ZAPRIONUS
View in CoL
CLADE
The early branches within the major
Drosophila
clade indicate a Eurasian origin ( Fig. 2
View Figure 2
). Nevertheless, most early branches of this clade are restricted to Southeast Asia and the Pacific (SEA), strongly suggesting that the clade originated in the latter region (Table S2). The cosmopolitan
Drosophila busckii Coquillett, 1901
, which is sister to all remaining species, is the type species of the SEA subgenus
Dorsilopha
(see also Grimaldi, 1990; Robe et al., 2010).
Samoaia leonensis Wheeler & Kambysellis, 1966
, a member of the Pacific genus
Samoaia
, is the next species to diverge from the remaining lineages. Geographical consistency and morphological data indicate that
Samoaia
is monophyletic, but the type species,
Samoaia ocellaris Malloch, 1934
, was unavailable. Therefore, the status of this genus remains to be ascertained ( Grimaldi, 1990; O’Grady & DeSalle, 2008). The remaining lineage divides to form the
Zaprionus
clade and the main
Drosophila
cluster ( Fig. 1
View Figure 1
).
The
Zaprionus
View in CoL
clade includes the SEA
Liodrosophila aerea Okada, 1956
View in CoL
, which joins the clade consisting of the SEA
Drosophila repletoides (Carson & Okada, 1980)
plus
Zaprionus
View in CoL
. The
repletoides
species group is currently unassigned to higher rankings ( Yassin, 2013), but our topology suggests that it belongs to the
Zaprionus
View in CoL
clade (see also Van der Linde et al., 2010).
Zaprionus
View in CoL
and
Samoaia
View in CoL
are currently assigned to the
Zaprionus
View in CoL
genus group ( Grimaldi, 1990; Yassin et al., 2010), but our results suggest that
Samoaia
View in CoL
is sister to a much larger group that includes
Hirtodrosophila
View in CoL
,
Dichaetophora
View in CoL
,
Mycodrosophila
View in CoL
, the Hawaiian Drosophilid clade, the subgenera
Siphlodora
and
Drosophila
View in CoL
, and the
Zaprionus
View in CoL
clade. Because the type species of
Zaprionus
View in CoL
(
Zaprionus vittiger Coquillett, 1901
View in CoL
) and
Liodrosophila
View in CoL
(
L. aerea
View in CoL
) were sampled, our results indicate that these genera belong to the
Zaprionus
View in CoL
clade (see also O’Grady & Markow, 2009).
Our timescale shows that during the early Oligocene, an Old World
Zaprionus
View in CoL
ancestor diverged to form the subgenera
Anaprionus (Eurasia)
and Zap- rionus (Africa). Our time estimates imply that the Oligocene
Zaprionus
View in CoL
radiation did not prevent the Miocene radiation of the
melanogaster
subgroup, but may have impeded the radiation of the African
ananassae
and
montium
lineages, which remained undiversified ( Fig. 2
View Figure 2
). The difference in the
melanogaster
subgroup may be related to distinct ancestral ecological requirements or to sampling error; these alternatives remain to be tested using additional data.
In a recent Bayesian molecular analysis, one
Zaprionus species
(
Zaprionus
K1) clustered with high support in a clade that included
Drosophila funebris (Fabricius, 1787) (Yassin et al., 2010)
. In our tree, however,
Zaprionus
is monophyletic, and
D. funebris
clusters elsewhere. Furthermore, Bayesian analyses are known to inflate clade support, and their statistical support may not hold if more consistent statistical tests are performed ( Suzuki et al. 2002). Even so, because this undescribed
Zaprionus species
was not included in our data set, the current diagnosis for
Zaprionus
may not represent a true clade. In a recent review of African
Zaprionus, Yassin & David (2010)
proposed a new definition of the species groups within
Zaprionus
based on morphological and molecular data. Their classification agrees well with our major
Zaprionus
clades ( Fig. 2
View Figure 2
), except that
Zaprionus tsacasi Yassin, 2008
(from the
inermis
group) is tightly clustered with
Zaprionus taronus Chassagnard & Tsacas, 1993
(from the
vittiger
group), well inside the
vittiger
clade.