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Yoshimura, T; Suzuki, Koji; Kiyosawa, H; Ono, Tsuneo; Hattori, Hiroshi; Kuma, Kenshi; Nishioka, Jun (2013): Impacts of elevated CO2 on particulate and dissolved organic matter production: microcosm experiments using iron-deficient plankton communities in open subarctic waters [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.842185, Supplement to: Yoshimura, T et al. (2013): Impacts of elevated CO2 on particulate and dissolved organic matter production: microcosm experiments using iron-deficient plankton communities in open subarctic waters. Journal of Oceanography, 69(5), 601-618, https://doi.org/10.1007/s10872-013-0196-2

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Abstract:
Response of phytoplankton to increasing CO2 in seawater in terms of physiology and ecology is key to predicting changes in marine ecosystems. However, responses of natural plankton communities especially in the open ocean to higher CO2 levels have not been fully examined. We conducted CO2 manipulation experiments in the Bering Sea and the central subarctic Pacific, known as high nutrient and low chlorophyll regions, in summer 2007 to investigate the response of organic matter production in iron-deficient plankton communities to CO2 increases. During the 14-day incubations of surface waters with natural plankton assemblages in microcosms under multiple pCO2 levels, the dynamics of particulate organic carbon (POC) and nitrogen (PN), and dissolved organic carbon (DOC) and phosphorus (DOP) were examined with the plankton community compositions. In the Bering site, net production of POC, PN, and DOP relative to net chlorophyll-a production decreased with increasing pCO2. While net produced POC:PN did not show any CO2-related variations, net produced DOC:DOP increased with increasing pCO2. On the other hand, no apparent trends for these parameters were observed in the Pacific site. The contrasting results observed were probably due to the different plankton community compositions between the two sites, with plankton biomass dominated by large-sized diatoms in the Bering Sea versus ultra-eukaryotes in the Pacific Ocean. We conclude that the quantity and quality of the production of particulate and dissolved organic matter may be altered under future elevated CO2 environments in some iron-deficient ecosystems, while the impacts may be negligible in some systems.
Keyword(s):
Biomass/Abundance/Elemental composition; Bottles or small containers/Aquaria (<20 L); Ceratium sp.; Chaetoceros sp.; Community composition and diversity; Coscinodiscus sp.; Dinobryon balticum; Entire community; Gymnodinium sp.; Laboratory experiment; Mesodinium rubrum; Micro-nutrients; Neodenticula seminae; North Pacific; Open ocean; Parafavella sp.; Pelagos; Prorocentrum sp.; Pseudo-nitzschia sp.; Rhizosolenia sp.; Temperate; Thalassiothrix sp.; Tropidoneis sp.
Further details:
Lavigne, Héloïse; Epitalon, Jean-Marie; Gattuso, Jean-Pierre (2014): seacarb: seawater carbonate chemistry with R. R package version 3.0. https://cran.r-project.org/package=seacarb
Coverage:
Median Latitude: 51.205000 * Median Longitude: -175.515000 * South-bound Latitude: 49.020000 * West-bound Longitude: -177.010000 * North-bound Latitude: 53.390000 * East-bound Longitude: -174.020000
Date/Time Start: 2007-07-13T00:00:00 * Date/Time End: 2007-07-30T00:00:00
Event(s):
Bering_Sea * Latitude: 53.390000 * Longitude: -177.010000 * Date/Time Start: 2007-07-13T00:00:00 * Date/Time End: 2007-07-27T00:00:00 * Method/Device: Experiment (EXP)
subarctic_Pacific * Latitude: 49.020000 * Longitude: -174.020000 * Date/Time Start: 2007-07-16T00:00:00 * Date/Time End: 2007-07-30T00:00:00 * Method/Device: Experiment (EXP)
Comment:
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne et al, 2014) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI). The date of carbonate chemistry calculation is 2015-01-29.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEvent
2SiteSiteYoshimura, T
3Time in daysTimedaysYoshimura, T
4Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmYoshimura, Ttreatment
5ReplicateReplYoshimura, T
6Chlorophyll aChl aµg/lYoshimura, T> 10 µm
7Chlorophyll aChl aµg/lYoshimura, T0.7-10 µm
8Ammonium[NH4]+µmol/lYoshimura, TFluorescence determination
9Nitrate and Nitrite[NO3]- + [NO2]-µmol/lYoshimura, TSpectrophotometric
10Nitrite[NO2]-µmol/lYoshimura, TSpectrophotometric
11Phosphate[PO4]3-µmol/lYoshimura, TSpectrophotometric
12SilicateSi(OH)4µmol/lYoshimura, TSpectrophotometric
13Carbon, organic, particulatePOCµmol/lYoshimura, T
14Nitrogen, total, particulateTPNµmol/lYoshimura, T
15Carbon, organic, dissolvedDOCµmol/lYoshimura, T
16Phosphorus, organic, dissolvedDOPµmol/lYoshimura, T
17Chlorophyll aChl aµg/lYoshimura, THigh Performance Liquid Chromatography (HPLC)
18FucoxanthinFucoµg/lYoshimura, THigh Performance Liquid Chromatography (HPLC)
1919-HexanoyloxyfucoxanthinHex-fucoµg/lYoshimura, THigh Performance Liquid Chromatography (HPLC)
20PeridininPeridµg/lYoshimura, THigh Performance Liquid Chromatography (HPLC)
21BacteriaBact#/mlYoshimura, TFlow cytometry
22SynechococcusSynechococcus#/mlYoshimura, TFlow cytometry
23EukaryotesEuka#/mlYoshimura, TFlow cytometry
24DiatomsDiatoms%Yoshimura, Trelative contribution to Chl-a
25HaptophytesHaptophytes%Yoshimura, Trelative contribution to Chl-a
26SpeciesSpeciesYoshimura, T
27Cell densityCells#/mlYoshimura, T
28Temperature, waterTemp°CYoshimura, T
29SalinitySalYoshimura, T
30Alkalinity, totalATµmol/kgYoshimura, TPotentiometric titration
31Carbon, inorganic, dissolvedDICµmol/kgYoshimura, TCoulometric titration
32Carbonate system computation flagCSC flagYang, YanCalculated using seacarb after Nisumaa et al. (2010)
33pHpHYang, YanCalculated using seacarb after Nisumaa et al. (2010)total scale
34Carbon dioxideCO2µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
35Fugacity of carbon dioxide (water) at sea surface temperature (wet air)fCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
36Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
37Bicarbonate ion[HCO3]-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
38Carbonate ion[CO3]2-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
39Aragonite saturation stateOmega ArgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
40Calcite saturation stateOmega CalYang, YanCalculated using seacarb after Nisumaa et al. (2010)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
6772 data points

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