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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
    Publication Date: 2020-12-18
    Description: Hekla is a frequently active volcano with an infamously short pre-eruptive warning period. Our project contributes to the ongoing work on improving Hekla’s monitoring and early warning systems. In 2012 we began monitoring gas release at Hekla. The dataset comprises semi-permanent near-real time measurements with a MultiGAS system, quantification of diffuse gas flux, and direct samples analysed for composition and isotopes (δ13C, δD and δ18O). In addition, we used reaction path modelling to derive information on the origin and reaction pathways of the gas emissions. Hekla’s quiescent gas composition was CO2-dominated (0.8 mol fraction) and the δ13C signature was consistent with published values for Icelandic magmas. The gas is poor in H2O and S compared to hydrothermal manifestations and syn-eruptive emissions from other active volcanic systems in Iceland. The total CO2 flux from Hekla central volcano (diffuse soil emissions) is at least 44 T d−1, thereof 14 T d−1 are sourced from a small area at the volcano’s summit. There was no detectable gas flux at other craters, even though some of them had higher ground temperatures and had erupted more recently. Our measurements are consistent with a magma reservoir at depth coupled with a shallow dike beneath the summit. In the current quiescent state, the composition of the exsolved gas is substantially modified along its pathway to the surface through cooling and interaction with wall-rock and groundwater. The modification involves both significant H2O condensation and scrubbing of S-bearing species, leading to a CO2-dominated gas emitted at the summit. We conclude that a compositional shift towards more S- and H2O-rich gas compositions if measured in the future by the permanent MultiGAS station should be viewed as sign of imminent volcanic unrest on Hekla.
    Description: The research leading to these results has received funding from the Icelandic Centre for Research (RANNIS, grant number 110002-0031); the European Community’s Seventh Framework Programme under Grant Agreement No. 308377 (Project FUTUREVOLC); and the International Civil Aviation Organization.
    Description: Published
    Description: 80-99
    Description: 6V. Pericolosità vulcanica e contributi alla stima del rischio
    Description: JCR Journal
    Keywords: Hekla ; Multi-GAS ; degassing ; volcanic unrest ; 04.08. Volcanology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 3
    Publication Date: 2022-05-26
    Description: © The Author(s), 2017. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Geology 46 (2018): 55-58, doi:10.1130/G39413.1.
    Description: Primitive basalt melt inclusions from Borgarhraun, northern Iceland, display large correlated variations in CO2 and nonvolatile incompatible trace elements (ITEs) such as Nb, Th, Rb, and Ba. The average CO2/ITE ratios of the Borgarhraun melt inclusion population are precisely determined (e.g., CO2/Nb = 391 ± 16; 2σM [two standard errors of the mean], n = 161). These data, along with published data on five other populations of undegassed mid-oceanic ridge basalt (MORB) glasses and melt inclusions, demonstrate that upper mantle CO2/Ba and CO2/Rb are nearly homogeneous, while CO2/Nb and CO2/Th are broadly correlated with long-term indices of mantle heterogeneity reflected in Nd isotopes (143Nd/144Nd) in five of the six regions of the upper mantle examined thus far. Our results suggest that heterogeneous carbon contents of the upper mantle are long-lived features, and that average carbon abundances of the mantle sources of Atlantic MORB are higher by a factor of two than those of Pacific MORB. This observation is correlated with a similar distinction in water contents and trace elements characteristic of subduction fluids (Ba, Rb). We suggest that the upper mantle beneath the younger Atlantic Ocean basin contains components of hydrated and carbonated subduction-modified mantle from prior episodes of Iapetus subduction that were entrained and mixed into the upper mantle during opening of the Atlantic Ocean basin.
    Description: Maclennan is supported by Natural Environment Research Council grant NE/M000427/1. This research was supported by the Carnegie Institution of Washington.
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 4
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    The @journal of physical chemistry 〈Washington, DC〉 78 (1974), S. 1150-1153 
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Physics
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    R & D management 22 (1992), S. 0 
    ISSN: 1467-9310
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Economics
    Notes: Based on different contractual forms and their associated degrees of organizational integration, a typology of strategies for technology acquisition (sourcing) is constructed. Based on a sample of corporations in Europe, Japan and US, it is shown that external acquisition of technology through various strategies increases in importance in general. Product case studies further show that external acquisition of technology is associated with technology diversification into increasingly costly new technologies. As a result corporations become multi-technological (‘multech’). At the same time quasi-integrated corporate systems of innovation arise in which in-house R&D is managed together with a mix of strategies for external acquisition of technology, using various contractual forms. This presents new challenges to traditional in-house R&D management. Technology diversification is moreover shown to be associated with growth of sales as well as with growth of R&D expenditures. A high level of external technology acquisition presents risks that ought to lead companies to consider technology based product diversification.
    Type of Medium: Electronic Resource
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  • 6
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Physics
    Type of Medium: Electronic Resource
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  • 7
    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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  • 8
    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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  • 9
    ISSN: 1365-2109
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract. The paper describes the development and current status of salmon, Salmo salar L., ranching in Iceland, with a special emphasis on recapture techniques and homing to the release sites. Many ranching operations are located at release sites with little or no rearing activity except for a short acclimatization period before release. This technique was a breakthrough in Icelandic ranching development, as most suitable ranching sites do not have suitable conditions for smolt rearing.Ranching is mostly practised on the west coast of Iceland, where ranched salmon made up over 80% of the total catch in 1991. The largest ranching stations are Kollafjördur and Vogavík in south-western Iceland and two stations, Lárós and Silfurlax, located on the outer part of Snæfellsnes. Combined releases in 1991 were about 6 million smolts and 130 thousand salmon were harvested from ranching.Ranched salmon are mostly harvested from June to August with a peak run in July. The methods of recapture vary considerably. At Kollafjördur Fish Farm, which has river water for attraction, the salmon are mostly caught in riverine traps of conventional design, but during periods of draught an estuarine seining process has been practised to secure bright salmon. At Vogavík, which only has pumped well water for attraction, catches have been based on efficient estuarine traps. Similar methods have been used at the Silfurlax operation in Hraunsfjördur.Homing to ranching sites has been shown to be fairly precise, especially if smolts are released in fresh water and suitable ranching stocks are used. There are indications that the Kollafjördur ranching strain, which has been developed over a period of 25 years, has better homing than wild stocks. Considerable straying has been observed, primarily between ranching stations and into the outflows of large land-based salmon farms. Straying into salmon streams seems to vary from year to year and is greatest in the vicinity of large ranching stations. It seems to occur in late summer, possibly as a result of inadequate recapture techniques at the ranching sites.
    Type of Medium: Electronic Resource
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  • 10
    ISSN: 0012-821X
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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