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ORIGINALARTICLE
Hidden phylogeographic complexity
in the Sierra Madre Oriental: the case
of the Mexican tulip poppy Hunnemannia
fumariifolia (Papaveraceae)
Victoria Sosa*, Eduardo Ruiz-Sanchez and Flor C. Rodriguez-Gomez
Departamento de Biologia Evolutiva, Instituto
de Ecologia, Veracruz, Mexico
*Correspondence: Victoria Sosa, Departamento
de Biologia Evolutiva, Instituto de Ecologia,
A. C., Apartado Postal 63, 91000 Xalapa,
Veracruz, Mexico.
E-mail: [email protected]
ABSTRACT
Aim A phylogeographic study of the endemic Mexican tulip poppy
Hunnemannia fumariifolia (Papaveraceae) was conducted to determine: (1) the
historical processes that influenced its geographical pattern of genetic variation;
(2) whether isolation by distance was one of the main factors that caused genetic
divergence in populations of this species; and (3) whether genetic flow still exists
between populations from northern arid zones (Chihuahuan Desert and Sierra
Madre Oriental) and those from southern arid zones (Tehuacan-Cuicatlan
Valley) – populations that are separated by the Transvolcanic Belt.
Location Xerophytic vegetation in Mexico.
Methods Chloroplast DNA (cpDNA) sequences of three regions, trnH-psbA,
rpl32-trnL(UAG) and ndhF-rpl32, were obtained for 85 individuals from 17
populations sampled in the field, covering the entire range of H. fumariifolia. The
evolutionary history of these populations was investigated using a nested clade
phylogeographic analysis and also by conducting various population genetic
analyses.
Results In total, 17 haplotypes were detected, 14 of which were found in the
Sierra Madre Oriental. Differentiation among populations based on cpDNA
variation (GST = 0.787, SE 0.0614) indicated population structure in
H. fumariifolia, corroborated by a fixation index (FST) of 0.907. Results from
analysis of molecular variance found that most of the total variation (90.71%,
P < 0.001) was explained by differences among populations. Three regions were
determined based on geological correspondence – the Chihuahuan Desert, Sierra
Madre Oriental and Tehuacan-Cuicatlan Valley – and the variation between them
was significant (43.39%, P < 0.001). Results of a Mantel test showed a significant
correlation between genetic and geographic distances (r = 0.511; P = 0.0001),
suggesting a pattern of isolation by distance, which was corroborated by nested
clade phylogeographic analysis. Mismatch distribution analysis indicated a
sudden demographic expansion.
Main conclusions Our study found that isolation by distance influenced
genetic divergence in populations of H. fumariifolia. The finding that allopatric
fragmentation influenced genetic divergence in populations in the Sierra Madre
Oriental may be a reflection of the complex geology of the area. Our results
suggest that the areas located in the north of the Sierra Madre Oriental acted as
post-glacial refugia for some populations.
Keywords
Allopatric fragmentation, Chihuahuan Desert, contiguous range expansion,
long-distance dispersal, Mexico, phylogeography, post-glacial refugia, Sierra
Madre Oriental, Tehuacan-Cuicatlan Valley.
Journal of Biogeography (J. Biogeogr.) (2009) 36, 18–27
18 www.blackwellpublishing.com/jbi ª 2008 The Authors
doi:10.1111/j.1365-2699.2008.01957.x Journal compilation ª 2008 Blackwell Publishing Ltd
INTRODUCTION
In Mexico, the Late Eocene, middle to Late Miocene and
Pleistocene were characterized by cooling climates (Graham,
1987). The mid-Pleistocene was drier than the Late Pleistocene
in the desert areas of Mexico, where there were extensive
palaeolakes (Metcalfe, 2006). In contrast, climatic changes
during the Late Pleistocene and Holocene were smaller in
magnitude than those occurring in other parts of the tropics
and subtropics (Metcalfe et al., 2000). However, northern
Mexico was much wetter than it is at present as a result of
winter rain from the mid-latitudes (Metcalfe et al., 2000,
2002).
The centre of Mexico comprises the Mexican Plateau, which
is crossed by mountain ranges and segmented by deep rifts.
The plateau is bordered by two mountain ranges, the Sierra
Madre Oriental and the Sierra Madre Occidental, which
converge south of the plateau (Fig. 1). The Transvolcanic Belt
is a large mountain range running from west to east in central
Mexico (Fig. 1). It harbours 13 of the highest peaks of Mexico.
Many valleys and basins divide the Transvolcanic Belt, which is
considered to be a group of active volcanic mountains of
recent origin.
Topographic diversity, climate change, and access to both
temperate and tropical source areas account for the diverse
flora and vegetation of Mexico (Rzedowski, 1978, 1993).
A great proportion of the endemic flora of Mexico is located in
the country’s arid regions (Rzedowski, 1993). The majority of
desertic vegetation is located in the north, but the southern
Tehuacan-Cuicatlan Valley and the Balsas River Basin also
possess xerophytic habitats (Rzedowski, 1978). The largest
desert is the Chihuahuan Desert, which covers most of
northern-central Mexico and extends northwards across
western Texas and southern New Mexico (Schmidt, 1979).
The Chihuahuan Desert and the Tehuacan-Cuicatlan Valley
are separated by the Transvolcanic Belt (Fig. 1). It has been
argued that the Tehuacan-Cuicatlan flora is phytogeographi-
cally related to that of other semi-arid regions, among them
the Chihuahuan Desert (Smith, 1965; Villasenor et al., 1990).
We selected the only species of the endemic Mexican
genus Hunnemannia (Papaveraceae) and conducted a phy-
logeographic study to investigate the evolutionary history of
plant populations distributed in northern and southern
desertic areas. The Mexican tulip poppy, Hunnemannia
fumariifolia Sweet, is a herbaceous perennial that grows in
xerophytic habitats. Hunnemannia is related to Eschscholzia
Figure 1 Geographical distribution of Hunnemannia fumariifolia in Mexico. Population numbers correspond to those in Table 1; haplo-
types to those in Table 2.
Phylogeography of Hunnemannia fumariifolia
Journal of Biogeography 36, 18–27 19ª 2008 The Authors. Journal compilation ª 2008 Blackwell Publishing Ltd
and Dendromecon and forms part of the Eschscholzioideae, a
group of genera from western North America and Mexico
(Hoot et al., 1997). Hunnemannia fumariifolia has a variable
morphology, varying mainly in the size of the plants and the
depth of the indentation of leaves. Small plants with deeply
incised leaves have been considered a different species
(H. hintoniorum, Nesom, 1992); however, these traits are
variable at the population level and are not limited to a
geographic area.
Hunnemannia is found in the Chihuahuan Desert, in the
Sierra Madre Oriental and also in the arid zone of the
Tehuacan-Cuicatlan Valley, growing on gypsum soils (Fig. 1).
The distribution of H. fumariifolia lies within the morphotec-
tonic provinces proposed by Ferrusquia-Villafranca (1993), i.e.
the Chihuahua-Cohauila Plateau, the Sierra Madre Oriental
and the Transvolcanic Belt.
Among methods to estimate gene flow and genetic popu-
lation divergence, nested clade phylogeographic analysis
(NCPA, Templeton et al., 1995), which takes into account
the processes that cause genetic differences in natural popu-
lations, is one of the most common in phylogeographic
studies. Furthermore, NCPA was intended to discriminate
among a wide array of processes and events that shape species
history, such as allopatric fragmentation, contiguous range
expansion, and restricted gene flow caused by isolation by
distance (Templeton et al., 1995). Despite some criticisms of
this method (Knowles & Maddison, 2002; Petit, 2008), NCPA
is still the only method with the potential for disentangling
multiple and overlying effects of historical and recurrent events
within a given data set (Templeton, 2004). In this phylogeo-
graphic study, NCPA was performed with ANeCA, one of the
most recent programs available (Panchal, 2007; Panchal &
Beaumont, 2007).
The aim of this study was to investigate the evolutionary
history of populations from the entire range of H. fumariifolia
based on three chloroplast DNA regions, namely rpl32-
trnL(UAG), ndhF-rpl32 and trnH-psbA, using a NCPA and
population genetic analyses. Three major questions are
addressed: (1) Which historical processes influenced the
geographical pattern of genetic variation in H. fumariifolia?
(2) Was isolation by distance one of the main factors that
caused genetic divergence in populations of this species?
(3) Does genetic flow still exist between populations from the
southern arid zones and those from the northern deserts –
populations that are separated by the Transvolcanic Belt?
MATERIALS AND METHODS
Sampling
A total of 85 individuals from 17 populations were sampled in
the field, in a north–south 900-km transect, covering the entire
geographical range of H. fumariifolia (Table 1). Three to seven
individuals were collected per population. Fresh leaves and
flowers were gathered from each individual, and dried in silica
gel.
DNA extraction, amplification, and sequencing
Total genomic DNA was isolated from silica-gel-dried leaf
tissue using the modified 2X CTAB method (Rogers &
Bendich, 1985; Doyle & Doyle, 1987). The chloroplast
spacers rpl32-trnL(UAG) and ndhF-rpl32 were amplified and
sequenced using the primers and protocols of Shaw et al.
(2007). The trnH-psbA region was amplified and sequenced
using primers trnH2 (Tate & Simpson, 2003) and psbA (Sang
et al., 1997) based on the protocols of Shaw et al. (2005).
Amplification products and DNA were purified using QIA-
quick columns (Quiagen, Valencia, CA, USA) following the
protocols provided by the manufacturer. Clean products were
sequenced using Taq BigDye terminator cycle sequencing kits
(Perkin Elmer Applied Biosystems, Foster City, CA, USA)
using an ABI 310 automated DNA sequencer (Perkin Elmer
Applied Biosystems). Electropherograms were edited and
assembled using sequencher 4.1 (Gene Codes, Ann Arbor,
MI, USA). Sequences were manually aligned with Se-Al
v. 2.0a11 (Rambaut, 2002).
Nested clade phylogeographic analysis and molecular
variability
Nested clade phylogeographic analysis was performed following
the approach of Templeton et al. (2005) using the program
ANeCA (Panchal, 2007). A statistical parsimony network was
obtained using the program tcs (Clement et al., 2000). Based on
the resulting network, nested clades were defined following the
rules of Templeton et al. (1987) and Templeton & Sing (1993).
Clade (Dc) and nested clade (Dn) distances were estimated to
assess the association between the nested cladograms and
geographic distances among sampled localities (Templeton
Table 1 Localities, studied populations of Hunnemannia
fumariifolia, haplotypes and sample size (in parentheses).
Population Location
Latitude and
longitude
Altitude
(m a.s.l.) Haplotype
1 Galeana N24!44¢ W99!58¢ 1746 A(5) K(1)
2 Bonanza N24!36¢ W101!26¢ 2296 C(4)
3 La Escondida N24!04¢ W99!57¢ 1714 I(4) J(3)
4 Real de Catorce N23!42¢ W100!51¢ 2650 C(4) O(1)
5 Cerro Tahti N20!41¢ W99!24¢ 2020 D(5)
6 Coixtlahuaca N17!43¢ W97!22¢ 1953 N(5)
7 San Isidro N25!21¢ W100!20¢ 1736 G(4) Q(1)
8 La Luz N25!21¢ W100!18¢ 1355 G(4)
9 Cienega N25!22¢ W100!13¢ 1355 G(5) H(1)
10 Altares N24!43¢ W99!53¢ 1420 A(5)
11 Rio de San Jose N24!34¢ W99!55¢ 1480 P(5)
12 Zaragoza N23!59¢ W99!47¢ 1374 I(4) A(1)
13 Ciudad del Maız N22!27¢ W99!40¢ 1420 B(3)
E(1) F(1)
14 Arteaga N21!13¢ W99!49¢ 1248 B(3)
15 Tolantongo N20!36¢ W99!01¢ 1900 L(5)
16 Mezquititlan N20!31¢ W98!38¢ 1408 L(6) M(1)
17 Tequixtepec N17!45¢ W97!20¢ 2002 N(3)
V. Sosa et al.
20 Journal of Biogeography 36, 18–27
ª 2008 The Authors. Journal compilation ª 2008 Blackwell Publishing Ltd
et al., 1995). The program geodis (Posada et al., 2000) was used
to test the null hypothesis of no geographic association of clades
and nested clades, with a 95% confidence level, and with 10,000
permutations. If values were significant, the inference key of
Templeton (2004) was used to recognize probable populational
processes and/or historical events of the clades.
Parameters of population diversity, i.e. average within-
population gene diversity (hS), total gene diversity (hT) and
genetic differentiation over all populations (GST), as well as
equivalent parameters (vS, vT, NST), were also estimated,
taking into account the evolutionary distance of haplotypes
using HaploNst and permut (http://www.pierroton.inra.fr/
genetics/labo/Software/index.html) (Pons & Petit, 1995,
1996). Population structure (FST) was also estimated. Analysis
of molecular variance (amova, Excoffier et al., 1992) based
on sequences was performed to assess genetic differentiation
within and among populations as well as among geographical
regions. Sampling populations were grouped into three
geographical regions – the Chihuahuan Desert, Sierra Madre
Oriental and Tehuacan-Cuicatlan Valley – corresponding to
morphotectonic provinces (Ferrusquia-Villafranca, 1993).
Parameters of demographic and spatial expansion (s, h0,
h1), including a mismatch distribution analysis (MDA), were
estimated with 1000 parametric boostrap replicates, as well as
Harpending’s raggedness index (r) (Rogers & Harpending,
1992; Schneider & Excoffier, 1999; Excoffier, 2004). The
genetic matrix distance was constructed in paup* v. 4.0b10
(Swofford, 2003). The appropriate likelihood model (F81+I)
based on the Akaike information criterion was found with
ModelTest v. 3.07 (Posada & Crandall, 1998). These
analyses and the amova were performed using the program
arlequin v. 3.01 (Excoffier et al., 2005). Significance tests
were conducted with 10,000 permutations. Spatial genetic
structure was also assessed by testing the significance of
isolation by distance (IBD) with a Mantel test with 10,000
random permutations with the matrices of pairwise popula-
tion differentiation statistics (FST) and the natural logarithm
of the geographical distances (Rousset, 1997). The test was
performed using the program tfpga v. 1.3 (Miller, 1997).
GenBank accession numbers of the cpDNA rpl32-trnL(UAG)
sequences are EU169024–EU169030; ndhF-rpl32 sequences
are EU169018–EU169023; and trnH-psbA sequences are
EF464658–EF464664.
RESULTS
Sequence analysis
The length of the three cpDNA regions (rpl32-trnL(UAG),
ndhF-rpl32 and trnH-psbA) was 2163 bp. Fourteen substitu-
tions were detected in positions 83, 297, 389, 491, 723, 1024,
1039, 1137, 1167, 1290, 1590, 1854, 1885 and 1958. Five indels
(in positions 436–444, 446–451, 502–503, 742–744 and 1788–
1804) were coded as a single-mutation change. The 30-bp
inversion near the 3¢ end of trnH-psbA in positions 2100–2129
was included in analyses by manually reversing the region and
then coding it as a single evolutionary event that resulted in a
single mutation. The rest of the mutations included short
indels of 1 or 2 bp counted as a single-mutation site in
positions 2036 and 2037 (Table 2).
Haplotype relationships and geographical distribution
In total, 17 haplotypes were detected (Table 2, Fig. 1).
Parsimony analysis resulted in a resolved network (Fig. 2).
Haplotype A is connected to K by one substitution and to P by
a hypothetical haplotype. Haplotype G is connected to Q and
M. Haplotype L is connected to M and I by one substitution.
Haplotype F is connected to I and B by three and four
hypothetical haplotypes, respectively. Haplotype B is con-
nected to O by one substitution. All these haplotypes are
interior. Haplotypes at the tips of the parsimony network are D
and H, both connected to M by one hypothetical haplotype.
Haplotype E is connected to B by two hypothetical haplotypes,
and, finally, haplotypes C and N are connected to O by one
substitution (Fig. 2).
With regard to the Sierra Madre region, six populations
have one haplotype [La Luz (G); Altares (A); Rio San Jose (P);
Arteaga (B); Tolantongo (L); Cerro Tahti (D)], and six
populations have two haplotypes [Galeana (A, I); La Escondida
(I, J); San Isidro (G, Q); Cienega (H, G); Zaragoza (A, I);
Mezquititlan (L, M)]. Ciudad del Maiz has three haplotypes
(B, E, F). In the Chihuahuan Desert region, Bonanza has a
single haplotype (C) and Real de Catorce has two haplotypes
(C, O). In the Tehuacan-Cuicatlan Valley region, both
Coixtlahuca and Tequixtepec have the same haplotype (N)
(Tables 1 and 2; Fig. 2).
Chloroplast haplotype diversity and population
differentiation
Differentiation among populations based on cpDNA variation
(GST = 0.787, SE 0.0614) indicated population structure in
H. fumariifolia, corroborated by a fixation index (FST) of 0.907.
Within-population gene diversity (hS) was 0.201 (SE 0.0579).
Total gene diversity (hT) was 0.947 (SE 0.0138). Differentiation
for ordered alleles (NST) (0.913, SE 0.0395) was higher than
that for GST (U = 2.85, P < 0.01), indicating phylogeograph-
ical structure of cpDNA in H. fumariifolia. Parameters vS and
vT showed values almost identical to hS and hT (0.083, SE
0.0377; 0.0953, SE 0.0431, respectively). The results of the
amova are presented in Table 3. Most of the total variation
(90.71%, P < 0.001) was explained by differences among
populations. The three regions (Chihuahuan Desert, Sierra
Madre Oriental and Tehuacan-Cuicatlan Valley) showed a
significant (43.39%, P < 0.001) variation among themselves,
suggesting that the three separately distributed groups have a
strong genetic differentiation. Results of the Mantel test
showed a significant correlation between the pairwise estimates
of FST and the natural logarithm of the geographical distances
(r = 0.511; P = 0.0001), suggesting a pattern of isolation by
distance.
Phylogeography of Hunnemannia fumariifolia
Journal of Biogeography 36, 18–27 21ª 2008 The Authors. Journal compilation ª 2008 Blackwell Publishing Ltd
Demographic and nested clade phylogeographic
analysis
Mismatch distribution analysis links the number of differences
between haplotypes and haplotype frequency, and in our
analysis was unimodal. It showed a significant deviation from
the sudden expansion model. Estimated parameters from the
total cladogram were s = 9.539, h0 = 0.000 and h1 = 18.496.
Based on Harpending’s raggedness index (r = 0.449,
P = 0.03), the hypothesis of sudden demographic expansion
Table 2 Seventeen haplotypes of Hunnemannia fumariifolia were recognized based on three chloroplast DNA sequences, rpl32-trnL(UAG),
ndhF-rpl32 and trnH-psbA.
Sequence Position Collection Sites
Haplotype
82344444444444445577771111111111111111111111111122222222222222222222222222222222
GBERCXSLNARZMOTQU
39833334444445590024440011257777777777778888888933111111111111111111111111111111
7667890167890112332342336998899999999990000058500000000000011111111112222222222
n Region4977008901234567890123445867012345678901234567890123456789
A CGA------ATATAGTTTG---CACTGCATTAATATGAAATGATTTATA-CCCGCCCTCTTGATAAACAAGAAATTTCGG 50000000050100000 11 SMO
B A.GCTATAT------G...---......-----------------CGG.-****************************** 00000000000033000 6 SMO
C A.G......------G...---......-----------------CGG--.............................. 04040000000000000 8 CD
D .A.......------G--.---..A.T....................G.-.............................. 00005000000000000 5 SMO
E A.G......------G...---......-----------------....-****************************** 00000000000010000 1 SMO
F .A.......------G--T---......-----------------CGG.-****************************** 00000000000010000 1 SMO
G .A.......------G--.AAA.....A...................G.-.............................. 00000044500000000 13 SMO
H .A.......------G--.---.CA......................G.-****************************** 00000000100000000 1 SMO
I .A.......------G--T---...G.....................G.-.............................. 00400000000400000 8 SMO
J .A.......------G--T---...G.....................G.-.............................. 00300000000000000 3 SMO
K ...------ATATAG....---...G.......................-.............................. 10000000000000000 1 SMO
L .A.......------G--.---.........................G.-.............................. 00000000000000560 11 SMO
M .A.......------G--.---...G.....................G.-.............................. 00000000000000010 1 SMO
N A.G......------G...---......-----------------CGG.A.............................. 00000500000000003 8 T-CV
O A.G......------G...---......-----------------CGG.-.............................. 00010000000000000 1 CD
P .........ATATAG....---.........................G.-.............................. 00000000005000000 5 SMO
Q .A.......------G--.AAAT....A...................G.-.............................. 00000010000000000 1 SMO
G: Galeana; B: Bonanza; E: La Escondida; R: Real de Catorce; C: Cerro Tahti; X: Coixtlahuaca; S: San Isidro; L: La Luz; N: Cienega; A: Altares; R: Rio
San Jose; Z: Zaragoza; M: Ciudad del Maiz; O: Arteaga; T: Tolantongo; Q: Mezquititlan; U: Tequixtepec. CD: Chihuahuan Desert; SMO: Sierra Madre
Oriental; T-CV: Tehuacan-Cuicatlan Valley.
Sequence with *: fragment 30-bp inversion; –: indel.
Figure 2 Statistical parsimony network
and resulting set of nested clades of the 17
cpDNA haplotypes found in Hunnemannia
fumariifolia. A–Q: sampled haplotypes.
Solid bars: hypothetical haplotypes.
The number of individuals is given in
parentheses.
V. Sosa et al.
22 Journal of Biogeography 36, 18–27
ª 2008 The Authors. Journal compilation ª 2008 Blackwell Publishing Ltd
was accepted. We also performed MDA separately for each
clade resulting from NCPA that resulted in contiguous range
expansion and inclusive outcome clades (2-3, 3-2 and 2-4).
The raggedness index in clades 2-4 and 3-2 showed non-
significant values of P (r = 0.178, P = 0.23; r = 0.016,
P = 0.81), but that in clade 2-3 showed significant values
(r = 0.209, P = 0.01).
Nested clade phylogeographic analysis showed a significant
relationship between genetic and geographical distributions in
H. fumariifolia (Table 4). Restricted gene flow with isolation
by distance was detected in clades 1-4 and 3-1. Clade 1-4
included haplotypes C and O from the Chihuahuan Desert,
and haplotype N from the Tehuacan-Cuicatlan Valley. Clade
3-1 had all haplotypes in the Sierra Madre Oriental (SMO).
Clades 1-9 and 2-2 showed allopatric fragmentation. Clade 1-9
had a distribution in the north (haplotype J) and in the south
(haplotype L) of the SMO. Clade 2-2 included haplotypes
A-K, P, distributed in the north of the SMO (Figs 1 & 2).
Contiguous range expansion was detected in clades 2-3 and
3-2. Restricted gene flow with isolation/dispersal but with
some long-distance dispersal over intermediate areas not
occupied by the species, or past gene flow followed by
extinction of intermediate populations was detected in clade
2-1. An inclusive outcome was observed in clade 2-4 and in the
entire cladogram (Table 4).
DISCUSSION
Population differentiation
Hunnemannia fumariifolia showed population differentiation
(GST = 0.787 and FST = 0.907). The GST value was in agree-
ment with other plant phylogeographical studies (GST = 0.60–
0.96) (e.g. Demesure et al., 1996; El Mousadik & Petit, 1996;
Dumolin-Lapegue et al., 1997; Dutech et al., 2000; Cavers
et al., 2003; Huang et al., 2004; Marchelli & Gallo, 2006; Ikeda
& Setoguchi, 2007). Genetic differentiation in plants has been
attributed to limited seed or pollen dispersal (Petit et al.,
2005), and limited genetic structure has been attributed to high
dispersal ability (e.g. Palme et al., 2003; Jones et al., 2006; Wu
et al., 2006; Chung et al., 2007). In our results, NST (0.913) was
significantly higher than GST (0.787), suggesting that pairs of
different haplotypes from the same population have more
similar sequences than pairs of different haplotypes from
Table 3 Results of the analysis of molecular variance for 17
populations of Hunnemannia fumariifolia grouped in three
geographical regions (Chihuahuan Desert, Sierra Madre Oriental
and Tehuacan-Cuicatlan Valley) based on cpDNA sequence data.
Source of variation d.f.
Sum of
squares
Variance
components
Percentage
of variation
(%)
Among populations (total) 16 0.132 0.00162 90.71*
Within populations 68 0.011 0.0017 9.29
(1,3,5,7,8,9,10,11,12,13,14,
15,16) vs. (2,4) vs. (6,17)
Among groups 2 0.042 0.00107 43.39*
Among populations
within groups
14 0.089 0.00123 49.89*
Within populations 68 0.011 0.00017 6.72*
*P < 0.001.
Table 4 Results of the nested clade phylogeographical analysis and interpretations according to the revised inference key of Templeton
et al. (2005) for 17 populations of Hunnemannia fumariifolia from Mexico.
Nested
clade v2 P-value Dc Dn
Inference
chain Inferred pattern
1-4 18.7 0.0000 33.9928S )62.219 1-2-3-4 NO Restricted gene flow with isolation
by distance
1-9 14.0 0.0010 No interior/tip
clades exist
1-19 NO Allopatric fragmentation
2-1 37.8333 0.000 )41.7955L 212.1502L 1-2-3-5-6-7-8 YES Restricted gene flow/dispersal but
with some long-distance dispersal
over intermediate areas not occupied
by the species; or past gene flow
followed by extinction of intermediate
populations
2-2 16.0 0.0000 )14.4461S )9.7687S 1-19 NO Allopatric fragmentation
2-3 27.0 0.0010 )308.4168S )306.4102S 1-2-11-12 NO Contiguous range expansion
2-4 14.5918 0.0000 No interior/tip
clades exist
1-2 IO Inconclusive outcome
3-1 37.0 0.0000 198.4136L 159.9941L 1-2-3-4 NO Restricted gene flow with isolation
by distance
3-2 54.8333 0.0000 )116.4518S )109.1562S 1-2-11-12 NO Contiguous range expansion
Total
cladogram
78.2963 0.0000 No interior/tip
clades
1-2 IO Inconclusive outcome
Dc and Dn are the clade and nested clade distances, respectively.
Phylogeography of Hunnemannia fumariifolia
Journal of Biogeography 36, 18–27 23ª 2008 The Authors. Journal compilation ª 2008 Blackwell Publishing Ltd
distinct populations (Pons & Petit, 1996). Similar results, in
which NST is higher than GST, have been reported in a number
of phylogeographical studies of plants (e.g. El Mousadik &
Petit, 1996; Dumolin-Lapegue et al., 1997; Cavers et al., 2003;
Petit et al., 2005; Marchelli & Gallo, 2006; Aizawa et al., 2007).
Isolation by distance and allopatric fragmentation
Isolation by distance can be studied through the correlation of
genetic and geographical distances and also through nested
clade analysis (e.g. Cuenca et al., 2003). Results of our Mantel
test found a significant correlation between genetic and
geographical distances in H. fumariifolia, suggesting isolation
by distance. Furthermore, NCPA found three clades (1-4, 2-1
and 3-1) with evidence for restricted gene flow and isolation by
distance, but clade 2-1 also showed dispersal but with some
long-distance dispersal, or past gene flow followed by extinc-
tion of intermediate populations. Clade 1-4 included individ-
uals of four populations, two of them from the Chihuahuan
Desert (Bonanza and Real de Catorce), and two from the
Tehuacan-Cuicatlan Valley (Coixtlahuca and Tequixtepec).
These two regions are separated by the Transvolcanic Belt and
a distance of c. 800 km (Fig. 1). Clade 3-1 grouped individuals
from nine populations, all of them from the SMO. Some
populations (Galeana, San Isidro, La Luz, Cienega, Altares, Rio
San Jose and Zaragoza) are in the north of the SMO, whereas
two of them (Cerro Tahti and Mezquititlan) are in the south of
the SMO, and the two groups are separated by 400 km
(Fig. 1).
Nested clade phylogeographic analysis also found two clades
(1-9 and 2-2) in which processes such as allopatric fragmen-
tation influenced genetic divergence. Clade 1-9 included
individuals from three populations, namely Mezquititlan and
Tolantongo in the south and La Escondida in the north of the
SMO. Clade 2-2 included individuals from four populations
(Galeana, Altares, Rio San Jose and Zaragoza), all of them in
the north of the SMO. We suggest that allopatric fragmenta-
tion could be a result of the uplift of groups of mountains
within the SMO. The SMO is one of the most convoluted
geological regions of Mexico. In the north, it includes groups
of mountains in southern Nuevo Leon, western Tamaulipas
and northern San Luis Potosi. Another band of mountains
extends westwards to Nuevo Leon across southern Coahuila.
These groups of mountains were lifted in different periods in a
complex way (Ferrusquia-Villafranca, 1993).
The complex processes found in populations of H. fumarii-
folia, such as restricted gene flow with isolation by distance or
long-distance dispersal, allopatric fragmentation and/or con-
tiguous range expansion, have been reported in a number of
other plant phylogeographical studies (e.g. Bittkau & Comes,
2005; Wu et al., 2006; Cornman & Arnold, 2007).
Post-glacial refugia
There is debate over the importance of northerly and southerly
refugia in Europe and over the existence of the so-called
‘cryptic’ northern refugia (Lopez de Heredia et al., 2007;
Bhagwat & Willis, 2008). However, there is agreement over a
common phylogeographical pattern of distribution that has
been detected by Taberlet & Cheddadi (2002) in the vegetation
of the temperate regions of the Northern Hemisphere. During
cold periods, the geographical ranges of most species were
restricted to a single refugium or a few refugia in the south.
During subsequent warming, species expanded their ranges,
mainly northwards, colonizing areas according to their dispersal
abilities and ecological requirements. When the climate became
cooler, northern populations disappeared, leaving no descen-
dants. This agrees with previous studies that determined that
refugia were located in southern areas of north-eastern North
America and of unglaciated western North America (Brunsfeld
et al., 2001; Soltis et al., 2006). Phylogeographical studies have
found that, if genetic diversity is high, areas acted either as a
refugium or as mixing zones of organisms (Huang et al., 2004).
In the first case, haplotypes are closely related, whereas the latter
case may include distantly related haplotypes (Petit et al., 2002;
Huang et al., 2004; Marchelli & Gallo, 2006; Wu et al., 2006).
Our mismatch distribution analysis results suggest that areas in
the north of the SMO acted as post-glacial refugia for some
populations of H. fumariifolia. This coincides with the climate
changes of the Pleistocene, during which the northern portion
of Mexico was wetter (Metcalfe et al., 2000, 2002).
Our results indicated that some populations of the SMO are
the consequence of post-glacial range expansion, as indicated by
parameters for sudden expansion models. The same pattern of
distribution is found in another desert plant, Agave lechuguilla,
for which populations seem to have originated in the north and
more recently to have colonized the south (Silva-Montellano &
Eguiarte, 2003). In contrast, for the creosote bush, Larrea
tridentata, another desert plant, populations recently colonized
the north from southern refugia (Duran et al., 2005).
During the Pleistocene the Tehuacan-Cuicatlan Valley was
moister and cooler, with regular winter frosts (McNeish et al.,
1972). During this period, the valley had extensive grassland.
Many cacti, Agave and other desert plants could not live under
such conditions. The transition to the recent climate regime
occurred in the period 7800–7400 bc (McNeish et al., 1972).
Therefore, we suggest that populations of the Mexican tulip
poppy survived in refugia in the northern SMO before this
climatic transition. Phylogeographical studies of other plant
species with a similar geographical distribution to that of
H. fumariifolia would be valuable for understanding the
evolutionary histories of North American xerophytic plants.
In summary, our study found that the historical processes
that influenced the geographical pattern of genetic variation in
H. fumariifolia were restricted gene flow with isolation by
distance, allopatric fragmentation, and sudden demographic
expansion. In addition, isolation by distance was detected as
the main factor that shaped distributional patterns in popu-
lations of this species. Moreover, there is no current genetic
flow between populations from the SMO and those from the
Chihuahuan Desert, nor between these northern populations
and those from the Tehuacan-Cuicatlan Valley.
V. Sosa et al.
24 Journal of Biogeography 36, 18–27
ª 2008 The Authors. Journal compilation ª 2008 Blackwell Publishing Ltd
ACKNOWLEDGEMENTS
We thank two anonymous referees for their suggestions, which
improved our paper. We also thank Pablo Carrillo, Arturo De
Nova and Daniel de la Rosa for assistance with fieldwork, Carla
Gutierrez for her suggestions on a previous version of the
manuscript, and Bianca Delfosse for editing the English. DNA
extraction and sequencing were made possible through a grant
to V.S. by CONACYT (P39601526).
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BIOSKETCHES
Victoria Sosa holds a full-time research position at the
Institute of Ecology in Xalapa, Mexico. Her interests are in the
phytogeography, systematics and conservation of the endemic
flora of Mexico.
Eduardo Ruiz-Sanchez is a graduate student in the PhD
program of Systematics at the Institute of Ecology in Xalapa,
Mexico. His interests are in the phytogeography and system-
atics of the flora of Mexico.
Flor C. Rodriguez-Gomez is a student in the Master’s
program at the Institute of Ecology in Xalapa. Her interest is in
population genetics.
Editor: Jorge Crisci
Phylogeography of Hunnemannia fumariifolia
Journal of Biogeography 36, 18–27 27ª 2008 The Authors. Journal compilation ª 2008 Blackwell Publishing Ltd