By James W. Collinson (auth.), Thomas N. Taylor, Edith L. Taylor (eds.)
Antarctic Paleobiology discusses the present prestige of paleobiology, largely paleobotany and palynology in Antarctica, and the interrelationship of Antarctic floras to these of alternative Gondwana continents. It offers a large insurance of the main teams of vegetation at the one hand, whereas at the different looking to assessment the vegetational heritage and the actual and organic parameters that effect the distribution of floras via time and area. The biologic task is mentioned inside a framework of the geologic heritage, together with the tectonic and paleogeographic background of the area. ultimately, the reader will discover a complete bibliography of Gondwana paleobotany and palynology.
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Additional info for Antarctic Paleobiology: Its Role in the Reconstruction of Gondwana
Entire-margined angiosperm leaf forms appear to be slightly more diverse than in the Cenomanian, but sampling is limited. Campanian-Maastrichtian Asseinblages The upper part of the nonmarine Kogosukruk Tongue of the Prince Creek Formation is well exposed along 80 km of the Colville River between Uluksrak Bluffs and Ocean Point, northern Alaska. These coal-bearing rocks are considered to be of late Campanian to Maastrichtian age based on the palynoflora (Frederiksen et al. 1986) and the underlying marine Rogers Creek member, which was dated using invertebrates (Brosge and Whittington 1966).
Based on the megafossils, no major vegetational change is evident during the period of deposition of the Kogusukruk Tongue. However, the later coals appear to contain less woody material than do the earlier ones, which may reflect a diminution of the climax forest ecosystem and more open vegetation. Regionally, the vegetation was dominated by the deciduous conifer Parataxodium wigginsii, which, because of the size and morphology are 3-Cretaceous Polar Vegetation and Climate of associated leafy shoots, branches, and logs, is interpreted to have reached small tree stature.
Palaeoclimatol. Palaeoecol. 61:33-77 Ziegler AM, Scotese CR, Barrett SF (1983) Mesozoic and Cenozoic paleogeographic maps. In Broshe P, Sundermann J (eds) Tidal Friction and the Earth's Rotation. Springer Verlag, Berlin, pp 240-252 4---The South Polar Forest Ecosystem Geoffrey T. Creber The solar energy input into the very high input since the wood is a fuel and may be southern latitudes determines the maximum burned to release what was originally solar productivity level that could have been energy.
Antarctic Paleobiology: Its Role in the Reconstruction of Gondwana by James W. Collinson (auth.), Thomas N. Taylor, Edith L. Taylor (eds.)