THE
ASTERINIDAE
View in CoL
,
GANERIIDAE, AND
SOLASTERIDAE
The
Asterinidae
View in CoL
has occupied a controversial position in the history of asteroid classification, having been placed in
Spinulosida
View in CoL
in Fisher (1911) and others (e.g. Sladen, 1889) but later independently reassigned to the
Valvatida
View in CoL
by Blake (1987) and Gale (1987b). Classification and revision within the
Asterinidae
View in CoL
has been a constant source of activity (e.g. A.M. Clark, 1983; O’Loughlin & Waters, 2004), but the distinctive morphology of asterinids has generally suggested a derived and potentially monophyletic assemblage with only limited subdivision (e.g. the
Tremasterinae Sladen, 1889
View in CoL
; Anseropodinae Fisher, 1906; summary in Spencer & Wright, 1966). Waters et al. (2004a) provided the first molecular phylogenetic treatment of the
Asterinidae
View in CoL
that included taxa beyond
Asterina
View in CoL
+
Patiriella
View in CoL
, using mitochondrial COI, 12S, and 16S rRNA data, primarily from Australasian taxa. Their phylogenetic tree did not support monophyly for the
Asterinidae
View in CoL
, but was the basis for subsequent far-reaching taxonomic revisions ( O’Loughlin & Waters, 2004).
Basal relationships in the large clade subtended by node P in Figure 1
View Figure 1
were mostly unresolved. Somewhat better resolution was obtained in the two-gene tree ( Fig. 2
View Figure 2
) for some groups, such as
Parvulastra
View in CoL
and
Kampylaster
View in CoL
+
Anseropoda antarctica
View in CoL
. However, support for all basal nodes in the asterinid clade of our two-gene tree (i.e. those subtended by node 1 in Figure 2
View Figure 2
) was also relatively poor (<50%), suggesting that basal relationships within this group will require further study. However, when placed into the context of greater taxonomic sampling, our phylogenetic results mirror the results of Waters et al. (2004a) and cast substantial doubt on the monophyly of the
Asterinidae
View in CoL
. This strongly suggests that the
Asterinidae
View in CoL
, as traditionally defined, is a paraphyletic assemblage. The stemward positions on node P of all the asterinid taxa suggest that they occupy a relatively plesiomorphic condition, forming more of a grade relative to more derived taxa, such as the solasterids and the ganeriids. This represents a significant shift in perception of the
Asterinidae
View in CoL
, which has historically been supported by distinct morphological autapomorphies and has been perceived more as a derived, terminal branch (e.g. Blake, 1987; Gale, 1987b) rather than as an ancestral grouping.
Several of the other phylogenetic and taxonomic results produced by Waters, O’Loughlin & Roy (2004a) and O’Loughlin & Waters (2004), especially the monophyly of the higher branches, such as
Meridiastra
,
Patiria
,
Paranepanthia
,
Aquilonastra
, and
Parvulastra
, are upheld by our results. The basal branches in Waters, O’Loughlin & Roy (2004a) are clarified in our results.
Dermasterias
, which was shown embedded within the ingroup
Asterinidae
, is clearly removed from the
Asterinidae
by our trees. Our examplar species of
Nepanthia
,
Nepanthia grangei
, differs from that of Waters, O’Loughlin & Roy (2004a) who used
Nepanthia troughtoni
but our result shows
Nepanthia
as the sister to the ganeriid
Tarachaster australis
.
Tremaster
View in CoL
has traditionally been placed in the
Asterinidae
View in CoL
but has been separated by some workers (e.g. Sladen, 1889; Smith & Tranter, 1985) into the
Tremasterinae
View in CoL
, which included
Tremaster
View in CoL
,
Stegnaster
View in CoL
, and two fossil tremasterines ( Spencer & Wright, 1966). Jangoux (1982) disagreed with this classification and removed
Stegnaster
View in CoL
from the
Tremasterinae
View in CoL
, a conclusion that is consistent with our mitochondrial-only tree ( Fig. 2
View Figure 2
). Available data support
Tremaster
View in CoL
as a divergent lineage within the
Asterinidae
View in CoL
with uncertain affinities.
Derived members of the ‘asterinid’ clade include primarily former members of the
Solasteridae
View in CoL
and the
Ganeriidae
, plus the
Leilasteridae
View in CoL
. The solasterid + asterinid relationship, as supported by molecular data, was first observed by Wada, Komatsu & Satoh (1996) and later developed by Matsubara et al. (2004). The presence of ganeriid taxa, such as
Cycethra
and
Perknaster
, within the asterinid clade is consistent with historical classifications that have demonstrated affinities between asterinids and ganeriids. The
Ganeriidae
have always been supported as similar to or morphologically close to the
Asterinidae
View in CoL
. Early classifications (e.g. Sladen, 1889) included
Cycethra
and
Ganeria
as members of the Ganeriinae, part of a subfamily within the
Asterinidae
View in CoL
. This affinity has been further supported by contemporary morphology-based phylogenies ( Blake, 1987; Gale, 1987b). Further sampling will be necessary to test the monophyly and affinities of the
Ganeriidae
.
The
Solasteridae, sensu A. M. Clark (1996)
View in CoL
was largely supported as monophyletic with the sole exception of the Antarctic
Cuenotaster involutus
, which was included as the sister clade to the ganeriid
Perknaster
. Although much work remains to be completed regarding this question, some morphological characters are consistent with
Cuenotaster
as a member of the
Ganeriidae
.
Jurassic fossils are known for taxa within the clade subtended by node P (
Solasteridae
View in CoL
+
Asterinidae
View in CoL
+
Ganeriidae
+
Leilasteridae
View in CoL
) but are limited to the
Asterinidae
View in CoL
and the
Solasteridae
View in CoL
. Asterinid fossils are limited to those showing affinities with
Tremaster
View in CoL
in the subfamily
Tremasterinae
View in CoL
.
Tremaster
View in CoL
is supported on a long branch as sister group to a clade containing
Nepanthia
View in CoL
and
Tarachaster
View in CoL
( Fig. 2
View Figure 2
). Tremasterine fossils, such as
Mesotremaster felli Hess, 1972
View in CoL
and
Mesotremaster zbindeni Hess, 1981
View in CoL
from Germany and
Protremaster uniserialis Smith & Tranter, 1985
View in CoL
from Antarctica have been collected from Jurassic strata. Nontremasterine asterinid fossils are unknown.
Plesiosolaster
(described as
Brachisolaster
View in CoL
) moretonis was re-described and discussed by Blake (1993) and further discussed by Villier, Charbonnier & Bernard (2009) from the Jurassic of England and is the only well-preserved fossil solasterid known. Although a full phylogenetic analysis was not undertaken, Blake hypothesized that the multiarmed condition for solasterids was derived relative to a more ancestral
Lophaster
View in CoL
or
Rhipidaster
View in CoL
-like morphology. Blake’s hypothesis is consistent with our phylogenetic tree ( Figure 1
View Figure 1
). This may imply that the lineage containing multiarmed taxa (
Solaster
View in CoL
and
Crossaster
View in CoL
) may be closely associated with the Jurassic occurrence of multiple arms in the
Solasteridae
View in CoL
.