L. Hably szerk.: Studia Botanica Hungarica 18. 1985 (Budapest, 1985)

Kordos-Szakály, Márta: Stratigraphical revision of some Hungarian Badenian-Sarmatian floras

The leaf-type group assignment of the eight examined Hungarian floras are shown in Table 1. Table 1. Gregor' s leaf-type index in the examined localities leaf types Locality a b c d f g h i k 1 m n o p q r s t U V w X Eger-Tihamér 3 ­­4 2 4 4 3 4 ­3 2 3 4 - 3 3 ­­- - 4 ­Buják 4 3 4 ­4 3 3 3 3 3 3 2 4 3 4 ­­4 ­- - 4 ­Mikófalva 3 3 3 4 ­3 3 3 2 3 2 2 ­3 4 ­­­4 - - ­4 Bánhorváti 3 2 2 ­4 2 1 3 1 1 3 1 3 2 1 ­3 4 Sály 3 3 4 2 3 2 2 3 2 3 2 1 ­2 4 ­­3 4 _ _ _ ­Balaton 4 3 ­3 ­2 l 3 1 2 2 1 3 1 4 ­3 1 2 - - 3 ­Nógrádszakál-Páris ­3 3 ­­2 1 4 2 3 1 1 ­3 2 ­­­3 2 - ­3 Nógrádszakál-Bertece 4 3 ­­­4 2 4 2 3 2 2 ­1 4 ­­­­2 - ­­As a result of this, the leaf-type composition of the individual floras can be determined and assign­ment can be made to the ecological flora types determined by GREGOR on the basis of the analyses of numerous samples. GREGOR (1982) has separated the following flora types: fgilm-flora: deciduous, with few exotic elements, juglandoiden, aceroiden, quercoiden and carpinoi­den (Pliocene, MN 10 zone) defgikm-flora: deciduous, with more exotic elements, conifers and other components like above (Pliocene, Upper Miocene, MN 9 zone) dg-flora: a sub-unit of the previous zone, pine-maple flora (Pliocene, MN 9 zone) defgm-flora: a part of the defgikm-flora, rich in conifers and characterized by a special Gingko­form (Upper Miocene, MN 8/9 zone) eilmp(h)-flora: a flora characteristic for humid environment with Populus , Salix, Quercus and few exotic elements (Upper Miocene, MN 7/8 and 8 zones) ab(h)-flora: typically deciduous flora with high number of evergreens, especially with laurel-leaf types and smaller leguminous plants (Middle and Upper Miocene, MN 4-7 zones) abehlm-flora: a sub-unit of the previous one characterized by the Daphnogene s often occurring monotypically, with many exotic elements, smaller leguminous plants and carpinoid form (Middle Miocene, MN 5-7 zones) abdeim-flora: a somewhat older assemblage, but not very much different from the previous one (Lower Miocene, MN 4b/5 zones) adgi-flora: an Acer-Quercus predominated flora with great number of indeciduous elements and cinnamonides and palm trees (Upper Oligocène, Lower Miocene, MN 1-3 zones) The characteristic leaf types and GREGOR' s flora-types of the eight Hungarian floras exam­ined are the following: Bánhorváti fgikm defgikm(o) Balaton fgimo defgikm(o) Sály fgilm defgikm (o) Mikófalva bgilm defgikm(b) Buják bgilm defgikm(b) Paris fgilm defgikm(u) Bertece gilmou defgikm(u) Eger-Tihamér elmnqr eilmp The letter codes characteristic for the leaf types help us to determine the floras that are very similar to each other. Similarity of the Bánhorváti-Balaton-Sály, Mikófalva-Buják (completely iden­tical!), Paris-Bertece sites and the independence of the Eger-Tihamér site could be ascertained (Tig. 1). These results are concordant with the time-distance analyses based on the common spe­cies and the kindred circles, and the flora sequence defined by cluster analysis. Assignment of the eight Hungarian floras to the Gregor-flora types represented a more diffi­cult task. It seems evident however, that all sites represent a transition between the fgilm and defgikm floras, except for the Eger-Tihamér assemblage, and could be classified into no other group. Considering the leaf-type codes, they are nearer the flora type fgilm. However, based on the relevant descriptions and chronological correlation they can be assigned to the defgikm flora-

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