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  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: Duarte, Carlos Manuel; Delgado-Huertas, Antonio; Anton, Andrea; Carrillo-de-Albornoz, Paloma; López-Sandoval, Daffne C; Agustí, Susana; Almahasheer, Hanan; Marbà, Núria; Hendriks, Iris; Krause-Jensen, Dorte; Garcias-Bonet, Neus (2018): Stable isotope (δ13C, δ15N, δ18O, δD) composition and nutrient concentration of Red Sea primary producers. Frontiers in Marine Science, 5, https://doi.org/10.3389/fmars.2018.00298
    Publication Date: 2023-01-13
    Description: Data of stable isotope composition (δ13C, δ15N, δD, δ18O) and nutrient concentration (%N and %C) of primary producers (halophytes, macroalgae, mangroves, seagrasses, and seston) in the Red Sea
    Keywords: 1; 10; 11; 12; 13; 14; 15; 16; 17; 18; 19; 2; 20; 21; 22; 23; 24; 25; 26; 27; 28; 29; 3; 30; 31; 32; 33; 34; 35; 36; 37; 38; 39; 4; 40; 41; 42; 43; 44; 45; 46; 47; 48; 49; 5; 50; 51; 52; 53; 54; 55; 56; 57; 58; 59; 6; 60; 61; 62; 63; 64; 65; 66; 67; 68; 69; 7; 70; 71; 72; 73; 74; 75; 76; 77; 78; 79; 8; 80; 81; 82; 83; 84; 85; 86; 87; 88; 89; 9; 90; 91; 92; 93; Al Azizi; Al-Azizi-CCF-spring; C10-16; C1-16; C1-17; C2-17; C3-16; C4-16; C4-17; C5-16; C5-17; C6-16; C6-17; C7-16; C7-17; C8-16; C8-17; C9-16; C9-17; Carbon, organic, total; Carbon/Nitrogen ratio; CCF0602; CCF0702; CCF0808; CCF0902; CCF1002; CCF2ALR1; CCF2ALR2; CCF2AWR1; CCF2AWR2; CCF2DR1; CCF2DR2; CCF2DS1; CCF2THR3; CCF2THS1; CCF2YBR2; CCF2YBR3; CCF2YBS1; CCFALR1; CCFALR2; CCFALR3; CCFALS1; CCFAWR1; CCFAWR3; CCF Benthic Cruise Summer 2017; CCF Benthic Cruise Winter 2017; CCFDR1; CCFDR2; CCFDS1; CCF Pelagic Cruise Spring 2017; CCFTHR1; CCFTHS1; CCFYBR1; CCFYBR2; CCFYBS1; Economic_city-M; Economic_city-S; Economic_city-Sa; Event label; Habitat; Identification; Khor_Alkharar-M; Khor_Alkharar-S; Khor_Alkharar-Sa; Latitude of event; Longitude of event; M1-16; M1-17; M2-16; M2-17; M3-16; M3-17; M4-16; M4-17; M5-16; M5-17; M6-16; M7-16; Macrophytes; MULT; Multiple investigations; Nitrogen, organic; Pelagic_Station; Petro_Rabigh-M; Petro_Rabigh-S; Red Sea; Red Sea Seagrass and Mangrove Surveys 2016; Red Sea Seagrass and Mangrove Surveys 2017; S10-16; S10-17; S11-16; S11-17; S1-16; S1-17; S12-16; S2-16; S2-17; S3-16; S3-17; S4-16; S4-17; S5-16; S5-17; S6-16; S6-17; S7-16; S8-16; S8-17; S9-16; S9-17; Taxon/taxa; Thuwal_Island-M; Thuwal_Island-S; Thuwal 2438; Thuwal-CCF-summer; Thuwal-CCF-winter; Thuwal-Macrophytes-17; Thuwal-Seagrass-16; δ13C; δ15N; δ18O; δ Deuterium
    Type: Dataset
    Format: text/tab-separated-values, 5645 data points
    Location Call Number Limitation Availability
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  • 2
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    Unknown
    PANGAEA
    In:  Supplement to: Garcias-Bonet, Neus; Delgado Huertas, Antonio; Carrillo-de-Albornoz, Paloma; Anton, Andrea; Almahasheer, Hanan; Marbà, Núria; Hendriks, Iris; Krause-Jensen, Dorte; Duarte, Carlos Manuel (2019): Carbon and nitrogen concentrations, stocks, and isotopic compositions in Red Sea seagrass and mangrove sediments. Frontiers in Marine Science, 6, 267, https://doi.org/10.3389/fmars.2019.00267
    Publication Date: 2023-02-08
    Description: Data on carbon and nitrogen stocks and stable isotope composition (δ13C, δ15N) in Red Sea seagrass and mangrove sediments
    Keywords: 10; 12; 14; 15; 17; 19; 2; 25; 28; 29; 30; 35; 4; 46; 49; 5; 57; 59; 60; 62; 64; 65; 69; 7; 71; 73; 74; 76; 78; 79; 83; 88; 90; 91; 93; Calcium carbonate; Carbon, inorganic, total; Carbon, inorganic stock; Carbon, organic, per unit sediment mass; Carbon, organic, total; Carbon, organic stock; Carbon/Nitrogen ratio; CCF2DS1; CCF2THS1; CCF2YBS1; CCF Benthic Cruise Summer 2017; Cruise/expedition; Density, wet bulk; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Economic_city; Economic_city-1; Economic_city-2; Economic_city-3; Event label; Habitat; Khor_Alkarar; Khor_Alkarar-1; Khor_Alkarar-2; Khor_Alkarar-3; M1-16; M1-17; M2-16; M2-17; M3-16; M3-17; M4-16; M4-17; M5-16; M5-17; M6-16; M7-16; Macrophytes; mangrove ecosystems; marine sediments; MULT; Multiple investigations; Nitrogen, per unit sediment mass; Nitrogen, total; Nitrogen stock; Petro_Rabigh; Red Sea; Red Sea Seagrass and Mangrove Surveys 2016; Red Sea Seagrass and Mangrove Surveys 2017; Replicate; S10-16; S10-17; S11-16; S1-16; S1-17; S12-16; S2-16; S2-17; S3-16; S3-17; S4-16; S4-17; S5-16; S5-17; S6-16; S6-17; S7-16; S8-16; S9-16; S9-17; Sample code/label; seagrass ecosystems; Taxon/taxa; Thuwal; Thuwal 2438; Thuwal-CCF-summer; Thuwal-Macrophytes-17; Thuwal-Seagrass-16; δ13C, organic carbon; δ15N, bulk sediment
    Type: Dataset
    Format: text/tab-separated-values, 7601 data points
    Location Call Number Limitation Availability
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  • 3
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    Unknown
    PANGAEA
    In:  Supplement to: García-Corral, Lara S; Holding, Johnna; Carrillo-de-Albornoz, Paloma; Steckbauer, Alexandra; Pérez-Lorenzo, Maria; Navarro, Nuria; Serret, Pablo; Gasol, Josep M; Morán, Xosé Anxelu G; Estrada, Marta; Fraile-Nuez, Eugenio; Benítez-Barrios, Verónica M; Agustí, Susana; Duarte, Carlos Manuel (2017): Temperature dependence of plankton community metabolism in the subtropical and tropical ocean. Global Biogeochemical Cycles, 31(7), 1141-1154, https://doi.org/10.1002/2017GB005629
    Publication Date: 2023-07-05
    Description: Here we assess the temperature dependence of the metabolic rates (gross primary production - GPP, community respiration - CR and the ratio GPP/CR) of oceanic plankton communities. We compile data from 133 stations of the Malaspina 2010 Expedition, distributed among the subtropical and tropical Atlantic, Pacific and Indian oceans. We used the in vitro technique to measured metabolic rates during 24 h incubations at three different sampled depths: surface, 20% and 1% of the photosynthetically active radiation measured at surface. We also measured the % of ultraviolet B radiation (UVB) penetrating at surface waters. GPP and CR rates increased with warming, albeit different responses were observed for each sampled depth. The overall GPP/CR ratio declined with warming. Higher activation energies (Ea's) were derived for both processes (GPPChla = 0.97; CRChla = 1.26; CRHPA= 0.95 eV) compared to those previously reported. The Indian Ocean showed the highest Ea (GPPChla = 1.70; CRChla = 1.48; CRHPA= 0.57 eV), while the Atlantic Ocean showed the lowest (GPPChla = 0.86; CRChla = 0.77; CRHPA= -0.13 eV). We believe that the difference between previous assessments and the ones presented here can be explained by the overrepresentation of Atlantic communities in the previous data sets. We found that UVB radiation also affects the temperature dependence of surface GPP, which decreased rather than increased under high levels of UVB. Ocean warming, which causes stratification and oligotrophication of the subtropical and tropical oceans, may lead to reduced surface GPP as a result of increased penetration of UVB radiation.
    Keywords: 29HE20101215; 29HE20110117; 29HE20110211; 29HE20110317; 29HE20110416; 29HE20110513; 29HE20110619; Bio-Rosette; BRO; Canarias Sea; Caribbean Sea; Chlorophyll a; DATE/TIME; DEPTH, water; Depth comment; Event label; Gross primary production/Respiration rate ratio; Gross primary production of oxygen; Gross primary production of oxygen, standard error; Hespérides; Indian Ocean; LATITUDE; LONGITUDE; MALASPINA_LEG1; MALASPINA_LEG1_003-2; MALASPINA_LEG1_006-2; MALASPINA_LEG1_007-2; MALASPINA_LEG1_008-2; MALASPINA_LEG1_009-2; MALASPINA_LEG1_010-2; MALASPINA_LEG1_011-2; MALASPINA_LEG1_012-2; MALASPINA_LEG1_013-2; MALASPINA_LEG1_014-2; MALASPINA_LEG1_015-2; MALASPINA_LEG1_016-2; MALASPINA_LEG1_017-2; MALASPINA_LEG1_018-2; MALASPINA_LEG1_019-2; MALASPINA_LEG1_020-2; MALASPINA_LEG1_021-2; MALASPINA_LEG1_022-2; MALASPINA_LEG1_023-2; MALASPINA_LEG1_024-2; MALASPINA_LEG1_025-2; MALASPINA_LEG2; MALASPINA_LEG2_027-2; MALASPINA_LEG2_028-2; MALASPINA_LEG2_029-2; MALASPINA_LEG2_030-2; MALASPINA_LEG2_031-2; MALASPINA_LEG2_032-2; MALASPINA_LEG2_033-2; MALASPINA_LEG2_034-2; MALASPINA_LEG2_035-2; MALASPINA_LEG2_037-2; MALASPINA_LEG2_038-2; MALASPINA_LEG2_040-2; MALASPINA_LEG2_041-2; MALASPINA_LEG2_042-2; MALASPINA_LEG2_043-2; MALASPINA_LEG2_044-2; MALASPINA_LEG3; MALASPINA_LEG3_045-2; MALASPINA_LEG3_046-2; MALASPINA_LEG3_047-2; MALASPINA_LEG3_048-2; MALASPINA_LEG3_049-2; MALASPINA_LEG3_050-2; MALASPINA_LEG3_051-2; MALASPINA_LEG3_052-2; MALASPINA_LEG3_053-2; MALASPINA_LEG3_054-2; MALASPINA_LEG3_055-2; MALASPINA_LEG3_056-2; MALASPINA_LEG3_057-2; MALASPINA_LEG3_058-2; MALASPINA_LEG3_059-2; MALASPINA_LEG3_060-2; MALASPINA_LEG3_061-2; MALASPINA_LEG3_062-2; MALASPINA_LEG3_063-2; MALASPINA_LEG3_064-2; MALASPINA_LEG3_065-2; MALASPINA_LEG3_066-2; MALASPINA_LEG3_067-2; MALASPINA_LEG3_068-2; MALASPINA_LEG4; MALASPINA_LEG4_069-2; MALASPINA_LEG4_070-2; MALASPINA_LEG4_071-2; MALASPINA_LEG4_072-2; MALASPINA_LEG4_073-2; MALASPINA_LEG4_074-2; MALASPINA_LEG4_075-2; MALASPINA_LEG4_076-2; MALASPINA_LEG4_077-2; MALASPINA_LEG4_078-2; MALASPINA_LEG5; MALASPINA_LEG5_079-2; MALASPINA_LEG5_082-2; MALASPINA_LEG5_083-2; MALASPINA_LEG5_084-2; MALASPINA_LEG5_085-2; MALASPINA_LEG5_086-2; MALASPINA_LEG5_087-2; MALASPINA_LEG5_088-2; MALASPINA_LEG5_090-2; MALASPINA_LEG5_091-2; MALASPINA_LEG5_092-2; MALASPINA_LEG5_093-2; MALASPINA_LEG5_094-2; MALASPINA_LEG5_095-2; MALASPINA_LEG5_096-2; MALASPINA_LEG5_097-2; MALASPINA_LEG5_098-2; MALASPINA_LEG5_099-2; MALASPINA_LEG6; MALASPINA_LEG6_101-2; MALASPINA_LEG6_102-2; MALASPINA_LEG6_103-2; MALASPINA_LEG6_104-2; MALASPINA_LEG6_106-2; MALASPINA_LEG6_107-2; MALASPINA_LEG6_108-2; MALASPINA_LEG6_109-2; MALASPINA_LEG6_110-2; MALASPINA_LEG6_111-2; MALASPINA_LEG6_112-2; MALASPINA_LEG6_113-2; MALASPINA_LEG6_114-2; MALASPINA_LEG6_115-2; MALASPINA_LEG6_116-2; MALASPINA_LEG6_117-2; MALASPINA_LEG6_118-2; MALASPINA_LEG6_119-2; MALASPINA_LEG6_120-2; MALASPINA_LEG6_121-2; MALASPINA_LEG6_122-2; MALASPINA_LEG6_123-2; MALASPINA_LEG6_124-2; MALASPINA_LEG6_125-2; MALASPINA_LEG7; MALASPINA_LEG7_127-2; MALASPINA_LEG7_128-2; MALASPINA_LEG7_129-2; MALASPINA_LEG7_130-2; MALASPINA_LEG7_131-2; MALASPINA_LEG7_132-2; MALASPINA_LEG7_133-2; MALASPINA_LEG7_134-2; MALASPINA_LEG7_135-2; MALASPINA_LEG7_136-2; MALASPINA_LEG7_137-2; MALASPINA_LEG7_138-2; MALASPINA_LEG7_139-2; MALASPINA_LEG7_140-2; MALASPINA_LEG7_141-2; MALASPINA_LEG7_142-2; MALASPINA_LEG7_143-2; MALASPINA_LEG7_144-2; MALASPINA_LEG7_145-2; MALASPINA_LEG7_146-2; MH005_003; MH008_006; MH009_007; MH010_008; MH011_009; MH012_010; MH013_011; MH014_012; MH015_013; MH016_014; MH017_015; MH018_016; MH019_017; MH020_018; MH021_019; MH022_020; MH023_021; MH024_022; MH025_023; MH026_024; MH027_025; MH036_027; MH037_028; MH038_029; MH039_030; MH040_031; MH041_032; MH042_033; MH043_034; MH044_035; MH046_037; MH047_038; MH049_040; MH050_041; MH051_042; MH052_043; MH053_044; MH061_045; MH062_046; MH063_047; MH064_048; MH065_049; MH066_050; MH067_051; MH072_052; MH073_053; MH074_054; MH075_055; MH076_056; MH077_057; MH078_058; MH079_059; MH080_060; MH081_061; MH082_062; MH083_063; MH084_064; MH086_066; MH087_067; MH095_069; MH096_070; MH097_071; MH098_072; MH099_073; MH100_074; MH101_075; MH103_077; MH104_078; MH124_080; MH126_082; MH127_083; MH128_084; MH129_085; MH130_086; MH131_087; MH132_088; MH134_090; MH135_091; MH136_092; MH137_093; MH138_094; MH139_095; MH140_096; MH141_097; MH142_098; MH143_099; MH150_101; MH151_102; MH152_103; MH153_104; MH155_106; MH156_107; MH157_108; MH158_109; MH159_110; MH160_111; MH161_112; MH162_113; MH163_114; MH164_115; MH165_116; MH166_117; MH167_118; MH169_120; MH170_121; MH171_122; MH172_123; MH173_124; MH174_125; MH188_127; MH189_128; MH190_129; MH191_130; MH193_131; MH194_132; MH195_133; MH196_134; MH197_135; MH198_136; MH199_137; MH200_138; MH201_139; MH202_140; MH203_141; MH204_142; MH205_143; MH206_144; MH207_145; MH208_146; North Pacific Ocean; Percentage; Prokaryotes, heterotroph; Respiration rate, oxygen; Respiration rate, oxygen, standard error; South Atlantic Ocean; South Pacific Ocean; Station label; Tasman Sea; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 3905 data points
    Location Call Number Limitation Availability
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