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Fjord

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Most cited protocols related to «Fjord»

Gametes from wild Atlantic salmon originating from the Etne River (59°40′N, 5°56′E), Hordaland, and farmed salmon originating from the Norwegian Mowi strain were used to generate three cross-types for this experiment in 2009; (i) ten pure wild families; (ii) ten pure farmed families; and (iii) ten F1 hybrid families, generated by crossing farmed females with wild males. Thus, the hybrid families were maternal and paternal half siblings of the farmed and wild families, respectively. These three experimental groups are from now referred to as farmed (Mowi), hybrid (Mowi x Etne) and wild (Etne).
The Etne River has the largest wild salmon stock in Hordaland [51] and salmon used as parents were collected directly from the river. The Mowi strain from Marin Harvest is the oldest Norwegian farmed strain [45] . This strain was established from large multi-sea winter fish collected from the River Bolstad in the Vosso watercourse and the River Åroy, in addition to wild salmon caught in the sea outside of western Norway, near Oster fjord and Sotra [6] , [52] . Phenotypic selection for growth, late maturation and fillet quality was conducted until 1999, when a family based selection program consisting of 250 females and 80 males was initiated [6] . In our study we used the offspring of the 9–10th generation of selected parents.
All families were established November 17, 2009, at the hatchery located on the river Etne. Unfertilized ova and milt from 10 male and 10 female farmed salmon were collected from the Mowi breeding station located at Askøy and transported to the Etne hatchery. Wild salmon were caught by rod in October – November, 2009, transported to the hatchery located on the Etne river, and stripped upon the arrival of farmed gametes (for family crosses, see Table S1). Adipose fin clips were collected from all parental fish and scale samples from wild parents were collected and analyzed by the Norwegian gene bank for wild salmon (The Norwegian Directorate for Nature Management), to confirm that wild salmon were not escapees from farms [53] .
All 30 families were incubated in the dark in single-family units, at temperatures of approximately 3.5°C (range 2.0–6.6°C), until the eyed-egg stage. Dead eggs were picked daily and February 17–18, 2010, shocked to sort out dead eggs. One hybrid family was at this point excluded from the study due to high egg mortality; hence the wild, farmed and hybrid origins were represented by 10∶10:9 families, respectively. Weight and volume measurements of eggs from all families were taken on March 17, 2010. On the same day, equal numbers of fertilized eggs per family (n = 50) were counted out and sorted into four replicated mixed trays (n = 1450; Figure 1). Experimental groups were transported to the Matre research station March 18, 2010.
The four replicates continued their incubation at the Matre hatchery at approximately 5°C (range 4–5.6°C). April 19, 2010, all four replicates were transferred to 1.5 m3 tanks, continuously supplied with fresh water at an average temperature of 13.2°C (range 10.7–15.6°C). All experimental groups were kept under 24 hour daily light throughout the experiment. Fry were presented with a commercial diet starting on April 22, 2010. A standard feeding table for appropriate temperatures was used to calculate the feeding ration. The fish were feed with commercial pelleted fish feed (Biomar, Myre, Norway), 12 hours per day by automatic feeders, 09.00–21.00. Pellet sizes were adjusted to the mean fish weight (W, g) after weighing a sample of 50 individuals per tank. Due to visible differences in weight among individual fish within each tank, a combination of pellet sizes were used according to supplier’s protocol to ensure that all fish were given suitable feed. Mortality was recorded daily, however dead individuals were not assigned to family.
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Publication 2013
Clip Diet Eggs Females Fishes Fjord Gametes Genes Hybrids Light Males Mothers Obesity Parent Phenotype Rivers Salmo salar Sibling Strains Zygote
Adult Sycon specimens were collected from fjords located near Bergen, Norway (+60° 27' 33", +4° 56' 1") during the reproductive season from May to September (2008 to 2011). For in-situ hybridization, samples were immediately fixed in 100 mM MOPS, pH 7.5; 0.5 M sodium chloride; 2 mM MgSO4; 4% paraformaldehyde; 0.05% glutaraldehyde over night at 4°C, stepped into and extensively washed in 70% EtOH and stored at −20°C until processing. Macro sections of sponges in 24 well plates (Nunc) were rehydrated and washed in PBS/0.1% Tween (PTw). Samples were pretreated with 7.5 μg/mL proteinase K for 10 minutes at 37°C, followed by quenching with glycine (2 mg/mL PTw). Acetylation was performed by serial treatment with 0.1 M triethanolamine containing 0, 1.5, and 3 μl/mL acetic anhydride. Re-fixation was done in 4% paraformaldehyde/0.05% glutaraldehyde in PBS for 1 h at room temperature, followed by extensive washing in PTw. Tissue was prehybridized as previously described
[33 (link)] in 2 mL-tubes for 90 to 180 min at 51°C. Probe hybridization was done with denatured RNA probe (0.1-0.3 ng/μL, approximately 1 kb) for 12 to 18 h at 51°C. Stringent washes were carried out at 55°C as following: 1 × 10 min in hybridization buffer; 2 × 10 min 50% formamide/4 × SSC/0.1%; 2 × 10 min 50% formamide/2 × SSC/0.1% Tween; 2 × 10 min 25% formamide/2 × SSC/0.1% Tween, followed by 3 × 15 min 2 × SSC/0.1% Tween at room temperature. Samples were transferred to maleic acid buffer and incubated in 2% (w/v) Blocking Reagent (Roche) for 60 min at room temperature. After overnight incubation with AP-coupled anti-Digoxigenin-Fab fragments (Sigma, 1:5,000) at 4°C, samples were washed in maleic acid buffer at least 6 × 30 min. Probe was detected using NBT/BCIP as substrate (Roche) with tissue equilibrated in alkaline phosphatase buffer (100 mM sodium chloride, 50 mM MgCl2, 100 mM Tris pH 9.5, 0.1% Tween, 1 mM Levamisole). The staining reaction (0.5 to 3 days) was stopped with PBS/0.5% Tween, samples were transferred to 100% glycerol for microscopy or ethanol-dehydrated and embedded in epoxy resin (Sigma) for sectioning. Pictures of whole mount samples and sections were taken using a Nikon DS-U3 microscope and processed in Photoshop.
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Publication 2012
acetic anhydride Acetylation Acid Hybridizations, Nucleic Adult Alkaline Phosphatase Buffers Digoxigenin Endopeptidase K Epoxy Resins Ethanol Fjord formamide Glutaral Glycerin Glycine Immunoglobulins, Fab In Situ Hybridization Levamisole Magnesium Chloride maleic acid Microscopy morpholinopropane sulfonic acid paraform Porifera Reproduction RNA Probes Sodium Chloride Sulfate, Magnesium Tissues triethanolamine Tromethamine Tweens
Approximately 10 000 single-cell G.pseudospinescens organisms were isolated by hand from Gullmar Fjord sediment (Risgaard-Petersen et al., 2006 (link)). After washing, total DNA was extracted using the QIAamp DNA Micro Kit and sequenced by Illumina Genome Analyser II. Using Edena (Hernandez et al., 2008 (link)), 9 950 730 32 nt reads were assembled with parameters m=16 and M=16, which yielded the highest N50 value (N50=170). The raw data and assembly are available from the Gene Expression Omnibus (GEO) under accession number GSE26664. The total DNA of a eukaryote may contain up to three different translation codes (De Grey, 2005 (link)): nuclear, mitochondrial and plastid (if the organism is photosynthetic, but this is not the case for G.pseudospinescens). To avoid mixing these signals, the user can choose to feed individual contigs to FACIL, but this might lead to a bad genetic code prediction due to shortage of data. Thus, we selected those contigs that were likely derived from the G.pseudospinescens mitochondrial genome as follows. The 8456 assembled contigs were queried by BlastX version 2.2.22+ (Camacho et al., 2009 (link)) against all proteins encoded by completely sequenced mitochondria, downloaded from NCBI organelle genome resources (http://www.ncbi.nlm.nih.gov/genomes/GenomesHome.cgi?taxid=2759) on July 28, 2010. Importantly, we used the standard genetic code for this BlastX search in order not to impose a bias in the genetic code on the contigs and our results. The 150 contigs with a high-scoring BlastX hit (E-value ≤0.01) were considered to be of mitochondrial origin (average length 223 nt, median length 191 nt). These sequences are available as ‘example’ input data on the FACIL web server. They contain fragments of mitochondrial genes like cytochrome B and several ATP synthase, cytochrome-c oxidase and NADH dehydrogenase subunits. We found no evidence for multiple copies (e.g. a nuclear and a mitochondrially encoded copy) of the encoded genes after a BlastN search (E-value ≤0.01) of the contigs against themselves.
Publication 2011
Cells Cytochromes b Eukaryotic Cells Fjord Gene Expression Genes Genes, Mitochondrial Genetic Code Genome Genome, Mitochondrial Mitochondria Mitochondrial Inheritance NADH Cytochrome c Oxidoreductase Nitric Oxide Synthase Organelles Oxidase, Cytochrome-c Photosynthesis Plastids Proteins Protein Subunits
All further calculations and statistical analyses were realized in R (www.r-project.org).
Each parameter was summed (surface analysed, available substrate) or averaged (CTD data, coral patch size, coral abundance, coral shape) for each site within 10 m depth intervals. The fraction of available substrate effectively colonized by the corals was calculated in each depth interval (% used = 100 ∗ patch size/available substrate). The data on substrate and coral distribution were imported in ArcGIS for graphical representation (Figs. 4 and 5).
To investigate eventual relationships between the coral distribution parameters (coral abundance and substrate usage) and the environmental parameters (temperature, salinity, pH, oxygen and available substrate) in Comau Fjord multiple linear regression analyses were performed.
All primary data are available at http://doi.pangaea.de/10.1594/PANGAEA.811911.
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Publication 2013
Coral Figs Fjord Oxygen Salinity
Narwhals were live-captured in August 2013–2016 from a field station (Hjørnedal) near the southwestern tip of Milne Land in the Scoresby Sound fjord complex (Fig 1). Whale captures were accomplished using set nets (40 or 80 m length, 5–8 m deep) in collaboration with local Inuit hunters (see [2 ] for more information). Handling of captured whales was conducted near shore by six persons in survival suits standing on either side of the whale to restrict its movements and support it, if needed. Gender of the whale was determined based on presence (male) or absence (female) of a tusk.
Five female narwhals, one accompanied by a calf, and one male narwhal (Table 1) were instrumented with Acousonde acoustic and orientation tags (www.acousonde.com), whose float had been modified to accommodate an Argos transmitter (Wildlife Computers SPOT5) in addition to a VHF transmitter (ATS Telemetry). The Acousonde recorders were attached to the skin with suction cups, on the rear half of the animal, to the side of the dorsal ridge (Fig 1B). To extend the longevity of the attachment, one or two 1-mm nylon lines were threaded through the top of the dorsal ridge. The Acousonde was held to the lines with magnesium corrodible links, which ensured release of the recorder after 3–8 days of attachment (Table 1). Once detached from the whale, the Argos transmitter provided its position to the field station, and the VHS transmitter enabled close-up relocation of the package. All deployed tags were retrieved 1–4 days after their release from the whale.
In addition to the Acousonde, a satellite transmitter was also deployed on the whales for long-term tracking following procedures described in Heide-Jørgensen et al. [2 , 21 ]. The females were instrumented with tags from Wildlife Computers (Redmond, WA; Freya: Mk10; Thora, Mára, and Frida: SPLASH tag; Eistla: SPLASH tag with Fastloc® GPS option), while Balder, the male, was instrumented with a CTD tag from SMRU (Sea Mammal Research Unit, St Andrews, UK). Eistla’s calf remained nearby while its mother was being instrumented. Both mother and calf were observed leaving together after Eistla’s release.
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Publication 2018
Acoustics Alopecia Animals ARID1A protein, human Cetacea Females Fjord Inuit Magnesium Males Mammals Monodon monoceros Mothers Movement Nylons Skin Sound Suction Drainage Telemetry

Most recents protocols related to «Fjord»

Maxwell Bay (62°25′S; 58°85′W) is located between King George Island and Nelson Island in the South Shetland Islands of Antarctica. It is a common fjord-like Antarctic embayment characterized by a U-shaped deep basin. Fieldwork was carried out in Barton Peninsula, Fildes Peninsula, Weaver Peninsula, and Ardley Island located around Maxwell Bay (Fig. 1). The study area includes the Antarctic Specially Protected Areas (ASPAs) that are designated to protect environmental and scientific values such as breeding bird colonies, relatively extensive flora, and geological features under the Antarctic Treaty System. Narębski Point (ASPA No. 171) encloses penguin colonies and is located on the southeast coast of Barton Peninsula, King George Island. Ardley Island is an islet that is 1.9 km long and is located off the southwest end of King George Island. Bird colonies inhabit the area, and the whole island has been designated as ASPA No. 150 (Fig. 1).

Maxwell Bay, King George Island, Antarctica. Lichen samples were collected from (1) Barton Peninsula, (2) Weaver Peninsula, (3, 4) Fildes Peninsula, and (5) Ardley Island. Antarctic Specially Protected Area (ASPA) No. 171 and ASPA No. 150 marked with asterisks

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Publication 2023
Aves Fjord Lichens Spheniscidae
Northern shrimp were
collected with shrimp pots in fjords in northern Norway in October
2019 and acclimatized in the research laboratory until the start of
the experiment (details can be found in the Supporting Information (SI)).
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Publication 2023
Fjord Marijuana Abuse

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Publication 2023
Adult Animals Diet Females Fjord Heart Institutional Animal Care and Use Committees Phocoena phocoena Positive Reinforcement Respiratory Rate
The southern coast of Chile, also known as the Chilean Patagonia (41 to 55° S), constitutes one of the most extensive fjord and channel systems in the world (Figure 1). This system has a rugged bathymetry, dissected coastline, and strong but highly variable water column stratification. Marked salinity gradients exhibit seasonal and latitudinal patterns determined by heavy riverine inflow from ice melting in late spring (November–December) and persistent rainfall with an average of 2700 mm y−1 and up to 5000 mm in exceptional years [72 (link),73 (link)]. Summer heating breaks the winter–spring thermal inversion and generates stronger thermohaline gradients [59 (link)].
Circulation in the Patagonian fjords is of two-layered estuarine-type, with a variable (5–10 m) estuarine surface water (EW) and a more uniform saltier lower layer, the Subantarctic Water (SAAW, S > 33) reaching 150 m depth [74 ]. Mixing of the two layers at the interface generates Modified Subantarctic Water (MSAAW, S = 31–33) [59 (link)]. Depending on freshwater inputs, different water masses can be identified within the estuarine surface water: Estuarine Fresh Water (EFW, S = 11–21), Estuarine Saline Water (ESW, S = 21–31). When salinity is less than 11, the water is classified as Fresh Water (FW) [52 (link)]. The Pitipalena (PIT) (~ 43°S), and Puyuhuapi (PUY) (~ 44° S) fjords, in the Aysén region, form part of this great fjord system. PUY (100 km) is much longer than PIT (22 km), the latter being more semi-enclosed [59 (link),60 (link),75 (link)]. Unlike PIT fjord, PUY has two connections with oceanic waters, one through the Moraleda Channel in the mouth and another through the Jacaf Channel close to the head [59 (link)]. In the two fjords, the main freshwater inputs come from riverine inflows and rainfall. The main river flowing into PUY (Cisnes, average river discharge 218 m3s−1) has its mouth located by the middle reaches of this fjord [75 (link),76 (link)]. In contrast, in PIT, the Palena river, with a four-fold average river discharge (800 m3s−1), is located at the mouth [60 (link)]. These characteristics affect hydrodynamic conditions, including stratification and water residence time, which is maximal in PUY (~250 days) compared to PIT fjord (~200 days) [77 ,78 ], directly promoting phytoplankton retention and HAB development.
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Publication 2023
Fjord Head Hydrodynamics Inversion, Chromosome Oral Cavity Patient Discharge Phytoplankton Retention (Psychology) Rivers Salinity
Measurements of abiotic and biotic factors were carried out hourly or every 2 h during intensive 24 h surveys at a fixed station on each fjord. The aim was to study small-scale interactions that modulate the time–depth distribution of Dinophysis and potential ciliate prey populations in two NW Patagonian fjords. The circadian variability, potential vertical migration, and specific division rate of Dinophysis species were evaluated in PIT (March 18–19) (Figure 1B) and PUY (February 18–19) (Figure 1C) fjords, two coastal sites with distinct hydrodynamic conditions, but subject to recurring toxic outbreaks. Sampling in 2020 was carried out in summer, i.e., the season with the highest probability of occurrence of these events [34 (link)]. In both surveys, observations on division phases began at 18:00 h.
Vertical profiles of temperature, salinity, dissolved oxygen, and in vivo chla fluorescence were obtained with an RBR CTD (conductivity–temperature–depth) profiler (https://rbr-global.com) model Concerto3 equipped with a Turner Designs CYCLOPS-7 fluorometer (excitation 460 nm, emission 620–715 nm). The (CTD) probe was cast hourly to 50 m depth. CTD data processing was carried out with the software provided by the manufacturer and depicted using the Ocean Data View software version 5.1 [79 ]. Additionally, temperature, dissolved oxygen, and chlorophyll-a sensors were installed at 2 m and 6 m at the fixed sampling locations in PUY and PIT fjords. A MiniDOT oxygen logger (www.pme.com) was used to obtain the temperature and dissolved oxygen records. In addition, a C-Fluor logger model CYCLOPS-7 (www.pme.com/products/cfluor-logger, accessed on 9 December 2022) was installed at 6 m.
Water samples of 100 mL for quantitative analysis of Dinophysis species and their potential micro-ciliate prey were collected every 2 h at 2 m intervals, from the surface to 20 m, and at 25 m, and 30 m, with a 5 L Niskin bottle, and immediately fixed with neutral Lugol’s iodine solution [80 (link)].
Plankton nets (20 μm mesh) were towed vertically from 20 m to the surface twice every hour. Samples of 100 mL were taken from the first tow and fixed with neutral Lugol’s solution [80 (link)]. These samples were used to estimate frequency of cells undergoing mitosis and in situ daily specific division rates (μ) (see Section 4.5). A second net tow was collected for toxin analyses. The whole content of the net collector was filtered through Whatman GF/F fiberglass filters (25 mm Ø, 0.7 μm pore size) (Whatman, Maidstone, England), the filters and filtered material placed in a cryotube, mixed with 1 mL analysis grade methanol, and stored in the laboratory at −20 °C until analysis.
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Publication 2023
CD3EAP protein, human Cells Chlorophyll A Ciliata cyclocephaly Disease Outbreaks Electric Conductivity Fjord Fluorescence Hydrodynamics Iodine Lugol's solution Methanol Mitosis Oxygen Plankton Population Group Salinity Toxins, Biological

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More about "Fjord"

Fjord is an innovative AI-powered protocol optimization platform that empowers researchers to accelerate their scientific discoveries.
By leveraging intelligent comparisons across a vast corpus of literature, preprints, and patents, Fjord helps users quickly identify the most effective protocols, products, and techniques for their research needs.
This intuitive tool unlocks new insights and enhances the research workflow, allowing scientists to focus on breakthroughs rather than tedious manual searches.
Fjord's AI-driven approach optimizes the research process, enabling users to enhance productivity and drive meaningful progress in their field of study.
The platform's intelligent comparison capabilities can be utilized to explore a wide range of related topics and techniques, such as the use of Fluorescein dye for microscopy, Stereomicroscope imaging, the ULM-500 microplate reader, the power of T7 and SP6 RNA polymerases, the Cellic® CTec2 enzyme complex, the Nikon 80i light microscope, the PGEM-T Easy Vector System II for cloning, the IButton DS1922L temperature logger, and the RNAlater solution for RNA preservation.
By integrating these complementary tools and techniques, researchers can unlock new possibilities and accelerate their discoveries using the powerful Fjord and PubCompare.ai platform.
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