Controls on Nutrient Cycling in Estuarine Mangrove Lake Sediments

We estimated the net exchange of nitrogen and phosphorus species using core incubations under light and dark conditions in estuarine lakes that are the aquatic interface between the freshwater Everglades and marine Florida Bay. These lakes and adjacent shallow water Florida Bay environments are site...

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Main Authors: Michael S. Owens, Stephen P. Kelly, Thomas A. Frankovich, David T. Rudnick, James W. Fourqurean, Jeffrey C. Cornwell
Format: Article
Language:English
Published: MDPI AG 2021-06-01
Series:Journal of Marine Science and Engineering
Subjects:
Online Access:https://www.mdpi.com/2077-1312/9/6/626
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author Michael S. Owens
Stephen P. Kelly
Thomas A. Frankovich
David T. Rudnick
James W. Fourqurean
Jeffrey C. Cornwell
author_facet Michael S. Owens
Stephen P. Kelly
Thomas A. Frankovich
David T. Rudnick
James W. Fourqurean
Jeffrey C. Cornwell
author_sort Michael S. Owens
collection DOAJ
description We estimated the net exchange of nitrogen and phosphorus species using core incubations under light and dark conditions in estuarine lakes that are the aquatic interface between the freshwater Everglades and marine Florida Bay. These lakes and adjacent shallow water Florida Bay environments are sites where the restoration of hydrological flows will likely have the largest impact on salinity. Sediment respiration, measured by oxygen uptake, averaged (±S.D.) −2400 ± 1300, −300 ± 1000, and 1900 ± 1400 μmol m<sup>−2</sup> h<sup>−1</sup> for dark incubations, light incubations, and gross photosynthesis estimates, respectively, with dark incubations consistent with oxygen uptake measured by microelectrode profiles. Although most fluxes of soluble reactive phosphorus, nitrate, and N<sub>2</sub>–N were low under both light and dark incubation conditions, we observed a number of very high efflux events of NH<sub>4</sub><sup>+</sup> during dark incubations. A significant decrease in NH<sub>4</sub><sup>+</sup>flux was observed in the light. The largest differences between light and dark effluxes of NH<sub>4</sub><sup>+</sup> occurred in lakes during periods of low coverage of the aquatic macrophyte <i>Chara hornemannii</i> Wallman, with NH<sub>4</sub><sup>+</sup> effluxes > 200 μmol m<sup>−2</sup> h<sup>−1</sup>. Increasing freshwater flow from the Everglades is expected to expand lower salinity environments suitable for <i>Chara</i>, and therefore, diminish the sediment NH<sub>4</sub><sup>+</sup> effluxes that may fuel algal blooms.
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spelling doaj.art-6564b2bebe744d50a0e00d177d94f43a2023-11-21T22:47:17ZengMDPI AGJournal of Marine Science and Engineering2077-13122021-06-019662610.3390/jmse9060626Controls on Nutrient Cycling in Estuarine Mangrove Lake SedimentsMichael S. Owens0Stephen P. Kelly1Thomas A. Frankovich2David T. Rudnick3James W. Fourqurean4Jeffrey C. Cornwell5Horn Point Laboratory, University of Maryland Center for Environmental Science, Cambridge, MD 21613, USASouth Florida Water Management District, West Palm Beach, FL 33406, USAInstitute of Environment, Florida International University, Miami, FL 33131, USASouth Florida Natural Resources Center, Everglades National Park, Homestead, FL 33030, USAInstitute of Environment, Florida International University, Miami, FL 33131, USAHorn Point Laboratory, University of Maryland Center for Environmental Science, Cambridge, MD 21613, USAWe estimated the net exchange of nitrogen and phosphorus species using core incubations under light and dark conditions in estuarine lakes that are the aquatic interface between the freshwater Everglades and marine Florida Bay. These lakes and adjacent shallow water Florida Bay environments are sites where the restoration of hydrological flows will likely have the largest impact on salinity. Sediment respiration, measured by oxygen uptake, averaged (±S.D.) −2400 ± 1300, −300 ± 1000, and 1900 ± 1400 μmol m<sup>−2</sup> h<sup>−1</sup> for dark incubations, light incubations, and gross photosynthesis estimates, respectively, with dark incubations consistent with oxygen uptake measured by microelectrode profiles. Although most fluxes of soluble reactive phosphorus, nitrate, and N<sub>2</sub>–N were low under both light and dark incubation conditions, we observed a number of very high efflux events of NH<sub>4</sub><sup>+</sup> during dark incubations. A significant decrease in NH<sub>4</sub><sup>+</sup>flux was observed in the light. The largest differences between light and dark effluxes of NH<sub>4</sub><sup>+</sup> occurred in lakes during periods of low coverage of the aquatic macrophyte <i>Chara hornemannii</i> Wallman, with NH<sub>4</sub><sup>+</sup> effluxes > 200 μmol m<sup>−2</sup> h<sup>−1</sup>. Increasing freshwater flow from the Everglades is expected to expand lower salinity environments suitable for <i>Chara</i>, and therefore, diminish the sediment NH<sub>4</sub><sup>+</sup> effluxes that may fuel algal blooms.https://www.mdpi.com/2077-1312/9/6/626nutrient fluxesEvergladessediment<i>Chara</i>water management
spellingShingle Michael S. Owens
Stephen P. Kelly
Thomas A. Frankovich
David T. Rudnick
James W. Fourqurean
Jeffrey C. Cornwell
Controls on Nutrient Cycling in Estuarine Mangrove Lake Sediments
Journal of Marine Science and Engineering
nutrient fluxes
Everglades
sediment
<i>Chara</i>
water management
title Controls on Nutrient Cycling in Estuarine Mangrove Lake Sediments
title_full Controls on Nutrient Cycling in Estuarine Mangrove Lake Sediments
title_fullStr Controls on Nutrient Cycling in Estuarine Mangrove Lake Sediments
title_full_unstemmed Controls on Nutrient Cycling in Estuarine Mangrove Lake Sediments
title_short Controls on Nutrient Cycling in Estuarine Mangrove Lake Sediments
title_sort controls on nutrient cycling in estuarine mangrove lake sediments
topic nutrient fluxes
Everglades
sediment
<i>Chara</i>
water management
url https://www.mdpi.com/2077-1312/9/6/626
work_keys_str_mv AT michaelsowens controlsonnutrientcyclinginestuarinemangrovelakesediments
AT stephenpkelly controlsonnutrientcyclinginestuarinemangrovelakesediments
AT thomasafrankovich controlsonnutrientcyclinginestuarinemangrovelakesediments
AT davidtrudnick controlsonnutrientcyclinginestuarinemangrovelakesediments
AT jameswfourqurean controlsonnutrientcyclinginestuarinemangrovelakesediments
AT jeffreyccornwell controlsonnutrientcyclinginestuarinemangrovelakesediments