Abstract
Includes a new stratigraphic interpretation based on both palyno- and lithostratigraphy. Since the palynologic succession is very similar to those in the Southern Alps and Greenland, a comparison between those localities is also made. It is shown that: palynologic assemblages undergo a drastic change within the boundary interval; in the subsurface of Israel, the succession assigned to the Late Permian Lueckisporites virkkiae Zone is characterized by striate bisaccate pollen; at the top of the Permian succession is a horizon rich in reworked palynomorphs and other land-derived organic debris; acritarchs are abundant in layers in the lower part of the stratal sequence here regarded as Early Triassic; lycopodes, such as Kraeuselisporites and Endosporites papillatus are among the first representatives of land plants above the "acritarch spike'. Following Visscher & Brugman's (1988) ideas on the nature of the Permo-Traissic boundary in the Southern Alps, a vegetative succession for the boundary interval is suggested. -from Author
| Original language | English |
|---|---|
| Pages (from-to) | 134-145 |
| Number of pages | 12 |
| Journal | Unknown Journal |
| DOIs | |
| State | Published - 1992 |
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