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544 results for “ammonium”
Fig. 4 in Attraction of Bactrocera cucurbitae and Bactrocera dorsalis (Diptera: Tephritidae) to beer waste and other protein sources laced with ammonium acetate
Fig. 4. Response of males of Bactrocera cucurbitae and B. dorsalis to GF-120® NF Naturalyte® Fruit Fly Bait (= GF-120), beer waste, Nu-Lure® Insect Bait (= Nu-Lure), and water (negative control) either in the absence (A), or presence (B) of ammonium acetate (= AA). For each species, different letters (lowercase: B. cucurbitae; uppercase: B. dorsalis) indicate significant differences according to ANOVA and the Fisher LSD tests at P ≤ 0.05.
Experimental CCN properties of 6 pollenkitts and two mixtures with ammonium sulfate reported in the study "Cloud condensation nuclei activity of six pollenkitts and the influence of their surface activity" by Prisle et al. (2019)
<p>Critical dry particle size Dp<sub>50</sub> measured for supersaturations 0.1–1.4% with a DMT CCN Counter (CCN-100). Size and composition resolved, and size-averaged hygroscopicity values calculated using the method presented by Rose et al. (2010), Cloud condensation nuclei in polluted air and biomass burning smoke near the mega-city Guangzhou, China - Part 1: Size-resolved measurements and implications for the modeling of aerosol particle hygroscopicity and CCN activity, <em>Atmospheric Chemistry and Physics</em>, <em>10</em>, 3365–3383.</p>
Text-fig. 3. Coeloma vigil A. MILNE-EDWARDS. Nearly complete specimens from several different layers. A – layer 15; B – layer 11; C – layer 16. All specimens are deposited at KGP MH. Key: ch=chelipeds; es=eye stalks; p=pereiopods. Scale bar 10 mm. Specimens were covered with ammonium chloride prior to photography. in The Priabonian Bryozoan-Decapod Association From The Borové Formation (The Ďurkovec Quarry, Ne Slovakia) And Its Palaeoecological Implications
Text-fig. 3. Coeloma vigil A. MILNE-EDWARDS. Nearly complete specimens from several different layers. A – layer 15; B – layer 11; C – layer 16. All specimens are deposited at KGP MH. Key: ch=chelipeds; es=eye stalks; p=pereiopods. Scale bar 10 mm. Specimens were covered with ammonium chloride prior to photography.
Text-fig. 2. Condylopyge cf. rex (BARRANDE, 1846), middle Cambrian, latest Cambrian Stage 5 and lower Drumian, Jince Formation, Příbram-Jince Basin. a. internal mould of isolated cephalon (Specimen CGS CW 17), Potůček near Rejkovice locality (= locality 12 in Fatka and Kordule 1992) in lower levels of the Paradoxides (Eccaparadoxides) pusillus Zone. b. latex cast of external mould of isolated pygidium (Specimen CGS FK 63), Potůček near Rejkovice locality (= locality 12 in Fatka and Kordule 1992) in lower levels of the Paradoxides (Eccaparadoxides) pusillus Zone. c. internal mould of isolated cephalon (Specimen CGS CW 18), foot of the slope known as Vinice near Jince (locality 20 in Fatka and Kordule 1992) in lower levels of the Onymagnostus hybridus Zone. Condylopyge rex (BARRANDE, 1846), middle Cambrian, lower Drumian, Buchava Formation, Paradoxides (Eccaparadoxides) pusillus Zone, Skryje-Týřovice Basin. d. internal mould of isolated cephalon (NM-L43011a), Karáskovská rokle - nad chatami. e. internal mould of isolated pygidium (NM-L43014), Lůmek u Týřovic. f. internal mould of isolated cephalon (NM-L43013), Lůmek u Týřovic. Whitened with ammonium chloride sublimate. All scale bars are 1 mm. Photographs by Martin Valent (National Museum Prague). in Condylopyge Hawle Et Corda, 1847 In The Příbram-Jince Basin (Barrandian Area, The Czech Republic, Agnostida)
Text-fig. 2. Condylopyge cf. rex (BARRANDE, 1846), middle Cambrian, latest Cambrian Stage 5 and lower Drumian, Jince Formation, Příbram-Jince Basin. a. internal mould of isolated cephalon (Specimen CGS CW 17), Potůček near Rejkovice locality (= locality 12 in Fatka and Kordule 1992) in lower levels of the Paradoxides (Eccaparadoxides) pusillus Zone. b. latex cast of external mould of isolated pygidium (Specimen CGS FK 63), Potůček near Rejkovice locality (= locality 12 in Fatka and Kordule 1992) in lower levels of the Paradoxides (Eccaparadoxides) pusillus Zone. c. internal mould of isolated cephalon (Specimen CGS CW 18), foot of the slope known as Vinice near Jince (locality 20 in Fatka and Kordule 1992) in lower levels of the Onymagnostus hybridus Zone. Condylopyge rex (BARRANDE, 1846), middle Cambrian, lower Drumian, Buchava Formation, Paradoxides (Eccaparadoxides) pusillus Zone, Skryje-Týřovice Basin. d. internal mould of isolated cephalon (NM-L43011a), Karáskovská rokle - nad chatami. e. internal mould of isolated pygidium (NM-L43014), Lůmek u Týřovic. f. internal mould of isolated cephalon (NM-L43013), Lůmek u Týřovic. Whitened with ammonium chloride sublimate. All scale bars are 1 mm. Photographs by Martin Valent (National Museum Prague).
Text-fig. 7. p4 of U. deningeri from Šandalja I compared with other bear species. a: Šandalja I (specimen H; 1 – occlusal, 2 – lingual view), b: U. etruscus, Casa Frata (private collection), c: U. etruscus, Olivola (IGF 4605), d: U. deningeri, C 718 cave (NM-Rv 20003), e: U. t. mediterraneus, Azykh cave (ZIN 32549) (all in occlussal view). Specimens coated by ammonium chloride; d reversed. in Šandalja I (Croatia) And
Text-fig. 7. p4 of U. deningeri from Šandalja I compared with other bear species. a: Šandalja I (specimen H; 1 – occlusal, 2 – lingual view), b: U. etruscus, Casa Frata (private collection), c: U. etruscus, Olivola (IGF 4605), d: U. deningeri, C 718 cave (NM-Rv 20003), e: U. t. mediterraneus, Azykh cave (ZIN 32549) (all in occlussal view). Specimens coated by ammonium chloride; d reversed.
Text-fig. 6. m2 of U. deningeri from Šandalja I (a: specimen G; 1– occlusal, 2 – lingual view) compared with Late Biharian U. deningeri from C 718 cave (b: NM-R 9740, c: NM-Ra 129; both occlusal view). Specimens coated by ammonium chloride; a reversed. in Šandalja I (Croatia) And
Text-fig. 6. m2 of U. deningeri from Šandalja I (a: specimen G; 1– occlusal, 2 – lingual view) compared with Late Biharian U. deningeri from C 718 cave (b: NM-R 9740, c: NM-Ra 129; both occlusal view). Specimens coated by ammonium chloride; a reversed.
Text-fig. 4. m1 of U. t. mediterraneus from Šandalja I compared with other bear species. All teeth in occlusal view. a: Šandalja I (specimen C), b: U. t. mediterraneus, Mauer (SMNS 10166), c: U. t. mediterraneus, Azykh (ZIN 32549), d: U. etruscus, Olivola (IGF 4605), e: U. etruscus, Upper Valdarno (IGF 913), f: U. deningeri, Koněprusy caves (NM-Rv 20008). Specimens coated by ammonium chloride; a, d, f reversed. in Šandalja I (Croatia) And
Text-fig. 4. m1 of U. t. mediterraneus from Šandalja I compared with other bear species. All teeth in occlusal view. a: Šandalja I (specimen C), b: U. t. mediterraneus, Mauer (SMNS 10166), c: U. t. mediterraneus, Azykh (ZIN 32549), d: U. etruscus, Olivola (IGF 4605), e: U. etruscus, Upper Valdarno (IGF 913), f: U. deningeri, Koněprusy caves (NM-Rv 20008). Specimens coated by ammonium chloride; a, d, f reversed.
Text-fig. 3. m2 and m3 of U. t. mediterraneus from Šandalja I compared with other bear species. a–e: m2, f–g: m3. a: Šandalja I (specimen A; 1 – occlusal, 2 – lingual, 3 – buccal view), b: Šandalja I (specimen B; occlusal view), c: U. t. mediterraneus, Grotta di Reale (IGF 4807V; 1 – occlusal, 2 – lingual view), d: U. etruscus, Olivola (IGF 4605; occlusal view), e: U. etruscus, Upper Valdarno (IGF 908; occlusal view), f: Šandalja I (specimen B; occlusal view), g: U. etruscus, Olivola (IGF 4588; occlusal view). Specimens coated by ammonium chloride; a, b, e, f, g reversed. in Šandalja I (Croatia) And
Text-fig. 3. m2 and m3 of U. t. mediterraneus from Šandalja I compared with other bear species. a–e: m2, f–g: m3. a: Šandalja I (specimen A; 1 – occlusal, 2 – lingual, 3 – buccal view), b: Šandalja I (specimen B; occlusal view), c: U. t. mediterraneus, Grotta di Reale (IGF 4807V; 1 – occlusal, 2 – lingual view), d: U. etruscus, Olivola (IGF 4605; occlusal view), e: U. etruscus, Upper Valdarno (IGF 908; occlusal view), f: Šandalja I (specimen B; occlusal view), g: U. etruscus, Olivola (IGF 4588; occlusal view). Specimens coated by ammonium chloride; a, b, e, f, g reversed.
Model output for "Enrichment of ammonium in the future ocean threatens diatom productivity"
<p>Each netcdf file (.nc) contains model output from simulations performed with the<br> NEMO-PISCES global ocean-biogeochemistry model. These simulations were<br> forced by physical output from the IPSL-CM5A Earth System Model, which <br> performed both the natural (no anthropogenic activities) and RCP8.5 scenarios.</p> <p>Variables in spin-up "ptrc" files are:</p> <p> name title I J K L<br> PHY (Nano)Phytoplankton Concentrati 1:360 1:180 1:31 1:12<br> PHY2 Diatoms Concentration 1:360 1:180 1:31 1:12<br> O2 Oxygen Concentration 1:360 1:180 1:31 1:12<br> PREO2 Abiotic Oxygen Concentration 1:360 1:180 1:31 1:12<br> FER Dissolved Iron Concentration 1:360 1:180 1:31 1:12<br> NO3 Nitrate Concentration 1:360 1:180 1:31 1:12<br> NO2 Nitrite Concentration 1:360 1:180 1:31 1:12<br> NH4 Ammonium Concentration 1:360 1:180 1:31 1:12<br> NO3_15 15N Nitrate Concentration 1:360 1:180 1:31 1:12<br> NO2_15 15N Nitrite Concentration 1:360 1:180 1:31 1:12<br> NH4_15 15N Ammonium Concentration 1:360 1:180 1:31 1:12<br> O2_18 18O Dissolved Oxygen Concentrat 1:360 1:180 1:31 1:12<br> NO3_18 18O Nitrate Concentration 1:360 1:180 1:31 1:12<br> NO2_18 18O Nitrite Concentration 1:360 1:180 1:31 1:12</p> <p> </p> <p>Variables in scenario "ptrc" files are:</p> <p> name title I J K L<br> PHY (Nano)Phytoplankton Concentrati 1:360 1:180 1:31 1:12<br> PHY2 Diatoms Concentration 1:360 1:180 1:31 1:12<br> ZOO (Micro)Zooplankton Concentratio 1:360 1:180 1:31 1:12<br> ZOO2 Mesozooplankton Concentration 1:360 1:180 1:31 1:12<br> O2 Oxygen Concentration 1:360 1:180 1:31 1:12<br> PREO2 Abiotic Oxygen Concentration 1:360 1:180 1:31 1:12<br> FER Dissolved Iron Concentration 1:360 1:180 1:31 1:12<br> NO3 Nitrate Concentration 1:360 1:180 1:31 1:12<br> NO2 Nitrite Concentration 1:360 1:180 1:31 1:12<br> NH4 Ammonium Concentration 1:360 1:180 1:31 1:12<br> DOC Dissolved organic Concentration 1:360 1:180 1:31 1:12<br> POC Small organic carbon Concentrat 1:360 1:180 1:31 1:12<br> GOC Big organic carbon Concentratio 1:360 1:180 1:31 1:12<br> NO3_15 15N Nitrate Concentration 1:360 1:180 1:31 1:12<br> NO2_15 15N Nitrite Concentration 1:360 1:180 1:31 1:12<br> NH4_15 15N Ammonium Concentration 1:360 1:180 1:31 1:12<br> PHY_15 15N Nanophytoplankton Concentra 1:360 1:180 1:31 1:12<br> PHY2_15 15N Diatoms Concentration 1:360 1:180 1:31 1:12<br> DOC_15 15N Dissolved organic Concentra 1:360 1:180 1:31 1:12<br> POC_15 15N Small particulate Concentra 1:360 1:180 1:31 1:12<br> GOC_15 15N Large particulate Concentra 1:360 1:180 1:31 1:12<br> ZOO_15 15N Microzooplankton Concentrat 1:360 1:180 1:31 1:12<br> ZOO2_15 15N Mesozooplankton Concentrati 1:360 1:180 1:31 1:12<br> O2_18 18O Dissolved Oxygen Concentrat 1:360 1:180 1:31 1:12<br> NO3_18 18O Nitrate Concentration 1:360 1:180 1:31 1:12<br> NO2_18 18O Nitrite Concentration 1:360 1:180 1:31 1:12</p> <p>Variables in the scenario "diad" files are:</p> <p> name title I J K L<br> PH PH 1:360 1:180 1:31 1:12<br> HEUP Euphotic layer depth 1:360 1:180 ... 1:12<br> PAR Photosynthetically Available Ra 1:360 1:180 1:31 1:12<br> PARDM Daily mean PAR 1:360 1:180 1:31 1:12<br> PPPHYN Primary production of nanophyto 1:360 1:180 1:31 1:12<br> PPPHYD Primary production of diatoms 1:360 1:180 1:31 1:12<br> PPNEWN New Primary production of nanop 1:360 1:180 1:31 1:12<br> PPNEWD New Primary production of diato 1:360 1:180 1:31 1:12<br> PPNO2N NO2 Primary production of nanop 1:360 1:180 1:31 1:12<br> PPNO2D NO2 Primary production of diato 1:360 1:180 1:31 1:12<br> NITRNH4 Ammonia-oxidation rate (NH4-->N 1:360 1:180 1:31 1:12<br> NITRNO2 Nitrite-oxidation rate (NO2-->N 1:360 1:180 1:31 1:12<br> MUAOA Growth rate of ammonia oxidiser 1:360 1:180 1:31 1:12<br> MUAOAMAX Max potential ammonia oxidation 1:360 1:180 1:31 1:12<br> LAOANH4 Substrate limitation of NH4 oxi 1:360 1:180 1:31 1:12<br> LAOAFER Iron limitation of NH4 oxidatio 1:360 1:180 1:31 1:12<br> LAOAPAR Light limitation of NH4 oxidati 1:360 1:180 1:31 1:12<br> LAOAPH pH limitation of NH4 oxidation 1:360 1:180 1:31 1:12<br> LNOBNO2 Substrate limitation of NO2 oxi 1:360 1:180 1:31 1:12<br> LNOBFER Iron limitation of NO2 oxidatio 1:360 1:180 1:31 1:12<br> LNOBPAR Light limitation of NO2 oxidati 1:360 1:180 1:31 1:12<br> NFIX Nitrogen fixation 1:360 1:180 1:31 1:12<br> RIVER_NO3<br> Nitrate added by rivers 1:360 1:180 ... 1:12<br> NDEP_NO3 Nitrate added by deposition 1:360 1:180 ... 1:12<br> REMIN Oxic remineralization of OM (DO 1:360 1:180 1:31 1:12<br> EXCR1 Excretion by microzooplankton 1:360 1:180 1:31 1:12<br> EXCR2 Excretion by mesozooplankton 1:360 1:180 1:31 1:12<br> DENITNO3 Denitrification rate (NO3-->NO2 1:360 1:180 1:31 1:12<br> DENITNO2 Denitrification rate (NO2-->N2) 1:360 1:180 1:31 1:12<br> ANAMMOX Anaerobic oxidation of NH4 (NH4 1:360 1:180 1:31 1:12<br> ALTREM Alternative anaerobic remin (DO 1:360 1:180 1:31 1:12<br> SDEN3D Sed denitrification of OM (NO3- 1:360 1:180 1:31 1:12<br> SREM3D Sed remineralisation of OM (DOC 1:360 1:180 1:31 1:12<br> <br> Files:</p> <ul> <li> ETOPO_nitr_kaoafer00_1m_ptrc.nc</li> <li> ETOPO_nitr_kaoafer00_1m_diad.nc</li> <li> ETOPO_nitr_kaoafer00_2ndpicontrol_1m_ptrc_2081-2100_ave.nc</li> <li> ETOPO_nitr_kaoafer00_2ndpicontrol_1m_diad_2081-2100_ave.nc</li> <li> ETOPO_nitr_kaoafer00_acid_1m_ptrc_2081-2100_ave.nc</li> <li> ETOPO_nitr_kaoafer00_acid_1m_diad_2081-2100_ave.nc</li> <li> ETOPO_nitr_kaoafer00_warm_1m_ptrc_2081-2100_ave.nc</li> <li> ETOPO_nitr_kaoafer00_warm_1m_diad_2081-2100_ave.nc</li> <li> ETOPO_nitr_kaoafer00_circ_1m_ptrc_2081-2100_ave.nc</li> <li> ETOPO_nitr_kaoafer00_circ_1m_diad_2081-2100_ave.nc</li> <li> ETOPO_nitr_kaoafer00_full_1m_ptrc_2081-2100_ave.nc</li> <li> ETOPO_nitr_kaoafer00_full_1m_diad_2081-2100_ave.nc</li> <li> ETOPO_nitr_kaoafer00_picontrolalt_1m_ptrc_2081-2100_ave.nc</li> <li> ETOPO_nitr_kaoafer00_picontrolalt_1m_diad_2081-2100_ave.nc</li> <li> ETOPO_nitr_kaoafer00_acidalt_1m_ptrc_2081-2100_ave.nc</li> <li> ETOPO_nitr_kaoafer00_acidalt_1m_diad_2081-2100_ave.nc</li> <li> ETOPO_nitr_kaoafer00_fullalt_1m_ptrc_2081-2100_ave.nc</li> <li> ETOPO_nitr_kaoafer00_fullalt_1m_diad_2081-2100_ave.nc</li> </ul> <p> </p> <p>Naming convention:<br> "ETOPO" - refers to being on a regular 1x1 degree horizontal grid<br> "nitri" - refers to the developed PISCES model with explicit two-step nitrification<br> "kaoafer00" - refers to no iron limitation of AOA <br> "1m" - refers to the timestep resolution, here 1 month. Thus, all data presented here is monthly averaged values.<br> "2ndpicontrol" - refers to preindustrial control run<br> "acid" - refers to the control run + ocean acidification<br> "warm" - refers to the control run + warming<br> "circ" - refers to the control run + circulation change<br> "full" - refers to the control run + ocean acidification + warming + circulation change<br> "picontrolalt" - refers to preindustrial control run (alternative pH parameterisation)<br> "acidalt" - refers to the control run + ocean acidification (alternative pH parameterisation)<br> "fullalt" - refers to the control run + ocean acidification + warming + circulation change (alternative pH parameterisation)<br> <br> Contact: Pearse.Buchanan@liverpool.ac.uk or pbuchanan@carnegiescience.edu</p> <p> </p>
Fig. 1a–d in Description of Epistylis camprubii n. sp., a Species Highly Tolerant to Ammonium and Nitrite
Fig. 1a–d. Morphological and oral infraciliature details of Epistylis camprubii. a – detail of the zooid. PD – peristomial disk; PL – peristomial lip; CV – contractile vacuole; Ma – macronucleus; Mi – micronucleus; b – scheme of a colony; c – oral infraciliature. Pk – polykinety; H – haplokinety; G – germinal kinety; P1 – polykinety 1; P2 – polykinety 2; P3 – polykinety 3; d – morphological characteristics measured. PDd – peristomial disk diameter; PLw – peristomial lip width; PLh – peristomial lip height; Zl – zooid lenght; Zw – zooid width; Sw – stalk width. Scale bars: 25 µm.
Fig. 5. The preferred 18s in Description of Epistylis camprubii n. sp., a Species Highly Tolerant to Ammonium and Nitrite
Fig. 5. The preferred 18s rRNA tree under maximum likelihood (ML). Rectangles on branches denote the support recovered in analyses under alternative inference methods. Left rectangle refers to maximum likelihood (ML), the middle one to Bayesian inference (BI) and the right one to maximum parsimony (MP). Black coloured rectangle indicates bootstrap support> 80 or posterior probability> 0.95, grey rectangle indicates clade recovered but with lower support than the former values, and white rectangle indicates the clade was not recovered. Main Epistylis clade boxed.
Fig. 4 in Description of Epistylis camprubii n. sp., a Species Highly Tolerant to Ammonium and Nitrite
Fig. 4. Frequency of the number of zooids per colony observed in Epistylis camprubii colonies (number of analyzed colonies = 71).
Fig. 3a–e in Description of Epistylis camprubii n. sp., a Species Highly Tolerant to Ammonium and Nitrite
Fig. 3a–e. Images of Epistylis camprubii, after silver staining method. a – view of the longitudinal fibers and the oral infraciliature; b – detail of the aboral trochal band of a feeding zooid; c – aboral trochal band of a zooid during swimmer formation; d–e – oral infraciliature details. H – haplokinety; G – germinal kinety; Pk – polykinety; P1 – polykinety 1; P2 – polykinety 2; P3 – polykinety 3. Scale bars: 15 µm.
Fig. 2a–j in Description of Epistylis camprubii n. sp., a Species Highly Tolerant to Ammonium and Nitrite
Fig. 2a–j. Images of Epistylis camprubii, in vivo. a–b – example of colonies; c–d – two examples of extended zooids; e – zooid during conjugation; f – conjugation; g – contracted zooid; h–j – images of the stalk and branches, from smoother and larger to shorter and thicker. Scale bars: 25 µm.
Data from: Plant ammonium sensitivity is associated with the external pH adaptation, repertoire of nitrogen transporters, and nitrogen requirement
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Phosphate and ammonium from experiemental plots near Toolik Lake, AK from 2003
Soluble reactive phosphorus (SRP) and ammonium in waters from tussock tundra and wet sedge plots near Toolik Lake, AK during the summer of 2003.
Phosphate and ammonium from experiemental plots near Toolik Lake, AK from 2004
Soluble reactive phosphorus (SRP) and ammonium in waters from tussock tundra and wet sedge plots near Toolik Lake, AK during the summer of 2004.
Dissolved organic carbon, phosphate, and ammonium from experiemental plots near Toolik Lake, AK from 2005
Dissolved organic carbon, SRP, and ammonium in waters from tussock tundra and wet sedge plots near Toolik Lake, AK during the summer of 2005 .
Phosphate and ammonium from experiemental plots near Toolik Lake, AK from 2006
Soluble reactive phosphorus (SRP) and ammonium in waters from tussock tundra and wet sedge plots near Toolik Lake, AK during the summer of 2006.
Soil Ammonium and Nitrate rates in and out of the Moose Exclosures on the Tanana River Floodplain , Fall 2001
Soil ammonium and nitrate rates were sampled both inside and out of the moose exclosures located on the Tanana River Floodplain. Samples were collected in the fall of 2001.
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