Current state and long-term changes of the Crenomytilus grayanus community in Vostok Bay, Sea of Japan

2008 ◽  
Vol 39 (4) ◽  
pp. 272-278 ◽  
Author(s):  
Yu. A. Galysheva
Keyword(s):  
Sea Of Japan ◽  
Vostok Bay ◽  
Crenomytilus Grayanus ◽  
Current State ◽  
Long Term Changes

scholarly journals Hydrochemical and microbiological assessment of the current state of the Vostok Bay. 

2020 ◽  
pp. 64-72
Author(s):  
Н.К. ХРИСТОФОРОВА ◽  
Т.В. БОЙЧЕНКО ◽  
А.Д. КОБЗАРЬ
Keyword(s):  
Sea Of Japan ◽  
Marine Reserve ◽  
Water Area ◽  
The Sea Of Japan ◽  
Vostok Bay ◽  
Environmental Situation ◽  
Current State ◽  
Microbiological Indicators

Проведены химико-экологические и микробиологические исследования современного состояния поверхностных прибрежных вод зал. Восток (Японское море). Наиболее напряженная экологическая ситуация отмечена в бухте Гайдамак, в районах у Волчанецкой протоки и устья р. Литовка. Протока, а также приустьевая зона р.Литовка являются главными тревожными участками в морском заказнике Залив Восток . The current state of the Vostok Bay water area (the Sea of Japan) is estimated using hydrochemical and microbiological indicators. The most intense environmental situation was noted for Gaydamak Bight, the area near the Volchanets duct and the mouth of the Litovka River. The duct, as well as the mouth of the Litovka River, are the main alarming sites in the Vostok Bay marine reserve.

IX. Discussion

1965 ◽  
Vol 258 (1088) ◽  
pp. 107-108
Keyword(s):  
Geophysical Methods ◽  
Continental Drift ◽  
Tectonic Activity ◽  
Geological Time ◽  
The Past ◽  
Current State ◽  
The Earth ◽  
Long Term Changes ◽  
History Of

Although the primary subject of the Symposium was continental drift, this is only one aspect of a larger problem. Eventually, consideration of changes in magmatic, metamorphic and tectonic activity through the history of the crust should enable us to put forward a hypothesis to account for the behaviour of the upper parts of the Earth through geological time. As had been pointed out, most geophysical methods provided information about the current state of the Earth and part of the great value of palaeomagnetic studies lay in the fact that they produced information about the past. Some information about the behaviour of possible convection cells during continental drift could be obtained from other long-term changes in the crust. The incidence of magmatic and metamorphic activity gave some indication as to the distribution of regions where there had been an unusually high accession of heat in the past.

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