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Assessment of a sheltered euhaline area of the Southeastern Bay of Biscay to sustain bivalve production in terms of phytoplankton community composition

100%

Bilbao J., Muniz O., Rodriguez J. G., Revilla M., Laza-Matinez A., Seoane S.

Oceanologia

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2021

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tom 63

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nr 1

2

Change of physico-chemical conditions and phytoplankton composition in a humic lake caused by liming and fertilisation

100%

Hutorowicz A.

International Journal of Ecohydrology and Hydrobiology

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2003

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tom 03

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nr 2

173-183

3

Phytoplankton composition and abundance at surface depths within different lake habitats

100%

Marshall H. G., Burchardt L., Kokocinski M., Stefaniak K., Semcheski M.

Oceanological and Hydrobiological Studies

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2007

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tom 36

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nr Suppl.1

4

Relationship among biomass of algae and concentration of chlorophyll a, against the taxonomic structure of phytoplankton in three lakes on Lublin Polesie region

84%

Mencfel R.

Teka Komisji Ochrony i Kształtowania Środowiska Przyrodniczego

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2013

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tom 10

5

Recent trophic changes and phytoplankton composition in lake Drummond, within the Dismal Swamp, Virginia

84%

Marshall H. G.

Seria Biologiczna. Uniwersytet im. Adama Mickiewicza w Poznaniu

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1990

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tom 43

6

Seasonal changes in phytoplankton composition and diversity in the Epe Lagoon, Nigeria

84%

Nwankwo D. I.

Acta Hydrobiologica

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1998

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tom 40

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nr 2

7

Seasonal changes occurring over four years in a reservoir's phytoplankton composition

84%

Kozak A.

Polish Journal of Environmental Studies

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2005

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tom 14

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nr 4

In the period 1993-1996, the Maltański Reservoir was found to host 233 phytoplankton taxa, belonging to 9 taxonomic classes. The most numerous were cyanobacteria. After regression of the Cyanobacteria-induced water blooming in the spring, chrysophytes, cryptophytes, green algae or diatoms were dominant. The remaining taxonomic groups were clearly less numerous. Changes in the number of a cells and of individual organisms and changes in the phytoplankton biomass were monitored in seasonal cycles. The shares of individual size fractions, i. e., of microplankton (>60 μm) and nanoplankton (2-60 μm) in the total numerical force and biomass of phytoplankton were estimated. Considering the size structure of phytoplankton organisms, nanoplankton comprised 50-100%, particularly in the period between November, 1994 and April, 1995, as well as in the early summer (May, June). Microplankton prevailed in total numbers of organisms between April and October, in particular. High correlation were noted between the number of organisms, number of cells and biomass of phytoplankton on one hand and the physico-chemical parameters of water such as transparency, temperature, pH, BOD₅ index, conductivity and total phosphorus on the other. This pointed to the role played by these parameters in the development of algae. On the other hand, dissolved phosphates, nitrite and ammonium nitrogen exerted no limiting effects on the development of phytoplankton.

8

Changes in the trophic state and phytoplankton composition and abundance in Loch Lomond, Scotland, UK

84%

Krokowski J. T.

Oceanological and Hydrobiological Studies

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2007

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tom 36

|

nr Suppl.1

9

Distribution of phytoplankton along the thermohaline gradient in the North-Eastern Adriatic channel; winter aspect

67%

Vilicic D., Kuzmic M., Bosak S., Silovic T., Hrustic E., Buric Z.

Oceanologia

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2009

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tom 51

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nr 4

The distribution of phytoplankton and its relation to the hydrographic features in the north-eastern Adriatic was investigated in February 2008. The area of interest included a thermohaline gradient in the channel situated between the coast and the islands lying parallel to the coast. The gradient is controlled by the influx of oligotrophic karstic riverine water at the south-eastern end,subma rine springs in the middle part,an d warmer offshore waters at the north-western end of the channel. The change of temperature and salinity in the estuarine transition zone was accompanied by abundant diatoms and dinoflagellates below the halocline,with dominant chain-forming diatoms (Chaetoceros, Bacteriastrum) in abundances reaching 5×105 cells dm−3. The impact of coastal submarine springs detected by infrared remote sensing resulted in the growth of cyanobacteria in the nitrogen-depleted surface waters. The greater contribution of picoplankton, as well as of nanoplanktonic coccolithophorids and cryptophytes,in the outer channel system indicated their preference for oligotrophic conditions. Flow cytometric counts of nanophytoplankton were 10–30 times greater than inverted microscope counts. Cyanobacteria were about five times more abundant than picoeukaryotes. The study demonstrates how different techniques (remote sensing and in situ investigations) can be useful in understanding the biological and hydrographic set-up in the specific oligotrophic eastern Adriatic coastal environment.

Ograniczanie wyników

Assessment of a sheltered euhaline area of the Southeastern Bay of Biscay to sustain bivalve production in terms of phytoplankton community composition

Change of physico-chemical conditions and phytoplankton composition in a humic lake caused by liming and fertilisation

Phytoplankton composition and abundance at surface depths within different lake habitats

Relationship among biomass of algae and concentration of chlorophyll a, against the taxonomic structure of phytoplankton in three lakes on Lublin Polesie region

Recent trophic changes and phytoplankton composition in lake Drummond, within the Dismal Swamp, Virginia

Seasonal changes in phytoplankton composition and diversity in the Epe Lagoon, Nigeria

Seasonal changes occurring over four years in a reservoir's phytoplankton composition

Changes in the trophic state and phytoplankton composition and abundance in Loch Lomond, Scotland, UK

Distribution of phytoplankton along the thermohaline gradient in the North-Eastern Adriatic channel; winter aspect