Lake initiation and ecosystem change: A paleoenvironmental reconstruction from sedimentary records in Goldstream Valley, Alaska

Global warming has a direct impact on the degradation of permafrost and the resulting ground subsidence. Thermokarst lakes develop. During the formation of thermokarst lakes, the thawing of permafrost releases methane and carbon, which was locked in the frozen ground before. As a result, the generat...

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Main Author: Ertel, Sophie
Format: Thesis
Language:unknown
Published: 2019
Subjects:
Online Access:https://epic.awi.de/id/eprint/49094/
https://hdl.handle.net/10013/epic.ad5fe16a-8f7d-4112-88ea-b3aca3b0877a
id ftawi:oai:epic.awi.de:49094
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spelling ftawi:oai:epic.awi.de:49094 2024-09-15T18:29:53+00:00 Lake initiation and ecosystem change: A paleoenvironmental reconstruction from sedimentary records in Goldstream Valley, Alaska Ertel, Sophie 2019 https://epic.awi.de/id/eprint/49094/ https://hdl.handle.net/10013/epic.ad5fe16a-8f7d-4112-88ea-b3aca3b0877a unknown Ertel, S. (2019) Lake initiation and ecosystem change: A paleoenvironmental reconstruction from sedimentary records in Goldstream Valley, Alaska , Master thesis, University of Mainz. hdl:10013/epic.ad5fe16a-8f7d-4112-88ea-b3aca3b0877a EPIC381 p. Thesis notRev info:eu-repo/semantics/other 2019 ftawi 2024-06-24T04:21:00Z Global warming has a direct impact on the degradation of permafrost and the resulting ground subsidence. Thermokarst lakes develop. During the formation of thermokarst lakes, the thawing of permafrost releases methane and carbon, which was locked in the frozen ground before. As a result, the generation of thermokarst lakes is directly linked to climatic changes. The aim of this research is to reconstruct the initiation of lakes which are situated in the discontinuous permafrost of Goldstream Valley, Central Alaska. In course of an expedition in summer 2017, cores from eleven thermokarst lakes were taken from Goldstream Valley in Central Alaska. The samples were analysed for sedimentological and biochemical parameters. Additionally, macro remains were examined. There are three classes of thermokarst lakes within this research: Lakes which develop over a longer period of time and lakes which developed in less time. The third class includes lakes where the initiation phase was not caught within the selected transition zones, but it is assumed they also developed over a longer period of time and therefore belong to class one. A distinct peat layer is characteristic for lakes of class one. The analysed macro remains reflect the degree of degradation of the sediment except in one case. In case of biochemical analyses, the macro remains are only partly reflected. An implication of thermokarst lake development is a release of a high amount of methane and carbon dioxide while thermokarst lakes develop. So, the more time a lake needs to originate, the higher the emissions of methane and carbon dioxide are. Lakes that form within less time therefore emit less methane and carbon dioxide. Thesis permafrost Thermokarst Alaska 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 Global warming has a direct impact on the degradation of permafrost and the resulting ground subsidence. Thermokarst lakes develop. During the formation of thermokarst lakes, the thawing of permafrost releases methane and carbon, which was locked in the frozen ground before. As a result, the generation of thermokarst lakes is directly linked to climatic changes. The aim of this research is to reconstruct the initiation of lakes which are situated in the discontinuous permafrost of Goldstream Valley, Central Alaska. In course of an expedition in summer 2017, cores from eleven thermokarst lakes were taken from Goldstream Valley in Central Alaska. The samples were analysed for sedimentological and biochemical parameters. Additionally, macro remains were examined. There are three classes of thermokarst lakes within this research: Lakes which develop over a longer period of time and lakes which developed in less time. The third class includes lakes where the initiation phase was not caught within the selected transition zones, but it is assumed they also developed over a longer period of time and therefore belong to class one. A distinct peat layer is characteristic for lakes of class one. The analysed macro remains reflect the degree of degradation of the sediment except in one case. In case of biochemical analyses, the macro remains are only partly reflected. An implication of thermokarst lake development is a release of a high amount of methane and carbon dioxide while thermokarst lakes develop. So, the more time a lake needs to originate, the higher the emissions of methane and carbon dioxide are. Lakes that form within less time therefore emit less methane and carbon dioxide.
format Thesis
author Ertel, Sophie
spellingShingle Ertel, Sophie
Lake initiation and ecosystem change: A paleoenvironmental reconstruction from sedimentary records in Goldstream Valley, Alaska
author_facet Ertel, Sophie
author_sort Ertel, Sophie
title Lake initiation and ecosystem change: A paleoenvironmental reconstruction from sedimentary records in Goldstream Valley, Alaska
title_short Lake initiation and ecosystem change: A paleoenvironmental reconstruction from sedimentary records in Goldstream Valley, Alaska
title_full Lake initiation and ecosystem change: A paleoenvironmental reconstruction from sedimentary records in Goldstream Valley, Alaska
title_fullStr Lake initiation and ecosystem change: A paleoenvironmental reconstruction from sedimentary records in Goldstream Valley, Alaska
title_full_unstemmed Lake initiation and ecosystem change: A paleoenvironmental reconstruction from sedimentary records in Goldstream Valley, Alaska
title_sort lake initiation and ecosystem change: a paleoenvironmental reconstruction from sedimentary records in goldstream valley, alaska
publishDate 2019
url https://epic.awi.de/id/eprint/49094/
https://hdl.handle.net/10013/epic.ad5fe16a-8f7d-4112-88ea-b3aca3b0877a
genre permafrost
Thermokarst
Alaska
genre_facet permafrost
Thermokarst
Alaska
op_source EPIC381 p.
op_relation Ertel, S. (2019) Lake initiation and ecosystem change: A paleoenvironmental reconstruction from sedimentary records in Goldstream Valley, Alaska , Master thesis, University of Mainz. hdl:10013/epic.ad5fe16a-8f7d-4112-88ea-b3aca3b0877a
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