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Notes: The responses to photoinhibition of photosynthesis at low temperature and subsequent recovery were examined in Arabidopsis thaliana (ecotype Columbia) developed at 4°C cold-acclimating conditions, 23°C non-acclimating conditions and for non-acclimated plants shifted to 4°C (cold-shifted). These responses were determined in planta using Chl fluorescence imaging. We show that cold acclimation results in an increased tolerance to photoinhibition in comparison with non-acclimated plants and that growth and development at low temperature is essential for this to occur. Cold-shifted plants were not as tolerant as the cold-acclimated plants. In addition, we demonstrate this tolerance is as a result of growth under high PSII excitation pressure, that can be modulated by growth temperature or growth irradiance. Cold-acclimated and cold-shifted plants fully recover from photoinhibition in the dark, whereas non-acclimated plants show reduced levels of recovery and demonstrate a requirement for light. The role of the PSII repair cycle, PSII quenching centres, and the use of Chl fluorescence imaging to monitor photoinhibitory responses in planta are discussed.

Notes: We reconsider the potential energy surface of the He–LiH system recently examined by Gianturco and co-workers [F. A. Gianturco et al., Chem. Phys. 215, 227 (1997)]. We compute the He–LiH interaction energy at the CCSD(T) level using large correlation consistent atomic basis sets supplemented with bond functions. To capture the severe anisotropy of the He–LiH potential, we interpolate our ab initio points in the angular direction with cubic splines, then expand the splines in terms of Legendre polynomials. The resulting smooth potential surface differs substantially from that of Gianturco et al.; in particular, our attractive He–LiH well is more than twice as deep as that of Gianturco et al., with a He–LiH binding energy of De=176.7 cm−1. © 1999 American Institute of Physics.

Notes: Young people with disabilities are often excluded from the labour market. The present paper describes an evaluation of an innovative 2-year pilot initiative called Vocational Opportunities in Training for Employment (VOTE) implemented in Northern Ireland to provide employment training and support for vulnerable young adults with a wide range of disabilities. The principal aims of the study were to assess the impact of the new service in the extent to which: (1) it had created and developed training and employment opportunities for young people; and (2) promoted inclusive working partnerships. Documentary analysis was used as a basis for describing and assessing the project objectives in combination with face- to-face interviews with a small number of key stakeholders. A total of 122 young people participated in the initiative in the pilot period, during which time 160 qualifications were obtained. Key stakeholders expressed positive views about the initiative, and in particular, its therapeutic benefits and the extent of interagency working and shared learning. The VOTE initiative achieved considerable success in enabling a significant proportion of young adults to engage in society by developing social and employment skills, and by improving their employment opportunities and prospects. Factors critical to the continued success of this and similar initiatives include: the close involvement of parents; addressing the concerns of local employers; the sympathetic treatment of workplace issues; and effective partnership working.

Notes: Variegation in the immutans (im) mutant of Arabidopsis is induced by a nuclear recessive gene. The white leaf sectors of im contain abnormal plastids lacking pigments and organized lamellae, whereas the green leaf sectors possess normal-appearing chloroplasts. IMMUTANS codes for a thylakoid membrane terminal oxidase that functions as a safety valve to dissipate excess energy. Previous studies have shown that the green sectors of im, regardless of illumination conditions, have anatomical adaptations that are reminiscent of acclimation to high-light stress. It has been suggested that these adaptations provide a means of enhancing photosynthesis to feed the white sectors and maximize plant growth. We have utilized Chl fluorescence imaging to better understand these compensatory mechanisms using, as our experimental material, im leaves with predominantly green (img) or predominantly white (imw) tissues. The samples were examined under conditions of normal growth or high-light stress (photoinhibition). Steady-state fluorescence quenching revealed that the green sectors of the imw leaves had lower levels of 1 − qp than the img leaves, and that this was accompanied by increased electron transport rates. In response to short-term high-light exposure, the green sectors of the imw leaves displayed enhanced non-photochemical quenching (NPQ), which correlated with increased xanthophyll pool sizes and increased amounts of several different Lhcb polypeptides and the PsbS protein. In summary, our data show that, compared with primarily green leaves (img), the green sectors of predominantly white leaves (imw) have elevated rates of electron transport and an enhanced NPQ capacity. We conclude that, in the absence of IM, green sectors develop morphological and biochemical adaptations that allow them to maximize photosynthesis to feed the white sectors, and to protect against photodamage.

Notes: Abstract Multi- and single-channel seismic profiles are used to investigate the structural evolution of back-arc rifting in the intra-oceanic Izu-Bonin Arc. Hachijo and Aoga Shima Rifts, located west of the Izu-Bonin frontal arc, are bounded along-strike by structural and volcanic highs west of Kurose Hole, North Aoga Shima Caldera and Myojin Sho arc volcanoes. Zig-zag and curvilinear faults subdivide the rifts longitudinally into an arc margin (AM), inner rift, outer rift and proto-remnant arc margin (PRA). Hachijo Rift is 65 km long and 20–40 km wide. Aoga Shima Rift is 70 km long and up to 45 km wide. Large-offset border fault zones, with convex and concave dip slopes and uplifted rift flanks, occur along the east (AM) side of the Hachijo Rift and along the west (PRA) side of the Aoga Shima Rift. No cross-rift structures are observed at the transfer zone between these two regions; differential strain may be accommodated by interdigitating rift-parallel faults rather than by strike- or oblique-slip faults. In the Aoga Shima Rift, a 12 km long flank uplift, facing the flank uplift of the PRA, extends northeast from beneath the Myojin Knoll Caldera. Fore-arc sedimentary sequences onlap this uplift creating an unconformity that constrains rift onset to ∼1-2Ma. Estimates of extension (∼3km) and inferred age suggest that these rifts are in the early syn-rift stage of back-arc formation. A two-stage evolution of early back-arc structural evolution is proposed: initially, half-graben form with synthetically faulted, structural rollovers (ramping side of the half-graben) dipping towards zig-zagging large-offset border fault zones. The half-graben asymmetry alternates sides along-strike. The present ‘full-graben’ stage is dominated by rift-parallel hanging wall collapse and by antithetic faulting that concentrates subsidence in an inner rift. Structurally controlled back-arc magmatism occurs within the rift and PRA during both stages. Significant complications to this simple model occur in the Aoga Shima Rift where the east-dipping half-graben dips away from the flank uplift along the PRA. A linear zone of weakness caused by the greater temperatures and crustal thickness along the arc volcanic line controls the initial locus of rifting. Rifts are better developed between the arc edifices; intrusions may be accommodating extensional strain adjacent to the arc volcanoes. Pre-existing structures have little influence on rift evolution; the rifts cut across large structural and volcanic highs west of the North Aoga Shima Caldera and Aoga Shima. Large, rift-elongate volcanic ridges, usually extruded within the most extended inner rift between arc volcanoes, may be the precursors of sea floor spreading. As extension continues, the fissure ridges may become spreading cells and propagate toward the ends of the rifts (adjacent to the arc volcanoes), eventually coalescing with those in adjacent rift basins to form a continuous spreading centre. Analysis of the rift fault patterns suggests an extension direction of N80°E ± 10° that is orthogonal to the trend of the active volcanic arc (N10°W). The zig-zag pattern of border faults may indicate orthorhombic fault formation in response to this extension. Elongation of arc volcanic constructs may also be developed along one set of the possible orthorhombic orientations. Border fault formation may modify the regional stress field locally within the rift basin resulting in the formation of rift-parallel faults and emplacement of rift-parallel volcanic ridges. The border faults dip 45–55° near the surface and the majority of the basin subsidence is accommodated by only a few of these faults. Distinct border fault reflections decreases dips to only 30° at 2.5 km below the sea floor (possibly flattening to near horizontal at 2.8 km although the overlying rollover geometry shows a deeper detachment) suggesting that these rifting structures may be detached at extremely shallow crustal levels.

Notes: [Auszug] JONES, in his interpretation of the activity cycle of the mosquito Culex pipiens fatigans Wied. in constant light (LL) following a light : dark (LD) regime of 12 h light and 12 h dark1, stated that it was possible to calculate that the first peak should have occurred about 18 h after light-on or 6 ...

Notes: [Auszug] Metamorphic core complexes are domal uplifts of metamorphic and plutonic rocks bounded by shear zones that separate them from unmetamorphosed cover rocks. Interpretations of how these features form are varied and controversial, and include models involving extension on low-angle normal faults, ...