THE DISCOVERY AND ITS SIGNIFICANCE OF FOSSIL PLANTS AT LATE DEVONIAN-EARLY CARBONIFEROUS IN EASTERN LIAONING
范国清
Abstract
范国清
Abstract
The absence of the Late Ordovician-Early Carboniferous strata in the North China Platform has been considered as a final conclusion, but the author (1986—1989), during the study on lithofacies and palaeogeography in the Carboniferous-Permian of Liaoning, obtained some fossil plants, Sublepidodendron sp., Lepidostrobus grabaui, Connophyllum sp., Stigmariaficoides, Neuropteris gigantea, Lepidostro bophyllum and so on at G-layer bauxite and the roof of the lower part of Benxi Group in the Middle Carboniferous at Gaotaizi, Niuxintai in Benxi and Nuanhezi in Huairen County. While Liu Fa (1987) found fossil ani-
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The absence of the Late Ordovician-Early Carboniferous strata in the North China Platform has been considered as a final conclusion, but the author (1986—1989), during the study on lithofacies and palaeogeography in the Carboniferous-Permian of Liaoning, obtained some fossil plants, Sublepidodendron sp., Lepidostrobus grabaui, Connophyllum sp., Stigmariaficoides, Neuropteris gigantea, Lepidostro bophyllum and so on at G-layer bauxite and the roof of the lower part of Benxi Group in the Middle Carboniferous at Gaotaizi, Niuxintai in Benxi and Nuanhezi in Huairen County. While Liu Fa (1987) found fossil ani-
Key concepts: Carboniferous, Devonian, Paleontology, Geology, Permian, Paleozoic, Palaeogeography, Ordovician