explaining temporal variations in soil CO₂ efflux was soil water content. During periods of high soil water content CO₂ emission decreased, probably due to lower diffusion and CO₂ production rates. During the 2-year study period inter-annual variation in soil CO₂ efflux was not detected.     

Increased erythritol production in Torula sp. by Mn2+and Cu2+

The production of erythritol and the erythritol yield from glucose by Torula sp. were improved, in increasing order, by supplementing with 10 mg MnSO₄4H₂O l^–1, 2 mg CuSO₄5H₂O l^–1, and both 10 mg MnSO₄4H₂O l^–1 and 2 mg CuSO₄5H₂O l^–1. Mn²⁺ decreased the intracellular concentration of erythritol, whereas Cu²⁺ increased the activity of erythrose reductase in cells. These results suggest that Mn²⁺ altered the permeability of cells, whereas Cu²⁺ increased the activity of erythrose reductase in cells.     

Sugar conformation of a stereospecific 2′-R or 2′-S deuterium-labeled DNA decamer studied with proton-proton J coupling constants

The sugar conformation of a DNA decamer was studied with proton-proton ³J coupling constants. Two samples, one comprising stereospecifically labeled 2-R-²H for all residues and the other 2-S-²H, were prepared by the method of Kawashima et al. [J. Org. Chem. (1995) 60, 6980–6986; Nucleosides Nucleotides (1995) 14, 333–336], the deuterium labeling being highly stereospecific 99% for all 2-²H, 98% for 2-²H of A, C, and T, and 93% for 2-²H of G). The ³J values of all H1-H2 and H1-H2 pairs, and several H2-H3 and H2-H3 pairs were determined by line fitting of 1D spectra with 0.1–0.2 Hz precision. The observed J coupling constants were explained by the rigid sugar conformation model, and the sugar conformations were found to be between C3-exo and C2-endo with _m values of 26° to 44°, except for the second and 3 terminal residues C2 and C10. For the C2 and C10 residues, the lower fraction of S-type conformation was estimated from J_H1H2 and J_H1H2 values. For C10, the N–S two-site jump model or Gaussian distribution of the torsion angle model could explain the observed J values, and 68% S-type conformation or C1-exo conformation with 27° distribution was obtained, respectively. The differences between these two motional models are discussed based on a simple simulation of J-coupling constants.     

The Use of the [13C]/[12C] Ratio for the Assay of the Microbial Oxidation of Hydrocarbons

The study deals with a comparative analysis of the relative abundances of the carbon isotopes ¹²C and ¹³C in the metabolites and biomass of the Burkholderia sp. BS3702 and Pseudomonas putida BS202-p strains capable of utilizing aliphatic (n-hexadecane) and aromatic (naphthalene) hydrocarbons as sources of carbon and energy. The isotope compositions of the carbon dioxide, biomass, and exometabolites produced during the growth of Burkholderia sp. BS3702 on n-hexadecane (¹³C = –44.6 ± 0.2) were characterized by the values of ¹³C_{CO 2} = –50.2 ± 0.4, ¹³C_biom = –46.6 ± 0.4, and ¹³C_exo = –41.5 ± 0.4, respectively. The isotope compositions of the carbon dioxide, biomass, and exometabolites produced during the growth of the same bacterial strain on naphthalene (¹³C = –21 ± 0.4) were characterized by the isotope effects ¹³C_{CO 2} = –24.1 ± 0.4, ¹³C_biom = –19.2 ± 0.4, and ¹³C_exo = –19.1 ± 0.4, respectively. The possibility of using the isotope composition of metabolic carbon dioxide for the rapid monitoring of the microbial degradation of petroleum hydrocarbons in the environment is discussed.     

Analysis of primary food sources and trophic relationships of aquatic animals in a mangrove-fringed estuary,Khung Krabaen Bay (Thailand) using dual stable isotope techniques

Stable carbon (¹³C) and nitrogen (¹⁵N) isotopes were used to elucidate primary food sources and trophic relationships of organisms in Khung Krabaen Bay and adjacent offshore waters. The three separate sampling sites were mangroves, inner bay and offshore. The ¹³C values of mangrove leaves were –28.2 to –29.4, seagrass –10.5, macroalgae –14.9 to –18.2, plankton –20.0 to –21.8, benthic detritus –15.1 to –26.3, invertebrates –16.5 to –26.0, and fishes –13.4 to –26.3. The ¹⁵N values of mangrove leaves were 4.3 to 5.7, seagrass 4.3, macroalgae 2.2 to 4.4, plankton 5.7 to 6.4 , benthic detritus 5.1 to 5.3, invertebrates 7.2 to 12.2 , and fishes 6.3 to 15.9. The primary producers had distinct ¹³C values. The ¹³C values of animals collected from mangroves were more negative than those of animals collected far from shore. The primary carbon sources that support food webs clearly depended on location. The contribution of mangroves to food webs was confined only to mangroves, but a mixture of macroalgae and plankton was a major carbon source for organisms in the inner bay area. Offshore organisms clearly derived their carbon through the planktonic food web. The ¹⁵N values of consumers were enriched by 3–4 relative to their diets. The ¹⁵N data suggests that some of aquatic animals had capacity to change their feeding habits according to places and availability of foods and as a result, individuals of the same species could be assigned to different trophic levels at different places.