In ancient Greek myths, the Black Sea was named Pontus Axeinus, meaning “Inhospitable Sea.” Once a lake connected to the Caspian Sea, the Black Sea became connected to the Mediterranean after the opening of the Dardanelles in the interglacial period (100 000-150 000 years ago). It was then again isolated and only about 6 000 years ago reconnected to the Sea of Marmara and Mediterranean Sea.
The Black Sea biota - the combination of flora and fauna - reflects the general processes that have influenced the ecosystem of the sea.
The number of species in the Black Sea is around one third of that in the Mediterranean. Despite recent changes in absolute numbers, the ratio remains close to three: 10 000 species in the Mediterranean versus 3 700 species in the Black Sea.
According to their origins, there are five types of groups: Pontiac relics, Mediterranean species, Boreal-Atlantic relics, Freshwater species and Alien species.
The most ancient inhabitants are found in waters with low salinity.
These constitute the most numerous element in the Black Sea fauna, comprising up to 80 % of the total fauna. Most prefer warm, saline waters, and are found in the upper layers of the sea.
Marine species originating from cold seas and living in deep layers of the sea.
Introduced by river discharges and usually found in the sea water during the maximum river run-off.
Established populations of alien species introduced by various routes.
The main cause of the increasing eutrophication in the sea is nutrient inputs from the rivers. The catchment area of the Black Sea is over 2 million square kilometers, five times the size of the sea itself. The drainage basin entirely or partially covers 22 countries in Europe and Asia Minor. The largest volume of river flow entering the sea comes from the north-western part of the basin. Depending on meteorological, hydrothermal, and hydrobiological conditions during summer and autumn, oxygen deficiency (hypoxia or anoxia) and mass mortality caused by eutrophication have become an annual event in the north-western shelf area where anoxic zones expanded from covering 3 500 square kilometers in 1973 to 40 000 square kilometers in 1990. This level of eutrophication also puts the 13 % of water volume of the shelf area that is not anoxic under severe stress.
Oil spills cause serious deterioration of the coastal marine ecosystem through contamination of water and sediment, aesthetics quality, etc. Some 170 thousand tones of oil products are discharged into the Black Sea every year with sewage. Pollutants and toxic agents are also carried to the sea in river waters. The highest concentrations of hydrocarbons (petroleum residuals) were detected in the Danube, Dnieper and Dniester river estuaries and other point sources of pollution located off the shores of Romania and Bulgaria where oil production and refining is carried out. The Danube River accounts for 48 % of the 111 000 tones of oil entering the Black Sea via rivers each year. In addition, ports, oil terminals and their immediate surroundings, and straits are at risk from maritime accidents involving ships transporting crude oil. In Sevastopol Bay, the major port for the Black Sea navy, oil concentrations more than 100 times higher than background level were measured.
Large-scale construction of cascade dams on the Dnieper and Don and other rivers has led to the loss of spawning areas for the sturgeon and other valuable fish species due to their being cut off from the sea. Moreover the drastic decrease of annual river flow has resulted in apparent hydro-chemical and biochemical changes, with catastrophic effects in the low salinity basins. Significant damage to the productivity of sea areas is also caused by the intake of cooling water by various installations along the coast. Despite the fact that about 80 % of these have fish protection devices at their water intake, their efficiency remains rather low and several thousands tones of fish die each year. Implementation of a new technology to control the quality of coastal waters and increase biodiversity, the construction of artificial reefs, began in the 1970s. At present, special constructions have been built in Constanța port (Romania) and Odessa Bay (Ukraine).
Over-exploitation has affected fish stocks. Commercial fishing in the Dnieper and Dniester estuaries has been reduced. Some valuable species such as mackerel, bonito and horse mackerel in the Black Sea and pike, perch, roach and bream in the Sea of Azov have practically disappeared. Of the 26 commercial fish species found in the period 1960 to 1970, only five were left by 1980. By the mid-1980s, sturgeon catches had nearly reached the average annual amount for the 1930s of 1 000 tones, but farm-produced fish accounting for more than 90 % of the total catch. Commercial mussel farming is practiced in all countries except Georgia and Turkey. Importation of species for aquaculture has induced severe alterations at the ecosystem level.
Marine flora of the Black Sea originates mostly from the northern Atlantic and the Mediterranean Sea. Species diversity is nearly 4 times less than in the Mediterranean due to environmental factors unique to the Black Sea: low salinity, high eutrophication and cold winters during which the sea surface in the north-western part and in some other areas is ice-covered. Some indigenous species have been inhabitants of the Black Sea since the Ice Age.
There are four species of Black Sea mammals: the monk seal and three species of dolphins, the bottlenosed dolphin, the common dolphin and the harbour porpoise. There are over 450 terrestrial and marine species of seabird in Europe. In the Black Sea, seven of those species are currently under threat, in terms of species distribution and population size. There are about 5600 species of fish found in the Black Sea.