Microbial Nutrient Limitation in Arctic Lakes in a Permafrost Landscape of Southwest Greenland
Permafrost is degrading across regions of the Arctic, which can lead to increases in nutrient concentrations in surface freshwaters. The oligotrophic state of many arctic lakes suggests that enhanced nutrient inputs may have important effects on these systems, but little is known about microbial nut...
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ftmaineuniv:oai:digitalcommons.library.umaine.edu:etd-3423 2023-06-11T04:08:54+02:00 Microbial Nutrient Limitation in Arctic Lakes in a Permafrost Landscape of Southwest Greenland Burpee, Benjamin Todd 2015-08-01T07:00:00Z application/pdf https://digitalcommons.library.umaine.edu/etd/2374 https://digitalcommons.library.umaine.edu/context/etd/article/3423/viewcontent/BurpeeBT2015_OCR.pdf unknown DigitalCommons@UMaine https://digitalcommons.library.umaine.edu/etd/2374 https://digitalcommons.library.umaine.edu/context/etd/article/3423/viewcontent/BurpeeBT2015_OCR.pdf Electronic Theses and Dissertations Freshwater ecology Bacteria Permafrost Greenland Fresh Water Studies text 2015 ftmaineuniv 2023-05-04T18:02:23Z Permafrost is degrading across regions of the Arctic, which can lead to increases in nutrient concentrations in surface freshwaters. The oligotrophic state of many arctic lakes suggests that enhanced nutrient inputs may have important effects on these systems, but little is known about microbial nutrient limitation patterns in these lakes. I investigated microbial extracellular enzyme activities (EEAs) to infer seasonal nutrient dynamics and limitation across 24 lakes in southwest Greenland during summer (June and July). From early to late summer, enzyme activities that indicate microbial carbon (C), nitrogen (N), and phosphorus (P) demand increased in both the epilimnia and hypolimnia by 74% on average. Microbial investment in P acquisition was generally higher than that for N. Interactions among EEAs indicated that bacteria were primarily P limited. Dissolved organic matter (DOM, measured as dissolved organic carbon) was strongly and positively correlated with microbial P demand (R2 = 0.84 in July), while there were no relationships between DOM and microbial N demand. Microbial P limitation in June epilimnia (R2 = 0.67) and July hypolimnia (R2 = 0.57) increased with DOM concentration. The consistency of microbial P limitation from June to July was related to the amount of DOM present, with some low DOM lakes becoming N-limited in July. The results suggest that future changes in P or DOM inputs to these lakes are likely to alter microbial nutrient limitation patterns. Text Arctic Greenland permafrost The University of Maine: DigitalCommons@UMaine Arctic Greenland |
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The University of Maine: DigitalCommons@UMaine |
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Freshwater ecology Bacteria Permafrost Greenland Fresh Water Studies |
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Freshwater ecology Bacteria Permafrost Greenland Fresh Water Studies Burpee, Benjamin Todd Microbial Nutrient Limitation in Arctic Lakes in a Permafrost Landscape of Southwest Greenland |
topic_facet |
Freshwater ecology Bacteria Permafrost Greenland Fresh Water Studies |
description |
Permafrost is degrading across regions of the Arctic, which can lead to increases in nutrient concentrations in surface freshwaters. The oligotrophic state of many arctic lakes suggests that enhanced nutrient inputs may have important effects on these systems, but little is known about microbial nutrient limitation patterns in these lakes. I investigated microbial extracellular enzyme activities (EEAs) to infer seasonal nutrient dynamics and limitation across 24 lakes in southwest Greenland during summer (June and July). From early to late summer, enzyme activities that indicate microbial carbon (C), nitrogen (N), and phosphorus (P) demand increased in both the epilimnia and hypolimnia by 74% on average. Microbial investment in P acquisition was generally higher than that for N. Interactions among EEAs indicated that bacteria were primarily P limited. Dissolved organic matter (DOM, measured as dissolved organic carbon) was strongly and positively correlated with microbial P demand (R2 = 0.84 in July), while there were no relationships between DOM and microbial N demand. Microbial P limitation in June epilimnia (R2 = 0.67) and July hypolimnia (R2 = 0.57) increased with DOM concentration. The consistency of microbial P limitation from June to July was related to the amount of DOM present, with some low DOM lakes becoming N-limited in July. The results suggest that future changes in P or DOM inputs to these lakes are likely to alter microbial nutrient limitation patterns. |
format |
Text |
author |
Burpee, Benjamin Todd |
author_facet |
Burpee, Benjamin Todd |
author_sort |
Burpee, Benjamin Todd |
title |
Microbial Nutrient Limitation in Arctic Lakes in a Permafrost Landscape of Southwest Greenland |
title_short |
Microbial Nutrient Limitation in Arctic Lakes in a Permafrost Landscape of Southwest Greenland |
title_full |
Microbial Nutrient Limitation in Arctic Lakes in a Permafrost Landscape of Southwest Greenland |
title_fullStr |
Microbial Nutrient Limitation in Arctic Lakes in a Permafrost Landscape of Southwest Greenland |
title_full_unstemmed |
Microbial Nutrient Limitation in Arctic Lakes in a Permafrost Landscape of Southwest Greenland |
title_sort |
microbial nutrient limitation in arctic lakes in a permafrost landscape of southwest greenland |
publisher |
DigitalCommons@UMaine |
publishDate |
2015 |
url |
https://digitalcommons.library.umaine.edu/etd/2374 https://digitalcommons.library.umaine.edu/context/etd/article/3423/viewcontent/BurpeeBT2015_OCR.pdf |
geographic |
Arctic Greenland |
geographic_facet |
Arctic Greenland |
genre |
Arctic Greenland permafrost |
genre_facet |
Arctic Greenland permafrost |
op_source |
Electronic Theses and Dissertations |
op_relation |
https://digitalcommons.library.umaine.edu/etd/2374 https://digitalcommons.library.umaine.edu/context/etd/article/3423/viewcontent/BurpeeBT2015_OCR.pdf |
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1768382526567481344 |