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Notes on the sea caves of sub-Antarctic Macquarie Island, Southern Ocean

Published online by Cambridge University Press:  04 December 2009

Stephen Harris ,
Geof Copson  and
Louisa d'Arville
Stephen Harris
Affiliation:
Resource Management and Conservation Division, Department of Primary Industries, Parks, Water and Environment, GPO Box 44, Hobart, Tasmania 7001, Australia ([email protected])
Geof Copson
Affiliation:
Red Chapel Avenue, Sandy Bay, Tasmania, Australia
Louisa d'Arville
Affiliation:
Kingston Beach, Tasmania 7001, Australia
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Abstract

Caves of marine origin occur in tectonically uplifted stacks on the coastal terrace and in plateau edge cliffs at a number of locations around Macquarie Island. Some of the caves have been located and their distributions mapped. Four of the best known caves are mapped in detail. Aspects of their geology, structure and biology, including speleothem development, clastic deposits, faunal remains and subfossil deposits are explored. Many of these caves contain deposits, which may have the potential to be investigated, as beach and peat deposits have been, for dating key time periods in the island's evolution. The palaeoenvironmental research potential of the sea caves on Macquarie Island has yet to be exploited. Further knowledge about these caves will assist in the understanding of the processes that have acted on Macquarie Island and other polar and sub-polar islands.

Type
Research Article
Information
Polar Record , Volume 46 , Issue 2 , April 2010 , pp. 136 - 145
Copyright
Copyright © Cambridge University Press 2009

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References

Adamson, D.A., Selkirk, P.M., Price, D.M., Ward, N., and Selkirk, J.M.. 1996 Pleistocene uplift and palaeoenvironments of Macquarie Island: evidence from palaeobeaches and sedimentary deposits. In Banks, M.R., and Brown, M.J. (editors). Climate succession and glacial history of the southern hemisphere over the last five million years. Papers and Proceedings of the Royal Society of Tasmania 130 (2): 25–32.CrossRefGoogle Scholar
Anderson, E.A. 1978. Cave survey and map standards. ASF Newsletter 79: 1–18.Google Scholar
Australian Antarctic Data Centre. 2004. Macquarie Island 1:50000 topographic map. Hobart: Australian Antarctic Division, Department of Environment and Heritage.Google Scholar
Colhoun, E.A., and Goede, A.. 1973. Fossil penguin bones, C14 dates and the raised marine terrace of Macquarie Island: some comments. Search 4: 499–501.Google Scholar
Cumpston, J.S. 1968. Macquarie Island. Melbourne: Department of Internal Affairs, Antarctic Division (ANARE scientific reports, series A (1)).Google Scholar
Griffin, B.J. 1982. Igneous and metamorphic petrology of lavas and dykes of the Macquarie Island ophiolite complex. Unpublished Ph.D. dissertation, University of Tasmania, Department of Geology.Google Scholar
Kiernan, K., and McConnell, A.. 1999 Geomorphology of the sub-Antarctic Australian territory of Heard Island-McDonald Island. Australian Geographer 30 (2): 159–165.CrossRefGoogle Scholar
Kiernan, K., and McConnell, A.. 2000. Management considerations for the Heard Island lava tube caves. Papers and Proceedings of the Royal Society of Tasmania 133 (2): 13–22.CrossRefGoogle Scholar
Kiernan, K., and McConnell, A.. 2008. Periglacial processes on Heard Island, southern Indian Ocean. Papers and Proceedings of the Royal Society of Tasmania 141 (2): 1–12.CrossRefGoogle Scholar
Kiernan, K., McConnell, A., and Yates, A.. 1998. Tube-fed pahoehoe lava flow features of Azorella Peninsula, Heard Island, southern Indian Ocean. Polar Record 24 (190): 225–235.CrossRefGoogle Scholar
Langenegger, O., and Verwoerd, W.J.. 1971. Topographic survey. In: Van Zinderen Bakker, Snr. E.M., Winterbottom, J.M., and Dyer, R.A.. Marion and Prince Edward Islands. Cape Town: A.A. Balkema (report on the South African biological and geological expedition 1965–1966).Google Scholar
Ledingham, R., and Peterson, J.A.. 1984. Raised beach deposits and the distribution of structural lineaments on Macquarie Island. Papers and Proceedings of the Royal Society of Tasmania 118: 223–235.CrossRefGoogle Scholar
Meredith, C. 1985. A search for fossil seabirds on Macquarie Island. Australasian Seabird Group Newsletter 22.Google Scholar
Oliver, R.L., Finlay, H.J., and Fleming, C.A.. 1950. The geology of Campbell Island. Wellington; DSIR (Cape expedition series, bulletin 3).Google Scholar
Otvos, E.G. 1976. ‘Pseudokarst’ and ‘pseudokarst terrains’: problems of terminology. Geological Society of America Bulletin 87 (7): 1021–1027.2.0.CO;2>CrossRefGoogle Scholar
Parks and Wildlife Service. 2006. Macquarie Island nature reserve and World Heritage Area management plan, Hobart: Parks and Wildlife Service: Department of Tourism, Arts and the Environment.Google Scholar
Selkirk, P.M., Seppelt, R.D., and Selkirk, D.R.. 1990. Subantarctic Macquarie Island: environment and biology. Cambridge: Cambridge University Press (studies in polar research).Google Scholar
Sutton, G. 1958. Glacier Island. Edinburgh: Travel Book Club Edition.Google Scholar
Terauds, A., and Stewart, F.. 2008. Subantarctic wilderness: Macquarie Island. Crows Nest: Jacana/Allen and Unwin.Google Scholar
Townrow, K. 1987. Settlers, sealers and scientists: archaeological survey of Macquarie Island, summer 1986/87. Tasmania: Department of Lands, Parks and Wildlife (unpublished report).Google Scholar
Varne, R., and Rubenach, M.J.. 1973. Geology of Macquarie Island in relation to tectonic environment. In: Coleman, P.J. (editor). The western Pacific island arcs, marginal seas, geochemistry. Perth: University of Western Australia Press: 535–541.Google Scholar
Vestjens, W.J.M. 1963. Remains of the extinct banded rail at Macquarie Island. The Emu 62: 249–250.CrossRefGoogle Scholar