Through combining the characteristics of the reservoir, source, seal, and the trap evolution, the Sarvak accumulation genesis and evolution are discussed.
Combined with the trap evolution, the accumulation evolution can be summarized as follows: the Sarvak play became a paleo-anticlinal trap in the Alpine tectonic activity after the late Cretaceous (96 Ma) and then was relatively peaceful in the later long geologic period.
This weather-dependent variation of peristome slipperiness leads to an intermittent and unpredictable activation of Nepenthes pitcher traps, which might make the evolution of specific avoidance behaviors more difficult [173].
According to the previous findings of regional tectonic activities and deposition time of the flattened formations, the genesis and stages of the trap evolution are analyzed and determined.
The evolution of spore traps has continued since the Hirst trap was developed, using the second air intake of a cascade impactor and sample collection changing from a waxed slide to a tape on a circular drum.
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Evidence for the evolution of "snap-traps" of Dionaea and Aldrovanda from a flypaper trap like D. regia has also emerged and been argued for based on molecular data.
Moreover, ecological studies would help to clarify the selective pressures that have led to the evolution of different trapping strategies in this carnivorous genus.
But, if we also consider the evolution of the air traps and the melt and weld lines, which greatly influence the aesthetic factor, the resulting limiting thickness is 650 μm in the centre of biconcave lenses and 500 μm in the peripheric area of biconvex lenses.
