The Réunion Subchron vegetation and climate history of the northeastern Russian Arctic inferred from the Lake El'gygytgyn pollen record
The 318-m-thick sediment record from Lake El'gygytgyn provides unique opportunities for a detailed examination of environmental changes during the Reunion Subchron polarity reversal event (2.1384-2.1216MyrBP) in the northeastern Russian Arctic. The paper describes vegetation and climate fluctua...
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| Autor*in: |
Zhao, W.W [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Rechteinformationen: |
Nutzungsrecht: © COPYRIGHT 2015 Elsevier B.V. |
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| Systematik: |
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| Übergeordnetes Werk: |
Enthalten in: Palaeogeography, palaeoclimatology, palaeoecology - Amsterdam [u.a.] : Elsevier, 1965, 436(2015), Seite 167-177 |
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| Übergeordnetes Werk: |
volume:436 ; year:2015 ; pages:167-177 |
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| DOI / URN: |
10.1016/j.palaeo.2015.06.047 |
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| 245 | 1 | 4 | |a The Réunion Subchron vegetation and climate history of the northeastern Russian Arctic inferred from the Lake El'gygytgyn pollen record |
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| 520 | |a The 318-m-thick sediment record from Lake El'gygytgyn provides unique opportunities for a detailed examination of environmental changes during the Reunion Subchron polarity reversal event (2.1384-2.1216MyrBP) in the northeastern Russian Arctic. The paper describes vegetation and climate fluctuations between ~2.15 and 2.10MyrBP as inferred from palynological data. Biome reconstructions indicate that throughout this interval the tundra (TUND) biome generally has higher affinity scores as compared to cold steppe (STEP) or cold deciduous forest (CLDE). An exception is the climatic optimum between ~2.139 and 2.131MyrBP, coinciding with Marine Isotope Stage 81 (approximately the Reunion Subchron), when the CLDE biome has the highest scores. Landscape-openness indices suggest that more closed vegetation characterized most of the interval between 2.146 and 2.127MyrBP, when deciduous forest and shrubs expanded in the regional vegetation and climate was relatively warm and wet. Peaks in green algal colonies (Botryococcus) and Zygnema-type spores ~2.150-2.146, ~2.131-2.123, and ~2.112-2.102MyrBP indicate expansions of shallow-water habitats and lowered lake levels. Comparisons with biome reconstructions from other interglacial intervals at Lake El'gygytgyn suggest that precession-related summer insolation intensity and obliquity-related duration of summer daylight are major controls on the onset of interglaciations, whereas obliquity probably plays a more significant role on vegetation succession at northern high latitudes during the Pleistocene. | ||
| 540 | |a Nutzungsrecht: © COPYRIGHT 2015 Elsevier B.V. | ||
| 650 | 4 | |a Interglacial periods | |
| 650 | 4 | |a Biomes | |
| 650 | 4 | |a Ecology and history | |
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| 650 | 4 | |a Deciduous forests | |
| 650 | 4 | |a Tundra ecology | |
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| 700 | 1 | |a Andreev, A.A |4 oth | |
| 700 | 1 | |a Wennrich, V |4 oth | |
| 700 | 1 | |a Tarasov, P.E |4 oth | |
| 700 | 1 | |a Anderson, P |4 oth | |
| 700 | 1 | |a Lozhkin, A.V |4 oth | |
| 700 | 1 | |a Melles, M |4 oth | |
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10.1016/j.palaeo.2015.06.047 doi PQ20160617 (DE-627)OLC1966367422 (DE-599)GBVOLC1966367422 (PRQ)c1573-3cc179084a42d5a9c05ed3e283c1d895db9e5b0ed824023cf23413d492e87d410 (KEY)0057041920150000436000000167runionsubchronvegetationandclimatehistoryofthenort DE-627 ger DE-627 rakwb eng 570 550 930 DNB TE 1000 AVZ rvk Zhao, W.W verfasserin aut The Réunion Subchron vegetation and climate history of the northeastern Russian Arctic inferred from the Lake El'gygytgyn pollen record 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The 318-m-thick sediment record from Lake El'gygytgyn provides unique opportunities for a detailed examination of environmental changes during the Reunion Subchron polarity reversal event (2.1384-2.1216MyrBP) in the northeastern Russian Arctic. The paper describes vegetation and climate fluctuations between ~2.15 and 2.10MyrBP as inferred from palynological data. Biome reconstructions indicate that throughout this interval the tundra (TUND) biome generally has higher affinity scores as compared to cold steppe (STEP) or cold deciduous forest (CLDE). An exception is the climatic optimum between ~2.139 and 2.131MyrBP, coinciding with Marine Isotope Stage 81 (approximately the Reunion Subchron), when the CLDE biome has the highest scores. Landscape-openness indices suggest that more closed vegetation characterized most of the interval between 2.146 and 2.127MyrBP, when deciduous forest and shrubs expanded in the regional vegetation and climate was relatively warm and wet. Peaks in green algal colonies (Botryococcus) and Zygnema-type spores ~2.150-2.146, ~2.131-2.123, and ~2.112-2.102MyrBP indicate expansions of shallow-water habitats and lowered lake levels. Comparisons with biome reconstructions from other interglacial intervals at Lake El'gygytgyn suggest that precession-related summer insolation intensity and obliquity-related duration of summer daylight are major controls on the onset of interglaciations, whereas obliquity probably plays a more significant role on vegetation succession at northern high latitudes during the Pleistocene. Nutzungsrecht: © COPYRIGHT 2015 Elsevier B.V. Interglacial periods Biomes Ecology and history Analysis Deciduous forests Tundra ecology Climate Andreev, A.A oth Wennrich, V oth Tarasov, P.E oth Anderson, P oth Lozhkin, A.V oth Melles, M oth Enthalten in Palaeogeography, palaeoclimatology, palaeoecology Amsterdam [u.a.] : Elsevier, 1965 436(2015), Seite 167-177 (DE-627)130007803 (DE-600)417718-6 (DE-576)015553892 0031-0182 nnns volume:436 year:2015 pages:167-177 http://dx.doi.org/10.1016/j.palaeo.2015.06.047 Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_21 GBV_ILN_70 GBV_ILN_2027 GBV_ILN_2173 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4112 GBV_ILN_4305 TE 1000 AR 436 2015 167-177 |
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10.1016/j.palaeo.2015.06.047 doi PQ20160617 (DE-627)OLC1966367422 (DE-599)GBVOLC1966367422 (PRQ)c1573-3cc179084a42d5a9c05ed3e283c1d895db9e5b0ed824023cf23413d492e87d410 (KEY)0057041920150000436000000167runionsubchronvegetationandclimatehistoryofthenort DE-627 ger DE-627 rakwb eng 570 550 930 DNB TE 1000 AVZ rvk Zhao, W.W verfasserin aut The Réunion Subchron vegetation and climate history of the northeastern Russian Arctic inferred from the Lake El'gygytgyn pollen record 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The 318-m-thick sediment record from Lake El'gygytgyn provides unique opportunities for a detailed examination of environmental changes during the Reunion Subchron polarity reversal event (2.1384-2.1216MyrBP) in the northeastern Russian Arctic. The paper describes vegetation and climate fluctuations between ~2.15 and 2.10MyrBP as inferred from palynological data. Biome reconstructions indicate that throughout this interval the tundra (TUND) biome generally has higher affinity scores as compared to cold steppe (STEP) or cold deciduous forest (CLDE). An exception is the climatic optimum between ~2.139 and 2.131MyrBP, coinciding with Marine Isotope Stage 81 (approximately the Reunion Subchron), when the CLDE biome has the highest scores. Landscape-openness indices suggest that more closed vegetation characterized most of the interval between 2.146 and 2.127MyrBP, when deciduous forest and shrubs expanded in the regional vegetation and climate was relatively warm and wet. Peaks in green algal colonies (Botryococcus) and Zygnema-type spores ~2.150-2.146, ~2.131-2.123, and ~2.112-2.102MyrBP indicate expansions of shallow-water habitats and lowered lake levels. Comparisons with biome reconstructions from other interglacial intervals at Lake El'gygytgyn suggest that precession-related summer insolation intensity and obliquity-related duration of summer daylight are major controls on the onset of interglaciations, whereas obliquity probably plays a more significant role on vegetation succession at northern high latitudes during the Pleistocene. Nutzungsrecht: © COPYRIGHT 2015 Elsevier B.V. Interglacial periods Biomes Ecology and history Analysis Deciduous forests Tundra ecology Climate Andreev, A.A oth Wennrich, V oth Tarasov, P.E oth Anderson, P oth Lozhkin, A.V oth Melles, M oth Enthalten in Palaeogeography, palaeoclimatology, palaeoecology Amsterdam [u.a.] : Elsevier, 1965 436(2015), Seite 167-177 (DE-627)130007803 (DE-600)417718-6 (DE-576)015553892 0031-0182 nnns volume:436 year:2015 pages:167-177 http://dx.doi.org/10.1016/j.palaeo.2015.06.047 Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_21 GBV_ILN_70 GBV_ILN_2027 GBV_ILN_2173 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4112 GBV_ILN_4305 TE 1000 AR 436 2015 167-177 |
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10.1016/j.palaeo.2015.06.047 doi PQ20160617 (DE-627)OLC1966367422 (DE-599)GBVOLC1966367422 (PRQ)c1573-3cc179084a42d5a9c05ed3e283c1d895db9e5b0ed824023cf23413d492e87d410 (KEY)0057041920150000436000000167runionsubchronvegetationandclimatehistoryofthenort DE-627 ger DE-627 rakwb eng 570 550 930 DNB TE 1000 AVZ rvk Zhao, W.W verfasserin aut The Réunion Subchron vegetation and climate history of the northeastern Russian Arctic inferred from the Lake El'gygytgyn pollen record 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The 318-m-thick sediment record from Lake El'gygytgyn provides unique opportunities for a detailed examination of environmental changes during the Reunion Subchron polarity reversal event (2.1384-2.1216MyrBP) in the northeastern Russian Arctic. The paper describes vegetation and climate fluctuations between ~2.15 and 2.10MyrBP as inferred from palynological data. Biome reconstructions indicate that throughout this interval the tundra (TUND) biome generally has higher affinity scores as compared to cold steppe (STEP) or cold deciduous forest (CLDE). An exception is the climatic optimum between ~2.139 and 2.131MyrBP, coinciding with Marine Isotope Stage 81 (approximately the Reunion Subchron), when the CLDE biome has the highest scores. Landscape-openness indices suggest that more closed vegetation characterized most of the interval between 2.146 and 2.127MyrBP, when deciduous forest and shrubs expanded in the regional vegetation and climate was relatively warm and wet. Peaks in green algal colonies (Botryococcus) and Zygnema-type spores ~2.150-2.146, ~2.131-2.123, and ~2.112-2.102MyrBP indicate expansions of shallow-water habitats and lowered lake levels. Comparisons with biome reconstructions from other interglacial intervals at Lake El'gygytgyn suggest that precession-related summer insolation intensity and obliquity-related duration of summer daylight are major controls on the onset of interglaciations, whereas obliquity probably plays a more significant role on vegetation succession at northern high latitudes during the Pleistocene. Nutzungsrecht: © COPYRIGHT 2015 Elsevier B.V. Interglacial periods Biomes Ecology and history Analysis Deciduous forests Tundra ecology Climate Andreev, A.A oth Wennrich, V oth Tarasov, P.E oth Anderson, P oth Lozhkin, A.V oth Melles, M oth Enthalten in Palaeogeography, palaeoclimatology, palaeoecology Amsterdam [u.a.] : Elsevier, 1965 436(2015), Seite 167-177 (DE-627)130007803 (DE-600)417718-6 (DE-576)015553892 0031-0182 nnns volume:436 year:2015 pages:167-177 http://dx.doi.org/10.1016/j.palaeo.2015.06.047 Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_21 GBV_ILN_70 GBV_ILN_2027 GBV_ILN_2173 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4112 GBV_ILN_4305 TE 1000 AR 436 2015 167-177 |
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10.1016/j.palaeo.2015.06.047 doi PQ20160617 (DE-627)OLC1966367422 (DE-599)GBVOLC1966367422 (PRQ)c1573-3cc179084a42d5a9c05ed3e283c1d895db9e5b0ed824023cf23413d492e87d410 (KEY)0057041920150000436000000167runionsubchronvegetationandclimatehistoryofthenort DE-627 ger DE-627 rakwb eng 570 550 930 DNB TE 1000 AVZ rvk Zhao, W.W verfasserin aut The Réunion Subchron vegetation and climate history of the northeastern Russian Arctic inferred from the Lake El'gygytgyn pollen record 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The 318-m-thick sediment record from Lake El'gygytgyn provides unique opportunities for a detailed examination of environmental changes during the Reunion Subchron polarity reversal event (2.1384-2.1216MyrBP) in the northeastern Russian Arctic. The paper describes vegetation and climate fluctuations between ~2.15 and 2.10MyrBP as inferred from palynological data. Biome reconstructions indicate that throughout this interval the tundra (TUND) biome generally has higher affinity scores as compared to cold steppe (STEP) or cold deciduous forest (CLDE). An exception is the climatic optimum between ~2.139 and 2.131MyrBP, coinciding with Marine Isotope Stage 81 (approximately the Reunion Subchron), when the CLDE biome has the highest scores. Landscape-openness indices suggest that more closed vegetation characterized most of the interval between 2.146 and 2.127MyrBP, when deciduous forest and shrubs expanded in the regional vegetation and climate was relatively warm and wet. Peaks in green algal colonies (Botryococcus) and Zygnema-type spores ~2.150-2.146, ~2.131-2.123, and ~2.112-2.102MyrBP indicate expansions of shallow-water habitats and lowered lake levels. Comparisons with biome reconstructions from other interglacial intervals at Lake El'gygytgyn suggest that precession-related summer insolation intensity and obliquity-related duration of summer daylight are major controls on the onset of interglaciations, whereas obliquity probably plays a more significant role on vegetation succession at northern high latitudes during the Pleistocene. Nutzungsrecht: © COPYRIGHT 2015 Elsevier B.V. Interglacial periods Biomes Ecology and history Analysis Deciduous forests Tundra ecology Climate Andreev, A.A oth Wennrich, V oth Tarasov, P.E oth Anderson, P oth Lozhkin, A.V oth Melles, M oth Enthalten in Palaeogeography, palaeoclimatology, palaeoecology Amsterdam [u.a.] : Elsevier, 1965 436(2015), Seite 167-177 (DE-627)130007803 (DE-600)417718-6 (DE-576)015553892 0031-0182 nnns volume:436 year:2015 pages:167-177 http://dx.doi.org/10.1016/j.palaeo.2015.06.047 Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_21 GBV_ILN_70 GBV_ILN_2027 GBV_ILN_2173 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4112 GBV_ILN_4305 TE 1000 AR 436 2015 167-177 |
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10.1016/j.palaeo.2015.06.047 doi PQ20160617 (DE-627)OLC1966367422 (DE-599)GBVOLC1966367422 (PRQ)c1573-3cc179084a42d5a9c05ed3e283c1d895db9e5b0ed824023cf23413d492e87d410 (KEY)0057041920150000436000000167runionsubchronvegetationandclimatehistoryofthenort DE-627 ger DE-627 rakwb eng 570 550 930 DNB TE 1000 AVZ rvk Zhao, W.W verfasserin aut The Réunion Subchron vegetation and climate history of the northeastern Russian Arctic inferred from the Lake El'gygytgyn pollen record 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The 318-m-thick sediment record from Lake El'gygytgyn provides unique opportunities for a detailed examination of environmental changes during the Reunion Subchron polarity reversal event (2.1384-2.1216MyrBP) in the northeastern Russian Arctic. The paper describes vegetation and climate fluctuations between ~2.15 and 2.10MyrBP as inferred from palynological data. Biome reconstructions indicate that throughout this interval the tundra (TUND) biome generally has higher affinity scores as compared to cold steppe (STEP) or cold deciduous forest (CLDE). An exception is the climatic optimum between ~2.139 and 2.131MyrBP, coinciding with Marine Isotope Stage 81 (approximately the Reunion Subchron), when the CLDE biome has the highest scores. Landscape-openness indices suggest that more closed vegetation characterized most of the interval between 2.146 and 2.127MyrBP, when deciduous forest and shrubs expanded in the regional vegetation and climate was relatively warm and wet. Peaks in green algal colonies (Botryococcus) and Zygnema-type spores ~2.150-2.146, ~2.131-2.123, and ~2.112-2.102MyrBP indicate expansions of shallow-water habitats and lowered lake levels. Comparisons with biome reconstructions from other interglacial intervals at Lake El'gygytgyn suggest that precession-related summer insolation intensity and obliquity-related duration of summer daylight are major controls on the onset of interglaciations, whereas obliquity probably plays a more significant role on vegetation succession at northern high latitudes during the Pleistocene. Nutzungsrecht: © COPYRIGHT 2015 Elsevier B.V. Interglacial periods Biomes Ecology and history Analysis Deciduous forests Tundra ecology Climate Andreev, A.A oth Wennrich, V oth Tarasov, P.E oth Anderson, P oth Lozhkin, A.V oth Melles, M oth Enthalten in Palaeogeography, palaeoclimatology, palaeoecology Amsterdam [u.a.] : Elsevier, 1965 436(2015), Seite 167-177 (DE-627)130007803 (DE-600)417718-6 (DE-576)015553892 0031-0182 nnns volume:436 year:2015 pages:167-177 http://dx.doi.org/10.1016/j.palaeo.2015.06.047 Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_21 GBV_ILN_70 GBV_ILN_2027 GBV_ILN_2173 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4112 GBV_ILN_4305 TE 1000 AR 436 2015 167-177 |
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réunion subchron vegetation and climate history of the northeastern russian arctic inferred from the lake el'gygytgyn pollen record |
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The Réunion Subchron vegetation and climate history of the northeastern Russian Arctic inferred from the Lake El'gygytgyn pollen record |
| abstract |
The 318-m-thick sediment record from Lake El'gygytgyn provides unique opportunities for a detailed examination of environmental changes during the Reunion Subchron polarity reversal event (2.1384-2.1216MyrBP) in the northeastern Russian Arctic. The paper describes vegetation and climate fluctuations between ~2.15 and 2.10MyrBP as inferred from palynological data. Biome reconstructions indicate that throughout this interval the tundra (TUND) biome generally has higher affinity scores as compared to cold steppe (STEP) or cold deciduous forest (CLDE). An exception is the climatic optimum between ~2.139 and 2.131MyrBP, coinciding with Marine Isotope Stage 81 (approximately the Reunion Subchron), when the CLDE biome has the highest scores. Landscape-openness indices suggest that more closed vegetation characterized most of the interval between 2.146 and 2.127MyrBP, when deciduous forest and shrubs expanded in the regional vegetation and climate was relatively warm and wet. Peaks in green algal colonies (Botryococcus) and Zygnema-type spores ~2.150-2.146, ~2.131-2.123, and ~2.112-2.102MyrBP indicate expansions of shallow-water habitats and lowered lake levels. Comparisons with biome reconstructions from other interglacial intervals at Lake El'gygytgyn suggest that precession-related summer insolation intensity and obliquity-related duration of summer daylight are major controls on the onset of interglaciations, whereas obliquity probably plays a more significant role on vegetation succession at northern high latitudes during the Pleistocene. |
| abstractGer |
The 318-m-thick sediment record from Lake El'gygytgyn provides unique opportunities for a detailed examination of environmental changes during the Reunion Subchron polarity reversal event (2.1384-2.1216MyrBP) in the northeastern Russian Arctic. The paper describes vegetation and climate fluctuations between ~2.15 and 2.10MyrBP as inferred from palynological data. Biome reconstructions indicate that throughout this interval the tundra (TUND) biome generally has higher affinity scores as compared to cold steppe (STEP) or cold deciduous forest (CLDE). An exception is the climatic optimum between ~2.139 and 2.131MyrBP, coinciding with Marine Isotope Stage 81 (approximately the Reunion Subchron), when the CLDE biome has the highest scores. Landscape-openness indices suggest that more closed vegetation characterized most of the interval between 2.146 and 2.127MyrBP, when deciduous forest and shrubs expanded in the regional vegetation and climate was relatively warm and wet. Peaks in green algal colonies (Botryococcus) and Zygnema-type spores ~2.150-2.146, ~2.131-2.123, and ~2.112-2.102MyrBP indicate expansions of shallow-water habitats and lowered lake levels. Comparisons with biome reconstructions from other interglacial intervals at Lake El'gygytgyn suggest that precession-related summer insolation intensity and obliquity-related duration of summer daylight are major controls on the onset of interglaciations, whereas obliquity probably plays a more significant role on vegetation succession at northern high latitudes during the Pleistocene. |
| abstract_unstemmed |
The 318-m-thick sediment record from Lake El'gygytgyn provides unique opportunities for a detailed examination of environmental changes during the Reunion Subchron polarity reversal event (2.1384-2.1216MyrBP) in the northeastern Russian Arctic. The paper describes vegetation and climate fluctuations between ~2.15 and 2.10MyrBP as inferred from palynological data. Biome reconstructions indicate that throughout this interval the tundra (TUND) biome generally has higher affinity scores as compared to cold steppe (STEP) or cold deciduous forest (CLDE). An exception is the climatic optimum between ~2.139 and 2.131MyrBP, coinciding with Marine Isotope Stage 81 (approximately the Reunion Subchron), when the CLDE biome has the highest scores. Landscape-openness indices suggest that more closed vegetation characterized most of the interval between 2.146 and 2.127MyrBP, when deciduous forest and shrubs expanded in the regional vegetation and climate was relatively warm and wet. Peaks in green algal colonies (Botryococcus) and Zygnema-type spores ~2.150-2.146, ~2.131-2.123, and ~2.112-2.102MyrBP indicate expansions of shallow-water habitats and lowered lake levels. Comparisons with biome reconstructions from other interglacial intervals at Lake El'gygytgyn suggest that precession-related summer insolation intensity and obliquity-related duration of summer daylight are major controls on the onset of interglaciations, whereas obliquity probably plays a more significant role on vegetation succession at northern high latitudes during the Pleistocene. |
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| title_short |
The Réunion Subchron vegetation and climate history of the northeastern Russian Arctic inferred from the Lake El'gygytgyn pollen record |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a2200265 4500</leader><controlfield tag="001">OLC1966367422</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230714165334.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">160206s2015 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.palaeo.2015.06.047</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">PQ20160617</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC1966367422</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)GBVOLC1966367422</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(PRQ)c1573-3cc179084a42d5a9c05ed3e283c1d895db9e5b0ed824023cf23413d492e87d410</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(KEY)0057041920150000436000000167runionsubchronvegetationandclimatehistoryofthenort</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">570</subfield><subfield code="a">550</subfield><subfield code="a">930</subfield><subfield code="q">DNB</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">TE 1000</subfield><subfield code="q">AVZ</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Zhao, W.W</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="4"><subfield code="a">The Réunion Subchron vegetation and climate history of the northeastern Russian Arctic inferred from the Lake El'gygytgyn pollen record</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2015</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The 318-m-thick sediment record from Lake El'gygytgyn provides unique opportunities for a detailed examination of environmental changes during the Reunion Subchron polarity reversal event (2.1384-2.1216MyrBP) in the northeastern Russian Arctic. The paper describes vegetation and climate fluctuations between ~2.15 and 2.10MyrBP as inferred from palynological data. Biome reconstructions indicate that throughout this interval the tundra (TUND) biome generally has higher affinity scores as compared to cold steppe (STEP) or cold deciduous forest (CLDE). An exception is the climatic optimum between ~2.139 and 2.131MyrBP, coinciding with Marine Isotope Stage 81 (approximately the Reunion Subchron), when the CLDE biome has the highest scores. Landscape-openness indices suggest that more closed vegetation characterized most of the interval between 2.146 and 2.127MyrBP, when deciduous forest and shrubs expanded in the regional vegetation and climate was relatively warm and wet. Peaks in green algal colonies (Botryococcus) and Zygnema-type spores ~2.150-2.146, ~2.131-2.123, and ~2.112-2.102MyrBP indicate expansions of shallow-water habitats and lowered lake levels. Comparisons with biome reconstructions from other interglacial intervals at Lake El'gygytgyn suggest that precession-related summer insolation intensity and obliquity-related duration of summer daylight are major controls on the onset of interglaciations, whereas obliquity probably plays a more significant role on vegetation succession at northern high latitudes during the Pleistocene.</subfield></datafield><datafield tag="540" ind1=" " ind2=" "><subfield code="a">Nutzungsrecht: © COPYRIGHT 2015 Elsevier B.V.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Interglacial periods</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Biomes</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Ecology and history</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Analysis</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Deciduous forests</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Tundra ecology</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Climate</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Andreev, A.A</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wennrich, V</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Tarasov, P.E</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Anderson, P</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Lozhkin, A.V</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Melles, M</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Palaeogeography, palaeoclimatology, palaeoecology</subfield><subfield code="d">Amsterdam [u.a.] : Elsevier, 1965</subfield><subfield code="g">436(2015), Seite 167-177</subfield><subfield code="w">(DE-627)130007803</subfield><subfield code="w">(DE-600)417718-6</subfield><subfield code="w">(DE-576)015553892</subfield><subfield code="x">0031-0182</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:436</subfield><subfield code="g">year:2015</subfield><subfield code="g">pages:167-177</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">http://dx.doi.org/10.1016/j.palaeo.2015.06.047</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-FOR</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_21</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2027</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2173</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4029</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="936" ind1="r" ind2="v"><subfield code="a">TE 1000</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">436</subfield><subfield code="j">2015</subfield><subfield code="h">167-177</subfield></datafield></record></collection>
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