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ORIGINAL PAPER
Phylogeography of the European stalked barnacle(Pollicipes pollicipes): identification of glacial refugia
Daniel Campo • Jose Molares • Lucia Garcia •
Pino Fernandez-Rueda • Claudia Garcia-Gonzalez •
Eva Garcia-Vazquez
Received: 3 February 2009 / Accepted: 16 September 2009 / Published online: 10 October 2009
� Springer-Verlag 2009
Abstract The alternation of glacial and interglacial
events during the Pleistocene has produced changes in
species distribution ranges leading to bottlenecks and
alterations of patterns of gene flow. The European stalked
barnacle, Pollicipes pollicipes, is a sessile pedunculate
cirripede that inhabits the rocky intertidal frame, from
Senegal to the northwestern coast of France. In this work,
we have analyzed a fragment of the mitochondrial gene
cytochrome c oxidase subunit I for 569 individuals of
P. pollicipes in order to investigate whether the shifts in
climatic conditions that occurred during the Pleistocene
influenced the current pattern of distribution of genetic
variation of P. pollicipes. A pre-last glacial maximum
pattern of demographic expansion was found, in concor-
dance with many other North Atlantic marine species. On
the other hand, three potential glacial refugia were identi-
fied: North African coasts, northwestern Iberian Peninsula
and English Channel/Brittany.
Introduction
Climate oscillations that occurred during the Pleistocene
had a dramatic effect on the geographic distribution of
terrestrial and marine species (Avise 2000), especially the
last glacial maximum (LGM), which occurred about
20,000 years ago during the Vistula glaciation. In Europe,
the extent of the marine glaciation reached as far south as
the northern limit of the Bay of Biscay, covering the British
Islands (Svendsen et al. 2004). These conditions were
especially unfavorable for sessile organisms (e.g., sea-
weeds, seagrasses and sessile invertebrates) and forced
populations into refugial areas from which they expanded
once the ice receded. The effect of such range fluctuations
left a genetic signature on the populations, which can be
measured, since we expect a higher genetic diversity within
refugial areas than in more recently colonized habitats and
high genetic differentiation between refugia (Hewitt 1996,
2004). This has allowed phylogeographers to detect glacial
refugia and infer interglacial recolonization pathways. For
marine species of the North Atlantic, these refugia were
mostly located in southern areas including Atlantic islands,
North African coast and the Mediterranean, and many
recent studies suggest the existence of Pleistocene refugial
areas at the south of the Bay of Biscay (off the coast of
northwestern Iberian Peninsula), the English Channel/
Brittany area, the southwest of Ireland and the west coast
of Iceland (reviewed in Gomez et al. 2007).
Communicated by M. I. Taylor.
Electronic supplementary material The online version of thisarticle (doi:10.1007/s00227-009-1305-z) contains supplementarymaterial, which is available to authorized users.
D. Campo � C. Garcia-Gonzalez � E. Garcia-Vazquez
Departamento de Biologia Funcional, Universidad de Oviedo,
C/Julian Claveria s/n, 33006 Oviedo, Spain
Present Address:D. Campo (&)
Molecular and Computational Biology,
University of Southern California, 1050 Childs Way,
RRI, Los Angeles, CA 90089, USA
e-mail: [email protected]
J. Molares
Centro de Investigacions Marinas, Conselleria de Pesca
e Asuntos Maritimos, Pedras de Coron s/n,
36620 Vilanova de Arousa, Pontevedra, Spain
L. Garcia � P. Fernandez-Rueda
Centro de Experimentacion Pesquera, Consejerıa de Medio
Ambiente y Desarrollo Rural, Direccion General de Pesca,
Avda. Prıncipe de Asturias s/n, 33212 Gijon, Spain
123
Mar Biol (2010) 157:147–156
DOI 10.1007/s00227-009-1305-z
The European stalked barnacle, Pollicipes pollicipes
(Gmelin 1790), is a sessile pedunculate cirripede that
inhabits the rocky intertidal frame, in zones exposed to
strong swell. Its current distribution spans from the coast of
Senegal to the northwestern coast of France (Brittany)
(Barnes 1996). There is also an isolated population in Cape
Verde Islands, which is genetically differentiated from the
rest (Quinteiro et al. 2007). Adults are hermaphrodite and
reproduce by copulation with internal fertilization. The
reproductive period lasts 7 months, from March to Sep-
tember (Molares et al. 1994), and its larval development
takes about 1 month, with six naupliar and one cyprid
stages. All larvae are planktonic and exhibit active mobility.
After the naupliar stages, the cyprid settles specifically to the
peduncle of adult individuals, then they move to the base and
fix permanently to the rock. As a consequence, adult indi-
viduals of P. pollicipes constitute dense aggregations.
To our knowledge, only two published studies to date deal
with genetic data of P. pollicipes. Van Syoc (1995) studied the
phylogenetic relationships of three species of the genus Pol-
licipes, and Quinteiro et al. (2007) investigated the influence of
coastal currents and mesoscale hydrographic features on the
population genetic structure of P. pollicipes. Quinteiro et al.
(2007) also suggested the existence of southern refugia (trop-
ical and subtropical latitudes) during Pleistocene glaciations.
In the present study, we investigated the mitochondrial
DNA (mtDNA) phylogeography for the entire range of dis-
tribution of the European stalked barnacle (Pollicipes pol-
licipes) using a fragment of the subunit I of the cytochrome c
oxidase (COI). The objective was to elucidate whether
extreme climatic conditions occurred during the Pleistocene
have had any influence on the current pattern of distribution of
genetic variation of P. pollicipes, specially in populations
from the northernmost boundary of its range of distribution.
Materials and methods
Samples
A total of 569 adult individuals of P. pollicipes from 11
different locations were collected, covering the entire range
of distribution of the species, from Mauritania to Brittany
(France) (Fig. 1; Table 1). The population from Cape Verde
Islands was not included in the present study due to its
unclear current taxonomic position (Quinteiro et al. 2007).
Whole individuals were collected directly from the rock and
preserved in absolute ethanol until DNA extraction.
DNA extraction, PCR amplification and sequencing
Total DNA was extracted from a small piece of muscle
(about 1 mm3) using a Chelex Resin protocol (Estoup et al.
1996) and kept at 4�C until needed. PCR amplification of a
fragment of the COI gene was initially carried out using the
set of primers K–N described by Van Syoc (1995). After-
ward, from an alignment of COI sequences obtained from
GenBank (EF032142–EF032154; Quinteiro et al. 2007),
we designed a new primer to obtain better amplification
results (primer D: 50-TGGAGGTTTTGGAAACTGAC-30).This new primer was employed in combination with the
primer N (replacing primer K). PCR were carried out in a
total volume of 40 ll containing 59 Go Taq� Flexi Buffer,
250 lM of each dNTP, 40 pmol of each primer, 0.2 ll of
Go Taq� Polymerase 5 U/ll (Promega) and 4 ll of DNA.
They were performed in a GeneAmp� PCR system 9700
(Applied Biosystems) with the following conditions: an
initial denaturing step at 95�C for 5 min, followed by 30
cycles of denaturing at 95�C for 30 s, annealing (for 30 s)
at 50�C and an extension at 72�C for 30 s, ending with a
final extension at 72�C for 10–15 min.
PCR products were visualized in 50 ml 1.5% agarose
gels with 3 ll of 10 mg/ml ethidium bromide. Stained
bands were excised from the gel, and DNA was purified
with a Wizard� SV Gel and PCR Clean-Up System (Pro-
mega) prior to sequencing. Automated fluorescence
Fig. 1 Map showing the 11 sampling sites of P. pollicipes along its
distribution range. Population codes as in Table 1
148 Mar Biol (2010) 157:147–156
123
sequencing was performed on an ABI PRISM 3100
Genetic Analyzer (Applied Biosystems) with BigDye 3.1
Terminator system, in the Unit of Genetic Analysis of the
University of Oviedo (Spain).
Population genetics
Sequences were edited using the BioEdit Sequence
Alignment Editor software (Hall 1999) and aligned with
the ClustalW application (Thompson et al. 1994) included
in BioEdit.
Since most of the neutrality tests based on nucleotide
changes are sensitive to demographic shifts, we conducted
the McDonald and Kreitman test (McDonald and Kreitman
1991) using P. polymerus as an outgroup to test whether
selection is acting on P. pollicipes COI sequences.
P. polymerus COI sequence was obtained from the com-
plete mitochondrial genome available in GenBank under
Accession number AY456188.
Haplotype diversity (Hd) and nucleotide diversity (p)
for each population were calculated with the program
ARLEQUIN version 3.01 (Excoffier et al. 2005). Due to
differences in sample size among populations, haplotype
diversity values were standardized to the smallest sample
size using the program RAREFAC (Petit et al. 1998).
The ModelTest (ver. 3.06) software (Posada and
Crandall 1998) was employed to determine the model of
sequence evolution that best fitted our dataset and to cal-
culate the proportion of invariable sites and the value of the
gamma distribution shape parameter. Population pairwise
FST values were calculated employing Tamura–Nei dis-
tances (Tamura and Nei 1993) and a value of the gamma
distribution shape parameter of 1.1698 (see ‘‘Results’’ for
the outcome of the ModelTest) with the program ARLE-
QUIN. ARLEQUIN was also employed to perform an
analysis of the molecular variance (AMOVA; Excoffier
et al. 1992) to test its hierarchical distribution at three
levels: within populations (UST), among populations (USC)
and among groups of populations (UCT). We tested several
different a priori grouping combinations, splitting popula-
tions into 2, 3 and 4 groups (Brittany vs. the rest of pop-
ulations; Brittany vs. Iberian Peninsula vs. Africa; Brittany
vs. north coast of Iberian Peninsula vs. west coast of
Iberian Peninsula vs. Africa), and that configuration with
the highest value of UCT and statistically significant was
chosen as the most likely geographic subdivision. The
statistical significance of both analyses (pairwise FST
and AMOVA) was tested through 99,224 permutations.
To test for isolation by distance, we performed a Mantel
test as implemented in ARLEQUIN, estimating the sig-
nificance level by 50,000 permutations. With this analysis,
we determined whether there is a significant correlation
between a matrix of geographic distances (represented by
the minimum coastline distance in kilometers) and a matrix
of genetic distances (FST).
Demographic history
To detect whether the populations have undergone demo-
graphic and/or range expansion, we compared the observed
frequency of pairwise sequence differences (mismatch
distribution) to the expected distribution under a sudden
expansion model with the SSD statistic (sum of squared
differences) using 1,000 bootstrap replicates, in ARLE-
QUIN. We also computed Fu’s Fs (Fu 1997) and the R2
statistic (Ramos-Onsins and Rozas 2002) for all samples
using DNASP version 4.50.3 (Rozas et al. 2003) and
estimated its significance with 1,000 coalescent simula-
tions. With this program, we can also calculate s, which
allows us to then estimate the time in generations since the
Table 1 Abbreviated codes, geographic coordinates (latitude and longitude), number of individuals (N) and haplotypes (Nh), number of private
haplotypes (Nph), percentage of Nph with respect to N (%Ph) and values of haplotype diversity (Hd) and nucleotide diversity (p) for each
location sampled
Population Code Lat/long N Nh Nph %Ph Hd p
Saint Guenole, France SG 48�19021.7000N/4�2509.9800O 35 20 5 14.3 0.950 0.0099
Quiberon, France QUIB 47�28050.9700N/3� 8031.2600O 44 15 1 2.3 0.909 0.0088
Jaizkibel, Spain JAI 43�23023.9500N/1�4806.9200O 31 14 0 0 0.938 0.0079
Monpas, Spain MON 43�2008.4400N/1�58018.6000O 35 16 0 0 0.936 0.0072
Ribadesella, Spain RIB 43�28010.1200N/5�3028.2600O 60 25 7 11.7 0.933 0.0088
Punta de la Cruz, Spain CRUZ 43�33035.7200N/7�1017.2700O 60 27 12 20 0.951 0.0082
Corme, Spain COR 43�15044.7200N/8�5805.2000O 57 25 8 14 0.945 0.0078
Vila do Conde, Portugal VC 41�21042.9500N/8�45046.5500O 30 17 1 3.3 0.940 0.0084
Berlengas, Portugal BER 39�24050.3600N/9�30025.1300O 128 30 11 8.6 0.914 0.0067
Agadir, Morocco AGA 30�24058.2100N/9�38046.1500O 53 21 5 9.4 0.923 0.0069
Mauritania MAU 18�24027.9200N/16� 5050.3200O 36 22 4 11.1 0.951 0.0068
Mar Biol (2010) 157:147–156 149
123
population expansion (t) with the formula t = s/2uk (where
u is the substitution rate in changes per nucleotide per
million years, and k is the length of the sequence).
Times of haplotypes coalescence (tmrca: time to the
most recent common ancestor) and the limits of the 95%
highest posterior density (HPD) interval, for the whole
sample and for each of the groups, were estimated with the
program BEAST ver. 1.4.8 (Drummond and Rambaut
2007). We did a run of 10 million generations sampling
every 1,000 under the strict molecular clock model
implementing the HKY substitution model, and con-
straining the priors for gamma and proportion of invariable
sites according to the values obtained in ModelTest. The
tree prior selected was exponential growth (based on
results for SSD, R2 and Fu’s Fs statistics), whereas priors
for the rest of parameters were left as default. In every case,
effective sample sizes (ESS) were all above 100, and a
good mix of the chains was observed.
To test whether COI sequences follow a molecular clock
model, we performed a relative ratio test (Tajima 1993) in
MEGA4 (Tamura et al. 2007) with many different com-
binations of ingroup and outgroup sequences, and also
including P. polymerus COI sequence as outgroup. At least
two different substitution rates have been applied to the
mitochondrial COI of P. pollicipes. Van Syoc (1995)
employed a divergence rate of 2% per million years (pmy),
an average value commonly accepted for the whole
mtDNA, to estimate divergence times between species of
Pollicipes, whereas Wares (2001) estimated a rate of 3.1%
pmy for barnacle species of the genus Euraphia, and
applied it to the genus Chthamalus. This rate was cali-
brated using divergence values between species separated
by the Panama Isthmus, and it is in concordance with other
crustacean estimates (Wares 2001). Quinteiro et al. (2007)
employed this latter rate to calculate a little bit faster one
for mitochondrial control region in P. pollicipes. We
therefore decided to employ the rate of 3.1% pmy, as it has
been estimated from barnacles divergence data.
Phylogeographic analysis
We performed a nested clade analysis (NCA) to test for
geographic associations between related haplotypes and to
distinguish between contemporary and historical events
influence in the current distribution of genetic diversity. To
do this, a parsimony network was constructed using the
program TCS version 1.21 (Clement et al. 2000), which
implements the statistical parsimony method described by
Templeton et al. (1992). Ambiguities in the cladogram
(represented by loops) were solved following the three
criteria proposed in Pfenninger and Posada (2002). The
network was then nested by hand following the procedures
described in Templeton et al. (1987) (Fig. 2), and the NCA
was done with the program GEODIS version 2.4 (Posada
et al. 2000), through 10,000 permutations. As P. pollicipes
is a coastal species, a matrix of pairwise geographic dis-
tances between populations (the same employed for the
Mantel test) was input. The output was interpreted using
the latest available inference key (http://darwin.uvigo.
es/software/geodis.html). On the other hand, the use of
NCPA for phylogeographic inference has been lately
questioned (see respective article series in Mol Ecol, 2008),
mainly due to its inability for evaluating the relative sup-
port for the different alternative scenarios. However, we
decided to use this method as one approach more as it
can propose phylogeographic scenarios that can be sup-
ported and reinforced with other methods (Garrick et al.
2008).
Results
Population genetics
After editing and aligning all the sequences, a total dataset
of 444 base pairs (bp) length was obtained. A total of 83
haplotypes were found from the 569 P. pollicipes COI
sequences (Table S1). Only 6 out of these 83 were found in
all populations, and 54 were private haplotypes (i.e.,
present in a single location), being 53 singletons. Haplo-
type sequences are available in the GenBank database
(http://www.ncbi.nlm.nih.gov) under the accession numbers
EU998656–EU998738. The McDonald and Kreitman test
was not significant (Fisher’s exact test, P = 0.14), indi-
cating that these COI sequences are not under selection.
Total number of haplotypes (Nh), number of private
haplotypes (Nph) and percentage of Nph with respect to N
(%Ph), as well as values of standardized haplotype diver-
sity (Hd) and nucleotide diversity (p) for each sample are
listed in Table 1. Highest values of %Ph were found in
Saint Guenole, Ribadesella, Punta de la Cruz, Corme and
Mauritania. All populations showed high haplotypic
diversity, the values for Saint Guenole, Punta de la Cruz
and Mauritania being the highest ones. On the other hand,
we found low differentiation among haplotypes and groups
of haplotypes (Fig. 2), being separated by single substi-
tutions.
The model of evolution obtained with ModelTest as best
fitting our dataset was the Tamura and Nei (1993), with a
proportion of invariable sites of 0.5544 and a gamma dis-
tribution shape parameter of 1.1698. Population pairwise
FST were calculated following this model (Table 2).
Although FST values were generally low, there were some
significant genetic differences. Populations from Brittany
(Saint Guenole and Quiberon) showed significant differ-
ences with many of the other samples, except with those
150 Mar Biol (2010) 157:147–156
123
from southeastern Bay of Biscay (Jaizkibel and Monpas)
and Vila do Conde (northern Portugal).
Two grouping configurations yielded significant values
of UCT in the AMOVA. In one of them, populations from
Brittany (Saint Guenole and Quiberon) were on one group,
and all the other populations on another group. The other
significant configuration was that splitting samples in three
groups: Brittany, Iberian Peninsula and Africa. The first
one (two groups of samples) obtained the highest among
group variation (UCT), indicating that the significance of
the second one (three groups) could be due to the among
group variation of the first partition. Thus, we took as the
most likely regional configuration the first one (i.e., Brit-
tany vs. the rest of samples), and the AMOVA revealed
that 2.96% of the variance could be explained by differ-
ences between these two groups (UCT = 0.02962,
P \ 0.05; Table 3). In addition, variation among popula-
tions within groups (0.15%) was not significant
Fig. 2 Statistical parsimony
cladogram showing the nestedclade design for the 83
haplotypes of P. pollicipesfound in the present study. Each
branch represents a mutational
step and the black dots denote
missing haplotypes. Biological
inferences are detailed in
Table 5
Table 2 Matrix of pairwise FST genetic distances between P. pollicipes populations
Population 1 2 3 4 5 6 7 8 9 10
1: SG
2: QUIB 0
3: JAI 0.01344 0.01094
4: MON 0.01864 0.01823 0
5: RIB 0.02746* 0.00603 0 0
6: CRUZ 0.03110* 0.02238* 0 0 0
7: COR 0.02788* 0.02354* 0 0 0.00594 0
8: VC 0 0 0.00748 0.00549 0 0.01153 0.00919
9: BER 0.05656* 0.03886* 0 0 0.00190 0 0.00817 0.02603*
10: AGA 0.03865* 0.00895 0.00985 0.00240 0 0.00520 0.00656 0 0.00517
11: MAU 0.06806* 0.06028* 0.00607 0.00223 0.00794 0 0.00845 0.04641* 0.00393 0.02002
They were calculated employing the Tamura–Nei correction and a value of the gamma distribution shape parameter of 1.1698. Significant values
after 99,224 permutations are indicated with an asterisk
Mar Biol (2010) 157:147–156 151
123
(USC = 0.00150) supporting that the main differentiation
was among groups. In addition, most molecular variation
was explained by within population variability (96.89%),
which agrees with the high levels of haplotype diversity
found in all samples.
A positive correlation was found between genetic and
geographic distances, which yielded a significant value
of the correlation coefficient in the Mantel test
(r = 0.441911, P \ 0.05), indicating a scenario of isola-
tion by distance. However, there was a wide dispersion of
the data, explained by some low FST values between distant
populations. Moreover, when we removed the two Brittany
localities (SG and QUIB), Mantel test became non-signif-
icant (r = 0.326241, P = 0.14).
Demographic history
Sudden demographic expansion was supported by non-
significant SSD values for Saint Guenole, Ribadesella,
Punta de la Cruz and Agadir populations (Table 4). For
other four samples (Jaizkibel, Monpas, Corme and Mau-
ritania), the least square procedure did not converge after
1,800 steps, not allowing to achieve a value of the SSD
statistic. The statistic R2 yielded significant values indi-
cating demographic expansion in Ribadesella, Punta de la
Cruz, Vila do Conde, Berlengas, Agadir and Mauritania.
Moreover, the Fs statistic, which is more sensitive to
population growth in large samples (Ramos-Onsins and
Rozas 2002), was significant in all samples except Quib-
eron. On the other hand, SSD values for the fitting to the
range expansion model were non-significant (therefore
supporting range expansion) for Saint Guenole, Quiberon,
Ribadesella and Agadir (data not shown).
Relative ratio test yielded non-significant values for all
tested combinations of ingroup and outgroup sequences. This
means that nucleotide substitutions accumulate in a clocklike
manner in the COI sequences here analyzed, and therefore we
can apply a fixed substitution rate. Values of s ranged from
2.242 for Berlengas to 3.613 for Quiberon. The overall s value
for Brittany samples was 3.243 whereas for the rest of
localities was 2.388. Generation time of P. pollicipes has been
observed to be of 1 year, at least in populations of the Iberian
Peninsula (Cruz 1993; Molares 1993). Thus, assuming this
value as a mean for all populations along its distribution range
and using the substitution rate of 3.1% pmy (estimated in
barnacles), the time since demographic expansion is calcu-
lated to be 117,807 years ago for Brittany populations and
86,748 years for Iberian and African samples, both falling
within the Eem interglacial. On the other hand, times of
haplotype coalescence (tmrca) were 198,258 (106,903–
297,387) years (Holstein interglacial) for Brittany samples,
and 167,645 (114,774–226,387) years (Warthe/Saale glacia-
tion) in the case of Iberian and African samples.
Phylogeography
NCA yielded significant results for six clades (Table 5), at
different nesting levels. A biological pattern could be
Table 3 Analyses of molecular variance (AMOVA) of the Pollicipes pollicipes COI sequences
Source of variation Variance
components
Percentage
of variation
U statistic P value
Brittany vs. the rest of samples Among groups 0.05281 2.96 0.02962 0.019
Among populations within groups 0.00260 0.15 0.00150 0.292
Within populations 1.72757 96.89 0.03108 0.008
Brittany vs. Iberian Peninsula vs. Africa Among groups 0.02646 1.51 0.01506 0.023
Among populations within groups 0.00313 0.18 0.00181 0.287
Within populations 1.72757 98.32 0.01684 0.009
Regional configurations with significant value of among groups variation (UCT) are shown. The first one has a higher UCT value, and therefore it
has been taken as the most likely configuration
Table 4 SSD statistic and neutrality tests values for the Pollicipespollicipes populations analyzed in this study
Population SSD R2 Fs s
SG 0.00433 0.0841 -9.5880* 3.249
QUIB 0.03707 0.0906 -3.2085 3.613
JAI – 0.0855 -4.4198* 2.521
MON – 0.0687 -6.7820* 2.592
RIB 0.01431 0.0570* -12.5158* 2.770
CRUZ 0.00413 0.0457* -16.6692* 2.587
COR – 0.0567 -14.9515* 2.396
VC 0.02721 0.0625* -8.0651* 2.686
BER 0.01650 0.0389* -16.9178* 2.242
AGA 0.00668 0.0551* -10.9764* 2.341
MAU – 0.0510* -17.0997* 2.455
Abbreviation codes for population names are given in Table 1.
Numbers in bold letter for SSD values indicate non-significant values
after 1,000 bootstrap replicates, whereas asterisks for R2 and Fs
values indicate significant values (P \ 0.05) through 1,000 coalescent
simulations. Values of s (mutational parameter to estimate time since
demographic expansion) are also shown
152 Mar Biol (2010) 157:147–156
123
inferred for four of them. For Clade 1-20, which includes
haplotypes from Saint Guenole, Punta de la Cruz, Vila do
Conde, Berlengas, Agadir and Mauritania, the inference
was restricted gene flow with isolation by distance. For
Clade 1-25, including haplotypes from all the populations
but Agadir, the outcome was a contiguous range expansion.
For Clade 2-1, the estimated pattern was again restricted
gene flow with isolation by distance. Finally, for Clade 3-2,
the inference was past fragmentation followed by a range
expansion.
Discussion
According to our results, at least two groups of P. pollic-
ipes populations can be identified, one comprises the
French Brittany and the other one includes the rest of the
distribution range. This result agrees with Quinteiro et al.
(2007), who also found significant differences between
Brittany and Iberian Peninsula samples. In addition, our
results also point out isolation by distance as an important
biological factor in shaping the current pattern of popula-
tion structure for P. pollicipes. When excluding Brittany
localities from the analysis, it became non-significant,
suggesting that those more divergent populations were
responsible for the initial significance. However, NCPA
also suggested such a pattern to be present, and Quinteiro
et al. (2007) detected a weak, although significant, pattern
of isolation by distance with mitochondrial D-loop
sequences analysis and suggested that this may reflect the
divergent oceanographic features between European and
African regions.
With the exception of pairwise comparisons involving
Brittany populations, very low levels of genetic divergence
have been found in the present study. This could be due to
either high levels of ongoing gene flow, recent colonization
after a period of isolation, or a combination of both
(Stamatis et al. 2004). Quinteiro et al. (2007) found high
Table 5 Results of the nested
clade analysis (NCA)
Only clades with significant
values of clade (Dc), nested
clade (Dn) and/or interior-tip
distances (I-T) are shown.
Significantly small (S) or large
(L) values are indicated. We
also indicate the steps followed
in the inference key for each
clade and the biological inferred
pattern. The nested cladogram is
shown in Fig. 2
Clade Subclades Dc Dn Steps in the key Inferred pattern
1-13 3 1-2-11-17-NO Inconclusive outcome
14
17
32
47 S
61
76
I-T
1-20 9 1-2-3-4-NO Restricted gene flow with
isolation by distance42
63 S S
I-T
1-25 10 S S 1-19-20-2-11-YES-12-NO Contiguous range expansion
81 L
I-T S S
2-1 1-25 S S 1-2-3-4-NO Restricted gene flow
with isolation by distance1-26 L
I-T L
3-1 2-1 L 1-2-11-17-NO Inconclusive outcome
2-2
2-3
2-4
2-5
I-T
3-2 2-6 1-2-3-5-6-13-YES Past fragmentation followed
by range expansion2-7 S
2-8 L
2-9 L L
2-10
I-T
Mar Biol (2010) 157:147–156 153
123
levels of gene flow for P. pollicipes, which must be med-
iated by larval drift and likely favored by oceanographic
features. A gene flow of just a few individuals per gener-
ation is sufficient to prevent the rise of genetic differenti-
ation between populations (Hartl and Clark 1997). In
contrast, the high number of private haplotypes found
could indicate restricted gene flow (Allendorf and Luikart
2007) or past fragmentation of populations. The results
here obtained suggest that the most likely scenario for the
P. pollicipes samples here analyzed is a past population
fragmentation and moderate to high levels of ongoing gene
flow. NCPA supported this scenario and suggested sub-
sequent range expansion of the fragmented populations. In
addition, a clear pattern of both demographic and range
expansions has been observed in all the localities sampled,
as derived from the mismatch distributions and neutrality
tests results. The starting point of such expansions and the
time of coalescence of the haplotypes seems to be older in
the case of Brittany populations. Estimated dates for these
events were associated with glacial and/or interglacial
periods within the Pleistocene. We estimated a time since
demographic expansion of about 118,000 years for Brit-
tany and 87,000 for Iberian and African populations, both
coinciding with the Eem interglacial period, whereas the
times to the most recent common ancestor were 198,000
(Holstein interglacial) and 168,000 (Warthe/Saale glacia-
tion) years, respectively. Therefore, according to all the
results obtained in this study, we can conclude that the
extreme climatic conditions occurred during the Pleisto-
cene, with alternation of glaciations and interglacial peri-
ods, had a strong influence in the contemporary distribution
of the genetic variation of the European stalked barnacle,
P. pollicipes.
Glacial refugia and contact zones
Genetic signatures of areas that served as refugia for bio-
diversity during Pleistocene glacial stages typically consist
of a higher genetic (haplotypic) diversity with respect to
the adjacent, more recently recolonized areas, and a high
number of private haplotypes; we also expect a high
genetic differentiation between refugia, as genealogical
lineages evolve separately in each one (Hewitt 1996, 2004;
Provan and Bennett 2008). On the other hand, secondary
contact zones, where individuals from different refugia
meet during recolonization at interglacial periods, are also
characterized by high genetic diversity; however, we do not
expect the presence of locally restricted haplotypes (i.e.,
private haplotypes) at these zones. In addition, contact
zones between previously fragmented populations can be
also inferred from the NCA if haplotypes belonging to
different fragmented groups are now present in the same
location (Templeton 2001). In the present study, the
highest haplotypic diversity values have been found in
samples from Saint Guenole, a population located in north
Brittany near the English Channel; in Punta de la Cruz,
located in the northwest of the Iberian Peninsula and in
Mauritania, in North Africa. In addition, Saint Guenole, the
three northwestern Iberian localities (Ribadesella, Punta de
la Cruz and Corme) and the two African samples exhibited
high percentages of private haplotypes (Table 1). All these
data together suggest the existence of a Pleistocene refugial
area off the North African coasts and two northern addi-
tional glacial refugia for P. pollicipes, in the English
Channel/Brittany region and in the northwestern Iberian
Peninsula. These two northern areas have also been sug-
gested to act as refugia for other marine sessile species
(Gomez et al. 2007 for a review; Hoarau et al. 2007;
Provan and Bennett 2008). The high levels of gene flow
encountered for this species (Quinteiro et al. 2007; present
study) could have rapidly homogenized the expanding
populations from North Africa and Iberian Peninsula,
impeding the detection of genetic differences. On the other
hand, the existence in southwestern France of a region
spanning along the coasts of Aquitaine, Poitou-Charentes
and Pays de la Loire, which is characterized by long sandy
beaches and lack of rocky environments, can constitute a
partial barrier for P. pollicipes larval dispersal from the
Iberian Peninsula to Brittany and vice versa, making
homogenization of those populations much slower, even
though gene flow in this area is favored by the Iberian
Poleward Current.
Recolonization pathways
Recolonization pathways from refugial areas should not be
difficult to infer for a species that inhabits the high inter-
tidal zone of continental coasts. In the case of the Brittany
refugium, habitat expansion at interglacial periods was
likely southward, since there is no occurrence of P. pol-
licipes northern than Brittany and genetic diversity
decreased from north to south. From the Iberian refugium,
diversity decreased southward but not to the east; in this
case, although the haplotype diversity was lower for all
samples eastern to Punta de la Cruz, it increased from
Ribadesella to Jaizkibel. In addition, all the haplotypes
found in Monpas and Jaizkibel were also present in both
Brittany and the rest of Iberian samples, and no private
haplotypes were found. This could be explained by a sec-
ondary contact in that area between individuals from the
Brittany and Iberian Peninsula groups during the intergla-
cial expansions since Jaizkibel is located at the eastern
boundary of the Iberian range of distribution. Finally,
expansion from African populations should be toward the
north, since this is the southernmost limit of the species.
Although Quinteiro et al. (2007) only recognized one
154 Mar Biol (2010) 157:147–156
123
refugium for P. pollicipes at tropical and subtropical lati-
tudes, the values of haplotypic diversity found by them at
the AT-rich region of the mitochondrial control region and
a flanking fragment are in agreement with the data here
presented, since they decreased from western Iberian
Peninsula to the south and to the east, and from Canary
Islands to Morocco.
Comparative phylogeography
For marine sessile organisms, climatic conditions during
glacial periods were likely even harder than for non-sessile
species, due to their low capacity of displacement to more
suitable areas, the exposure to cold atmosphere during low-
tide periods (Marko 2004) and the change in sea level
(down to 120 m at LGM). Most marine species are sug-
gested to have followed a pre-LGM expansion model
(Duran et al. 2004; Stamatis et al. 2004; Chevolot et al.
2006; Hoarau et al. 2007), with the exception of some
North Atlantic taxa (Wares and Cunningham 2001) and
two species of the genus Zoostera in Europe (Coyer et al.
2004; Olsen et al. 2004). This could be due to the fact that
climatic conditions during Pleistocene glaciations were less
severe in Europe than in North America, where LGM
conditions should have been especially difficult for rocky
intertidal species (Wares and Cunningham 2001). On the
other hand, the Warthe/Saale glaciation (180,000–
128,000 years ago), which preceded the Eem interglacial
period, probably had a broader effect than the LGM
(Kellaway et al. 1975). Thus, the pattern of demographic
expansion during the Eem interglacial found for P. pol-
licipes is in concordance with that found in many other
marine invertebrates and sessile species of the North
Atlantic, like the bivalve Macoma balthica (Luttikhuizen
et al. 2003), the polychaete tubeworms Pectinaria koreni,
P. auricoma and Owenia fusiformis (Jolly et al. 2006), the
red alga Palmaria palmata (Provan et al. 2005) and the
brown seaweed Fucus serratus (Hoarau et al. 2007). In
addition, Van Syoc (1994) also found a congeneric species,
the eastern Pacific goose barnacle, P. elegans, to have been
affected by periods of cooling and warming during the
Pleistocene, leading to the separation of two differentiated
amphitropical subpopulations with alternating periods of
genetic exchange and isolation.
Conclusions
The current pattern of distribution of the genetic diversity
in the European stalked barnacle, P. pollicipes, can be at
least partially explained by climatic conditions that
occurred during the Pleistocene. During cold glaciation
periods, populations could survive in southern areas off the
North African coast and in two small northern refugial
areas, in the English Channel (Brittany region) and in
northwestern Iberian Peninsula. During warmer interglacial
stages, populations expanded from these areas and sec-
ondary contacts between individuals from those groups
could take place, impeding a total genetic differentiation of
such lineages, and so preventing differential evolution and
speciation events. High levels of gene flow due to high
capacity of larval dispersal also allowed a rapid homoge-
nization of populations, and thus most of the genetic dif-
ferentiation that could arise during population contractions
in refugial areas has been currently minimized.
The identification of cryptic refugia has important
implications in current and future periods of global climate
change (Provan and Bennett 2008) in order to predict and
model the ecological behavior of the species. On the other
hand, barnacles are very plastic species (Barnes and Barnes
1962; Crisp and Bourget 1985) and this, together with the
high levels of gene flow found for P. pollicipes, could
likely guarantee its survival in future climatic changes.
Acknowledgments Samples were collected with the help of Ramon
Riveiro, Jorge L. Alcazar and other anonymous collaborators. We
want to thank Dr. Galice Hoarau for precious help in focusing the
paper. Dr. David Posada helped us with the NCA. Prof. Francis
Juanes revised the article and corrected the English. We also want
to thank two anonymous reviewers for helpful comments. This study
has been financially supported by the Xunta de Galicia (Spain), Grant
SV-05-XUNTA-1.
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