Study of β-1,3-glucanase activity during autolysis of Aspergillus nidulans by FPLC ion-exchange chromatography

The behaviour of β-1,3-glucanase activity during Aspergillus nidulans autolysis was studied in a basal medium and in the same medium supplemented with 0.5 g l^-1 of microcrystalline cellulose, laminarin, pectin, seedling of Lycopersicum esculentum extract, chitin and xylan respectively. In any case β-1,3-glucanase activity was detected in the culture fluid before the onset of the autolysis, but afterwards a progressive increase of β-1,3-glucanase activity took place with incubation time. In the media supplemented with pectin and seedling of Lycopersicum esculentum extract higher activity in the first days of autolysis was found. The activity at the end of the studied process by sample was 2.5, 2.1, 2.5, 1.9, 2.2, 2.3 and 2.3 U, and the specific activity 83, 53, 85, 55, 64, 90 and 53 mU mg^-1 of protein for each medium respectively. The β-1,3-glucanase activity in Aspergillus nidulans seems to be related to autolysis and not to the presence of different substances in the culture medium. The behaviour of β-1,3-glucanase activity during the degradative process was followed by FPLC ion-exchange chromatography. Three proteins (I, II, III) with β-1,3-glucanase activity were separated and quantified. These proteins have similar behaviour in all the media. Proteins I and II increase progressively with incubation time but protein III is only present at the first and last days of autolysis.     

Rapid conversion of spirostans into furostan skeletons at room temperature

We report a facile protocol to obtain 22-substituted furostans and pseudosapogenins in high yields from (25R)- and (25S)-sapogenins. This method involves the treatment of the sapogenin with acetic-trifluoroacetic mixed anhydride and BF(3)·OEt(2) at room temperature, followed by the addition of a nucleophile (H(2)O, MeOH or KSeCN). In the case of 22-hydroxyfurostans, they can be transformed to pseudosapogenins by treatment with p-toluensulfonic acid.     

The C-terminal region of hPrp8 interacts with the conserved GU dinucleotide at the 5' splice site

A U5 snRNP protein, hPrp8, forms a UV-induced crosslink with the 5' splice site (5'SS) RNA within splicing complex B assembled in trans- as well as in cis-splicing reactions. Both yeast and human Prp8 interact with the 5'SS, branch site, polypyrimidine tract, and 3'SS during splicing. To begin to define functional domains in Prp8 we have mapped the site of the 5'SS crosslink within the hPrp8 protein. Immunoprecipitation analysis limited the site of crosslink to the C-terminal 5060-kDa segment of hPrp8. In addition, size comparison of the crosslink-containing peptides generated with different proteolytic reagents with the pattern of fragments predicted from the hPrp8 sequence allowed for mapping of the crosslink to a stretch of five amino acids in the C-terminal portion of hPrp8 (positions 1894-1898). The site of the 5'SS:hPrp8 crosslink falls within a segment spanning the previously defined polypyrimidine tract recognition domain in yPrp8, suggesting that an overlapping region of Prp8 may be involved both in the 5'SS and polypyrimidine tract recognition events. In the context of other known interactions of Prp8, these results suggest that this protein may participate in formation of the catalytic center of the spliceosome.     

Role of uronic acids present in phytopathogenic fungi as inducers of polygalacturonases during autolysis

The presence of uronic acids in the culture fluid and mycelium of the fungi: Alternaria alternata, Botrytis cinerea, Drechslera halodes, Fusarium culmorum, Fusarium oxysporum, Monilinia fructigena, Mucor mucedo, Rhizopus stolonifer and Trichoderma hamatum was detected and quantified. In these fungi the concentration of uronic acids increased during the growth phase and the maximal concentrations were found at the end of the growth phase or onset of autolysis both in the mycelium as well as in the culture fluid. The uronic acids were metabolized during the first days of autolysis decreasing to constant levels until the end of the autolytic period studied.The variations in the activity of polygalacturonase and polymethylgalacturonase present in the culture fluid were determined at the onset and during autolysis in these fungi. These enzymic activities were found in the culture fluid of these fungi, with exception of M. rouxii, and they showed an increasing activity in the first days of autolysis and later a slight increase or decrease was observed. The presence of uronic acids in these phytopathogenic or saprophytic fungi and the low levels detected during autolysis could be related to the induction of pectic enzymes and the pathogenicity of these fungi.     

Patterns and drivers of Araucaria araucana forest growth along a biophysical gradient in the northern Patagonian Andes: Linking tree rings with satellite observations of soil moisture

Araucaria araucana (Araucaria) is a long‐lived conifer growing along a sharp west–east biophysical gradient in the Patagonian Andes. The patterns and climate drivers of Araucaria growth have typically been documented on the driest part of the gradient relying on correlations with meteorological records, but the lack of in situ soil moisture observations has precluded an assessment of the growth responses to soil moisture variability. Here, we use a network of 21 tree‐ring width chronologies to investigate the spatiotemporal patterns of tree growth through the entire gradient and evaluate their linkages with regional climate and satellite‐observed surface soil moisture variability. We found that temporal variations in tree growth are remarkably similar throughout the gradient and largely driven by soil moisture variability. The regional spatiotemporal pattern of tree growth was positively correlated with precipitation (r = 0.35 for January 1920–1974; P < 0.01) and predominantly negatively correlated with temperature (r = ?0.38 for January–March 1920–1974; P < 0.01) during the previous growing season. These correlations suggest a temporally lagged growth response to summer moisture that could be associated with known physiological carry‐over processes in conifers and to a response to moisture variability at deeper layers of the rooting zone. Notably, satellite observations revealed a previously unobserved response of Araucaria growth to summer surface soil moisture during the current rather than the previous growing season (r = 0.65 for 1979–2000; P < 0.05). This new response has a large spatial footprint across the mid‐latitudes of the South American continent (35°–45°S) and highlights the potential of Araucaria tree rings for palaeoclimatic applications. The strong moisture constraint on tree growth revealed by satellite observations suggests that projected summer drying during the coming decades may result in regional growth declines in Araucaria forests and other water‐limited ecosystems in the Patagonian Andes.