Tropical forest and mangrove history from southeastern Mexico: a 5000 yr pollen record and implications for sea level rise

A 250 cm long core from El Palmar, a swamp area located along the Rio Hondo river in the south of the Yucatan Peninsula, near the Belizean border, reveals the environmental history of the mangrove and tropical forest of the last 5000 years. The period between 5000 and 4600 b.p. shows sandy deposits, which form the early infill and development of the swamp. A medium-statured tropical forest covered the area and members of the Moraceae and Fabacaeae dominated this early forest. The period between 4600 and 4000 b.p. presents a clear change to a mangrove system with Conocarpus erecta and Rhizophora mangle as dominant trees. This vegetational change is due to flooding of the Rio Hondo river, which deposits sediments of high salinity due to higher sea-level. The medium-statured forest became established at some distance from the swamp area. After 4400 b.p. C. erecta appears as the dominant mangrove species and the R. mangle stands are less predominant in the area. The tropical forest was close to the swamp area and was mainly composed of members of the Moraceae, Arecaceae and Fabaceae as dominant taxa of this vegetational mosaic.     

Development and eustatic control of an Upper Jurassic reef complex (Saint Germain-de-Joux,Eastern France)

Summary This study consists of a sedimentological and diagenetical analysis of reef facies from the Upper Kimmeridgian (sensu gallico). The investigated deposits are situated in eastern France, about fifty kilometres west of the city of Geneva (Switzerland). The reef complex is a fine example of vertical development and facies differentiation. It is subdivided into two distinct sequences by a perforated hardground horizon and sand shoals. The onset of the first reef sequence is characterized by a pioneer growth stage followed by up to 20 m of reef-core and-flank facies. Corals forming the reef-core are typically the ramose variety ofCalamophylliopsis flabellum. The second reef sequence has a reef-core with an average thickness of about 5 m. Corals, however, display much more varied morphologies, and in some areas massive rudist (Heterodiceras) build-ups occur. Development of the second reef sequence was seriously weakened by a storm which produced a 2 m thick accumulation of coral rubble. A shallowing-upwards trend gradually leads to the formation of beach deposits, followed by a newly detected black-pebble horizon. Diagenesis is an important aspect of the reef complex. Especially noteworthy is the dolomitization of certain horizons. At the base of the reef formation, the passage of the phreatic mixing zone provoked invasive dolomitization in large irregular patches (probably deposits richer in Mg-calcite). Some of the beds above the black-pebble horizon, in particular a deposit of accumulated microbial mats, are also dolomitized. In this case, dolomitization is stratiform and is interpreted as having precipitated under conditions of evaporative pumping. The sedimentary record clearly shows the imprint of eustasy. The reef complex was initiated during a transgressive cycle and the hardground found between the two reef sequences is interpreted as a maximum flooding surface (mfs). At the top of the sequence, the horizon overlain by the black-pebble conglomerate is believed to represent the new sequence boundary SB140. Other significant features identified from the St. Germain-de-Joux deposits include the discovery of a new foraminifera,Troglotella incrustans, which is only marginally covered here but is the topic of another paper (Wernli & Fookes, 1992); the subdivision of the first coralligenous level defined byPelletier (1953) into two reef sequences; and a proposition to redefine the ‘Calcaires de la Semine’ (Bernier, 1984). The investigations carried out in the past on the Kimmeridgian deposits in the area of St. Germain-de-Joux were mostly based on stratigraphy and palaeontology. These reefs are among the finest known in the Jura Mountains, but no thorough study had been made on their sedimentological aspects. The aim of this study is to fill this void and also to clarify the more confusing aspects of local stratigraphy (paper based onFookes, 1991).     

Intracellular compartmentation of two enzymes of berberine biosynthesis in plant cell cultures

Out of the eight enzymes involved in the biosynthesis of the isoquinoline alkaloid berberine, at least, two enzymes, berberine bridge enzyme and (S)-tetrahydroprotoberberine oxidase, are exclusively located in a vesicle with a specific gravity of =1.14 g·cm^–3 as shown by direct enzymatic assay as well as immunoelectrophoresis. Electronmicroscopic examination of the enzyme-containing particulate preparation from Berberis wilsoniae var. subcaulialata cultured cells demonstrated that it is composed mainly of membranous vesicles. The protein composition of this preparation reveals the presence of only about 20 separable proteins, of which two major ones are berberine bridge enzyme and (S)-tetrahydroprotoberberine oxidase. Incubation of these vesicles with the substrate (S)-reticuline in the presence and absence of S-adenosyl-l-methionine leads to the formation of a red product which was identified as dehydroscoulerine. If the cytoplasmic enzyme S-adenosyl-l-methionine:(S)-scoulerine-9-O-methyltransferase is added to the vesicle preparation in the presence of (S)-reticuline and S-adenosyl-l-methionine, not dehydroscoulerine but columbamine, the immediate precursor of berberine is formed. Some of the quaternary alkaloids are located inside the vesicles; fusion of these vesicles leads to vacuoles containing the quaternary alkaloids. These vesicles are the first highly specific and unique compartment serving only alkaloid biosynthesis; they are found in members of four different plant families and in cell cultures as well as in differentiated tissue.Abbreviations BBE berberine bridge enzyme - STOX (S)-tetrahydroprotoberberine oxidase Dedicated to Professor Karl Decker, Freiburg, on the occasion of his 60^th birthday     

Cytochemical localization and function of the 3-linked glucan callose in the developing cotton fibre cell wall

Summary Several recent biochemical studies concerning the hemicellulosic content of the developing cotton fibre wall have pointed to an important increase of 1,3-linked glucans at the onset of the secondary wall formation and their slow decrease until the end of fibre development (Meinert andDelmer 1977,Huwyler et al. 1978, 1979,Maltby et al. 1979). These almost insoluble glucans are extra-cellular and possibly associated with the S₁ or winding layer, but no other data on their exact localization were given.By means of a specific fluorescence method, using a 0.05% decolourized aniline blue solution, we show that one of these 3-linked glucans,callose, is always localized, independently of the fibre age, in the innermost wall layer bordering the cell lumen, from the onset of the secondary thickening up to the end of fibre development. Some possible roles assumed by these callose deposits are suggested and discussed. They may be involved in the normal mechanism of cellulose biosynthesis, as being effectively consumed by turnover or, more probably, as forming a permanently restored interface or matrix where cellulose microfibrils undergo a sort of maturation and are oriented before their definitive incorporation in the organized cell wall. They are not to be confused with the wound callose deposits which characterize damaged or immature fibres.     

The differential allosteric regulation of two chorismate-mutase isoenzymes of Nicotiana silvestris

The reaction catalyzed by chorismate mutase (EC 5.4.99.5) is a crucial step for biosynthesis of two aromatic amino acids as well as for the synthesis of phenylpropanoid compounds. The regulatory properties of two chorismate-mutase isoenzymes expressed in Nicotiana silvestris Speg. et Comes are consistent with their differential roles in pathway flow routes ending with l-phenylalanine and l-tyrosine on one hand (isoenzyme CM-1), and ending with secondary metabolites on the other hand (isoenzyme CM-2). Isoenzyme CM-1 was very sensitive to allosteric control by all three aromatic amino acids. At pH 6.1, l-tryptophan was a potent allosteric activator (K _a =1.5 M), while feedback inhibition was effected by l-tyrosine (K _i =15 M) or by l-phenylalanine (K_i=15 M). At pH 6.1, all three effectors acted competitively, influencing the apparent K _m for chorismate. All three allosteric effectors protected isoenzyme CM-1 at pH 6.1 from thermal inactivation at 52° C. l-Tryptophan abolished the weak positive cooperativity of substrate binding found with isoenzyme CM-1 only at low pH. At pH 7.2, the allosteric effects of l-tyrosine and l-tryptophan were only modestly different, in striking contrast to results obtained with l-phenylalanine. At pH 7.2 (i) the K _i for l-phenylalanine was elevated over 30-fold to 500 M, (ii) the kinetics of inhibition became non-competitive, and (iii) l-phenylalanine now failed to protect isoenzyme CM-1 against thermal inactivation. l-Phenylalanine may act at different binding sites depending upon the intracellular pH milieu. In-vitro data indicated that the relative ability of allosteric activation to dominate over allosteric inhibition increases markedly with both pH and temperature. The second isoenzyme, CM-2, was inhibited competitively by caffeic acid (K _i =0.2 mM). Aromatic amino acids failed to affect CM-2 activity over a broad range of pH and temperature. Inhibition curves obtained in the presence of caffeic acid were sigmoid, yielding an interaction coefficient (from Hill plots) of n=1.8.Abbreviation DAHP synthase 3-deoxy-d-arabino-heptulosonate 7-phosphate synthase     

The callovian (Middle Jurassic) crinoids from northern Lithuania

Callovian strata in northern Lithuania (Papilė area) have yielded some crinoid taxa[Chariocrinus andreae (Desor),Balanocrinus berchteni Hess —Pugin,B. subteres (Münster inGoldfuss) andIsocrinus nicoleti (Desor)], which have not been described from this area. The only form known previously wasBalanocrinus pentagonalis (Goldfuss).Palaeocomaster jaegeri n. sp. is the first free-living crinoid recorded from the Callovian of eastern Europe. It is characterized by possessing a very low, strongly flattened and narrow radial cavity. A very similar crinoid assemblage is known from the Callovian glacially-derived clays exposed in the Łuków region (eastern Poland), which were originally located near the Baltic Sea during the Middle Jurassic. It is considered that the allochthonous Callovian deposits from Poland are facies equivalents of the deposits known from Lithuania. The sole significant exception is the domination of free-moving comatulids (Comatulida) in the sediments known from the Papilė region, which may suggest that the Lithuanian sea basin was a little shallower than that located farther west in the Baltic area.      

Dasycladales from the Upper Maastrichtian of Salento Peninsula (Puglia, southern Italy)

Summary A rich dasycladalean assemblage, mainly consisting of new taxa, has been discovered in upper Maastrichtian coarse bioclastic limestones of shelf margin facies cropping out along the southeastern coast of Salento peninsula (Puglia, Southern Italy). It consists of 8 species grouped into 6 genera:Cymopolia decastroi Parente 1994;C. barattoloi Parente, 1994;Zittelina fluegeli n.sp;Jodotella koradae (Dieni, Massari & Radoicic, 1983) nov. comb.;Barattoloporella salentina n. gen. n. sp.;Morelletpora dienii n. sp.;Neomeris spp. (two different species). Zittelina fluegeli n. sp. is characterized by an ovoid thallus with calcification made by a calcareous wall enveloping only the proximal part of the branches (except in basal whorls) and by closely packed, and partly coalescent, calcified ampullae arranged all around the median and distal portion of branches. The transferral ofNeomeris (Larvaria) koradae Dieni, Massari & Radoicic, 1983 into the genusJodotella, with the new combinationJodotella koradae, is proposed on the basis of new observations on the number and arrangement of fertile ampullae. The new genusBarattoloporella, type-speciesBarattoloporella salentina n. gen. n. sp., is erected for dasycladalean algae characterized by a segmented thallus. Each segment consists of: a) basal and apical sterile whorls made by primary branches only, b) central fertile whorls made by primary branches bearing in terminal position one fertile ampulla and one or two secondary branches. morelletpora dienii n. sp. is characterized by a segmented thallus with barrel shaped to pear shaped repetitive elements, consisting of simple whorls of first order branches only. Shape of the branches varies from regularly phloiophorous to more or less differentiated in a stalk and a swollen portion, with or without a subterminal constriction. This is by far the most diverse dasycladalean assemblage ever found in the Maastrichtian. Its diversity supports the conclusion that, within the Late Cretaceous, the Maastrichtian represents a maximum in dasycladalean diversity. Its taxonomic composition strenghtens the hypothesis that dasycladaleans were hardly affected by K/T mass extinction.     

Dasycladalean green algae from the Upper Triassic of Mt. Rotonda (Verbicaro Unit, Calabria-Lucania Border, Southern Italy)

Summary A rich and diverse dasycladalean algae association is described from the Upper Triassic succession of Mt. Rotonda (Calabria-Lucania border, Southern Italy). This association consists of:Neoteutloporella rajkae n.sp.,Griphoporella bechst?dti n.sp.,Physoporella zamparelliae n.sp.,Spinaporella andalusica Flügel & Flügel-Kahler, 1984,S.? granadaensis Flügel & Flügel-Kahler, 1984,Chinianella? sp.,Gyroporella sp.,Griphoporella? sp. andPhysoporella aff.leptotheca. Neoteutloporella rajkae n.sp. is characterised by an undulated calcareous skeleton with short acrophore primary laterals bearing a tuft of 4–6 elongate, segmented, trichophore secondary laterals. This species allows to extend back to the Upper Triassic the stratigraphic range of the genusNeoteutloporella, previously known only from Upper Jurassic levels. Griphoporella bechst?dti n.sp. has a cylindrical calcareous skeleton and primary laterals only, consisting of a thin proximal part followed by a swollen portion that pinches out distally and finally opens outward with a cup-like swelling. Physoporella zamparelliae n.sp. is characterised by a calcareous skeleton made by partly welded thin individual sheaths enclosing the laterals. The laterals are piriferous, vertically compressed, roughly triangular both in vertical and in verticillar section. In some specimens they end with a spine-like thin apophysis. This species confirms that the typical Middle Triassic genusPhysoporella survived up into the Norian. The dasycladalean algal association of the Norian of Mt. Rotonda shows some similarities with the algal association found in the Upper Triassic of the Betic Cordillera whereas it is markedly different from the rich association occurring in the Upper Triassic of Sicily and of the Northern Calcareous Alps. This pattern is coupled with a different composition of the platform margin communities: microbial/serpulids bioconstructions in the Upper Triassic of the Calabria-Lucania border and of Alpujarridevs. Dachstein-type reefs in Sicily and the Northern Calcareous Alps. This indicates that the palaeoceanographic and palaeogeographic conditions controlled both the development of the different platform margin and of the different algal assemblages.     

Barbafera carnica Senowbari-Daryan, 1980: A Triassic worm-tube

Summary Barbafera carnica Senowbari-Daryan (1980), a Carnian reef fossil of uncertain systematic position, is redescribed based on extraordinarily preserved material from Carnian reef boulders of the Cassian Formation of the Southern Alps (Dolomites/Italy).Barbafera is interpreted as a worm tube characterized by a complicated wall structure.Barbafera may belong to the family SerpulidaeRafinesque.     

Holocene mangrove dynamics and sea-level changes in northern Brazil, inferences from the Taperebal core in northeastern Pará State

A 450 cm sediment core from Taperebal, in the mangrove region of northeastern Pará State in northern Brazil has been studied through pollen analysis in order to reconstruct mangrove development and dynamics and to infer relative sea-level (RSL) changes during the Holocene. Six AMS radiocarbon dates, which provide a somewhat limited age control with some uncertainties, suggest early and late Holocene deposits interrupted by a hiatus between them. A patchy vegetation of coastal Amazon rain forest, restinga, salt marsh and some mangrove, which was dominated by Avicennia, covered the study area during the early Holocene period. The occurrence of an early Avicennia dominated mangrove phase has not been reported so far from other sites in northern Brazil. During the mid Holocene mangroves mostly replaced the former coastal Amazon rain forest, restinga and some salt marsh vegetation, reflecting the rise in the RSL. Rhizophora trees expanded markedly and Avicennia became rare. In the sediment core there is apparently a gap between the depths of 115 and 85 cm (possibly starting between 5900 and 5750 b.p.). The deposits above 85 cm are of modern age and were probably deposited during the last decades. This gap can be explained by the lowering of the RSL as is shown for other northern Brazilian coastal sites. The deposition of sediments during the last decades suggests that the modern RSL is high compared to other periods in the Holocene. Pollen data from these deposits show that Rhizophora trees dominate the mangrove forests, also indicating a high RSL.     

<Emphasis Type="Italic">Melanopsis</Emphasis> from Al-Qarn,Jordan Valley (Gastropoda: Cerithioidea)

Fossil species ofMelanopsis from a freshwater formation in the Jordan Valley (near Al-Qarn) were investigated and the deposits containing these species are formally described as Al-Qarn Formation. Four species were found:Melanopsis buccinoidea Olivier,M. tchernovi Heller & Sivan,M. costata Olivier andM. aaronsohni Blanckenhorn.Melanopsis costata was represented by two groups, “stepped” and “non-stepped”, the latter differing in its lower figurativity index. Intermediates were found betweenM. buccinoidea andM. tchernovi; they may be hybrids. TheMelanopsis assemblage bridges the faunal gap, in the Jordan Valley, between the 2 Ma lake of ‘Erq el Ahmar on the one hand and the 0.8–1.7 Ma lake of ‘Ubeidiya on the other. This suggests an early Pleistocene age of about 1.8 million years for the Al-Qarn Formation.     

Environmental distribution of trace fossils in the Jurassic of Kachchh (Western India)

Summary Trace fossils occur abundantly in Middle Jurassic rocks of the Kachchh Basin. They are found in environments ranging from beach sequences down to central parts of the basin. For stratinomic reasons, they are particularly well preserved in storm deposits. Their distribution pattern exhibits a clear relationship to the hydrodynamic conditions and, secondarily, to bathymetry, and follows the classic ichnofacies concept ofSeilacher (1967). High energy nearshore areas and submarine shoals are represented by members of the Skolithos ichnofacies such asOphiomorpha nodosa, Arenicolites, Diplocraterion parallelum, andRhizocorallium jenense. The storm-influenced ramp contains both members of the Cruziana ichnofacies (e.g.Rhizocorallium irregulare, Thalassinoides suevicus, Taenidium serpentinum, Chondrites) and the Skolithos ichnofacies (in particularOphiomorpha). The former were produced during interstorm phases, the latter are of post-storm origin. Carbonate ramp environments of low to intermediate energy also contain members of the Cruziana ichnofacies, whilst equivalent siliciclastic environments are characterized by a low-diversity Zoophycos ichnofacies. Low energy basinal environments of fine-grained substrates contain an impoverished Cruziana ichnofacies consisting ofChondrites, Trichichnus andThalassinoides suevicus. 32 ichnotaxa are briefly described, among themSphaerichnus lobatus ichnogen. et ichnosp. nov.     

Uptake of L-leucine by Trout Red Blood Cells and Peripheral Lymphocytes

The uptake of l-leucine by trout red blood cells and peripheral lymphocytes has been analyzed. The present study shows two functionally different Na⁺-independent systems for apolar branched-chain amino acids. They are designated as L systems because they share some properties with the mammalian L system. The carrier present in red blood cells has low K _m values, is trans-stimulable and not stereospecific for leucine uptake; on the other hand, the system present in lymphocytes is stereospecific for leucine uptake and trans-inhibitable. Both carriers are pH sensitive in a similar fashion at low pHs, but there are important differences at higher pH values (above neutrality). These properties are compared with these of the asc systems previously reported in these cells. Received: 2 June 1995/Revised: 7 March 1996     

A monoclonal antibody to feruloylated-(1→4)-β-<Emphasis Type="SmallCaps">d</Emphasis>-galactan

We report the isolation and characterization of a monoclonal antibody, designated LM9, against feruloylated-(14)--d-galactan. This epitope is a structural feature of cell wall pectic polysaccharides of plants belonging to the family Amaranthaceae (including the Chenopodiaceae). Immuno-assays and immunofluorescence microscopy indicated that LM9 binding is specific to samples and cell walls obtained from species belonging to this family. In a series of competitive-inhibition enzyme-linked immunosorbent assays with potential oligosaccharide haptens, the most effective inhibitor was O-[6-O-(trans-feruloyl)--d-galactopyranosyl]-(14)-d-galactopyranose (Gal₂F). LM9 is therefore a useful antibody probe for the analysis of phenolic substitution of cell wall pectic polymers and of cell wall structure in the Amaranthaceae including sugar beet (Beta vulgaris L.) and spinach (Spinacia oleracea L.).Abbreviations DA Degree of acetylation - DM Degree of methyl esterification - ELISA Enzyme-linked immunosorbent assay - IDA Immunodot assay     

Cytochemical identification of arabinogalactan protein in the outer epidermal wall of maize coleoptiles

Artificial carbohydrate antigen (Yariv reagent), fluorescence-labeled -l-fucose-binding lectin, and -D-galactose-binding lectin were used to localize arabinogalactan protein in sections of maize (Zea mays L.) coleoptiles. All three probes bind to cell walls of vascular tissue and the outer epidermis. Intense staining is obtained at the outer and inner faces of the growth-controlling outer epidermal wall. At the inner face of this wall the auxin-inducible osmiophilic particles, hitherto observed only by electron microscope (Kutschera et al. 1987, Planta 170, 168–180), are strongly stained by all three probes and can therefore be identified as deposits of arabinogalactan protein. It is proposed that this proteoglycan acts as an epidermal wallloosening factor in auxin-mediated coleoptile growth.Abbreviation AGP arabinogalactan protein I thank Dr. R. Bergfeld for the electron micrograph of Fig. 13. This work was supported by the Deutsche Forschungsgemeinschaft.     

Extracellular deamination of l-amino acids by Chlamydomonas reinhardtii cells

When grown in the light and in a Tris-acetate phosphate medium, cells of Chlamydomonas reinhardtii Dang. can use the following l-amino acids as a sole nitrogen source: asparagine, glutamine, arginine, lysine, alanine, valine, leucine, isoleucine, serine, methionine, histidine, and phenylalanine, whereas, in the absence of acetate, the cells only used l-arginine. The utilization system in the acetate medium consisted of an extracellular deaminating activity induced by l-amino acids; it took between 10 to 30 h before the system appeared in cells previously grown with ammonium. This deaminase activity was nonspecific, required an organic carbon source for its de-novo synthesis, and was sensitive to high ammonium concentration and light deprivation.Abbreviations HPLC high-performance liquid chromatography - TAP Tris-acetate-phosphate This work was supported by a grant of the CAICYT, Spain. The secretarial assistance of C. Santos and I. Molina is gratefully acknowledged.To whom correspondence should be addressed.     

The Miocene Architectonicidae (Gastropoda) of Chile

Three new species of Architectonicidae Heliacinae,Heliacus (Torinista) chonos, Heliacus (Grandeliacus) antu andSolatisonax bieleri, are described. These include the first reports ofGrandeliacus andSolatisonax from Chile.Solarium australe Philippi, 1887 is an earlier name forHeliacus (Torinista) bahamondei Frassinetti & Covacevich, 1981, but is a junior homonym ofS. australe Philippi, 1849. Type material and new specimens of the five previously described architectonicid species from Chile are described and figured for comparison. Together with other gastropod taxa from the same deposits, Architectonicidae provide evidence for tropical to subtropical water temperatures in central Chile during the early Miocene.     

Transport und Umsatz von Polyalkoholen bei der Hefe Rhodotorula gracilis (glutinis)

Zusammenfassung Die Polyalkohole Sorbitol, d-Mannitol, Ribitol, Xylitol, d-Arabitol, l-Arabitol und Erythritol werden von der obligat aeroben Hefe Rhodotorula gracilis über einen beweglichen Träger in der Zellmembran aufgenommen. Der Transportmechanismus ist aktiv, das erreichte Akkumulationsverhältnis ist jedoch bei allen Polyalkoholen erheblich geringer als bei Monosacchariden. Es nimmt, wie auch bei Monosacchariden, mit steigender Außenkonzentration ab, sogar auf Werte kleiner als 1.Kinetische Daten weisen darauf hin, daß das Trägersystem für Polyalkohole identisch ist mit dem für Monosaccharide, jedoch für Polyalkohole eine wesentlich geringere Affinität und maximale Geschwindigkeit aufweist. Aufgrund des hohen Affinitätsunterschiedes wird die Polyalkoholaufnahme in der Anwesenheit von Monosacchariden unterbunden.Die aufgenommenen Polyalkohole werden im Zellinneren nicht umgesetzt; eine Ausnahme stellen Ribitol und l-Arabitol dar, in deren Anwesenheit ein Abbausystem für Pentitole induziert wird.

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Transport and utilization of alditols in the yeast Rhodotorula gracilis (glutinis) I. Constitutive transport of alditols

The obligate aerobic yeast Rhodotorula gracilis was found to take up the alditols d-glucitol, d-mannitol, ribitol, xylitol, d-arabinitol, l-arabinitol and erythritol by means of a constitutive mobile membrane carrier. This uptake involved active transport, that is, it was dependent on the supply of metabolic energy, leading to the accumulation of alditols inside the cells. The accumulation ratio (intracellular concentration to extracellular concentration, S _i /S _o ) was much lower for alditols than for monosaccharides. As for monosaccharides, this ratio decreased with increasing extracellular concentration, even to values below 1.The kinetic data showed that the carrier system for alditols was identical to that for monosaccharides, though it had a much lower affinity and maximum velocity for alditols. Hence the uptake of alditols was blocked in the presence of monosaccharides.Only ribitol and l-arabinitol were catabolized following enzyme induction. The other alditols were not broken down.

     

The activity of powdery-mildew haustoria after feeding the host cells with different sugars,as measured with a potentiometric cyanine dye

The biotrophic parasite Erysiphe graminis f. sp. hordei produces haustoria within the cells of its host Hordeum vulgare. To determine the physiological activity of these haustoria, the electric potential across the membranes in the mitochondria of the haustorium was studied. The membrane potential was estimated with the fluorescent potentiometric cyanine dye 3,3-dibutyloxacarbocyanine iodide. The addition of depolarizing agents (carbonylcyanide m-chlorophenylhydrazone, 2,4-dinitrophenol or KCN) to infected cells resulted in an increase of fluorescence after the addition of low concentrations or a decrease of fluorescence after the addition of higher concentrations. When the infected host cell was fed with increasing concentrations of d-glucose (25, 50, 75 mM), corresponding decreases of fluorescence were measured immediately in the mitochondria of the fungal haustoria. Sucrose induced a similar reduction of fluorescence about 20 min late. d-Galactose and d-fructose induced a somewhat smaller reduction of fluorescence, l-glucose and d-glucitol had no effect. The results indicate that haustoria take up glucose from the host cells immediately. Sucrose, d-galactose and d-fructose seem to require time to be metabolized before their products reach the fungal haustorium or mitochondria.Abbreviations CCCP carbonylcyanide m-chlorophenylhydrazone - DiOC₄(3) 3,3-dibutyloxacarbocyanine iodide - DNP 2,4-dinitrophenol