Unravelling the enigmatic origin of calcitic nanofibres in soils and caves: purely physicochemical or biogenic processes?

Calcitic nanofibres are ubiquitous habits of sec- ondary calcium carbonate (CaCO3 ) accumulations observed in calcareous vadose environments. Despite their widespread occurrence, the origin of these nanofeatures remains enig- matic. Three possible mechanisms fuel the debate: (i) purely physicochemical processes, (ii) mineralization of rod-shaped bacteria, and (iii) crystal precipitation on organic templates. Nanofibres can be either mineral (calcitic) or organic in na- ture. They are very often observed in association with needle fibre calcite (NFC), another typical secondary CaCO3 habit in terrestrial environments. This association has contributed to some confusion between both habits, however they are truly two distinct calcitic features and their recurrent asso- ciation is likely to be an important fact to help understanding the origin of nanofibres. In this paper the different hypotheses that currently exist to explain the origin of calcitic nanofibres are critically reviewed. In addition to this, a new hypothe- sis for the origin of nanofibres is proposed based on the fact that current knowledge attributes a fungal origin to NFC. As this feature and nanofibres are recurrently observed together, a possible fungal origin for nanofibres which are associated with NFC is investigated. Sequential enzymatic digestion of the fungal cell wall of selected fungal species demonstrates that the fungal cell wall can be a source of organic nanofibres. The obtained organic nanofibres show a striking morpho- logical resemblance when compared to their natural coun- terparts, emphasizing a fungal origin for part of the organic nanofibres observed in association with NFC. It is further hy- pothesized that these organic nanofibres may act as templates for calcite nucleation in a biologically influenced mineraliza- tion process, generating calcitic nanofibres. This highlights the possible involvement of fungi in CaCO3 biomineraliza- tion processes, a role still poorly documented. Moreover, on a global scale, the organomineralization of organic nanofi- bres into calcitic nanofibres might be an overlooked process deserving more attention to specify its impact on the biogeo- chemical cycles of both Ca and C.

Uranium-enrichment in soils and plants in the vicinity of a pitchblende vein at La Creusaz-Les Marecottes (W of Martigny, Valais, Switzerland)

In the NE part of the Aiguilles Rouges Massif near Martigny, at the eastern contact of the Variscan Vallorcine granite to adjacent gneisses, a series of pitchblende (UO2)-veins occur. This paper determines the level of enrichment and mobility of uranium in soils situated in the vicinity of such a UO2-vein 7 km west of Martigny. Within an area of 50 x 100 m, situated on a relatively steep slope and characterized by a strong gramma-ray anomaly, six soil profiles including their plant cover and a reference soil profile outside the influence of the UO2-vein have been examined. The soil shows pH-values between 4 and 5 and is colluvial. The applied analytical methods for the metal contents include extraction methods, common for soil studies, and bulk analysis performed with X-ray fluorescence and ICP-MS. Uranium contents found in the uppermost 20 cm of the soil profiles vary from 2,500 ppm close to the vein to 15 ppm at the lowermost point of the study area. The reference soil has around 3 ppm uranium. At greater depth (20 to 40 cm) the U-content decreases to about half of the surface values, indicating a vertical transport of uranium within the soil profile. No systematic dependance of uranium-contents to grain size (amount of clay) nor to the amount of organic matter has been found. However, the good correlation between uranium and free iron oxide concentration suggests adsorption of uranium on iron oxy-hydroxides. The ashes of grass and mosses contain up to 90 ppm U, the blueberry and redwood only up to 3 ppm. Our observations suggest that at the surface the uranium is transported by downhill creep (solifluxion) of uranium-rich rock fragments. Liberated by oxidation of the uppermost fragments in a given soil column, the uranium migrates vertically until the conditions are favourable to adsorption onto Fe-oxy-hydroxides. However, as high U-contents of local surface water show, this adsorption does not lead to a significant retention of the uranium.

Measuring mechanical impedance in clayey gravelly soils

Mechanical impedance of clayey and gravelly soils is often needed to interpret experimental results from tillage and other field experiments. Its measurement is difficult with manual and hydraulic penetrometers, which often bend or break in such soils. The purpose of this study was to evaluate the feasibility of a hand-operated "Stolf" impact penetrometer to measure mechanical impedance (soil resistance). The research was conducted in Raleigh, North Carolina, USA (35º 45'N, 78º 42'W, elevation 75 m). Corn was planted on April 19, 1991. Penetrometer measurements were taken on May 10, 1991, in 5 cm intervals to 60 cm at 33 locations on a transect perpendicular to the corn rows in each of four tillage treatments. The data permitted three-dimensional displays showing how mechanical impedance changed with depth and distance along the transect. The impact penetrometer proved to be a useful tool to collect quantitative mechanical impedance data on "hard" clayey and/or gravelly soils which previously were difficult to reliably quantify.

Nitrogen fractions in the microbial biomass in soils of southern Brazil

The reaction of nitrogen compounds with ninhydrin can be used as an indicator of cytoplasmic materials released from microbial cells killed by fumigation. Total-N, ninhydrin-reactive-N (NR-N), ammonium-N (A-N), and α-amino-N in the microbial biomass of soils from the State of Rio Grande do Sul, Brazil, were determined, in 1996, in 0.5 mol L-1 K2SO4 extracts of fumigated and non-fumigated soils. Total-N varied from 20.3 to 104.4 mg kg-1 and the ninhydrin-reactive-N corresponded, in average, to 27% of this. The ninhydrin-reactive-N was made up of 67% ammonium-N and 33% aminoacids with the amino group at the α-carbon position. It was concluded that colorimetric analysis of NR-N and A-N may be used as a direct measure of microbial N in soil. This simple and rapid procedure is adequate for routine analyses.

Calibration of time domain reflectometry (DTR) for soil moisture measurements in cultivated peat soils

Tiivistelmä: TDR-mittausten kalibrointi viljeltyjen turvemaiden kosteuden mittaamiseen

Iron oxides in plinthic soils on sedimentary deposits in northeastern Brazil

This study was conducted to examine the distribution and nature of Fe oxides in plinthic soils on the sediments of Barreiras Group (in the state of Piauí) and Itapecuru Formation (in the state of Maranhão) in Northeastern Brazil. Four pedons were selected: a "plinthic, dystrophic, epieutrophic Gray Podzolic with low activity clay" and a "dystrophic Plinthosol with low activity clay" (both Plinthic Kandiustalfs) on the Barreiras sediments, as well as an "eutrophic Plinthosol with low activity clay" and an "allic Plinthosol with low activity clay" (both Plinthustalfs) on the Itapecuru sediments. Soil samples were fractionated into > 2 mm (pisoliths), water-stable aggregates (plinthite) and matrices; the aggregates and matrices were further fractionated into sand, silt and clay sizes. Dithionite extractable iron (Fe d) and aluminum (Al d), as well as oxalate extractable iron (Fe o), were determined for all fractions, and X-ray diffraction analyses were performed on the pisoliths. It was observed that the Plinthustalfs contain more iron oxides, exhibit more extensive plinthite development and have a greater potential for further plinthite development than the Kandiustalfs. The distribution of values for the Fe d indicates that plinthite formation and induration in all soils were accompanied by an enrichment of Fe oxides in all particle size fractions. This Fe segregation was accompanied by aggregation of particles leading to a greater degree of crystallinity, as indicated by analysis of the ratios of Al d:Fe d. Larger ratios of goethite to hematite, and relatively smaller amounts of silicates in the more mature pisoliths were revealed by X-ray diffraction analysis. Ratios of Al d:Fe d were larger in the Kandiustalfs than in the Plinthustalfs, and also larger than expected for Al-substituted Fe oxides. According to ratios of Al d:Fe d, Fe mobilization in all soils has likely occurred under reducing conditions, facilitated by organic matter on the soil surface.

Nuclear well logging in soils. Calibration of slim hole nuclear tools gamma-gamma and neutron-thermal neutron.

The calculation of elasticity parameters by sonic and ultra sonic wave propagation in saturated soils using Biot's theory needs the following variables : forpiation density and porosity (p, ø), compressional and shear wave velocities (Vp, Vs), fluid density, viscosity and compressibility (Pfi Ilfi Ki), matrix density and compressibility (p" K), The first four parameters can be determined in situ using logging probes. Because fluid and matrix characteristics are not modified during core extraction, they can be obtained through laboratory measurements. All parameters necessitate precise calibrations in various environments and for specific range of values encountered in soils. The slim diameter of boreholes in shallow geophysics and the high cost of petroleum equipment demand the use of specific probes, which usually only give qualitative results. The measurement 'of density is done with a gamma-gamma probe and the measurement of hydrogen index, in relation to porosity, by a neutron probe. The first step of this work has been carried out in synthetic formations in the laboratory using homogeneous media of known density and porosity. To establish borehole corrections different casings have been used. Finally a comparison between laboratory and in situ data in cored holes of known geometry and casing has been performed.

IRF6 is a mediator of the Notch pro-differentiation and tumour suppressive function in keratinocytes

I. Résumé large publicIRF6 est un médiateur de Notch dans la différenciation des kératinocytes et dans sa fonction de suppresseur de tumeursLa peau est l'organe le plus important du corps humain, elle représente chez l'adulte une surface d'environ 1,5 m2 et elle est composée de 2000 milliards de cellules. La peau est composée de plusieurs types cellulaires dont les kératinocvtes. Ces cellules, qui se trouvent dans la couche la plus externe de la peau (Pépiderme), nous protègent de la déshydratation et des agressions externes telles que les infections et rayons ultraviolets. Cette fonction de « barrière » est mise en place grâce à un processus appelé différenciation des kératinocvtes durant lequel les kératinocytes deviennent matures et finalement meurent pour former la couche cornée la plus externe difficilement pénétrable. L'homéostasie tissulaire est un mécanisme qui régule l'équilibre entre prolifération, différentiation et mort cellulaire. Une perturbation de cet équilibre peut mener à la formation d'une tumeur. Il existe différents types de tumeurs de la peau. Nous nous sommes intéressés aux «carcinomes spino-cellulaires» (SCC) qui se développent à partir des keratinocytes en différenciation. Notch est une molécule impliquée positivement dans la différenciation des kératinocytes et joue un rôle prépondérant dans la suppression des tumeurs kératinocytaires comme les SCC dans lesquelles Notch est faiblement exprimé. L'implication de Notch dans la différenciation et dans la carcinogenèse kératinocytaire n'est plus controversée, mais les mécanismes qui sont à la base de ces fonctions restent encore à élucider. IRfF6 est une protéine qui, d'après sa structure, a été classée parmi une famille de régulateurs de la défense de l'organisme (IRFs). Des études ultérieures ont montré qu'IRf 6 n'a pas de rôle dans la réponse immunitaire mais qu'il est plutôt impliqué dans le développement de l'épiderme. Dans ce travail, nous avons établi que, dans les kératinocytes, l'expression d'IPJF6 est contrôlé par Notch et que, comme pour ce dernier, elle est réduite dans les SCCs. De plus, nous avons observé qu'IRF6 régule les mêmes gènes que Notch, et qu'il est en effet un médiateur de la fonction de Notch dans la différenciation des kératinocytes. Parmi les gènes contrôlés par l'axe Notch-IRF6 il y en a trois qui sont sur-exprimés dans les SCCs et qui sont réprimés par cet axe. Il s'agit d'une part d'IRF3 et IRF7, deux autres membres de la famille IRF, et du récepteur EGFR (Epidermal growth factor receptor), un oncogène (un gène impliqué dans l'accélération de la formation de tumeurs). Dans leur ensemble, ces découvertes nous informent sur les mécanismes impliqués dans les fonctions pro-differentiatrice et tumeur suppressive de Notch. Plus encore, elles ouvrent des perspectives intéressantes quant au développement de nouvelles approches thérapeutiques dans le traitement des cancers.II. RésuméLa voie de signalisation de Notch joue un rôle très important dans la différenciation cellulaire et dans la carcinogenèse de nombreux tissus. Dans les kératinocytes, elle agit comme suppresseur de tumeurs, fonction altérée dans les cancers spino cellulaires SCC (tumeurs kératinocytaires) de part la perte d'expression de Notch.Bien que les fonctions pro-différenciatrice et tumeur-suppressive de la voie de signalisation de Notch soient aujourd'hui reconnues, les mécanismes sous-jacents restent à explorer.Dans ce travail, nous montrons qu'IRF6, un membre de la famille des régulateurs de la voie de l'interféron (IRF), ne possédant pas de rôles dans la réponse immunitaire mais essentiel dans le développement de l'épiderme, est d'autant plus exprimé que le kératinocytes sont différenciées alors que son expression est drastiquement diminuée dans les SCC. De façon intéressante, l'expression d'IRF6 durant la différenciation kératinocytaire est directement contrôlée par Notch.Dans les kératinocytes l'expression accrue d'IRP6 a les mêmes effets que 1'activation de la voie de Notch induisant les marqueurs de différentiation des couches supra-basales de l'épiderme et inhibant ceux de la couche basale impliqués dans la prolifération cellulaire. Cependant IRF6 n'est pas impliqué dans la régulation d'autres cibles de Notch, comme p21WAFI/CiP' et Hesl. Comme Notch, IRF6 contrôle négativement l'expression de EGFR et IRF3/7. De ce fait EGFR et IRF3 et IRF7 sont fortement exprimés dans les SCCs humaines où l'expression de Notch et IRF6 est fortement réduite.En conclusion, nous avons démontré qu'IRF6 est une cible directe de Notch/CSL dans les keratinocytes qui medie les effets "non-canonique" de cette voie de signalisation dans la différentiation et dans la suppression tumorale.III. SummaryThe Notch pathway is an important regulator of differentiation and carcinogenesis. In keratinocytes it acts as tumour suppressor and the Notch gene is markedly reduced in keratinocyte-derived squamous cell carcinoma (SCC). While the pro-differentiation and tumour suppressive functions of Notch signalling in keratinocytes are well established, the underlying mechanisms are still poorly understood, We report here that Interferon Regulatory Factor 6 (IRF6), an IRF family member with an essential role in epidermal development, is downmodulated in SCC and is induced in differentiating cells. We observed that the induction of IRF6 in differentiating keratinocytes is suppressed by Notch inhibition. IRF6 expression is also decreased in mice with keratinocyte-specific deletion of the Notch 1/2.Moreover we show that the expression of this gene is induced by Notch activation through a CSL-dependent mechanism even under conditions of protein synthesis inhibition, with endogenous Notch 1 binding to the IRF6 promoter.Increased IRJF6 expression is necessary for the impact of Notch activation on differentiation markers K1 and Involucrin, and proliferation markers integrins and p63, but not on other "canonical" Notch targets like p21WAF1/Cipl, Hes1 and Hey1. Like Notch 1, IRF6 down-modulates expression of epidermal growth factor receptor (EGFR) as well as two other IRF family members, IRF3 and 7, which we previously linked to positive control of p63 expression. Expression of IRF3, IRF7 and EGFR is enhanced in cutaneous squamous cell carcinomas, illustrating a strikingly opposite pattern compared to Notch and IRF6.Thus, IRF6 is a primary Notch target in keratinocytes, which mediates the effects of this pathway on differentiation and contributes to tumor suppression.

Chemical characterization and infrared spectroscopy of soil organic matter from two southern brazilian soils

Soil organic matter from the surface horizon of two Brazilian soils (a Latosol and a Chernosol), in bulk samples (in situ SOM) and in HF-treated samples (SOM), was characterized by elemental analyses, diffuse reflectance (DRIFT) and transmission Fourier transform infrared spectroscopy (T-FTIR). Humic acids (HA), fulvic acids (FA) and humin (HU) isolated from the SOM were characterized additionally by ultraviolet-visible spectroscopy (UV-VIS). After sample oxidation and alkaline treatment, the DRIFT technique proved to be more informative for the detection of "in situ SOM" and of residual organic matter than T-FTIR. The higher hydrophobicity index (HI) and H/C ratio obtained in the Chernosol samples indicate a stronger aliphatic character of the organic matter in this soil than the Latosol. In the latter, a pronounced HI decrease was observed after the removal of humic substances (HS). The weaker aliphatic character, the higher O/C ratio, and the T-FTIR spectrum obtained for the HU fraction in the Latosol suggest the occurrence of surface coordination of carboxylate ions. The Chernosol HU fraction was also oxygenated to a relatively high extent, but presented a stronger hydrophobic character in comparison with the Latosol HU. These differences in the chemical and functional group composition suggest a higher organic matter protection in the Latosol. After the HF treatment, decreases in the FA proportion and the A350/A550 ratio were observed. A possible loss of FA and condensation of organic molecules due to the highly acid medium should not be neglected.

Use of long-term suppressive acyclovir after hematopoietic stem-cell transplantation: impact on herpes simplex virus (HSV) disease and drug-resistant HSV disease.

The effect that long-term use of suppressive acyclovir (ACV) has on both overall herpes simplex virus (HSV) disease and ACV-resistant HSV disease was examined in 3 consecutive cohorts of hematopoietic stem-cell transplant (HCT) recipients (n=2049); cohort 1 received ACV for 30 days after HCT, cohort 2 received it for 1 year after HCT, and cohort 3 received it for an extended period (i.e., >1 year) if the patient's immunosuppression continued after 1 year. The 2-year probability of HSV disease was 31.6% (95% confidence interval [CI], 28.0%-35%) in cohort 1, 3.9% (95% CI, 2.7%-5.2%) in cohort 2, and 0% in cohort 3 (P<.001). ACV-resistant HSV disease developed in 10 patients in cohort 1 (2-year probability, 1.3% [95% CI, 0.8%-2.7%]), in 2 patients in cohort 2 (2-year probability, 0.2% [95% CI, 0%-0.8%]; P=.006), and in 0 patients in cohort 3 (cohort 2 vs. cohort 3, P=.3). Long-term use of suppressive prophylactic ACV appears to prevent the emergence of drug-resistant HSV disease in HCT.

Peanut response to lime and molybdenum application in low pH soils

Liming acid soils is considered to assure the availability of Mo in crops. Additionally, in peanuts (Arachis hypogaea L.) the positive response to liming is associated to a better supply of Ca+2, Mo for the nitrogenase-complex activity, and other non-nitrogen fixing activities of the crop. This study was thus undertaken to assess the effect of lime, Mo, and the lime-Mo interaction on peanut crop, on an acid Ultisol at the Mococa Experimental Station, Instituto Agronômico, São Paulo State, Brazil, from 1987 to 1990. A randomized complete block design with four replications, in a 4 x 4 factorial arrangement, was used in the study. The factors included four lime rates (0, 2, 4, and 6 t ha-1) broadcast and incorporated into the soil, and Mo (0, 100, 200, and 300 g ha-1) as (NH4)2MoO4 applied as seed dressing. Lime was applied once at the beginning of the study while Mo was applied at every planting. Peanut seed cv 'tatu' was used. Significant increase in peanut kernel yield with liming was only evident in the absence of Mo, whereas the peanut response to Mo was observed in two out of the three harvests. A higher yield response (28 % increase) was found when Mo was applied without liming. Soil molybdenum availability, as indicated by plant leaf analysis, increased significantly when lime was applied. Molybdenum fertilization led to higher leaf N content, which in turn increased peanut yield in treatments with smaller lime doses.

Modelling the risk of nitrate leaching from two soils amended with five different biosolids

High N concentrations in biosolids are one of the strongest reasons for their agricultural use. However, it is essential to understand the fate of N in soils treated with biosolids for both plant nutrition and managing the environmental risk of NO3--N leaching. This work aimed at evaluating the risk of NO3--N leaching from a Spodosol and an Oxisol, each one treated with 0.5-8.0 dry Mg ha-1 of fresh tertiary sewage sludge, composted biosolids, limed biosolids, heat-dried biosolids and solar-irradiated biosolids. Results indicated that under similar application rates NO3--N accumulated up to three times more in the 20 cm topsoil of the Oxisol than the Spodosol. However, a higher water content held at field capacity in the Oxisol compensated for the greater nitrate concentrations. A 20 % NO3--N loss from the root zone in the amended Oxisol could be expected. Depending on the biosolids type, 42 to 76 % of the NO3--N accumulated in the Spodosol could be expected to leach down from the amended 20 cm topsoil. NO3--N expected to leach from the Spodosol ranged from 0.8 (composted sludge) to 3.5 times (limed sludge) the amounts leaching from the Oxisol treated alike. Nevertheless, the risk of NO3--N groundwater contamination as a result of a single biosolids land application at 0.5-8.0 dry Mg ha-1 could be considered low.

Classification of acid sulphate soils of Finland according to Soil Taxonomy and the FAO/Unesco legend

Selostus: Suomen happamien sulfaattimaiden kansainvälinen luokittelu