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  • Haematology  (2)
  • Meteorology and Climatology  (2)
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Years
  • 1
    Publication Date: 2021-05-19
    Description: The present study evaluated the effect of Lactobacillus plantarum as a probiotic on the growth performance and haematological parameters of juvenile rainbow trout (Oncorhynchus mykiss) weighing 29.6±1.8 g immunized with streptococcus/lactococcus bivalent vaccine for 60 days at 16±1.5ºC. Fish were randomly allocated to 4 equal groups: probiotic (g kg^-1 feed equal to 10^8 cells g ^-1 ) supplemented diet group (group P), vaccinated fish fed with a normal diet (group V), vaccinated fish fed with probiotic (group P+V) and unvaccinated fish fed normal diet (group C). Results showed that weight gain, final weight, condition factor and thermalunit growth coefficient were improved in P+V group compared with other groups but was significantly different from groups V and C (p〈0.05). Also, feed conversion ratio in the P+V group was lower than other trails (p〈0.05). In addition, white blood cell count (WBC) in groups V and P+V were significantly higher than in both P and C groups (p〈0.05). Also, PCV was significantly increased (p〈0.05) in both P and P+V groups compared to group V and the control group. No significant difference (p〉0.05) was found in RBC, Hb, MCH, MCHC and MCV levels among the different experimental groups. These data show that application of L. plantarum could be a benefit of vaccinated trout, enhancing fish growth and haematological parameters.
    Description: Published
    Keywords: Lactobacillus plantarum ; Rainbow trout ; Haematological ; Oncorhynchus mykiss ; Streptococcosis ; Lactococcosis ; Probiotic ; Juvenile ; Haematology ; Growth ; Vaccine ; Fish
    Repository Name: AquaDocs
    Type: Journal Contribution , Refereed
    Format: pp.283-295
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  • 2
    Publication Date: 2021-05-19
    Description: The present study evaluated the effect of Lactobacillus plantarum as a probiotic on the growth performance and haematological parameters of juvenile rainbow trout (Oncorhynchus mykiss) weighing 29.6±1.8 g immunized with streptococcus/lactococcus bivalent vaccine for 60 days at 16±1.5ºC. Fish were randomly allocated to 4 equal groups: probiotic (g kg^-1 feed equal to 10^8 cells g ^-1 ) supplemented diet group (group P), vaccinated fish fed with a normal diet (group V), vaccinated fish fed with probiotic (group P+V) and unvaccinated fish fed normal diet (group C). Results showed that weight gain, final weight, condition factor and thermalunit growth coefficient were improved in P+V group compared with other groups but was significantly different from groups V and C (p〈0.05). Also, feed conversion ratio in the P+V group was lower than other trails (p〈0.05). In addition, white blood cell count (WBC) in groups V and P+V were significantly higher than in both P and C groups (p〈0.05). Also, PCV was significantly increased (p〈0.05) in both P and P+V groups compared to group V and the control group. No significant difference (p〉0.05) was found in RBC, Hb, MCH, MCHC and MCV levels among the different experimental groups. These data show that application of L. plantarum could be a benefit of vaccinated trout, enhancing fish growth and haematological parameters.
    Description: Published
    Keywords: Lactobacillus plantarum ; Trout ; Probiotic ; Haematology ; Growth ; Vaccine ; Streptococcosis/lactococcosis
    Repository Name: AquaDocs
    Type: Journal Contribution , Refereed
    Format: pp.283-295
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  • 3
    Publication Date: 2019-05-21
    Description: Transport from the Northern Hemisphere (NH) midlatitudes to the Arctic plays a crucial role in determining the abundance of trace gases and aerosols that are important to Arctic climate via impacts on radiation and chemistry. Here we examine this transport using an idealized tracer with a fixed lifetime and predominantly midlatitude land-based sources in models participating in the Chemistry Climate Model Initiative (CCMI). We show that there is a 25%-45% difference in the Arctic concentrations of this tracer among the models. This spread is correlated with the spread in the location of the Pacific jet, as well as the spread in the location of the Hadley Cell (HC) edge, which varies consistently with jet latitude. Our results suggest that it is likely that the HC-related zonal-mean meridional transport rather than the jet-related eddy mixing is the major contributor to the inter-model spread in the transport of land-based tracers into the Arctic. Specifically, in models with a more northern jet, the HC generally extends further north and the tracer source region is mostly covered by surface southward flow associated with the lower branch of the HC, resulting in less efficient transport poleward to the Arctic. During boreal summer, there are poleward biases in jet location in free-running models, and these models likely underestimate the rate of transport into the Arctic. Models using specified dynamics do not have biases in the jet location, but do have biases in the surface meridional flow, which may result in differences in transport into the Arctic. In addition to the land-based tracer, the midlatitude-to-Arctic transport is further examined by another idealized tracer with zonally uniform sources. With equal sources from both land and ocean, the inter-model spread of this zonally uniform tracer is more related to variations in parameterized convection over oceans rather than variations in HC extent, particularly during boreal winter. This suggests that transport of land-based and oceanic tracers or aerosols towards the Arctic differs in pathways and therefore their corresponding inter-model variabilities result from different physical processes.
    Keywords: Meteorology and Climatology
    Type: GSFC-E-DAA-TN68258 , Atmospheric Chemistry and Physics (ISSN 1680-7316) (e-ISSN 1680-7324); 19; 8; 5511-5528
    Format: application/pdf
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  • 4
    Publication Date: 2019-07-13
    Description: Understanding and modeling the large-scale transport of trace gases and aerosols is important for interpreting past (and projecting future) changes in atmospheric composition. Here we show that there are large differences in the global-scale atmospheric transport properties among the models participating in the IGAC SPARC ChemistryClimate Model Initiative (CCMI). Specifically, we find up to 40% differences in the transport timescales connecting the Northern Hemisphere (NH) midlatitude surface to the Arctic and to Southern Hemisphere high latitudes, where the mean age ranges between 1.7 and 2.6 years. We show that these differences are related to large differences in vertical transport among the simulations, in particular to differences in parameterized convection over the oceans. While stronger convection over NH midlatitudes is associated with slower transport to the Arctic, stronger convection in the tropics and subtropics is associated with faster interhemispheric transport. We also show that the differences among simulations constrained with fields derived from the same reanalysis products are as large as (and in some cases larger than) the differences among free-running simulations, most likely due to larger differences in parameterized convection. Our results indicate that care must be taken when using simulations constrained with analyzed winds to interpret the influence of meteorology on tropospheric composition.
    Keywords: Meteorology and Climatology
    Type: GSFC-E-DAA-TN61613 , GSFC-E-DAA-TN65002 , Atmospheric Chemistry and Physics (ISSN 1680-7316) (e-ISSN 1680-7324); 18; 10; 7217–7235
    Format: text
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