Maintenance of optical quality during crystalline lens growth

Vertebrate lenses grow throughout life by the division of cells at the lens surface. The fibre cells thus produced are gradually covered by newer tissue, giving a layered structure. During growth, the lens must remain transparent and retain its refractile properties. The severity of these constraints is perhaps most evident in teleost fish which have a spherical lens that may increase in volume by a thousandfold during the first year of life. The dioptric power of the teleost fish eye is vested entirely in this spherical lens, as water, the cornea and the intraocular vitreous humour have almost identical refractive indices. Spherical lenses of uniform refractive index produce poor images because rays entering at different distances from the optic axis are focused at different distances from the lens. Teleost fish do not suffer from this imperfection and it has long been presumed that this is because there exists a refractive index gradient having a high value in the centre and decreasing continuously and symmetrically with radius in all directions. Here we demonstrate in the African cichlid fish, Haplochromis burtoni, that a refractive index gradient does exist, although its form is significantly different from that previously postulated.     

Magma-maintained rift segmentation at continental rupture in the 2005 Afar dyking episode

Seafloor spreading centres show a regular along-axis segmentation thought to be produced by a segmented magma supply in the passively upwelling mantle. On the other hand, continental rifts are segmented by large offset normal faults, and many lack magmatism. It is unclear how, when and where the ubiquitous segmented melt zones are emplaced during the continental rupture process. Between 14 September and 4 October 2005, 163 earthquakes (magnitudes greater than 3.9) and a volcanic eruption occurred within the approximately 60-km-long Dabbahu magmatic segment of the Afar rift, a nascent seafloor spreading centre in stretched continental lithosphere. Here we present a three-dimensional deformation field for the Dabbahu rifting episode derived from satellite radar data, which shows that the entire segment ruptured, making it the largest to have occurred on land in the era of satellite geodesy. Simple elastic modelling shows that the magmatic segment opened by up to 8 m, yet seismic rupture can account for only 8 per cent of the observed deformation. Magma was injected along a dyke between depths of 2 and 9 km, corresponding to a total intrusion volume of approximately 2.5 km3. Much of the magma appears to have originated from shallow chambers beneath Dabbahu and Gabho volcanoes at the northern end of the segment, where an explosive fissural eruption occurred on 26 September 2005. Although comparable in magnitude to the ten year (1975-84) Krafla events in Iceland, seismic data suggest that most of the Dabbahu dyke intrusion occurred in less than a week. Thus, magma intrusion via dyking, rather than segmented normal faulting, maintains and probably initiated the along-axis segmentation along this sector of the Nubia-Arabia plate boundary.     

Using administrative data sources in the estimation of emigration

It is important that migration is measured accurately, for example to inform population estimates and projections. However, current sources of information present challenges in producing robust estimates of emigration from Great Britain. This article reports on work carried out by the Office for National Statistics to investigate the potential for using administrative data sources to contribute to the measurement of emigration.