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Extra info for Antarctic Paleobiology: Its Role in the Reconstruction of Gondwana

Example text

Parasites feed either on living plants or estry practice, the volume of wood produced animals and scavengers feed on the latter's annually per unit area of forest floor can be dead remains. Every organism in the ecosys- calculated (Creber and Chaloner, 1984a, tem is thus dependent on the energy input 1984b, 1985; Creber 1986; Creber and Francis either directly or indirectly. The solar input of 1987; Hamilton and Christie 1971). 4 g/cm 3). The total energy content is found continent a temperate ecosystem.

Bull. US GeoL Surv. 1614:61-74 Jefferson TH (1981) Palaeobotanical contributions to the geology of Alexander Island, Antarctica. Unpubl. PhD dissertation, Cambridge University, England Jefferson TH (1982) Fossil forests from the Lower Cretaceous of Alexander Island, Antarctica. Palaeontology 25:681-708 Jefferson TH, MacDonald DIM (1981) Fossil wood from South Georgia. Bull. British Antarctic Survey 54:57-64 Jones PB (1983) The cordilleran connection-a link between Arctic and Pacific sea-floor spreading.

Recent paleogeographic reconstructions (Lawver et al. 1985) place the Antarctic Peninsula at about 60 0 S, which is outside the region where light constraints are most strongly felt. Climate and Vegetation Most information comes from woods. 78 mm. He attributed the uneven growth pattern to reaction wood due to gravitational stimulus, but also admitted that it might have been caused by mutual shading, implying a partially closed canopy forest. While clearly some of Jefferson's trees were displaced from the vertical, many were not.

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