Seawater carbonate chemistry and fatty acid content of plankton

Ocean Acidification (OA) effects on marine plankton are most often considered in terms of inorganic carbon chemistry, but decreasing pH may influence other aspects of cellular metabolism. Here we present the effects of OA on the fatty acid (FA) content and composition of an artificial phytoplankton...

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Bibliographic Details
Main Authors: Wang, Tifeng, Tong, Shanying, Liu, Nana, Li, Futian, Wells, Mark L, Gao, Kunshan
Format: Dataset
Language:English
Published: PANGAEA 2017
Subjects:
EXP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.890803
https://doi.org/10.1594/PANGAEA.890803
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.890803
record_format openpolar
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Alkalinity
total
all-cis-4,7,10,13,16,19-Docosahexaenoic acid of total fatty acids
all-cis-6,9,12,15,18-Heneicosapentaenoic acid of total fatty acids
Aragonite saturation state
Behaviour
Bicarbonate ion
Biomass/Abundance/Elemental composition
Calcite saturation state
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Carbon dioxide
Chlorophyll a
Coast and continental shelf
Day of experiment
Docosahexaenoic acid
Eicosapentaenoic acid
Entire community
EXP
Experiment
Fatty acids
saturated
standard deviation
Field experiment
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Grazing rate
Group
Mesocosm or benthocosm
Monounsaturated fatty acids
Name
n-fatty acid C14:0
n-fatty acid C16:1
n-fatty acid C18:0
n-fatty acid C18:1n9
North Pacific
OA-ICC
Ocean Acidification International Coordination Centre
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
Pelagos
Percentage
spellingShingle Alkalinity
total
all-cis-4,7,10,13,16,19-Docosahexaenoic acid of total fatty acids
all-cis-6,9,12,15,18-Heneicosapentaenoic acid of total fatty acids
Aragonite saturation state
Behaviour
Bicarbonate ion
Biomass/Abundance/Elemental composition
Calcite saturation state
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Carbon dioxide
Chlorophyll a
Coast and continental shelf
Day of experiment
Docosahexaenoic acid
Eicosapentaenoic acid
Entire community
EXP
Experiment
Fatty acids
saturated
standard deviation
Field experiment
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Grazing rate
Group
Mesocosm or benthocosm
Monounsaturated fatty acids
Name
n-fatty acid C14:0
n-fatty acid C16:1
n-fatty acid C18:0
n-fatty acid C18:1n9
North Pacific
OA-ICC
Ocean Acidification International Coordination Centre
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
Pelagos
Percentage
Wang, Tifeng
Tong, Shanying
Liu, Nana
Li, Futian
Wells, Mark L
Gao, Kunshan
Seawater carbonate chemistry and fatty acid content of plankton
topic_facet Alkalinity
total
all-cis-4,7,10,13,16,19-Docosahexaenoic acid of total fatty acids
all-cis-6,9,12,15,18-Heneicosapentaenoic acid of total fatty acids
Aragonite saturation state
Behaviour
Bicarbonate ion
Biomass/Abundance/Elemental composition
Calcite saturation state
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Carbon dioxide
Chlorophyll a
Coast and continental shelf
Day of experiment
Docosahexaenoic acid
Eicosapentaenoic acid
Entire community
EXP
Experiment
Fatty acids
saturated
standard deviation
Field experiment
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Grazing rate
Group
Mesocosm or benthocosm
Monounsaturated fatty acids
Name
n-fatty acid C14:0
n-fatty acid C16:1
n-fatty acid C18:0
n-fatty acid C18:1n9
North Pacific
OA-ICC
Ocean Acidification International Coordination Centre
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
Pelagos
Percentage
description Ocean Acidification (OA) effects on marine plankton are most often considered in terms of inorganic carbon chemistry, but decreasing pH may influence other aspects of cellular metabolism. Here we present the effects of OA on the fatty acid (FA) content and composition of an artificial phytoplankton community (Phaeodactylum tricornutum, Thalassiosira weissflogii, and Emiliania huxleyi) in a fully replicated, 4 m**3 mesocosm study in subtropical coastal waters (Wuyuan Bay, China, 24.52°N, 117.18°E) at present day (400 μatm) and elevated (1000 μatm) pCO2 concentrations. Phytoplankton growth occurred in three phases during the 33-day experiment: an initial exponential growth leading to senescence and a subsequent decline phase. Phytoplankton sampled from these mesocosms were fed to mesozooplankton collected by net haul from Wuyuan Bay. Concentrations of saturated fatty acids (SFA) in both phytoplankton and mesozooplankton remained high under acidified and non-acidified conditions. However, polyunsaturated fatty acids (PUFA) and monounsaturated fatty acids (MUFA) increased significantly more under elevated pCO2 during the late exponential phase (Day 13), indicating increased nutritional value for zooplankton and higher trophic levels. Indeed, uptake rates of the essential FA docosahexaenoic acid (C20:5n3, DHA) increased in mesozooplankton under acidified conditions. However, mesozooplankton grazing rates decreased overall with elevated pCO2. Our findings show that these selected phytoplankton species have a relatively high tolerance to acidification in terms of FA production, and local mesozooplankton in these subtropical coastal waters can maintain their FA composition under end of century ocean acidification conditions.
format Dataset
author Wang, Tifeng
Tong, Shanying
Liu, Nana
Li, Futian
Wells, Mark L
Gao, Kunshan
author_facet Wang, Tifeng
Tong, Shanying
Liu, Nana
Li, Futian
Wells, Mark L
Gao, Kunshan
author_sort Wang, Tifeng
title Seawater carbonate chemistry and fatty acid content of plankton
title_short Seawater carbonate chemistry and fatty acid content of plankton
title_full Seawater carbonate chemistry and fatty acid content of plankton
title_fullStr Seawater carbonate chemistry and fatty acid content of plankton
title_full_unstemmed Seawater carbonate chemistry and fatty acid content of plankton
title_sort seawater carbonate chemistry and fatty acid content of plankton
publisher PANGAEA
publishDate 2017
url https://doi.pangaea.de/10.1594/PANGAEA.890803
https://doi.org/10.1594/PANGAEA.890803
op_coverage LATITUDE: 24.520000 * LONGITUDE: 118.200000 * DATE/TIME START: 2013-06-15T00:00:00 * DATE/TIME END: 2013-06-15T00:00:00
long_lat ENVELOPE(118.200000,118.200000,24.520000,24.520000)
genre Ocean acidification
genre_facet Ocean acidification
op_source Supplement to: Wang, Tifeng; Tong, Shanying; Liu, Nana; Li, Futian; Wells, Mark L; Gao, Kunshan (2017): The fatty acid content of plankton is changing in subtropical coastal waters as a result of OA: Results from a mesocosm study. Marine Environmental Research, 132, 51-62, https://doi.org/10.1016/j.marenvres.2017.10.010
op_relation Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James C; Gentili, Bernard; Proye, Aurélien; Soetaert, Karline; Rae, James (2016): seacarb: seawater carbonate chemistry with R. R package version 3.1. https://cran.r-project.org/package=seacarb
https://doi.pangaea.de/10.1594/PANGAEA.890803
https://doi.org/10.1594/PANGAEA.890803
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1594/PANGAEA.89080310.1016/j.marenvres.2017.10.010
_version_ 1810469263932129280
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.890803 2024-09-15T18:27:58+00:00 Seawater carbonate chemistry and fatty acid content of plankton Wang, Tifeng Tong, Shanying Liu, Nana Li, Futian Wells, Mark L Gao, Kunshan LATITUDE: 24.520000 * LONGITUDE: 118.200000 * DATE/TIME START: 2013-06-15T00:00:00 * DATE/TIME END: 2013-06-15T00:00:00 2017 text/tab-separated-values, 4287 data points https://doi.pangaea.de/10.1594/PANGAEA.890803 https://doi.org/10.1594/PANGAEA.890803 en eng PANGAEA Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James C; Gentili, Bernard; Proye, Aurélien; Soetaert, Karline; Rae, James (2016): seacarb: seawater carbonate chemistry with R. R package version 3.1. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.890803 https://doi.org/10.1594/PANGAEA.890803 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Wang, Tifeng; Tong, Shanying; Liu, Nana; Li, Futian; Wells, Mark L; Gao, Kunshan (2017): The fatty acid content of plankton is changing in subtropical coastal waters as a result of OA: Results from a mesocosm study. Marine Environmental Research, 132, 51-62, https://doi.org/10.1016/j.marenvres.2017.10.010 Alkalinity total all-cis-4,7,10,13,16,19-Docosahexaenoic acid of total fatty acids all-cis-6,9,12,15,18-Heneicosapentaenoic acid of total fatty acids Aragonite saturation state Behaviour Bicarbonate ion Biomass/Abundance/Elemental composition Calcite saturation state Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Chlorophyll a Coast and continental shelf Day of experiment Docosahexaenoic acid Eicosapentaenoic acid Entire community EXP Experiment Fatty acids saturated standard deviation Field experiment Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Grazing rate Group Mesocosm or benthocosm Monounsaturated fatty acids Name n-fatty acid C14:0 n-fatty acid C16:1 n-fatty acid C18:0 n-fatty acid C18:1n9 North Pacific OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos Percentage dataset 2017 ftpangaea https://doi.org/10.1594/PANGAEA.89080310.1016/j.marenvres.2017.10.010 2024-07-24T02:31:33Z Ocean Acidification (OA) effects on marine plankton are most often considered in terms of inorganic carbon chemistry, but decreasing pH may influence other aspects of cellular metabolism. Here we present the effects of OA on the fatty acid (FA) content and composition of an artificial phytoplankton community (Phaeodactylum tricornutum, Thalassiosira weissflogii, and Emiliania huxleyi) in a fully replicated, 4 m**3 mesocosm study in subtropical coastal waters (Wuyuan Bay, China, 24.52°N, 117.18°E) at present day (400 μatm) and elevated (1000 μatm) pCO2 concentrations. Phytoplankton growth occurred in three phases during the 33-day experiment: an initial exponential growth leading to senescence and a subsequent decline phase. Phytoplankton sampled from these mesocosms were fed to mesozooplankton collected by net haul from Wuyuan Bay. Concentrations of saturated fatty acids (SFA) in both phytoplankton and mesozooplankton remained high under acidified and non-acidified conditions. However, polyunsaturated fatty acids (PUFA) and monounsaturated fatty acids (MUFA) increased significantly more under elevated pCO2 during the late exponential phase (Day 13), indicating increased nutritional value for zooplankton and higher trophic levels. Indeed, uptake rates of the essential FA docosahexaenoic acid (C20:5n3, DHA) increased in mesozooplankton under acidified conditions. However, mesozooplankton grazing rates decreased overall with elevated pCO2. Our findings show that these selected phytoplankton species have a relatively high tolerance to acidification in terms of FA production, and local mesozooplankton in these subtropical coastal waters can maintain their FA composition under end of century ocean acidification conditions. Dataset Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(118.200000,118.200000,24.520000,24.520000)