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Prouty, Nancy G; Cohen, Anne L; Yates, Kimberly Kaye; Storlazzi, Curt D; Swarzenski, Peter W; White, Lisa D (2017): Seawater carbonate chemistry and bioerosion of croal reef [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.923983

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Abstract:
Ocean acidification (OA), the gradual decline in ocean pH and [CO3 ] 2- caused by rising levels of atmospheric CO2, poses a significant threat to coral reef ecosystems, depressing rates of calcium carbonate (CaCO3) production, and enhancing rates of bioerosion and dissolution. As ocean pH and [CO3] 2- decline globally, there is increasing emphasis on managing local stressors that can exacerbate the vulnerability of coral reefs to the effects of OA. We show that sustained, nutrient rich, lower pH submarine groundwater discharging onto nearshore coral reefs off west Maui lowers the pH of seawater and exposes corals to nitrate concentrations 50 times higher than ambient. Rates of coral calcification are substantially decreased, and rates of bioerosion are orders of magnitude higher than those observed in coral cores collected in the Pacific under equivalent low pH conditions but living in oligotrophic waters. Heavier coral nitrogen isotope (delta15N) values pinpoint not only site-specific eutrophication, but also a sewage nitrogen source enriched in 15N. Our results show that eutrophication of reef seawater by land-based sources of pollution can magnify the effects of OA through nutrient driven-bioerosion. These conditions could contribute to the collapse of coastal coral reef ecosystems sooner than current projections predict based only on ocean acidification.
Keyword(s):
Benthos; Calcification/Dissolution; Coast and continental shelf; Entire community; Field observation; Growth/Morphology; Rocky-shore community; South Pacific; Tropical
Supplement to:
Prouty, Nancy G; Cohen, Anne L; Yates, Kimberly Kaye; Storlazzi, Curt D; Swarzenski, Peter W; White, Lisa D (2017): Vulnerability of Coral Reefs to Bioerosion From Land‐Based Sources of Pollution. Journal of Geophysical Research: Oceans, 122(12), 9319-9331, https://doi.org/10.1002/2017JC013264
Further details:
Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James C; Gentili, Bernard; Hagens, Mathilde; Hofmann, Andreas; Mueller, Jens-Daniel; Proye, Aurélien; Rae, James; Soetaert, Karline (2019): seacarb: seawater carbonate chemistry with R. R package version 3.2.12. https://CRAN.R-project.org/package=seacarb
Coverage:
Median Latitude: 20.313129 * Median Longitude: -156.231100 * South-bound Latitude: 20.312400 * West-bound Longitude: -156.231100 * North-bound Latitude: 20.315000 * East-bound Longitude: -156.231100
Date/Time Start: 2013-07-01T00:00:00 * Date/Time End: 2013-07-31T00:00:00
Minimum DEPTH, water: m * Maximum DEPTH, water: m
Event(s):
Kahekili * Latitude: 20.313100 * Longitude: -156.231100 * Date/Time Start: 2013-07-01T00:00:00 * Date/Time End: 2013-07-31T00:00:00 * Method/Device: Experiment (EXP)
Comment:
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2019) 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 by seacarb is 2020-10-14.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1TypeTypeProuty, Nancy Gstudy
2IdentificationIDProuty, Nancy Gcoral
3Core lengthCore lengthcmProuty, Nancy G
4DEPTH, waterDepth watermProuty, Nancy GGeocode
5LATITUDELatitudeProuty, Nancy GGeocode
6LONGITUDELongitudeProuty, Nancy GGeocode
7YearsYearsProuty, Nancy GLifespan
8ThicknessThickmmProuty, Nancy GTissue
9DistanceDistancemProuty, Nancy Goffshor
10DistanceDistancemProuty, Nancy Gfrom seep, blank=at seep
11DirectionDirectiondegProuty, Nancy Gfrom seep
12YearsYearsProuty, Nancy G
13Growth rateµmm/aProuty, Nancy G
14Growth rate, standard deviationµ std dev±Prouty, Nancy G
15DensityDensityg/cm3Prouty, Nancy G
16Calcification rateCalc rateg/cm2/aProuty, Nancy G
17PercentagePerc%Prouty, Nancy GVolume bioerosion
18Bioerosion rateBioerosiong/m2/aProuty, Nancy G
19Bioerosion rateBioerosiong/m2/aProuty, Nancy GPredicted
20δ15Nδ15N‰ airProuty, Nancy G
21δ15N, standard deviationδ15N std dev±Prouty, Nancy G
22ReplicatesRepl#Prouty, Nancy G
23Aragonite saturation stateOmega ArgProuty, Nancy GCalculated using CO2SYS
24Aragonite saturation state, standard deviationOmega Arg std dev±Prouty, Nancy GCalculated using CO2SYS
25pHpHProuty, Nancy Gtotal scale
26pH, standard deviationpH std dev±Prouty, Nancy Gtotal scale
27SalinitySalProuty, Nancy G
28Salinity, standard deviationSal std dev±Prouty, Nancy G
29Nitrate[NO3]-µmol/lProuty, Nancy G
30Nitrate, standard deviationNO3 std dev±Prouty, Nancy G
31Temperature, waterTemp°CProuty, Nancy G
32Carbonate system computation flagCSC flagYang, YanCalculated using seacarb after Nisumaa et al. (2010)
33Carbon dioxideCO2µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
34Fugacity of carbon dioxide (water) at sea surface temperature (wet air)fCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
35Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
36Bicarbonate ion[HCO3]-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
37Carbonate ion[CO3]2-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
38Carbon, inorganic, dissolvedDICµmol/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:
191 data points

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