文摘
Fruit endocarps assigned to Mastixia amygdalaeformis provide the first evidence that mastixioid plants were present in the Pannonian Basin. Fossils were collected from the upper Miocene (Tortonian, regional stratigraphy: Pannonian) deposits of the Rudab¨¢nya-Vilmos outcrop which is close to the mammal locality yielding the famous remains of Rudapithecus hungaricus. The accompanying flora indicates mainly swamp and aquatic associations and comprises dominantly deciduous elements. A relict element of the flora, Daphnogene (Lauraceae) has the last occurrence documented from Hungary. Fruits of Mastixia from the upper Miocene locality at Rudab¨¢nya indicate an additional European refugium of ¡°younger mastixioid¡± floras in the Pannonian Basin. The late Miocene landscape, palaeoecology and palaeogeography of the Pannonian Basin, was basically determined by Lake Pannon. The presence of a mastixioid flora corroborates a humid, warm temperate climate and the establishment of habitats providing refuge of thermophilic elements close to the lake.