Results of Expeditionary Studies of the Onezhskiy Bay in the White Sea in September, 2019

A. V. Tolstikov1, ✉, N. E. Galakhina1, T. A. Belevich2, 3, N. V. Usov4, R. E. Zdorovennov1

1 Northern Water Problems Institute of the Karelian Research Centre, Russian Academy of Sciences, Petrozavodsk, Russian Federation

2 M. V. Lomonosov Moscow State University, Faculty of Biology, Moscow, Russian Federation

3 A. N. Belozersky Research Institute of Physico-Chemical Biology of the M. V. Lomonosov Moscow State University, Moscow, Russian Federation

4 Zoological Institute, Russian Academy of Sciences, St. Petersburg, Russian Federation

e-mail: alexeytolstikov@mail.ru

Abstract

Purpose. The purpose of the study consists in identifying the characteristic features of the distribution of hydrophysical and biogeochemical parameters of marine environment depending on the tide phases in the Onezhskiy Bay (the White Sea) in September.

Methods and Results. In the cruise of the R/V «Ekolog» (September 6–11, 2019), synchronous integrated hydrological and biogeochemical studies were for the first time performed in the Onezhskiy Bay depending on the phase of a tidal cycle in September. The standard methods applied for this purpose included two sections in the White Sea, namely along the Western Solovetskaya Salma Strait and through the Onezhskiy Bay from north to south. This permitted to determine the chlorophyll a and nutrients contents, the taxonomic composition, abundance and biomass of phytoplankton including its vertical distribution within the photic zone, as well as the qualitative and quantitative composition of zooplankton. Organic forms of nitrogen (0.62–0.83 mg/l) prevailed among the nutrients in the Onezhskiy Bay, the contents of Pmin and Porg were close (on average 9 μg/l), the concentration of phosphorus mineral forms was predominant in the water bottom layer at the deep-sea stations. In the Western Solovetskaya Salma, the phytoplankton biomass average values during high and low water were 6.75 ± 1.18 mg C/m3 and 10.25 ± 11.34 mg C/m3, and in the Onezhskiy Bay – 8.07 ± 2.43 mg C/m3 and 16.61 ± 13.54 mg C/m3, respectively. Phytoplankton was represented by diatoms, dinophytes, cryptophytes and dictyochas. In the southern part of the Onezhskiy Bay, a significant increase in the abundance of all common zooplankton species was found at night.

Conclusions. In the area under study, the impact of the tidal cycle phases on spatial and temporal variability of the marine environment characteristics was manifested in a change in the thickness of the layer of temperature and salinity surface anomalies; position of the Onezhskiy frontal section shifted by 8–9 km; the changes in the nitrites, ammonium ions and chlorophyll a concentrations, and also in the phytoplankton biomass were statistically insignificant; the composition of dominant phytoplankton species did not change; the horizontal distribution of zooplankton, primarily its warm- forms, corresponded to the water temperature horizontal gradient: in the southern part of the Onezhskiy Bay, the abundance of boreal species is by orders of magnitude higher than that near the boundary with the basin.

Keywords

White Sea, Onezhskiy Bay, comprehensive research, nutrients, chlorophyll a, phytoplankton, zooplankton

Acknowledgements

The study was carried out within the state assignment "Comprehensive research of the White Sea and the watershed in the interests of the development of the Arctic zone of the Russian Federation" No. 121021700122-7 and the Development program of the Interdisciplinary Scientific and Educational School of the M. V. Lomonosov Moscow State University "The future of the planet and global environmental changes". The authors are grateful to the expedition members Nikishova E. P., Ph.D. (Geogr.) Konik A. A. and Ph.D. (Geogr.) Svergun E. I., as well as the crew of the R/V “Ecolog”.

Original russian text

Original Russian Text © The Authors, 2023, published in MORSKOY GIDROFIZICHESKIY ZHURNAL, Vol. 39, Iss. 4 (2023)

For citation

Tolstikov, A.V., Galakhina, N.E., Belevich, T.A., Usov, N.V. and Zdorovennov, R.E., 2023. Results of Expeditionary Studies of the Onezhskiy Bay in the White Sea in September, 2019. Physical Oceanography, 30(4), pp. 468-483.

References

  1. Lisitsyn, A.P. and Nemirovskaya, I.A., eds., 2013. The White Sea System. Vol. 3: Dispersed Sedimentary Hydrosphere Material, Microbial Processes and Pollution. Moscow: Scientific World, 668 p. (in Russian).
  2. Zdorovennov, R.E., Tolstikov, A.V., Georgiev, A.P. and Zimin, A.V., 2018. [Investigation of the Dynamics of Frontal Sections and Frontal Zones under the Influence of a Semidiurnal Tidal Cycle in the White Sea]. In: R. I. Nigmatulin, S. K. Konovalov, N. I. Golubeva and A. N. Bulatova, eds., 2018. Expedition Research on Research Vessels of the FASO of Russia and the Svalbard Archipelago in 2017. MHI, pp. 78-83 (in Russian).
  3. Glukhovsky, B.Kh., ed., 1991. Hydrometeorology and Hydrochemistry of the Seas of the USSR. Vol. 2: White Sea. Iss. 1: Hydrometeorological Conditions. Leningrad: Gidrometeoizdat, 240 p. (in Russian).
  4. Zimin, A.V., 2018. Sub-Tidal Processes and Phenomena in the White Sea. Moscow: Geos, 220 p. (in Russian).
  5. Chernov, I., Tolstikov, A. and Iakovlev, N., 2017. Modelling of Tracer Transport in the White Sea. In: RAT, 2017. Environment. Technology. Resources – Proceedings of the 11th International Scientific and Practical Conference. Rezekne, Latvia: Rezekne Academy of Technologies. Vol. 1, pp. 54-58. doi:10.17770/etr2017vol1.2594
  6. Arar, E.J. and Collins, G.B., 1997. Method 445.0. In Vitro Determination of Chlorophyll a and Pheophytin a in Marine and Freshwater Algae by Fluorescence. Revision 1.2. Cincinnati, Ohio: U.S. Environmental Protection Agency, 22 p.
  7. Hillebrand, H., Dürselen, C.-D., Kirschtel, D., Pollingher, U. and Zohary, T., 1999. Biovolume Calculation for Pelagic and Benthic Microalgae. Journal of Phycology, 35(2), pp. 403-424. doi:10.1046/j.1529-8817.1999.3520403.x
  8. Menden-Deuer, S. and Lessard, E.J., 2000. Carbon to Volume Relationships for Dinoflagellates, Diatoms, and Other Protist Plankton. Limnology and Oceanography, 45(3), pp. 569-579. doi:10.4319/lo.2000.45.3.0569
  9. Demidov, A.B., Kopelevich, O.V., Mosharov, S.A., Sheberstov, S.V. and Vazyulya, S.V., 2017. Modelling Kara Sea Phytoplankton Primary Production: Development and Skill Assessment of Regional Algorithms. Journal of Sea Research, 125, pp. 1-17. doi:10.1016/j.seares.2017.05.004
  10. Kravchenko, I.Yu., 2012. [Biogenic Elements and Organic Matter in the Water of the Coastal Part of the White Sea]. In: P. A. Lozovik, 2012. Organic Matter and Biogenic Elements in Inland Waters and Marine Waters. Proceedings of the V All-Russian Symposium with International Participation. 10-14 September 2012, Petrozavodsk, Republic of Karelia, Russia. Petrozavodsk: Karelian Research Centre of the Russian Academy of Sciences, pp. 274-276 (in Russian).
  11. Zubaha, M.A. and Usov, N.V., 2004. Optimum Temperatures for Common Zooplankton Species in the White Sea. Russian Journal of Marine Biology, 30(5), pp. 293-297. doi:10.1023/B:RUMB.0000046547.26708.3e
  12. Prygunkova, R.V., 1974. [Certain Peculiarities in the Seasonal Development of Zooplankton in the Chupa Inlet of the White Sea]. In: B. E. Bykhovsky, ed., 1974. Seasonal Phenomena in the Life of the White and Barents Seas. Explorations of the Fauna of the Seas, Vol. 13. Leningrad: Nauka, pp. 4-55 (in Russian).
  13. Pertsova, N.M., 1990. [On Ecology of the Boreal Copepods Centropages Hamatus Lilljeborg and Temora Longicornis Müller in the White Sea and Their Areals]. In: P. V. Matekin, ed., 1990. Biological Resource of the White Sea: Publications of MSU White Sea Biological Station. Moscow: MSU Publishing. Vol. 7, pp. 80-92 (in Russian).
  14. Prudkovsky, A.A., 2003. The Life Cycle of Acartia Bifilosa (Copepoda, Calanoida) in the White Sea (Chernorechenskaya Inlet, Kandalaksha Bay). In: MSU, 2003. Trudy of Pertsov White Sea Biological Station, Moscow State University. Moscow: Moscow University Press. Vol. 9, pp. 164-168 (in Russian).

Download the article (PDF)