Changing dynamics of Alaskan peatlands in the continuous permafrost zone

Peatlands in the continuous permafrost region store globally important amounts of organic carbon, but the stability of this store is threatened by climate warming. Reconstructions from peatlands using sensitive indicators of environmental change, such as testate amoebae, offer insight into the way t...

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Main Author: Taylor, Liam
Format: Thesis
Language:English
Published: University of Leeds 2018
Subjects:
Online Access:https://etheses.whiterose.ac.uk/22398/
https://etheses.whiterose.ac.uk/22398/1/Taylor_LS_Geography_MSc_2018.pdf
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spelling ftwhiterose:oai:etheses.whiterose.ac.uk:22398 2023-05-15T17:57:12+02:00 Changing dynamics of Alaskan peatlands in the continuous permafrost zone Taylor, Liam 2018-09 text https://etheses.whiterose.ac.uk/22398/ https://etheses.whiterose.ac.uk/22398/1/Taylor_LS_Geography_MSc_2018.pdf en eng University of Leeds https://etheses.whiterose.ac.uk/22398/1/Taylor_LS_Geography_MSc_2018.pdf Taylor, Liam (2018) Changing dynamics of Alaskan peatlands in the continuous permafrost zone. MSc by research thesis, University of Leeds. cc_by_nc_sa CC-BY-NC-SA Thesis NonPeerReviewed 2018 ftwhiterose 2023-01-30T21:25:57Z Peatlands in the continuous permafrost region store globally important amounts of organic carbon, but the stability of this store is threatened by climate warming. Reconstructions from peatlands using sensitive indicators of environmental change, such as testate amoebae, offer insight into the way these ecosystems have responded to past climate changes throughout the late-Holocene. This thesis aims to use palaeoenvironmental reconstructions from two peatlands in the Alaskan North Slope, adjacent to Toolik Lake, to understand their recent past and predict future dynamics to projected warming. To do so, the ecology of testate amoebae from peatlands across the Alaskan North Slope was explored to identify the controlling variables in their distribution. Multivariate statistical analysis shows that pore water electrical conductivity (EC), a proxy for peatland trophic status, was the primary control on testate amoeba distribution, with water table depth (WTD) the secondary control. Two transfer functions were produced to reconstruct EC and WTD with good predictive power. Reconstructions identified that both peatlands at Toolik Lake were mostly moderately-wet, minerotrophic rich fens throughout the late-Holocene, but have undergone a rapid transition to dry, oligotrophic poor fens with post-1850 CE warming. Alongside this ecosystem state shift, there has also been a three-fold increase in carbon accumulation rate post-1850 CE. Overall, this thesis extends the utility of testate amoebae as hydrological indicators into continuous permafrost peatlands; and suggests that rapid ecosystem state shifts may have occurred with recent climatic warming, which may indicate increased rates of carbon sequestration in the future. Thesis permafrost White Rose eTheses Online (Universities Leeds, Sheffield, York)
institution Open Polar
collection White Rose eTheses Online (Universities Leeds, Sheffield, York)
op_collection_id ftwhiterose
language English
description Peatlands in the continuous permafrost region store globally important amounts of organic carbon, but the stability of this store is threatened by climate warming. Reconstructions from peatlands using sensitive indicators of environmental change, such as testate amoebae, offer insight into the way these ecosystems have responded to past climate changes throughout the late-Holocene. This thesis aims to use palaeoenvironmental reconstructions from two peatlands in the Alaskan North Slope, adjacent to Toolik Lake, to understand their recent past and predict future dynamics to projected warming. To do so, the ecology of testate amoebae from peatlands across the Alaskan North Slope was explored to identify the controlling variables in their distribution. Multivariate statistical analysis shows that pore water electrical conductivity (EC), a proxy for peatland trophic status, was the primary control on testate amoeba distribution, with water table depth (WTD) the secondary control. Two transfer functions were produced to reconstruct EC and WTD with good predictive power. Reconstructions identified that both peatlands at Toolik Lake were mostly moderately-wet, minerotrophic rich fens throughout the late-Holocene, but have undergone a rapid transition to dry, oligotrophic poor fens with post-1850 CE warming. Alongside this ecosystem state shift, there has also been a three-fold increase in carbon accumulation rate post-1850 CE. Overall, this thesis extends the utility of testate amoebae as hydrological indicators into continuous permafrost peatlands; and suggests that rapid ecosystem state shifts may have occurred with recent climatic warming, which may indicate increased rates of carbon sequestration in the future.
format Thesis
author Taylor, Liam
spellingShingle Taylor, Liam
Changing dynamics of Alaskan peatlands in the continuous permafrost zone
author_facet Taylor, Liam
author_sort Taylor, Liam
title Changing dynamics of Alaskan peatlands in the continuous permafrost zone
title_short Changing dynamics of Alaskan peatlands in the continuous permafrost zone
title_full Changing dynamics of Alaskan peatlands in the continuous permafrost zone
title_fullStr Changing dynamics of Alaskan peatlands in the continuous permafrost zone
title_full_unstemmed Changing dynamics of Alaskan peatlands in the continuous permafrost zone
title_sort changing dynamics of alaskan peatlands in the continuous permafrost zone
publisher University of Leeds
publishDate 2018
url https://etheses.whiterose.ac.uk/22398/
https://etheses.whiterose.ac.uk/22398/1/Taylor_LS_Geography_MSc_2018.pdf
genre permafrost
genre_facet permafrost
op_relation https://etheses.whiterose.ac.uk/22398/1/Taylor_LS_Geography_MSc_2018.pdf
Taylor, Liam (2018) Changing dynamics of Alaskan peatlands in the continuous permafrost zone. MSc by research thesis, University of Leeds.
op_rights cc_by_nc_sa
op_rightsnorm CC-BY-NC-SA
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