Spatial Distribution of Phytoplankton in the Subarctic Estuary (Kem’ River, the White Sea)
- Авторы: Radchenko I.G.1, Ilyash L.V.1, Shevchenko V.P.2, Zdorovennov R.E.3, Novigatsky A.N.2, Politova N.V.2, Tolstikov A.V.3
- 
							Учреждения: 
							- Department of Biology, Moscow State University
- Shirshov Institute of Oceanology, Russian Academy of Sciences
- Northern Water Problems Institute, Karelian Research Centre, Russian Academy of Sciences
 
- Выпуск: Том 59, № 3 (2019)
- Страницы: 305-315
- Раздел: Marine Biology
- URL: https://journals.rcsi.science/0001-4370/article/view/149863
- DOI: https://doi.org/10.1134/S0001437019030184
- ID: 149863
Цитировать
Аннотация
The species composition and biomass of phytoplankton, as well as hydrological characteristics, were estimated during four spatial surveys in the Subarctic tidal Kem’ River estuary and adjacent area of Onega Bay (White Sea, Russia) in June–July 2008–2011. The study area was divided into the zones (river, transition, and marine), based on salinity variation of the surface water layer. In total, 318 species of phytoplankton were recorded, 143 species were found in the river zone, 225 in the transition zone, and 106 in the marine zone. Diatoms were represented by the greatest number of species in all zones. The highest phytoplankton biodiversity in the surface layer was found in the transition zone. The averages of total phytoplankton biomass in the surface layer (B0) in different years varied as 2.8–16.9 mgC/m3. Although B0 did not differ significantly between zones (except 2011, when B0 was the highest in the river zone), the dissimilarity in the phytoplankton community structure in the river, transition and marine zones was 61–95%. The similarity of phytoplankton at stations of each zone was poor (22–53%); the lowest values were observed in the transition zone. It is postulated that the tidal cycle determines the spatial and temporal heterogeneity of the phytoplankton composition, structure, and abundance in the Kem’ River estuary in summer.
Об авторах
I. Radchenko
Department of Biology, Moscow State University
							Автор, ответственный за переписку.
							Email: IraRadchenko@yandex.ru
				                					                																			                												                	Россия, 							Moscow, 119234						
L. Ilyash
Department of Biology, Moscow State University
														Email: IraRadchenko@yandex.ru
				                					                																			                												                	Россия, 							Moscow, 119234						
V. Shevchenko
Shirshov Institute of Oceanology, Russian Academy of Sciences
														Email: IraRadchenko@yandex.ru
				                					                																			                												                	Россия, 							Moscow, 117997						
R. Zdorovennov
Northern Water Problems Institute, Karelian Research Centre, Russian Academy of Sciences
														Email: IraRadchenko@yandex.ru
				                					                																			                												                	Россия, 							Petrozavodsk, 185030						
A. Novigatsky
Shirshov Institute of Oceanology, Russian Academy of Sciences
														Email: IraRadchenko@yandex.ru
				                					                																			                												                	Россия, 							Moscow, 117997						
N. Politova
Shirshov Institute of Oceanology, Russian Academy of Sciences
														Email: IraRadchenko@yandex.ru
				                					                																			                												                	Россия, 							Moscow, 117997						
A. Tolstikov
Northern Water Problems Institute, Karelian Research Centre, Russian Academy of Sciences
														Email: IraRadchenko@yandex.ru
				                					                																			                												                	Россия, 							Petrozavodsk, 185030						
Дополнительные файлы
 
				
			 
						 
					 
						 
						 
						 
									 
  
  
  
  
  Отправить статью по E-mail
			Отправить статью по E-mail  Открытый доступ
		                                Открытый доступ Доступ предоставлен
						Доступ предоставлен Только для подписчиков
		                                		                                        Только для подписчиков
		                                					