Investigations on sediment profile PG1111 from Taymyr Peninsula, Siberia ...
In order to evaluate the sensitivity of aquatic and terrestrial ecosystems to climatic changes, lithological (sediment structure and color, grain size, physical properties) and biochemical (TOC, TOC/TN, d13C of TOC and carbonates) investigations were carried out on an 11.12 m-long sediment core from...
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ftdatacite:10.1594/pangaea.727577 2024-09-15T18:11:41+00:00 Investigations on sediment profile PG1111 from Taymyr Peninsula, Siberia ... Harwart, Stefanie K Hagedorn, Birgit Melles, Martin Wand, Ulrich 1999 application/zip https://dx.doi.org/10.1594/pangaea.727577 https://doi.pangaea.de/10.1594/PANGAEA.727577 en eng PANGAEA https://dx.doi.org/10.1111/j.1502-3885.1999.tb00212.x Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Composite Core RU-Land_1993_Norilsk_Taymyr AWI Arctic Land Expedition Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn Quaternary Environment of the Eurasian North QUEEN article Collection Supplementary Publication Series of Datasets 1999 ftdatacite https://doi.org/10.1594/pangaea.72757710.1111/j.1502-3885.1999.tb00212.x 2024-08-01T10:58:30Z In order to evaluate the sensitivity of aquatic and terrestrial ecosystems to climatic changes, lithological (sediment structure and color, grain size, physical properties) and biochemical (TOC, TOC/TN, d13C of TOC and carbonates) investigations were carried out on an 11.12 m-long sediment core from Lama Lake (Central Siberia, Putorana Plateau). According to the pollen data, the sequence represents the termination of the Pleistocene, and the entire Holocene. It is composed of highly terrigenous and stratified clays and silts. Sediment structure, grain-size distribution, carbonate contents and physical properties of the sediment indicate that glaciers were present in the catchment area of Lama Lake during the period Oldest Dryas to Allerød. For the same time period, d13C values of TOC give indications of a perennial ice cover. Since the Allerød, organic matter accumulation has increased, caused by an increasing input of land vegetation and aquatic primary production as revealed by relations TOC contents, ... : Supplement to: Harwart, Stefanie K; Hagedorn, Birgit; Melles, Martin; Wand, Ulrich (1999): Lithological and biochemical properties in sediments of Lama Lake as indicators for the late Pleistocene and Holocene ecosystem development of the southern Taymyr Peninsula, Central Siberia. Boreas, 28(1), 167-180 ... Article in Journal/Newspaper Ice permafrost Taymyr Taymyr Peninsula Siberia DataCite |
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Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Composite Core RU-Land_1993_Norilsk_Taymyr AWI Arctic Land Expedition Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn Quaternary Environment of the Eurasian North QUEEN |
spellingShingle |
Composite Core RU-Land_1993_Norilsk_Taymyr AWI Arctic Land Expedition Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn Quaternary Environment of the Eurasian North QUEEN Harwart, Stefanie K Hagedorn, Birgit Melles, Martin Wand, Ulrich Investigations on sediment profile PG1111 from Taymyr Peninsula, Siberia ... |
topic_facet |
Composite Core RU-Land_1993_Norilsk_Taymyr AWI Arctic Land Expedition Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn Quaternary Environment of the Eurasian North QUEEN |
description |
In order to evaluate the sensitivity of aquatic and terrestrial ecosystems to climatic changes, lithological (sediment structure and color, grain size, physical properties) and biochemical (TOC, TOC/TN, d13C of TOC and carbonates) investigations were carried out on an 11.12 m-long sediment core from Lama Lake (Central Siberia, Putorana Plateau). According to the pollen data, the sequence represents the termination of the Pleistocene, and the entire Holocene. It is composed of highly terrigenous and stratified clays and silts. Sediment structure, grain-size distribution, carbonate contents and physical properties of the sediment indicate that glaciers were present in the catchment area of Lama Lake during the period Oldest Dryas to Allerød. For the same time period, d13C values of TOC give indications of a perennial ice cover. Since the Allerød, organic matter accumulation has increased, caused by an increasing input of land vegetation and aquatic primary production as revealed by relations TOC contents, ... : Supplement to: Harwart, Stefanie K; Hagedorn, Birgit; Melles, Martin; Wand, Ulrich (1999): Lithological and biochemical properties in sediments of Lama Lake as indicators for the late Pleistocene and Holocene ecosystem development of the southern Taymyr Peninsula, Central Siberia. Boreas, 28(1), 167-180 ... |
format |
Article in Journal/Newspaper |
author |
Harwart, Stefanie K Hagedorn, Birgit Melles, Martin Wand, Ulrich |
author_facet |
Harwart, Stefanie K Hagedorn, Birgit Melles, Martin Wand, Ulrich |
author_sort |
Harwart, Stefanie K |
title |
Investigations on sediment profile PG1111 from Taymyr Peninsula, Siberia ... |
title_short |
Investigations on sediment profile PG1111 from Taymyr Peninsula, Siberia ... |
title_full |
Investigations on sediment profile PG1111 from Taymyr Peninsula, Siberia ... |
title_fullStr |
Investigations on sediment profile PG1111 from Taymyr Peninsula, Siberia ... |
title_full_unstemmed |
Investigations on sediment profile PG1111 from Taymyr Peninsula, Siberia ... |
title_sort |
investigations on sediment profile pg1111 from taymyr peninsula, siberia ... |
publisher |
PANGAEA |
publishDate |
1999 |
url |
https://dx.doi.org/10.1594/pangaea.727577 https://doi.pangaea.de/10.1594/PANGAEA.727577 |
genre |
Ice permafrost Taymyr Taymyr Peninsula Siberia |
genre_facet |
Ice permafrost Taymyr Taymyr Peninsula Siberia |
op_relation |
https://dx.doi.org/10.1111/j.1502-3885.1999.tb00212.x |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.72757710.1111/j.1502-3885.1999.tb00212.x |
_version_ |
1810449261638189056 |