2021
DOI: 10.1016/j.scitotenv.2020.144201
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Biogeochemistry of macrophytes, sediments and porewaters in thermokarst lakes of permafrost peatlands, western Siberia

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Cited by 24 publications
(12 citation statements)
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“…Moreover, the β-diversity, especially the β-diversity of abundant subcommunities, also had a significant relationship between sediment and water (Figure 5). These connections between sediment and water might be the results of thermokarst lakes formation and evolution processes, during which, nutrients and other elements are continuously released to water from permafrost and sediment (Mackelprang et al, 2017; In’T Zandt et al, 2020; Manasypov et al, 2021).…”
Section: Discussionmentioning
confidence: 99%
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“…Moreover, the β-diversity, especially the β-diversity of abundant subcommunities, also had a significant relationship between sediment and water (Figure 5). These connections between sediment and water might be the results of thermokarst lakes formation and evolution processes, during which, nutrients and other elements are continuously released to water from permafrost and sediment (Mackelprang et al, 2017; In’T Zandt et al, 2020; Manasypov et al, 2021).…”
Section: Discussionmentioning
confidence: 99%
“…Permafrost is widespread in high latitude and high elevation regions, covering about one quarter of land surface in the Northern Hemisphere and experiencing severe warming than the remainder of the globe (Qiu and Cheng, 1995; Zhang et al, 1999). Thermokarst lakes are forming as a result of permafrost thaw, acting as an important and widespread aquatic ecosystems in cold regions (Kokelj and Jorgenson, 2013; Farquharson et al, 2016) with significant roles in hydrological, ecological, and biogeochemical processes (Chin et al, 2016; In’T Zandt et al, 2020; Manasypov et al, 2021). In Arctic and sub-Arctic area, thermokarst lakes cover up to 40% of the permafrost area (de Jong et al, 2018).…”
Section: Introductionmentioning
confidence: 99%
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“…Permafrost is widespread in high latitude and high elevation regions, covering approximately one-quarter of the land surface in the Northern Hemisphere and experiencing more severe warming than the remainder of the globe ( Qiu and Cheng, 1995 ; Zhang et al, 1999 ). Thermokarst lakes are forming as a result of permafrost thaw, acting as important and widespread aquatic ecosystems in cold regions ( Kokelj and Jorgenson, 2013 ; Farquharson et al, 2016 ) with significant roles in hydrological, ecological, and biogeochemical processes ( Chin et al, 2016 ; In’T Zandt et al, 2020 ; Manasypov et al, 2021 ). In the Arctic and sub-Arctic area, thermokarst lakes cover up to 40% of the permafrost area ( de Jong et al, 2018 ).…”
Section: Introductionmentioning
confidence: 99%
“…Thermokarst lakes, also known as thaw lakes, are formed as a result of thawing ice-rich permafrost, acting as a ubiquitous landscape feature in the cold region with ecological and biogeochemical importance (Kokelj and Jorgenson, 2013;Chin et al, 2016;In'T Zandt et al, 2020;Manasypov et al, 2021). Thermokarst lakes evolve through vertical and horizontal permafrost degradation with the lake areas ranging from a few square meters to hundreds of square kilometers (Grosse et al, 2013).…”
Section: Introductionmentioning
confidence: 99%