Data from: Phylogenetic and biogeographic history of the Snooks (Centropomidae: Carangiformes) spanning the closure of the Isthmus of Panama
Data files
Feb 06, 2025 version files 188.31 KB
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Areas_Snooks.txt
1.54 KB
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Concatenate_snooks_NF
172.44 KB
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FigTree1_in_Ma.tre
3.62 KB
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FigTreeMCMCTree.tre
3.91 KB
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manual_dispersal_multipliers_OLD.txt
1.39 KB
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README.md
5.38 KB
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timeperiods.txt
27 B
Abstract
Aim: Amphiamerican New World fishes provide a unique opportunity to explore the impact of geological processes and the formation of geographic barriers on biological diversification across both spatial and temporal dimensions. We employed phylogenetic and biogeographic methods to assess the impact of the emergence of the isthmus of Panama on the evolutionary history of snooks.
Location: Eastern tropical Pacific and western Atlantic Oceans.
Methods: Bayesian methods were used for phylogenetic inference and divergence time estimation, incorporating the fossil record of Carangidae, Centropomidae, Istiophoriformes, Latidae, and Sphyraenidae to establish a timeline using the methods of stratigraphic intervals for node calibration density specification. Biogeographic models were fitted to test the hypothesis that transisthmian vicariant events are coeval with the Isthmus closure. To estimate ancestral range probability and perform stochastic mapping, we utilized BioGeoBears and the parameters from the best-fitting model. This allowed us to estimate the quantity and kind of biogeographical events.
Results: Our results suggest a sister relationship between Centropomidae and Sphyraenidae with a common ancestor that originated in the Upper Cretaceous (~78.51 Ma). The biogeographic model BAYAreaLIKE + j indicated speciation in sympatry and dispersal (founder effect) as the primary modes of speciation in the genus Centropomus. The dispersion in the family Centropomidae was estimated from the Tropical Eastern Pacific to the tropical western Atlantic since the Oligocene.
Main conclusions: The alignment of divergence times with ancestral species distributions suggests a possible synchrony between the current distribution in Centropomus species and the processes of the formation of the Isthmus of Panama during the Miocene. However, the evidence of only two transisthmic pair suggests that this event was not determinant in allopatric interbasin speciation. Furthermore, recent diversification events within each basin imply an influence of post-closure environmental conditions on the evolution of this group of fishes.
https://doi.org/10.5061/dryad.9s4mw6mpr
Code and data for the Phylogenetic and biogeographic history of the Snooks (Centropomidae: Carangiformes) spanning the closure of the Isthmus of Panama (Ossa-Hernández, Ballen, Acero-P, & Tavera, 2024).
This repository has the following structure:
├── divtime │ ├── clock_modsel │ │ ├── gbm │ │ │ ├── 1..64 │ │ └── iln │ │ ├── 1..64 │ ├── mcmctree1_GBM │ ├── mcmctree1_ILN │ ├── mcmctree2_GBM │ ├── mcmctree2_ILN │ ├── mcmctree3_GBM │ ├── mcmctree3_ILN │ ├── mcmctree4_GBM │ ├── mcmctree4_ILN │ └── phylips ├── mrbayes ├── sequences ├── strat_intervals
sequences
This directory stores the DNA sequences in fasta format used in this study, along with the substitution model selected for each locus. Concatenated versions in both fasta and nexus formats are available along with a file identifying the partition positions in the concatenated dataset.
**Concatenate_snooks_NF **Corresponds to the concatenated matrix composed of five partitions, used for the construction of the phylogenetic hypothesis.
mrbayes
Here we will find the MrBayes script (concatenated.mb) and the output of four independet runs as well as the summarised files.
strat_intervals
The posterior of the origination time for each of the groups used is found here. The files in tsv format include the fossil occurrences. The script strat_interval_posteriors.R will call the code provided in Wang et al. (2016) for the calculations of the posterior density and then return and plot the posterior along with the fossil occurrences used in Figure 1.
The posteriors on the origination time for each group are then used as calibrations on their respective nodes using the truncated Cauchy distribution.
divtime
The maximum credibility tree found in the previous step was used for clock model selection and divergence time estimation using MCMCtree.
phylips
Data in phylip format. Necessary for MCMCtree.
clock_modsel
The file in.BV is the approximation of the multilocus dataset using the gradient and Hessian matrix for use in the approximate likelihood calculations, as generated by MCMCtree.
The stepping stones method used for clock model selection will be found here, under iln for the independent lognormal clock, and under gbm for the geometric Brownian motion model (also known as autocorrelated model). Each of these directories will have three important scripts: step_stones.R, mcmctree.ctl, and run_stepstones.sh. The first one will used the second one in order to generate each of the 64 stones, whereas the third one will iterate over each of the stone directories and submit them.
After finishing the stone runs, the script ../summarise_models.R was used in order to calculate the marginal likelihood for each model and carry out model selection.
Four independent analyses using either the iln or gbm models were carried out (mcmctreeN_MOD where N is the run number 1--4 and MOD is the model, ILN for independent lognormal and GBM for the autocorrelated clock). However, only those of the best model are presented and discussed in the article.
BioGeoBEARS
Biogeographical analyses were performed using the R package "BioGeoBEARs" authored by Nicholas J. Matzke. The scripts were adjusted to our data based on what Nicholas J. Matzke published at http://phylo.wikidot.com/biogeobears. The following tex files were used as inputs for the analysis:
Areas Snooks.txt: A PHYLIP-formatted geography file specifying the geographic areas of the species for the analysis.
**Time_periods.txt:**A file represent a time periods file for a time-stratified analysis. The oldest age correspond to the age of the root of your tree, and there can only be one such age.
**Manual_dispersal_multipliers_OLD.txt: **This file defines the areas permitted during each time period specified in the Time_periods.txt file.
TREE:
The files FigTreein Ma and FigTree are the philogenetic reconstruction in .tree format.
Reference
Ossa‐Hernández, N., Ballen, G. A., P, A. A., & Tavera, J. (2025). Phylogenetic and biogeographic history of the Snooks (Centropomidae: Carangiformes) spanning the closure of the Isthmus of Panama. Journal of Biogeography, 52(1), 232-244.
+: Shared first authorship *: Corresponding author
Sharing/Access information
Links to other publicly accessible locations of the data:
- All the code and data necessary for reproducing the results are available on Zenodo (DOI https://doi.org/10.5281/zenodo.10535162) as well as on https://github.com/gaballench/centropomidae_divtime.
Code/Software
The code for the biogeographical analyses were taken and adapted from http://phylo.wikidot.com/biogeobears, Author: Nicholas J. Matzke.
We collected specimens at local fish markets and landing areas across Caribbean and Pacific localities. All specimens collected were preserved and stored at the fish collection of Universidad del Valle (CIR-UV). Fishes were photographed, and a small fragment of the right pectoral fin was preserved in 96% ethanol and stored at -20 °C.
We extracted DNA following the Salting Out protocol (Sambrook et al. 1989). Four mitochondrial genes (12SrRNA, 16SrRNA, Cytochrome oxidase subunit I - COI, and cytochrome b -CYB) and one nuclear marker, a single-copy locus TMO-4c4 were amplified. The PCR amplification reactions were conducted in a final volume of 15µl containing 1 µl of DNA of stock concentration, 1.5 µl 10X reaction buffer BD (0.8M Tris -HCL, 0.2 M(NH4)2SO4; Solis Bio Dyne), 1.2 µl of 2.0 mM MgCl2, 0.4 mM premixed deoxynucleotide triphosphates, 0.1 µl of 5Uml Taq FIREPOL DNA polymerase (Solis Bio Dyne), and 0.2 µl of each oligonucleotide primer, each at 20mM concentration.
- Ossa Hernandez, Natalia; Tavera, Jose; Ballen, Gustavo A.; Acero Pizarro, Arturo (2025). Data from: Phylogenetic and biogeographic history of the Snooks (Centropomidae: Carangiformes) spanning the closure of the Isthmus of Panama. Zenodo. https://doi.org/10.5281/zenodo.13769601
- Ossa Hernandez, Natalia; Tavera, Jose; Ballen, Gustavo A.; Acero Pizarro, Arturo (2025). Data from: Phylogenetic and biogeographic history of the Snooks (Centropomidae: Carangiformes) spanning the closure of the Isthmus of Panama. Zenodo. https://doi.org/10.5281/zenodo.13769600
- Ossa‐Hernández, Natalia; Ballen, Gustavo A.; P, Arturo Acero; Tavera, Jose (2024). Phylogenetic and Biogeographic History of the Snooks (Centropomidae: Carangiformes) Spanning the Closure of the Isthmus of Panama. Journal of Biogeography. https://doi.org/10.1111/jbi.15018
- Ossa-Hernández, Natalia; Ballen, Gustavo A.; Acero P., Arturo; Tavera, Jose (2024). Phylogenetic and biogeographic history of the Snooks (Centropomidae: Carangiformes) spanning the closure of the Isthmus of Panama [Preprint]. Cold Spring Harbor Laboratory. https://doi.org/10.1101/2024.01.22.576679
