@ARTICLE{TreeBASE2Ref19325,
author = {Jen-Pan Huang and Chung-Ping Lin},
title = {Lineage-Specific Late Pleistocene Expansion of An Endemic Subtropical Gossamer-Wing Damselfly, Euphaea formosa in Taiwan},
year = {2011},
keywords = {},
doi = {10.1186/1471-2148-11-94},
url = {http://},
pmid = {},
journal = {BMC Evolutionary Biology},
volume = {11},
number = {},
pages = {94},
abstract = {Background: Pleistocene glacial oscillations have significantly affected the historical population dynamics of temperate taxa. However, the general effects of recent climatic changes on the evolutionary history and genetic structure of extant subtropical species remain poorly understood. In the present study, phylogeographic and historical demographic analyses based on mitochondrial and nuclear DNA sequences were used. The aim was to investigate whether Pleistocene climatic cycles, paleo-drainages or mountain vicariance of Taiwan shaped the evolutionary diversification of a subtropical gossamer-wing damselfly, Euphaea formosa. Results: E. formosa populations originated in the middle Pleistocene period (0.3 Mya) and consisted of two evolutionarily independent lineages. It is likely that they derived from the Pleistocene paleo-drainages of northern and southern Minjiang, or alternatively by divergence within Taiwan. The ancestral North-central lineage colonized northwestern Taiwan first and maintained a slowly growing population throughout much of the early to middle Pleistocene period. The ancestral widespread lineage reached central-southern Taiwan and experienced a spatial and demographic expansion into eastern Taiwan. This expansion began approximately 30,000 years ago in the Holocene interglacial period. The ancestral southern expansion into eastern Taiwan indicates that the central mountain range (CMR) formed a barrier to east-west expansion. However, E. formosa populations in the three major biogeographic regions (East, South, and North-Central) exhibit no significant genetic partitions, suggesting that river drainages and mountains did not form strong geographical barriers against gene flow among extant populations. Conclusions: The present study implies that the antiquity of E. formosa?s colonization is associated with its high dispersal ability and larval tolerance to the late Pleistocene dry grasslands. The effect of late Pleistocene climatic changes on the subtropical damselfly?s historical demography is lineage-specific, depending predominantly on its colonization history and geography. It is proposed that the Riss and W?rm glaciations in the late Pleistocene period had a greater impact on the evolutionary diversification of subtropical insular species than the last glacial maximum (LGM).}
}
Taxa for Study 11020
Citation title:
"Lineage-Specific Late Pleistocene Expansion of An Endemic Subtropical Gossamer-Wing Damselfly, Euphaea formosa in Taiwan".
Study name:
"Lineage-Specific Late Pleistocene Expansion of An Endemic Subtropical Gossamer-Wing Damselfly, Euphaea formosa in Taiwan".
This study is part of submission 11010
(Status: Published).
Taxa
ID |
Taxon Label |
NCBI taxid |
uBIO namebankID |
1756834 |
Alternaria alternata |
187756
|
5952497
|
1756835 |
Astragalus amphioxys CB Sample 16 5 |
|
3874076
|
1756844 |
Astragalus lentiginosus CB Sample 12 1 |
20416
|
3874134
|
1756839 |
Astragalus lentiginosus CB Sample 17 1 |
20416
|
3874134
|
1756838 |
Astragalus lentiginosus CB Sample 18-2 rpoB |
20416
|
3874134
|
1756850 |
Astragalus mollissimus CB Sample 10 1 |
90190
|
3874150
|
1756845 |
Astragalus mollissimus CB Sample 28 1 |
90190
|
3874150
|
1756847 |
Astragalus mollissimus CB Sample 30 4trnCR |
90190
|
3874150
|
1756841 |
Astragalus mollissimus CB Sample 6 1 rpoB |
90190
|
3874150
|
1756849 |
Astragalus mollissimus CB Sample 7 1 |
90190
|
3874150
|
1756843 |
Astragalus strictus XZ |
|
3769063
|
1756854 |
Astragalus variabilis NM |
545218
|
3906219
|
1756814 |
Brachycladium papaveris |
570640
|
|
1756816 |
Crivellia papaveracea |
84587
|
|
1756829 |
Embellisia allii |
230009
|
3193191
|
1756825 |
Exserohilum pedicellatum |
119929
|
3193704
|
1756828 |
Lewia infectoria |
45303
|
3021733
|
1756823 |
Nimbya caricis |
230008
|
3040178
|
1756852 |
Oxytropis falcata DTH |
|
3906273
|
1756846 |
Oxytropis falcata QL |
|
3906273
|
1756856 |
Oxytropis glabra TGL |
483874
|
2840842
|
1756840 |
Oxytropis glabra XJ |
483874
|
2840842
|
1756842 |
Oxytropis kansuensis MY |
|
3769360
|
1756837 |
Oxytropis kansuensis TZ |
|
3769360
|
1756855 |
Oxytropis ochrocephala Guyuan |
|
2840846
|
1756851 |
Oxytropis ochrocephala Haiyuan |
|
2840846
|
1756848 |
Oxytropis sericea CB Sample 29 1trnCR |
90234
|
3874441
|
1756836 |
Oxytropis sericea CB Sample 34 2trnCR |
90234
|
3874441
|
1756853 |
Oxytropis sericepetala XZ |
|
|
1756807 |
Pleospora herbarum |
33177
|
3872269
|
1756799 |
Stemphylium vesicarium |
119933
|
3216944
|
1756817 |
Ulocladium atrum |
119953
|
3072512
|
1756822 |
Undifilum bornmuelleri |
570681
|
|
1756811 |
Undifilum cinereum |
|
|
1756832 |
Undifilum fulvum 12a 1Fa |
|
|
1756801 |
Undifilum fulvum hm588123 |
|
|
1756833 |
Undifilum oxytropis B9 |
570715
|
|
1756800 |
Undifilum oxytropis DAOM 237697 |
|
|
1756809 |
Undifilum oxytropis L12 |
570715
|
|
1756815 |
Undifilum oxytropis OlB9 |
570715
|
|
1756802 |
Undifilum sp. AS |
|
|
1756827 |
Undifilum sp. AV |
|
|
1756826 |
Undifilum sp. FEL1a |
|
|
1756812 |
Undifilum sp. FEL1b |
|
|
1756813 |
Undifilum sp. FEL2 |
|
|
1756810 |
Undifilum sp. FEL3 |
|
|
1756821 |
Undifilum sp. FEL4 |
|
|
1756831 |
Undifilum sp. FEL6 |
|
|
1756803 |
Undifilum sp. OM |
|
|
1756830 |
Undifilum sp. TGL |
|
|
1756804 |
Undifilum sp. nhz1 |
|
|
1756797 |
Undifilum sp. nhz2 |
|
|
1756818 |
Undifilum sp. nhz3 |
|
|
1756798 |
Undifilum sp. og |
|
|
1756796 |
Undifilum sp. oktz |
|
|
1756819 |
Undifilum sp. okxn21 |
|
|
1756824 |
Undifilum sp. ol |
|
|
1756820 |
Undifilum sp. oy21 |
|
|
1756808 |
Undifilum sp. oy3p |
|
|
1756806 |
Undifilum sp. xgb |
|
|
1756805 |
Undifilum sp. xh3 |
|
|