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Barcoding the fishes of Mesoamerica and the Caribbean
0
100
200
300
400
500
600
700
800
900
1000
No. Individual by Region
San Juan
Chiapas-Nicaragua
Chiriqui
Bocas
Santa Maria
Chagres
Tuira
Atrato-San Juan
Grand Total
0
20
40
60
80
100
120
140
160
180
200
No. Families No. Genera No. Species Total No. Ind.
Fish Barcodes Submitted to BOLD
MF Submitted
FWF Submitted
Why barcode Neotropical fish?
•Leverage local enthusiasm for DNA-based scientific inference to promote ichthyological discovery
•Use ichthyological discovery and interest in Neotropical fish to accelerate molecular systematics training for Latin American scientists
•Promote phylogenetic analysis of Neotropical fish through availability of high-quality DNA
•BOLD facilitates collaboration among geographically dispersed investigators
•GENBANK barcodes provide an additional window into a student’s science
•COI barcodes provide an additional ~600 bp of DNA sequence data, which in combination with additional genes distributed around the mitochondrial molecule (e.g. cyt b and ATP synthase) increase likelihood of detecting pseudogenes and contribute to the 2000 bp “needed” for a robust phylogenetic estimate of mtDNA
relationship
Characidae - Astyanax (“aeneus”, includes Bramocharax) - Brycon (‘striatulus’ group, includes chagrensis, behreae, sp. nov. “Bocas”, guatemalensis) - Hyphessobrycon - Roeboides
Heptapteridae - Rhamdia guatemalensis (includes wagneri) - Rhamdia laticauda (includes reddelli, parryi, rogersi, cabrerai, nicaraguensis)
Gymnotidae - Gymnotus
Synbranchidae - Synbranchus + Ophisternon
Study taxa
Miller (1966), Myers (1966)Mesoamerica colonized by primary freshwater fishes following the Pliocene completion of the Panama land bridge. Evidence: Low species diversity of primary freshwater fish species in nuclear Mesoamerica (north of Lake Nicaragua) in comparison to secondary freshwater fishes (Cichlidae, Poecilidae, etc.).
Bussing (1976, 1985)Mesoamerica colonized by freshwater fishes in two waves: “Old Southern” (early Tertiary) and “New Southern” (Pliocene). Evidence: Broad distribution and species richness of “Old Southern” clades, in comparison to narrow, southern distribution and species poverty of the “New Southern” clades.
Testing the alternative hypotheses of Miller and Myers versus Bussing is of general interest for understanding the role that evolutionary time plays in:
• geographic range expansion following invasion
• speciation
• alternative outcomes in the evolutionary assembly of a biota
Marine Geminates
0
1
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5
0.0000.002
0.0040.010
0.0300.050
0.0700.090
0.1100.130
0.1500.170
0.1900.210
0.2300.250
0.2700.290
Gymnotus
0
1
2
3
Marine Geminates
Rhamdia guatemalensis
0
5
10
15
20
25
30
Brycon
0
1
2
3
4
5
6
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9
Gymnotus
Rhamdia guatemalensis
Brycon
Roeboides
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1
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10
Roeboides
(10 genera)
R
ob
.
10 MY2 MY 20 MY3 MY1 MY
Pim
A.
As
t.
BR
W.
Hy
p.
Gy
m.
Sy
n.
Cy
p.
Bra
.
Ra
L.
Ra
G.
Pim
B.
FINAL CLOSURE OF THE PANAMA LAND BRIDGE: 3.1-3.5 MILLION
YEARS BEFORE PRESENT
BR
E.
5 MY
Relative Time Line
PRESENT
10 MY2 MY 20 MY3 MY1 MY
FINAL CLOSURE OF THE PANAMA LAND BRIDGE: 3.1-3.5 MILLION
YEARS BEFORE PRESENT
5 MY
Relative Time Line
PRESENT
Rhamdia guatemalensis
Brycon striatulus group
Late colonists with extreme ranges
10 MY2 MY 20 MY3 MY1 MY
FINAL CLOSURE OF THE PANAMA LAND BRIDGE: 3.1-3.5 MILLION
YEARS BEFORE PRESENT
5 MY
Relative Time Line
PRESENT
Brycon argenteus groupBrachyhypopomus
Early colonists with range expansions cut short
500 Km
Mexico
area ofmain map
LAKE N.
BRW 1
BRW chagres
BRW 2
BRW 3
BRW 4
Rio P. Chic o
Rio A c la
Rio Casjac a l
Rio Cuango
LAKE N.
Rio Acla
Rio P. Chico
Rio Casjacal
Rio Cuango
not shown
BRE 2
BRE 1
BRE acla
BRE p.chico
BRE tuira
BRE bayano
BRE 3
BRE atrato
BRE casjacal
BRE cuango
BRE patia
(b)
(c)
BRE
BRW
A Crude Estimate of the Expansionary Waves of Immigration Assumptions: molecular clock calibration = 3.6% Ks per million years P f , mean historical immigrant propagule (size N=300) K f , mean drainage carrying capacity (N=25,000) Duration of the expansionary waves represented by the polytomies for the Brycon striatulus lineage, approximately 100,000 years
f edge, the mean frequency of dispersal events at the leading edge of the colonizing wave
(BRW = 3600 years) f saturated, the mean frequency of events resulting in the replacement of a resident mtDNA
with that of immigrant’s
(K f /
Pf )
f edge = f saturated
In this Brycon example, the calculated value of f saturated equals 300,000 years, which is the mean time interval between the turnover of occupant lineages by immigrant ones.
500 Km
Mexico
area ofmain map
LAKE N.
BRW 1
BRW chagres
BRW 2
BRW 3
BRW 4
Rio P. Chic o
Rio A c la
Rio Casjac a l
Rio Cuango
LAKE N.
Rio Acla
Rio P. Chico
Rio Casjacal
Rio Cuango
not shown
BRE 2
BRE 1
BRE acla
BRE p.chico
BRE tuira
BRE bayano
BRE 3
BRE atrato
BRE casjacal
BRE cuango
BRE patia
(b)
(c)
BRE
BRW
• Miller and Myers vs Bussing: The former authors had it right and all primary fishes found in northern Mesoamerica dispersed from South America around the time of the Pliocene (~3 MYA) completion of the Panama landbridge.
• geographic range is not strongly influenced by the time since colonization of Mesoamerica.
• speciation is not evident in Mesoamerica primary freshwater fishes in spite of significant phylogeographic structure, phylogenetic evidence indicating that dispersal is not strongly limiting, and ‘experimental’ evidence (not shown) demonstrating that communities are not saturated.
• evolutionary assembly of the Mesoamerican freshwater fish fauna, and striking differences with South American ichthyofauna is explained, in part, by the late arrival of primary freshwater fishes to Mesoamerica.