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Data from: Historical processes and contemporary ocean currents drive genetic structure in the seagrass Thalassia hemprichii in the Indo-Australian Archipelago

The University of Western Australia
Hernawan, Udhi E. ; Van Dijk, Kor-Jent ; Kendrick, Gary A. ; Feng, Ming ; Biffin, Edward ; Lavery, Paul S. ; McMahon, Kathryn
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ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2FANDS&rft_id=info:doi10.5061/dryad.404rm&rft.title=Data from: Historical processes and contemporary ocean currents drive genetic structure in the seagrass Thalassia hemprichii in the Indo-Australian Archipelago&rft.identifier=10.5061/dryad.404rm&rft.publisher=DRYAD&rft.description=Understanding spatial patterns of gene flow and genetic structure is essential for the conservation of marine ecosystems. Contemporary ocean currents and historical isolation due to Pleistocene sea-level fluctuations have been predicted to influence the genetic structure in marine populations. In the Indo-Australian Archipelago (IAA), the world's hotspot of marine biodiversity, seagrasses are a vital component but population genetic information is very limited. Here, we reconstructed the phylogeography of the seagrass Thalassia hemprichii in the IAA based on single nucleotide polymorphisms (SNPs) and then characterised the genetic structure based on a panel of 16 microsatellite markers. We further examined the relative importance of historical isolation and contemporary ocean currents in driving the patterns of genetic structure. Results from SNPs revealed three population groups: eastern Indonesia, western Indonesia (Sunda Shelf), and Indian Ocean; while the microsatellites supported five population groups (eastern Indonesia, Sunda Shelf, Lesser Sunda, Western Australia, and Indian Ocean). Both SNPs and microsatellites showed asymmetrical gene flow among population groups with a trend of south-westward migration from eastern Indonesia. Genetic diversity was generally higher in eastern Indonesia and decreased southwestward. The pattern of genetic structure and connectivity is attributed partly to the Pleistocene sea level fluctuations modified to a smaller level by contemporary ocean currents.,SNP_seq_dataSequence data is in phylip format. Site ID name for each sample can be found the sampling site GPS coordinate fileTh_SNP_data_UdhiHernawan_Chapter3.phyGenotype_msatsGenotype data is in GeAlEx format. Site ID for each sample can be found in the sampling site GPS coordinate file.Genalex_Th3all_IAA.xlsxSampling site GPS coordinatesGPS site IAA.xlsx,&rft.creator=Hernawan, Udhi E. &rft.creator=Van Dijk, Kor-Jent &rft.creator=Kendrick, Gary A. &rft.creator=Feng, Ming &rft.creator=Biffin, Edward &rft.creator=Lavery, Paul S. &rft.creator=McMahon, Kathryn &rft.date=2016&rft.relation=http://research-repository.uwa.edu.au/en/publications/a5cde752-0ae1-4465-be53-4e471170e2a5&rft_subject=gene flow&rft_subject=geological history&rft_subject=microsatellite&rft_subject=Thalassia hemprichii&rft_subject=single nucleotide polymorphisms&rft_subject=ocean current&rft.type=dataset&rft.language=English Access the data

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Understanding spatial patterns of gene flow and genetic structure is essential for the conservation of marine ecosystems. Contemporary ocean currents and historical isolation due to Pleistocene sea-level fluctuations have been predicted to influence the genetic structure in marine populations. In the Indo-Australian Archipelago (IAA), the world's hotspot of marine biodiversity, seagrasses are a vital component but population genetic information is very limited. Here, we reconstructed the phylogeography of the seagrass Thalassia hemprichii in the IAA based on single nucleotide polymorphisms (SNPs) and then characterised the genetic structure based on a panel of 16 microsatellite markers. We further examined the relative importance of historical isolation and contemporary ocean currents in driving the patterns of genetic structure. Results from SNPs revealed three population groups: eastern Indonesia, western Indonesia (Sunda Shelf), and Indian Ocean; while the microsatellites supported five population groups (eastern Indonesia, Sunda Shelf, Lesser Sunda, Western Australia, and Indian Ocean). Both SNPs and microsatellites showed asymmetrical gene flow among population groups with a trend of south-westward migration from eastern Indonesia. Genetic diversity was generally higher in eastern Indonesia and decreased southwestward. The pattern of genetic structure and connectivity is attributed partly to the Pleistocene sea level fluctuations modified to a smaller level by contemporary ocean currents.,SNP_seq_dataSequence data is in phylip format. Site ID name for each sample can be found the sampling site GPS coordinate fileTh_SNP_data_UdhiHernawan_Chapter3.phyGenotype_msatsGenotype data is in GeAlEx format. Site ID for each sample can be found in the sampling site GPS coordinate file.Genalex_Th3all_IAA.xlsxSampling site GPS coordinatesGPS site IAA.xlsx,

Notes

External Organisations
Edith Cowan University; Indonesian Institute of Sciences; University of Adelaide
Associated Persons
Ming Feng (Creator); Paul S. Lavery (Creator); Kathryn McMahon (Creator)Udhi E. Hernawan (Creator); Kor-Jent Van Dijk (Creator); Edward Biffin (Creator)

Issued: 2016-12-19

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