CARBONIC ANHYDRASE AND CARBON FIXATION IN COCCOLITHOPHORIDS1

Rates of carbon fixation in coccolithophorids in culture, unlike many other algae, are carbon limited at ambient levels of dissolved inorganic carbon (DIC). Apparently, plants often rely on activity of carbonic anhydrase (CA) to raise the level of CO₂ in cells and achieve carbon saturation. However, CA activities in the coccolithophorids, Coccolithus (= Emiliania) huxleyi Lohmann and Hymenomonas (=Cricosphaera) carterae Braarud, were either not detectable or very low compared to activities in other systems, including other algae, higher plants, and representative animals. Furthermore, additions of CA to medium with 2 mM DIC at pH 8.1 resulted in nearly 30% enhancement of photosynthesis, but not coccolith formation. Although carbon fixation in coccolithophorids can be suppressed by the CA inhibitor acetazolamide, studies of CaCO₃ nucleation revealed a non-specific effect of the inhibitor. Using a 30 min assay based on pH decreases accompanying loss of dissolved. CO₃^2-, inhibition of crystal formation in the absence of CA at 1 mM acetazolamide was demonstrated for decalcified crab carapace, a tissue with which normal CaCo₃ deposition in vitro has been shown. The results suggest only a minor role for CA in coccolithophorids.     

Increased CO<Subscript>2</Subscript> and the effect of pH on growth and calcification of <Emphasis Type="Italic">Pleurochrysis carterae</Emphasis> and <Emphasis Type="Italic">Emiliania huxleyi</Emphasis> (Haptophyta) in semicontinuous cultures

The effects of changes in CO₂ and pH on biomass productivity and carbon uptake of Pleurochrysis carterae and Emiliania huxleyi in open raceway ponds and a plate photobioreactor were studied. The pH of P. carterae cultures increased during day and decreased at night, whereas the pH of E. huxleyi cultures showed no significant diurnal changes. P. carterae coccolith production occurs during the dark period, whereas in E. huxleyi, coccolith production is mainly during the day. Addition of CO₂ at constant pH (pH-stat) resulted in an increase in P. carterae biomass and coccolith productivity, while CO₂ addition lowered E. huxleyi biomass and coccolith production. Neither of these algae could grow at less than pH 7.5. Species-specific diurnal pH and pCO₂ variations could be indicative of significant differences in carbon uptake between these two species. While E. huxleyi has been suggested to be predominantly a bicarbonate user, our results indicate that P. carterae may be using CO₂ as the main C source for photosynthesis and calcification.     

COCCOLITH-ASSOCIATED POLYSACCHARIDES FROM CELLS OF EMILIANIA HUXLEYI (HAPTOPHYCEAE)1

Coccoliths of Emiliania huxleyi (Lohmann) Hay and Mohler, a unicellular calcifying alga, consist of calcite closely associated with an acidic, Ca²⁺-binding polysaccharide. This polysaccharide is thought to play a regulatory role in coccolith synthesis by interfering with CaCO₃ crystallization. Here we show that the polysaccharides from three different strains, A 92, L and 92 D, all inhibit the precipitation of CaCO₃ in vitro to the same extent. The monosaccharide compositions of the A 92 and L polysaccharide are similar. The 92 D material, however, deviates from the other two: it contains significantly lower amounts of methylated sugars and ribose, and elevated levels of rhamnose and galactose. It also contains antigenic determinants not detected in the A 92 and L polysaccharides. In contrast to the latter two macromolecules the 92 D polysaccharide migrates as two bands upon polyacrylamide gel electrophoresis, possibly resulting from complexing with small amounts of protein. The coccolith polysaccharide from L cells, cultured at an elevated growth rate, also migrates as two bands. This phenomenon is due to an increase in molecular size distribution. The results suggest that certain properties of the molecule may be subject to variation without interfering with its function.     

Three Types of Acidic Polysaccharides Associated with Coccolith of Pleurochrysis haptonemofera: Comparison with Pleurochrysis carterae and Analysis Using Fluorescein-Isothiocyanate-Labeled Lectins

In the coccolithophorid microalgae acidic polysaccharides are considered to be involved in the formation of the calcified scale, coccolith. Characteristics of the acidic polysaccharides extracted from the cell surface of the coccolithophorid Pleurochrysis haptonemofera were analyzed. The acidic polysaccharides on the cell surface can be detected by measuring fluorescence of cells after fluorescein-isothiocyanate-labeled lectin staining by flow cytometry. Flow cytometric analyses revealed that the acidic polysaccharides remained on the cell surface even after CaCO₃ in the coccolith was dissolved by lowering pH, but they were extracted by subsequent EDTA or EGTA treatment, suggesting that they are bound not into the CaCO₃ crystals of the coccolith, but onto the surface via Ca²⁺. Analyses of the acidic polysaccharides by anion exchange chromatography, colloidal precipitation with divalent cations, and polyacrylamide gel electrophoresis (PAGE) revealed that P. haptonemofera has 3 types of acidic polysaccharides (Ph-PS-l, -2, and -3). The PAGE patterns suggested that Ph-PS-2 has a repeated structure with a broad range of molecular weight, as in Pleurochrysis carterae, while Ph-PS-1 and -3 contain several minor components in addition to a major component, respectively. The minor components in Ph-PS-1 and -3 that have not been found in P. carterae might be characteristic of P. haptonemofera. Analyses of both the cell surface treated by various concentrations of EDTA and EGTA and the extracts suggested that Ph-PS-2, which is distinguishable by a higher affinity to concanavalin A, is bound onto the coccolith surface more intensely than the other two types of acidic polysaccharides.     

Formation and mosaicity of coccolith segment calcite of the marine algae Emiliania huxleyi

Coccolithophores belong to the most abundant calcium carbonate mineralizing organisms. Coccolithophore biomineralization is a complex and highly regulated process, resulting in a product that strongly differs in its intricate morphology from the abiogenically produced mineral equivalent. Moreover, unlike extracellularly formed biological carbonate hard tissues, coccolith calcite is neither a hybrid composite, nor is it distinguished by a hierarchical microstructure. This is remarkable as the key to optimizing crystalline biomaterials for mechanical strength and toughness lies in the composite nature of the biological hard tissue and the utilization of specific microstructures. To obtain insight into the pathway of biomineralization of Emiliania huxleyi coccoliths, we examine intracrystalline nanostructural features of the coccolith calcite in combination with cell ultrastructural observations related to the formation of the calcite in the coccolith vesicle within the cell. With TEM diffraction and annular dark‐field imaging, we prove the presence of planar imperfections in the calcite crystals such as planar mosaic block boundaries. As only minor misorientations occur, we attribute them to dislocation networks creating small‐angle boundaries. Intracrystalline occluded biopolymers are not observed. Hence, in E. huxleyi calcite mosaicity is not caused by occluded biopolymers, as it is the case in extracellularly formed hard tissues of marine invertebrates, but by planar defects and dislocations which are typical for crystals formed by classical ion‐by‐ion growth mechanisms. Using cryo‐preparation techniques for SEM and TEM, we found that the membrane of the coccolith vesicle and the outer membrane of the nuclear envelope are in tight proximity, with a well‐controlled constant gap of ~4 nm between them. We describe this conspicuous connection as a not yet described interorganelle junction, the “nuclear envelope junction”. The narrow gap of this junction likely facilitates transport of Ca²⁺ ions from the nuclear envelope to the coccolith vesicle. On the basis of our observations, we propose that formation of the coccolith utilizes the nuclear envelope–endoplasmic reticulum Ca²⁺‐store of the cell for the transport of Ca²⁺ ions from the external medium to the coccolith vesicle and that E. huxleyi calcite forms by ion‐by‐ion growth rather than by a nanoparticle accretion mechanism.     

Immunolocalization of an Acid Phosphatase from Pearl Oyster (<Emphasis Type="Italic">Pinctada fucata</Emphasis>) and Its In Vitro Effects on Calcium Carbonate Crystal Formation

Distribution of an acid phosphatase, AcPase I, from pearl oyster (Pinctada fucata) in different tissues was investigated via enzyme activity determination and immunohistochemistry. Positive reactions were observed in sections of digestive gland, base of gill filaments, and epithelia of the outer side of the middle fold and the inner side of the outer fold, which indicated AcPase I might participate in processes besides immune defense, such as calcium metabolism or shell formation. Its effects on CaCO₃ crystal formation were studied in vitro. Results revealed that AcPase I inhibited CaCO₃ precipitation in a dose-dependent manner and had no affinity for calcium. CaCO₃ crystals induced by AcPase I exhibited a cluster needle-like morphology, which proved to be aragonite. The morphology and size of the aragonites varied with different concentrations of AcPase I. Our observations described here may provide important clues to further understanding of the correlations between mineralization and immune defense in the oyster.     

COCCOLITH-ASSOCIATED POLYSACCHARIDES FROM CELLS OF EMILIANIA HUXLEYI (HAPTOPHYCEAE)1

Coccoliths of Emiliania huxleyi (Lohmann) Hay and Mohler, a unicellular calcifying alga, consist of calcite closely associated with an acidic, Ca²⁺-binding polysaccharide. This polysaccharide is thought to play a regulatory role in coccolith synthesis by interfering with CaCO₃ crystallization. Here we show that the polysaccharides from three different strains, A 92, L and 92 D, all inhibit the precipitation of CaCO₃ in vitro to the same extent. The monosaccharide compositions of the A 92 and L polysaccharide are similar. The 92 D material, however, deviates from the other two: it contains significantly lower amounts of methylated sugars and ribose, and elevated levels of rhamnose and galactose. It also contains antigenic determinants not detected in the A 92 and L polysaccharides. In contrast to the latter two macromolecules the 92 D polysaccharide migrates as two bands upon polyacrylamide gel electrophoresis, possibly resulting from complexing with small amounts of protein. The coccolith polysaccharide from L cells, cultured at an elevated growth rate, also migrates as two bands. This phenomenon is due to an increase in molecular size distribution. The results suggest that certain properties of the molecule may be subject to variation without interfering with its function.     

The effect of adenosine triphosphate,magnesium chloride and phospholipids on crystal formation in the demineralized shell-repair membrane of the snail,Helix pomatia L.

Summary The effect of adenosine triphosphate (ATP), magnesium chloride (MgCl₂) and phospholipids on the calcium-binding activity and crystal formation within the decalcified shell-repair membrane of the snail, Helix pomatia, was studied in vitro. The application of ATP produced a characteristic dual effect on calcification: (1) It strongly inhibited the formation of inorganic calcium carbonate (CaCO₃) crystals. (2) It stimulated the development of organic crystalline bodies and induced deposition of amorphous calcium carbonate. The demineralized shell-repair membranes became white and rigid after incubation for 7 days in the medium containing 1.0mM ATP. The inhibitory effect of Mg²⁺ on CaCO₃ crystal formation was diminished by reduction of the concentration of MgCl₂ in the incubation solution. Thus, after incubation for only 24h, 1.0mM MgCl₂ promoted the formation of birefringent CaCO₃ crystals within the repair membranes. The principal effect of phospholipids on the demineralized shell-repair membrane was stimulatory, but after application of phospholipids to the medium, the formation of crystals proceeded slowly. The very large, composite crystals that were formed within the repair membranes showed strong birefringence. In all cases the development of the crystals and the organic crystalline bodies occurred in close vicinity to the amoebocytes. The role of ATP, MgCl₂ and phospholipids in the recalcification of shell-repair membrane is discussed.The author wishes to thank Mrs. E. Hellmén for valuable technical assistance     

Stable isotope fractionation of strontium in coccolithophore calcite: Influence of temperature and carbonate chemistry

Marine calcifying eukaryotic phytoplankton (coccolithophores) is a major contributor to the pelagic production of CaCO₃ and plays an important role in the biogeochemical cycles of C, Ca and other divalent cations present in the crystal structure of calcite. The geochemical signature of coccolithophore calcite is used as palaeoproxy to reconstruct past environmental conditions and to understand the underlying physiological mechanisms (vital effects) and precipitation kinetics. Here, we present the stable Sr isotope fractionation between seawater and calcite (Δ^88/86Sr) of laboratory cultured coccolithophores in individual dependence of temperature and seawater carbonate chemistry. Coccolithophores were cultured within a temperature and a pCO₂ range from 10 to 25°C and from 175 to 1,240 μatm, respectively. Both environmental drivers induced a significant linear increase in coccolith stable Sr isotope fractionation. The temperature correlation at constant pCO₂ for Emiliania huxleyi and Coccolithus braarudii is expressed as Δ^88/86Sr = ?7.611 × 10^?3 T + 0.0061. The relation of Δ^88/86Sr to pCO₂ was tested in Emiliania huxleyi at 10 and 20°C and resulted in Δ^88/86Sr = ?5.394 × 10^?5 pCO₂ – 0.0920 and Δ^88/86Sr = ?5.742 × 10^?5 pCO₂ – 0.1351, respectively. No consistent relationship was found between coccolith Δ^88/86Sr and cellular physiology impeding a direct application of fossil coccolith Δ^88/86Sr as coccolithophore productivity proxy. An overall significant correlation was detected between the elemental distribution coefficient (D_Sr) and Δ^88/86Sr similar to inorganic calcite with a physiologically induced offset. Our observations indicate (i) that temperature and pCO₂ induce specific effects on coccolith Δ^88/86Sr values and (ii) that strontium elemental ratios and stable isotope fractionation are mainly controlled by precipitation kinetics when embedded into the crystal lattice and subject to vital effects during the transmembrane transport from seawater to the site of calcification. These results provide an important step to develop a coccolith Δ^88/86Sr palaeoproxy complementing the existing toolbox of palaeoceanography.     

Light-dependent coccolith formation in the two forms of Coccolithus pelagicus

Summary Two methods were employed for measuring coccolith formation and photosynthesis in coccolithophorids. The first method was based on measurements of ¹⁴C radioactivity of cells on membrane filters before and after acid treatment. The second method involved a conversion of ¹⁴C in coccoliths or whole cells to BaCO₃ prior to counting. It was observed that in determinations of photosynthetic (or total) ¹⁴C by the first method, the count rate produced by a given amount of the isotope was 30–40% lower in the non-motile and motile forms of Coccolithus pelagicus than in C. huxleyi. There was no similarly great discrepancy in determinations of coccolith ¹⁴C.Light-dependent coccolith formation was demonstrated in both forms of C. pelagicus. The non-motile form may deposit several times more carbon in its coccoliths than it assimilates photosynthetically. In the motile form, coccolith carbon amounts to less than 2% of photosynthetic carbon.     

The effect of carbonic anhydrase,urea and urease on the calcium carbonate deposition in the shell-repair membrane of the snail,Helix pomatia L.

Summary The effect of carbonic anhydrase (CA), urea and urease on the CaCO₃ deposition in the shell-repair membrane of the snail, Helix pomatia, was studied by injection of CA separately or in combination with urease. This treatment resulted in increased deposits of CaCO₃ and apparent crystal formation within the shell-repair membranes compared with those of the controls. The reactions to CA combined with urea were not uniform. Formation of organic crystalline structures and dendritic spherulites was observed in some of these membranes, whereas the deposition of CaCO₃ crystals was suppressed. Administration of urea alone inhibited the formation of large CaCO₃ crystals, whereas urease stimulated this process. The reaction of young snails was greater compared to adults. The membranes of young snails contained tighly packed, small CaCO₃ crystals and organic crystalline structures, which indicated increase of the calcifying centra and their successive mineralization. The results support the assumption that carbonic anhydrase and urease enhance the rate of calcium carbonate deposition and crystal formation in Helix pomatia.     

Polyanion-mediated mineralization — assembly and reorganization of acidic polysaccharides in the Golgi system of a coccolithophorid alga during mineral deposition

Summary Immunolocalization of two highly acidic polysaccharides (PS-1 and PS-2) in a calcifying algaPleurochrysis carterae is described throughout the mineralization process, from before crystal nucleation through the cessation of crystal growth. This unicellular coccolithophorid alga is a useful model for mineralization because it produces calcified scales known as coccoliths in homogeneous cell culture. PS-1 and PS-2 were localized in the crystal coats of mature coccoliths and in electron dense Golgi particles. The polyanions are synthesized in medial Golgi cisternae and co-aggregate with calcium ions into discrete 25 nm particles. Particle-laden vesicles bud from cisternal margins and fuse with a coccolith-forming saccule containing an organic oval-shaped scale which forms the base of the future coccolith. The particles are localized on the base before the onset of mineral deposition and are present in the coccolith saccule throughout the period of crystal (CaCO₃) nucleation and growth. During the final phase of coccolith formation, the particles disappear, and the mature crystals acquire an amorphous coat containing PS-1 and PS-2 polysaccharides which remain with the mineral phase after the coccoliths are extruded from the cell. Postulated mechanisms of polyanion-mediated mineralization are reviewed and their relevance to the calcification of coccoliths is addressed.Abbreviations PS-1 polysaccharide one - PS-2 polysaccharide two - BSA bovine serum albumin - SDS sodium dodecyl sulfate - MES 2-(N-morpholino)-ethanesulfonic acid - EDTA ethylenediaminetetraacetic acid - DHA 3-deoxy-lyxo-2-heptulosaric acid - TCA trichloroacetic acid     

Strain improvement of <Emphasis Type="Italic">Sporosarcina pasteurii</Emphasis> for enhanced urease and calcite production

Phenotypic mutants of Sporosarcina pasteurii (previously known as Bacillus pasteurii) (MTCC 1761) were developed by UV irradiation to test their ability to enhance urease activity and calcite production. Among the mutants, Bp M-3 was found to be more efficient compared to other mutants and wild-type strain. It produced the highest urease activity and calcite production compared to other isolates. The production of extracellular polymeric substances and biofilm was also higher in this mutant than other isolates. Microbial sand plugging results showed the highest calcite precipitation by Bp M-3 mutant. Scanning electron micrography, energy-dispersive X-ray and X-ray diffraction analyses evidenced the direct involvement of bacteria in CaCO₃ precipitation. This study suggests that calcite production by the mutant through biomineralization processes is highly effective and may provide a useful strategy as a sealing agent for filling the gaps or cracks and fissures in any construction structures.     

Suitability of the alkalistable carbonic anhydrase from a polyextremophilic bacterium <Emphasis Type="Italic">Aeribacillus pallidus</Emphasis> TSHB1 in biomimetic carbon sequestration

Carbonic anhydrase (CA) was produced from the polyextremophilic (halotolerant, moderately thermophilic and alkaliphilic) bacterium Aeribacillus pallidus TSHB1 isolated from water and sediment samples of Choti Anhoni hot spring of Pipariya, Madhya Pradesh (India), is being reported to be suitable for carbon sequestration. Growth and CA production were inhibited at higher CO₂ concentration (5–10 %). Under optimized culture variables (tryptone 0.8 %, yeast extract 0.08 %, glucose 1 %, micronutrient solution 1 %, inoculums size 1.10 %, agitation 200 at pH 8, and temperature 55 °C), 3.7-fold higher CA production was attained than that under unoptimized conditions. The zymogram analysis of the partially purified CA revealed an activity band corresponding to 32 kDa. The enzyme is stable in the pH range between 8.0 and 11.0 with T _1/2 of 40, 15, and 8 min at 60, 70, and 80 °C, respectively. The CA of A. pallidus displayed a marked enhancement in the rate of CaCO₃ precipitation from aqueous CO₂. The CA-aided formation of CaCO₃ was 42.5 mg mg^?1 protein. Scanning electron microscopy revealed the formation of rhomboid calcite crystals. This is the first report on the production and applicability of CA from the polyextremophilic A. pallidus in carbon sequestration.     

Direct monitoring of the electron pool effect of cytochrome<Emphasis Type="Italic"> c</Emphasis><Subscript>3</Subscript> by highly sensitive EQCM measurements

Cytochrome c₃ from Desulfovibrio vulgaris has four hemes per molecule, and a redox change at the hemes alters the conformation of the protein, leading to a redox-dependent change in the interaction of cytochrome c₃ with redox partners (an electron acceptor or an electron donor). The redox-dependent change in this interaction was directly monitored by the high-performance electrochemical quartz crystal microbalance (EQCM) technique that has been improved to give high sensitivity in solution. In this method, cytochrome c₃ molecules in solution associate electrostatically with a viologen-immobilized quartz crystal electrode as a monolayer, and redox of the associating cytochrome c₃ is controlled by the immobilized viologen. This technique makes it possible to measure the access of cytochrome c₃ to the electrode or repulsion from the electrode, and hence interconversion between an electrostatic complex and an electron transfer complex on the cytochrome c₃ and the viologen as a mass change accompanying a potential sweep is monitored. In addition, simultaneous measurement of a mass change and a potential step reveals that the cytochrome c₃ stores electrons when the four hemes are reduced (an electron pool effect), that is, the oxidized cytochrome c₃ facilitates acceptance of electrons from the immobilized viologen molecule, but the reduced cytochrome c₃ donates the accepted electrons to the viologen with difficulty.     

THE FINE STRUCTURE OF HYMENOMONAS (CRICOSPHAERA) CARTERAE. II. OBSERVATIONS ON SCALE AND COCCOLITH PRODUCTION

The fine structure of the marine coccolithophorid Hymenomonas (Cricosphaera) carterae (Braarud & Fagerland) Manton & Peterfi is reported. Details of the formation of the circular organic body scales are presented. Their formation is shown to be closely linked with the presence of tubules found within the Golgi cisternae. The details of coccolith production are also discussed. The formation of the organic matrix scale appears to be associated with a densely staining organelle, the intracellular coccolith pre-cursor. The precise mechanisms involved in the mineralization of the organic matrix scale is not known but 2 possibilities are discussed. The production of coccoliths in H. carterae is compared with coccolith production in other coccolithophorids that have been investigated finestructurally.     

A mineralogical characterization of biogenic calcium carbonates precipitated by heterotrophic bacteria isolated from cryophilic polar regions

Precipitation of calcium carbonate (CaCO_3(s)) can be driven by microbial activity. Here, a systematic approach is used to identify the morphological and mineralogical characteristics of CaCO_3(s) precipitated during the heterotrophic growth of micro‐organisms isolated from polar environments. Focus was placed on establishing mineralogical features that are common in bioliths formed during heterotrophic activity, while in parallel identifying features that are specific to bioliths precipitated by certain microbial phylotypes. Twenty microbial isolates that precipitated macroscopic CaCO_3(s) when grown on B4 media supplemented with calcium acetate or calcium citrate were identified. A multimethod approach, including scanning electron microscopy, high‐resolution transmission electron microscopy, and micro‐X‐ray diffraction (μ‐XRD), was used to characterize CaCO_3(s) precipitates. Scanning and transmission electron microscopy showed that complete CaCO_3(s) crystal encrustation of Arthrobacter sp. cells was common, while encrustation of Rhodococcus sp. cells did not occur. Several euhedral and anhedral mineral formations including disphenoid‐like epitaxial plates, rhomboid‐like aggregates with epitaxial rhombs, and spherulite aggregates were observed. While phylotype could not be linked to specific mineral formations, isolates tended to precipitate either euhedral or anhedral minerals, but not both. Three anhydrous CaCO_3(s) polymorphs (calcite, aragonite, and vaterite) were identified by μ‐XRD, and calcite and aragonite were also identified based on TEM lattice‐fringe d value measurements. The presence of certain polymorphs was not indicative of biogenic origin, although several mineralogical features such as crystal‐encrusted bacterial cells, or casts of bacterial cells embedded in mesocrystals are an indication of biogenic origin. In addition, some features such as the formation of vaterite and bacterial entombment appear to be linked to certain phylotypes. Identifying phylotypes consistent with certain mineralogical features is the first step toward discovering a link between these crystal features and the precise underlying molecular biology of the organism precipitating them.     

In memoriam

Microcosm experiments were performed to identify the influence of bacterial cell surfaces on the morphology, mineralogy, size and solubility of CaCO₃ precipitated in response to the enzymatic hydrolysis of urea in an artificial groundwater (AGW) by the ureolytic bacteria, Bacillus pasteurii. In each microcosm, B. pasteurii were contained within a cellulose dialysis membrane (10 K Dalton MWCO), resulting in bacteria-inclusive and bacteria-free AGW solution. Urea hydrolysis by B. pasteurii resulted in the production of ammonium and an increase in pH in the whole AGW solution. This initiated predominantly rhombohedral calcite precipitation at the same critical saturation state ( S _critical = 12) in the B. pasteurii-inclusive and bacteria-free zone of the AGW, indicating the mineralogy and morphology of CaCO₃ precipitation is not controlled by B. pasteurii surfaces. However, the temporal evolution of distinctly different lognormal crystal-size-distributions in the B. pasteurii-inclusive and bacteria-free zone of the AGW resulted from identical changes in bulk solution chemistry. Specifically, B. pasteurii increased the size and size variance of crystals, and led to a greater crystal growth rate throughout the experiments, relative to bacteria-free AGW. Calculated crystal solubility (ln K _S0 ) was lower for crystals > 4000 nm in diameter, reflecting smaller molar surface areas. This suggests that the larger crystals generated in the presence of B. pasteurii have a lower affinity for re-dissolution than those generated in the bacteria-free AGW, which may act as a positive feedback to maintain larger crystal sizes in the presence of B. pasteurii. During ureolysis, higher bacterial concentrations may therefore generate larger and less soluble carbonate crystals. This has important implications for the adaptation of bacterial ureolysis as a method for precipitating calcium carbonate and co-precipitating metals and radionuclides in contaminated aquifers.     

Changes in the cell ultrastructure of the haloalkaliphilic endoevaporite cyanobacterium <Emphasis Type="Italic">‘Euhalothece natronophila’</Emphasis> during fossilization

The ultrastructure of the haloalkaliphilic endoevaporite cyanobacterium ‘Euhalothece natronophila’ Z-M001 from the soda Lake Magadi was investigated during the initial stages of fossilization in a model experimental system. The cyanobacterium was cultivated in concentrated carbonate solution supplemented with calcium chloride. It was revealed that the amorphous CaCO₃ formed under these conditions could interact with the cell wall during the first stages of ‘E. natronophila’ calcification. Evidence is presented that the surface layer of the ‘E. natronophila’ envelope, presumably containing polysaccharide and/or (glyco)protein components, can be involved in the adsorption and subsequent crystallization of CaCO₃ with the formation of a massive “shell” embedding the morphologically intact cells. It was established that the ultrastructure of the cell wall and the intrathylakoid space changed during CaCO₃ mineralization. During the later fossilization stages, cells covered by the calcium-containing “shell” were apparently mummified, and mostly retained their original shape. The encapsulation of cyanobacteria in the trona globule was characterized by a different pattern. It probably involved tight binding of the growing crystal to the glycocalyx components that are anchored in the outer membrane. This may result in its detachment from the underlying peptidoglycan layer. The peptidoglycan was retained, and the protoplasts were ultrastructurally similar to the intact ones. Cyanobacteria incorporated in large trona crystals underwent degradation, deformation, and destruction. This accounts for the fact that massive trona deposits of Lake Magadi lack cyanobacterial fossils that are abundant in calcium-containing strata.     

Growth,net photosynthesis and leaf nutrient status of <Emphasis Type="Italic">Fagus crenata</Emphasis> seedlings grown in brown forest soil acidified with H<Subscript>2</Subscript>SO<Subscript>4</Subscript> or HNO<Subscript>3</Subscript> solution

To obtain basic information for evaluating critical loads of acid deposition for protecting Japanese beech forests, growth, net photosynthesis and leaf nutrient status of Fagus crenata seedlings grown for two growing seasons in brown forest soil acidified with H₂SO₄ or HNO₃ solution were investigated. The whole-plant dry mass of the seedlings grown in the soil acidified by the addition of H₂SO₄ or HNO₃ solution was significantly less than that of the seedlings grown in the control soil not supplemented with H⁺ as H₂SO₄ or HNO₃ solution. However, the degrees of reduction in the whole-plant dry mass and net photosynthetic rate of the seedlings grown in the soil acidified by the addition of H⁺ as H₂SO₄ solution at 100 mg l^–1 on the basis of air-dried soil volume (S-100 treatment) were greater than those of the seedlings grown in the soil acidified by the addition of H⁺ as HNO₃ solution at 100 mg l^–1 (N-100 treatment). The concentrations of Al and Mn in the leaves of the seedlings grown in the S-100 treatment were significantly higher than those in the N-100 treatment. A positive correlation was obtained between the molar ratio of (Ca+Mg+K)/(Al+Mn) in the soil solution and the relative whole-plant dry mass of the seedlings grown in the acidified soils to that of the seedlings grown in the control soil. Based on the results, we concluded that the negative effects of soil acidification due to sulfate deposition are greater than those of soil acidification due to nitrate deposition on growth, net photosynthesis and leaf nutrient status of F. crenata, and that the molar ratio of (Ca+Mg+K)/(Al+Mn) in soil solution is a suitable soil parameter for evaluating critical loads of acid deposition in efforts to protect F. crenata forests in Japan.