Paleolimnological reconstructions of Holocene Environments and Climate from Lake Lyadhej-To, Ural Mountains, Northern Russia
A sediment core recovered in Lake Lyadhej-To at the northwestern edge of the Ural Mountains reflects the complete Holocene environmental history from ~11,000 cal. yrs BP. Five limnological episodes are identified in the diatom and geochemical records. The initial lake stage, Episode I (~11,000-10,85...
Main Authors: | , , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
2004
|
Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/5993/ https://epic.awi.de/id/eprint/5993/1/Cre2002a.pdf https://hdl.handle.net/10013/epic.16547 https://hdl.handle.net/10013/epic.16547.d001 |
id |
ftawi:oai:epic.awi.de:5993 |
---|---|
record_format |
openpolar |
spelling |
ftawi:oai:epic.awi.de:5993 2023-09-05T13:15:27+02:00 Paleolimnological reconstructions of Holocene Environments and Climate from Lake Lyadhej-To, Ural Mountains, Northern Russia Cremer, H. Andreev, Andrei Hubberten, Hans-Wolfgang Wischer, Frank 2004 application/pdf https://epic.awi.de/id/eprint/5993/ https://epic.awi.de/id/eprint/5993/1/Cre2002a.pdf https://hdl.handle.net/10013/epic.16547 https://hdl.handle.net/10013/epic.16547.d001 unknown https://epic.awi.de/id/eprint/5993/1/Cre2002a.pdf https://hdl.handle.net/10013/epic.16547.d001 Cremer, H. , Andreev, A. orcid:0000-0002-8745-9636 , Hubberten, H. W. and Wischer, F. (2004) Paleolimnological reconstructions of Holocene Environments and Climate from Lake Lyadhej-To, Ural Mountains, Northern Russia , Arctic, antarctic and alpine research, 36 (2), pp. 147-155 . hdl:10013/epic.16547 EPIC3Arctic, antarctic and alpine research, 36(2), pp. 147-155, ISSN: 1523-0430 Article isiRev 2004 ftawi 2023-08-22T19:45:49Z A sediment core recovered in Lake Lyadhej-To at the northwestern edge of the Ural Mountains reflects the complete Holocene environmental history from ~11,000 cal. yrs BP. Five limnological episodes are identified in the diatom and geochemical records. The initial lake stage, Episode I (~11,000-10,850 cal. yrs BP), was characterized by the absence of biogenic production and a high influx of clastic sediments. Episode II (~10,850-8650 cal. yrs BP) is characterized by ice-free conditions during summer, highest bioproductivity, strong growth of planktic diatoms and anoxic bottom waters. This period represents the Holocene climatic optimum. Deterioration of climatic conditions commenced in Episode III (~8650-7000 cal. yrs BP) as indicated by distinctly lower bioproductivity and longer persistence of winter ice on the lake. During Episode IV (~7000-2500 cal. yrs BP) the diatom and pollen records indicate that temperatures were cool and the growing season was short. Finally, in Episode V (~2500 cal. yrs BP to present) limnological conditions, indicated by increased organic carbon and diatom deposition, initially suggest improved conditions followed by a return to modern conditions beginning ~500 cal. yrs BP. The pollen stratigraphy from Lake Lyadhej-To is consistent with other paleoclimatic records from northern Eurasia, confirming rapid postglacial warming, the presence of dense tree forests during the climatic optimum and finally a gradual southward retreat of the treeline towards its modern location. Article in Journal/Newspaper Antarctic and Alpine Research Arctic ural mountains Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
institution |
Open Polar |
collection |
Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
op_collection_id |
ftawi |
language |
unknown |
description |
A sediment core recovered in Lake Lyadhej-To at the northwestern edge of the Ural Mountains reflects the complete Holocene environmental history from ~11,000 cal. yrs BP. Five limnological episodes are identified in the diatom and geochemical records. The initial lake stage, Episode I (~11,000-10,850 cal. yrs BP), was characterized by the absence of biogenic production and a high influx of clastic sediments. Episode II (~10,850-8650 cal. yrs BP) is characterized by ice-free conditions during summer, highest bioproductivity, strong growth of planktic diatoms and anoxic bottom waters. This period represents the Holocene climatic optimum. Deterioration of climatic conditions commenced in Episode III (~8650-7000 cal. yrs BP) as indicated by distinctly lower bioproductivity and longer persistence of winter ice on the lake. During Episode IV (~7000-2500 cal. yrs BP) the diatom and pollen records indicate that temperatures were cool and the growing season was short. Finally, in Episode V (~2500 cal. yrs BP to present) limnological conditions, indicated by increased organic carbon and diatom deposition, initially suggest improved conditions followed by a return to modern conditions beginning ~500 cal. yrs BP. The pollen stratigraphy from Lake Lyadhej-To is consistent with other paleoclimatic records from northern Eurasia, confirming rapid postglacial warming, the presence of dense tree forests during the climatic optimum and finally a gradual southward retreat of the treeline towards its modern location. |
format |
Article in Journal/Newspaper |
author |
Cremer, H. Andreev, Andrei Hubberten, Hans-Wolfgang Wischer, Frank |
spellingShingle |
Cremer, H. Andreev, Andrei Hubberten, Hans-Wolfgang Wischer, Frank Paleolimnological reconstructions of Holocene Environments and Climate from Lake Lyadhej-To, Ural Mountains, Northern Russia |
author_facet |
Cremer, H. Andreev, Andrei Hubberten, Hans-Wolfgang Wischer, Frank |
author_sort |
Cremer, H. |
title |
Paleolimnological reconstructions of Holocene Environments and Climate from Lake Lyadhej-To, Ural Mountains, Northern Russia |
title_short |
Paleolimnological reconstructions of Holocene Environments and Climate from Lake Lyadhej-To, Ural Mountains, Northern Russia |
title_full |
Paleolimnological reconstructions of Holocene Environments and Climate from Lake Lyadhej-To, Ural Mountains, Northern Russia |
title_fullStr |
Paleolimnological reconstructions of Holocene Environments and Climate from Lake Lyadhej-To, Ural Mountains, Northern Russia |
title_full_unstemmed |
Paleolimnological reconstructions of Holocene Environments and Climate from Lake Lyadhej-To, Ural Mountains, Northern Russia |
title_sort |
paleolimnological reconstructions of holocene environments and climate from lake lyadhej-to, ural mountains, northern russia |
publishDate |
2004 |
url |
https://epic.awi.de/id/eprint/5993/ https://epic.awi.de/id/eprint/5993/1/Cre2002a.pdf https://hdl.handle.net/10013/epic.16547 https://hdl.handle.net/10013/epic.16547.d001 |
genre |
Antarctic and Alpine Research Arctic ural mountains |
genre_facet |
Antarctic and Alpine Research Arctic ural mountains |
op_source |
EPIC3Arctic, antarctic and alpine research, 36(2), pp. 147-155, ISSN: 1523-0430 |
op_relation |
https://epic.awi.de/id/eprint/5993/1/Cre2002a.pdf https://hdl.handle.net/10013/epic.16547.d001 Cremer, H. , Andreev, A. orcid:0000-0002-8745-9636 , Hubberten, H. W. and Wischer, F. (2004) Paleolimnological reconstructions of Holocene Environments and Climate from Lake Lyadhej-To, Ural Mountains, Northern Russia , Arctic, antarctic and alpine research, 36 (2), pp. 147-155 . hdl:10013/epic.16547 |
_version_ |
1776197258878910464 |