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  • 1
    Book
    Book
    Copenhagen : Internat. Council for the Exploration of the Sea
    Associated volumes
    Keywords: Zooplankton
    In: 2010/11
    Type of Medium: Book
    Pages: 208 S , Ill., graph. Darst.
    ISBN: 9788774821250
    Series Statement: ICES cooperative research report 318
    Language: English
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  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Polar research 10 (1991), S. 0 
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: Sagitta elegans var. arctica, the dominant and locally abundant chaetognath in the Barents sea, was collected from the upper 50 m in Arctic water masses during an ice edge bloom in early summer 1983. In situ sampling was made along a transect at discrete depths with a 375 μm mesh net mounted on a plankton pump. Prey composition and feeding rate were estimated from gut content analyses on preserved specimens combined with data on digestion times from previous studies. No diel variations were found in feeding activity. The diet reflected the composition of available prey in the zooplankton and consisted mainly of nauplii, small copepods (early stages of Calanus, Pseudocalanus, Oithona) and appendicularians. Prey usually occurred as a single item in the gut.Mean prey body width related to chaetognath head width yielded a power curve, with a large amount of scatter, showing that chaetognaths in the Barents Sea can use a wide spectrum of prey sizes. Similarly, maximum prey body width was related to chaetognath head width as a power curve, reflecting the existence of an upper prey size limitation due to the chaetognath mouth size. The highest abundance of S. elegans (5 specimens m−3), and the most intense feeding activity, were found within or beneath the maximum zooplankton biomass. Further, distribution and feeding were affected by light intensity, salinity, and the population structure of 5. elegans var. arctica.Estimated feeding rates ranged between 0.30 and 1.05 prey items per chaetognath day−1. This corresponds to an ingestion of 8-54 μg AFDW day−1, and a consumption of 0.08–0.22% of the zooplankton standing stock day−1. From these rates, the calculated yearly ingestion by S. elegans var. arctica was 3% of the annually secondary production.
    Type of Medium: Electronic Resource
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  • 3
    Publication Date: 2024-02-17
    Description: Mesopelagic organisms play a critical role in marine ecosystems, channelling energy and organic matter across food webs and serving as the primary prey for many open-ocean predators. Nevertheless, trophic pathways involving mesopelagic organisms are poorly understood and their contribution to food web structure remains difficult to assess (St. John et al., 2016). Existing data to assess mesopelagic feeding interactions and energy transfer are scattered in the literature or remain unpublished, making it difficult to locate and use such datasets. As part of the EU funded project SUMMER - Sustainable Management of Mesopelagic Resources H2020-BG-2018-2, GA: 817806) (https://summerh2020.eu/), we created MesopTroph, a georeferenced database of diet, trophic biogeochemical markers, and energy content of mesopelagic organisms and other marine taxa from the Northeast Atlantic and Mediterranean Sea, compiled from 191 published and non-published sources. MesopTroph includes seven datasets: (i) diet compositions from stomach content analysis, (ii) stable isotopes of carbon and nitrogen (δ13C and δ15N), (iii) fatty acid trophic markers (FATM), (iv) major and trace elements, (v) energy density, (vi) estimates of diet proportions, and (vii) trophic positions. The database contains information from 4918 samples, representing 51119 specimens from 499 species or genera, covering a wide range of trophic guilds and taxonomic groups. Metadata provided for each record include the location, dates and method of sample collection, taxonomic ranks (phylum, class, order, family), number and size (or size range) of sampled organisms, method/model used in data analysis, reference and DOI of the original data source. Compiled data were checked for errors, missing information, and to avoid duplicate entries, and scientific names and taxonomy were standardized.
    Keywords: diet composition; diet proportions; energy density; fatty acids; major and trace element data; Mediterranean; megafauna; mesopelagic food web; mesopelagic organisms; North Atlantic; Stable isotopes; Stomach contents; SUMMER; Sustainable Management of Mesopelagic Resources; trophic markers; trophic position
    Type: Dataset
    Format: application/zip, 7 datasets
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  • 4
    Publication Date: 2024-03-02
    Description: Stomach contents analysis is a standard dietary assessment method that potentially enables quantifying diet components with high taxonomic resolution. We compiled diet compositions from stomach content analysis from 75 unique species or genera: 32 fish, 19 marine mammals, 14 elasmobranchs, 9 seabirds and one marine turtle. Data were gathered from 89 published sources that included samples collected between 1885 and 2016 throughout the central and Northeast Atlantic, and the Mediterranean Sea. When available, we reported the percentage number of individuals of a prey type as a proportion of the total number of prey items (%N), the proportion of a prey item by weight (%W), and the proportion of stomachs containing a particular prey item (i.e. percent frequency of occurrence, %F). For each data record, we also provided the sampling location, geographic coordinates, month and year of sample collection, method of sample collection, taxonomic ranks (phylum, class, order, family), number and size (or size range) of sampled organisms, as well as the reference and DOI of the original data source, for further details on the samples analysed and/or the analytical techniques used.
    Keywords: Adriatic_Sea_comp; Azores_comp; Azores-Iberian_Peninsula_comp; Azores-Madeira-Galicia_comp; Balearic_Sea_comp; Baltic_Sea_comp; bathypelagic fish; Bay_of_Biscay_comp; Bay_of_Biscay_western_Channel_comp; Bay_of_Malaga_comp; Bear_Island_comp; Canary_Islands_comp; Cariaco_Trench_Caribbean_Sea_comp; Catalonian_Sea_comp; Charlie-Gibbs_Fracture_comp; Class; Coast_of_Finmark_comp; Coast_of_Kola_comp; Comment; Danois_Bank_Cantabria_Bay_Biscay_comp; Denmark_comp; DEPTH, water; diet composition; elasmobranchs; England_western_channel_comp; Event label; Family; Faraday_Seamount_comp; Faroe_Islands_comp; Faroe_Shetland_Islands_comp; France_comp; Galicia_comp; Gear; Greece_comp; Gulf_of_Cadiz_comp; Gulf_of_Lions_comp; Hyeres_archipelago_comp; Iceland_comp; Ionian_Sea_comp; Ireland_comp; large pelagic fish; LATITUDE; Levantine_Sea_comp; Location; Lofoten_Vesteralen_comp; LONGITUDE; Madeira_comp; marine mammals; marine turtles; Mauritania_Cape_Verde_comp; mesopelagic fish; mesopelagic food web; Mid-Atlantic_Bight_comp; Month; Netherlands_comp; North_Sea_comp; Northeast_Atlantic_comp; Number of individuals; Number of prey; Occurrence; Ocean and sea region; Order; Organisms; pelagic fish; Persistent Identifier; Phylum; Portugal_comp; Prey, mass; Prey taxa; Record number; Reference/source; Replicates; Reykjanes_Ridge_comp; Sample ID; Scotland_comp; Seabirds; Size; Southwest_Ireland_comp; Spain_comp; stomach content analysis; Strait_of_Gibraltar_comp; Strait_of_Messina_comp; Strait_of_Sicily-Gulf_of_Gabes_comp; SUMMER; Sustainable Management of Mesopelagic Resources; Taxon/taxa; Taxon/taxa, unique identification; Taxon/taxa, unique identification (Semantic URI); Taxon/taxa, unique identification (URI); Tyrrhenian_Sea_comp; West_of_Spitsbergen_comp; Year of observation
    Type: Dataset
    Format: text/tab-separated-values, 283941 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Melle, Webjørn; Runge, Jeffrey A; Head, Erica J H; Plourde, Stéphane; Castellani, Claudia; Licandro, Priscilla; Pierson, James; Jónasdóttir, Sigrún Huld; Johnson, C; Broms, Cecilie; Debes, Høgni; Falkenhaug, Tone; Gaard, Eilif; Gislason, Astthor; Heath, Michael R; Niehoff, Barbara; Nielsen, Torkel Gissel; Pepin, Pierre; Stenevik, Erling Kaare; Chust, Guillem (2015): Biogeography of key mesozooplankton species in the North Atlantic and egg production of Calanus finmarchicus. Earth System Science Data, 7(2), 223-230, https://doi.org/10.5194/essd-7-223-2015
    Publication Date: 2024-05-28
    Description: Here we present a new, pan-North-Atlantic compilation of data on key mesozooplankton species, including the most important copepod, Calanus finmarchicus. Distributional data of eight representative zooplankton taxa, from recent (2000-2009) Continuous Plankton Recorder data, are presented, along with basin-scale data of the phytoplankton colour index. Then we present a compilation of data on C. finmarchicus, including observations of abundance, demography, egg production and female size, with accompanying data on temperature and chlorophyll. . This is a contribution by Canadian, European and US scientists and their institutions.
    Keywords: Basin Scale Analysis, Synthesis and Integration; EURO-BASIN
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 6
    Publication Date: 2024-05-28
    Keywords: Arendal_st_2; AZMP_Anticosti_Gyre; AZMP_Gaspe_Current; AZMP_Rimouski_Station; AZMP_Station_27; AZMP_Station_Halifax_2; Basin Scale Analysis, Synthesis and Integration; BONGO; Bongo net; Central_Labrador_Sea; Central Norwegian Sea; Depth, bottom/max; Depth, top/min; Eastern_Labrador_Sea; Eastern Norwegian Sea; EURO-BASIN; Event label; Faroe_Shelf_station_; Faroese Shelf; Faroe-Shetland Channel; Foinaven; Gulf of Maine; Labrador_Shelf; Labrador_Slope; Labrador Sea; Labrador shelf; Labrador slope; Langanes_NA; Latitude of event; Longitude of event; MSN; Multiple opening/closing net; Murchinson; Newfoundland Shelf; Northeastern Iceland; Northern Iceland; Northern Norwegian Shelf; North Sea; North Sea, Scotland Shelf; Northwest Gulf of St. Lawrence; Ring net; RN; Saltenfjorden; Sampling date; Scotian Shelf; Siglunes_section; Southern Iceland; Southern Norway Shelf; St. Lawrence Estuary, lower; Stonehaven; Svinoy_section_Arctic; Svinoy_section_Atlantic; Svinoy_section_coastal; Temperature, water; Vestmannaeyjar; Weather_Station_Mike; West_Greenland_shelf; West Greenland; Wilkinson_Basin; WP2; WP-2 towed closing plankton net
    Type: Dataset
    Format: text/tab-separated-values, 2679 data points
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  • 7
    Publication Date: 2024-05-28
    Keywords: Arendal_st_2; AZMP_Anticosti_Gyre; AZMP_Gaspe_Current; AZMP_Rimouski_Station; AZMP_Station_27; AZMP_Station_Halifax_2; Basin Scale Analysis, Synthesis and Integration; BONGO; Bongo net; Calanus finmarchicus, c1; Calanus finmarchicus, c2; Calanus finmarchicus, c3; Calanus finmarchicus, c4; Calanus finmarchicus, c5; Calanus finmarchicus, female; Calanus finmarchicus, male; Central_Labrador_Sea; Central Norwegian Sea; Depth, bottom/max; Depth, top/min; Eastern_Labrador_Sea; Eastern Norwegian Sea; EURO-BASIN; Event label; Faroe_Shelf_station_; Faroese Shelf; Faroe-Shetland Channel; Foinaven; Gulf of Maine; Labrador_Shelf; Labrador_Slope; Labrador Sea; Labrador shelf; Labrador slope; Langanes_NA; Latitude of event; Longitude of event; MSN; Multiple opening/closing net; Murchinson; Newfoundland Shelf; Northeastern Iceland; Northern Iceland; Northern Norwegian Shelf; North Sea; North Sea, Scotland Shelf; Northwest Gulf of St. Lawrence; Ring net; RN; Saltenfjorden; Sampling date; Scotian Shelf; Siglunes_section; Southern Iceland; Southern Norway Shelf; St. Lawrence Estuary, lower; Stonehaven; Svinoy_section_Arctic; Svinoy_section_Atlantic; Svinoy_section_coastal; Vestmannaeyjar; Weather_Station_Mike; West_Greenland_shelf; West Greenland; Wilkinson_Basin; WP2; WP-2 towed closing plankton net
    Type: Dataset
    Format: text/tab-separated-values, 5167 data points
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  • 8
    Publication Date: 2017-12-19
    Description: Highlights: • The Subpolar Front is distinct along its northern edge but to the south it forms a more diffuse zone. • North-south water-mass hydrography is strongest down to depths of 500–800 m. • The frontal biogeographic signature is strong near the surface but decreases with greater depth. • This strong surface feature is therefore not a good predictor of deep pelagic biogeography. Broad-scale patterns in the distribution of deep-sea pelagic species and communities are poorly known. An important question is whether biogeographic boundaries identified from surface features are important in the deep mesopelagic and bathypelagic. We present community analyses of discrete-depth samples of mesozooplankton and micronekton to full-ocean depth collected in the area where the Mid-Atlantic Ridge is crossed by the Subpolar Front. The results show that the distributional discontinuity associated with the front, which is strong near the surface, decreases with increasing depth. Both the frontal separation near the surface and the community convergence at increasing depths were clearer for mesozooplankton than for micronekton
    Type: Article , PeerReviewed
    Format: text
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  • 9
    Publication Date: 2022-01-21
    Description: Aim: Invasive species are of increasing global concern. Nevertheless, the mechanisms driving further distribution after the initial establishment of non‐native species remain largely unresolved, especially in marine systems. Ocean currents can be a major driver governing range occupancy, but this has not been accounted for in most invasion ecology studies so far. We investigate how well initial establishment areas are interconnected to later occupancy regions to test for the potential role of ocean currents driving secondary spread dynamics in order to infer invasion corridors and the source–sink dynamics of a non‐native holoplanktonic biological probe species on a continental scale. Location: Western Eurasia. Time period: 1980s–2016. Major taxa studied: ‘Comb jelly’ Mnemiopsis leidyi. Methods: Based on 12,400 geo‐referenced occurrence data, we reconstruct the invasion history of M. leidyi in western Eurasia. We model ocean currents and calculate their stability to match the temporal and spatial spread dynamics with large‐scale connectivity patterns via ocean currents. Additionally, genetic markers are used to test the predicted connectivity between subpopulations. Results: Ocean currents can explain secondary spread dynamics, matching observed range expansions and the timing of first occurrence of our holoplanktonic non‐native biological probe species, leading to invasion corridors in western Eurasia. In northern Europe, regional extinctions after cold winters were followed by rapid recolonizations at a speed of up to 2,000 km per season. Source areas hosting year‐round populations in highly interconnected regions can re‐seed genotypes over large distances after local extinctions. Main conclusions: Although the release of ballast water from container ships may contribute to the dispersal of non‐native species, our results highlight the importance of ocean currents driving secondary spread dynamics. Highly interconnected areas hosting invasive species are crucial for secondary spread dynamics on a continental scale. Invasion risk assessments should consider large‐scale connectivity patterns and the potential source regions of non‐native marine species.
    Type: Article , PeerReviewed
    Format: text
    Format: text
    Format: other
    Format: text
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  • 10
    Publication Date: 2021-06-19
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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