Ice volume changes (1936-1990-2007) and ground-penetrating radar studies of Ariebreen, Hornsund, Spitsbergen

Ariebreen is a small (0.37 km2) valley glacier located in southern Spitsbergen. Our ground-penetrating radar surveys of the glacier show that it is less than 30 m thick on average, with a maximum thickness of 82 m, and it appears to be entirely cold. By analysing digital terrain models of the ice surface from different dates, we determine the area and volume changes during two periods, 1936-1990 and 1990-2007. The total ice volume of the glacier has decreased by 73% during the entire period 1936-2007, which is equivalent to a mean mass balance rate of -0.6190.17 m/yr w.eq. The glacier thinning rate has increased markedly between the first and second periods, from -0.5090.22 to -0.9590.17 m/yr w.eq.

Ice volume estimates from ground-penetrating radar surveys, Wedel Jarlsberg Land glaciers, Svalbard

One of the aims of the SvalGlac project is to obtain an improved estimate, with reliable error estimates, of the volume of Svalbard glaciers and their potential contribution to sea level rise. As part of this work, we present volume calculations, with detailed error estimates, for eight glaciers on Wedel Jarlsberg Land, southern Spitsbergen, Svalbard. The volume estimates are based upon a dense net of GPR-retrieved ice thickness data collected over several field campaigns spanning the period 2004-2011. The total area and volume of the ensemble are 502.9±18.6 km2 and 80.72±2.85 km3, respectively. Excluding Ariebreen (a tiny glacier, menor que 0.4 km2 in area), the individual areas, volumes and average ice thickness lie within 4.7-141.0 km2, 0.30-25.85 km3 and 64-183 m, respectively. The maximum recorded ice thickness, ca. 619±13 m, is found in Austre Torellbreen. To estimate the ice volume of small non-echo-sounded tributary glaciers, we used a function providing the best fit to the ice thickness along the centre line of a collection of such tributaries where echo-soundings were available, and assuming parabolic cross-sections. We did some tests on the effect on the measured ice volumes of the distinct radio-wave velocity (RWV) of firn as compared to ice, and cold versus temperate ice, concluding that the changes in volume implied by such corrections were within the error bounds of our volume estimate using a constant RWV for the entire glacier inferred from common mid-point measurements on the upper ablation area.

A small nucleolar RNA requirement for site-specific ribose methylation of rRNA in Xenopus

Vertebrate cells contain a large number of small nucleolar RNA (snoRNA) species, the vast majority of which bind fibrillarin. Most of the fibrillarin-associated snoRNAs can form 10- to 21-nt duplexes with rRNA and are thought to guide 2′-O-methylation of selected nucleotides in rRNA. These include mammalian UHG (U22 host gene)-encoded U25–U31 snoRNAs. We have characterized two novel human snoRNA species, U62 and U63, which similarly exhibit 15- (with one interruption) and 12-nt complementarities and are therefore predicted to direct 2′-O-methylation of A590 in 18S and A4531 in 28S rRNA, respectively. To establish the function of antisense snoRNAs in vertebrates, we exploited the Xenopus oocyte system. Cloning of the Xenopus U25–U31 snoRNA genes indicated that they are encoded within multiple homologs of mammalian UHG. Depletion of U25 from the Xenopus oocyte abolished 2′-O-methylation of G1448 in 18S rRNA; methylation could be restored by injecting either the Xenopus or human U25 transcript into U25-depleted oocytes. Comparison of Xenopus and human U25 sequences revealed that only boxes C, D, and D′, as well as the 18S rRNA complement, were invariant, suggesting that they may be the only elements required for U25 snoRNA stability and function.