Title Influences on and origins of terrestrial biodiversity of the sub-antarctic islands
Author Convey, P.
Author Affil Convey, P., British Antarctic Survey, Cambridge, United Kingdom. Other: University of Tasmania, Australia
Source Papers and Proceedings of the Royal Society of Tasmania, Vol.141(Part 1), p.83- 93, ; Forum on the sub-Antarctic, Hobart, Tasmania, Australia, July 6-7, 2006, edited by P.M. Selkirk, P.G. Quilty and M. Davies. Publisher: Royal Society of Tasmania, Hobart, Tasmania, Australia. ISSN: 0080- 4703
Publication Date Nov. 2007
Notes In English. 124 refs. GeoRef Acc. No: 284184. CRREL Acc. No: 62004629
Index Terms animals; ecology; human activity; Indian Ocean Islands--Crozet Islands; Indian Ocean Islands--Kerguelen Islands; West Pacific Ocean Islands--Macquarie Island; Indian Ocean Islands--Prince Edward Island Group; Atlantic Ocean Islands--South Georgia; Southern Ocean; Atlantic Ocean Islands; biodiversity; biota; Crozet Islands; Indian Ocean Islands; Kerguelen Islands; Macquarie Island; Prince Edward Island Group; Scotia Sea Islands; South Georgia; subantarctic regions; terrestrial environment; West Pacific Ocean Islands
Abstract The "sub-Antarctic" is a region of the planet characterised by small and extremely isolated island landmasses set in the vastness and harsh conditions of the Southern Ocean. Although there is no universally applicable definition of the sub-Antarctic, based on eco-climatic criteria (temperature and the presence/absence of trees or woody shrubs) a useful terrestrial biogeographic region can be defined that includes only those islands which lie close to the oceanic Antarctic Polar Frontal Zone (PFZ). These range between roughly 47°S and 54°S and include South Georgia in the South Atlantic sector of the Southern Ocean, Marion and Prince Edward islands, Iles Kerguelen and Crozet, and Heard and McDonald islands in the Indian Ocean sector, and Macquarie Island in the Pacific Ocean sector. These islands have widely differing origins and geological histories. This paper provides an overview of their biodiversity and of the major patterns in biogeography. The majority of islands are of relatively recent origin, and there are only very limited indications of a more ancient biogeographical history (Gondwana- breakup timescale) to be found in the contemporary biota. Amongst the sub-Antarctic biota, there are examples supporting two general hypotheses relating to their origin: the Insulantarctic and the multiregional scenarios. Sub-Antarctic terrestrial ecosystems, which are of biodiversity and conservation significance globally, are under considerable contemporary pressure through the twin influences of possible anthropogenic climate change, and the introduction and establishment of invasive non-indigenous species.
Publication Type conference paper or compendium article
Record ID 84020