Christine Siegert
Datos Biográficos
| ID | 5776811 |
|---|---|
| NOMBRE | Christine Siegert |
| NOMBRES | Christine |
| APELLIDO | Siegert |
| FIRMA | SIEGERT C |
| AFILIACIONES | Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung |
| VERIFICADO | No |
| TOTAL DE OBRAS | 12 |
| TOTAL DE CITAS | 0 |
| TOTAL COMO AUTOR | 12 |
| TOTAL COMO EDITOR | 0 |
| PRIMER AÑO DE PUBLICACIÓN | 1996 |
| AÑO MÁS RECIENTE DE PUBLICACIÓN | 2017 |
| ÍNDICE H | 0 |
Rapid thermokarst evolution during the mid-Holocene in Central Yakutia, Russia
The reconstruction of Holocene thermokarst landform evolution is important to understand the potential impact of current global climate change on permafrost regions. A multi-proxy approach was applied to analyse the sedimentological and biogeochemical characteristics as well as pollen and lacustrine microfossils of a core profile drilled in a small pingo within a large Central Yakutian thermokarst basin (alas). Age–depth modelling with macrofossi…
Carl Maria von Weber
Musikwissenschaft digital
Sedimentary characteristics and origin of the Late Pleistocene Ice Complex on north-east Siberian Arctic coastal lowlands and islands – A review
Ludwig Van Beethoven
Bernhard Wartischlager
Palaeobotanical evidence for warm summers in the East Siberian Arctic during the last cold stage
Plant macrofossils from the “Mamontovy Khayata” permafrost sequence (71°60′N, 129°25′E) on the Bykovsky Peninsula reflect climate and plant biodiversity in west Beringia during the last cold stage. 70 AMS and 20 conventional 14 C dates suggest sediment accumulation between about 60,000 and 7500 14 C yr B.P. The plant remains prove that during the last cold-stage arctic species ( Minuartia arctica , Draba spp., Kobresia myosuroides ) coexisted wit…
Late Quaternary ice sheet history of northern Eurasia
Oper in der Toskana in der zweiten Hälfte des 18. Jahrhunderts
Late Pleistocene and Holocene Vegetation and Climate on the Taymyr Lowland, Northern Siberia
Pollen records from perennially frozen sequences provide vegetation and climate reconstruction for the last 48,000 14 C years in the central part of Taymyr Peninsula. Open larch forest with Alnus fruticosa and Betula nana grew during the Kargin (Middle Weichselian) Interstade, ca. 48,000–25,000 14 C yr B.P. The climate was generally warmer and wetter than today. Open steppe-like communities with Artemisia , Poaceae, Asteraceae, and herb tundralik…
Paleoenvironmental and paleoclimatic records from permafrost deposits in the Arctic region of Northern Siberia
Effect of Permafrost and Palaeo-Environmental History on Soil Formation in the lower Kolyma Lowland, Siberia
Danish Journal of Geography 96: 40–50, 1996. The Geography of soils has been studied in the tundra of the sandy Kolyma Lowland between latitudes 69 ° and 70 ° N. Generally, soils show characteristics indicative of variable intensity of previous fossil Podzol formation in the present day cryoturbated active layer. Hence, the transformation, transfer and segregation of chemical substances in the soil profile can be interpreted as evidence of palaeo…
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Effect of Permafrost and Palaeo-Environmental History on Soil Formation in the lower Kolyma Lowland, Siberia
Danish Journal of Geography 96: 40–50, 1996. The Geography of soils has been studied in the tundra of the sandy Kolyma Lowland between latitudes 69 ° and 70 ° N. Generally, soils show characteristics indicative of variable intensity of previous fossil Podzol formation in the present day cryoturbated active layer. Hence, the transformation, transfer and segregation of chemical substances in the soil profile can be interpreted as evidence of palaeo…
Late Pleistocene and Holocene Vegetation and Climate on the Taymyr Lowland, Northern Siberia
Pollen records from perennially frozen sequences provide vegetation and climate reconstruction for the last 48,000 14 C years in the central part of Taymyr Peninsula. Open larch forest with Alnus fruticosa and Betula nana grew during the Kargin (Middle Weichselian) Interstade, ca. 48,000–25,000 14 C yr B.P. The climate was generally warmer and wetter than today. Open steppe-like communities with Artemisia , Poaceae, Asteraceae, and herb tundralik…
Paleoenvironmental and paleoclimatic records from permafrost deposits in the Arctic region of Northern Siberia
Late Quaternary ice sheet history of northern Eurasia
Oper in der Toskana in der zweiten Hälfte des 18. Jahrhunderts
Palaeobotanical evidence for warm summers in the East Siberian Arctic during the last cold stage
Plant macrofossils from the “Mamontovy Khayata” permafrost sequence (71°60′N, 129°25′E) on the Bykovsky Peninsula reflect climate and plant biodiversity in west Beringia during the last cold stage. 70 AMS and 20 conventional 14 C dates suggest sediment accumulation between about 60,000 and 7500 14 C yr B.P. The plant remains prove that during the last cold-stage arctic species ( Minuartia arctica , Draba spp., Kobresia myosuroides ) coexisted wit…
Bernhard Wartischlager
Ludwig Van Beethoven
Musikwissenschaft digital
Sedimentary characteristics and origin of the Late Pleistocene Ice Complex on north-east Siberian Arctic coastal lowlands and islands – A review
Carl Maria von Weber
Rapid thermokarst evolution during the mid-Holocene in Central Yakutia, Russia
The reconstruction of Holocene thermokarst landform evolution is important to understand the potential impact of current global climate change on permafrost regions. A multi-proxy approach was applied to analyse the sedimentological and biogeochemical characteristics as well as pollen and lacustrine microfossils of a core profile drilled in a small pingo within a large Central Yakutian thermokarst basin (alas). Age–depth modelling with macrofossi…
Climate change and permafrost (6 obras) · Geology and Paleoclimatology Research (6 obras) · Arctic (5 obras) · Geography (5 obras) · Physical geography (5 obras) · Art (4 obras) · Geology (4 obras) · Geology (4 obras) · Holocene (4 obras) · Musicology and Musical Analysis (4 obras)