| Despite, or
perhaps because of (Patterson 1981), an
excellent fossil record, the
relationships of the conifers to other
seed plants are still not entirely clear.
Whilst conifers have usually been
accepted as a monophyletic group
(Chaw et al. 1997; Stefanovíc
et al. 1998), some recent
phylogenetic studies have suggested that
extant conifers are paraphyletic, with
the Gnetales as sister to Pinus L.
(Bowe, Coat & dePamphilis 2000).
This result appears to be especially
strongly supported by mitochondrial and
chloroplast sequences (Chaw et al.
2000). However, in the absence of
any morphological evidence for such a
relationship, and with the great depth of
branching events within the gymnosperms
(>300 Ma), other workers (e.g. Graham,
S. W. et al. 2002) have suggested
that conifer paraphyly is a statistical
artefact of long branch attraction sensu
Felsenstein (1978). Graham et
al. considered that substitutions are
unlikely to provide useful phylogenetic
resolution in such an ancient group, and
instead sought evidence of major genomic
rearrangements to support hypotheses of
phylogenetic relationships (Graham, S. W.
et al. 2002). Within the
conifers, evidence is growing for a
sister-group relationship between the
Araucariaceae and a clade consisting of
the Podocarpaceae and the Phyllocladaceae
(Chaw et al. 1997; Stefanovíc
et al. 1998; Chaw et al.
2000). Recently, Graham et al.
(2002) reported that a unique
triplication of the rps7 gene on
the chloroplast genome defines a clade
containing all members of the
Podocarpaceae (including Phyllocladaceae)
and Araucariaceae. This group of
families is often referred to as the
southern conifers (e.g.
Enright & Hill 1995; Enright &
Ogden 1995; Hill & Brodribb 1999).
Within the
Araucariaceae itself, phylogenetic
relationships are not at well understood.
Different studies of different genes have
resolved different relationships between
the three genera Wollemia, Agathis
and Araucaria (including Eutassa
Salisb. sensu de Laubenfels
(2002)) (Gilmore & Hill 1997;
Setoguchi et al. 1998; Codrington
et al. 2002), although all studies to
date have supported the monophyly of each
of the larger genera. Setoguchi et
al. (1998) provided the most
comprehensive treatment so far of the
phylogeny of the family, based on the rbcL
gene, but their tree is poorly resolved,
and much of the phylogenetic structure
within Agathis is poorly
supported, with almost all of it
collapsing in the strict consensus tree.
Additionally, many of the taxa in their
study cannot be identified confidently as
the voucher material they cite is of
uncertain provenance or dubious
geographical locality. However,
their study does show support for
Jaffrés (1995) hypothesis that the
diversity of the Araucariaceae in New
Caledonia is the result of rapid
post-Eocene speciation of
neo-endemic lineages, rather than the
persistence of relictual palaeo-endemics.
Recent efforts at
a phylogeny of Agathis have not
sampled densely among the Malesian
species (Ryan & Whiffin 2002). Beyond
increased support for the Jaffré
hypothesis of the monophyly of the New
Caledonian species of Agathis
(Ryan & Whiffin 2002), contrary to
the taxonomic schemes of Page and
Whitmore (Page 1980; Whitmore 1980;
Whitmore & Page 1980) and de
Laubenfels (1988), no study has yet
recovered robust phylogenetic structure
within the genus: indeed, within both the
New Caledonian species of Araucaria
and the genus Agathis there is
remarkably little genetic differentiation
in the rbcL gene (Setoguchi et
al. 1998), although for one
Australian species of Araucaria
the 18S rRNA sequence, highly conserved
in many eukaryotes, provides a useful
marker for population level studies
(Graham, G. C. et al. 1996).
Almost all the
phylogenetic studies that have so far
been carried out on Agathis sequence
data have been conducted using only a
single specimen for each species
examined, with the notable exception of
that of Ryan & Whiffin (2002). Consequently,
there has been very little examination of
the issue of paraphyletic species (sensu
Crisp & Chandler 1996) in the genus
or the possible polyphyly of some of the
questionably distinct montane species of
Western Malesia (Waters & Farjon
2002). Ryan & Whiffin (2002)
suggested, on the basis of sampling
primarily cultivated material, that Agathis
montana de Laub. was paraphyletic
with respect to Agathis moorei (Lindl.)
Mast. Further phylogenetic studies,
with denser sampling both across the
genus and within species, will be
necessary to address these questions and
understand the relationships of the
Malesian species, as well as Agathis
macrophylla (Lindl.) Mast. and
Agathis silbae de Laub., on
geologically young islands, to those on
the Gondwanan fragments of New Caledonia,
New Zealand, and Queensland, given that
the explanation offered by Whitmore &
Page (1980) lacks evidential support.
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