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  • 1
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    PANGAEA
    In:  The Centre for Environment Fisheries and Aquaculture Science, Lowestoft | Supplement to: Pinnegar, John Keith; Goñi, Nicolas; Trenkel, Verena M; Arrizabalaga, Haritz; Melle, Webjørn; Keating, James; Óskarsson, Guomundur J (2015): A new compilation of stomach content data for commercially important pelagic fish species in the northeast Atlantic. Earth System Science Data, 7(1), 19-28, https://doi.org/10.5194/essd-7-19-2015
    Publication Date: 2023-03-07
    Description: Fish stomach content records extracted from the DAPSTOM 4.5 database (held at the UK Centre for Environment, Fisheries and Aquaculture Science - CEFAS). Data collated as part of the EU Euro-Basin project and specifically concerning herring (Clupea harengus), mackerel (Scomber scombrus), blue whiting (Micromesistius poutassou), albacore (Thunnus alalunga) and bluefin tuna (Thunnus thynnus). The data set consist of 20720 records - collected throughout the northeast Atlantic, between 1906 and 2011 - mostly during routine fisheries monitoring research cruises.
    Keywords: Basin Scale Analysis, Synthesis and Integration; Beach seine; BEAM; Beam trawl; Biscay; ICES Retangle = 16E6; sub-area = VIII; division = VIIIc; Biscay; ICES Retangle = 16E7; sub-area = VIII; division = VIIId; Biscay; ICES Retangle = 17E7; sub-area = VIII; division = VIIId; Biscay; ICES Retangle = 18E7; sub-area = VIII; division = VIIId; Biscay; ICES Retangle = 19E7; sub-area = VIII; division = VIIId; Biscay; ICES Retangle = 20E6; sub-area = VIII; division = VIIIb; Biscay; ICES Retangle = 20E6; sub-area = VIII; division = VIIId; Biscay; ICES Retangle = 21E6; sub-area = VIII; division = VIIIa; Biscay; ICES Retangle = 21E6; sub-area = VIII; division = VIIId; Biscay; ICES Retangle = 21E7; sub-area = VIII; division = VIIId; Biscay; ICES Retangle = 22E5; sub-area = VIII; division = VIIIa; Biscay; ICES Retangle = 22E6; sub-area = VIII; division = VIIIa; Biscay; ICES Retangle = 22E6; sub-area = VIII; division = VIIId; Biscay; ICES Retangle = 23E2; sub-area = VIII; division = VIIIa; Biscay; ICES Retangle = 23E3; sub-area = VIII; division = VIIId; Biscay; ICES Retangle = 23E4; sub-area = VIII; division = VIIIa; Biscay; ICES Retangle = 23E6; sub-area = VIII; division = VIIIa; Biscay; ICES Retangle = 24E2; sub-area = VIII; division = VIIIa; Biscay; ICES Retangle = 24E4; sub-area = VIII; division = VIIIa; Biscay; ICES Retangle = 24E5; sub-area = VIII; division = VIIIa; BSE; BULLEN-1906-64; BULLEN-1906-65; BULLEN-1906-66; BULLEN-1906-67; BULLEN-1906-68; BULLEN-1906-69; BULLEN-1906-70; BULLEN-1906-71; BULLEN-1906-72; BULLEN-1906-73; BULLEN-1906-74; BULLEN-1906-75; BULLEN-1907-100; BULLEN-1907-101; BULLEN-1907-102; BULLEN-1907-103; BULLEN-1907-104; BULLEN-1907-105; BULLEN-1907-106; BULLEN-1907-107; BULLEN-1907-108; BULLEN-1907-109; BULLEN-1907-110; BULLEN-1907-111; BULLEN-1907-112; BULLEN-1907-114; BULLEN-1907-115; BULLEN-1907-116; BULLEN-1907-117; BULLEN-1907-118; BULLEN-1907-119; BULLEN-1907-120; BULLEN-1907-121; BULLEN-1907-122; BULLEN-1907-123; BULLEN-1907-124; BULLEN-1907-125; BULLEN-1907-126; BULLEN-1907-127; BULLEN-1907-128; BULLEN-1907-129; BULLEN-1907-130; BULLEN-1907-131; BULLEN-1907-132; BULLEN-1907-133; BULLEN-1907-134; BULLEN-1907-135; BULLEN-1907-136; BULLEN-1907-137; BULLEN-1907-138; BULLEN-1907-139; BULLEN-1907-140; BULLEN-1907-141; BULLEN-1907-76; BULLEN-1907-77; BULLEN-1907-78; BULLEN-1907-79; BULLEN-1907-80; BULLEN-1907-81; BULLEN-1907-82; BULLEN-1907-83; BULLEN-1907-84; BULLEN-1907-85; BULLEN-1907-86; BULLEN-1907-88; BULLEN-1907-89; BULLEN-1907-90; BULLEN-1907-91; BULLEN-1907-92; BULLEN-1907-93; BULLEN-1907-94; BULLEN-1907-95; BULLEN-1907-96; BULLEN-1907-97; BULLEN-1907-98; BULLEN-1907-99; Celtic Sea; ICES Retangle = 25E0; sub-area = VII; division = VIIj; Celtic Sea; ICES Retangle = 25E1; sub-area = VII; division = VIIh; Celtic Sea; ICES Retangle = 25E2; sub-area = VII; division = VIIh; Celtic Sea; ICES Retangle = 25E3; sub-area = VII; division = VIIh; Celtic Sea; ICES Retangle = 26E1; sub-area = VII; division = VIIh; Celtic Sea; ICES Retangle = 27D9; sub-area = VII; division = VIIj; Celtic Sea; ICES Retangle = 27E0; sub-area = VII; division = VIIj; Celtic Sea; ICES Retangle = 27E1; sub-area = VII; division = VIIh; Celtic Sea; ICES Retangle = 27E2; sub-area = VII; division = VIIh; Celtic Sea; ICES Retangle = 27E3; sub-area = VII; division = VIIh; Celtic Sea; ICES Retangle = 27E4; sub-area = VII; division = VIIh; Celtic Sea; ICES Retangle = 28D8; sub-area = VII; division = VIIj; Celtic Sea; ICES Retangle = 28D9; sub-area = VII; division = VIIj; Celtic Sea; ICES Retangle = 28E0; sub-area = VII; division = VIIj; Celtic Sea; ICES Retangle = 28E2; sub-area = VII; division = VIIh; Celtic Sea; ICES Retangle = 29D8; sub-area = VII; division = VIIj; Celtic Sea; ICES Retangle = 29D9; sub-area = VII; division = VIIj; Celtic Sea; ICES Retangle = 29E1; sub-area = VII; division = VIIg; Celtic Sea; ICES Retangle = 29E2; sub-area = VII; division = VIIg; Celtic Sea; ICES Retangle = 30D9; sub-area = VII; division = VIIj; Celtic Sea; ICES Retangle = 30E0; sub-area = VII; division = VIIj; Celtic Sea; ICES Retangle = 30E2; sub-area = VII; division = VIIg; Celtic Sea; ICES Retangle = 30E3; sub-area = VII; division = VIIg; Celtic Sea; ICES Retangle = 30E4; sub-area = VII; division = VIIf; Celtic Sea; ICES Retangle = 31D8; sub-area = VII; division = VIIj; Celtic Sea; ICES Retangle = 31D9; sub-area = VII; division = VIIj; Celtic Sea; ICES Retangle = 31E0; sub-area = VII; division = VIIj; Celtic Sea; ICES Retangle = 31E2; sub-area = VII; division = VIIg; Celtic Sea; ICES Retangle = 31E3; sub-area = VII; division = VIIg; Celtic Sea; ICES Retangle = 31E4; sub-area = VII; division = VIIg; Celtic Sea; ICES Retangle = 31E5; sub-area = VII; division = VIIf; Celtic Sea; ICES Retangle = 32D8; sub-area = VII; division = VIIj; Celtic Sea; ICES Retangle = 32D9; sub-area = VII; division = VIIj; Celtic Sea; ICES Retangle = 32E3; sub-area = VII; division = VIIg; Celtic Sea; ICES Retangle = 32E4; sub-area = VII; division = VIIg; Celtic Sea; ICES Retangle = 33D8; sub-area = VII; division = VIIj; CEND02-09-10; CEND02-09-12; CEND02-09-13; CEND02-09-14; CEND02-09-16; CEND02-09-17; CEND02-09-18; CEND02-09-22; CEND02-09-24; CEND02-09-25; CEND02-09-28; CEND02-09-38; CEND02-09-51; CEND02-09-9; CEND-04-10-1; CEND-04-10-105; CEND-04-10-106; CEND-04-10-107; CEND-04-10-13; CEND-04-10-14; CEND-04-10-15; CEND-04-10-17; CEND-04-10-2; CEND-04-10-24; CEND-04-10-25; CEND-04-10-26; CEND-04-10-27; CEND-04-10-34; CEND-04-10-35; CEND-04-10-36; CEND-04-10-37; CEND-04-10-4; CEND-04-10-43; CEND-04-10-44; CEND-04-10-45; CEND-04-10-46; CEND-04-10-47; CEND-04-10-5; CEND-04-10-53; CEND-04-10-55; CEND-04-10-56; CEND-04-10-57; CEND-04-10-59; CEND-04-10-6; CEND-04-10-60; CEND-04-10-61; CEND-04-10-69; CEND-04-10-7; CEND-04-10-70; CEND-04-10-71; CEND-04-10-72; CEND-04-10-73; CEND-04-10-79; CEND-04-10-8; CEND-04-10-80; CEND-04-10-81; CEND-04-10-84; CEND-04-10-87; CEND-04-10-88; CEND-04-10-89; CEND-04-10-9; CEND-04-10-94; CEND-04-10-95; CEND-04-10-96; CEND-04-10-97; CEND-04-10-98; CEND-04-11-1; CEND-04-11-11; CEND-04-11-12; CEND-04-11-13; CEND-04-11-15; CEND-04-11-17; CEND-04-11-18; CEND-04-11-19; CEND-04-11-2; CEND-04-11-20; CEND-04-11-21; CEND-04-11-22; CEND-04-11-23; CEND-04-11-24; CEND-04-11-25; CEND-04-11-26; CEND-04-11-27; CEND-04-11-29; CEND-04-11-3; CEND-04-11-30; CEND-04-11-31; CEND-04-11-32; CEND-04-11-33; CEND-04-11-34; CEND-04-11-35; CEND-04-11-36; CEND-04-11-37; CEND-04-11-38; CEND-04-11-39; CEND-04-11-41; CEND-04-11-42; CEND-04-11-43; CEND-04-11-44; CEND-04-11-45; CEND-04-11-46; CEND-04-11-49; CEND-04-11-50; CEND-04-11-52; CEND-04-11-53; CEND-04-11-54; CEND-04-11-56; CEND-04-11-57; CEND-04-11-6; CEND-04-11-60; CEND-04-11-62; CEND-04-11-63; CEND-04-11-65; CEND-04-11-66; CEND-04-11-67; CEND-04-11-69; CEND-04-11-7; CEND-04-11-70; CEND-04-11-71; CEND-04-11-72; CEND-04-11-73; CEND-04-11-75; CEND-04-11-76; CEND-04-11-78; CEND-04-11-8; CEND-04-11-80; CEND-04-11-82; CEND-04-11-83; CEND-04-11-85; CEND-04-11-87; CEND-04-11-9; CEND-04-11-90; CEND-04-11-91; CEND-19-11-10; CEND-19-11-13; CEND-19-11-14; CEND-19-11-18; CEND-19-11-20; CEND-19-11-21; CEND-19-11-24; CEND-19-11-25; CEND-19-11-34; CEND-19-11-36; CEND-19-11-37; CEND-19-11-40; CEND-19-11-42; CEND-19-11-76; CEND-19-11-8; CEND-19-11-83; CIROL03-86-27; CIROL03-86-28; CIROL03-86-30; CIROL03-86-31; CIROL03-86-34; CIROL03-86-36; CIROL03-86-38; CIROL03-86-40; CIROL03-86-41; CIROL03-86-54; CIROL03-86-55; CIROL03-86-56; CIROL03-86-57; CIROL03-86-58; CIROL03-86-59; CIROL03-86-67; CIROL03-86-68; CIROL03-86-69; CIROL03-86-70; CIROL03-86-93; CIROL03-86-95; CIROL03-87-1; CIROL03-87-10; CIROL03-87-13; CIROL03-87-14; CIROL03-87-2; CIROL03-87-20; CIROL03-87-22; CIROL03-87-28; CIROL03-87-29; CIROL03-87-3; CIROL03-87-39; CIROL03-87-43; CIROL03-87-44; CIROL03-87-5; CIROL03-87-51; CIROL03-87-57; CIROL03-87-6; CIROL03-87-7; CIROL03-87-8; CIROL03-91-10; CIROL03-91-11; CIROL03-91-15; CIROL03-91-16; CIROL03-91-18; CIROL03-91-19; CIROL03-91-2; CIROL03-91-20; CIROL03-91-21; CIROL03-91-
    Type: Dataset
    Format: text/tab-separated-values, 227043 data points
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  • 2
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Inorganic chemistry 24 (1985), S. 1330-1333 
    ISSN: 1520-510X
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Annals of the New York Academy of Sciences 514 (1987), S. 0 
    ISSN: 1749-6632
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Natural Sciences in General
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Annals of the New York Academy of Sciences 514 (1987), S. 0 
    ISSN: 1749-6632
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Natural Sciences in General
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Oxford [u.a.] : International Union of Crystallography (IUCr)
    Acta crystallographica 52 (1996), S. 3000-3002 
    ISSN: 1600-5759
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Oxford [u.a.] : International Union of Crystallography (IUCr)
    Acta crystallographica 52 (1996), S. 1091-1093 
    ISSN: 1600-5759
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Oxford [u.a.] : International Union of Crystallography (IUCr)
    Acta crystallographica 51 (1995), S. 611-613 
    ISSN: 1600-5759
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 8
    ISSN: 1434-6052
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract Charged particle multiplicity distributions and pseudo-rapidity density distributions from16O induced nuclear collisions at 200 and 60A GeV are presented. The data were taken, using a minimumbias trigger, with the WA80 set-up at the CERN SPS. In this presentation we focus on how the yield of charged particles depends on the projectile energy, the mass number of the target nucleus and the energy measured in a uranium-plastic sampling calorimeter covering angles close to zero degrees. The data are compared to simulations from the event generator FRITIOF.
    Type of Medium: Electronic Resource
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  • 9
    ISSN: 1434-6052
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract Transverse momentum (p T) distributions fo inclusive photons and neutral pions at midrapidity are measured with a lead glass calorimeter in 60 and are measured with a lead glass calorimeter in 60 and 200A·Gev16O+nucleus and and proton+nucleus reactions. Inclusive photon distributions are compared for central and peripheral reactions. The degree of centrality is determined either from the charged particle multiplicity or from the remaining projectile energy in the forward direction. Deviations from a nucleus+nucleus interaction model based upon linear extrapolation from p+p reactions are observed in central16O+Au data. The variation of theaverage transverse momentum is investigated as function of centrality. The target-mass and energy dependence of π0 p T distributions are presented. For16O+Au a change of slope in these distributions is observed atp t ≈0.8 GeV/c compatible with hydrodynamic expansion models.
    Type of Medium: Electronic Resource
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  • 10
    ISSN: 1434-6052
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract Target remnants withZ〈3 from proton-nucleus and16O-nucleus reactions at 60 and 200 GeV/nucleon were measured in the angular range from 30° to 160° (−1.7〈η〈1.3) employing the Plastic Ball detector. The excitation energy of the target spectator matter in central oxygen-induced collisions is found to be high enough to allow for complete disintegration of the target nucleus into fragments withZ〈3. The average longitudinal momentum transfer per proton to the target in central collisions is considerably higher in the case of16O-induced reactions (≈300 MeV/c) than in proton-induced reactions (≈130 MeV/c). The baryon rapidity distributions are roughly in agreement with one-fluid hydrodynamical calculations at 60 GeV/nucleon16O+Au but are in disagreement at 200 GeV/nucleon, indicating the higher degree of transparency at the higher bombarding energy. Both, the transverse momenta of target spectators and the entropy produced in the target fragmentation region are compared to those attained in head-on collisions of two heavy nuclei at Bevalac energies. They are found to be comparable or do even exceed the values for the participant matter at beam energies of about 1–2 GeV/nucleon.
    Type of Medium: Electronic Resource
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