@ARTICLE{TreeBASE2Ref20737,
author = {Chenyang Liao and Stephen R. Downie and Xingjin He and Yan Yu},
title = {Historical biogeography of the Angelica group (Apiaceaetribe Selineae) inferred from analyses of nrDNA and cpDNA sequences},
year = {2012},
keywords = {Angelica, biogeography, disjunct distribution, divergence time},
doi = {10.1111/j.1759-6831.2012.00182.x},
url = {},
pmid = {},
journal = {Journal of Systematics and Evolution},
volume = {50},
number = {3},
pages = {206--217},
abstract = {Biogeographical patterns and diversi?cation processes of Asia-centered angiosperm groups have been
signi?cantly affected by themultistage uplift of theHimalayas?Tibetan Plateau since the Late Tertiary. The divergence
time of the largely East Asian Angelica group (Apiaceae, subfamily Apioideae, tribe Selineae) was initially analyzed
using BEAST and nrDNA internal transcribed spacer sequence data from 96 representatives of tribe Selineae and
relatives. Further analyses of the biogeographical history of the Angelica group were carried out using BEAST,
S-DIVA,RASP, and LAGRANGE on datasets containing all or some of the following loci: nrDNA internal and external
transcribed spacers; cpDNA rps16 intron; and cpDNA rps16-trnK, rpl32-trnL, and trnL-trnT intergenic spacers.
The results suggested that the Angelica group was originally present in the East Palearctic during the global cooling
of the late Middle Miocene (13.6 Mya) and that the Angelica s.s. clade originated in the same region at 10.2
Mya. Subsequent diversi?cations of the Angelica s.s. clade intensi?ed in the East Palearctic during the middle
Late Miocene (10.0?7.0 Mya) and in the eastern Himalayan Zone during the late Pliocene and Pleistocene (<4.0
Mya). These diversi?cations likely correspondedwith plateau uplift-driven climatic changes. Considering elevational
reconstructions, the differential responses to altitude appear to be the primary factor explaining the recent radiation of
the group in the eastern Himalayas. The North American species of the Angelica group were retrieved as polyphyletic
and their migrations involved six independent dispersals to North America at least since the middle Late Miocene,
including four times from northeast Asia and twice from Europe.}
}
Citation for Study 11565
Citation title:
"Historical biogeography of the Angelica group (Apiaceaetribe Selineae) inferred from analyses of nrDNA and cpDNA sequences".
Study name:
"Historical biogeography of the Angelica group (Apiaceaetribe Selineae) inferred from analyses of nrDNA and cpDNA sequences".
This study is part of submission 11555
(Status: Published).
Citation
Liao C., Downie S.R., He X., & Yu Y. 2012. Historical biogeography of the Angelica group (Apiaceaetribe Selineae) inferred from analyses of nrDNA and cpDNA sequences. Journal of Systematics and Evolution, 50(3): 206-217.
Authors
-
Liao C.
(submitter)
-
Downie S.R.
-
He X.
-
Yu Y.
Abstract
Biogeographical patterns and diversi?cation processes of Asia-centered angiosperm groups have been
signi?cantly affected by themultistage uplift of theHimalayas?Tibetan Plateau since the Late Tertiary. The divergence
time of the largely East Asian Angelica group (Apiaceae, subfamily Apioideae, tribe Selineae) was initially analyzed
using BEAST and nrDNA internal transcribed spacer sequence data from 96 representatives of tribe Selineae and
relatives. Further analyses of the biogeographical history of the Angelica group were carried out using BEAST,
S-DIVA,RASP, and LAGRANGE on datasets containing all or some of the following loci: nrDNA internal and external
transcribed spacers; cpDNA rps16 intron; and cpDNA rps16-trnK, rpl32-trnL, and trnL-trnT intergenic spacers.
The results suggested that the Angelica group was originally present in the East Palearctic during the global cooling
of the late Middle Miocene (13.6 Mya) and that the Angelica s.s. clade originated in the same region at 10.2
Mya. Subsequent diversi?cations of the Angelica s.s. clade intensi?ed in the East Palearctic during the middle
Late Miocene (10.0?7.0 Mya) and in the eastern Himalayan Zone during the late Pliocene and Pleistocene (<4.0
Mya). These diversi?cations likely correspondedwith plateau uplift-driven climatic changes. Considering elevational
reconstructions, the differential responses to altitude appear to be the primary factor explaining the recent radiation of
the group in the eastern Himalayas. The North American species of the Angelica group were retrieved as polyphyletic
and their migrations involved six independent dispersals to North America at least since the middle Late Miocene,
including four times from northeast Asia and twice from Europe.
Keywords
Angelica, biogeography, disjunct distribution, divergence time
External links
About this resource
- Canonical resource URI:
http://purl.org/phylo/treebase/phylows/study/TB2:S11565
- Other versions:
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NeXML
- Show BibTeX reference
@ARTICLE{TreeBASE2Ref20737,
author = {Chenyang Liao and Stephen R. Downie and Xingjin He and Yan Yu},
title = {Historical biogeography of the Angelica group (Apiaceaetribe Selineae) inferred from analyses of nrDNA and cpDNA sequences},
year = {2012},
keywords = {Angelica, biogeography, disjunct distribution, divergence time},
doi = {10.1111/j.1759-6831.2012.00182.x},
url = {},
pmid = {},
journal = {Journal of Systematics and Evolution},
volume = {50},
number = {3},
pages = {206--217},
abstract = {Biogeographical patterns and diversi?cation processes of Asia-centered angiosperm groups have been
signi?cantly affected by themultistage uplift of theHimalayas?Tibetan Plateau since the Late Tertiary. The divergence
time of the largely East Asian Angelica group (Apiaceae, subfamily Apioideae, tribe Selineae) was initially analyzed
using BEAST and nrDNA internal transcribed spacer sequence data from 96 representatives of tribe Selineae and
relatives. Further analyses of the biogeographical history of the Angelica group were carried out using BEAST,
S-DIVA,RASP, and LAGRANGE on datasets containing all or some of the following loci: nrDNA internal and external
transcribed spacers; cpDNA rps16 intron; and cpDNA rps16-trnK, rpl32-trnL, and trnL-trnT intergenic spacers.
The results suggested that the Angelica group was originally present in the East Palearctic during the global cooling
of the late Middle Miocene (13.6 Mya) and that the Angelica s.s. clade originated in the same region at 10.2
Mya. Subsequent diversi?cations of the Angelica s.s. clade intensi?ed in the East Palearctic during the middle
Late Miocene (10.0?7.0 Mya) and in the eastern Himalayan Zone during the late Pliocene and Pleistocene (<4.0
Mya). These diversi?cations likely correspondedwith plateau uplift-driven climatic changes. Considering elevational
reconstructions, the differential responses to altitude appear to be the primary factor explaining the recent radiation of
the group in the eastern Himalayas. The North American species of the Angelica group were retrieved as polyphyletic
and their migrations involved six independent dispersals to North America at least since the middle Late Miocene,
including four times from northeast Asia and twice from Europe.}
}
- Show RIS reference
TY - JOUR
ID - 20737
AU - Liao,Chenyang
AU - Downie,Stephen R.
AU - He,Xingjin
AU - Yu,Yan
T1 - Historical biogeography of the Angelica group (Apiaceaetribe Selineae) inferred from analyses of nrDNA and cpDNA sequences
PY - 2012
KW - Angelica
KW - biogeography
KW - disjunct distribution
KW - divergence time
UR -
N2 - Biogeographical patterns and diversi?cation processes of Asia-centered angiosperm groups have been
signi?cantly affected by themultistage uplift of theHimalayas?Tibetan Plateau since the Late Tertiary. The divergence
time of the largely East Asian Angelica group (Apiaceae, subfamily Apioideae, tribe Selineae) was initially analyzed
using BEAST and nrDNA internal transcribed spacer sequence data from 96 representatives of tribe Selineae and
relatives. Further analyses of the biogeographical history of the Angelica group were carried out using BEAST,
S-DIVA,RASP, and LAGRANGE on datasets containing all or some of the following loci: nrDNA internal and external
transcribed spacers; cpDNA rps16 intron; and cpDNA rps16-trnK, rpl32-trnL, and trnL-trnT intergenic spacers.
The results suggested that the Angelica group was originally present in the East Palearctic during the global cooling
of the late Middle Miocene (13.6 Mya) and that the Angelica s.s. clade originated in the same region at 10.2
Mya. Subsequent diversi?cations of the Angelica s.s. clade intensi?ed in the East Palearctic during the middle
Late Miocene (10.0?7.0 Mya) and in the eastern Himalayan Zone during the late Pliocene and Pleistocene (<4.0
Mya). These diversi?cations likely correspondedwith plateau uplift-driven climatic changes. Considering elevational
reconstructions, the differential responses to altitude appear to be the primary factor explaining the recent radiation of
the group in the eastern Himalayas. The North American species of the Angelica group were retrieved as polyphyletic
and their migrations involved six independent dispersals to North America at least since the middle Late Miocene,
including four times from northeast Asia and twice from Europe.
L3 - 10.1111/j.1759-6831.2012.00182.x
JF - Journal of Systematics and Evolution
VL - 50
IS - 3
SP - 206
EP - 217
ER -
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