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Autonomic failure (AF) is a common source of orthostatic hypotension (OH) in Parkinson's disease (PD). The diagnosis of AF is difficult on clinical grounds alone. We used autonomic testing and 24-h BP monitoring (ABPM) in 122 PD patients to evaluate the diagnostic accuracy of AF by (1) the reduced heart rate increase to fall in blood pressure (BP) ratio (ΔHR/ΔSBP), (2) reverse dipping (RD), and (3) increased diurnal systolic BP standard deviation (SD-SBP). Among patients with OH, ΔHR/ΔSBP yielded the best accuracy (85%), with excellent sensitivity (92%) and acceptable specificity (67%). RD and, to a lesser extent, SD-SBP had high specificity (93% and 73%, respectively) but low sensitivity, resulting in overall moderate accuracy (66% and 55%, respectively). In patients with OH, the addition of ABPM indexes to ΔHR/ΔSBP did not result in a significant improvement of accuracy. In patients without OH, RD and SD-SBP may be useful showing an accuracy of 72% and 81%, respectively, with high negative predictive value when both RD and increased SD-SBP are absent. The integration of bedside (∆HR/∆SBP) and ABPM-derived indexes can assist the clinician in screening PD patients for AF and guide referral to autonomic testing.

In this work we present the hydrogeophysical imaging of a key sector of the Quaternary Po foreland basin (northern Italy), focussing on the reconstruction of clastic aquifers and aquitards in a complex tectono-sedimentary subsurface architecture. The study area includes the relic reliefs of Casalpusterlengo and Zorlesco, two smooth morphological features involving uplifted and gently folded Pleistocene marine to alluvial sediments, plausibly linked to the buried Northern Apennines thrust and fold belt. The geophysical data include 35 Direct Current Vertical Electrical Soundings collected over a 37 km2 wide area, acquired with Schlumberger array and maximum half-spacing of 500 m. 1-D resistivity-depth profiles were computed for each VES. An integrated hydrostratigraphic approach was applied, to constrain the interpretation of the geophysical data along several cross-sections, including the comparison of resistivity soundings to stratigraphic logs, borehole electric logs and the pore-water properties. The resistivity interfaces, traceable with the same laterally continuous vertical polarity, were used to develop an electrostratigraphic model in order to portray the stacking of electrostratigraphic units down to 200 m below ground surface. Their vertical associations show a general upward increase of electrical resistivity. This assemblage mimics the regional coarsening upwards depositional trend, from the conductive units of the Plio-Pleistocene marine-to-transitional depositional systems to the resistive units of the Middle–Late Pleistocene fluvial and alluvial plain depositional systems. Middle Pleistocene depositional systems host an alternation of North-dipping, high-to-intermediate permeability aquifer systems (70–180 Ωm, thickness of 5–70 m) separated by low permeability aquitards (20–50 Ωm, thickness up to 40 m). These units pinch out against the Casalpusterlengo and Zorlesco relic reliefs, where they cover the uplifted and folded regional aquitard (20–50 Ωm) formed by Pliocene-Lower Pleistocene clays to sandy silts with gravel lenses in agreement with borehole data. In the deepest part of the local stratigraphy, a broad low-resistivity anomaly (< 10 Ωm) was clearly mapped through the study area. By comparison with electrical borehole logs in deep oil-wells, it could be interpreted as the fresh–saltwater interface due to the presence of connate waters and brines hosted by the marine-to-transitional shales.

Wavelet transform analysis of experimentally measured intensity fluctuations distinguishes the transition from low frequency fluctuations at moderate feedback to stable operation at strong feedback. Comparison of these results with those of a wavelet analysis of lowpass filtered solutions of the Lang-Kobayashi equations for deterministic evolution of a single mode semiconductor laser with optical feedback finds substantial agreement in the part of the wavelet spectrum corresponding to slow dynamics. Substantial disagreement is found in the fast dynamics, which lessens when noise is added to the equations.

Secretogranin II (chromogranin C) is an acidic tyrosine-sulfated secretory protein, known to be a marker of neuroendocrine secretory products and of specific neuroendocrine tumours. In order to obtain anti-secretogranin II monoclonal antibodies for cell biology studies and, in particular, for clinical applications, we immunized mice with a secretogranin II-enriched fraction prepared from homogenates of bovine anterior pituitaries. Hybridoma supernatants obtained from the splenocytes of a hyperimmune mouse, screened with an enzyme-linked immunosorbent assay, were analyzed by both immunocytochemistry and two-dimensional immunoblotting. By using this experimental approach, we were able to identify two monoclonal antibodies (8G1 and 5A7) which recognize bovine secretogranin II. Both immunocytochemistry and immunoblotting revealed that one of them, the 5A7 antibody, cross-reacts with the human antigen. The distribution patterns of the immunoreactivity, obtained by immunocytochemistry with the 5A7 antibody in animal and human tissues, partially overlap those, obtained by using a polyclonal antiserum elicited against bovine secretogranin II, previously described. Moreover, the 5A7, but not the polyclonal antibody, reacts with some duodeno-jejunal cells. In conclusion, both the 5A7 and 8G1 antibodies can be useful for cell biology studies. The 5A7 antibody can be used for the detection of secretogranin II in human tissues and should be of help in clinical and pathological practices.

The presence of small G proteins was investigated by [γ- 35 S]GTP-binding in 3 human neuroblastoma cell lines, IMR-32, SK-N-BE and SH-SY5Y, before and after treatment with differentiating agents (dibutyryl-cAMP, 5-bromodeoxyuridine or retinoic acid) which induce the appearance of secretory organelles. One major component of about 24 kDa and 3 minor components of smaller M r were found to bind specifically [γ- 35 S]GTP in all 3 cell lines already before differentiation. Differentiation did not affect the expression of small G proteins in IMR-32 cells and only modestly affected it in the other two cell lines. The possibility that the expression of small G proteins in neuroblastoma cells is not coupled with the assembly of secretory organelles is discussed.

Actinomycin D and puromycin inhibit the light-stimulated synthesis of amaranthin in Amaranthus tricolor seedlings. This result suggests that the phytochrome-mediated formation of the pigment is controlled by P 730 through the activation of potentially active genes, in agreement with Mohr's hypothesis on the mode of action of phytochrome.

Amaranthin synthesis in Amaranthus tricolor seedlings is stimulated by kinetin in darkness. This stimulation, which does not depend on the phytochrome status, is inhibited by actinomycin D and puromycin. The kinetin-induced amaranthin synthesis can be interpreted on the basis of gene activation.

Physcion, fallacinol, fallacinal, parietinic acid and emodin have been isolated from extracts of Xanthoria parientina . A much higher concentration of total anthraquinones was found in X. parietina var. aureola which contains, besides these five pigments, small amounts of citreorosein and emodic acid.

Light stimulates the betaxanthin accumulation in Celosia plumosa . The induction is partially reversed by far-red and inhibited by actinomycin D, puromycin, salicylaldoxime and 2,4-dinitrophenol, while 3-(3,4-dichlorophenyl)-1,1-dimethylurea has an inhibitory effect only when photosynthesis is operative. In darkness betaxanthins synthesis is promoted by kinetin.

The accumulation of amaranthin in kinetin-treated seedlings of Amaranthus tricolor is significantly increased following exposure to light. This enhancement, which appears to be phytochrome-controlled since it is saturated at low energy levels of irradiation and is far-red reversible, involves the synthesis of enzymes which mediate the effect of light on pigment formation. However, this does not depend on the direct intervention of photo-activated phytochrome at the DNA level.

Amaranthin formation in seedlings of Amaranthus tricolor is controlled by two photoreactions, one, a high-energy reaction, and the other a low-energy reaction controlled by phytochrome. Elongation of the hypocotyl in A. tricolor seedlings is also phytochrome controlled.