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. (2020). Foster rather than biological parental telomere length predicts offspring survival and telomere length in king penguins.
Keywords: gene and early life environmental effects growth penguins reproduction investment telomere
Programme: 119
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Vimeux, F.; Masson, V.; Jouzel, J.; Stievenard, M.; Petit, J.R. (1999). Glacial-interglacial changes in ocean surface conditions in the Southern Hemisphere. Nature, 398(6726), 410–413.
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Vimeux F., Masson V., Jouzel J., Petit J.R., Steig E.J., Stievenard M., Aikmae R. & White J.W.C. (2001). Holocene hydrological cycle changes in the Southern Hemisphere documented in East Antarctic deuterium excess records. Climate dynamics, 17(7), 503–513.
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Vimeux F., Masson V., Delaygue G., Jouzel J., Petit J.R. , Stievenard M., Vaikmae R. & White J.W.C. (2001). A 420,000 year deuterium excess record from East Antarctica : Information on past changes in the origin of precipitation at Vostok. J. Geophys. Res., 106(d23), 31863–31873.
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Vilmer N., Pick M., Schwenn R., Ballatore P. & Villain J.P. (2003). On the solar origin of interplanetary coronal mass ejections observed in the vicinity of the Earth. Annales geophysicae, 21, 847–862.
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Villien C. (2007).
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Villeret V., Chessa J.P., Gerday C., Vanbeeumen J. (1997). Preliminary crystal structure of the alkaline protease from the Antarctic Pseudomonas aeruginosa. Protein Sci., 6, 2462–2464.
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Villemin, T., H. Geirsson, E. Sturkell, and F. Jouanne. (2009).
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. (2013). From surface fault traces to a fault growth model: The Vogar Fissure Swarm of the Reykjanes Peninsula, Southwest Iceland
. JOURNAL OF STRUCTURAL GEOLOGY, 51, 38–51.
Abstract: The Vogar Fissure Swarm is one of four en-echelon fracture swarms that connect the Reykjanes Ridge to the South Iceland Seismic Zone and the Western Volcanic Zone. Occurring in an area of flat topography, this fissure swarm is clearly visible at the surface, where it can be seen to affect recent postglacial lavas. Using remote sensing methods to identify and measure all the faults and fractures in the swarm, combined with additional field observations and measurements, we measured 478 individual fractures, 33% of them being faults and 67% being fissures. The fracture lengths show roughly log-normal distributions. Most of the individual fractures belong to 68 main composite fractures, seven of which are longer than 2500 m and correspond to the main fault scarps of the fissure swarm. We showed that these main faults are distributed along five, equally spaced zones, ∼500 m apart and a few kilometers long. We drawn 71 across-strike profiles to characterize the shape of the fault scarps, and 5 along-strike profiles to characterize the evolution of vertical throw along the main faults. Each fault consists of a coalescence of individual segments of approximately equal length. Fault throws are never larger than 10 m and are smallest at the junctions between individual segments. Analyses of along-strike throw profiles allowed us to determine the early stages of growth after coalescence. The earliest stage is characterized by an increase in the throw of the central parts of segments. This is followed by a second stage during which the throw increases at the junctions between segments, progressively erasing these small-throw zones.
Keywords: Divergent plate boundary, Fissure swarm, Icelandic rift, Normal fault growth, Photogrammetric techniques, remote sensing,
Programme: 316
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Villemin T., Sonnette L., Plateaux R. & Bergerat F. (2011).
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