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Abstract  Two single-channel seismic (SCS) data sets collected in 2000 and 2005 were used for a four-dimensional (4D) time-lapse analysis of an active cold vent (Bullseye Vent). The data set acquired in 2000 serves as a reference in the applied processing sequence. The 4D processing sequence utilizes time- and phase-matching, gain adjustments and shaping filters to transform the 2005 data set so that it is most comparable to the conditions under which the 2000 data were acquired. The cold vent is characterized by seismic blanking, which is a result of the presence of gas hydrate in the subsurface either within coarser-grained turbidite sands or in fractures, as well as free gas trapped in these fracture systems. The area of blanking was defined using the seismic attributes instantaneous amplitude and similarity. Several areas were identified where blanking was reduced in 2005 relative to 2000. But most of the centre of Bullseye Vent and the area around it were seen to be characterized by intensified blanking in 2005. Tracing these areas of intensified blanking through the three-dimensional (3D) seismic volume defined several apparent new flow pathways that were not seen in the 2000 data, which are interpreted as newly generated fractures/faults for upward fluid migration. Intensified blanking is interpreted as a result of new formation of gas hydrate in the subsurface along new fracture pathways. Areas with reduced blanking may be zones where formerly plugged fractures that had trapped some free gas may have been opened and free gas was liberated. [ABSTRACT FROM AUTHOR]

Plants in the genus Nepenthes obtain a substantial nutrient supply by trapping insects in highly modified leaves. A broad zone of the inner surface of these pitchers is densely covered with wax crystals on which most insects lose their footing. This slippery wax surface, capturing prey and preventing its escape from the trap, plays a pivotal role in the carnivorous syndrome. To understand the mechanism of slipperiness, the present investigation aimed at an ultrastructural and physico-chemical characterization of the wax crystals in pitchers of N. alata Blanco. Scanning electron microscopy revealed that entire platelets protruded perpendicularly from the surface. Methods were developed that allowed the mechanical removal of wax crystals from the pitcher surface. It could be shown that the sampling was selective for the epicuticular wax, relevant for plant?insect interactions. The crystals consisted of a mixture of aliphatic compounds dominated by very-long-chain aldehydes. Triacontanal, at 43% the most abundant constituent, was largely responsible for crystal formation. Solubility data indicate that the Nepenthes crystals contained polymeric forms of this aldehyde. The resulting mechanical properties of the polymer crystals and the mechanism of slipperiness are discussed. [ABSTRACT FROM AUTHOR]