Matskási István (szerk.): A Magyar Természettudományi Múzeum évkönyve 90. (Budapest 1998)

Bajzáth, J.: Plant macrofossils from the Hungarian Pleistocene III. Palaeobotanical study of Győrújfalu, Western Hungary

Table 1 (continued) Taxa frequency [m] 20 25 28 30 33 Rubus caesius LINNAEUS, 1753 Sagina procumbens LINNAEUS, 1753 Sagittaria sagitlifolia LlNNAEUS, 1753 Salix sp. Schoenoplectus lacustris (L.) PALLA, 1888 Schoenoplectus mucronatus (L.) PALLA, 1888 Schoenoplectus tabernaemontani (C. C. GMEL.) PALLA, 1888 Scirpus radicans SCHKUHR, 1 793 Scirpus s pp. Scirpus sylvaticus LlNNAEUS, 1753 Sonchus arvensis LlNNAEUS, 1753 Sparganium emersum REHMANN, 1872 Stachys palustris LlNNAEUS, 1753 Stachys sylvatica LINNAEUS, 1753 Stratiotes aloides LlNNAEUS, 1753 Thalictrum flavum LlNNAEUS, 1753 Typha latifolia LINNAEUS, 1753 Urtica dioica LlNNAEUS, 1753 Viola palustris LlNNAEUS, 1753 Viola rupeslris F. W. SCHMIDT, 1791 Vitis sylvestris C. C. GMELIN, 1937 + 2 + 2 species such as Stratiotes aloides, Hydrocharis morsus-ranae, Nymphaea alba, Caldesia parnassifolia and Salvinia natans, Azolla filiculoides formed the so-called Brasenia-complex, which indicates the climatic optimum of an interglacial. Curiously, the typical subcontinental thermophylus species (Brasenia sp., Aldrovanda vesiculosa, Trapa natans) after which the complex was named are missing. The presence of several southern geographical elements (Picea omorikoides, Carpinus betulus, Ostrya carpinifolia, Caldesia parnassifolia etc.) indicates the influence of the Mediterranean region on the flora. The mixture of taxa with different ecological requirements and geographical distribution could be related to changes in the climatic condition. The percentage of selected ecological groups in the interglacial flora of Győrújfalu is as follows: terrestrial 21%, mire species 53%, aquatic 26%. A comparison of Győrújfalu with other Hungarian localities is not possible as there is no other Cromerian macroflora known in Hungary. There are only a few sporadic mac-