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- W2033589219 abstract "Samples from 32 boreholes and outcropts of the Miocene in Hungary have been studied palynologically. The spores and pollen grains have been classified into tropical, subtropical and temperate elements. Changes in the number of species in the elements and their frequencies through the Miocene (25 to 5.6 m.y.) indicate changes in climate. Tropical elements dominate the early Miocene, decrease to a certain degree in the middle Miocene and almost totally disappear at the end of the late Miocene. The number of subtropical elements increases in the early Miocene and decreases subsequently whereas there is a gradual increase in the number of temperature elements throughout the whole period. This evidence indicates a trend of slow cooling in the climate of the Hungarian Miocene." @default.
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- W2033589219 date "1990-10-01" @default.
- W2033589219 modified "2023-10-16" @default.
- W2033589219 title "Climatic changes in the Hungarian Miocene" @default.
- W2033589219 doi "https://doi.org/10.1016/0034-6667(90)90057-p" @default.
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