Appendix A. Gene identity within the cultivated species, and between the cultivated species and different wild species in tomato

High salinity is a severe constraint on tomato growth and productivity in many regions and situations. To obtain an ideal gene donor for improving the salt tolerance of tomato cultivars, the potential of tolerance response to salinity were evaluated for 14 tomato accessions including wild and cultivated species. By investigation of seed germination and seedling survival, a common cultivar, Solanum lycopersicum 'moneymaker', is evidenced significantly salt-tolerant among them and correspondingly, a wild accession, Solanum cheesmanniae 'LA0317', is most vulnerable to salinity. The performance of Moneymaker and LA0317 upon salinity was then compared in detail for their growth inhibition and some physiological changes. Complete dominance of Moneymaker and its high gene identity in tomato species lead us to use it in microarray experiment and apply it as gene donor for salt tolerance. The results indicated some mechanism differences between Moneymaker and LA0317 in salt response, proposed the potentially high salt tolerance of cultivated tomato and implied that Moneymaker is a valuable gene donor in this field, potentially minimizing the growth inhibition and yield reduction in transgenic plants.

Palynological investigations of profile Cergowa in Poland

The decomposition rate of organic, Compounds, following the death of a plant, is dependent on several external factors. Assimilatory pigments generally undergo a rapid degradation. In certain condition, however, their decomposition may be considerably retarded; e.g. compounds similar to chlorophyll and some carotenoids, as a and ß-carotene, lutein and others, may persist several thousand years in marine and lake Sediments (Vallentyne 1960). Derivatives of chlorophyll were also found in the surface layer of wood soil (Gorham 1959). In this connection the question arises, in what a way a still different environment, namely peat, influences the decomposition rate of pigments. The starting point in these investigations was the fact observed by one of the co-authors, that many subfossil fir needles from various depths of the peat bog in Cergowa Gora were bright yellow green pigmented. Macroscopic otoservations have already suggested that, at least, a part of the pigments did not undergo decomposition. A study was undertaken with the aim to determine the quantitative and qualitative changes in assimilatory pigments, occurring in fir needles in dependence on the pexiod of time they were lying in the peat bog.