The evolution of inter-genomic variation in arbuscular mycorrhizal fungi

Contexte: Les champignons mycorhiziens à arbuscules (AMF) établissent des relations symbiotiques avec la plupart des plantes grâce à leurs réseaux d’hyphes qui s’associent avec les racines de leurs hôtes. De précédentes études ont révélé des niveaux de variation génétique extrêmes pour des loci spécifiques permettant de supposer que les AMF peuvent contenir des milliers de noyaux génétiquement divergents dans un même cytoplasme. Si aucun processus de reproduction sexuée n’a jusqu’ici été observé chez ces mycorhizes, on constate cependant que des niveaux élevés de variation génétique peuvent être maintenus à la fois par l’échange de noyaux entre hyphes et par des processus fréquents de recombinaison entre noyaux. Les AMF se propagent par l’intermédiaire de spores qui contiennent chacune un échantillon d’une population initiale de noyaux hétérogènes, directement hérités du mycélium parent. À notre connaissance les AMF sont les seuls organismes qui ne passent jamais par un stade mononucléaire, ce qui permet aux noyaux de diverger génétiquement dans un même cytoplasme. Ces aspects singuliers de la biologie des AMF rendent l’estimation de leur diversité génétique problématique. Ceci constitue un défi majeur pour les écologistes sur le terrain mais également pour les biologistes moléculaires dans leur laboratoire. Au-delà même des problématiques de diversité spécifique, l’amplitude du polymorphisme entre noyaux mycorhiziens est mal connue. Le travail proposé dans ce manuscrit de thèse explore donc les différents aspects de l’architecture génomique singulière des AMF. Résultats L’ampleur du polymorphisme intra-isolat a été déjà observée pour la grande sous-unité d’ARN ribosomal de l’isolat Glomus irregulare DAOM-197198 (précédemment identifié comme G. intraradices) et pour le gène de la polymerase1-like (PLS) de Glomus etunicatum isolat NPI. Dans un premier temps, nous avons pu confirmer ces résultats et nous avons également pu constater que ces variations étaient transcrites. Nous avons ensuite pu mettre en évidence la présence d’un goulot d’étranglement génétique au moment de la sporulation pour le locus PLS chez l’espèce G. etunicatum illustrant les importants effets d’échantillonnage qui se produisaient entre chaque génération de spore. Enfin, nous avons estimé la différentiation génétique des AMF en utilisant à la fois les réseaux de gènes appliqués aux données de séquençage haut-débit ainsi que cinq nouveaux marqueurs génomiques en copie unique. Ces analyses révèlent que la différenciation génomique est présente de manière systématique dans deux espèces (G. irregulare et G. diaphanum). Conclusions Les résultats de cette thèse fournissent des preuves supplémentaires en faveur du scénario d’une différenciation génomique entre noyaux au sein du même isolat mycorhizien. Ainsi, au moins trois membres du genre Glomus, G. irregulare, G. diaphanum and G. etunicatum, apparaissent comme des organismes dont l’organisation des génomes ne peut pas être décrit d’après un modèle Mendélien strict, ce qui corrobore l’hypothèse que les noyaux mycorhiziens génétiquement différenciés forment un pangenome.

Comparative mitochondrial genomics toward understanding genetics and evolution of arbuscular mycorrhizal fungi

Les champignons mycorhiziens arbusculaires (CMA) sont très répandus dans le sol où ils forment des associations symbiotiques avec la majorité des plantes appelées mycorhizes arbusculaires. Le développement des CMA dépend fortement de la plante hôte, de telle sorte qu'ils ne peuvent vivre à l'état saprotrophique, par conséquent ils sont considérés comme des biotrophes obligatoires. Les CMA forment une lignée évolutive basale des champignons et ils appartiennent au phylum Glomeromycota. Leurs mycélia sont formés d’un réseau d’hyphes cénocytiques dans lesquelles les noyaux et les organites cellulaires peuvent se déplacer librement d’un compartiment à l’autre. Les CMA permettent à la plante hôte de bénéficier d'une meilleure nutrition minérale, grâce au réseau d'hyphes extraradiculaires, qui s'étend au-delà de la zone du sol explorée par les racines. Ces hyphes possèdent une grande capacité d'absorption d’éléments nutritifs qui vont être transportés par ceux-ci jusqu’aux racines. De ce fait, les CMA améliorent la croissance des plantes tout en les protégeant des stresses biotiques et abiotiques. Malgré l’importance des CMA, leurs génétique et évolution demeurent peu connues. Leurs études sont ardues à cause de leur mode de vie qui empêche leur culture en absence des plantes hôtes. En plus leur diversité génétique intra-isolat des génomes nucléaires, complique d’avantage ces études, en particulier le développement des marqueurs moléculaires pour des études biologiques, écologiques ainsi que les fonctions des CMA. C’est pour ces raisons que les génomes mitochondriaux offrent des opportunités et alternatives intéressantes pour étudier les CMA. En effet, les génomes mitochondriaux (mt) publiés à date, ne montrent pas de polymorphismes génétique intra-isolats. Cependant, des exceptions peuvent exister. Pour aller de l’avant avec la génomique mitochondriale, nous avons besoin de générer beaucoup de données de séquençages de l’ADN mitochondrial (ADNmt) afin d’étudier les méchanismes évolutifs, la génétique des population, l’écologie des communautés et la fonction des CMA. Dans ce contexte, l’objectif de mon projet de doctorat consiste à: 1) étudier l’évolution des génomes mt en utilisant l’approche de la génomique comparative au niveau des espèces proches, des isolats ainsi que des espèces phylogénétiquement éloignées chez les CMA; 2) étudier l’hérédité génétique des génomes mt au sein des isolats de l’espèce modèle Rhizophagus irregularis par le biais des anastomoses ; 3) étudier l’organisation des ADNmt et les gènes mt pour le développement des marqueurs moléculaires pour des études phylogénétiques. Nous avons utilisé l’approche dite ‘whole genome shotgun’ en pyroséquençage 454 et Illumina HiSeq pour séquencer plusieurs taxons de CMA sélectionnés selon leur importance et leur disponibilité. Les assemblages de novo, le séquençage conventionnel Sanger, l’annotation et la génomique comparative ont été réalisés pour caractériser des ADNmt complets. Nous avons découvert plusieurs mécanismes évolutifs intéressant chez l’espèce Gigaspora rosea dans laquelle le génome mt est complètement remanié en comparaison avec Rhizophagus irregularis isolat DAOM 197198. En plus nous avons mis en évidence que deux gènes cox1 et rns sont fragmentés en deux morceaux. Nous avons démontré que les ARN transcrits les deux fragments de cox1 se relient entre eux par épissage en trans ‘Trans-splicing’ à l’aide de l’ARN du gene nad5 I3 qui met ensemble les deux ARN cox1.1 et cox1.2 en formant un ARN complet et fonctionnel. Nous avons aussi trouvé une organisation de l’ADNmt très particulière chez l’espèce Rhizophagus sp. Isolat DAOM 213198 dont le génome mt est constitué par deux chromosomes circulaires. En plus nous avons trouvé une quantité considérable des séquences apparentées aux plasmides ‘plasmid-related sequences’ chez les Glomeraceae par rapport aux Gigasporaceae, contribuant ainsi à une évolution rapide des ADNmt chez les Glomeromycota. Nous avons aussi séquencé plusieurs isolats de l’espèces R. irregularis et Rhizophagus sp. pour décortiquer leur position phylogénéque et inférer des relations évolutives entre celles-ci. La comparaison génomique mt nous montré l’existence de plusieurs éléments mobiles comme : des cadres de lecture ‘open reading frames (mORFs)’, des séquences courtes inversées ‘short inverted repeats (SIRs)’, et des séquences apparentées aux plasimdes ‘plasmid-related sequences (dpo)’ qui impactent l’ordre des gènes mt et permettent le remaniement chromosomiques des ADNmt. Tous ces divers mécanismes évolutifs observés au niveau des isolats, nous permettent de développer des marqueurs moléculaires spécifiques à chaque isolat ou espèce de CMA. Les données générées dans mon projet de doctorat ont permis d’avancer les connaissances fondamentales des génomes mitochondriaux non seulement chez les Glomeromycètes, mais aussi de chez le règne des Fungi et les eucaryotes en général. Les trousses moléculaires développées dans ce projet peuvent servir à des études de la génétique des populations, des échanges génétiques et l’écologie des CMA ce qui va contribuer à la compréhension du rôle primorial des CMA en agriculture et environnement.

L-glutaminase production by marine fungi

This study presents the L-Glutaminase Production by Marine Fungi. Enzymes are involved in all aspects of biochemical conversion from the simple enzyme or fermentation conversion to the complex techniques in genetic engineering. Enzyme industry is one among the major industries of the world and there exists a great market for enzymes in general. Food industry is recognized as the largest consumer for commercial enzymes (Lon sane and Ramakrishna, 1989). In industry, enzymes are frequently used for process improvement, for instance to enable the utilization of new types of raw materials or for improving the physical properties of a material so that it can be more easily processed. They are the focal point of biotechnological processe. The marine biosphere is one of the richest of the earth's innumerable habitats, yet is one of the least well characterized. The marine biosphere covers more than two third of the world's surface, our knowledge of marine microorganisms, in particular fungi, is still very limited (Molitoris and Schumann, 1986). The results obtained in the present study the following conclusions are drawn. Beauveria bassiana isolated form marine sediment has immense potential as an Industrial organism for production of L-glutaminase as an extracellular enzyme employing either submerged fermentnation or solid state fermentation

Chitinase production by.marine fungi

In this thesis an attempt is made to explore the potential of marine fungi for the production of chitinolytic enzymes and to recognize the ability to hydrolyse native chitin through submerged as well as solid substrate fermentation culture conditions, using wheat bran and shellfish processing waste such as ‘prawn waste’ as solid substrates. Attempt was made to isolate a potential chitinase producing fungus from marine environment and to develop an ideal bioprocess for the production ofchitolytic enzymes.Present study indicate scope for utilization of B. bassiana for industrial production of chitinase using prawn waste as solid substrate employing solid substrate fermentation.

Process Improvement of Coir Pith Degradation Involving White Rot Fungi By Substitution of Urea With Nitrogen Fixing Bacteria and Application of Biodegraded Coir Pith as Plant Growth Medium

In this study, a novel improved technology could be developed to convert the recalcitrant coir pith into environmental friendly organic manure. The standard method of composting involves the substitution of urea with nitrogen fixing bacteria viz. Azotobacter vinelandii and Azospirillum brasilense leading to the development of an improved method of coir pith. The combined action of the microorganisms could enhance the biodegradation of coir pith. In the present study, Pleurotus sajor caju, an edible mushroom which has the ability to degrade coir pith, and the addition of nitrogen fixing bacteria like Azotobacter vinelandii and Azospirillum brasilense could accelerate the action of the fungi on coir pith. The use of these microorganisms brings about definite changes in the NPK, Ammonia, Organic Carbon and Lignin contents in coir pith. This study will encourage the use of biodegraded coir pith as organic manure for agri/horti purpose to get better yields and can serve as a better technology to solve the problem of accumulated coir pith in coir based industries

Studies on arbuscular mycorrhiza (AM) in the Alentejo (Portugal) using pea mutants resistant to AM fungi as a control tool for field conditions

The utilization and management of arbuscular mycorrhiza (AM) symbiosis may improve production and sustainability of the cropping system. For this purpose, native AM fungi (AMF) were sought and tested for their efficiency to increase plant growth by enhanced P uptake and by alleviation of drought stress. Pot experiments with safflower (Carthamus tinctorius) and pea (Pisum sativum) in five soils (mostly sandy loamy Luvisols) and field experiments with peas were carried out during three years at four different sites. Host plants were grown in heated soils inoculated with AMF or the respective heat sterilized inoculum. In the case of peas, mutants resistant to AMF colonization were used as non-mycorrhizal controls. The mycorrhizal impact on yields and its components, transpiration, and P and N uptake was studied in several experiments, partly under varying P and N levels and water supply. Screening of native AMF by most probable number bioassays was not very meaningful. Soil monoliths were placed in the open to simulate field conditions. Inoculation with a native AMF mix improved grain yield, shoot and leaf growth variables as compared to control. Exposed to drought, higher soil water depletion of mycorrhizal plants resulted in a haying-off effect. The growth response to this inoculum could not be significantly reproduced in a subsequent open air pot experiment at two levels of irrigation and P fertilization, however, safflower grew better at higher P and water supply by multiples. The water use efficiency concerning biomass was improved by the AMF inoculum in the two experiments. Transpiration rates were not significantly affected by AM but as a tendency were higher in non-mycorrhizal safflower. A fundamental methodological problem in mycorrhiza field research is providing an appropriate (negative) control for the experimental factor arbuscular mycorrhiza. Soil sterilization or fungicide treatment have undesirable side effects in field and greenhouse settings. Furthermore, artificial rooting, temperature and light conditions in pot experiments may interfere with the interpretation of mycorrhiza effects. Therefore, the myc- pea mutant P2 was tested as a non-mycorrhizal control in a bioassay to evaluate AMF under field conditions in comparison to the symbiotic isogenetic wild type of var. FRISSON as a new integrative approach. However, mutant P2 is also of nod- phenotype and therefore unable to fix N2. A 3-factorial experiment was carried out in a climate chamber at high NPK fertilization to examine the two isolines under non-symbiotic and symbiotic conditions. P2 achieved the same (or higher) biomass as wild type both under good and poor water supply. However, inoculation with the AMF Glomus manihot did not improve plant growth. Differences of grain and straw yields in field trials were large (up to 80 per cent) between those isogenetic pea lines mainly due to higher P uptake under P and water limited conditions. The lacking N2 fixation in mutants was compensated for by high mineral N supply as indicated by the high N status of the pea mutant plants. This finding was corroborated by the results of a major field experiment at three sites with two levels of N fertilization. The higher N rate did not affect grain or straw yields of the non-fixing mutants. Very efficient AMF were detected in a Ferric Luvisol on pasture land as revealed by yield levels of the evaluation crop and by functional vital staining of highly colonized roots. Generally, levels of grain yield were low, at between 40 and 980 kg ha-1. An additional pot trial was carried out to elucidate the strong mycorrhizal effect in the Ferric Luvisol. A triplication of the plant equivalent field P fertilization was necessary to compensate for the mycorrhizal benefit which was with five times higher grain yield very similar to that found in the field experiment. However, the yield differences between the two isolines were not always plausible as the evaluation variable because they were also found in (small) field test trials with apparently sufficient P and N supply and in a soil of almost no AMF potential. This similarly occurred for pea lines of var. SPARKLE and its non-fixing mycorrhizal (E135) and non-symbiotic (R25) isomutants, which were tested in order to exclude experimentally undesirable benefits by N2 fixation. In contrast to var. FRISSON, SPARKLE was not a suitable variety for Mediterranean field conditions. This raises suspicion putative genetic defects other than symbiotic ones may be effective under field conditions, which would conflict with the concept of an appropriate control. It was concluded that AMF resistant plants may help to overcome fundamental problems of present research on arbuscular mycorrhiza, but may create new ones.

Composition and stability of organic matter fractions in soils under different land use regimes

Soil organic matter (SOM) vitally impacts all soil functions and plays a key role in the global carbon (C) cycle. More than 70% of the terrestric C stocks that participate in the active C cycle are stored in the soil. Therefore, quantitative knowledge of the rates of C incorporation into SOM fractions of different residence time is crucial to understand and predict the sequestration and stabilization of soil organic carbon (SOC). Consequently, there is a need of fractionation procedures that are capable of isolating functionally SOM fractions, i.e. fractions that are defined by their stability. The literature generally refers to three main mechanisms of SOM stabilization: protection of SOM from decomposition by (i) its structural composition, i.e. recalcitrance, (ii) spatial inaccessibility and/or (iii) interaction with soil minerals and metal ions. One of the difficulties in developing fractionation procedures for the isolation of functional SOM fractions is the marked heterogeneity of the soil environment with its various stabilization mechanisms – often several mechanisms operating simultaneously – in soils and soil horizons of different texture and mineralogy. The overall objective of the present thesis was to evaluate present fractionation techniques and to get a better understanding of the factors of SOM sequestration and stabilization. The first part of this study is attended to the structural composition of SOM. Using 13C cross-polarization magic-angle spinning (CPMAS) nuclear magnetic resonance (NMR) spectroscopy, (i) the effect of land use on SOM composition was investigated and (ii) examined whether SOM composition contributes to the different stability of SOM in density and aggregate fractions. The second part of the present work deals with the mineral-associated SOM fraction. The aim was (iii) to evaluate the suitability of chemical fractionation procedures used in the literature for the isolation of stable SOM pools (stepwise hydrolysis, treatments using oxidizing agents like Na2S2O8, H2O2, and NaOCl as well as demineralization of the residue obtained by the NaOCl treatment using HF (NaOCl+HF)) by pool sizes, 13C and 14C data. Further, (iv) the isolated SOM fractions were compared to the inert organic matter (IOM) pool obtained for the investigated soils using the Rothamsted Carbon Model and isotope data in order to see whether the tested chemical fractionation methods produce SOM fractions capable to represent this pool. Besides chemical fractionation, (v) the suitability of thermal oxidation at different temperatures for obtaining stable SOC pools was evaluated. Finally, (vi) the short-term aggregate dynamics and the factors that impact macroaggregate formation and C stabilization were investigated by means of an incubation study using treatments with and without application of 15N labeled maize straw of different degradability (leaves and coarse roots). All treatments were conducted with and without the addition of fungicide. Two study sites with different soil properties and land managements were chosen for these investigations. The first one, located at Rotthalmünster, is a Stagnic Luvisol (silty loam) under different land use regimes. The Ah horizons of a spruce forest and continuous grassland and the Ap and E horizons of two plots with arable crops (continuous maize and wheat cropping) were examined. The soil of the second study site, located at Halle, is a Haplic Phaeozem (loamy sand) where the Ap horizons of two plots with arable crops (continuous maize and rye cropping) were investigated. Both study sites had a C3-/C4-vegetational change on the maize plot for the purpose of tracing the incorporation of the younger, maize-derived C into different SOM fractions and the calculation of apparent C turnover times of these. The Halle site is located near a train station and industrial areas, which caused a contamination with high amounts of fossil C. The investigation of aggregate and density fractions by 13C CPMAS NMR spectroscopy revealed that density fractionation isolated SOM fractions of different composition. The consumption of a considerable part (10–20%) of the easily available O-alkyl-C and the selective preservation of the more recalcitrant alkyl-C when passing from litter to the different particulate organic matter (POM) fractions suggest that density fractionation was able to isolate SOM fractions with different degrees of decomposition. The spectra of the aggregate fractions resembled those of the mineral-associated SOM fraction obtained by density fractionation and no considerable differences were observed between aggregate size classes. Comparison of plant litter, density and aggregate size fractions from soil under different land use showed that the type of land use markedly influenced the composition of SOM. While SOM of the acid forest soil was characterized by a large content (> 50%) of POM, which contained high amounts of spruce-litter derived alkyl-C, the organic matter in the biologically more active grassland and arable soils was dominated by mineral-associated SOM (> 95%). This SOM fraction comprised greater proportions of aryl- and carbonyl-C and is considered to contain a higher amount of microbially-derived organic substances. Land use can alter both, structure and stability of SOM fractions. All applied chemical treatments induced considerable SOC losses (> 70–95% of mineral-associated SOM) in the investigated soils. The proportion of residual C after chemical fractionation was largest in the arable Ap and E horizons and increased with decreasing C content in the initial SOC after stepwise hydrolysis as well as after the oxidative treatments with H2O2 and Na2S2O8. This can be expected for a functional stable pool of SOM, because it is assumed that the more easily available part of SOC is consumed first if C inputs decrease. All chemical treatments led to a preferential loss of the younger, maize-derived SOC, but this was most pronounced after the treatments with Na2S2O8 and H2O2. After all chemical fractionations, the mean 14C ages of SOC were higher than in the mineral-associated SOM fraction for both study sites and increased in the order: NaOCl < NaOCl+HF ≤ stepwise hydrolysis << H2O2 ≈ Na2S2O8. The results suggest that all treatments were capable of isolating a more stable SOM fraction, but the treatments with H2O2 and Na2S2O8 were the most efficient ones. However, none of the chemical fractionation methods was able to fit the IOM pool calculated using the Rothamsted Carbon Model and isotope data. In the evaluation of thermal oxidation for obtaining stable C fractions, SOC losses increased with temperature from 24–48% (200°C) to 100% (500°C). In the Halle maize Ap horizon, losses of the young, maize-derived C were considerably higher than losses of the older C3-derived C, leading to an increase in the apparent C turnover time from 220 years in mineral-associated SOC to 1158 years after thermal oxidation at 300°C. Most likely, the preferential loss of maize-derived C in the Halle soil was caused by the presence of the high amounts of fossil C mentioned above, which make up a relatively large thermally stable C3-C pool in this soil. This agrees with lower overall SOC losses for the Halle Ap horizon compared to the Rotthalmünster Ap horizon. In the Rotthalmünster soil only slightly more maize-derived than C3-derived SOC was removed by thermal oxidation. Apparent C turnover times increased slightly from 58 years in mineral-associated SOC to 77 years after thermal oxidation at 300°C in the Rotthalmünster Ap and from 151 to 247 years in the Rotthalmünster E horizon. This led to the conclusion that thermal oxidation of SOM was not capable of isolating SOM fractions of considerably higher stability. The incubation experiment showed that macroaggregates develop rapidly after the addition of easily available plant residues. Within the first four weeks of incubation, the maximum aggregation was reached in all treatments without addition of fungicide. The formation of water-stable macroaggregates was related to the size of the microbial biomass pool and its activity. Furthermore, fungi were found to be crucial for the development of soil macroaggregates as the formation of water-stable macroaggregates was significantly delayed in the fungicide treated soils. The C concentration in the obtained aggregate fractions decreased with decreasing aggregate size class, which is in line with the aggregate hierarchy postulated by several authors for soils with SOM as the major binding agent. Macroaggregation involved incorporation of large amounts maize-derived organic matter, but macroaggregates did not play the most important role in the stabilization of maize-derived SOM, because of their relatively low amount (less than 10% of the soil mass). Furthermore, the maize-derived organic matter was quickly incorporated into all aggregate size classes. The microaggregate fraction stored the largest quantities of maize-derived C and N – up to 70% of the residual maize-C and -N were stored in this fraction.

Fungi.

Guía de hongos del Reino Unido y Europa. Cada hongo está fotografiado en su entorno natural para identificar los comestibles de los venenosos. Hay una escala de cada especie para una indicación exacta de su tamaño.

Geological and fossil evidence.

La historia de la Tierra y de las diferentes formas de vida sobre ella se pueden conocer mediante el estudio de las rocas, los estratos, los fósiles y los restos animales y humanos conservados. Al final del libro hay una pequeña bibliografía y direcciones de páginas web.

Plants and fungi : multicelled life.

Este título pertenece a una serie que ofrece en profundidad una visión de las células en todo el mundo vivo, su estructura y los procesos en que se basa la vida en la Tierra. Examina cómo funcionan las células para formar la gran variedad de plantas y hongos que vemos a nuestro alrededor. Analiza la estructura de una célula vegetal, y señala las formas en que ésta difiere de una típica célula animal. Se muestra cómo se han especializado las células de las plantas para que puedan llevar a cabo diferentes funciones, desde la fotosíntesis hasta la reproducción. También explica las diferencias entre las plantas y hongos, y cómo los hongos y algas pueden unirse para formar líquenes. Tiene índice, glosario, referencias bibliográficas y un cuadro de clasificación del reino vegetal.

Rock and fossil hunter.

Para saber qué buscar, dónde ir, y consejos de expertos sobre las rocas y la búsqueda de fósiles es lo que se ofrece en esta publicación con más de treinta actividades que ayudan a los niños a explorar, observar, y entender el mundo natural que les rodea, de forma educativa y divertida. Incluye una lista del equipo necesario y consejos útiles sobre cómo sacar el máximo provecho del estudio de las rocas y los fósiles. Algunas actividades tiene que realizarse en compañía de adultos y están identificadas con un símbolo. También incluye dos desplegables, que muestran la forma de identificar los principales tipos de rocas, minerales y fósiles que los niños pueden encontrar en los sitios más accesibles.

The role of fungi and bacteria on the organic matter decomposition process in streams: interaction and relevance in biofilms

L'objectiu d'aquest estudi és el d'investigar sobre l'ús de matèria orgànica per part dels fongs i bacteris que colonitzen diferents substrats bentònics en rius Mediterranis i analitzar l'efecte dels factors ambientals i antròpics sobre l'estabilitat estructural i funcional de les comunitats del biofilm. La metodologia emprada en aquest estudi consisteix en: i) anàlisi de la biomassa bacteriana i fúngica, ii) anàlisi de la composició de les comunitats bentòniques (identificació d'hifomicets aquàtics i anàlisi del 16S rDNA bacterià), i iii) anàlisi de l'activitat enzimàtica extracel·lular relacionada amb el reciclatge de matèria orgànica en rius.