Bacterioplankton counting methods

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Short description: Methods for the estimation of the abundance of bacterioplankton in a specific body of water

Bacterioplankton counting is the estimation of the abundance of bacterioplankton in a specific body of water, which is useful information to marine microbiologists. Various counting methodologies have been developed over the years to determine the number present in the water being observed. Methods used for counting bacterioplankton include epifluorescence microscopy, flow cytometry, measures of productivity through frequency of dividing cells (FDC), thymidine incorporation, and leucine incorporation.

Factors such as salinity, temperature, latitude, various nutrient levels, water movement and the presence of other organisms can affect bacterioplankton enumeration.[1][2][3][4][5] Changes in these factors affect the bacterioplankton count, causing it to vary by body of water, location, distance from shore and season.[6][7][8]

Bacterioplankton count is usually expressed in cells per ml (cells ml−1).

Uses

In understanding marine microbiology and the aquatic ecosystem, bacterioplankton counts can be useful. Observation of bacterioplankton number can provide more information in the following:

  • Processes involved in various nutrient cycling in the aquatic systems[9][10]
  • For aquatic productivity [11]
  • For determining environmental changes, especially extremes [12]
    • Variation in bacterioplankton count not derived by seasonal adjustments can provide correlation with environmental stresses such as having a significant shift in nutrient levels within a body of water[13][14][15]
  • Nutrient composition in aquatic ecosystem [16]
  • Abundance and conditions of other aquatic organisms (i.e. shrimp) [17]

Epifluorescence microscopy

Fluorescence microscope light pathway

Epifluorescence microscopy is an advanced optical microscope technique that relies on the use of fluorescent dyes that bind to specific biological markers, which then emit a distinctive emission spectra that is identified through the lens. Fluorescent dyes include DAPI, Acridine Orange, SYBR Green 1, and YO-PRO-1, all of which are capable of staining both DNA and RNA structures in biological samples such as bacteria and viruses.[18][19][20][21] However, DNA staining is primarily used for bacterial cell identification. With modern epifluorescence microscopy, the industry standard for estimating and counting bacterial cell quantities is by the use of a DAPI stain.[22] This technique can be performed for samples from a wide range of environments and locations, such as seawater, various sources of freshwater, as well as soils and sediments.[22]

Enumeration technique

In a standard experiment, prepared bacterial samples are placed onto counting slides and then viewed under an epifluorescence microscope. Magnification is set to a level where the 0.1 X 0.1 mm square units on the counting slide are clearly visible.[23] To quantify the bacteria, cells are counted in 5-30 random square unit field-of-views and an average bacteria count per field is tabulated.[22] This value is then extrapolated to estimate the total bacterial cell-count per mL by determining the total number of fields-of-view on the slide deposition area and multiplying this by the average bacterial count per counting unit.[23]

Reliability

To enumerate bacterial cell quantities, only small portions of bacteria in a sample are physically counted for logistical reasons, upon which total abundances are estimated by extrapolation. Mean values are then used for comparison among samples. However the accuracy of this technique, where tabulation of only a small subset is used to estimate total abundance quantities, has been brought into question.[22] Primarily, it has been shown that the distribution of bacterial cells on counting slides can be uneven and inconsistent.[22] In addition, to get a legitimate estimate of bacterial counts by using this technique, it has been suggested that more than 350 individual cells, from 20 fields of view must be measured.[22] This can be not only time-consuming, but difficult to achieve in certain samples.

Flow Cytometry

The inner working of a flow cytometer

Flow cytometric analysis (or, flow cytometry) is a common procedure in many clinical applications. However, despite its discovery more than three decades ago, its adoption by aquatic microbial ecology in enumeration of bacterioplankton, has been relatively slow.[24] Its use is yet to surpass epifluorescence microscopy.[25] Despite both abundance estimation techniques being relatively accurate, flow cytometry is less prone to human error, more precise, pertains a higher resolution and is capable of examining tens of thousands of cells in a matter of minutes.[24] Flow cytometry is also able to provide information regarding size, activity and morphology of cells besides abundance of cells.[26]

Flow cytometry can be used to distinguish and quantify both photosynthetic and non-photosynthetic bacterioplankton.[26] Quantification of photosynthetic prokaryotes such as cyanobacteria and picoeukaryotic algae is made possible by the ability of photosynthetic pigments to fluoresce.[27] For instance, the different formation of photosynthetic pigments in the two major photosynthetic prokaryotes, Prochlorococcus and Synechococcus, enable their very distinction.[28][29][30] Prochlorococcus contains divynyl-chlorophylls a and b which display solely red fluorescence under excitation by blue or UV light, while Synechococcus emits both orange and red fluorescence; orange from phycobilins and red from chlorophyll. Besides fluorescence, Prochlorococcus and Synechococus are of significantly different sizes and hence deliver different scatter signals upon flow cytometric analysis. This further helps in their differentiation.[31] Quantification of prochlorococcus is considered a major breakthrough as it has almost only been possible through flow cytometry. This is due to the inability of epifluorescence microscopy to detect the low chlorophyll autofluorescence present in Prochlorococcus.[26]

Besides photosynthetic bacterioplankton, non-photosynthetic bacterioplankton can also be enumerated by flow cytometry. This is done via DNA or food vacuole staining.[27] Flow cytometry has especially been successful at differentiating Prochloroccocus from heterotrophic bacteria, whose counts were initially confounded due to their similar size.

Use of epifluorescence microscopy over flow cytometry in many microbial ecology labs can be blamed on a number of economic and practical factors. First, the use of commercial flow cytometers requires the expertise of a rigorously trained technician. Second, flow cytometers are fairly expensive in comparison to epi-fluorescence microscopy apparatus. Third, many flow cytometers are designed to examine blood cells; oceanic bacteria are relatively small and hence approach limit of resolution in many commercial flow cytometers.[32]

Enumeration Process

Flow cytometric quantification of bacterioplankton involves four steps: fixation, staining, data processing and data interpretation.

Fixation

Fixation is done to not only preserve sample, but also to increase permeability of cells to stains.[24] However, most common fixation agents have the capacity to alter cells by changing certain aspects such as size, how light is scattered, autofluorescence and nucleic acids. This is problematic as flow cytometric distinction of cells relies on these qualities. Some fixatives also lead to complete loss of cells.[24] Presently, some of the agents used in the fixation process include two variations of formaldehyde (formalin and paraformaldehyde), 70% ethanol, glutaraldehyde and TCA.[33] It is presumed that the best fixation agent for protein and nucleic acids is paraformaldehyde due to its ability to swiftly enter cells.[24]

Staining

In flow cytometry, staining enables distinction of bacterioplankton from non-bacterial particles. It involves the incubation of sample in the wide array of fluorochromes such as UV-excited dyes (DAPI and Hoechst 33342) and blue-light-excited nucleic acid dyes (TO-PRO-1,TOTO-1, SYBR Green I).[31] For a long time, flow cytometers utilized UV-excited dyes to examine bacterioplankton which could be used in either low-cost flow cytometers with limited sensitivity, or expensive flow cytometers with the high sensitivity needed to distinguish heterotrophic bacteria from autotrophs. The introduction of blue-excited dyes such as SYBR Green I, enabled high quality flow cytometric analysis of bacterioplankton on low-cost, high-sensitivity flow cytometers.[31]

Incubation times for optimum staining varies from compound to compound. UV-excited dyes can require an hour or more while blue-light-excited dyes require a mere 15 minutes.[24]

Staining can be accompanied by buffers such as Triton X-100 which make cells more permeable to stains. They are especially used in cell-impermeant dyes like TO-PRO-1. Buffers are also used to dilute dyes sensitive to ionic strength such as Picogreen, YO-PRO-1 and YOYO-1. The use of buffers however, can be harmful to cells as buffers like Triton-X-100 can not only extinguish chlorophyll fluorescence, but also create unwanted background fluorescence. This can increase the difficulty of distinguishing between heterotrophic bacteria and autotrophic prokaryotes.[24]

Counting

Cytometric analysis of cyanobacteria

In a flow cytometric analysis, over 200 cells pass in front of a laser beam or mercury lamp every second, a cell at a time. Photomultipliers gather the amount of light each particle scatters and the fluorescence emitted upon excitation. This information is then internalized and interpreted by the system as an event. However, despite the ability of flow cytometers to count cells with very little effort, most have no way of determining actual concentration of cells. This can be determined through a variety of methods including, use of reference beads whose quantity is pre-determined (helps determine the ratio of bacteria to beads), weight measurements before and after experiment and daily calibration of flow.[24]

A big advantage of flow cytometers is their ability to identify different populations of bacterioplankton. This discrimination is done via analysis of four factors; light scatter, green fluorescence, blue fluorescence and red fluorescence. Light scatter analysis is inadequate alone and is often examined alongside fluorescence for a number of reasons; first, sea water contains many particles that scatter light like bacteria. Second, the sizes of many oceanic bacteria approach limit of resolution. The amount of light scattered by cells is determined by not only size of cells, but also internal structure, refractive index, shape and orientation of particle. Scattered light is classified into either forward scatter (FSC) or side scatter (SSC). The former has been associated with cell volume and mass while the latter has been associated with index of refraction, content and granularity of cells [24]

When cell concentrations are higher than 2.5 × 106 cells per ml, the likelihood of more than once cell passing in close proximity and being recorded as a single event is magnified. This is known as coincidence and can be easily avoided by diluting sample before hand[31]

Measures of productivity

Frequency of dividing cells

Frequency of dividing cells (FDC) is a method used to predict the average growth rate of an aquatic heterotrophic bacterial community.[34] The method uses cell division, specifically septum formation, as a proxy for growth rate.[34] Cells are considered divided, when cavities between individual cells (invagination) are observed under epifluorescence microscopy.[34] FDC is based on the assumption that there relationship between the proportion of cells currently dividing and the growth rate in a bacterial community.[35]

Thymidine incorporation

Thymidine incorporation is one of the most extensively used methods to estimate bacterial growth.[36] Thymidine is a precursor for DNA, and DNA synthesis can be measured by tritiated thymidine incorporation into nucleic acids.[37] Thymidine incorporation measures growth based on rates of DNA synthesis, using the assumption that only growing cells can incorporate the radioactive thymidine to synthesize DNA.[38]

Weaknesses of this procedure include labeling of other molecules besides DNA when tritiated thymidine is added to a sample.[36] In cases of carbon limitation, thymidine may also be used as a carbon source instead of as a DNA precursor.[36] Results of thymidine incorporation experiments may be misleading when the proportion of thymidine incorporated into DNA compared to other molecules is not known.[36]

Leucine incorporation

Leucine incorporation is used as a measure of protein synthesis in aquatic bacteria communities.[39] Radio-labeled leucine is added to samples, and its accumulation into proteins, the hot trichloroacetic acid (CA)-insoluble parts of the cell is determined.[39] The samples are then collected on membrane filter.[39] Leucine protein is taken up by more than 50% of aquatic bacterial populations, and leucine incorporation can be used to estimate nitrogen utilization in the bacterial community.[39]

Marine seasonal succession dynamics

As bacterial populations have unique metabolisms and resource preferences, the use of high-resolution time-series analysis of bacterial compositions allows for the identification of patterns in seasonal bacterial succession.[40] Differences in bacterial community compositions give rise to particular permutations of interspecies bacterial interactions with photosynthetic plankton, protist grazers, and phages thereby impacting seasonality dynamics. Statistical methods used to verify patterns in population dynamics and composition are demonstrated to be replicable over some years, and environmental factors served as predictors of these temporal patterns.[41]

Seasonal succession in temperate regions

As seasonal successions of phytoplankton populations follow a consistent recurring pattern, bacterial dynamics and phytoplankton succession can be correlated.[40] In general, seasonal changes in bacterial composition follow changes in temperature and chlorophyll a, while nutrient availability limits bacterioplankton growth rates.[42][43][44][45][6][46] During water column mixing in late autumn/winter, nutrients brought to the surface kicks start a distinct diatom spring bloom followed by dinoflagellates.[40] After the spring bloom, bacterial production and growth become elevated due to the release of Dissolved organic matter (DOM) from phytoplankton decay.[47][48] In this early succession stage, members of the class Flavobacteria (Bacteroidetes) are typically the dominant components of the bacterial community.[49][50] Genome analysis and meta-transcriptomics have uncovered the presence of bacteria containing multiple hydrolytic enzymes facilitating the degradation and assimilation of DOM.[51][52][53][54] During spring blooms, some members of the Roseobacter clade (Alphaproteobacteria) and some Gammaproteobacteria are usually associated with DOM degradation.[48][49] As temperatures increase and the nutrients from the spring bloom gets depleted, smaller phytoplankton and cyanobacteria grow in the now oligotrophic waters.[40]

As waters become stratified in summer, Roseobacter, SAR86 (Gammaproteobacteria), and SAR11 (Alphaproteobacteria) clades of bacteria increase in abundance.[55][56] The frequently observed autumn diatom and dinoflagellate blooms are correlated with supplementary nutrient inputs and high-frequency sampling in the Baltic Sea found that in autumn, Actinomycetota generally increase followed by different autumn-specific Flavobacteria, SAR11, and Planctomycetota.[49]

In the Mediterranean Sea, deep winter mixing allows members of the SAR11 clade to achieve increased diversity as the oligotrophic populations that once dominated during the summer stratification die off slowly.[57] Among archaea in the Mediterranean Sea, Nitrososphaerota (formerly Thaumarchaeota) Marine Group I (MGI) and Euryarchaeota Marine Group II (MGII.B) populations became dominant in winter.[58] While in the Baltic Sea, winter mixing brings Campylobacterota and archaea populations to the surface from their deep habitat.[49]

References

  1. ↑ Long, Richard A.; Azam, Farooq (2001-12-05). "Microscale patchiness of bacterioplankton assemblage richness in seawater". Aquatic Microbial Ecology 26 (2): 103–113. doi:10.3354/ame026103. 
  2. ↑ He, Jianfeng; Zhang, Fang; Lin, Ling; Ma, Yuxin; Chen, Jianfang (2012). "Bacterioplankton and picophytoplankton abundance, biomass, and distribution in the Western Canada Basin during summer 2008". Deep Sea Research Part II: Topical Studies in Oceanography 81-84: 36–45. doi:10.1016/j.dsr2.2012.08.018. Bibcode: 2012DSRII..81...36H. 
  3. ↑ Wei, Chaoling; Bao, Sumin; Zhu, Xinyan; Huang, Xiangming (2008). "Spatio-temporal variations of the bacterioplankton community composition in Chaohu Lake, China". Progress in Natural Science 18 (9): 1115–1122. doi:10.1016/j.pnsc.2008.04.005. 
  4. ↑ López-Flores, Rocío; Boix, Dani; Badosa, Anna; Brucet, Sandra; Quintana, Xavier D. (2009). "Environmental factors affecting bacterioplankton and phytoplankton dynamics in confined Mediterranean salt marshes (NE Spain)". Journal of Experimental Marine Biology and Ecology 369 (2): 118–126. doi:10.1016/j.jembe.2008.11.003. 
  5. ↑ Medvinsky, Alexander B.; Adamovich, Boris V.; Aliev, Rubin R.; Chakraborty, Amit; Lukyanova, Elena V.; Mikheyeva, Tamara M.; Nikitina, Ljudmila V.; Nurieva, Nailya I. et al. (2017). "Temperature as a factor affecting fluctuations and predictability of the abundance of lake bacterioplankton". Ecological Complexity 32: 90–98. doi:10.1016/j.ecocom.2017.10.002. 
  6. ↑ 6.0 6.1 "Pyrosequencing reveals contrasting seasonal dynamics of taxa within Baltic Sea bacterioplankton communities". The ISME Journal 4 (2): 171–81. February 2010. doi:10.1038/ismej.2009.108. PMID 19829318. 
  7. ↑ "Pronounced summer to winter differences and higher wintertime richness in coastal Antarctic marine bacterioplankton". Environmental Microbiology 14 (3): 617–29. March 2012. doi:10.1111/j.1462-2920.2011.02601.x. PMID 22003839. 
  8. ↑ Straza, Tiffany R. A.; Ducklow, Hugh W.; Murray, Alison E.; Kirchman, David L. (2010-11-01). "Abundance and single-cell activity of bacterial groups in Antarctic coastal waters". Limnology and Oceanography 55 (6): 2526–2536. doi:10.4319/lo.2010.55.6.2526. Bibcode: 2010LimOc..55.2526S. 
  9. ↑ Currie, David J.; Kalff, Jaap (March 1984). "The relative importance of bacterioplankton and phytoplankton in phosphorus uptake in freshwater1". Limnology and Oceanography 29 (2): 311–321. doi:10.4319/lo.1984.29.2.0311. Bibcode: 1984LimOc..29..311C. 
  10. ↑ "Investigating Influential Factors on Bacterioplankton Community Composition: Results from a Field Study of Five Mesotrophic Lakes". Microbial Ecology 42 (4): 598–605. December 2001. doi:10.1007/s00248-001-0031-y. PMID 12024242. 
  11. ↑ Cotner, James B.; Biddanda, Bopaiah A. (2002-03-01). "Small Players, Large Role: Microbial Influence on Biogeochemical Processes in Pelagic Aquatic Ecosystems". Ecosystems 5 (2): 105–121. doi:10.1007/s10021-001-0059-3. 
  12. ↑ "Total resistance of native bacteria as an indicator of changes in the water environment". Environmental Pollution 174: 85–92. March 2013. doi:10.1016/j.envpol.2012.11.005. PMID 23246751. 
  13. ↑ Chen, Xinxin; Wang, Kai; Guo, Annan; Dong, Zhiying; Zhao, Qunfen; Qian, Jie; Zhang, Demin (2016). "Excess phosphate loading shifts bacterioplankton community composition in oligotrophic coastal water microcosms over time". Journal of Experimental Marine Biology and Ecology 483: 139–146. doi:10.1016/j.jembe.2016.07.009. 
  14. ↑ Dai, Wenfang; Zhang, Jinjie; Tu, Qichao; Deng, Ye; Qiu, Qiongfen; Xiong, Jinbo (2017). "Bacterioplankton assembly and interspecies interaction indicating increasing coastal eutrophication". Chemosphere 177: 317–325. doi:10.1016/j.chemosphere.2017.03.034. PMID 28319885. Bibcode: 2017Chmsp.177..317D. http://ir.rcees.ac.cn/handle/311016/39611. 
  15. ↑ Urakawa, Hidetoshi; Bernhard, Anne E. (2017). "Wetland management using microbial indicators". Ecological Engineering 108: 456–476. doi:10.1016/j.ecoleng.2017.07.022. 
  16. ↑ "Effect of nutrient loading on bacterioplankton community composition in lake mesocosms". Microbial Ecology 51 (2): 137–46. February 2006. doi:10.1007/s00248-005-0049-7. PMID 16435168. 
  17. ↑ Zhang, Demin; Wang, Xin; Xiong, Jinbo; Zhu, Jianlin; Wang, Yinong; Zhao, Qunfen; Chen, Heping; Guo, Annan et al. (2014). "Bacterioplankton assemblages as biological indicators of shrimp health status". Ecological Indicators 38: 218–224. doi:10.1016/j.ecolind.2013.11.002. 
  18. ↑ Tanious, Farial A.; Veal, James M.; Buczak, Henryk; Ratmeyer, Lynda S.; Wilson, W. David (1992-03-31). "DAPI (4',6-diamidino-2-phenylindole) binds differently to DNA and RNA: minor-groove binding at AT sites and intercalation at AU sites". Biochemistry 31 (12): 3103–3112. doi:10.1021/bi00127a010. PMID 1372825. 
  19. ↑ Gonzalez, Karen; Mcvey, Scott; Cunnick, Jess; Udovichenko, Igor P.; Takemoto, Dolores J. (1995). "Acridine orange differential staining of total DNA and RNA in normal and galactosemic lens epithelial cells in culture using flow cytometry". Current Eye Research 14 (4): 269–273. doi:10.3109/02713689509033525. PMID 7541739. 
  20. ↑ Noble, Rachel T.; Fuhrman, Jed A. (1998-02-13). "Use of SYBR Green I for rapid epifluorescence counts of marine viruses and bacteria". Aquatic Microbial Ecology 14 (2): 113–118. doi:10.3354/ame014113. 
  21. ↑ "Application of the novel nucleic acid dyes YOYO-1, YO-PRO-1, and PicoGreen for flow cytometric analysis of marine prokaryotes". Applied and Environmental Microbiology 62 (5): 1649–55. May 1996. doi:10.1128/AEM.62.5.1649-1655.1996. PMID 8633863. Bibcode: 1996ApEnM..62.1649M. 
  22. ↑ 22.0 22.1 22.2 22.3 22.4 22.5 Muthukrishnan, Thirumahal; Govender, Anesh; Dobretsov, Sergey; Abed, Raeid M. M. (2017-01-08). "Evaluating the Reliability of Counting Bacteria Using Epifluorescence Microscopy". Journal of Marine Science and Engineering 5 (1): 4. doi:10.3390/jmse5010004. 
  23. ↑ 23.0 23.1 O'Connor, John T.; O'Connor, Tom; Twait, Rick (2009). Water Treatment Plant Performance Evaluations and Operations. John Wiley & Sons, Inc.. pp. 193–198. doi:10.1002/9780470431474.app1. ISBN 9780470431474. 
  24. ↑ 24.0 24.1 24.2 24.3 24.4 24.5 24.6 24.7 24.8 Gasol, Josep M.; Giorgio, Paul A. del (2000-06-30). "Using flow cytometry for counting natural planktonic bacteria and understanding the structure of planktonic bacterial communities". Scientia Marina 64 (2): 197–224. doi:10.3989/scimar.2000.64n2197. ISSN 1886-8134. 
  25. ↑ Giorgio, Paul A. del; Bird, David F.; Prairie, Yves T.; Planas, Dolors (1996-06-01). "Flow cytometric determination of bacterial abundance in lake plankton with the green nucleic acid stain SYTO 13". Limnology and Oceanography 41 (4): 783–789. doi:10.4319/lo.1996.41.4.0783. ISSN 1939-5590. Bibcode: 1996LimOc..41..783G. 
  26. ↑ 26.0 26.1 26.2 Sieracki, Michael E.; Haugen, Elin M.; Cucci, Terry L. (1995-08-01). "Overestimation of heterotrophic bacteria in the Sargasso Sea: direct evidence by flow and imaging cytometry". Deep Sea Research Part I: Oceanographic Research Papers 42 (8): 1399–1409. doi:10.1016/0967-0637(95)00055-B. ISSN 0967-0637. Bibcode: 1995DSRI...42.1399S. 
  27. ↑ 27.0 27.1 Zubkov, M. V.; Burkill, P. H.; Topping, J. N. (2007-01-01). "Flow cytometric enumeration of DNA-stained oceanic planktonic protists". Journal of Plankton Research 29 (1): 79–86. doi:10.1093/plankt/fbl059. 
  28. ↑ WATERBURY, JOHN B.; WATSON, STANLEY W.; GUILLARD, ROBERT R. L.; BRAND, LARRY E. (January 1979). "Widespread occurrence of a unicellular, marine, planktonic, cyanobacterium". Nature 277 (5694): 293–294. doi:10.1038/277293a0. ISSN 1476-4687. Bibcode: 1979Natur.277..293W. 
  29. ↑ Chisholm, Sallie W.; Frankel, Sheila L.; Goericke, Ralf; Olson, Robert J.; Palenik, Brian; Waterbury, John B.; West-Johnsrud, Lisa; Zettler, Erik R. (1992-02-01). "Prochlorococcus marinus nov. gen. nov. sp.: an oxyphototrophic marine prokaryote containing divinyl chlorophyll a and b". Archives of Microbiology 157 (3): 297–300. doi:10.1007/BF00245165. ISSN 0302-8933. 
  30. ↑ Chisholm, Sallie W.; Olson, Robert J.; Zettler, Erik R.; Goericke, Ralf; Waterbury, John B.; Welschmeyer, Nicholas A. (July 1988). "A novel free-living prochlorophyte abundant in the oceanic euphotic zone". Nature 334 (6180): 340–343. doi:10.1038/334340a0. ISSN 1476-4687. Bibcode: 1988Natur.334..340C. 
  31. ↑ 31.0 31.1 31.2 31.3 "Enumeration and Cell Cycle Analysis of Natural Populations of Marine Picoplankton by Flow Cytometry Using the Nucleic Acid Stain SYBR Green I". Applied and Environmental Microbiology 63 (1): 186–93. January 1997. doi:10.1128/AEM.63.1.186-193.1997. PMID 16535483. Bibcode: 1997ApEnM..63..186M. 
  32. ↑ Giorgio, Paul A. del; Bird, David F.; Prairie, Yves T.; Planas, Dolors (June 1996). "Flow cytometric determination of bacterial abundance in lake plankton with the green nucleic acid stain SYTO 13". Limnology and Oceanography 41 (4): 783–789. doi:10.4319/lo.1996.41.4.0783. Bibcode: 1996LimOc..41..783G. 
  33. ↑ "Flow Cytometric Analysis of Characteristics of Hybridization of Species-Specific Fluorescent Oligonucleotide Probes to rRNA of Marine Nanoflagellates". Applied and Environmental Microbiology 63 (3): 938–44. March 1997. doi:10.1128/AEM.63.3.938-944.1997. PMID 16535558. Bibcode: 1997ApEnM..63..938R. 
  34. ↑ 34.0 34.1 34.2 "Frequency of dividing cells, a new approach to the determination of bacterial growth rates in aquatic environments". Applied and Environmental Microbiology 37 (5): 805–12. May 1979. doi:10.1128/AEM.37.5.805-812.1979. PMID 16345378. Bibcode: 1979ApEnM..37..805H. 
  35. ↑ "Frequency of dividing cells as an estimator of bacterial productivity". Applied and Environmental Microbiology 42 (1): 23–31. July 1981. doi:10.1128/AEM.42.1.23-31.1981. PMID 16345812. Bibcode: 1981ApEnM..42...23N. 
  36. ↑ 36.0 36.1 36.2 36.3 "Determining [HThymidine Incorporation into Bacterioplankton DNA: Improvement of the Method by DNase Treatment"]. Applied and Environmental Microbiology 53 (8): 1977–9. August 1987. doi:10.1128/AEM.53.8.1977-1979.1987. PMID 16347424. Bibcode: 1987ApEnM..53.1977S. 
  37. ↑ "Estimating Bacterioplankton Production by Measuring [3Hthymidine Incorporation in a Eutrophic Swedish Lake"]. Applied and Environmental Microbiology 45 (6): 1709–1721. June 1983. doi:10.1128/AEM.45.6.1709-1721.1983. PMID 16346304. Bibcode: 1983ApEnM..45.1709B. 
  38. ↑ "Bacterioplankton secondary production estimates for coastal waters of British Columbia, Canada, Antarctica, and California, USA". Applied and Environmental Microbiology 39 (6): 1085–1095. July 1980. doi:10.1128/AEM.39.6.1085-1095.1980. PMID 16345577. 
  39. ↑ 39.0 39.1 39.2 39.3 "Leucine incorporation and its potential as a measure of protein synthesis by bacteria in natural aquatic systems". Applied and Environmental Microbiology 49 (3): 599–607. March 1985. doi:10.1128/AEM.49.3.599-607.1985. PMID 3994368. Bibcode: 1985ApEnM..49..599K. 
  40. ↑ 40.0 40.1 40.2 40.3 "Marine Bacterioplankton Seasonal Succession Dynamics". Trends in Microbiology 25 (6): 494–505. June 2017. doi:10.1016/j.tim.2016.12.013. PMID 28108182. 
  41. ↑ "Annually reoccurring bacterial communities are predictable from ocean conditions". Proceedings of the National Academy of Sciences of the United States of America 103 (35): 13104–9. August 2006. doi:10.1073/pnas.0602399103. PMID 16938845. Bibcode: 2006PNAS..10313104F. 
  42. ↑ Pinhassi, Jarone; Hagström, Åke (2000-06-15). "Seasonal succession in marine bacterioplankton". Aquatic Microbial Ecology 21 (3): 245–256. doi:10.3354/ame021245. 
  43. ↑ Pinhassi, Jarone; Gómez-Consarnau, Laura; Alonso-Sáez, Laura; Sala, Maria Montserrat; Vidal, Montserrat; Pedrós-Alió, Carlos; Gasol, Josep M. (2006-10-10). "Seasonal changes in bacterioplankton nutrient limitation and their effects on bacterial community composition in the NW Mediterranean Sea". Aquatic Microbial Ecology 44 (3): 241–252. doi:10.3354/ame044241. 
  44. ↑ "Bacterial community dynamics during the winter-spring transition in the North Sea". FEMS Microbiology Ecology 59 (3): 622–37. March 2007. doi:10.1111/j.1574-6941.2006.00238.x. PMID 17381518. 
  45. ↑ "The seasonal structure of microbial communities in the Western English Channel". Environmental Microbiology 11 (12): 3132–9. December 2009. doi:10.1111/j.1462-2920.2009.02017.x. PMID 19659500. https://darchive.mblwhoilibrary.org/bitstream/1912/3133/1/EMI-2009-0253%20-%20resubmitted%20version.pdf. 
  46. ↑ "Defining seasonal marine microbial community dynamics". The ISME Journal 6 (2): 298–308. February 2012. doi:10.1038/ismej.2011.107. PMID 21850055. 
  47. ↑ "Dynamics of bacterial community composition and activity during a mesocosm diatom bloom". Applied and Environmental Microbiology 66 (2): 578–87. February 2000. doi:10.1128/AEM.66.2.578-587.2000. PMID 10653721. Bibcode: 2000ApEnM..66..578R. 
  48. ↑ 48.0 48.1 "Master recyclers: features and functions of bacteria associated with phytoplankton blooms". Nature Reviews. Microbiology 12 (10): 686–98. October 2014. doi:10.1038/nrmicro3326. PMID 25134618. 
  49. ↑ 49.0 49.1 49.2 49.3 "Disentangling seasonal bacterioplankton population dynamics by high-frequency sampling". Environmental Microbiology 17 (7): 2459–76. July 2015. doi:10.1111/1462-2920.12720. PMID 25403576. 
  50. ↑ Alderkamp, Anne-Carlijn; Sintes, Eva; Herndl, Gerhard J. (2006-12-21). "Abundance and activity of major groups of prokaryotic plankton in the coastal North Sea during spring and summer". Aquatic Microbial Ecology 45 (3): 237–246. doi:10.3354/ame045237. 
  51. ↑ "Ecology of marine Bacteroidetes: a comparative genomics approach". The ISME Journal 7 (5): 1026–37. May 2013. doi:10.1038/ismej.2012.169. PMID 23303374. 
  52. ↑ "Substrate-controlled succession of marine bacterioplankton populations induced by a phytoplankton bloom". Science 336 (6081): 608–11. May 2012. doi:10.1126/science.1218344. PMID 22556258. Bibcode: 2012Sci...336..608T. 
  53. ↑ "Recurring patterns in bacterioplankton dynamics during coastal spring algae blooms". eLife 5: e11888. April 2016. doi:10.7554/eLife.11888. PMID 27054497. 
  54. ↑ "Seasonal microbial community dynamics correlate with phytoplankton-derived polysaccharides in surface coastal waters". The ISME Journal 8 (1): 245–8. January 2014. doi:10.1038/ismej.2013.178. PMID 24132076. 
  55. ↑ Agawin, Nona S. R.; Duarte, Carlos M.; Agustí, Susana (1998-09-03). "Growth and abundance of Synechococcus sp. in a Mediterranean Bay: seasonality and relationship with temperature". Marine Ecology Progress Series 170: 45–53. doi:10.3354/meps170045. Bibcode: 1998MEPS..170...45A. 
  56. ↑ "Seasonality in bacterial diversity in north-west Mediterranean coastal waters: assessment through clone libraries, fingerprinting and FISH". FEMS Microbiology Ecology 60 (1): 98–112. April 2007. doi:10.1111/j.1574-6941.2006.00276.x. PMID 17250750. 
  57. ↑ "Seasonal dynamics of active SAR11 ecotypes in the oligotrophic Northwest Mediterranean Sea". The ISME Journal 9 (2): 347–60. February 2015. doi:10.1038/ismej.2014.129. PMID 25238399. 
  58. ↑ "Structure of the rare archaeal biosphere and seasonal dynamics of active ecotypes in surface coastal waters". Proceedings of the National Academy of Sciences of the United States of America 110 (15): 6004–9. April 2013. doi:10.1073/pnas.1216863110. PMID 23536290. Bibcode: 2013PNAS..110.6004H. 



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