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dc.contributor.authorRoca, Guillemes_ES
dc.contributor.authorPalacios, Javieres_ES
dc.contributor.authorRuiz-Halpern, Sergioes_ES
dc.contributor.authorMarbà, Núriaes_ES
dc.coverage.spatialname=Badia de Pollença; lat=-39.89604; long=3.14346es_ES
dc.coverage.spatialhttps://www.geonames.org/2512431/badia-de-pollenca.html-
dc.coverage.temporalstart=2017-10-01; end=2017-10-31es_ES
dc.date.accessioned2023-06-28T11:41:25Z-
dc.date.available2023-06-28T11:41:25Z-
dc.date.issued2022-04-13-
dc.identifier.citationRoca, Guillem; Palacios, Javier; Ruiz-Halpern, Sergio; Marbà, Núria; 2022; Dataset: Experimental carbon emissions from degraded Mediterranean seagrass (Posidonia oceanica) meadows under current and future summer temperatures [Dataset]; Zenodo; Version 1; https://doi.org/10.5281/zenodo.6427224es_ES
dc.identifier.urihttp://hdl.handle.net/10261/329922-
dc.descriptionThe dataset contains data on sediment C02 efflux rates, carbon emissions during the experiment (gm-2), % Organic Carbon, Organic Matter content of the Posidonia oceanica seagrass sediments collected in Pollença bay (North of Mallorca Island). Sediments were cultivated in 5 different seawater temperature treatments and two different agitation conditions. Sediments used in the experiment were extracted in October 2017 from the P. Oceanica meadow of Pollença in Mallorca Island at six-meter depth Figure (1). Sediments were sampled in October 2017 using sediment cores (9 cm ID and 30cm long) and directly transported to the laboratory. Only the top 10 cm of the sediment cores were used since this fraction is the most susceptible to erosion. Living seagrass tissues (roots, rhizomes, and leaves) were removed and sediment was mixed and homogenized. 40ml of sediments were poured into glass containers of 750ml with 500ml of seawater. Finally, each recipient contained a sediment layer of approximately 1.1cm in each container. Containers were placed at five different temperature baths (26,27.5, 29, 30.5, 32 ºC) simulating summer temperatures in the bay (Garcias-Bonet et al., 2019) at different agitation regimes (agitation/repose) to simulate exposed and sheltered conditions.10 containers were sampled right after the experiment started to provide initial sediment conditions. Five containers per temperature and agitation treatment were removed 7, 21, 43, 67, and 98 days from the experiment start, to analyse sediment organic matter and CaCO3 content. CO2 incubations were run 5, 14, 56, and 91 days from the experiment start. Sampling times were distributed considering that organic matter remineralisation was likely to follow an exponential trend, including a rapid phase of loss of the more labile material followed by a slower loss of more recalcitrant substrates (Arndt et al., 2013). The experiment was run in the dark to avoid photosynthesis in an isothermal chamber at 21ºC.es_ES
dc.descriptionOrganic carbon analysis: In each sampling time, organic matter content in sediments (OM %DW) was estimated as the percentage weight loss of dry sediment sample after combustion at 550ºC for 4 hours. Organic carbon (Corg) was calculated from OM content using the relation described in (Mazarrasa et al., 2017b) y = 0.29x – 0.64; (R2=0.98, p< 0.0001, n=60) OM and POC stocks along the experiment (mg OM ml-1 and mg POC ml-1) were estimated by multiplying the OM and POC (%DW) by the sediment dry weight (mg) remaining in each experimental unit and standardized to the initial volume of sediment (40 ml) introduced in every glass container. Inorganic carbon was estimated as the percentage weight loss of already combusted sediment (550ºC) after combustion at 1000ºC.-
dc.descriptionSediment CO2 production: Container headspace CO2 gas concentration was measured during 20 minutes continuum incubations (4 replicates) in each temperature and agitation treatment in all sampling times. CO2 air concentration measures were carried out using an Infra Red Gas Analyser EGM4 from PPSystems. Concentration of dissolved CO2 in seawater (in μmol CO2 L−1) was calculated from the concentration of CO2 (in ppm) measured in headspace air samples after equilibration as described in (Garcias-Bonet and Duarte, 2017; Wilson et al., 2012). Briefly, we calculate the dissolved CO2 remaining in seawater after equilibration with the air phase ([CO2]SW−eq) by, [CO2]SW−eq = 10−6 β [C CO2]Air P where β is the Bunsen solubility coefficient of CO2, calculated according to Wiesenburg and Guinasso (1979), as a function of seawater temperature and salinity; [CO2]Air is the CO2 concentration measured in containers headspace air (in ppm) and P is the atmospheric pressure (in atm) of dry air that was corrected by the effect of multiple sampling applying Boyle’s Law. Then, the initial CO2 concentration in seawater before the equilibrium ([CO2]SW−before eq) was calculated (in ml CO2 /ml H2O) by [CO2]SW−before eq = ([CH4]SW−eq VSw + 10−6 ([CO2]Air −[CO2]Air background) VAir)/VSW Where VSw is the volume of seawater in the core or in the seawater closed circuit, [CO2]Air background is the atmospheric CO2 background level and VAir is the volume of the headspace or the closed air circuit. Finally, the initial CO2 concentration was transformed to µmol CH4 L−1 by applying the ideal gas law. CO2 efflux values were calculated from CO2 variation per time unit. Then, we converted the rates to aerial (taking in account container surface) base, and thickness (in μmol m-2 s-1).-
dc.description.abstractThe dataset provides data on sediment C02 efflux rates (μmol CO2 m-2 s-1), carbon emissions during the experiment (gm-2), % Organic Carbon, Organic Matter content (g m-2) of the Posidonia oceanica seagrass sediments collected in Pollença bay (North of Mallorca Island). Sediments were cultivated in 5 different seawater temperature treatments and two different agitation conditions.es_ES
dc.description.tableofcontentsCO2 efflux.xlsxes_ES
dc.description.tableofcontentsdataset_units.xlsx-
dc.description.tableofcontentsSediment_Organic_Carbon.xlsx-
dc.formatapplication/vnd.ms-exceles_ES
dc.language.isoenges_ES
dc.publisherZenodoes_ES
dc.relation.isreferencedbyRoca, Guillem; Palacios, Javier; Ruiz-Halpern, Sergio; Marbà, Núria. Experimental Carbon Emissions From Degraded Mediterranean Seagrass (Posidonia oceanica) Meadows Under Current and Future Summer Temperatures. http://dx.doi.org/10.1029/2022JG006946. http://hdl.handle.net/10261/295839es_ES
dc.rightsopenAccesses_ES
dc.subjectC02 efflux rateses_ES
dc.subjectC02 emissionses_ES
dc.subjectSedimentes_ES
dc.subjectSeagrasses_ES
dc.subjectPosidonia Oceanicaes_ES
dc.subjectExperimentes_ES
dc.subjectTemperature treatmentes_ES
dc.subjectSediment suspensiones_ES
dc.subjectBlue carbones_ES
dc.subjectOrganic Carbones_ES
dc.titleDataset: Experimental carbon emissions from degraded Mediterranean seagrass (Posidonia oceanica) meadows under current and future summer temperatureses_ES
dc.typedatasetes_ES
dc.identifier.doi10.5281/zenodo.6427224-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttps://doi.org/10.5281/zenodo.6427224es_ES
dc.rights.licensehttps://creativecommons.org/licenses/by/4.0/legalcodees_ES
dc.relation.csicSíes_ES
oprm.item.hasRevisionno ko 0 false*
dc.contributor.orcidRoca, Guillem [0000-0002-8225-6047]es_ES
dc.contributor.contactPersonRoca, Guillem [guillemrocac@gmail.com]es_ES
dc.type.coarhttp://purl.org/coar/resource_type/c_ddb1es_ES
item.grantfulltextopen-
item.fulltextWith Fulltext-
item.openairecristypehttp://purl.org/coar/resource_type/c_ddb1-
item.languageiso639-1en-
item.cerifentitytypeProducts-
item.openairetypedataset-
Aparece en las colecciones: (IMEDEA) Conjuntos de datos
Ficheros en este ítem:
Fichero Descripción Tamaño Formato
Sediment_Organic_Carbon.xlsx43,38 kBMicrosoft Excel XMLVisualizar/Abrir
dataset_units.xlsx9,5 kBMicrosoft Excel XMLVisualizar/Abrir
CO2 efflux.xlsx52,2 kBMicrosoft Excel XMLVisualizar/Abrir
README.txt8,17 kBTextVisualizar/Abrir
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