Biogeography and Regional Classifications of Antarctica
In this chapter we refer to the ‘Antarctic’ in its widest sense. On land, we include the Antarctic continent and Peninsula, the various archipelagos of the Scotia arc, and the […]
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In this chapter we refer to the ‘Antarctic’ in its widest sense. On land, we include the Antarctic continent and Peninsula, the various archipelagos of the Scotia arc, and the […]
The deep sea is the largest environment on the planet, the least well known and one of the least studied. It contains extremely large habitats, and millions of km2 of […]
It is widely accepted that marine biogeography is largely shaped by direct effects of temperature (Angel, 1991; Murawski, 1993). Temperature also influences biodiversity patterns at various latitudes (e.g.,Royet al.,1998; Astorga […]
The Southern Ocean (Figure 11.1) is a major component within the global ocean and climate system. It not only unites the Atlantic Ocean with the Indian and Pacific Oceans, but […]
The continental shelf is the platform for many of the planet’s most productive ecosystems but it is exposed to high disturbance. At high latitudes, massive grounded ice sheets have extended […]
Analysis of the operation of ocean ecosystems requires an understanding of how the structure of the ecosystem is determined by interactions between physical, chemical and biological processes. Such analysis needs […]
The Antarctic Peninsula is one of three areas of the globe currently experiencing rapid regional climate change (King, 1994; Smith et al., 1996, King & Harangozo, 1998; Vaughan et al., […]
The Antarctic continent is almost entirely covered by a vast icecap that reaches 4 km in thickness. Despite this, the continent possesses a remarkable array of lake ecosystems, many of […]
An interpolated bedrock topography is presented for Flask Glacier, one of the tributaries of the remnant part of the Larsen B ice shelf, Antarctic Peninsula. The ice thickness distribution is […]
Antarctic terrestrial biodiversity is challenged by rapid climatic changes and expansion of the human footprint. As well as the potential for environmental damage at the local level, these challenges are […]
Chemosynthetic primary production by microbes supports abundant faunal assemblages at deep-sea hydrothermal vents, with zonation of invertebrate species typically occurring along physico-chemical gradients. Recently discovered vent fields on the East […]