An overview of late Holocene climate and environmental change inferred from Arctic lake sediment
Abstract The 14 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene climate and environmental change from Arctic lakes, with emphasis on the last 2000 years. The study sites span the high latitudes of North America and extend into northwestern Europe. The stu...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Kaufman, Darrell S. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2008 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer Science+Business Media B.V. 2008 |
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| Übergeordnetes Werk: |
Enthalten in: Journal of paleolimnology - Springer Netherlands, 1988, 41(2008), 1 vom: 14. Okt., Seite 1-6 |
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| Übergeordnetes Werk: |
volume:41 ; year:2008 ; number:1 ; day:14 ; month:10 ; pages:1-6 |
| Links: |
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| DOI / URN: |
10.1007/s10933-008-9259-6 |
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OLC2071088808 |
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| 520 | |a Abstract The 14 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene climate and environmental change from Arctic lakes, with emphasis on the last 2000 years. The study sites span the high latitudes of North America and extend into northwestern Europe. The studies rely on multiple proxy indicators to reconstruct past climate, including: varve thicknesses, chironomid, diatom, and pollen assemblages, biogenic-silica and organic-matter content, oxygen-isotope ratios in diatoms, and the frequency of lake-ice-rafted aggregates. These proxies primarily document changes in past summer temperatures, the main control on physical and biological processes in lakes at high latitudes. The records will be integrated into a larger network of paleoclimate sites to investigate the spatial and temporal variability of climate change and to compare the paleoclimate inferences with the output of general circulation models. | ||
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10.1007/s10933-008-9259-6 doi (DE-627)OLC2071088808 (DE-He213)s10933-008-9259-6-p DE-627 ger DE-627 rakwb eng 570 930 VZ 14 13 12 ssgn Kaufman, Darrell S. verfasserin aut An overview of late Holocene climate and environmental change inferred from Arctic lake sediment 2008 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2008 Abstract The 14 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene climate and environmental change from Arctic lakes, with emphasis on the last 2000 years. The study sites span the high latitudes of North America and extend into northwestern Europe. The studies rely on multiple proxy indicators to reconstruct past climate, including: varve thicknesses, chironomid, diatom, and pollen assemblages, biogenic-silica and organic-matter content, oxygen-isotope ratios in diatoms, and the frequency of lake-ice-rafted aggregates. These proxies primarily document changes in past summer temperatures, the main control on physical and biological processes in lakes at high latitudes. The records will be integrated into a larger network of paleoclimate sites to investigate the spatial and temporal variability of climate change and to compare the paleoclimate inferences with the output of general circulation models. Holocene climate change Arctic lakes Proxy climate records Enthalten in Journal of paleolimnology Springer Netherlands, 1988 41(2008), 1 vom: 14. Okt., Seite 1-6 (DE-627)131173782 (DE-600)1140218-0 (DE-576)090827198 0921-2728 nnns volume:41 year:2008 number:1 day:14 month:10 pages:1-6 https://doi.org/10.1007/s10933-008-9259-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_40 GBV_ILN_154 GBV_ILN_2027 GBV_ILN_4012 AR 41 2008 1 14 10 1-6 |
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10.1007/s10933-008-9259-6 doi (DE-627)OLC2071088808 (DE-He213)s10933-008-9259-6-p DE-627 ger DE-627 rakwb eng 570 930 VZ 14 13 12 ssgn Kaufman, Darrell S. verfasserin aut An overview of late Holocene climate and environmental change inferred from Arctic lake sediment 2008 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2008 Abstract The 14 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene climate and environmental change from Arctic lakes, with emphasis on the last 2000 years. The study sites span the high latitudes of North America and extend into northwestern Europe. The studies rely on multiple proxy indicators to reconstruct past climate, including: varve thicknesses, chironomid, diatom, and pollen assemblages, biogenic-silica and organic-matter content, oxygen-isotope ratios in diatoms, and the frequency of lake-ice-rafted aggregates. These proxies primarily document changes in past summer temperatures, the main control on physical and biological processes in lakes at high latitudes. The records will be integrated into a larger network of paleoclimate sites to investigate the spatial and temporal variability of climate change and to compare the paleoclimate inferences with the output of general circulation models. Holocene climate change Arctic lakes Proxy climate records Enthalten in Journal of paleolimnology Springer Netherlands, 1988 41(2008), 1 vom: 14. Okt., Seite 1-6 (DE-627)131173782 (DE-600)1140218-0 (DE-576)090827198 0921-2728 nnns volume:41 year:2008 number:1 day:14 month:10 pages:1-6 https://doi.org/10.1007/s10933-008-9259-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_40 GBV_ILN_154 GBV_ILN_2027 GBV_ILN_4012 AR 41 2008 1 14 10 1-6 |
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An overview of late Holocene climate and environmental change inferred from Arctic lake sediment |
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Abstract The 14 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene climate and environmental change from Arctic lakes, with emphasis on the last 2000 years. The study sites span the high latitudes of North America and extend into northwestern Europe. The studies rely on multiple proxy indicators to reconstruct past climate, including: varve thicknesses, chironomid, diatom, and pollen assemblages, biogenic-silica and organic-matter content, oxygen-isotope ratios in diatoms, and the frequency of lake-ice-rafted aggregates. These proxies primarily document changes in past summer temperatures, the main control on physical and biological processes in lakes at high latitudes. The records will be integrated into a larger network of paleoclimate sites to investigate the spatial and temporal variability of climate change and to compare the paleoclimate inferences with the output of general circulation models. © Springer Science+Business Media B.V. 2008 |
| abstractGer |
Abstract The 14 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene climate and environmental change from Arctic lakes, with emphasis on the last 2000 years. The study sites span the high latitudes of North America and extend into northwestern Europe. The studies rely on multiple proxy indicators to reconstruct past climate, including: varve thicknesses, chironomid, diatom, and pollen assemblages, biogenic-silica and organic-matter content, oxygen-isotope ratios in diatoms, and the frequency of lake-ice-rafted aggregates. These proxies primarily document changes in past summer temperatures, the main control on physical and biological processes in lakes at high latitudes. The records will be integrated into a larger network of paleoclimate sites to investigate the spatial and temporal variability of climate change and to compare the paleoclimate inferences with the output of general circulation models. © Springer Science+Business Media B.V. 2008 |
| abstract_unstemmed |
Abstract The 14 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene climate and environmental change from Arctic lakes, with emphasis on the last 2000 years. The study sites span the high latitudes of North America and extend into northwestern Europe. The studies rely on multiple proxy indicators to reconstruct past climate, including: varve thicknesses, chironomid, diatom, and pollen assemblages, biogenic-silica and organic-matter content, oxygen-isotope ratios in diatoms, and the frequency of lake-ice-rafted aggregates. These proxies primarily document changes in past summer temperatures, the main control on physical and biological processes in lakes at high latitudes. The records will be integrated into a larger network of paleoclimate sites to investigate the spatial and temporal variability of climate change and to compare the paleoclimate inferences with the output of general circulation models. © Springer Science+Business Media B.V. 2008 |
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An overview of late Holocene climate and environmental change inferred from Arctic lake sediment |
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