Journal of Systematics and Evolution
47 (5): 431–443 (2009)
doi: 10.1111/j.1759-6831.2009.00039.x
Phylogeny and evolution of Perezia (Asteraceae: Mutisieae:
Nassauviinae)
1
Beryl B. SIMPSON∗
1
2
Mary T. K. ARROYO 1 Sandra SIPE
1
Joshua McDILL
3
Marta DIAS de MORAES
(Integrative Biology and Plant Resources Center, The University of Texas, 1 University Station A6700, Austin, TX 78712, USA)
2
(Facultad de Ciencias, Universidad de Chile, Casilla 653, Santiago de Chile, Chile)
3
(Universidade Federal do Acre, Campus Floresta, Cruzeiro do Sul, Acre, Brazil)
Abstract A molecular phylogenetic analysis of most of the species of Perezia reveals that, as traditionally defined,
the genus is not monophyletic with two species more closely related to Nassauvia than to Perezia. In addition,
our results show that Burkartia (Perezia) lanigera is related to Acourtia and is the only member of that clade
in South America. The remaining species are monophyletic and show a pattern of an early split between a western
temperate and an eastern subtropical clade of species. Within the western clade, the phylogeny indicates a pattern
of diversification that proceeded from southern, comparatively low-elevation habitats to southern high-elevation
habitats, and ultimately into more northern high-elevation habitats. The most derived clades are found in the high
central Andes, where significant radiation has occurred.
Key words Andes, biogeography, Mutisieae, Nassauviinae, Perezia.
Perezia Lag., a genus of 30–35 primarily highelevation species, occurs exclusively in South America,
primarily in the central and southern Andes, and thus
constitutes a useful model for examining the evolution
of high-elevation floras in South America. Considered
until 1970 (Vuilleumier, 1970) to be the nominate section of a larger genus that also included Perezia section
Acourtia (D. Don) A. Gray, a North American taxon,
Perezia is now known to be distinct from Acourtia
D. Don and more closely related to South American
genera. Species of Perezia occur from sea level in Chile
and eastern Argentina to over 4000 m above sea level
(a.s.l.) in Bolivia and Peru and from Tierra del Fuego
to Colombia. Species range across most of the high
Andean habitats, except true páramo, with plant habit
often correlated with habitat. The genus has historically
included large foliose species that occur in the Nothofagus forests of the southern cone and in the Paraguay–
southern Brazil–Uruguay basin, as well as tiny rosettes
that grow in the very high-elevation puna of central
Bolivia.
Perezia is a member of the Nassauviinae, a subtribe of the Mutisieae with 25–27 exclusively America
genera (Hind, 2007). Perezia is the fifth largest genus in
the subtribe (Crisci, 1980). Vuilleumier (1970) monographed the group (as Perezia sect. Perezia; the other
∗
C
Received: 11 March 2009 Accepted: 2 May 2009
Author for correspondence. E-mail: beryl@mail.utexas.edu; Tel.: 512-4714335; Fax: 512-23-29529.
2009 Institute of Botany, Chinese Academy of Sciences
section, Acourtia, having been monographed previously
by Bacigalupi in 1931). In the 1970 monograph, Vuilleumier recognized 30 species. Since that work was published, four species have been added (or re-added) to
the genus based on morphology, namely P. lanigera
Hook. and Arn. (but see below), P. eryngioides (Cabrera) Crisci & Marticorena (described as a Trixis but
transferred to Perezia by Crisci and Marticorena), P.
catharinensis Cabrera, and P. volcanensis Cabrera. Two
species placed by Vuilleumier (1970) in synonymy under P. purpurea (i.e. P. atacamensis Phil. and P. burkartii Cabrera) were treated as distinct species by Cabrera
(1978). Of these taxa, Perezia lanigera Hook. & Arn.
has engendered the most controversy. The entity was
originally described as a Perezia but, in her monograph,
Vuilleumier (1970) excluded it from the genus because
of its aspect and the presence of wooly trichomes in the
leaf axils. No Perezia species has this type of trichome.
However, Cabrera (1971) considered these trichomes of
little importance and consistently treated the species as
a Perezia. Crisci (1976), like Vuilleumier (1970), considered the taxon distinct and erected the monotypic
genus Burkartia Crisci for it, with the comment that
Lophopappus Rusby was its closest relative.
In 1970, Vuilleumier suggested a potential relationship between Perezia and Leucheria Lag. based on
morphology. Cassini (1825) had earlier placed Perezia
with Holocheilus Cass., Leucheria, and Trixis P. Browne
in a subgroup of one of his three sections of the
Nassauviinae, but Crisci (1974) was the first to address relationships of the genera within the subtribe
432
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Vol. 47
No. 5
in a rigorous way. He scored a wide array of discrete
characters, five geographical and 85 morphological (including pollen shape and exine patterning), for 26 taxa
that he used in a numerical taxonomic study. In that
study, he used various combinations of two different
scoring methods and two different measures of similarity to generate three cladograms (Crisci, 1974). The
results were, in general, concordant with one another
and allowed him to draw several conclusions. One of
the conclusions was that the two sections of Perezia
were not “close” to one another and should be treated as
distinct genera (as suggested previously by Vuilleumier
1970). Second, he commented that Nassauvia and Triptilion were very closely “related”, as well as that Perezia
lanigera was more closely “related” to a cluster containing Proustia Lag., Lophopappus Rusby, Acourtia, and
Gochnatia glomeriflora A. Gray than to Perezia. Finally,
the results suggested that Perezia and Leucheria were
each rather isolated within the subtribe, possibly as a
“result of the great spectrum of types presented by the
two genera” (Crisci, 1974). Shortly after Crisci’s study,
Reveal and King (1973) formally re-elevated Acourtia
to generic status and provided the necessary new combinations for the caulescent species. A few years later,
Turner (1978) moved the North American scapiform
Perezia species into Acourtia.
Six years after his numerical taxonomic study,
Crisci (1980) used the same data set to produce phylogenetic hypotheses of relationships in the Nassauviinae.
Character polarity was determined based on several criteria and trees were constructed using a Wagner tree
algorithm. Three trees were produced, each with a different outgroup. With a hypothetical outgroup, Perezia
was sister to Panphalea DC. and Holocheilus was sister
to this pair. This same relationship was produced when
Trixis was used as the outgroup. With Dolichlasium Lag.
as the outgroup, Perezia was sister to a clade consisting
of Panphalea Lag., Moscharia Ruı́z & Pavón, Polyachyrus Lag., Calopappus Meyen, Nassauvia Comm.
ex Juss., and Triptilion Ruı́z & Pavón.
Within the past 10 years, there have been two published molecular studies that included several members
of the subtribe Nassauviinae. Using ndhF sequence data
and including representatives of Acourtia, Adenocaulon
Hook., Jungia L.f., Leucheria, Nassauvia, Perezia, and
Triptilion, Kim et al. (2002) reported that the Nassauviinae had only weak support as a clade but that within
the subtribe there were several well-supported subclades, one of which included Perezia as sister to a Nassauvia/Triptilion clade. Acourtia was sister to a clade
containing Trixis and Proustia (although this relationship collapsed in the strict consensus tree). Leucheria
was in a third clade, sister to Jungia. In a more re-
2009
cent study, Katinas et al. (2008) used internal transcribed spacer (ITS) and trnL-F sequence data to generate a phylogeny that they used to infer the evolution
of secondary heads in Nassauviinae. Their phylogeny
included 12 of the 25 genera of the tribe: Ameghinoa
Speg., Dolichlasium Lag., Holocheilus Cass., Jungia,
Leucheria, Moscharia, Nassauvia, Panphalea, Perezia
(four species), Polyachyrus Lag., Proustia Lag., and
Triptilion. Their results showed Perezia as sister to Panphalea and this clade sister to a clade of Nassauvia plus
Triptilion. In a paper circumscribing a segregate genus
of Perezia, namely Calorezia Panero, Panero (2007),
stated that his unpublished data showed that Perezia nutans Less. (and, by association, P. prenanthoides Less.)
was more closely related to Calopappus Meyen, Nassauvia, and Triptilion than to the rest of Perezia and,
hence, necessitated a new genus. Panero (2007) considered these three genera along with Panphalea and
Perezia to form a “Perezia clade”, called the Perezia
group in our discussions.
Within Perezia, only Vuilleumier (1970) has made
inferences about species relationships. In her 1970 revision, she conducted a numerical taxonomic study of
the genus using 24 numerical and 23 non-numerical
characters that were measured or scored for over 1200
herbarium specimens. Each species was usually represented by several different “populations” (two or more
specimens from the same locality). Each of these populations was designated as a terminal taxonomic unit,
with the numerical characters of each unit represented
by a mean and variance (calculated from the cluster of
specimens measured in the population). These values
were used to generate dendrograms based on a Mahalanobis’ generalized distance matrix. The dendrograms
were rooted by the a priori placement of P. pungens (H.
& B.) Less. as the first taxonomic unit. Perezia nutans
and P. prenanthoides and P. multiflora (H. & B.) Less.
and similar leafy species tended to be at the base of the
dendrogram, but most of the remainder of the terminal
units (populations) came out stepwise with terminal taxonomic units of several variable species scattered across
the dendrogram. Although there were some cohesive
clusters, the dendrograms did not provide easily interpretable relationships among the terminal taxonomic
units included.
Using the generalized distances as a rough guide
and combining them with the morphology underlying
them, Vuilleumier (1970) suggested six species groups
shown in Fig. 1 with distributions indicated in Fig. 2: A,
B. Assessing these groups together with paleoecological data, Vuilleumier (1970) postulated that the genus
arose early in the Tertiary in the warm open forests that
covered extratropical South America. Specifically, she
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2009 Institute of Botany, Chinese Academy of Sciences
SIMPSON et al.: Phylogeny of the Andean genus Perezia
433
Fig. 1. Species groups modified from Vuilleumier (1970). Note that the prenanthoides and the multiflora groups were considered quite distinct, whereas
taxa such as Perezia pilifera and Perezia carduncelloides could not be placed with certainty.
Fig. 2. Distribution of the species groups of Perezia (A) as delineated by Vuilleumier (1970) and the number of species in various parts of the generic
distribution (B). The species of the former prenanthoides group are excluded, but their distribution is indicated by the brackets that show the northern
and southern limits of their distribution in the Nothofagus forests of southern South America. The additional species of the multiflora group added after
1970 are included in both A and B.
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2009 Institute of Botany, Chinese Academy of Sciences
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suggested that the ancestral Perezia was similar in habit
to Perezia pungens and inhabited mid-to-low elevation
montane habitats of what is now the central Andes. As
drying began in the mid-Tertiary, Vuilleumier (1970)
postulated a split leading to the ancestor of the multiflora group in southern Brazil–eastern Argentina, the
ancestor of the prenanthoides group in the Nothofagus
forest, and the ancestor of the remaining species initially
at mid altitudes in the central Andean region. She suggested that this last group radiated in the high Andes and
southern Patagonia with speciation linked to drying in
the late Tertiary, the uplift of the Andes, and Pleistocene
climatic fluctuations.
Our purpose here is to generate hypotheses of infrageneric species relationships of Perezia using molecular data in order to assess the directions of change in
habit and habitat, and to test the patterns of relationships suggested by Vuilleumier (1970). To establish a
phylogeny that allows us to examine these patterns, we
have included most of the species of Perezia. Based
on the studies of Kim et al. (2002), Panero (2007),
and Katinas et al. (2008), we have included species of
Acourtia, Nassauvia, Panphalea, and Triptilion (all previously linked with Perezia in various ways), as well as
Adenocaulon and Lophopappus, two other genera in the
Nassauviinae.
1 Material and methods
1.1 Material
Material was obtained from herbarium specimens
(with permission) or collected in the field. Vouchers
and GenBank numbers are listed in Table 1. Included
in the ingroup were 28 of the 30–35 species of Perezia,
two accessions of Burkartia (Perezia) lanigera, the two
former species of Perezia now placed in Calorezia,
seven species of Acourtia, five species of Nassauvia,
three species of Adenocaulon, and one species each of
Leucheria, Panphalea, and Triptilion. Leucheria was
designated as the outgroup for the purposes of rooting.
1.2 Methods
1.2.1 DNA Sequencing DNA was isolated from
herbarium specimens or silica-dried leaf material using
a modified cetyltrimethylammonium bromide (CTAB)
protocol (Loockerman & Jansen, 1996). A PCR was
used to amplify the ITS region using primers P1 and
P4 of Kim and Jansen (1994), with internal primers (P2
and P3) also used for amplification or sequencing when
necessary.
The chloroplast intergenic spacers rpl32–ndhF and
trnL(UAG)–rpl32 were chosen based on their rates of
evolution and degree of phylogenetic utility as reported
2009
by Shaw et al. (2007) and Timme et al. (2007). Pereziaspecific internal primers were designed for the present
study to assist with amplification and sequencing when
necessary. The sequences of the primers used for these
regions are given in Table 2.
The PCR reactions contained 2.5 µL of 10× PCR
buffer; 2 µL of a 10 mmol/L stock solution of combined dNTPs, 2–4 µL of 25 mmol/L MgCl2 , 0.25 µL
of a 25 µmol/L stock solution of each forward and reverse primer, 2 µL of 3.3% (w/v) bovine serum albumin
(BSA), 1 unit Taq polymerase, 2–8 µL of 1:10 diluted
template DNA extract, and water to a final volume of
25 µL. For amplification of ITS, 1.25 µL dimethylsulfoxide (DMSO) was added to the reaction. Annealing
temperatures ranged between 45 ◦ C and 52 ◦ C depending on primers and template. The PCR reaction products were purified using exonuclease I and shrimp alkaline phosphatase to degrade unincorporated primers
and dNTPs (Werle et al., 1994), and then sequenced via
BigDye (v. 3.1) Terminator Cycle Sequencing (Applied
Biosystems, Foster City, CA, USA) at the Institute for
Cell and Molecular Biology Core Facility at the University of Texas (Austin, TX, USA).
Forward and reverse sequence reads were assembled into contigs and edited in Sequencher 4.5
(GeneCodes Corp., 2005), whereas the chloroplast sequences were aligned manually in MacClade 4.08 (Maddison & Maddison, 2005), and ITS sequences were
aligned using default settings in MUSCLE (Edgar,
2004), followed by manual adjustments in MacClade.
1.2.2 Phylogenetic analyses The three data matrices
were analyzed separately and in combination using maximum parsimony (MP) with PAUP∗ 4.0b10 (Swofford,
2002), Bayesian inference (BI) using MrBayes 3.1.2
(Huelsenbeck & Ronquist, 2001), and maximum likelihood (ML) with GARLI (Zwickl, 2006). Areas of uncertain alignment were excluded from all analyses, as were
autapomorphic insertions. The sequenced portions of
the 18S and 25S ribosomal subunits were also excluded
from the ITS matrix.
In PAUP, all characters were treated as equally
weighted and unordered, with gaps treated as missing data. The MP tree searches were conducted using the heuristic search option with 1000 randomaddition replicates and tree bisection–reconnection
(TBR) branch swapping, with no limitations placed on
the number of trees swapped to completion, and all
other settings at defaults. For MP bootstrapping, 500
bootstrap replicates were performed using the heuristic search option with one random addition replicate
and swapping to completion on a maximum of 10 000
trees. The incongruence length difference (ILD) test
(Farris et al., 1995), implemented in PAUP as the
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2009 Institute of Botany, Chinese Academy of Sciences
SIMPSON et al.: Phylogeny of the Andean genus Perezia
Table 1
Sources of material
Taxon
Acourtia coulteri (A. Gray)
Reveal & R.M. King
A. microcephala DC.
A. nana (A. Gray) Reveal &
R.M. King
A. purpusii (Brandegee) Reveal
& R.M. King
A. scapiformis (Bacigalupi)
Reveal & R.M. King
A. runcinata (D. Don) B. L.
Turner
A. wrightii (A. Gray) Reveal &
R.M. King
Adenocaulon bicolor Hook.
A. chilense Less.
A. lyratum S.F. Blake
Calopappus acerosus Meyen
Leucheria bridgesii Hook. &
Arn.
Lophopappus foliosus Rusby
Nassauvia aculeata Poepp. &
Endl.
N. digitata Wedd.
N. heterophylla (Phil.) Reiche
N. lagascae F. Meigen
N. pinnigera D. Don
Panphalea cardaminifolia Less.
Perezia atacamensis (Phil.)
Reiche∗
P. calophylla (Phil.) Reiche
P. carduncelloides Griseb.
P. carthamoides (D. Don)
Hook. & Arn.
P. ciliaris Hook. & Arn.
P. ciliosa (Phil.) Reiche
P. cirsiifolia Wedd.∗
P. coerulescens Wedd.
P. fonkii (Phil.) Reiche
P. integrifolia Wedd.∗
P. kingii Baker
P. lactucoides lactucoides
(Vahl) Less.
P. lactucoides ssp. palustris
(Phil.) Vuill.
P. lanigera Hook. &
Arn.∗ ∗ = Burkartia lanigera
(Hook. & Arn.) Crisci
P. linearis Less.
P. lyrata (Remy) Wedd.
P. magellanica (L.f.) Less.
P. mandonii Rusby
P. megalantha Speg.
P. multiflora (H. & B.) Less.
P. (Calorezia) nutans Less.∗
P. pedicularidifolia Less.
P. pilifera (D. Don) Hook. &
Arn.
P. pinnatifida (Humb. &
Bonpl.) Wedd.
P. pungens (Humb. & Bonpl.)
Less.
P. (Calorezia) prenanthoides
Less.∗ ∗
P. purpurata Wedd.
C
435
Voucher
Origin
Herbarium
GenBank No.
ITS
trnL–rpl32
rpl32–ndhF
H.H. Iltis 30784
Tamaulipas, Mexico
TEX
FJ979680
FJ979729
FJ979781
T. Ross 6616
B.L. Turner 7-22-07
California, USA
Texas, USA
TEX
TEX
FJ979679
FJ979682
N/A
FJ979732
FJ979780
FJ979784
G.B. Hinton 23607
Nuevo Leon, Mexico
TEX
FJ979681
FJ979730
FJ979782
J. Calzada 21592
Oaxaca, Mexico
TEX
FJ979683
FJ979733
FJ979785
W. M. Turner 76
Texas, USA
TEX
FJ979684
FJ979734
FJ979786
E.J. Lott 4829
Texas, USA
TEX
N/A
FJ979731
FJ979783
G. Helmkamp K-17
Ricardi & Marticorena 1923
D. E. Breedlove 13424
J. Panero & B. Crozier 8457
W. D. Clark 1350
Idaho, USA
Malleco, Chile
Chiapas, Mexico
Los Andes, Chile
Santiago, Chile
TEX
F
F
TEX
TEX
FJ979672
FJ979674
FJ979673
FJ979685
FJ979675
FJ979722
FJ979724
FJ979723
FJ979735
FJ979725
FJ979773
FJ979775
FJ979774
FJ979787
FJ979776
Sanders et al. 3325
Marticorena et al. 74
Jujuy, Argentina
Curico, Chile
TEX
F
FJ979676
FJ979688
FJ979726
FJ979738
FJ979777
FJ979790
K. Gengler et al. 11
C.P. Cowan 4250
C.P. Cowan 4238
C.P. Cowan 4239
M. Dias de Moraes 832
M.K. Arroyo et al. 94014
Reg. XIII, Chillan, Chile
Farellones, Chile
Farellones, Chile
Farellones, Chile
Santa Catarina, Brazil
Reg. II Atacama, Chile
TEX
TEX
TEX
TEX
TEX
CONC
FJ979690
FJ979687
FJ979686
FJ979691
FJ979669
FJ979657
FJ979740
FJ979737
FJ979736
FJ979741
FJ979719
FJ979707
FJ979792
FJ979789
FJ979788
FJ979793
FJ979770
FJ979758
B. S. Vuilleumier 189
B. B. Simpson 6-II-00-1
E. Wall s.n
Rio Negro, Argentina
Tucuman, Argentina
Mendoza, Argentina
GH
TEX
GH
N/A
FJ979655
FJ979641
FJ979700
FJ979705
FJ979692
FJ979751
FJ979756
FJ979742
St. Beck et al. 18088
St. Beck 26317
I. Henson 830
E. Garcia 886
Weigend et al. 6824
X. Menhofer X-1900
Rosengurth PE5334
O. Dollenz 648
Cochabamba, Bolivia
Arequipa, Peru
Cochabamba, Bolivia
La Paz, Bolivia
Rio Negro, Argentina
La Paz, Bolivia
Florida, Uruguay
Magellanes, Argentina
LPB
LPB
LPB
LPB
NY
LPB
GH
GH
FJ979644
FJ979645
FJ979646
FJ979649
FJ979660
FJ979654
FJ979667
FJ979659
FJ979694
FJ979695
FJ979696
FJ979699
FJ979710
FJ979704
FJ979717
FJ979709
FJ979745
FJ979746
FJ979747
FJ979750
FJ979761
FJ979755
FJ979768
FJ979760
B. Vuilleumier 204
Rio Negro, Argentina
GH
FJ979642
N/A
FJ979743
S. Albert 8-XI-2006-1
S. Albert 8-XI-2006-2
Santa Cruz, Argentina
Santa Cruz, Argentina
TEX
TEX
FJ979677
FJ979678
FJ979727
FJ979728
FJ979778
FJ979779
Pirion 3499
Marticorena et al. 194
O. Dollenz 708
I. Henson 1505
E. Pisano V. 5602
M. Madison 1044
J. Wen 7472
F. Jaffuel 3795
M.T.K. Arroyo 20680
Aisen, Chile
Reg. VII Talca, Chile
Isla Wollaston, Argentina
Cochabamba, Bolivia
Cerro Corona, Argentina
Cuzco, Peru
Chile
Chillan, Chile
Yerba Loca, Chile
GH
CONC
GH
LPB
GH
GH
F
GH
CONC
FJ979664
FJ979666
FJ979661
FJ979647
FJ979651
FJ979652
FJ979671
FJ979662
FJ979658
FJ979714
FJ979716
FJ979711
FJ979697
FJ979702
N/A
FJ979721
FJ979712
FJ979708
FJ979765
FJ979767
FJ979762
FJ979748
FJ979753
N/A
FJ979772
FJ979763
FJ979759
Hutchison 4250
Lima, Peru
GH
FJ979650
FJ979701
FJ979752
S. King et al. 285
Urubamba, Peru
GH
FJ979653
FJ979703
FJ979754
G. Seijo 1671
Neuquen, Argentina
NY
FJ979670
FJ979720
FJ979771
St. Beck 31111
Oruro, Bolivia
LPB
FJ979643
FJ979693
FJ979744
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436
Table 1
Journal of Systematics and Evolution
Vol. 47
No. 5
2009
Continued
Taxon
Voucher
Origin
Herbarium
GenBank No.
ITS
trnL–rpl32
rpl32–ndhF
P. recurvata (Vahl) Less.
E. Pisano V. 4045
Patagonia, Argentina
GH
FJ979663
FJ979713
FJ979713
P. squarrosa ssp. cubaetensis
O.S. Ribas et al. 2152
Parana, Brazil
TEX
FJ979668
FJ979718
FJ979769
(Less.) Vuill.
P. sublyrata Domke
J. L. Luteyn & L. Door 13773
La Paz, Bolivia
TEX
FJ979656
FJ979706
FJ979757
P. virens (D. Don) Hook. & Arn.
E. Wall 29.XII.1946
Aconcagua, Chile
NY
FJ979648
FJ979698
FJ979749
P. viscosa Less.
G. Montero O. 1304
Cautin, Chile
GH
FJ979665
FJ979715
FJ979766
Triptilion spinosum Ruiz &
Para & Rodriguez 109
Concepcion, Chile
F
FJ979689
FJ979739
FJ979791
Pavon
∗
Vuilleumier (1970) placed P. atacamensis in P. purpurata and P. cirsiifolia and P. integrifolia in P. coreulescens. Specimens referable to these synonyms
are included here because of doubt expressed by Vuilleumier about their placement.
∗∗
These species have been moved to the genera indicated in parentheses. The authorities listed here are for the original description in Perezia. In the
monograph of the genus.
N/A, not applicable.
Table 2
Primers used to amplify and sequence chloroplast intergenic spacers
Region
ndhF–rpl32
rpl32–trnL
Primer
Sequence (5′ –3′ )
Reference
ndhF
316A
316B
602A
602B
906A
906B
rpl32-R
rpl32-F
432A
432B
534A
534B
649A
649B
trnL (UAG)
GAA AGG TAT KAT CCA YGM ATA TT
GAG CAA GGA TAA AAA ATT AC
GTA ATT TTT TAT CCT TGC TC
CRT ATC CTT TAA CAG ATT K
MAA TCT GTT AAA GGA TAY G
GAG AGA TAA AGA ACG AGA AY
RTT CTC GTT CTT TAT CTC TC
CCA ATA TCC CTT YYT TTT CCA A
CAG TTC CAA AAA AAC GTA CTT C
CCC ATC GAC CTT TAC AAT AA
TTA TTG TAA AGG TCG ATG GG
GAA ATT CAT TGA TTC CAT G
CAT GGA ATC AAT GAA TTT C
GCY CAA AAC AGA ACT TAA TAG
CTA TTA AGT TCT GTT TTG RGC
CTG CTT CCT AAG AGC AGC GT
Shaw et al., 2007
Present study
Present study
Present study
Present study
Present study
Present study
Shaw et al., 2007
Shaw et al., 2007
Present study
Present study
Present study
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Shaw et al., 2007
partition homogeneity test, was used to assess conflict
between the chloroplast and nuclear data, with 100 replicates performed using the heuristic search option under
the same constraints as used for MP bootstraps.
In GARLI, 100 bootstrap replicates were performed for each marker and for the combined matrix,
using default settings and the GTR+G+I model. Bootstrap values were determined from a 50% majority rule
consensus of the best trees found in each bootstrap
replicate.
Prior to analysis in MrBayes, the number of substitution types and applicability of gamma rate heterogeneity (G) or invariant sites (I) for each marker were determined with the MrModelTest (Nylander, 2004) using
the Akaike Information Criterion (AIC). In MrBayes,
each marker was subjected to four million generations of
MCMC sampling, with tree topology, estimated model
parameters, and likelihood score saved every 100 generations and the automated diagnostic statistic comparing the parameters from two simultaneous runs every
ten-thousandth generation (with the first 25% of generations excluded as “burn-in”). Chain heating and priors
for model parameters were kept at default values, ex-
cept for the nucleotide frequency prior, which was set
to a dirichlet distribution. For the combined data analysis in MrBayes, the matrix was partitioned to apply
the appropriate substitution model (G) and I to each
marker; partition model parameters were unlinked and
allowed to vary independently for each partition, except
for branch length and topology. All Bayesian analyses
were terminated at four million generations as long as
the automated diagnostic statistic (average standard deviation of split frequencies) was below 0.01 by that time.
Runs were also checked for stationarity in the post-burnin sample by graphical plotting of −ln L scores against
generation time. Clade posterior probabilities were determined from a 50% majority rule consensus of the
post-burn-in sample of 60 000 trees (30 000 sampled
during stationarity from each simultaneous run).
2 Results
2.1 Sequence characteristics
Sequences of the ITS could not be obtained
from Perezia calophylla and Acourtia wrightii. Perezia
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SIMPSON et al.: Phylogeny of the Andean genus Perezia
Table 3
Marker
Parameters for the DNA markers used in the present study
Aligned
length
Included
bp
Variable
sites
rpl32
1049
829
265
ndhF–rpl32
1229
991
284
Combined CPL
2278
1820
549
ITS
762
599
315
CPL+ITS
3040
2419
864
N/A, not applicable; ITS, internal transcribed spacer; CPL, chloroplast loci.
lactucoides subsp. palustris and Acourtia microcephala
were lacking sequence from the rpl32–trnL intergenic
spacer, and Perezia multiflora was missing sequence
from both chloroplast markers. Table 3 provides descriptive statistics from parsimony analyses of the data
matrices assembled for the present study and the ML
substitution model type selected. Figure 3: A, B shows
the majority rule consensus trees for the Bayesian
analyses.
The parsimony-based ILD test indicated significant conflict between the chloroplast and ITS data partitions (P = 0.01). Topological incongruences between
the chloroplast and ITS (Fig. 3: A, B), mostly affecting placement of outgroup taxa, are discussed below.
Consequently, we combined our data to generate the
phylogeny shown in Fig. 4.
2.2 Phylogenetic results
Figure 3 shows a comparison between the phylogenies generated with the combined chloroplast markers and the sequences from ITS 1 and 2. Considering
Perezia, several discrepancies should be noted. First,
in the chloroplast (cp) DNA tree (Fig. 3: A), P. lactucoides is sister to P. megalantha, whereas the ITS data
(Fig. 3: B) show this species in a polytomy with the
majority of the species of the genus. However, we were
not able to obtain one of the chloroplast sequences from
P. lactucoides subsp. palustris, which probably led to
this difference. Second, P. virens in the chloroplast tree
(Fig. 3: A) is part of a polytomy with members of the
high Andean clade; however, in the ITS tree (Fig. 3: B)
it branches much lower in the cladogram and is sister
to P. linearis. Third, P. ciliosa is in an unresolved clade
with P. cirsiifolia and P. atacamensis in the chloroplast
tree (Fig. 3: A) but is sister to a clade of P. integrifolia,
P. pinnatifida, and P. purpurata in the ITS tree (Fig. 3:
B). Fourth, P. viscosa is part of a clade with P. linearis, P. pilifera, and P. recurvata in the chloroplast tree
(Fig. 3: A) and in a clade with P. lyrata and P. pedicularidifolia in the ITS tree (Fig. 3: B). The latter placement
seems more reasonable in terms of morphology. Finally,
P. coerulescens is in a completely unresolved clade of
central Andean species in both analyses, but the members of that clade differ in the two trees (Fig. 3: A, B).
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2009 Institute of Botany, Chinese Academy of Sciences
Informative
sites
Mean GC
content (%)
Substitution
model
168
154
322
238
560
24.14
23.69
25.03
56.15
33.17
GTR+G
GTR+G
N/A
GTR+I+G
N/A
Common to both analyses is the position of the P. multiflora group as sister to or in a basal polytomy with
the remaining members of the genus (Fig. 3: A, B).
Similarly, in the cp analysis (Fig. 3: A) there is a basal
grade of comparatively low elevation, generally humid
habit, southern South American species (P. calophylla
and P. fonkii) subsequent to the P. multiflora group,
whereas in the ITS tree (Fig. 3: B) the multiflora group
and several southern South American species (P. fonkii,
P. magellanica, and P. megalantha) form a polytomy
basal to the remaining species.
The prenanthoides group (= Calorezia) is distinct
from Perezia, although the chloroplast data (Fig. 3: A)
place it as sister to a clade of Calopappus, Nassauvia,
and Triptilion and the ITS (Fig. 3: B) places it as sister to the entire Perezia clade. In both analyses, Perezia
lanigera (= Burkartia) shows a strong relationship with
Acourtia, with the chloroplast data indicating it is sister
to Acourtia and the ITS data suggesting that it is embedded within Acourtia. Both show Nassauvia paraphyletic
with respect to Triptilion. Although other genera were
not sampled thoroughly, our data suggest that Panphalea
is always strongly supported as sister to Perezia.
The combined tree (Fig. 4) strongly supports the
multiflora group as sister to the rest of Perezia (Fig. 4:
a; note, the lowercase letters refer to labeled clades in
Fig. 4). It also shows a grade (Fig. 4: b, b′ ) of low elevation, humid habitat southern South American species
(P. fonkii, P. magellanica + P. megalantha) that is sister
to a clade (Fig. 4: c) containing the remaining species of
the genus. This large clade (Fig. 4: c) consists of a basal
polytomy of southern (south of approximately 40◦ S, except for P. pilifera, which has a distribution that extends
from 30◦ to 55◦ S latitude) species (P. lyrata + P. pedicularidifolia, a recurvata clade plus P. viscosa (Fig. 4: d),
P. calophylla, P. lactucoides) sister to a clade of central Andean species (Fig. 4: e). Perezia virens and subsequently P. carthamoides, the basal members of this
clade, occur relatively further south (∼35◦ S) than the
other members of this clade. All members of the most
derived clade (Fig. 4: f) occur from northwest Argentina
to Ecuador and all occur in high Andean habitats.
In the combined analysis, Panphalea is sister
to Perezia, Perezia (Burkartia) lanigera is sister to
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Fig. 3. Cladograms from the Bayesian majority rule consensuses constructed using (A) combined chloroplast DNA data and (B) internal transcribed spacer (ITS) data. The
Perezia group is the clade containing Acourtia, Burkartia, Calopappus, Calorezia, Nassauvia, Perezia, Panphalea, and Triptilion. Numbers above branches are the Bayesian
posterior probabilities. Numbers below the lines are the maximum likelihood/maximum parsimony bootstrap values.
SIMPSON et al.: Phylogeny of the Andean genus Perezia
439
Fig. 4. Bayesian majority rule cladogram based on the combined chloroplast and internal transcribed spacer (ITS) data. Numbers above branches are
the Bayesian posterior probabilities. Numbers below the lines are the maximum likelihood/maximum parsimony bootstrap values. The lowercase letters
refer to clades discussed in the text. The circles show latitudinal limits, with black circles indicating geographical distributions north of 30◦ S and white
circles showing distributions south of 30◦ S. Circles that are half black and half white indicate distributions that occur both north and south of 30◦ S. The
squares represent elevation, with black squares showing altitudinal distributions above 2500 m and white squares altitudinal distributions below 2500 m.
Squares that are half black and half white show that the elevational distribution of a species extends from below 2500 m to higher elevations.
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Acourtia, the prenanthoides group (Calorezia) is sister to a clade of Calopappus, Nassauvia, and Triptilion,
and Triptilion is embedded within Nassauvia.
3 Discussion
3.1 Phylogenetic relationships among species of
Perezia
Our finding that Perezia prenanthoides/nutans do
not cluster with the remainder of Perezia was not surprising given the fact that the two differ in habit and
habitat from all other Perezia species and were considered “isolated within the genus” by Vuilleumier (1970).
They are large (to 84 cm) branched, soft-leaved, caulescent species that occur in the Nothofagus forest of southern Chile, reaching the subalpine in central Chile. They
also have an “Acourtia” type of style branches (Crisci,
1974), unlike the species of Perezia. Thus, the segregation of this group into the separate genus Calorezia
(Panero, 2007) is justified, but our data (not shown)
for several samples of both species suggest that only
one species rather than two may be involved. Calopappus (often treated as a synonym of Nassauvia; Hind,
2007), one of the genera closest to Calorezia according
to Panero (2007), occurs above the treeline in the central
Chilean Andes. Nassauvia itself is primarily southern
South American. Although we sampled only five of the
38+ species, our data suggest that Nassauvia is paraphyletic with respect to Triptilion and that the latter
should be included within Nassauvia.
Our data confirm that Burkartia (Perezia) lanigera,
as suggested by Vuilleumier (1970), is not a Perezia.
Moreover our data indicate that it should either be considered a monophyletic genus (Burkartia, cf. Crisci,
1976) sister to the North American genus Acourtia
or perhaps a member of Acourtia because, according
to some of our phylogenetic reconstructions, Acourtia is paraphyletic with respect to Burkartia (Fig. 3:
B). Morphological characters that B. lanigera shares
with Acourtia but not with Perezia include a shrubby
habit, subsessile capitula, capitula with six to 14 florets, pubescent corolla, wooly trichomes, and a Trixis
Lag. type of pollen exine (Crisci, 1974). Until Acourtia
is more fully studied, we retain Burkartia as a monophyletic genus, but note that this is the only clade in
the Perezia group that has a New World amphitropical
disjunct distribution.
These new data enable the clarification of the
evolution of Perezia. Contrary to Vuilleumier’s (1970)
suggestions that the Perezia pungens group is “basal”
(= sister) to the rest of the genus, the Perezia multiflora group is clearly the sister to the rest of Perezia s.s.
2009
Table 4
Chromosome numbers of members of the Perezia clade
Chromosome Source∗
number
Taxon
Acourtia belizeana B. L. Turner
n = 18
1
A. carpholepis (A. Gray) Reveal & R. M.
∼27 pairs
1
King
A. nana (A. Gray) Reveal & R. M. King
n = 27
1
A. microcephala DC.
2n = 54
3
A. rigida DC.
n = 26
1
A. scapiformis (Bacig.) B.L. Turner
∼27 pairs
2
A. thurberi (A. Gray) Reveal & R. M. King
2n = 54
1
A. wrightii (A. Gray) Reveal & R. M. King
n = 27
1
Nassauvia aculeata var. robusta (Cabrera)
n = ∼44
1
Cabrera
N. axillaris D. Don
n = 11
1
N. chubutensis Speg.
n = 11
1
N. darwinii (Hook. & Arn.) O. Hoffm. &
n = 11
1
Dusén
N. gaudichaudii Cass.
2n = 22
2
N. glomerulosa D. Don
n = 11
1
N. lagascae F. Meigen
n = 11
1
N. magellanica J. F. Gmel.
n = 11
2
N. pygmaea (Cass.) Hook. f.
n = 11
1
N. revoluta D. Don
n = 11
1
N. serpens d’Urv.
n = 11
2
N. uniflora (D. Don) Hauman
n = 11
1
Panphalea bupleurifolia Less.
n=8
1
Perezia calophylla (Phil.) Reiche
2n = 24
3
P. carduncelloides Griseb.
2n = 24
3
P. ciliaris Hook & Arn.
2n = 24
3
P. ciliosa (Phil.) Reiche
2n = 24
2
P. coerulescens Wedd.
2n = 24
3
Perezia magellanica (L.f.) Lag.
n = 24
2
P. multiflora (Humb. & Bonpl.) Less.
n=8
1, 3
Perezia “nivalis” Wedd.
2n = 24
4
P. pedicularidifolia Less.
2n = 24
1
P. pilifera (D. Don. & Arn.) Hook.
n = 16
1
P. pungens (Humb. & Bonpl.) Less.
2n = 28
1, 3
P. recurvata (Vahl) Less.
2n = 24
1, 3
P. squarrosa ssp. cubaetensis (Less.) Vuill.
n=4
2
Triptilion gibbosum Remy
2n = 20
1
∗
Sources for the information as are follows: 1, Index to Plant
Chromosome Numbers (IPCN; available at http://mobot.mobot.org/
W3T/Search/ipcn.html, accessed 15 September 2008) and/or batch files
at that URL; 2, Crisci (1974); 3, Vuilleumier (1970); 4, Bolkhovskikh
et al. (1969).
(Fig. 4). This placement is consistent with the chromosome numbers (Table 4) known for species of this group:
2n = 8 for P. squarrosa subsp. cubaetensis and 2n = 16
for P. multiflora compared with 2n = 24 for the remaining species studied. Like most members of the multiflora
group, species of Panphalea (the sister genus to Perezia)
are also large (20–100 cm tall), have leafy stems,
and inflorescences of numerous small heads (Cabrera, 1953). In addition, the only chromosome count
made for that genus (Panphalea bupleurifolia) is n = 8
(Table 4).
Most of the Perezia species (those sister to the
multiflora group) form a clade with either a grade of
species of southern humid and alpine habitats (P. fonkii,
followed by a clade of P. magellanica plus P. megalantha) sister to the remaining species (Fig. 3: A) or with
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SIMPSON et al.: Phylogeny of the Andean genus Perezia
a basal polytomy of southern species (Fig. 3: B). Thus,
most of the species of the magellanica group of Vuilleumier (1970) constitute a grade rather than a group or
clade. The combined analysis supports the recurvata
group (Fig. 4: d) of Vuilleumier (1970) plus P. viscosa.
The members of the recurvata group are small loose
cushion-forming, narrow-leaved (often spiny) plants
(Vuilleumier, 1970), with P. viscosa anomalous morphologically in this group with its basal rosette of broad
oblanceolate leaves reminiscent of other members found
in Nothofagus forest. This clade and several other taxa
placed in the magellanica and pungens groups (Fig.
1) form a polytomy with a large clade of species that
occur from northwestern Argentina to Ecuador. This
northern clade contains a mixture of species placed in
the pungens and coerulescens groups by Vuilleumier
(1970).
3.2 Biogeographic implications
Considering the results as a whole, the confirmation that the prenanthoides group is sister to Calopappus and Nassauvia plus Triptilion strongly suggests that
the Perezia group (the clade of Calopappus, Nassauvia,
Panphalea, Perezia, and Triptilion) arose in southern,
probably southwestern, South America. However, Panphalea, the sister genus to Perezia, occurs in eastern Argentina and adjacent Uruguay and Paraguay. The species
of the multiflora clade, sister to the majority of Perezia
also occur predominantly in southeastern South America, with P. kingii occurring in northeastern Argentina
and Uruguay, P. squarrosa Less. in extreme southeastern Brazil and Uruguay, and both P. eryngioides and
P. catharinensis in Santa Catarina, Brazil. Within this
group of five species, only P. multiflora itself extends its
distribution westward into dry high regions of the central
Andes (and accounts for the seemingly broad distribution of this group; Fig. 2: A). Therefore, it would appear
that following the origination of the Perezia group, there
was a spread or dispersal into eastern subtropical South
America with either a recolonization of the southwestern Andes or a later radiation of an ancestral stock in
southwestern South America. Although the cladogram
in Fig. 4 suggests the former, it is possible that inclusion
of more species of both Panphalea and the multiflora
group will show these to be sister and consistent with
the second pattern.
The three species that branch sequentially to the
multiflora clade form a grade of taxa that occur in
relatively low-elevation moist forest or humid steppe
habitats south of 30◦ S. Although there is little resolution among the high Andean species (Fig. 4: c), it is
evident that the high-elevation species are the most derived and that the genus is of temperate South American
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2009 Institute of Botany, Chinese Academy of Sciences
441
origin, radiating in western South America from south
to north and from low to high elevation (Fig. 4).
As far as we can tell, the pattern we found in
Perezia does not completely match that of any temperate/Andean plant genus studied phylogenetically to
date. The most similar pattern to that of Perezia was
shown in a recent study by Hershkovitz et al. (2006a) for
the 20 species of Tropaeolum L. sect. Chilensia Sparre
(Tropaeolaceae). Although plagued by problems of uncertain rooting, the data of Hershkovitz et al. (2006a)
also indicate an east–west split in a basal clade (eastern Argentina, southern Chile). The remaining species
are primarily Chilean and show a pattern of diversification from southern mesophytic areas to central Mediterranean scrub habitats to northern deserts. However,
it should be noted that species of this section rarely
reach the elevations of many Perezia taxa (over 4000 m
a.s.l.) and,, unlike Perezia, Tropaeolum consists of 90
species, most of which (70 species) occur in tropical
America.
A molecular study of Chaetanthera Ruı́z & Pavón,
an Andean/Patagonian genus of the Mutisieae (Hershkovitz et al., 2006b), found some high-elevation
species to be derived from lowland stock, whereas others were interpreted to be relictual, migrating upward on
account of increasing aridity in the central Andes. In addition, a number of the lower-elevation species in southcentral Chile were found to be more derived. Regardless
of differences, Chaetanthera, like Perezia, underwent a
major species radiation in high-elevation habitats in the
more arid areas of the central Chilean Andes and puna.
In the small Andean genus Schizanthus (Solanaceae),
lowland species were shown to have diverged more recently than the few alpine species in that genus (Perez
et al., 2006). Yet another pattern is seen in Hamadryas,
a small dioecious, predominantly alpine genus of four
species in the Patagonian component of the Ranunculus
grade of Ranunculaceae. Its closest relatives are found
in the alpine of southern South America, Asia, North
America, and South Africa (Hoot et al., 2008). Finally,
a study of Ourisia (Plantaginaceae) by Meudt (2006)
and Meudt and Simpson (2007) indicated an origin in
south-central America (∼34◦ S) at mid elevation (800–
2400 m a.s.l.) and a subsequent spread both south and
north in the Andes as well as to New Zealand, where a
subsequent significant radiation occurred.
Clearly, rigorous phylogenies of many more groups
need to be performed before we can say whether the
Perezia or one of the other patterns is most commonly
found in genera with a predominance of species in temperate and high Andean regions of South America. It
is possible that the evolutionary patterns of radiation
are related to the location of the ancestors of the groups
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Vol. 47
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studied. Genera (clades) with tropical Andean ancestors
may commonly show the basal members of the clade to
be mesophytic with lowland xerophytic species derived,
whereas groups originating in temperate areas may commonly show patterns of late radiation in the very high
supraforest habitats of the tropical Andes.
Acknowledgements The authors are grateful for the
sample of Perezia lanigera supplied by Serge AUBERT
(Directeur du Jardin Alpin du Lautaret, Lautaret,
France) and thank José PANERO (Integrative Biology,
The University of Texas, Austin, TX, USA) for generously providing a portion of his sample of Calopappus
acerosus. Jun WEN (Smithsonian Institution, Washington DC, USA) kindly supplied the specimen for material
of Perezia nutans. The figures in the present study were
drawn by JM (coauthor) and Gwen GAGE (Computer
Illustrator, The University of Texas). The authors also
thank the curators of GH, LPB, NY, and TEX for allowing sampling of material used in the present study.
MTKA acknowledges funding from ICM P05-002.
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