Intercontinental dispersal by a microendemic burrowing reptile

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Electronic Supplementary Material for “Intercontinental dispersal by a
microendemic burrowing reptile (Dibamidae)” (Townsend et al.)
I. Supplemental materials and methods
(a) Divergence dating
When used for node calibrations, translated log-normal (TL) distributions effectively place a hard
bound on the minimum age and a soft bound (1) on the maximum age, a desirable property for most fossil
calibrations (2). We thus constructed TL distributions in BEAST with the lower bound of the 95% highest
probability density (HPD) at a point 1% more recent than the estimated fossil age, and we left (somewhat
arbitrarily) long probability tails for the soft maxima. The following fossil-based calibration points were
used (see figure S1 and table S1): (1) The oldest rhynchocephalian (3, 4) was used to constrain the
rhynchocephalian-squamate split within lepidosaurs; (2) the oldest known stem scincomorphs (here defined
as the clade containing the crown taxa Scincidae, Cordylidae, and Xantusiidae) (5, 6) were used to
constrain the scincomorph-iguanian split; (3) the oldest known anguimorph (6, 7) was used to constrain the
anguimorph-iguanian split; (4) the Lepidophyma-Xantusia split (8, 9), (5) the split between erycine and
boiine boids (10), (6) the oldest known helodermatid (11) was used to constrain the helodermatid-anguid
split, and (7) the oldest known crown pleurodont iguanian (12) was used to constrain the age of crowngroup pleurodont iguanians.
(b) Ancestral area inference
Our topological and divergence-dating results rule out Pangean vicariance and dispersal between
Europe and North America as plausible explanations for the current bicontinental distribution of dibamids.
Dispersal between Asia and North America is strongly implicated, but the direction of this dispersal is not
certain. We used two different methods to infer the distribution of the most recent common ancestor (mrca)
of mainland Asian Dibamus and Anelytropsis: (a) Dispersal-extinction-cladogenesis (DEC; 13) analysis in
Lagrange v.20090327 and (b) ancestral-state reconstruction in Mesquite (14). For each taxon in both
analyses, area of occurrence was coded as Mainland Asia, Malaysian Peninsula/Indonesia, or North
America. In the DEC analysis, no ancestral areas were excluded a priori, and no temporal limitations were
placed on dispersal. This method requires an ultrametric tree, and we used the BEAST chronogram for this
purpose. The online “Lagrange configurator” (http://www.reelab.net/lagrange/configurator/index) was used
to produce the Python script that was run locally. The DEC analysis found a 78% probability of an Old
World origin (52% probability of a widespread ancestor occupying Mainland+Peninsula/Indonesia, 26%
probability of a Peninsular/Indonesia ancestor), and a 15% probability that a widespread ancestor inhabited
both Peninsula/Indonesia and North America (only splits within 2 log-likelihood units of the maximum for
a given node are reported, thus the total is slightly less than 100%). This second scenario highlights a
problematic aspect of DEC in this case. As noted above, vicariance of a transcontinentally-distributed
ancestor can be rejected using tectonic and divergence-dating evidence. However, the DEC method is
designed to allow both vicariance and dispersal as possibilities. While it is true that Lagrange allows the
user to exclude some potential ancestral areas on the basis of biological implausibility (13), it is impossible
to sever all connections between two areas. For example, it is impossible to exclude both
Peninsula/Indonesia+North America and Mainland Asia+North America from consideration as potential
species ranges. This same issue also makes analysis using only two codings (Old World or New World)
meaningless; with that configuration, 100% probability is given to a widespread ancestor occupying Old
World and New World.
Ancestral-state reconstruction using models of character evolution (e.g., 15) is not entirely
appropriate either (reviewed in 13). However, its disallowance of vicariant subdivision of widespread
ancestral ranges may actually reflect some aspects of dibamid history better than the DEC method. We
therefore also applied an ML-based version of this method to our system using Mesquite (14) with the
Markov k-state, one-parameter model (all states equally probable). Likelihood optimization on the ML tree
also gave 79% probability of an Asian distribution for the mrca of mainland Asian Dibamus and
Anelytropsis (62% probability for mainland Asia, and 17% probability for Peninsula/Indonesia). In
analyses in which taxa are given one of only two codings (Old World or New World), the probability of an
Asian ancestral distribution is 95%. Thus, although both these methods of ancestral range inference have
their limitations, each supports dispersal from Old World to New World.
II. Geographic distribution of Dibamus and relative propensity for dispersal
The family Dibamidae displays a remarkably conserved morphology, and many
species are distinguishable by only relatively minor differences in scalation and vertebral
counts. The past 25 years has seen the number of recognized species grow from nine (16)
to 21 (17), an expansion largely resulting from the recognition of minute but clear
morphological differences during re-examination of existing collections, rather than
discovery of new populations. The current study has identified deep divergences among
several morphologically similar species, and it seems likely that cryptic species exist.
Even with the probable underestimate of species diversity in this group, a marked pattern
of microendemism is apparent.
Of the 21 currently recognized species of Dibamus, only two or three might be
described as having wide distributions. These include the type species, D. novaeguineae,
which probably occurs on at least western New Guinea, Sulawesi, and the Philippines,
and D. leucurus, which occurs on Sumatra, Borneo, and the southeast Philippines (16). D.
taylori probably occurs on several islands of the Lesser Sundas east of Wallace’s Line,
from Lombock to Wetar (16). Most Indonesian species are confined to single major
islands, and five Dibamus species are endemic to small coastal islands of the Malaysian
peninsula, mainland Southeast Asia, and major Indonesian islands (16-20). Considering
only mainland and peninsular forms, individual species’ distributions are almost
uniformly small. For example, Vietnam has six species, four of which are only known
from their type localities (20-22). Overall, more than half of Dibamus species are known
only from type localities. While this is no doubt partly due to their rarity in collections, a
general pattern of microendemism seems clear, and this in turn suggests the relatively
low vagility that might be expected from limbless, burrowing animals.
However, it is interesting to note that dibamids occur on both sides of Wallace’s
Line, a characteristic that has often been cited as evidence of exceptional dispersal ability
(16). Although this line (and its subsequent modifications) marks a sharp discontinuity in
mammal distributions, birds and reptiles actually show a more gradual east-west change
from Australian to Oriental faunal composition (e.g., see fig. 3.4 in 23). Several squamate
reptile groups, including agamids, gekkonids, scincids, varanids, and acrochordid,
colubrid, pythonid, elapid, typhlopid, viperid, and xenopeltid snakes straddle this line
(24). That dibamids fall into this group is not entirely surprising, as it is easy to imagine
these animals surviving short to moderate sea voyages within mats of flotsam washed
into the ocean during heavy rains. Whether they would be similarly capable of a much
longer trans-Pacific journey is unknown. The fact that several reptile taxa (among them
several those whose distributions span Wallace’s Line) seem clearly to have crossed into
the New World via Beringia (e.g., 25, 26, 27), and none appear to have made this move
via the Pacific, suggests that an overland route is most likely for dibamids as well.
I. SUPPLEMENTAL TABLES
Table S1. Divergence date calibration priors used in BEAST.
Median (95% CI)
(mya)
TLa zero-offset
(mean, st.dev.)
Node
Relevant fossil
Rhyncocephalian –
squamate
Scincomorph – iguanian
Indet. taxon
231 (225, 301)
224 (2.0, 1.2)
Balnealacerta
167 (162, 204)
161 (1.8, 1.0)
Anguimorph – iguanian
Parviraptor
167 (162, 204)
161 (1.8, 1.3)
Xantusia – Lepidophyma
Palaeoxantusia
57 (54.1, 105)
54 (1.0, 1.5)
Erycinae-Boinae
Titanoboa
59 (57.1, 108)
57 (1.0, 1.5)
Helodermatid-anguid
Primaderma
103 (97.4, 182)
97 (1.7, 1.4)
Age of crown pleurodont
iguanians
a
Translated lognormal.
Saichangurvel
28.5 (25, 71)
77 (1.2, 1.5)
Table S2. Likelihood-ratio test (LRT) comparisons of strict-clock vs. non-clock models
for various character subsets of the dibamids-only dataset.
Partition
Interpretation
2 * lnLa
All positions
85.4
Reject clock
Nuclear only
109.8
Reject clock
ND2
15.34
Fail to reject clock
BDNF
10.96
Fail to reject clock
CMOS
13.1
Fail to reject clock
DNAH3
11.76
Fail to reject clock
NKTR
199.76
Reject clock
R35
19.12
Reject clock
RAG1
16.14
Reject clock
a
Test statistic of the LRT, equal to twice the difference in log-likelihoods between the
strict-clock and non-clock analyses. The 2 critical value for all comparisons is 15.51
(0.05 level). All strict-clock analyses placed Anelytropsis as the sister taxon of the
mainland Dibamus clade.
Table S3. GenBank and voucher numbers used in molecular analyses. Non-standard
abbreviations: ATOL (Assembling the Tree of Life project number), AEH (Allen E.
Hebert field series), AMB (Aaron M. Bauer field series), BPN (Brice P. Noonan),
BSI (Sulawesi Biological Surveys and Inventory number of Jim McGuire), LG (Lee
Grismer field series), REE (Robert E. Espinoza field series), RLB (Robert L. Bezy
field number), SBH (S. Blair Hedges field series), and WES (Walter E. Schargel field
series).
TAXON
Voucher
ND2
BDNF
CMOS
AY662533
CAS 206704
AY662553
AB308463
AF128504
Leposoma
parietale
AY662543
A. xera
AY662541
HQ876244
--
GU457846
GU457862
EU402625
A. xera
AY662568
HQ876394
AF544722
AF294279
EU402616
--
--
EU402627
DQ465557
U71332
EU402619
AY987969
--
Sphenodon punctatus
ISIS 373002
Acontias meleagris
No voucher
Aeluroscalobates felinus
Agama agama
LG 6115
ROM 19895
Alopoglossus angulatum
H12975
Amphisbaena fuliginosa
BPN 988
Anelytropsis papillosus
Anilius scytale
Aspidoscelis tigris
MZFC 22828
WES 561
LSUMZ
H0503
SAMA
R54474
SDSU 4350
Basiliscus basiliscus
DMH 86-271
BPU82680
Bipes biporus
MVZ 236256
U71335
Boa constrictor
Calabaria reinhardtii
AEH 040
CAS 207831
AB177354
--
B.
canaliculatus
GU457877
EU402629
EU402631
Chamaeleo calyptratus
MVZ 230099
AF448744
GU457847
Coleonyx mitratus
Coleonyx variegatus
Cordylosaurus subtesselatus
DHL 446
TWR 1925
AMB 6860
HQ876230
HQ876231
HQ876225
Cordylus mossambicus
SDSU 4354
AB308466
NC008774
AY167393
C. polyzonus
AY662561
AF471115
AY099978
Chamaeleo sp.
AF039477
-HQ876391
AY217849
GU457869
DQ100147
Daboia russelli
CAS 213576
NC011391
Delma borea
SAMA
AY134583
Anolis carolinensis
Aspidites melanocephalus
AF039483
GU457870
DQ249061
HQ876229
EU402615
-AF137530
HQ876226
--
GU457876
EU402636
GU457867
AY987986
AF039482
AF471156
AY134547
Dibamus seramensis
Dibamus tiomanensis
Dipsosaurus_dorsalis
Elgaria multicarinata
Epicrates striatus
Eryx colubrinus
Eublepharis macularius
Gambelia wislizenii
R54004
ROM 36056
MVZ 224112
BSI 224
AMNH
144752
FMNH
258662
LSUMZ
H9546
TNHC 59521
LG 4676
TWR 1146
SDSU 3858
SBH 102399
No voucher
No voucher
TWR 1965
Gekko gekko
SDSU 3896
Gonatodes albogularis
Goniurosaurus kuroiwae
Heloderma suspectum
AEH 003
KUZ R62087
ISIS 100503
Lampropeltis getula
SDSU 4351
Lanthanotus borneensis
Leiocephalus barahonensis
Leiolepis belliana
Lepidophyma
flavimaculatum
Leptotyphlops humilis
Lichanura trivirgata
ISIS 393113
SBH 101427
CAS 210725
LACM
128548
SDSU 3939
SAMA
R54372
SDSNH 72826
Liolaemus belli
Liotyphlops albirostris
Micrurus fulvius
Morunasaurus annularis
Dibamus bourreti
Dibamus bourreti
Dibamus celebensis
Dibamus greeri
Dibamus montanus
Dibamus novaeguineae
Lialis burtonis
Oplurus cyclurus
HQ876245
AY662562
HQ876246
HQ876237
HQ876238
HQ876239
HQ876247
HQ876240
HQ876248
HQ876241
HQ876249
GU457863
HQ876395
AY662574
HQ876396
HQ876397
HQ876398
EU116679
HQ876250
HQ876251
AF049857
AF085620
--AB308467
U82682
MVZ 215314
AF114249
-AB308469
AF085603
L. calligaster
DQ902243
AY662537
EF591774
U82689
HQ876242
HQ876243
GQ853275
GU457854
EU402638
DQ465570
GU457864
HQ876217
HQ876399
HQ876400
AF148705
AF039479
AY099966
DQ465568
HQ876392
AY217842
EU402614
AY172929
GU457866
HQ876232
GU457856
EU402645
EF534923
HQ876393
AY662566
GU457859
HQ876223
HQ876216
AB162908
GU457873
AB079597
EU402648
AY662564
DQ119594
AY987982
L. sylvaticum
AY217891
AY099979
AY134599
GU457868
AF090850
--
EU402649
MVZ 196515
AF099223
HQ876220
SBH 172151
TWR Mi f
MVZ 163062
UMMZ
228595
-AY059006
AF528720
O. cuvieri
U82685
EU402650
EU402653
HQ876218
AY099974
L. elongatus
AY367881
AF544727
EF137421
--
GU457850
EU099697
P. thalassinus
AF049858
HQ876221
Uta
stansburiana
AF315389
EU423283
HQ876236
AY221342
Petrosaurus mearnsi
TWR 534
Phelsuma lineata
UMMZ
201554
DQ902091
Physignathus cocincinus
Plestiodon fasciatus
Polychrus marmoratus
MVZ 226495
SDSU 3836
No voucher
Rhacodactylus auriculatus
ABTC 06734
Rhineura floridana
CAS 195955
SAMA
R33647
FMNH
261569
Saltuarius cornutus
Shinisaurus crocodilurus
U82690
AY607299
AF528738
R. chahoua
DQ533741
AY605473
HQ876215
HQ876228
HQ876222
AF039476
AY217869
AY987983
HQ876235
AY172944
GU457878
AY369023
HQ876234
AY444022
S. platurus
AY172941
AF085604
GU457857
AY662565
Stenocercus guentheri
KU 202940
DQ080223
HQ876224
Strophurus ciliaris
ABTC 28467
AY368996
GU457865
AB080237
HQ876227
AF114251
AY662542
T. reticulatus
NC010971
U.
acanthinurus
U71325
HQ876233
GU457879
Tropidurus
plica
EF615737
S. intermedius
AF039469
T. sexlineatus
EF632288
EF534927
AY444025
EU402664
AF544733
GU457849
U. aegyptia
AF137531
AF528734
HQ876219
--
EU920057
GU457860
U71328
AB179620
X. grandis
XGU71333
EU402620
EU402668
DNAH3
NKTR
R35
RAG1
Sphenodon punctatus
Acontias meleagris
Aeluroscalobates felinus
Agama agama
Alopoglossus angulatum
GU457908
GU457931
HQ876417
EU402725
HQ876413
HQ876320
HQ876348
HQ876369
HQ876321
HQ876345
GU457969
GU457993
HQ876446
EU402825
HQ876442
Amphisbaena fuliginosa
GU457936
HQ876252
HQ876281
HQ876298
HQ876253
HQ876278
HQ876285
HQ876352
GU457998
Anelytropsis papillosus
Anilius scytale
GU457923
EU402734
HQ876311
HQ876289
HQ876383
HQ876355
GU457985
EU402834
Teratoscincus scincus
Trogonophis wiegmanni
FMNH
255512
CAS 227618
MVZ 162541
Typhlops jamaicensis
TNHC 55636
Uromastyx_hardwickii
SDSU 4353
Takydromus ocellatus
Xantusia vigilis
Xenopeltis unicolor
LSUMZ
H13960
SAMA
R51088
RLB 5518
CAS 212014
Xenosaurus platyceps
MZFC 9561
Urostrophis vautieri
Varanus acanthurus
TAXON
EU402617
V. rosenbergi
AF039480
AF148703
DQ465561
X. grandis
AY662567
Anolis carolinensis
Aspidites melanocephalus
Aspidoscelis tigris
Basiliscus_basiliscus
Bipes biporus
Boa constrictor
Calabaria reinhardtii
Chamaeleo calyptratus
Coleonyx mitratus
Coleonyx variegatus
Cordylosaurus
subtesselatus
Cordylus mossambicus
Daboia russelli
Delma borea
Dibamus bourreti
Dibamus bourreti
Dibamus celebensis
Dibamus greeri
Dibamus montanus
Dibamus novaeguineae
Dibamus seramensis
Dibamus tiomanensis
EU402726
EU402736
EU402729
HQ876403
HQ876416
EU402738
EU402740
GU457909
HQ876418
HQ876419
Dipsosaurus_dorsalis
HQ876406
Elgaria multicarinata
Epicrates striatus
Eryx colubrinus
Eublepharis macularius
GU457916
EU402746
EU402747
GU457925
Gambelia wislizenii
HQ876404
Gekko gekko
Gonatodes albogularis
Goniurosaurus kuroiwae
Heloderma suspectum
Lampropeltis getula
Lanthanotus borneensis
Leiocephalus
barahonensis
Leiolepis belliana
Lepidophyma
flavimaculatum
Leptotyphlops humilis
Lialis burtonis
Lichanura trivirgata
EU402724
GU457927
HQ876420
GU457917
EU402752
GU457920
TBA
GU457930
EU402745
GU457928
HQ876425
HQ876426
HQ876427
HQ876428
HQ876429
GU457924
HQ876430
HQ876431
HQ876411
HQ876402
GU457933
EU402755
GU457929
EU402756
HQ876266
HQ876297
HQ876282
HQ876258
HQ876286
HQ876291
HQ876293
HQ876255
HQ876299
HQ876300
HQ876277
HQ876334
HQ876365
HQ876349
HQ876326
HQ876353
HQ876357
HQ876359
HQ8763223
HQ876370
HQ876371
HQ876344
EU402826
EU402835
EU402829
TBA
HQ876445
EU402837
EU402839
GU457970
HQ876447
HQ876448
HQ876276
-HQ876309
HQ876312
HQ876313
HQ876314
HQ876315
HQ876316
HQ876317
HQ876318
HQ876319
HQ876261
HQ876343
HQ876367
HQ876381
HQ876384
HQ876385
HQ876386
HQ876387
HQ876388
DQ119613
HQ876389
HQ876390
HQ876329
GU457992
EU402843
GU457990
HQ876454
AY662645
HQ876455
HQ876456
HQ876457
GU457986
HQ876458
HQ876459
CAS208708
FJ356747
HQ876270
HQ876292
-HQ876301
HQ876259
GU457977
EU402844
EU402845
GU457987
HQ876306
HQ876308
HQ876302
HQ876272
-HQ876274
HQ876268
HQ876338
HQ876358
HQ876360
HQ876372
BYU47329
HQ876327
HQ876378
HQ876380
HQ876373
HQ876340
HQ876362
-HQ876336
HQ876256
HQ876283
HQ876324
HQ876350
AY662587
HQ876296
HQ876310
HQ876294
HQ876364
HQ876382
HQ876361
EU402851
GU457991
EU402852
HQ876441
HQ876434
EU402824
GU457989
HQ876449
GU457979
EU402848
GU457982
HQ876439
GU457995
Liolaemus belli
Liotyphlops albirostris
Micrurus fulvius
HQ876408
EU402757
EU402760
Morunasaurus annularis
HQ876405
Oplurus cyclurus
Petrosaurus mearnsi
Phelsuma lineata
Physignathus cocincinus
Plestiodon fasciatus
Polychrus marmoratus
Rhacodactylus auriculatus
Rhineura floridana
Saltuarius cornutus
Shinisaurus crocodilurus
Stenocercus guentheri
Strophurus ciliaris
Takydromus ocellatus
Teratoscincus scincus
Trogonophis wiegmanni
Typhlops jamaicensis
Uromastyx_hardwickii
Urostrophis vautieri
Varanus acanthurus
Xantusia vigilis
Xenopeltis unicolor
Xenosaurus platyceps
GU457912
HQ876409
HQ876424
HQ876401
HQ876415
HQ876410
HQ876423
GU457938
HQ876422
GU457918
HQ876412
GU457926
HQ876414
HQ876421
GU457939
EU402770
GU457911
HQ876407
GU457921
EU402730
EU402774
EU402727
HQ876263
HQ876290
HQ876295
HQ876260
HQ876331
HQ876356
HQ876363
HQ876328
HQ876436
EU402853
EU402856
FJ356741
HQ876264
HQ876265
HQ876307
HQ876254
HQ876280
HQ876267
-HQ876287
HQ876305
HQ876273
HQ876269
HQ876304
HQ876279
HQ876303
HQ876288
-HQ876257
HQ876262
HQ876275
HQ876284
-HQ876271
HQ876332
HQ876333
HQ876379
HQ876322
HQ876347
HQ876335
HQ876377
DQ119613
HQ876376
HQ876341
HQ876337
HQ876375
HQ876346
HQ876374
HQ876354
HQ876366
HQ876325
HQ876330
HQ876342
HQ876351
HQ876368
HQ876339
GU457973
HQ876437
HQ876453
HQ876432
HQ876444
HQ876438
HQ876452
GU458000
HQ876451
GU457980
HQ876440
GU457988
HQ876443
HQ876450
GU458001
EU402866
GU457972
HQ876435
GU457983
EU402830
EU402870
EU402827
Table S4. Primers used in molecular analyses. A non-exhaustive listing of primers used
for amplification and sequencing of each fragment is provided. Unless otherwise noted,
all primers are from Townsend et al. (28). Novel primers developed for this study are
indicated with an asterisk. Primer names ending with “f” are forward primers, and those
ending with “r” are reverse primers.
Gene
Primer name
Primer sequence (5’—3’)
ND2
L4437(f)a
(tRNAMET)
AAGCTTTCGGGCCCATACC
H5692(r)a
(tRNAASN)
TTGGGTGTTTAGCTGTTAA
BDNF_f
GACCATCCTTTTCCTKACTATGGTTATTTCATACTT
BDNF_r
CTATCTTCCCCTTTTAATGGTCAGTGTACAAAC
G73b
GCGGTAAAGCAGGTGAAGAAA
G74b
TGAGCATCCAAAGTCTCCAATC
DNAH3_f1
GGTAAAATGATAGAAGAYTACTG
DNAH3_r6
CTKGAGTTRGAHACAATKATGCCAT
NKTR_f8*
GTAArTGGGAyTCnGArTCAAATTC
NKTR_r13*
GTCTTYCTWACTTCATCAAACAGAG
RAG1_f1ac
CAGCTGYAGCCARTACCATAAAAT
RAG1_r2c
CTTTCTAGCAAAATTTCCATTCAT
BDNF
CMOS
DNAH3
NKTR
RAG-1
R35
a
R35_fd
GACTGTGGAYGAYTCGATCAGTGTGGTGCC
R35_rd
GCCAAAATGAGSGAGAARCGCTTCTGAGC
Macey et al. (29)
Saint et al. (30)
c
Wiens et al. (31)
d
Leaché (32)
b
III. SUPPLEMENTAL FIGURE
Figure S1. BEAST chronogram illustrating complete outgroup sampling. Nodes
marked by black dots were constrained using fossils as described in the main text and
table S1. Scale units are million years ago (Myr).
Supplemental References
1.
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