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  • 1
    Keywords: Hochschulschrift
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (112 Seiten = 7 MB) , Illustrationen, Graphen, Karte
    Edition: 2021
    Language: German
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  • 2
    Keywords: Hochschulschrift
    Type of Medium: Online Resource
    Pages: Online-Ressource (213 Seiten, 59 MB) , Illustrationen, Diagramme, Karten
    Language: German
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  • 3
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    Unknown
    In:  (PhD/ Doctoral thesis), Christian-Albrechts-Universität Kiel, Kiel, Germany, 213 pp
    Publication Date: 2017-09-21
    Type: Thesis , NonPeerReviewed
    Format: text
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  • 4
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    Unknown
    In:  (Diploma thesis), Christian-Albrechts-Universität Kiel, Kiel, Germany, 97 pp
    Publication Date: 2019-04-05
    Type: Thesis , NonPeerReviewed
    Format: text
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  • 5
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    Unknown
    Bundesforschungsanstalt für Fischerei
    In:  Studie im Auftrag des Bundesamtes für Naturschutz . Bundesforschungsanstalt für Fischerei, Hamburg, Germany, 82 pp.
    Publication Date: 2019-08-06
    Type: Report , NonPeerReviewed
    Format: text
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  • 6
    Publication Date: 2022-08-05
    Description: Macrorhamphosus scolopax spawns in the area around Meteor Seamount (30° N, 28° 30' W) from January until the middle of February. The first larval stages are living in the surface layer during nighttime, at daytime they stay in deeper layers. After reaching a length of about 5 mm, the larvae and smaller juveniles up to approximately 45 mm concentrate in the pleustal at daytime, at nighttime they migrate to probably 200 m depth. At a length of 40-50 mm and an age of about three months they leave the pleustal and move to the bottom. The animals on the Meteor Seamount grow to a length of 195 mm. The adults feed near the bottom, approximately a third of their food is benthic, the rest planktic. Macrorhamphosus gracilis spawns from February until the middle of March. The larvae and smaller juveniles behave like those of A1. scolopax. After leaving the pleustal, at least part of the stock stays pelagic. The adults live partly at the bottom and partly pelagic, they feed exclusively on planktonic food. On the Meteor Seamount the animals reach two years of age and a maximum length of 135 mm, which is less than in other areas.
    Type: Article , PeerReviewed
    Format: text
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  • 7
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    Bornträger
    Publication Date: 2022-08-25
    Description: The Great Meteor Seamount is situated in the subtropical NE Atlantic. The dimension of the plateau in the depth of 400m is 1465 km2 ; its lowest depth 275 m. 35 species have been caught above the plateau in 1967 and 1970 (voyages 9 c and 19; R. V. "Meteor") with a bottom trawl, the Agassiz-trawl, with BEYER's epibenthic closing net, the triangle-dredge and the chain-dredge. For comparison fishes of the same species were collected off Morocco, Mauretania and Senegal. The circular current system above the seamount and the low rates of the net transport are the reasons for the existence of the autochthonous demersal fish populations, in spite of the pelagic stages of development. A comparison of the populations of three species from the seamount and from the African shelf, using a multivariate method (linear discriminant function), indicates a genetical diverging development of the populations. An overlapping of the populations is only applicable for 1.7 % of the individuals. This argument for an autochthonus demersal fish fauna is corroborated by nearly the same composition of species in 1967 and 1970, the small differences in the dominance of the species and the great homogeneity of the fish fauna in the two years. The distribution of the species above the plateau is nearly uniform. The species Aulopus filamentosus, Phycis phycis, Macroramphosus scolopax, Anthias anthias, Antigonia capros, Capros aper, Callionymus phaeton and Arnoglossus rueppelli are characteristic for the fauna, as in 6 of 11 comparable catches these 8 species were present together. For the demersal fishes the plateau is a rather uniform biotope, for it is mainly covered with biogenic sand. The aggregations of the seamount's own plankton and nekton near the bottom in daytime is exclusively or partly the food for 94% of the fish species, while the bottom fauna is only utilized by 22% of the species. Only Callionymus phaeton feeds exclusively on bottom animals. Shrimps (predominantly Plesionika heterocarpus) are the favoured prey of the majority of fish species. Relative to the number of examined stomachs the small crustacea like ostracodes and copepods are most abundant. Fishes were found in the stomachs of 8 species. Moreover cuttle-fish are of some importance as food of the bigger fishes. A comparison of the food of respective species from the African shelf shows that the lower availability of food above the seamount has no influence on the feeding behaviour of the species. lt seems, that there is sufficient food at the seamount, so that the fishes must not put up with animals they disdain elsewhere. The fish fauna from the Great Meteor Seamount shows the greatest similarity with the demersal fish fauna of the African shelf between Gibraltar and Cap Blanc (28 species in common). The Great Meteor Seamount has only 24 species in common with Madeira and 17 with the Canary Islands. Two species suggest a possible influence of settlement from the Western Atlantic. These species also belong to the fauna of Madeira and the Josephine Seamount, while they are absent on the African shelf. The species Gnathophis codoniphorus, Callionymus sousai and probably also the ray of the genus Raja are endemic. The depth of the plateau (275-400 m) has a great influence on the composition of the fish fauna. Regarding the vertical distribution of the species in the rest of their distribution areas, the plateau of the Great Meteor Seamount is situated at the optimal depth.
    Type: Article , PeerReviewed
    Format: text
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  • 8
    Publication Date: 2023-03-03
    Keywords: CO2BaseSleipner; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Event label; Latitude of event; Longitude of event; North Sea; Pressure, water; Salinity; Temperature, water; Walther Herwig III; WH230; WH230_001; WH230_002; WH230_003; WH230_004; WH230_005; WH230_006; WH230_007; WH230_008; WH230_009; WH230_010; WH230_011; WH230_012; WH230_013; WH230_014; WH230_015; WH230_016; WH230_017; WH230_018; WH230_019; WH230_020; WH230_021; WH230_022; WH230_023; WH230_024; WH230_025; WH230_026; WH230_027; WH230_028; WH230_029; WH230_030; WH230_031; WH230_032; WH230_033; WH230_034; WH230_035; WH230_036; WH230_037; WH230_038; WH230_039; WH230_040; WH230_041; WH230_042; WH230_043; WH230_044; WH230_045; WH230_046; WH230_047; WH230_048; WH230_049; WH230_050; WH230_051; WH230_052; WH230_053; WH230_054; WH230_055; WH230_056; WH230_057; WH230_058; WH230_059; WH230_060; WH230_061; WH230_062; WH230_063; WH230_064; WH230_065; WH230_066; WH230_067; WH230_068; WH230_069; WH230_070; WH230_071; WH230_072; WH230_073; WH230_074; WH230_075; WH230_076; WH230_077; WH230_078; WH230_079; WH230_080; WH230_081; WH230_082; WH230_083; WH230_084; WH230_085; WH230_086; WH230_087; WH230_088; WH230_089; WH230_090; WH230_091; WH230_092; WH230_093; WH230_094; WH230_095; WH230_096; WH230_097; WH230_098; WH230_099; WH230_100; WH230_101; WH230_102; WH230_103; WH230_104
    Type: Dataset
    Format: text/tab-separated-values, 4777 data points
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  • 9
    Publication Date: 2023-03-03
    Keywords: CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Event label; Latitude of event; Longitude of event; North Sea; Pressure, water; Salinity; Temperature, water; Walther Herwig III; WH247; WH247_005; WH247_007; WH247_008; WH247_012; WH247_016; WH247_020; WH247_024; WH247_025; WH247_028; WH247_029; WH247_033; WH247_036; WH247_037; WH247_041; WH247_044; WH247_045; WH247_046; WH247_047
    Type: Dataset
    Format: text/tab-separated-values, 414 data points
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  • 10
    Publication Date: 2023-03-03
    Keywords: CO2BaseSleipner; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Event label; Latitude of event; Longitude of event; North Sea; Pressure, water; Salinity; Temperature, water; Walther Herwig III; WH277; WH277_001; WH277_002; WH277_003; WH277_004; WH277_005; WH277_006; WH277_007; WH277_008; WH277_009; WH277_010; WH277_011; WH277_012; WH277_013; WH277_014; WH277_015; WH277_016; WH277_017; WH277_018; WH277_019; WH277_020; WH277_021; WH277_022; WH277_023; WH277_024; WH277_025; WH277_026; WH277_027; WH277_028; WH277_029; WH277_030; WH277_031; WH277_032; WH277_033; WH277_034; WH277_035; WH277_036; WH277_037; WH277_038; WH277_039; WH277_040; WH277_041; WH277_042; WH277_043; WH277_044; WH277_045; WH277_046; WH277_047; WH277_048; WH277_049; WH277_050; WH277_051; WH277_052; WH277_053; WH277_054; WH277_055; WH277_056; WH277_057; WH277_058; WH277_059; WH277_060; WH277_061; WH277_062; WH277_063; WH277_064; WH277_065; WH277_066; WH277_067; WH277_068; WH277_069; WH277_070; WH277_071; WH277_072; WH277_073; WH277_074; WH277_075; WH277_076; WH277_077; WH277_078; WH277_079; WH277_080; WH277_081; WH277_082; WH277_083; WH277_084; WH277_085; WH277_086; WH277_087; WH277_088; WH277_089; WH277_090; WH277_091; WH277_092; WH277_093; WH277_094; WH277_095; WH277_096; WH277_097; WH277_098; WH277_099; WH277_100; WH277_101; WH277_102; WH277_103; WH277_104; WH277_105; WH277_106; WH277_107; WH277_108; WH277_109; WH277_110; WH277_111; WH277_112; WH277_113; WH277_114
    Type: Dataset
    Format: text/tab-separated-values, 5202 data points
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