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Evolution and biogeography of Lyallia and Hectorella (Portulacaceae), geographically isolated sisters from the Southern Hemisphere

Published online by Cambridge University Press:  16 August 2007

Steven J. Wagstaff  and
Françoise Hennion
Steven J. Wagstaff*
Affiliation:
Allan Herbarium, Landcare Research, PO Box 40, Lincoln 7640, New Zealand
Françoise Hennion
Affiliation:
UMR Ecobio, Université de Rennes 1, CNRS, Av du Général Leclerc, F-35042 Rennes, France
*
*Corresponding author:wagstaffs@landcareresearch.co.nz
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Abstract

The Southern Hemisphere contains many monotypic taxa, for which phylogenetic relationships are important to illuminate biogeographical history. The monotypic genus Lyallia is endemic to the sub-Antarctic Iles Kerguelen. A close relationship with another monotypic taxon, the New Zealand endemic Hectorella, was proposed. They share a dense cushion growth habit with small coriaceous leaves that lack stipules. The solitary flowers are bicarpellate with two sepals, 4–5 petals, 3–5 stamens and a bifid style. The fruit is an indehiscent capsule with 1–5 seeds. The flowers of Lyallia kerguelensis are hermaphroditic with four petals and three stamens whereas the flowers of Hectorella caespitosa are female, male or hermaphroditic, with five petals and five stamens. Lyallia kerguelensis is rare on Kerguelen, whereas Hectorella caespitosa is confined to the South Island of New Zealand. Our phylogenetic analysis of trnK/matK intergenic spacer and rbcL sequences provides evidence supporting a close relationship between Lyallia and Hectorella. The two species form a well-supported clade that is nested within the Portulacaceae. Divergence estimates suggest they shared a common ancestor during the late Tertiary long after the fragmentation of Gondwana. Such relationships underscore the importance of transoceanic dispersal and extinctions for plant evolution in the Southern Hemisphere.

Keywords

cushion plantdisjunct pairsdivergence timesMiocenemolecular phylogenysub-Antarctic
Type
BIOLOGICAL SCIENCES
Information
Antarctic Science , Volume 19 , Issue 4 , December 2007 , pp. 417 - 426
Copyright
Copyright © Antarctic Science Ltd 2007

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