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  • 1
    In: Marine and Freshwater Research, CSIRO Publishing, Vol. 74, No. 6 ( 2023-3-24), p. 522-534
    Abstract: Context We studied the virus component in the microbial food-web in the tropical coastal Sunda Shelf waters. Aims We investigated viral processes, including the lysogenic to lytic shift dynamics with seawater warming and nutrient enrichment. Methods We sampled nearshore and offshore waters of Peninsular Malaysia to provide a natural trophic gradient for correlational analyses. We also conducted laboratory experiments to investigate the changes in virus production rates and lysogeny, when temperature (range: 25–37°C) and nutrient concentrations (range: 0.1–1.0× marine-broth concentration) were manipulated. Key results Observations showed site-dependent differences in dissolved inorganic nutrient concentration, Chl-a (0.21–3.54 μg L−1) and bacterial abundance (4.09 × 105−9.41 × 105 cells mL−1), but not in viral abundance (measured as virus-like particles or VLP) (1.04 × 106−2.39 × 106 VLP mL−1) and virus production rates (0.59 × 105−4.55 × 105 VLP mL−1 h−1). From laboratory experiments, both warming and nutrient enrichment increased virus production (R2  〉  0.651), decreased lysogeny (R2  〉  0.743), and resulted in an increase of the viral lysis:bacterial production ratio, and a stronger viral control on bacterial production. Conclusions Although both seawater warming and nutrient enrichment increased virus production and reduced lysogeny, nutrient enrichment was a more important factor. Implications The increasing nutrient concentrations in these waters will increase virus production and virus top-down control of bacteria, and drive the ecosystem towards heterotrophy.
    Type of Medium: Online Resource
    ISSN: 1323-1650 , 1448-6059
    Language: English
    Publisher: CSIRO Publishing
    Publication Date: 2023
    detail.hit.zdb_id: 1283028-8
    SSG: 12
    SSG: 21,3
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  • 2
    Online Resource
    Online Resource
    CSIRO Publishing ; 2015
    In:  Marine and Freshwater Research Vol. 66, No. 8 ( 2015), p. 701-
    In: Marine and Freshwater Research, CSIRO Publishing, Vol. 66, No. 8 ( 2015), p. 701-
    Abstract: We investigated the dynamics of attached and free-living bacterial abundance over a period of 18 months in tropical coastal waters of Malaysia. We measured the abundance at both oligotrophic coastal water (Port Dickson) and eutrophic estuary (Klang), and hypothesised that attached bacteria are predominant in eutrophic waters. We found that bacterial abundance was higher at Klang than Port Dickson (Student’s t-test: t=4.87, d.f.=19, P 〈 0.001). Attached bacteria also formed a large fraction of the total bacteria at Klang (75% ±13s.d.) relative to Port Dickson (56% ±22), and showed preference for chlorophyll-a-based particles rather than total suspended solids. The bacterial community structure was clearly different between the two stations but was similar between the attached and free-living bacterial population. Our results showed the importance of attached bacteria in eutrophic water where they could play a major role in carbon and nutrient cycling.
    Type of Medium: Online Resource
    ISSN: 1323-1650
    Language: English
    Publisher: CSIRO Publishing
    Publication Date: 2015
    detail.hit.zdb_id: 1283028-8
    SSG: 12
    SSG: 21,3
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  • 3
    In: Marine and Freshwater Research, CSIRO Publishing, Vol. 53, No. 1 ( 2002), p. 1-
    Abstract: Temporal variations in dissolved oxygen, nutrient concentrations and oxygen utilization rates ( 〈 0.7 m fraction) were recorded for almost two years in the subarctic Funka Bay, Japan. Dissolved inorganic nitrogen ranged from 0 to 26 M, phosphate from 0 to 2 M and silicate from 1 to 64 M. There was evidence of nitrogen limitation. Dissolved oxygen concentration ranged from 130 to 440 M, and decreased to 〈 150 M in the bottom layer in summer. The rate of oxygen utilization, attributed to bacterial respiration, ranged from 0.6 to 9.3 M day–1 at 10 m depth, and from 0.8 to 5.0 M day–1 at 90 m depth, and was the principal mechanism causing the decrease in dissolved oxygen in the bottom layer in the summer. Bacterial growth efficiencies calculated for the 10 m and 90 m depths were similar: 1.6–17.2% and 1.4–23.6%, respectively. With the bacterial growth efficiencies 〈 25%, the bacteria in Funka Bay acted as a net sink of carbon, where 〉 75% of the organic matter flux through bacteria could be mineralized to CO2.
    Type of Medium: Online Resource
    ISSN: 1323-1650
    Language: English
    Publisher: CSIRO Publishing
    Publication Date: 2002
    detail.hit.zdb_id: 1283028-8
    SSG: 12
    SSG: 21,3
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  • 4
    Online Resource
    Online Resource
    CSIRO Publishing ; 2008
    In:  Marine and Freshwater Research Vol. 59, No. 1 ( 2008), p. 10-
    In: Marine and Freshwater Research, CSIRO Publishing, Vol. 59, No. 1 ( 2008), p. 10-
    Abstract: In the present study, the relationship between bacteria and phytoplankton in tropical coastal waters was investigated. The bacterial abundance, bacterial production, chlorophyll a concentration and net primary production were measured at several locations in the coastal waters of Peninsular Malaysia. Chlorophyll a concentration ranged from 0.40 to 32.81 μg L–1, whereas bacterial abundance ranged from 0.1 to 97.5 × 106 cells mL–1. Net primary production ranged from 8.49 to 55.95 μg C L–1 h–1, whereas bacterial production ranged from 0.17 to 70.66 μg C L–1 h–1. In the present study, the carbon conversion factor used to convert bacterial production (cells mL–1 h–1) into carbon units ranged from 10 to 32.8 fg C cell–1, and was estimated from the bacterial size distribution measured at each location. Both phototrophic and heterotrophic biomass (bacteria–chlorophyll a) and activity (bacterial production–net primary production) were significantly correlated, although their correlation coefficients (r2) were relatively low (r2 = 0.188 and r2 = 0.218 respectively). Linear regression analyses provided the following equations to represent the relationship between: bacteria and chlorophyll a (Chl a), log Bacteria = 0.413 log Chl a + 6.057 (P = 0.003); and between bacterial production (BP) and net primary production (NPP), log BP = 0.896 log NPP – 0.394 (P = 0.004), which fitted with published results well. Comparison of annual carbon fluxes confirmed the prevalence of net heterotrophy in these coastal waters, and together with the low correlation coefficients, suggested the role of allochthonous organic matter in supporting heterotrophic activity.
    Type of Medium: Online Resource
    ISSN: 1323-1650
    Language: English
    Publisher: CSIRO Publishing
    Publication Date: 2008
    detail.hit.zdb_id: 1283028-8
    SSG: 12
    SSG: 21,3
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  • 5
    Online Resource
    Online Resource
    CSIRO Publishing ; 2011
    In:  Marine and Freshwater Research Vol. 62, No. 4 ( 2011), p. 414-
    In: Marine and Freshwater Research, CSIRO Publishing, Vol. 62, No. 4 ( 2011), p. 414-
    Abstract: Heterotrophic nanoflagellate (HNF) grazing depends on both temperature and trophic status of an ecosystem. As most microbes already function at their temperature optimum in tropical waters, we hypothesised that HNF grazing rates would be higher in more productive sites such as estuaries than in less productive areas such as coastal waters. We sampled two estuaries and three coastal sites along the Straits of Malacca and the South China Sea near the Malaysia Peninsula. Bacterial abundance ranged 0.9–6.3 × 106 cells mL–1, whereas HNF abundance ranged 1.8–10.1 ×103 cells mL–1. Bacterial production ranged 1.1–12.7 × 105 cells mL–1 h–1, whereas HNF grazing rates were an order of magnitude lower at 1.0–78.5 × 104 cells mL–1 h–1. Bacterial abundance, net bacterial production and HNF grazing rates were higher in estuaries than coastal waters but HNF abundance did not differ between the two areas. Across all stations, HNF grazing rates increased with bacterial production, and accounted for ~33% of bacterial production. Our results suggest that in the tropical waters studied, there was a bacterial production–grazing imbalance. Other loss factors such as viral lysis, sedimentation or the presence of benthic filter feeders could account for this imbalance.
    Type of Medium: Online Resource
    ISSN: 1323-1650
    Language: English
    Publisher: CSIRO Publishing
    Publication Date: 2011
    detail.hit.zdb_id: 1283028-8
    SSG: 12
    SSG: 21,3
    Location Call Number Limitation Availability
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