Severe Coastal Hypoxia Interchange with Ocean Acidification: An Experimental Perturbation Study on Carbon and Nutrient Biogeochemistry

Normally atmospheric CO2 is the major driver of ocean acidification (OA); however, local discharge/degradation of organic matter (OM) and redox reactions can exacerbate OA in coastal areas. In this work we study the response of nutrient and carbon systems to pH decrease in relation to hydrographical...

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Published in:Journal of Marine Science and Engineering
Main Authors: Natalia Kapetanaki, Evangelia Krasakopoulou, Eleni Stathopoulou, Manos Dassenakis, Michael Scoullos
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2020
Subjects:
Online Access:https://doi.org/10.3390/jmse8060462
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spelling ftmdpi:oai:mdpi.com:/2077-1312/8/6/462/ 2023-08-20T04:08:54+02:00 Severe Coastal Hypoxia Interchange with Ocean Acidification: An Experimental Perturbation Study on Carbon and Nutrient Biogeochemistry Natalia Kapetanaki Evangelia Krasakopoulou Eleni Stathopoulou Manos Dassenakis Michael Scoullos agris 2020-06-23 application/pdf https://doi.org/10.3390/jmse8060462 EN eng Multidisciplinary Digital Publishing Institute Chemical Oceanography https://dx.doi.org/10.3390/jmse8060462 https://creativecommons.org/licenses/by/4.0/ Journal of Marine Science and Engineering; Volume 8; Issue 6; Pages: 462 CO 2 addition ocean acidification pH decline nitrification microcosm experiment anoxic sediment hypoxic/anoxic boundary Text 2020 ftmdpi https://doi.org/10.3390/jmse8060462 2023-07-31T23:40:47Z Normally atmospheric CO2 is the major driver of ocean acidification (OA); however, local discharge/degradation of organic matter (OM) and redox reactions can exacerbate OA in coastal areas. In this work we study the response of nutrient and carbon systems to pH decrease in relation to hydrographically induced intermittent characteristics and examine scenarios for future ocean acidification in a coastal system. Laboratory microcosm experiments were conducted using seawater and surface sediment collected from the deepest part of Elefsis Bay; the pH was constantly being monitored while CO2 gas addition was adjusted automatically. In Elefsis Bay surface pCO2 is already higher than global present atmospheric values, while near the bottom pCO2 reaches 1538 μatm and carbonate saturation states were calculated to be around 1.5. During the experiment, in more acidified conditions, limited alkalinity increase was observed and was correlated with the addition of bicarbonates and OM. Ammonium oxidation was decelerated and a nitrification mechanism was noticed, despite oxygen deficiency, paralleled by reduction of Mn-oxides. Phosphate was found significantly elevated for the first time in lower pH values, without reprecipitating after reoxygenation; this was linked with Fe(II) oxidation and Fe(III) reprecipitation without phosphate adsorption affecting both available dissolved phosphate and (dissolved inorganic nitrogen) DIN:DIP (dissolved inorganic phosphate)ratio. Text Ocean acidification MDPI Open Access Publishing Journal of Marine Science and Engineering 8 6 462
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic CO 2 addition
ocean acidification
pH decline
nitrification
microcosm experiment
anoxic sediment
hypoxic/anoxic boundary
spellingShingle CO 2 addition
ocean acidification
pH decline
nitrification
microcosm experiment
anoxic sediment
hypoxic/anoxic boundary
Natalia Kapetanaki
Evangelia Krasakopoulou
Eleni Stathopoulou
Manos Dassenakis
Michael Scoullos
Severe Coastal Hypoxia Interchange with Ocean Acidification: An Experimental Perturbation Study on Carbon and Nutrient Biogeochemistry
topic_facet CO 2 addition
ocean acidification
pH decline
nitrification
microcosm experiment
anoxic sediment
hypoxic/anoxic boundary
description Normally atmospheric CO2 is the major driver of ocean acidification (OA); however, local discharge/degradation of organic matter (OM) and redox reactions can exacerbate OA in coastal areas. In this work we study the response of nutrient and carbon systems to pH decrease in relation to hydrographically induced intermittent characteristics and examine scenarios for future ocean acidification in a coastal system. Laboratory microcosm experiments were conducted using seawater and surface sediment collected from the deepest part of Elefsis Bay; the pH was constantly being monitored while CO2 gas addition was adjusted automatically. In Elefsis Bay surface pCO2 is already higher than global present atmospheric values, while near the bottom pCO2 reaches 1538 μatm and carbonate saturation states were calculated to be around 1.5. During the experiment, in more acidified conditions, limited alkalinity increase was observed and was correlated with the addition of bicarbonates and OM. Ammonium oxidation was decelerated and a nitrification mechanism was noticed, despite oxygen deficiency, paralleled by reduction of Mn-oxides. Phosphate was found significantly elevated for the first time in lower pH values, without reprecipitating after reoxygenation; this was linked with Fe(II) oxidation and Fe(III) reprecipitation without phosphate adsorption affecting both available dissolved phosphate and (dissolved inorganic nitrogen) DIN:DIP (dissolved inorganic phosphate)ratio.
format Text
author Natalia Kapetanaki
Evangelia Krasakopoulou
Eleni Stathopoulou
Manos Dassenakis
Michael Scoullos
author_facet Natalia Kapetanaki
Evangelia Krasakopoulou
Eleni Stathopoulou
Manos Dassenakis
Michael Scoullos
author_sort Natalia Kapetanaki
title Severe Coastal Hypoxia Interchange with Ocean Acidification: An Experimental Perturbation Study on Carbon and Nutrient Biogeochemistry
title_short Severe Coastal Hypoxia Interchange with Ocean Acidification: An Experimental Perturbation Study on Carbon and Nutrient Biogeochemistry
title_full Severe Coastal Hypoxia Interchange with Ocean Acidification: An Experimental Perturbation Study on Carbon and Nutrient Biogeochemistry
title_fullStr Severe Coastal Hypoxia Interchange with Ocean Acidification: An Experimental Perturbation Study on Carbon and Nutrient Biogeochemistry
title_full_unstemmed Severe Coastal Hypoxia Interchange with Ocean Acidification: An Experimental Perturbation Study on Carbon and Nutrient Biogeochemistry
title_sort severe coastal hypoxia interchange with ocean acidification: an experimental perturbation study on carbon and nutrient biogeochemistry
publisher Multidisciplinary Digital Publishing Institute
publishDate 2020
url https://doi.org/10.3390/jmse8060462
op_coverage agris
genre Ocean acidification
genre_facet Ocean acidification
op_source Journal of Marine Science and Engineering; Volume 8; Issue 6; Pages: 462
op_relation Chemical Oceanography
https://dx.doi.org/10.3390/jmse8060462
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/jmse8060462
container_title Journal of Marine Science and Engineering
container_volume 8
container_issue 6
container_start_page 462
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