Titlebook: Antarctic Paleobiology; Its Role in the Reco Thomas N. Taylor,Edith L. Taylor Book 1990 Springer-Verlag New York Inc. 1990 Flora.Trias.Vege

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Permineralized , and , from Antarctica,80, and references cited therein). In fact, leaves of these types typify the megafossil assemblages to such an extent that Permian and Triassic Gondwana floras are commonly known as the. and. floras, respectively (e.g., Gould 1975; Retallack 1977; Schopf and Askin 1980).

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lationship of Antarctic floras to those of other Gondwana continents. It provides a broad coverage of the major groups of plants on the one hand, while on the other seeking to evaluate the vegetational history and the physical and biological parameters that influence the distribution of floras throu

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Chemisches Verhalten der Alkaloidet have provided palynological data (Fig. 7.1). To these records of in situ pollen and spores, there can be added information available from the palynomorphs that are recycled by glacial processes and incorporated into surficial sediments on the seafloor around Antarctica.

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Triassic Terrestrial Vertebrate Faunas of Antarctica,terval, 11 productive sites (Fig. 5.1) in the central portion of the range, near the Beardmore and Shackleton Glaciers, have been identified. Other areas explored that have not yielded vertebrates include the Allan Hills near the Dry Valleys of Southern Victoria Land and sections of Northern Victoria Land. (Hammer and Zawiskie 1982, Hammer 1987).

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Cretaceous and Tertiary Vegetation of Antarctica: A Palynological Perspective,t have provided palynological data (Fig. 7.1). To these records of in situ pollen and spores, there can be added information available from the palynomorphs that are recycled by glacial processes and incorporated into surficial sediments on the seafloor around Antarctica.