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Influence of nutrient enrichment on temporal and spatial dynamics of dissolved oxygen within northern temperate estuaries

In temperate estuaries of the southern Gulf of St. Lawrence, intermittent seasonal anoxia coupled with phytoplankton blooms is a regular occurrence in watersheds dominated by agricultural land use. To examine the spatial relationship between dissolved oxygen and phytoplankton throughout the estuary...

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Autores principales: Coffin, MRS, Knysh, KM, Roloson, SD, Pater, CC, Theriaul, E, Cormier, JM, Courtenay, SC, van den Heuvel, MR
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer International Publishing 2021
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8593059/
https://www.ncbi.nlm.nih.gov/pubmed/34779929
http://dx.doi.org/10.1007/s10661-021-09589-8
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author Coffin, MRS
Knysh, KM
Roloson, SD
Pater, CC
Theriaul, E
Cormier, JM
Courtenay, SC
van den Heuvel, MR
author_facet Coffin, MRS
Knysh, KM
Roloson, SD
Pater, CC
Theriaul, E
Cormier, JM
Courtenay, SC
van den Heuvel, MR
author_sort Coffin, MRS
collection PubMed
description In temperate estuaries of the southern Gulf of St. Lawrence, intermittent seasonal anoxia coupled with phytoplankton blooms is a regular occurrence in watersheds dominated by agricultural land use. To examine the spatial relationship between dissolved oxygen and phytoplankton throughout the estuary to assist in designing monitoring programs, oxygen depth profiles and chlorophyll measurements were taken bi-weekly from May to December in 18 estuaries. In five of those estuaries, dissolved oxygen data loggers were set to measure oxygen at hourly intervals and at multiple locations within the estuary the subsequent year. The primary hypothesis was that dissolved oxygen in the upper estuary (first 10% of estuary area) is predictive of dissolved oxygen mid-estuary (50% of estuary area). The second hypothesis was that hypoxia/superoxia in the estuary is influenced by temperature and tidal flushing. Oxygen depth profiles conducted in the first year of study provided preliminary support that dissolved oxygen in the upper estuary was related to dissolved oxygen throughout the estuary. However, dissolved oxygen from loggers deployed at 10% and 50% of estuary area did not show as strong a correlation as expected (less than half the variance explained). The strength of the correlation declined towards the end of summer. Spatial decoupling of oxygen within the estuary suggested influence of local conditions. Chlorophyll concentration seemed also to be dependent on local conditions as it appeared to be coupled with the presence of sustained anoxia in the upper estuary with blooms typically occurring within 7 to 14 days of anoxia. The practical implication for oxygen monitoring is that one location within the most severely impacted part of the estuary is not sufficient to fully evaluate the severity of eutrophication effects. SUPPLEMENTARY INFORMATION: The online version contains supplementary material available at 10.1007/s10661-021-09589-8.
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spelling pubmed-85930592021-11-19 Influence of nutrient enrichment on temporal and spatial dynamics of dissolved oxygen within northern temperate estuaries Coffin, MRS Knysh, KM Roloson, SD Pater, CC Theriaul, E Cormier, JM Courtenay, SC van den Heuvel, MR Environ Monit Assess Article In temperate estuaries of the southern Gulf of St. Lawrence, intermittent seasonal anoxia coupled with phytoplankton blooms is a regular occurrence in watersheds dominated by agricultural land use. To examine the spatial relationship between dissolved oxygen and phytoplankton throughout the estuary to assist in designing monitoring programs, oxygen depth profiles and chlorophyll measurements were taken bi-weekly from May to December in 18 estuaries. In five of those estuaries, dissolved oxygen data loggers were set to measure oxygen at hourly intervals and at multiple locations within the estuary the subsequent year. The primary hypothesis was that dissolved oxygen in the upper estuary (first 10% of estuary area) is predictive of dissolved oxygen mid-estuary (50% of estuary area). The second hypothesis was that hypoxia/superoxia in the estuary is influenced by temperature and tidal flushing. Oxygen depth profiles conducted in the first year of study provided preliminary support that dissolved oxygen in the upper estuary was related to dissolved oxygen throughout the estuary. However, dissolved oxygen from loggers deployed at 10% and 50% of estuary area did not show as strong a correlation as expected (less than half the variance explained). The strength of the correlation declined towards the end of summer. Spatial decoupling of oxygen within the estuary suggested influence of local conditions. Chlorophyll concentration seemed also to be dependent on local conditions as it appeared to be coupled with the presence of sustained anoxia in the upper estuary with blooms typically occurring within 7 to 14 days of anoxia. The practical implication for oxygen monitoring is that one location within the most severely impacted part of the estuary is not sufficient to fully evaluate the severity of eutrophication effects. SUPPLEMENTARY INFORMATION: The online version contains supplementary material available at 10.1007/s10661-021-09589-8. Springer International Publishing 2021-11-15 2021 /pmc/articles/PMC8593059/ /pubmed/34779929 http://dx.doi.org/10.1007/s10661-021-09589-8 Text en © Crown 2021 https://creativecommons.org/licenses/by/4.0/Open AccessThis article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) .
spellingShingle Article
Coffin, MRS
Knysh, KM
Roloson, SD
Pater, CC
Theriaul, E
Cormier, JM
Courtenay, SC
van den Heuvel, MR
Influence of nutrient enrichment on temporal and spatial dynamics of dissolved oxygen within northern temperate estuaries
title Influence of nutrient enrichment on temporal and spatial dynamics of dissolved oxygen within northern temperate estuaries
title_full Influence of nutrient enrichment on temporal and spatial dynamics of dissolved oxygen within northern temperate estuaries
title_fullStr Influence of nutrient enrichment on temporal and spatial dynamics of dissolved oxygen within northern temperate estuaries
title_full_unstemmed Influence of nutrient enrichment on temporal and spatial dynamics of dissolved oxygen within northern temperate estuaries
title_short Influence of nutrient enrichment on temporal and spatial dynamics of dissolved oxygen within northern temperate estuaries
title_sort influence of nutrient enrichment on temporal and spatial dynamics of dissolved oxygen within northern temperate estuaries
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8593059/
https://www.ncbi.nlm.nih.gov/pubmed/34779929
http://dx.doi.org/10.1007/s10661-021-09589-8
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