Ancient genetic bottleneck and Plio-Pleistocene climatic changes imprinted the phylobiogeography of European Black Pine populations
Abstract The historical changes in European Black Pine population size across the whole natural distribution in Europe and Asia Minor were analyzed facing the Plio-Pleistocene climatic fluctuations. Thirteen chloroplast SSRs and SNPs markers have been studied under the assumptions of “neutral evolut...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Naydenov, Krassimir D. [verfasserIn] Naydenov, Michel K. [verfasserIn] Alexandrov, Alexander [verfasserIn] Vasilevski, Kole [verfasserIn] Hinkov, Georgi [verfasserIn] Matevski, Vlado [verfasserIn] Nikolic, Biljana [verfasserIn] Goudiaby, Venceslas [verfasserIn] Riegert, Dave [verfasserIn] Paitaridou, Despina [verfasserIn] Christou, Andreas [verfasserIn] Goia, Irina [verfasserIn] Carcaillet, Christopher [verfasserIn] Escudero Alcantara, Adrian [verfasserIn] Ture, Cengiz [verfasserIn] Gulcu, Suleyman [verfasserIn] Gyuleva, Veselka [verfasserIn] Bojovic, Srdjan [verfasserIn] Peruzzi, Lorenzo [verfasserIn] Kamary, Salim [verfasserIn] Tsarev, Anatoly [verfasserIn] Bogunic, Faruk [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2017 |
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| Schlagwörter: |
Plio-Pleistocene climatic fluctuations |
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| Übergeordnetes Werk: |
Enthalten in: European journal of forest research - Berlin : Springer, 2004, 136(2017), 5-6 vom: 24. Aug., Seite 767-786 |
|---|---|
| Übergeordnetes Werk: |
volume:136 ; year:2017 ; number:5-6 ; day:24 ; month:08 ; pages:767-786 |
| Links: |
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| DOI / URN: |
10.1007/s10342-017-1069-9 |
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| Katalog-ID: |
SPR009741836 |
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| 100 | 1 | |a Naydenov, Krassimir D. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Ancient genetic bottleneck and Plio-Pleistocene climatic changes imprinted the phylobiogeography of European Black Pine populations |
| 264 | 1 | |c 2017 | |
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| 520 | |a Abstract The historical changes in European Black Pine population size across the whole natural distribution in Europe and Asia Minor were analyzed facing the Plio-Pleistocene climatic fluctuations. Thirteen chloroplast SSRs and SNPs markers have been studied under the assumptions of “neutral evolution.” Populations and meta-populations had different histories of migration routes, and they were strongly affected by complex patterns of isolation, fragmentation, speciation, expansion (1.88–4.28 Ma), purification selection (2.09–21.41 Ma) and bottleneck (1.85–21.76 Ma). A significant number of populations (min. 29–41%) were in equilibrium for very long periods. Generally, the bottleneck revealed by chloroplast DNA is weaker than the bottleneck revealed by nuclear DNA. The Ne immediately after the bottleneck reaches between 1820 and 3640 individuals. Generally, the historical effective population sizes shrink significantly for the Tertiary period from 10–15 up to 2.5 Ma in Western Europe (by 82%), followed by Asia Minor (69%) and the Balkan Peninsula (28%), likely resulting from important climatic changes. The rates and frequencies of stepwise westwards migration waves have been not sufficient to prevent isolation between the meta-populations and to suppress “sympatric speciation.” The migration was weak for the Pliocene, but was maximal for the Pleistocene, and finally silent for the present interglacial period, namely the Holocene. | ||
| 650 | 4 | |a Pinus nigra |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Plio-Pleistocene climatic fluctuations |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a cpDNA |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Historical effective population size |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Expansion |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Equilibrium |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Bottleneck |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Migration |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Naydenov, Michel K. |e verfasserin |4 aut | |
| 700 | 1 | |a Alexandrov, Alexander |e verfasserin |4 aut | |
| 700 | 1 | |a Vasilevski, Kole |e verfasserin |4 aut | |
| 700 | 1 | |a Hinkov, Georgi |e verfasserin |4 aut | |
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| 700 | 1 | |a Goudiaby, Venceslas |e verfasserin |4 aut | |
| 700 | 1 | |a Riegert, Dave |e verfasserin |4 aut | |
| 700 | 1 | |a Paitaridou, Despina |e verfasserin |4 aut | |
| 700 | 1 | |a Christou, Andreas |e verfasserin |4 aut | |
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| 700 | 1 | |a Carcaillet, Christopher |e verfasserin |4 aut | |
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| 700 | 1 | |a Ture, Cengiz |e verfasserin |4 aut | |
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| 700 | 1 | |a Bojovic, Srdjan |e verfasserin |4 aut | |
| 700 | 1 | |a Peruzzi, Lorenzo |e verfasserin |4 aut | |
| 700 | 1 | |a Kamary, Salim |e verfasserin |4 aut | |
| 700 | 1 | |a Tsarev, Anatoly |e verfasserin |4 aut | |
| 700 | 1 | |a Bogunic, Faruk |e verfasserin |4 aut | |
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10.1007/s10342-017-1069-9 doi (DE-627)SPR009741836 (SPR)s10342-017-1069-9-e DE-627 ger DE-627 rakwb eng 630 ASE 630 640 ASE 48.40 bkl Naydenov, Krassimir D. verfasserin aut Ancient genetic bottleneck and Plio-Pleistocene climatic changes imprinted the phylobiogeography of European Black Pine populations 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The historical changes in European Black Pine population size across the whole natural distribution in Europe and Asia Minor were analyzed facing the Plio-Pleistocene climatic fluctuations. Thirteen chloroplast SSRs and SNPs markers have been studied under the assumptions of “neutral evolution.” Populations and meta-populations had different histories of migration routes, and they were strongly affected by complex patterns of isolation, fragmentation, speciation, expansion (1.88–4.28 Ma), purification selection (2.09–21.41 Ma) and bottleneck (1.85–21.76 Ma). A significant number of populations (min. 29–41%) were in equilibrium for very long periods. Generally, the bottleneck revealed by chloroplast DNA is weaker than the bottleneck revealed by nuclear DNA. The Ne immediately after the bottleneck reaches between 1820 and 3640 individuals. Generally, the historical effective population sizes shrink significantly for the Tertiary period from 10–15 up to 2.5 Ma in Western Europe (by 82%), followed by Asia Minor (69%) and the Balkan Peninsula (28%), likely resulting from important climatic changes. The rates and frequencies of stepwise westwards migration waves have been not sufficient to prevent isolation between the meta-populations and to suppress “sympatric speciation.” The migration was weak for the Pliocene, but was maximal for the Pleistocene, and finally silent for the present interglacial period, namely the Holocene. Pinus nigra (dpeaa)DE-He213 Plio-Pleistocene climatic fluctuations (dpeaa)DE-He213 cpDNA (dpeaa)DE-He213 Historical effective population size (dpeaa)DE-He213 Expansion (dpeaa)DE-He213 Equilibrium (dpeaa)DE-He213 Bottleneck (dpeaa)DE-He213 Migration (dpeaa)DE-He213 Naydenov, Michel K. verfasserin aut Alexandrov, Alexander verfasserin aut Vasilevski, Kole verfasserin aut Hinkov, Georgi verfasserin aut Matevski, Vlado verfasserin aut Nikolic, Biljana verfasserin aut Goudiaby, Venceslas verfasserin aut Riegert, Dave verfasserin aut Paitaridou, Despina verfasserin aut Christou, Andreas verfasserin aut Goia, Irina verfasserin aut Carcaillet, Christopher verfasserin aut Escudero Alcantara, Adrian verfasserin aut Ture, Cengiz verfasserin aut Gulcu, Suleyman verfasserin aut Gyuleva, Veselka verfasserin aut Bojovic, Srdjan verfasserin aut Peruzzi, Lorenzo verfasserin aut Kamary, Salim verfasserin aut Tsarev, Anatoly verfasserin aut Bogunic, Faruk verfasserin aut Enthalten in European journal of forest research Berlin : Springer, 2004 136(2017), 5-6 vom: 24. Aug., Seite 767-786 (DE-627)378132512 (DE-600)2134019-5 1612-4677 nnns volume:136 year:2017 number:5-6 day:24 month:08 pages:767-786 https://dx.doi.org/10.1007/s10342-017-1069-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 48.40 ASE AR 136 2017 5-6 24 08 767-786 |
| spelling |
10.1007/s10342-017-1069-9 doi (DE-627)SPR009741836 (SPR)s10342-017-1069-9-e DE-627 ger DE-627 rakwb eng 630 ASE 630 640 ASE 48.40 bkl Naydenov, Krassimir D. verfasserin aut Ancient genetic bottleneck and Plio-Pleistocene climatic changes imprinted the phylobiogeography of European Black Pine populations 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The historical changes in European Black Pine population size across the whole natural distribution in Europe and Asia Minor were analyzed facing the Plio-Pleistocene climatic fluctuations. Thirteen chloroplast SSRs and SNPs markers have been studied under the assumptions of “neutral evolution.” Populations and meta-populations had different histories of migration routes, and they were strongly affected by complex patterns of isolation, fragmentation, speciation, expansion (1.88–4.28 Ma), purification selection (2.09–21.41 Ma) and bottleneck (1.85–21.76 Ma). A significant number of populations (min. 29–41%) were in equilibrium for very long periods. Generally, the bottleneck revealed by chloroplast DNA is weaker than the bottleneck revealed by nuclear DNA. The Ne immediately after the bottleneck reaches between 1820 and 3640 individuals. Generally, the historical effective population sizes shrink significantly for the Tertiary period from 10–15 up to 2.5 Ma in Western Europe (by 82%), followed by Asia Minor (69%) and the Balkan Peninsula (28%), likely resulting from important climatic changes. The rates and frequencies of stepwise westwards migration waves have been not sufficient to prevent isolation between the meta-populations and to suppress “sympatric speciation.” The migration was weak for the Pliocene, but was maximal for the Pleistocene, and finally silent for the present interglacial period, namely the Holocene. Pinus nigra (dpeaa)DE-He213 Plio-Pleistocene climatic fluctuations (dpeaa)DE-He213 cpDNA (dpeaa)DE-He213 Historical effective population size (dpeaa)DE-He213 Expansion (dpeaa)DE-He213 Equilibrium (dpeaa)DE-He213 Bottleneck (dpeaa)DE-He213 Migration (dpeaa)DE-He213 Naydenov, Michel K. verfasserin aut Alexandrov, Alexander verfasserin aut Vasilevski, Kole verfasserin aut Hinkov, Georgi verfasserin aut Matevski, Vlado verfasserin aut Nikolic, Biljana verfasserin aut Goudiaby, Venceslas verfasserin aut Riegert, Dave verfasserin aut Paitaridou, Despina verfasserin aut Christou, Andreas verfasserin aut Goia, Irina verfasserin aut Carcaillet, Christopher verfasserin aut Escudero Alcantara, Adrian verfasserin aut Ture, Cengiz verfasserin aut Gulcu, Suleyman verfasserin aut Gyuleva, Veselka verfasserin aut Bojovic, Srdjan verfasserin aut Peruzzi, Lorenzo verfasserin aut Kamary, Salim verfasserin aut Tsarev, Anatoly verfasserin aut Bogunic, Faruk verfasserin aut Enthalten in European journal of forest research Berlin : Springer, 2004 136(2017), 5-6 vom: 24. Aug., Seite 767-786 (DE-627)378132512 (DE-600)2134019-5 1612-4677 nnns volume:136 year:2017 number:5-6 day:24 month:08 pages:767-786 https://dx.doi.org/10.1007/s10342-017-1069-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 48.40 ASE AR 136 2017 5-6 24 08 767-786 |
| allfields_unstemmed |
10.1007/s10342-017-1069-9 doi (DE-627)SPR009741836 (SPR)s10342-017-1069-9-e DE-627 ger DE-627 rakwb eng 630 ASE 630 640 ASE 48.40 bkl Naydenov, Krassimir D. verfasserin aut Ancient genetic bottleneck and Plio-Pleistocene climatic changes imprinted the phylobiogeography of European Black Pine populations 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The historical changes in European Black Pine population size across the whole natural distribution in Europe and Asia Minor were analyzed facing the Plio-Pleistocene climatic fluctuations. Thirteen chloroplast SSRs and SNPs markers have been studied under the assumptions of “neutral evolution.” Populations and meta-populations had different histories of migration routes, and they were strongly affected by complex patterns of isolation, fragmentation, speciation, expansion (1.88–4.28 Ma), purification selection (2.09–21.41 Ma) and bottleneck (1.85–21.76 Ma). A significant number of populations (min. 29–41%) were in equilibrium for very long periods. Generally, the bottleneck revealed by chloroplast DNA is weaker than the bottleneck revealed by nuclear DNA. The Ne immediately after the bottleneck reaches between 1820 and 3640 individuals. Generally, the historical effective population sizes shrink significantly for the Tertiary period from 10–15 up to 2.5 Ma in Western Europe (by 82%), followed by Asia Minor (69%) and the Balkan Peninsula (28%), likely resulting from important climatic changes. The rates and frequencies of stepwise westwards migration waves have been not sufficient to prevent isolation between the meta-populations and to suppress “sympatric speciation.” The migration was weak for the Pliocene, but was maximal for the Pleistocene, and finally silent for the present interglacial period, namely the Holocene. Pinus nigra (dpeaa)DE-He213 Plio-Pleistocene climatic fluctuations (dpeaa)DE-He213 cpDNA (dpeaa)DE-He213 Historical effective population size (dpeaa)DE-He213 Expansion (dpeaa)DE-He213 Equilibrium (dpeaa)DE-He213 Bottleneck (dpeaa)DE-He213 Migration (dpeaa)DE-He213 Naydenov, Michel K. verfasserin aut Alexandrov, Alexander verfasserin aut Vasilevski, Kole verfasserin aut Hinkov, Georgi verfasserin aut Matevski, Vlado verfasserin aut Nikolic, Biljana verfasserin aut Goudiaby, Venceslas verfasserin aut Riegert, Dave verfasserin aut Paitaridou, Despina verfasserin aut Christou, Andreas verfasserin aut Goia, Irina verfasserin aut Carcaillet, Christopher verfasserin aut Escudero Alcantara, Adrian verfasserin aut Ture, Cengiz verfasserin aut Gulcu, Suleyman verfasserin aut Gyuleva, Veselka verfasserin aut Bojovic, Srdjan verfasserin aut Peruzzi, Lorenzo verfasserin aut Kamary, Salim verfasserin aut Tsarev, Anatoly verfasserin aut Bogunic, Faruk verfasserin aut Enthalten in European journal of forest research Berlin : Springer, 2004 136(2017), 5-6 vom: 24. Aug., Seite 767-786 (DE-627)378132512 (DE-600)2134019-5 1612-4677 nnns volume:136 year:2017 number:5-6 day:24 month:08 pages:767-786 https://dx.doi.org/10.1007/s10342-017-1069-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 48.40 ASE AR 136 2017 5-6 24 08 767-786 |
| allfieldsGer |
10.1007/s10342-017-1069-9 doi (DE-627)SPR009741836 (SPR)s10342-017-1069-9-e DE-627 ger DE-627 rakwb eng 630 ASE 630 640 ASE 48.40 bkl Naydenov, Krassimir D. verfasserin aut Ancient genetic bottleneck and Plio-Pleistocene climatic changes imprinted the phylobiogeography of European Black Pine populations 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The historical changes in European Black Pine population size across the whole natural distribution in Europe and Asia Minor were analyzed facing the Plio-Pleistocene climatic fluctuations. Thirteen chloroplast SSRs and SNPs markers have been studied under the assumptions of “neutral evolution.” Populations and meta-populations had different histories of migration routes, and they were strongly affected by complex patterns of isolation, fragmentation, speciation, expansion (1.88–4.28 Ma), purification selection (2.09–21.41 Ma) and bottleneck (1.85–21.76 Ma). A significant number of populations (min. 29–41%) were in equilibrium for very long periods. Generally, the bottleneck revealed by chloroplast DNA is weaker than the bottleneck revealed by nuclear DNA. The Ne immediately after the bottleneck reaches between 1820 and 3640 individuals. Generally, the historical effective population sizes shrink significantly for the Tertiary period from 10–15 up to 2.5 Ma in Western Europe (by 82%), followed by Asia Minor (69%) and the Balkan Peninsula (28%), likely resulting from important climatic changes. The rates and frequencies of stepwise westwards migration waves have been not sufficient to prevent isolation between the meta-populations and to suppress “sympatric speciation.” The migration was weak for the Pliocene, but was maximal for the Pleistocene, and finally silent for the present interglacial period, namely the Holocene. Pinus nigra (dpeaa)DE-He213 Plio-Pleistocene climatic fluctuations (dpeaa)DE-He213 cpDNA (dpeaa)DE-He213 Historical effective population size (dpeaa)DE-He213 Expansion (dpeaa)DE-He213 Equilibrium (dpeaa)DE-He213 Bottleneck (dpeaa)DE-He213 Migration (dpeaa)DE-He213 Naydenov, Michel K. verfasserin aut Alexandrov, Alexander verfasserin aut Vasilevski, Kole verfasserin aut Hinkov, Georgi verfasserin aut Matevski, Vlado verfasserin aut Nikolic, Biljana verfasserin aut Goudiaby, Venceslas verfasserin aut Riegert, Dave verfasserin aut Paitaridou, Despina verfasserin aut Christou, Andreas verfasserin aut Goia, Irina verfasserin aut Carcaillet, Christopher verfasserin aut Escudero Alcantara, Adrian verfasserin aut Ture, Cengiz verfasserin aut Gulcu, Suleyman verfasserin aut Gyuleva, Veselka verfasserin aut Bojovic, Srdjan verfasserin aut Peruzzi, Lorenzo verfasserin aut Kamary, Salim verfasserin aut Tsarev, Anatoly verfasserin aut Bogunic, Faruk verfasserin aut Enthalten in European journal of forest research Berlin : Springer, 2004 136(2017), 5-6 vom: 24. Aug., Seite 767-786 (DE-627)378132512 (DE-600)2134019-5 1612-4677 nnns volume:136 year:2017 number:5-6 day:24 month:08 pages:767-786 https://dx.doi.org/10.1007/s10342-017-1069-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 48.40 ASE AR 136 2017 5-6 24 08 767-786 |
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10.1007/s10342-017-1069-9 doi (DE-627)SPR009741836 (SPR)s10342-017-1069-9-e DE-627 ger DE-627 rakwb eng 630 ASE 630 640 ASE 48.40 bkl Naydenov, Krassimir D. verfasserin aut Ancient genetic bottleneck and Plio-Pleistocene climatic changes imprinted the phylobiogeography of European Black Pine populations 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The historical changes in European Black Pine population size across the whole natural distribution in Europe and Asia Minor were analyzed facing the Plio-Pleistocene climatic fluctuations. Thirteen chloroplast SSRs and SNPs markers have been studied under the assumptions of “neutral evolution.” Populations and meta-populations had different histories of migration routes, and they were strongly affected by complex patterns of isolation, fragmentation, speciation, expansion (1.88–4.28 Ma), purification selection (2.09–21.41 Ma) and bottleneck (1.85–21.76 Ma). A significant number of populations (min. 29–41%) were in equilibrium for very long periods. Generally, the bottleneck revealed by chloroplast DNA is weaker than the bottleneck revealed by nuclear DNA. The Ne immediately after the bottleneck reaches between 1820 and 3640 individuals. Generally, the historical effective population sizes shrink significantly for the Tertiary period from 10–15 up to 2.5 Ma in Western Europe (by 82%), followed by Asia Minor (69%) and the Balkan Peninsula (28%), likely resulting from important climatic changes. The rates and frequencies of stepwise westwards migration waves have been not sufficient to prevent isolation between the meta-populations and to suppress “sympatric speciation.” The migration was weak for the Pliocene, but was maximal for the Pleistocene, and finally silent for the present interglacial period, namely the Holocene. Pinus nigra (dpeaa)DE-He213 Plio-Pleistocene climatic fluctuations (dpeaa)DE-He213 cpDNA (dpeaa)DE-He213 Historical effective population size (dpeaa)DE-He213 Expansion (dpeaa)DE-He213 Equilibrium (dpeaa)DE-He213 Bottleneck (dpeaa)DE-He213 Migration (dpeaa)DE-He213 Naydenov, Michel K. verfasserin aut Alexandrov, Alexander verfasserin aut Vasilevski, Kole verfasserin aut Hinkov, Georgi verfasserin aut Matevski, Vlado verfasserin aut Nikolic, Biljana verfasserin aut Goudiaby, Venceslas verfasserin aut Riegert, Dave verfasserin aut Paitaridou, Despina verfasserin aut Christou, Andreas verfasserin aut Goia, Irina verfasserin aut Carcaillet, Christopher verfasserin aut Escudero Alcantara, Adrian verfasserin aut Ture, Cengiz verfasserin aut Gulcu, Suleyman verfasserin aut Gyuleva, Veselka verfasserin aut Bojovic, Srdjan verfasserin aut Peruzzi, Lorenzo verfasserin aut Kamary, Salim verfasserin aut Tsarev, Anatoly verfasserin aut Bogunic, Faruk verfasserin aut Enthalten in European journal of forest research Berlin : Springer, 2004 136(2017), 5-6 vom: 24. Aug., Seite 767-786 (DE-627)378132512 (DE-600)2134019-5 1612-4677 nnns volume:136 year:2017 number:5-6 day:24 month:08 pages:767-786 https://dx.doi.org/10.1007/s10342-017-1069-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 48.40 ASE AR 136 2017 5-6 24 08 767-786 |
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Enthalten in European journal of forest research 136(2017), 5-6 vom: 24. Aug., Seite 767-786 volume:136 year:2017 number:5-6 day:24 month:08 pages:767-786 |
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Enthalten in European journal of forest research 136(2017), 5-6 vom: 24. Aug., Seite 767-786 volume:136 year:2017 number:5-6 day:24 month:08 pages:767-786 |
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findex.gbv.de |
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Pinus nigra Plio-Pleistocene climatic fluctuations cpDNA Historical effective population size Expansion Equilibrium Bottleneck Migration |
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European journal of forest research |
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Naydenov, Krassimir D. @@aut@@ Naydenov, Michel K. @@aut@@ Alexandrov, Alexander @@aut@@ Vasilevski, Kole @@aut@@ Hinkov, Georgi @@aut@@ Matevski, Vlado @@aut@@ Nikolic, Biljana @@aut@@ Goudiaby, Venceslas @@aut@@ Riegert, Dave @@aut@@ Paitaridou, Despina @@aut@@ Christou, Andreas @@aut@@ Goia, Irina @@aut@@ Carcaillet, Christopher @@aut@@ Escudero Alcantara, Adrian @@aut@@ Ture, Cengiz @@aut@@ Gulcu, Suleyman @@aut@@ Gyuleva, Veselka @@aut@@ Bojovic, Srdjan @@aut@@ Peruzzi, Lorenzo @@aut@@ Kamary, Salim @@aut@@ Tsarev, Anatoly @@aut@@ Bogunic, Faruk @@aut@@ |
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2017-08-24T00:00:00Z |
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| author |
Naydenov, Krassimir D. |
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Naydenov, Krassimir D. ddc 630 bkl 48.40 misc Pinus nigra misc Plio-Pleistocene climatic fluctuations misc cpDNA misc Historical effective population size misc Expansion misc Equilibrium misc Bottleneck misc Migration Ancient genetic bottleneck and Plio-Pleistocene climatic changes imprinted the phylobiogeography of European Black Pine populations |
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630 ASE 630 640 ASE 48.40 bkl Ancient genetic bottleneck and Plio-Pleistocene climatic changes imprinted the phylobiogeography of European Black Pine populations Pinus nigra (dpeaa)DE-He213 Plio-Pleistocene climatic fluctuations (dpeaa)DE-He213 cpDNA (dpeaa)DE-He213 Historical effective population size (dpeaa)DE-He213 Expansion (dpeaa)DE-He213 Equilibrium (dpeaa)DE-He213 Bottleneck (dpeaa)DE-He213 Migration (dpeaa)DE-He213 |
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ddc 630 bkl 48.40 misc Pinus nigra misc Plio-Pleistocene climatic fluctuations misc cpDNA misc Historical effective population size misc Expansion misc Equilibrium misc Bottleneck misc Migration |
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ddc 630 bkl 48.40 misc Pinus nigra misc Plio-Pleistocene climatic fluctuations misc cpDNA misc Historical effective population size misc Expansion misc Equilibrium misc Bottleneck misc Migration |
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Ancient genetic bottleneck and Plio-Pleistocene climatic changes imprinted the phylobiogeography of European Black Pine populations |
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Ancient genetic bottleneck and Plio-Pleistocene climatic changes imprinted the phylobiogeography of European Black Pine populations |
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Naydenov, Krassimir D. |
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European journal of forest research |
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Naydenov, Krassimir D. Naydenov, Michel K. Alexandrov, Alexander Vasilevski, Kole Hinkov, Georgi Matevski, Vlado Nikolic, Biljana Goudiaby, Venceslas Riegert, Dave Paitaridou, Despina Christou, Andreas Goia, Irina Carcaillet, Christopher Escudero Alcantara, Adrian Ture, Cengiz Gulcu, Suleyman Gyuleva, Veselka Bojovic, Srdjan Peruzzi, Lorenzo Kamary, Salim Tsarev, Anatoly Bogunic, Faruk |
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Naydenov, Krassimir D. |
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10.1007/s10342-017-1069-9 |
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ancient genetic bottleneck and plio-pleistocene climatic changes imprinted the phylobiogeography of european black pine populations |
| title_auth |
Ancient genetic bottleneck and Plio-Pleistocene climatic changes imprinted the phylobiogeography of European Black Pine populations |
| abstract |
Abstract The historical changes in European Black Pine population size across the whole natural distribution in Europe and Asia Minor were analyzed facing the Plio-Pleistocene climatic fluctuations. Thirteen chloroplast SSRs and SNPs markers have been studied under the assumptions of “neutral evolution.” Populations and meta-populations had different histories of migration routes, and they were strongly affected by complex patterns of isolation, fragmentation, speciation, expansion (1.88–4.28 Ma), purification selection (2.09–21.41 Ma) and bottleneck (1.85–21.76 Ma). A significant number of populations (min. 29–41%) were in equilibrium for very long periods. Generally, the bottleneck revealed by chloroplast DNA is weaker than the bottleneck revealed by nuclear DNA. The Ne immediately after the bottleneck reaches between 1820 and 3640 individuals. Generally, the historical effective population sizes shrink significantly for the Tertiary period from 10–15 up to 2.5 Ma in Western Europe (by 82%), followed by Asia Minor (69%) and the Balkan Peninsula (28%), likely resulting from important climatic changes. The rates and frequencies of stepwise westwards migration waves have been not sufficient to prevent isolation between the meta-populations and to suppress “sympatric speciation.” The migration was weak for the Pliocene, but was maximal for the Pleistocene, and finally silent for the present interglacial period, namely the Holocene. |
| abstractGer |
Abstract The historical changes in European Black Pine population size across the whole natural distribution in Europe and Asia Minor were analyzed facing the Plio-Pleistocene climatic fluctuations. Thirteen chloroplast SSRs and SNPs markers have been studied under the assumptions of “neutral evolution.” Populations and meta-populations had different histories of migration routes, and they were strongly affected by complex patterns of isolation, fragmentation, speciation, expansion (1.88–4.28 Ma), purification selection (2.09–21.41 Ma) and bottleneck (1.85–21.76 Ma). A significant number of populations (min. 29–41%) were in equilibrium for very long periods. Generally, the bottleneck revealed by chloroplast DNA is weaker than the bottleneck revealed by nuclear DNA. The Ne immediately after the bottleneck reaches between 1820 and 3640 individuals. Generally, the historical effective population sizes shrink significantly for the Tertiary period from 10–15 up to 2.5 Ma in Western Europe (by 82%), followed by Asia Minor (69%) and the Balkan Peninsula (28%), likely resulting from important climatic changes. The rates and frequencies of stepwise westwards migration waves have been not sufficient to prevent isolation between the meta-populations and to suppress “sympatric speciation.” The migration was weak for the Pliocene, but was maximal for the Pleistocene, and finally silent for the present interglacial period, namely the Holocene. |
| abstract_unstemmed |
Abstract The historical changes in European Black Pine population size across the whole natural distribution in Europe and Asia Minor were analyzed facing the Plio-Pleistocene climatic fluctuations. Thirteen chloroplast SSRs and SNPs markers have been studied under the assumptions of “neutral evolution.” Populations and meta-populations had different histories of migration routes, and they were strongly affected by complex patterns of isolation, fragmentation, speciation, expansion (1.88–4.28 Ma), purification selection (2.09–21.41 Ma) and bottleneck (1.85–21.76 Ma). A significant number of populations (min. 29–41%) were in equilibrium for very long periods. Generally, the bottleneck revealed by chloroplast DNA is weaker than the bottleneck revealed by nuclear DNA. The Ne immediately after the bottleneck reaches between 1820 and 3640 individuals. Generally, the historical effective population sizes shrink significantly for the Tertiary period from 10–15 up to 2.5 Ma in Western Europe (by 82%), followed by Asia Minor (69%) and the Balkan Peninsula (28%), likely resulting from important climatic changes. The rates and frequencies of stepwise westwards migration waves have been not sufficient to prevent isolation between the meta-populations and to suppress “sympatric speciation.” The migration was weak for the Pliocene, but was maximal for the Pleistocene, and finally silent for the present interglacial period, namely the Holocene. |
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5-6 |
| title_short |
Ancient genetic bottleneck and Plio-Pleistocene climatic changes imprinted the phylobiogeography of European Black Pine populations |
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https://dx.doi.org/10.1007/s10342-017-1069-9 |
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Naydenov, Michel K. Alexandrov, Alexander Vasilevski, Kole Hinkov, Georgi Matevski, Vlado Nikolic, Biljana Goudiaby, Venceslas Riegert, Dave Paitaridou, Despina Christou, Andreas Goia, Irina Carcaillet, Christopher Escudero Alcantara, Adrian Ture, Cengiz Gulcu, Suleyman Gyuleva, Veselka Bojovic, Srdjan Peruzzi, Lorenzo Kamary, Salim Tsarev, Anatoly Bogunic, Faruk |
| author2Str |
Naydenov, Michel K. Alexandrov, Alexander Vasilevski, Kole Hinkov, Georgi Matevski, Vlado Nikolic, Biljana Goudiaby, Venceslas Riegert, Dave Paitaridou, Despina Christou, Andreas Goia, Irina Carcaillet, Christopher Escudero Alcantara, Adrian Ture, Cengiz Gulcu, Suleyman Gyuleva, Veselka Bojovic, Srdjan Peruzzi, Lorenzo Kamary, Salim Tsarev, Anatoly Bogunic, Faruk |
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| doi_str |
10.1007/s10342-017-1069-9 |
| up_date |
2024-07-04T02:53:25.078Z |
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1803615317610463232 |
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| score |
7.400522 |