Oxygen depletion and sediment respiration in ice‐covered arctic lakes

Processes regulating the rate of oxygen depletion determine whether hypoxia occurs and the extent to which greenhouse gases accumulate in seasonally ice-covered lakes. Here, we investigate the oxygen budget of four arctic lakes using high-frequency data during two winters in three shallow lakes (9–1...

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Main Authors: Schwefel, Robert, MacIntyre, Sally, Cortés, Alicia, Sadro, Steven
Format: Article in Journal/Newspaper
Language:unknown
Published: eScholarship, University of California 2023
Subjects:
Online Access:https://escholarship.org/uc/item/8cf8x2wx
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spelling ftcdlib:oai:escholarship.org:ark:/13030/qt8cf8x2wx 2023-09-05T13:17:17+02:00 Oxygen depletion and sediment respiration in ice‐covered arctic lakes Schwefel, Robert MacIntyre, Sally Cortés, Alicia Sadro, Steven 1470 - 1489 2023-07-01 application/pdf https://escholarship.org/uc/item/8cf8x2wx unknown eScholarship, University of California qt8cf8x2wx https://escholarship.org/uc/item/8cf8x2wx CC-BY-ND Limnology and Oceanography, vol 68, iss 7 Earth Sciences Environmental Sciences Biological Sciences Marine Biology & Hydrobiology article 2023 ftcdlib 2023-08-14T18:05:21Z Processes regulating the rate of oxygen depletion determine whether hypoxia occurs and the extent to which greenhouse gases accumulate in seasonally ice-covered lakes. Here, we investigate the oxygen budget of four arctic lakes using high-frequency data during two winters in three shallow lakes (9–13 m maximal depth) and four winters in 24 m deep main basin of Toolik Lake. Incubation experiments measured sediment metabolism. Volume-averaged oxygen depletion measured in situ was independent of water temperature and duration of the ice-covered period. Average rates were between 0.2 and 0.39 g O2 m−2 d−1 in the shallow lakes and between 0.03 and 0.14 g O2 m−2 d−1 in Toolik Lake, with higher rates in smaller lakes with their larger sediment area to volume ratio. Rates decreased to ~ 20%–50% of initial values in late winter in the shallow lakes but less or not at all in Toolik. The lack of a decline in Toolik Lake points to continued oxygen transport to the sediment–water interface where oxygen consumption occurs. In all lakes, lower in situ oxygen depletion than in incubation measurements points toward increasing anoxia in the lower water column depressing loss rates. In Toolik, oxygen loss during early winter was less in years with minimal snow cover. Penetrative convection occurred, which could mix downwards oxygen produced by photosynthesis or excluded during ice formation. Estimates of these terms exceeded photosynthesis measured in sediment incubations. Modeling under ice-oxygen dynamics requires consideration of optical properties and biological and transport processes that modify oxygen concentrations and distributions. Article in Journal/Newspaper Arctic University of California: eScholarship Arctic
institution Open Polar
collection University of California: eScholarship
op_collection_id ftcdlib
language unknown
topic Earth Sciences
Environmental Sciences
Biological Sciences
Marine Biology & Hydrobiology
spellingShingle Earth Sciences
Environmental Sciences
Biological Sciences
Marine Biology & Hydrobiology
Schwefel, Robert
MacIntyre, Sally
Cortés, Alicia
Sadro, Steven
Oxygen depletion and sediment respiration in ice‐covered arctic lakes
topic_facet Earth Sciences
Environmental Sciences
Biological Sciences
Marine Biology & Hydrobiology
description Processes regulating the rate of oxygen depletion determine whether hypoxia occurs and the extent to which greenhouse gases accumulate in seasonally ice-covered lakes. Here, we investigate the oxygen budget of four arctic lakes using high-frequency data during two winters in three shallow lakes (9–13 m maximal depth) and four winters in 24 m deep main basin of Toolik Lake. Incubation experiments measured sediment metabolism. Volume-averaged oxygen depletion measured in situ was independent of water temperature and duration of the ice-covered period. Average rates were between 0.2 and 0.39 g O2 m−2 d−1 in the shallow lakes and between 0.03 and 0.14 g O2 m−2 d−1 in Toolik Lake, with higher rates in smaller lakes with their larger sediment area to volume ratio. Rates decreased to ~ 20%–50% of initial values in late winter in the shallow lakes but less or not at all in Toolik. The lack of a decline in Toolik Lake points to continued oxygen transport to the sediment–water interface where oxygen consumption occurs. In all lakes, lower in situ oxygen depletion than in incubation measurements points toward increasing anoxia in the lower water column depressing loss rates. In Toolik, oxygen loss during early winter was less in years with minimal snow cover. Penetrative convection occurred, which could mix downwards oxygen produced by photosynthesis or excluded during ice formation. Estimates of these terms exceeded photosynthesis measured in sediment incubations. Modeling under ice-oxygen dynamics requires consideration of optical properties and biological and transport processes that modify oxygen concentrations and distributions.
format Article in Journal/Newspaper
author Schwefel, Robert
MacIntyre, Sally
Cortés, Alicia
Sadro, Steven
author_facet Schwefel, Robert
MacIntyre, Sally
Cortés, Alicia
Sadro, Steven
author_sort Schwefel, Robert
title Oxygen depletion and sediment respiration in ice‐covered arctic lakes
title_short Oxygen depletion and sediment respiration in ice‐covered arctic lakes
title_full Oxygen depletion and sediment respiration in ice‐covered arctic lakes
title_fullStr Oxygen depletion and sediment respiration in ice‐covered arctic lakes
title_full_unstemmed Oxygen depletion and sediment respiration in ice‐covered arctic lakes
title_sort oxygen depletion and sediment respiration in ice‐covered arctic lakes
publisher eScholarship, University of California
publishDate 2023
url https://escholarship.org/uc/item/8cf8x2wx
op_coverage 1470 - 1489
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source Limnology and Oceanography, vol 68, iss 7
op_relation qt8cf8x2wx
https://escholarship.org/uc/item/8cf8x2wx
op_rights CC-BY-ND
_version_ 1776198518236512256