New Zealand Journal of Zoology abstracts
Scree weta phylogeography: surviving glaciation and implications for
Pleistocene biogeography in New Zealand
STEVEN A. TREWICK*
Department of Zoology
University of Otago
P. O. Box 56
Dunedin, New Zealand
*Present address:
Department of Plant and Microbial Sciences,
University of Canterbury, Private Bag 4800, Christchurch, New Zealand.
Abstract The Pleistocene glaciation is thought to have had a
profound impact on the distribution of endemic biota. The intraspecific
phylogeography of the alpine-adapted scree weta,
Deinacrida
connectens Ander, was surveyed throughout its range in the South Island,
New Zealand using mitochondrial cytochrome oxidase I DNA sequence data. Seven
distinct genetic lineages were evident from mtDNA haplotypes, with each
occupying mountain ranges in discrete geographic regions. Genetic distances
among lineages were up to 8.2%, whereas within-lineage distances reached only
2.8%. The inferred age of lineages and the striking phylogeographic structure
exhibited by
D. connectens indicates that it radiated in response to
Pliocene mountain building. Maintenance of this structure is likely to relate
to the combined effects of mountain-top isolation during Pleistocene
interglacials and ice barriers to dispersal during glacials. Two lineages are
endemic to the central South Island, an area regarded as species poor due to
glacial-extirpation of much of the biota. It appears that
D.
connectens survived across much of the South Island in a mosaic of
ecological, rather than one or few, regional refugia. The Pleistocene
biogeography of New Zealand in general is discussed in the light of this
hypothesis.
Keywords alpine; mitochondrial DNA; COI; phylogeography;
Pleistocene glaciation
Z00027
Received 2 August 2000; accepted 10 April 2001
New Zealand Journal of Zoology, 2001, Vol. 28: 291-298
0301-4223/01/2803-0291 $7.00/0 (c) The Royal Society of New
Zealand 2001
PDF file of entire paper: medium quality (687K); (scanned from paper original: notes about this process)
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