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  • 2010-2014  (8)
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Keywords
Years
Year
  • 1
    Publication Date: 2012-07-30
    Print ISSN: 2572-4517
    Electronic ISSN: 2572-4525
    Topics: Geosciences
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  • 2
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Bonomo, Sergio; Grelaud, Michaël; Incarbona, Alessandro; Malinverno, Elisa; Placenti, Francesco; Bonanno, Angelo; Di Stefano, Enrico; Patti, Bernardo; Sprovieri, Mario; Genovese, Simona; Rumolo, Paola; Mazzola, Salvatore; Zgozi, Salem; Ziveri, Patrizia (2012): Living Coccolithophores from the Gulf of Sirte (Southern Mediterranean Sea) during the summer of 2008. Micropaleontology, 58(6), 487-503
    Publication Date: 2023-07-10
    Description: The Gulf of Sirte is a largely unexplored area in the southernmost Mediterranean Sea. We are presenting here 2008 summer data on the distribution pattern of living coccolithophores, a main phytoplankton calcifying group, in 105 samples from 20 stations. The survey includes coastal and offshore stations, enabling us to provide indications on the dynamics of phytoplankton productivity in relation to oceanographic processes. The total coccosphere concentrations show higher values in the offshore stations and lower ones for coastal sites. Umbellosphaera tenuis, Emiliania huxleyi, Florisphaera profunda, Syracosphaera pulchra HOL (Calyptrosphaera oblonga) and Rhabdosphaera spp. dominate the assemblages. The coccolithophore community shows the typical vertical zonation, with K-strategist taxa (among others U. tenuis, Rhabdosphaera spp. and Discosphaera tubifera) in the upper 75 meters depth and Lower Photic Zone taxa, dominated by F. profunda, below. The latter species shows its maximum development in the Deep Chlorophyll Maximum layer, which occurs in the upper part of the Levantine Intermediate Water, where the nutrient content is higher than in the overlying layers. The mesoscale oceanographic circulation significantly affects the spatial and vertical distribution of coccolithophores, with the thermocline and halocline depth shaping the vertical zonation of coccolithophore taxa and resulting in a strong lateral gradient within the gulf: in the eastern sector, under the influence of the Gulf of Sirte anticyclone, the DCM is deeper and so is the occurrence of K-strategist taxa and F. profunda.
    Keywords: Algirosphaera robusta; Bottle, Niskin; Braarudosphaera bigelowii; Calcidiscus leptoporus; Calciopappus spp.; Calciosolenia spp.; Ceratolithus cristatus; Coccoliths; Coccoliths, lower photic zone taxa; Coccoliths, upper photic zone taxa; Coronosphaera spp.; Cricosphaera spp.; DEPTH, water; Discosphaera tubifer; Elevation of event; Emiliania huxleyi; Event label; Florisphaera profunda; Fluorescence, chlorophyll; Gephyrocapsa oceanica; Gephyrocapsa spp.; Gladiolithus flabellatus; Helicosphaera carteri; Helicosphaera spp.; Holococcoliths; Latitude of event; Longitude of event; Mediterranean Sea; Mediterranean Sea Acidification in a Changing Climate; MedSeA; MedSudMed_08; MedSudMed_08_2718; MedSudMed_08_3013; MedSudMed_08_3022; MedSudMed_08_3368; MedSudMed_08_3377; MedSudMed_08_3385; MedSudMed_08_3742; MedSudMed_08_3751; MedSudMed_08_4079; MedSudMed_08_4085; MedSudMed_08_4094; MedSudMed_08_4412; MedSudMed_08_4418; MedSudMed_08_4427; MedSudMed_08_4760; MedSudMed_08_4766; MedSudMed_08_4775; MedSudMed_08_4784; MedSudMed_08_5067; MedSudMed_08_5105; Miscellaneous; NIS; Oolithotus fragilis; Oxygen; Picarola margalefi; Placoliths; Placoliths, small; Pontosphaera spp.; Rhabdosphaera spp.; Salinity; Scyphosphaera spp.; Syracosphaera spp.; Temperature, water; Thoracosphaera heimii; Umbellosphaera tenuis; Umbilicosphaera spp.; Urania
    Type: Dataset
    Format: text/tab-separated-values, 3744 data points
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  • 3
    Publication Date: 2024-02-16
    Keywords: Angeles Alvarino; Conductivity; CT; DATE/TIME; DEPTH, water; Event label; Fluorescence, chlorophyll; GEOTRACES; Global marine biogeochemical cycles of trace elements and their isotopes; LATITUDE; LONGITUDE; Mediterranean Sea; Mediterranean Sea Acidification in a Changing Climate; MedSeA; MedSeA2013/1; MedSeA2013/1-track; MedSeA2013/2; MedSeA2013/2-track; Salinity; Temperature, water; Thermosalinograph; TSG; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 13171 data points
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  • 4
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Beaufort, Luc; Probert, Ian; de Garidel-Thoron, Thibault; Bendif, E M; Ruiz-Pino, Diana; Metzi, N; Goyet, Catherine; Buchet, Noëlle; Coupel, Pierre; Grelaud, Michaël; Rost, Björn; Rickaby, Rosalind E M; De Vargas, Colomban (2011): Sensitivity of coccolithophores to carbonate chemistry and ocean acidification. Nature, 476, 80-83, https://doi.org/10.1038/nature10295
    Publication Date: 2024-03-15
    Description: About one-third of the carbon dioxide (CO2) released into the atmosphere as a result of human activity has been absorbed by the oceans, where it partitions into the constituent ions of carbonic acid. This leads to ocean acidification, one of the major threats to marine ecosystems and particularly to calcifying organisms such as corals, foraminifera and coccolithophores. Coccolithophores are abundant phytoplankton that are responsible for a large part of modern oceanic carbonate production. Culture experiments investigating the physiological response of coccolithophore calcification to increased CO2 have yielded contradictory results between and even within species. Here we quantified the calcite mass of dominant coccolithophores in the present ocean and over the past forty thousand years, and found a marked pattern of decreasing calcification with increasing partial pressure of CO2 and concomitant decreasing concentrations of CO3. Our analyses revealed that differentially calcified species and morphotypes are distributed in the ocean according to carbonate chemistry. A substantial impact on the marine carbon cycle might be expected upon extrapolation of this correlation to predicted ocean acidification in the future. However, our discovery of a heavily calcified Emiliania huxleyi morphotype in modern waters with low pH highlights the complexity of assemblage-level responses to environmental forcing factors.
    Keywords: Age, dated; Alkalinity, total; Antarctic; Aragonite saturation state; Bicarbonate ion; Calcite saturation state; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; CTD, Sea-Bird SBE 911plus; Emiliania huxleyi; Emiliania huxleyi, diameter; Emiliania huxleyi, weight; Emiliania huxleyi, weight, standard error; EPOCA; Estimated by measuring brightness in cross-polarized light (birefringence); EUR-OCEANS; European network of excellence for Ocean Ecosystems Analysis; European Project on Ocean Acidification; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Indian Ocean; LATITUDE; LONGITUDE; Measured and/or detected by SYRACO software; North Atlantic; North Pacific; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Phytoplankton; Replicates; Salinity; Sample ID; South Atlantic; South Pacific; Temperature, water; Titration potentiometric
    Type: Dataset
    Format: text/tab-separated-values, 16400 data points
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  • 5
    Publication Date: 2024-02-16
    Keywords: 10-Southern Crete; 11-Eastern Basin; 12-Nile Delta; 13-Lebanon; 14-Antikythera Strait; 15-Eastern Ionian Sea; 16-Otranto Strait; 17-Adriatic Sea; 18-Central Ionian; 19-Tyrrhenian Sea; 1-Atlantic; 20-Northern Alguero-Balear; 21-Central Alguero-Balear; 22-Catalano-Balear; 2-Gibraltar; 3-Alboran Sea; 4-Algeria; 5-Southern Alguero-Balear; 6-Strait of Sardine; 7a-Strait of Sicily; 7-Strait of Sicily; 8-Southwestern Sicily; 9-Ionian Sea; Adriatic Sea; Alboran Sea; Angeles Alvarino; Balear Sea; Bottle number; Conductivity; CTD; CTD/Rosette; CTD-RO; Date/Time of event; Density, mass density; DEPTH, water; Eastern Basin; Event label; Fluorescence, chlorophyll; GEOTRACES; Global marine biogeochemical cycles of trace elements and their isotopes; Ionian Sea; Latitude of event; Longitude of event; Mediterranean Sea Acidification in a Changing Climate; MedSeA; MedSeA2013/1; MedSeA2013/1_1; MedSeA2013/1_10; MedSeA2013/1_11; MedSeA2013/1_12; MedSeA2013/1_13; MedSeA2013/1_14; MedSeA2013/1_15; MedSeA2013/1_16; MedSeA2013/1_17; MedSeA2013/1_18; MedSeA2013/1_19; MedSeA2013/1_2; MedSeA2013/1_20; MedSeA2013/1_21; MedSeA2013/1_22; MedSeA2013/1_23; MedSeA2013/1_24; MedSeA2013/1_25; MedSeA2013/1_26; MedSeA2013/1_27; MedSeA2013/1_28; MedSeA2013/1_29; MedSeA2013/1_3; MedSeA2013/1_30; MedSeA2013/1_31; MedSeA2013/1_32; MedSeA2013/1_33; MedSeA2013/1_34; MedSeA2013/1_35; MedSeA2013/1_36; MedSeA2013/1_37; MedSeA2013/1_38; MedSeA2013/1_39; MedSeA2013/1_40; MedSeA2013/1_41; MedSeA2013/1_42; MedSeA2013/1_43; MedSeA2013/1_44; MedSeA2013/1_45; MedSeA2013/1_5; MedSeA2013/1_6; MedSeA2013/1_7; MedSeA2013/1_8; MedSeA2013/1_9; MedSeA2013/2; MedSeA2013/2_46; MedSeA2013/2_47; MedSeA2013/2_48; MedSeA2013/2_49; MedSeA2013/2_50; MedSeA2013/2_51; MedSeA2013/2_52; MedSeA2013/2_53; MedSeA2013/2_54; MedSeA2013/2_55; MedSeA2013/2_56; MedSeA2013/2_57; MedSeA2013/2_58; MedSeA2013/2_59; MedSeA2013/2_60; MedSeA2013/2_61; MedSeA2013/2_62; MedSeA2013/2_63; MedSeA2013/2_64; MedSeA2013/2_65; MedSeA2013/2_66; MedSeA2013/2_67; MedSeA2013/2_68; MedSeA2013/2_69; MedSeA2013/2_70; MedSeA2013/2_71; MedSeA2013/2_72; MedSeA2013/2_73; MedSeA2013/2_74; Optional event label; Oxygen; Oxygen sensor, SBE 43; Pressure, water; Pressure sensor, Digiquartz; Radiation, photosynthetically active; Salinity; Signal; South Atlantic Ocean; Strait of Gibraltar; Strait of Sicilia; Temperature, water; Temperature, water, potential; Tirreno Sea; Turbidity (Nephelometric turbidity unit); Western Basin
    Type: Dataset
    Format: text/tab-separated-values, 31176 data points
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  • 6
    facet.materialart.
    Unknown
    PANGAEA
    In:  Universitat Autònoma de Barcelona
    Publication Date: 2024-02-16
    Keywords: 10-Southern Crete; 11-Eastern Basin; 12-Nile Delta; 13-Lebanon; 14-Antikythera Strait; 15-Eastern Ionian Sea; 16-Otranto Strait; 17-Adriatic Sea; 18-Central Ionian; 19-Tyrrhenian Sea; 1-Atlantic; 20-Northern Alguero-Balear; 21-Central Alguero-Balear; 22-Catalano-Balear; 2-Gibraltar; 3-Alboran Sea; 4-Algeria; 5-Southern Alguero-Balear; 6-Strait of Sardine; 7a-Strait of Sicily; 7-Strait of Sicily; 8-Southwestern Sicily; 9-Ionian Sea; Adriatic Sea; Alboran Sea; Angeles Alvarino; Balear Sea; Conductivity; CTD; CTD/Rosette; CTD-RO; Date/Time of event; Density, mass density; DEPTH, water; Eastern Basin; Event label; Fluorescence, chlorophyll; GEOTRACES; Global marine biogeochemical cycles of trace elements and their isotopes; Ionian Sea; Latitude of event; Longitude of event; Mediterranean Sea Acidification in a Changing Climate; MedSeA; MedSeA2013/1; MedSeA2013/1_1; MedSeA2013/1_10; MedSeA2013/1_11; MedSeA2013/1_12; MedSeA2013/1_13; MedSeA2013/1_14; MedSeA2013/1_15; MedSeA2013/1_16; MedSeA2013/1_17; MedSeA2013/1_18; MedSeA2013/1_19; MedSeA2013/1_2; MedSeA2013/1_20; MedSeA2013/1_21; MedSeA2013/1_22; MedSeA2013/1_23; MedSeA2013/1_24; MedSeA2013/1_25; MedSeA2013/1_26; MedSeA2013/1_27; MedSeA2013/1_28; MedSeA2013/1_29; MedSeA2013/1_3; MedSeA2013/1_30; MedSeA2013/1_31; MedSeA2013/1_32; MedSeA2013/1_33; MedSeA2013/1_34; MedSeA2013/1_35; MedSeA2013/1_36; MedSeA2013/1_37; MedSeA2013/1_38; MedSeA2013/1_39; MedSeA2013/1_4; MedSeA2013/1_40; MedSeA2013/1_41; MedSeA2013/1_42; MedSeA2013/1_43; MedSeA2013/1_44; MedSeA2013/1_45; MedSeA2013/1_5; MedSeA2013/1_6; MedSeA2013/1_7; MedSeA2013/1_8; MedSeA2013/1_9; MedSeA2013/2; MedSeA2013/2_46; MedSeA2013/2_47; MedSeA2013/2_48; MedSeA2013/2_49; MedSeA2013/2_50; MedSeA2013/2_51; MedSeA2013/2_52; MedSeA2013/2_53; MedSeA2013/2_54; MedSeA2013/2_55; MedSeA2013/2_56; MedSeA2013/2_57; MedSeA2013/2_58; MedSeA2013/2_59; MedSeA2013/2_60; MedSeA2013/2_61; MedSeA2013/2_62; MedSeA2013/2_63; MedSeA2013/2_64; MedSeA2013/2_65; MedSeA2013/2_66; MedSeA2013/2_67; MedSeA2013/2_68; MedSeA2013/2_69; MedSeA2013/2_70; MedSeA2013/2_71; MedSeA2013/2_72; MedSeA2013/2_73; MedSeA2013/2_74; Optional event label; Oxygen; Oxygen sensor, SBE 43; Pressure, water; Pressure sensor, Digiquartz; Radiation, photosynthetically active; Salinity; Signal; South Atlantic Ocean; Strait of Gibraltar; Strait of Sicilia; Temperature, water; Temperature, water, potential; Tirreno Sea; Turbidity (Nephelometric turbidity unit); Western Basin
    Type: Dataset
    Format: text/tab-separated-values, 220597 data points
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  • 7
    Publication Date: 2024-02-02
    Keywords: 101; 107; 111; 116; 118; 560; 561; 562; 563; 564; 565; 566; 569; 570; 571; 573; 574; 575; 576; 577; 578; 579; 580; 590; 594; 596; 601; 602; 604; 80; 82; AB12MC; BANSIC-ST103; BANSIC-ST120; BANSIC-ST123; BANSIC-ST1270; BANSIC-ST136; BANSIC-ST139; BANSIC-ST1420; BANSIC-ST1426; BANSIC-ST1429; BANSIC-ST143; BANSIC-ST1431; BANSIC-ST1558; BANSIC-ST1567; BANSIC-ST160; BANSIC-ST167; BANSIC-ST170; BANSIC-ST1711; BANSIC-ST172; BANSIC-ST180; BANSIC-ST184; BANSIC-ST1846; BANSIC-ST1852; BANSIC-ST1855; BANSIC-ST188; BANSIC-ST199; BANSIC-ST213; BANSIC-ST2134; BANSIC-ST2140; BANSIC-ST2287; BANSIC-ST2422; BANSIC-ST2575; BANSIC-ST270; BANSIC-ST272; BANSIC-ST275; BANSIC-ST278; BANSIC-ST282; BANSIC-ST285; BANSIC-ST292; BANSIC-ST296; BANSIC-ST342; BANSIC-ST386; BANSIC-ST403; BANSIC-ST407; BANSIC-ST44; BANSIC-ST440; BANSIC-ST446; BANSIC-ST450; BANSIC-ST453; BANSIC-ST513; BANSIC-ST517; BANSIC-ST521; BANSIC-ST581; BANSIC-ST611; BANSIC-ST617; BANSIC-ST621; BANSIC-ST64; BANSIC-ST67; BANSIC-ST70; BANSIC-ST74; BANSIC-ST806; BANSIC-ST81; BANSIC-ST864; BANSIC-ST89; BANSIC-ST991; BANSIC-ST994; Chlorophyll a; Comment; Cyprus; DEPTH, sediment/rock; Eastern Mediterranean, Continental slope off Israel; Elevation of event; Eratosthenes Seamount; Event label; Florisphaera profunda; GeoB7704-1; GeoB7705-1; GeoB7714-1; GeoB7718-1; GeoB7720-1; GeoB7723-2; GeoB7725-2; Greece; Latitude of event; Le Noroit; Longitude of event; Lybia; M40/4; M40/4_MUC65; M40/4_MUC66; M40/4_MUC68; M40/4_MUC70; M40/4_MUC71; M40/4_MUC74; M40/4_MUC75; M40/4_MUC76-1; M40/4_MUC77A; M40/4_MUC87; M51/3; M51/3_560-1; M51/3_561-4; M51/3_562-5; M51/3_563-5; M51/3_564-2; M51/3_565-1; M51/3_566-3; M51/3_569-3; M51/3_570-2; M51/3_571; M51/3_573; M51/3_574-2; M51/3_575-6; M51/3_576-3; M51/3_577-1; M51/3_578; M51/3_579; M51/3_580; M51/3_590; M51/3_594; M51/3_596; M51/3_601-3; M51/3_602; M51/3_604; M52/2; Malta; MCAT01; Mediterranean Sea; Mediterranean Sea Acidification in a Changing Climate; MedSeA; Meteor (1986); MUC; MultiCorer; Nile Fan; Reference/source; SIN97-BC02; SIN97-BC03; SIN97-BC06; SIN97-BC07; SIN97-BC09; SINSAP-98; SINSAP98-BCAP1-2; SINSAP98-BCI0-1; SINSAP98-BCI01-2; Turkey; Urania; VICOMED_I; VICOMED_I-ANA; VICOMED_II; VICOMED_II-CRE; VICOMED_II-KHA; VICOMED_I-ION; VICOMED_II-PAN; VICOMED_I-MAL; VICOMED_I-RHO; VICOMED_I-YOS; Zyprus
    Type: Dataset
    Format: text/tab-separated-values, 355 data points
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  • 8
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Horigome, Mariana Tatsumi; Ziveri, Patrizia; Grelaud, Michaël; Baumann, Karl-Heinz; Marino, Gianluca; Mortyn, P G (2014): Environmental controls on the Emiliania huxleyi calcite mass. Biogeosciences, 11(8), 2295-2308, https://doi.org/10.5194/bg-11-2295-2014
    Publication Date: 2024-03-15
    Description: Although ocean acidification is expected to impact (bio)calcification by decreasing the seawater carbonate ion concentration, [CO3]2-, there exists evidence of non-uniform response of marine calcifying plankton to low seawater [CO3]2-. This raises questions on the role of environmental factors other than acidification and on the complex physiological responses behind calcification. Here we investigate the synergistic effect of multiple environmental parameters, including temperature, nutrient (nitrate and phosphate) availability, and seawater carbonate chemistry on the coccolith calcite mass of the cosmopolitan coccolithophore Emiliania huxleyi, the most abundant species in the world ocean. We use a suite of surface (late Holocene) sediment samples from the South Atlantic and southwestern Indian Ocean taken from depths lying well above the modern lysocline. The coccolith calcite mass in our results presents a latitudinal distribution pattern that mimics the main oceanographic features, thereby pointing to the potential importance of phosphorus and temperature in determining coccolith mass by affecting primary calcification and possibly driving the E. huxleyi morphotype distribution. This evidence does not necessarily argue against the potentially important role of the rapidly changing seawater carbonate chemistry in the future, when unabated fossil fuel burning will likely perturb ocean chemistry beyond a critical point. Rather our study highlights the importance of evaluating the combined effect of several environmental stressors on calcifying organisms to project their physiological response(s) in a high CO2 world and improve interpretation of paleorecords.
    Keywords: 06MT41_3; Age, maximum/old; Agulhas Basin; Agulhas Current; Alkalinity, total; Angola Basin; ANT-XI/4; Aragonite saturation state; Bicarbonate ion; Brazil Basin; Calcification/Dissolution; Calcite saturation state; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); CALYPSO; Calypso Corer; Cape Basin; Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; CD154; CD154-01-1K; CD154-02-3K; CD154-03-5K; CD154-04-6K; CD154-05-7K; CD154-07-7PK; CD154-09-9K; CD154-10-10K; CD154-15-13K; CD154-15-14K; CD154-16-15K; CD154-17-17K; CD154-18-18K; CD154-20-20K; CD154-23-24K; CD154-24-25K; Central South Atlantic; Charles Darwin; Chlorophyll a, interpolated; Chromista; Cluster type; Conrad Rise; East Brazil Basin; Emiliania huxleyi; Estimated by measuring brightness in cross-polarized light (birefringence); Event label; Field observation; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); GeoB1112-3; GeoB1203-2; GeoB1208-1; GeoB1217-1; GeoB1403-2; GeoB1405-7; GeoB1413-2; GeoB1414-2; GeoB1415-1; GeoB1417-1; GeoB1418-1; GeoB1419-1; GeoB1420-1; GeoB1901-1; GeoB1902-3; GeoB1903-1; GeoB1904-1; GeoB1905-1; GeoB1906-1; GeoB1907-1; GeoB2213-1; GeoB5112-5; GeoB5115-2; GeoB5121-2; GeoB5130-1; GeoB5134-1; GeoB5136-2; GeoB5137-1; GeoB5140-3; GeoB6402-9; GeoB6403-4; GeoB6406-1; GeoB6410-1; GeoB6411-4; GeoB6412-1; GeoB6417-2; GeoB6418-3; GeoB6419-1; GeoB6421-2; GeoB6425-1; GeoB6429-1; Giant box corer; GIK17836-1; GIK17843-1; GIK17851-1; GIK17862-1; GIK17866-1; GIK17884-1; GKG; Gravity corer (Kiel type); Guinea Basin; Haptophyta; Hierarchical cluster analysis (HCA); Indian-Antarctic Ridge; Indian Ocean; KAL; Kasten corer; Length; M12/1; M16/1; M23/3; M41/3; M46/4; M9/4; Marion Dufresne (1995); Mass; Mass, standard deviation; MD02-2594; MD128; Mediterranean Sea Acidification in a Changing Climate; MedSeA; Meteor (1986); MIC; Mid Atlantic Ridge; MiniCorer; MUC; MultiCorer; Nitrate, in water, interpolated; Northern Guinea Basin; OA-ICC; Ocean Acidification International Coordination Centre; Open ocean; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Pelagos; pH; Phosphate, in water, interpolated; Phytoplankton; Polarstern; PS2557-2; PS2558-1; PS2560-3; PS2561-1; PS2563-3; PS2565-2; PS2568-3; PS2569-1; PS2570-1; PS2606-3; PS2610-1; PS2611-2; PS30; PS30/004; PS30/013; PS30/023; PS30/030; PS30/043; PS30/051; PS30/104; PS30/105; PS30/106; PS30/144; PS30/155; PS30/156; Salinity, interpolated; Sample code/label; Sedimentation rate; Single species; SL; SO84; Sonne; South Atlantic; Southern Ocean; South Indian Ridge, South Indian Ocean; Species; ST. HELENA HOTSPOT; SWAF; Temperate; Temperature, water, interpolated; Tropical; Walvis Ridge; West Angola Basin; Width
    Type: Dataset
    Format: text/tab-separated-values, 3410 data points
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