The location of the Black Sea
Map of the Black Sea with bathymetry and surrounding relief
|Primary inflows||Danube, Dnieper, Southern Bug, Dniester, Don, Kuban, Rioni, Kızılırmak|
|Basin countries||Bulgaria, Romania, Ukraine, Russia, Georgia, Turkey|
A large number of countries included in drainage basins for inflow rivers
|Max. length||1,175 km (730 mi)|
|Surface area||436,402 km2 (168,500 sq mi)|
|Average depth||1,253 m (4,111 ft)|
|Max. depth||2,600 m (8,530 ft)|
|Water volume||547,000 km3 (131,200 cu mi)|
The Black Sea is a body of water and marginal sea of the Atlantic Ocean between Eastern Europe, the Caucasus, and Western Asia. It is supplied by a number of major rivers, such as the Danube, Dnieper, Southern Bug, Dniester, Don, and the Rioni. The watersheds of many countries drain into the Black Sea beyond the six that immediately border it.
The Black Sea has an area of 436,400 km2 (168,500 sq mi) (not including the Sea of Azov), a maximum depth of 2,212 m (7,257 ft), and a volume of 547,000 km3 (131,000 cu mi). It is constrained by the Pontic Mountains to the south, Caucasus Mountains to the east, Crimean Mountains to the north, Strandzha to the southwest, Balkan Mountains to the west, Dobrogea Plateau to the northwest, and features a wide shelf to the northwest.
The Black Sea is bordered by Ukraine, Romania, Bulgaria, Turkey, Georgia, and Russia. It has a positive water balance with an annual net outflow of 300 km3 (72 cu mi) per year through the Bosporus and the Dardanelles into the Aegean Sea. While the net flow of water through the Bosporus and Dardanelles (known collectively as the Turkish Straits) is out of the Black Sea, generally water is flowing in both directions simultaneously. Denser, more saline water from the Aegean flows into the Black Sea underneath the less dense, fresher outflowing water from the Black Sea. This creates a significant and permanent layer of deep water which does not drain or mix and is therefor anoxic. This anoxic layer is responsible for the preservation of ancient shipwrecks which have been found in the Black sea.
The Black Sea ultimately drains into the Mediterranean Sea, via the Turkish Straits and the Aegean Sea. The Bosporus Strait connects it to the small Sea of Marmara which in turn is connected to the Aegean Sea via the Strait of the Dardanelles. To the north the Black Sea is connected to the Sea of Azov by the Kerch Strait.
The water level has varied significantly over geological time. Due to these variations in the water level in the basin, the surrounding shelf and associated aprons have sometimes been dry land. At certain critical water levels, connections with surrounding water bodies can become established. It is through the most active of these connective routes, the Turkish Straits, that the Black Sea joins the world ocean. During geological periods when this hydrological link was not present, the Black Sea was an endorheic basin, operating independently of the global ocean system (similar to the Caspian Sea today). Currently, the Black Sea water level is relatively high; thus, water is being exchanged with the Mediterranean. The Turkish Straits connect the Black Sea with the Aegean Sea and comprise the Bosporus, the Sea of Marmara, and the Dardanelles. The Black Sea undersea river is a current of particularly saline water flowing through the Bosporus Strait and along the seabed of the Black Sea. The discovery of the river announced on August 1, 2010, was made by scientists at the University of Leeds and is the first of its kind in the world. The undersea river stems from salty water spilling through the Bosporus Strait from the Mediterranean Sea into the Black Sea, where the water has a lower salt content.
|6||Sevastopol||Russia (de facto)/Ukraine (de jure)||national-level municipality on the Crimean Peninsula||379,200|
Current names of the sea are usually equivalents of the English name "Black Sea", including these given in the countries bordering the sea:
- Abkhazian: Амшын Еиқәа, IPA: [ɑmʂɨn ɛjkʷʰɑ]
- Adyghe: Хы шӏуцӏэ, IPA: [xə ʃʼəw.t͡sʼa]
- Bulgarian: Черно море, IPA: [ˈt͡ʃɛrno moˈrɛ]
- Crimean Tatar: Къара денъиз, Qara deñiz IPA: [qɑrɑ deŋiz]
- Georgian: შავი ზღვა, translit.: shavi zghva, IPA: [ʃɑvi zɣvɑ]
- Laz and Mingrelian: უჩა ზუღა, IPA: [utʃɑ zuɣɑ], or simply ზუღა, IPA: [zuɣɑ], "Sea"
- Romanian: Marea Neagră, pronounced [ˈmare̯a ˈne̯aɡrə] (listen)
- Russian: Чёрное мо́рe, IPA: [ˈtɕornəjə ˈmorʲə]
- Turkish: Karadeniz, IPA: [kaˈɾadeniz]
- Ukrainian: Чорне море, IPA: [ˈtʃɔrnɛ ˈmɔrɛ]
Such names have not yet been shown conclusively to predate the 13th century.
In Greece, the historical name "Euxine Sea" holds a different meaning (see below), is still widely used:
- Greek: Eύξεινος Πόντος, romanized: Éfxinos Póndos, [ˈefksinos ˈpondos], lit. "Hospitable Sea"; the name Μαύρη Θάλασσα (Mávri Thálassa), [ˈmavri ˈθalasa], lit. "Black Sea" is used, but is much less common.
Historical names and etymology
The principal Greek name "Póntos Áxeinos" is generally accepted to be a rendering of Iranian word *axšaina- ("dark colored"), compare Avestan axšaēna- ("dark colored"), Old Persian axšaina- (color of turquoise), Middle Persian axšēn/xašēn ("blue"), and New Persian xašīn ("blue"), as well as Ossetic œxsīn ("dark gray"). The ancient Greeks, most likely those living to the north of the Black Sea, subsequently adopted the name and altered it to á-xe(i)nos. Thereafter, Greek tradition refers to the Black Sea as the "Inhospitable Sea", Πόντος Ἄξεινος Póntos Áxeinos, which is first attested in Pindar (c. 475 BC). The name was considered to be "ominous" and was later changed into the euphemistic name "Hospitable sea", Εὔξεινος Πόντος Eúxeinos Póntos, which was also for the first time attested in Pindar. This became the commonly used designation for the sea in Greek. In contexts related to mythology, the older form Póntos Áxeinos remained favored.
It has been erroneously suggested that the name was derived from the color of the water, or was at least related to climatic conditions. Black or dark in this context, however, referred to a system in which colors represent the cardinal points of the known world. Black or dark represented the north; red the south; white the west; and green or light blue for the east. The symbolism based on cardinal points was used on multiple occasions and is therefore widely attested. For example, the "Red Sea", a body of water reported since the time of Herodotus (c. 484–c. 425 BC) in fact designated the Indian Ocean, together with bodies of water now known as the Persian Gulf and the Red Sea. According to the same explanation and reasoning, it is therefore considered to be impossible for the Scythians, who principally roamed in present-day Ukraine and Russia, to have given the designation because they lived to the north of the sea, which would, therefore, be a southern body of water for them. The name could have only been given by people who were aware of both the northern "black/dark" and southern "red" seas; it is therefore considered probable it was given its name by the Achaemenids (550–330 BC).
Strabo's Geographica (1.2.10) reports that in antiquity, the Black Sea was often simply called "the Sea" (ὁ πόντος ho Pontos). He also thought the Black Sea was called "inhospitable" before Greek colonization because it was difficult to navigate and because its shores were inhabited by savage tribes. (7.3.6) The name was changed to "hospitable" after the Milesians had colonized the Pontus region of the southern shoreline, making it part of Greek civilization.
In Greater Bundahishn, a sacred Zoroastrian text written in Middle Persian, the Black Sea is called Siyābun. A 1570 map of Asia titled Asiae Nova Descriptio from Abraham Ortelius's Theatrum Orbis Terrarum labels the sea Mar Maggior ("Great Sea", compare Latin mare major).
English-language writers of the 18th century often used the name Euxine Sea (// or //) to refer to the Black Sea. Edward Gibbon, for instance, calls the sea by this name throughout The History of the Decline and Fall of the Roman Empire. During the Ottoman Empire period, the Black Sea was called either Bahr-e Siyah or Karadeniz, both meaning "the Black Sea" in Ottoman Turkish.
In the tenth-century geography book Hudud al-'Alam, which was written in Persian by an unknown author, the Black Sea is called Georgian Sea, Sea of Georgians (daryä-yi Gurziyan). Old Georgian sources of the 9th to 14th centuries, The Georgian Chronicles, used the name Speris Zğua (სპერის ზღუა), which means "The Sea of Speri", after the name of the Kartvelian tribe Speris or Saspers, now in Turkey. The modern names of the Black Sea (Chyornoye more, Karadeniz, etc.), originated in the 13th century.
Geology and bathymetry
The Black Sea is divided into two depositional basins—the Western Black Sea and Eastern Black Sea—separated by the Mid-Black Sea High, which includes the Andrusov Ridge, Tetyaev High, and Archangelsky High, extending south from the Crimean Peninsula. The basin includes two distinct relict back-arc basins which were initiated by the splitting of an Albian volcanic arc and the subduction of both the Paleo- and Neo-Tethys Oceans, but the timings of these events remain uncertain. Arc volcanism and extension occurred as the Neo-Tethys Ocean subducted under the southern margin of Laurasia during the Mesozoic. Uplift and compressional deformation took place as the Neotethys continued to close. Seismic surveys indicate that rifting began in the Western Black Sea in the Barremian and Aptian followed by the formation of oceanic crust 20 million years later in the Santonian. Since its initiation, compressional tectonic environments led to subsidence in the basin, interspersed with extensional phases resulting in large-scale volcanism and numerous orogenies, causing the uplift of the Greater Caucasus, Pontides, Southern Crimean Peninsula and Balkanides mountain ranges.
The ongoing collision between the Eurasian and African plates and westward escape of the Anatolian block along the North Anatolian Fault and East Anatolian Faults dictates the current tectonic regime, which features enhanced subsidence in the Black Sea basin and significant volcanic activity in the Anatolian region. These geological mechanisms, in the long term, have caused the periodic isolations of the Black Sea from the rest of the global ocean system.
The large shelf to the north of the basin is up to 190 km (120 mi) wide and features a shallow apron with gradients between 1:40 and 1:1000. The southern edge around Turkey and the eastern edge around Georgia, however, are typified by a narrow shelf that rarely exceeds 20 km (12 mi) in width and a steep apron that is typically 1:40 gradient with numerous submarine canyons and channel extensions. The Euxine abyssal plain in the centre of the Black Sea reaches a maximum depth of 2,212 metres (7,257.22 feet) just south of Yalta on the Crimean Peninsula.
The area surrounding the Black Sea is commonly referred to as the Black Sea Region. Its northern part lies within the Chernozem belt (black soil belt) which goes from eastern Croatia (Slavonia), along the Danube (northern Serbia, northern Bulgaria (Danubian Plain) and southern Romania (Wallachian Plain)) to northeast Ukraine and further across the Central Black Earth Region and southern Russia into Siberia.
Oil and natural gas
The Black Sea contains oil and natural gas resources but exploration in the sea is incomplete. As of 2017, 20 wells are in place. Throughout much of its existence, the Black Sea has had significant oil and gas-forming potential because of significant inflows of sediment and nutrient-rich waters. However, this varies geographically. For example, prospects are poorer off the coast of Bulgaria because of the large influx of sediment from the Danube River which obscured sunlight and diluted organic-rich sediments. Many of the discoveries to date have taken place offshore of Romania in the Western Black Sea and only a few discoveries have been made in the Eastern Black Sea.
During the Eocene, the Paratethys Ocean was partially isolated and sea levels fell. During this time sand shed off the rising Balkanide, Pontide and Caucasus mountains trapped organic material in the Maykop Suite of rocks through the Oligocene and early Miocene. Natural gas appears in rocks deposited in the Miocene and Pliocene by the paleo-Dnieper and pale-Dniester rivers, or in deep-water Oligocene-age rocks. Serious exploration began in 1999 with two deep-water wells, Limanköy-1 and Limanköy-2, drilled in Turkish waters. Next, the HPX (Hopa)-1 deepwater well targeted late Miocene sandstone units in Achara-Trialet fold belt (also known as the Gurian fold belt) along the Georgia-Turkey maritime border. Although geologists inferred that these rocks might have hydrocarbons that migrated from the Maykop Suite, the well was unsuccessful. No more drilling happened for five years after the HPX-1 well. Then in 2010, Sinop-1 targeted carbonate reservoirs potentially charged from the nearby Maykop Suite on the Andrusov Ridge, but the well-struck only Cretaceous volcanic rocks. Yassihöyük-1 encountered similar problems. Other Turkish wells, Sürmene-1 and Sile-1 drilled in the Eastern Black Sea in 2011 and 2015 respectively tested four-way closures above Cretaceous volcanoes, with no results in either case. A different Turkish well, Kastamonu-1 drilled in 2011 did successfully find thermogenic gas in Pliocene and Miocene shale-cored anticlines in the Western Black Sea. A year later in 2012, Romania drilled Domino-1 which struck gas prompting the drilling of other wells in the Neptun Deep. In 2016, the Bulgarian well Polshkov-1 targeted Maykop Suite sandstones in the Polshkov High and Russia is in the process of drilling Jurassic carbonates on the Shatsky Ridge as of 2018. 
The Black Sea is a marginal sea and is the world's largest body of water with a meromictic basin. The deep waters do not mix with the upper layers of water that receive oxygen from the atmosphere. As a result, over 90% of the deeper Black Sea volume is anoxic water. The Black Sea's circulation patterns are primarily controlled by basin topography and fluvial inputs, which result in a strongly stratified vertical structure. Because of the extreme stratification, it is classified as a salt wedge estuary.
The Black Sea only experiences water transfer with the Mediterranean Sea, so all inflow and outflow occurs in the Bosporus and Dardanelles. Inflow from the Mediterranean has a higher salinity and density than the outflow, creating the classical estuarine circulation. This means that the inflow of dense water from the Mediterranean occurs at the bottom of the basin while the outflow of fresher Black Sea surface-water into the Marmara Sea occurs near the surface. The outflow is 16 000 m3/s (around 500 km3/year) and the inflow is 11 000 m3/s (around 350 km3/year), acc to Gregg (2002).
The following water budget can be estimated:
- Water IN:
- Water OUT:
The southern sill of the Bosporus is located at -36.5 m below present sea level (deepest spot of the shallowest cross-section in the Bosporus, located in front of Dolmabahçe Palace) and has a wet section of around 38 000 m2. Inflow and outflow current speeds are averaged around 0.3 to 0.4 m/s, but much higher speeds are found locally, inducing significant turbulence and vertical shear. This allows for turbulent mixing of the two layers. Surface water leaves the Black Sea with a salinity of 17 psu and reaches the Mediterranean with a salinity of 34 PSU. Likewise, an inflow of the Mediterranean with salinity 38.5 PSU experiences a decrease to about 34 psu.
Mean surface circulation is cyclonic and waters around the perimeter of the Black Sea circulate in a basin-wide shelfbreak gyre known as the Rim Current. The Rim Current has a maximum velocity of about 50–100 cm/s. Within this feature, two smaller cyclonic gyres operate, occupying the eastern and western sectors of the basin. The Eastern and Western Gyres are well-organized systems in the winter but dissipate into a series of interconnected eddies in the summer and autumn. Mesoscale activity in the peripheral flow becomes more pronounced during these warmer seasons and is subject to interannual variability.
Outside of the Rim Current, numerous quasi-permanent coastal eddies are formed as a result of upwelling around the coastal apron and "wind curl" mechanisms. The intra-annual strength of these features is controlled by seasonal atmospheric and fluvial variations. During the spring, the Batumi eddy forms in the southeastern corner of the sea.
Beneath the surface waters—from about 50–100 meters—there exists a halocline that stops at the Cold Intermediate Layer (CIL). This layer is composed of cool, salty surface waters, which are the result of localized atmospheric cooling and decreased fluvial input during the winter months. It is the remnant of the winter surface mixed layer. The base of the CIL is marked by a major pycnocline at about 100–200 metres (330–660 ft) and this density disparity is the major mechanism for isolation of the deep water.
Below the pycnocline is the Deep Water mass, where salinity increases to 22.3 PSU and temperatures rise to around 8.9 °C. The hydrochemical environment shifts from oxygenated to anoxic, as bacterial decomposition of sunken biomass utilizes all of the free oxygen. Weak geothermal heating and long residence time create a very thick convective bottom layer.
Because of the anoxic water at depth, organic matter, including anthropogenic artifacts such as boat hulls, are well preserved. During periods of high surface productivity, short-lived algal blooms form organic rich layers known as sapropels. Scientists have reported an annual phytoplankton bloom that can be seen in many NASA images of the region. As a result of these characteristics the Black Sea has gained interest from the field of marine archaeology as ancient shipwrecks in excellent states of preservation have been discovered, such as the Byzantine wreck Sinop D, located in the anoxic layer off the coast of Sinop, Turkey.
Modelling shows the release of the hydrogen sulfide clouds in the event of an asteroid impact into the Black Sea would pose a threat to health—or even life—for people living on the Black Sea coast.
There have been isolated reports of flares on the Black Sea occurring during thunderstorms, possibly caused by lightning igniting combustible gas seeping up from the sea depths.
The Black Sea supports an active and dynamic marine ecosystem, dominated by species suited to the brackish, nutrient-rich, conditions. As with all marine food webs, the Black Sea features a range of trophic groups, with autotrophic algae, including diatoms and dinoflagellates, acting as primary producers. The fluvial systems draining Eurasia and central Europe introduce large volumes of sediment and dissolved nutrients into the Black Sea, but the distribution of these nutrients is controlled by the degree of physiochemical stratification, which is, in turn, dictated by seasonal physiographic development.
During winter, strong wind promotes convective overturning and upwelling of nutrients, while high summer temperatures result in a marked vertical stratification and a warm, shallow mixed layer. Day length and insolation intensity also controls the extent of the photic zone. Subsurface productivity is limited by nutrient availability, as the anoxic bottom waters act as a sink for reduced nitrate, in the form of ammonia. The benthic zone also plays an important role in Black Sea nutrient cycling, as chemosynthetic organisms and anoxic geochemical pathways recycle nutrients which can be upwelled to the photic zone, enhancing productivity.
The main phytoplankton groups present in the Black Sea are dinoflagellates, diatoms, coccolithophores and cyanobacteria. Generally, the annual cycle of phytoplankton development comprises significant diatom and dinoflagellate-dominated spring production, followed by a weaker mixed assemblage of community development below the seasonal thermocline during summer months and surface-intensified autumn production. This pattern of productivity is also augmented by an Emiliania huxleyi bloom during the late spring and summer months.
- Annual dinoflagellate distribution is defined by an extended bloom period in subsurface waters during the late spring and summer. In November, subsurface plankton production is combined with surface production, due to vertical mixing of water masses and nutrients such as nitrite. The major bloom-forming dinoflagellate species in the Black Sea is Gymnodinium sp. Estimates of dinoflagellate diversity in the Black Sea range from 193 to 267 species. This level of species richness is relatively low in comparison to the Mediterranean Sea, which is attributable to the brackish conditions, low water transparency and presence of anoxic bottom waters. It is also possible that the low winter temperatures below 4 °C (39 °F) of the Black Sea prevent thermophilous species from becoming established. The relatively high organic matter content of Black Sea surface water favor the development of heterotrophic (an organism that uses organic carbon for growth) and mixotrophic dinoflagellates species (able to exploit different trophic pathways), relative to autotrophs. Despite its unique hydrographic setting, there are no confirmed endemic dinoflagellate species in the Black Sea.
- The Black Sea is populated by many species of the marine diatom, which commonly exist as colonies of unicellular, non-motile auto- and heterotrophic algae. The life-cycle of most diatoms can be described as 'boom and bust' and the Black Sea is no exception, with diatom blooms occurring in surface waters throughout the year, most reliably during March. In simple terms, the phase of rapid population growth in diatoms is caused by the in-wash of silicon-bearing terrestrial sediments, and when the supply of silicon is exhausted, the diatoms begin to sink out of the photic zone and produce resting cysts. Additional factors such as predation by zooplankton and ammonium-based regenerated production also have a role to play in the annual diatom cycle.<, ref name="Oguz99"/> Typically, Proboscia alata blooms during spring and Pseudosolenia calcar-avis blooms during the autumn.
- Coccolithophores are a type of motile, autotrophic phytoplankton that produce CaCO3 plates, known as coccoliths, as part of their life cycle. In the Black Sea, the main period of coccolithophore growth occurs after the bulk of the dinoflagellate growth has taken place. In May, the dinoflagellates move below the seasonal thermocline, into deeper waters, where more nutrients are available. This permits coccolithophores to utilize the nutrients in the upper waters, and by the end of May, with favorable light and temperature conditions, growth rates reach their highest. The major bloom-forming species is Emiliania huxleyi, which is also responsible for the release of dimethyl sulfide into the atmosphere. Overall, coccolithophore diversity is low in the Black Sea, and although recent sediments are dominated by E. huxleyi, Braarudosphaera bigelowii, Holocene sediments have also been shown to contain Helicopondosphaera and Discolithina species.
- Cyanobacteria are a phylum of picoplanktonic (plankton ranging in size from 0.2 to 2.0 µm) bacteria that obtain their energy via photosynthesis, and are present throughout the world's oceans. They exhibit a range of morphologies, including filamentous colonies and biofilms. In the Black Sea, several species are present, and as an example, Synechococcus spp. can be found throughout the photic zone, although concentration decreases with increasing depth. Other factors which exert an influence on distribution include nutrient availability, predation, and salinity.
- The Black Sea along with the Caspian Sea is part of the Zebra mussel's native range. The mussel has been accidentally introduced around the world and become an invasive species where it has been introduced.
- The Common Carp's native range extends to The Black Sea along with the Caspian Sea and Aral Sea. Like the Zebra mussel the Common Carp is an invasive species when introduced to other habitats.
- Is another native fish that is also found in the Caspian Sea. It preys upon Zebra mussels. Like the mussels and common carp it has become invasive when introduced to other environments, like the Great Lakes.
- Marine Mammals and marine megafaunas
- Marine mammals present within the basin include two species of dolphins (common and bottlenose) and harbour porpoise inhabit the sea although all of these are endangered due to pressures and impacts by human activities. All the three species have been classified as a distinct subspecies from those in the Mediterranean and in Atlantic Seas and endemic to Black and Azov Seas, and are more active during nights in Turkish Straits. However, construction of the Crimean Bridge caused increases in nutrients and planktons in the waters, attracting large numbers of fish and more than 1,000 bottlenose dolphins. On the other hand, however, others claim that construction may cause devastating damages on ecosystem including dolphins.
- Critically endangered Mediterranean monk seals were historically abundant in Black Sea, and are regarded to have become extinct from the basin in 1997. Monk seals were present at the Snake Island until 1950s, and several locations such as the Danube Plavni Nature Reserve and Doğankent were last of hauling-out sites in post-1990. Very few animals still thrive in the Sea of Marmara.
- Ongoing Mediterranizations may or may not boost in increases of cetacean diversity in Turkish Straits hence in Black and Azov basins.
- Various species of pinnipeds, sea otter, and beluga whales were introduced into the Black Sea by mankind and later escaped either by accidental or purported causes. Of these, grey seal and beluga whales have been recorded with successful, long-term occurrences.
- Great white sharks are known to reach into the Sea of Marmara and Bosporus Strait and basking shark into Dardanelles although it is unclear whether or not these sharks may reach into the Black and Azov basins.
Ecological effects of pollution
Since the 1960s, rapid industrial expansion along the Black Sea coast line and the construction of a major dam has significantly increased annual variability in the N:P:Si ratio in the basin. In coastal areas, the biological effect of these changes has been an increase in the frequency of monospecific phytoplankton blooms, with diatom bloom frequency increasing by a factor of 2.5 and non-diatom bloom frequency increasing by a factor of 6. The non-diatoms, such as the prymnesiophytes Emiliania huxleyi (coccolithophore), Chromulina sp., and the Euglenophyte Eutreptia lanowii are able to out-compete diatom species because of the limited availability of Si, a necessary constituent of diatom frustules. As a consequence of these blooms, benthic macrophyte populations were deprived of light, while anoxia caused mass mortality in marine animals.
The decline in macrophytes was further compounded by overfishing during the 1970s, while the invasive ctenophore Mnemiopsis reduced the biomass of copepods and other zooplankton in the late 1980s. Additionally, an alien species—the warty comb jelly (Mnemiopsis leidyi)—was able to establish itself in the basin, exploding from a few individuals to estimated biomass of one billion metric tons. The change in species composition in Black Sea waters also has consequences for hydrochemistry, as Ca-producing coccolithophores influence salinity and pH, although these ramifications have yet to be fully quantified. In central Black Sea waters, Si levels were also significantly reduced, due to a decrease in the flux of Si associated with advection across isopycnal surfaces. This phenomenon demonstrates the potential for localized alterations in Black Sea nutrient input to have basin-wide effects.
Pollution reduction and regulation efforts have led to a partial recovery of the Black Sea ecosystem during the 1990s, and an EU monitoring exercise, 'EROS21', revealed decreased N and P values, relative to the 1989 peak. Recently, scientists have noted signs of ecological recovery, in part due to the construction of new sewage treatment plants in Slovakia, Hungary, Romania, and Bulgaria in connection with membership in the European Union. Mnemiopsis leidyi populations have been checked with the arrival of another alien species which feeds on them.
In the past, the range of the Asiatic lion extended from South Asia to the Balkans, possibly up to the Danube. Places like Turkey and the Trans-Caucasus were in this range. The Caspian tiger occurred in eastern Turkey and the Caucasus, at least. The lyuti zver (Old East Slavic for "fierce animal") that was encountered by Vladimir II Monomakh, Velikiy Kniaz of Kievan Rus' (which ranged to the Black Sea in the south), may have been a tiger or leopard, rather than a wolf or lynx, due to the way it behaved towards him and his horse.
Short-term climatic variation in the Black Sea region is significantly influenced by the operation of the North Atlantic oscillation, the climatic mechanisms resulting from the interaction between the north Atlantic and mid-latitude air masses. While the exact mechanisms causing the North Atlantic Oscillation remain unclear, it is thought the climate conditions established in western Europe mediate the heat and precipitation fluxes reaching Central Europe and Eurasia, regulating the formation of winter cyclones, which are largely responsible for regional precipitation inputs and influence Mediterranean Sea Surface Temperatures (SST's).
The relative strength of these systems also limits the amount of cold air arriving from northern regions during winter. Other influencing factors include the regional topography, as depressions and storms systems arriving from the Mediterranean are funneled through the low land around the Bosporus, Pontic and Caucasus mountain ranges acting as waveguides, limiting the speed and paths of cyclones passing through the region.
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Some islands in the Black sea belong to Bulgaria, Romania, Turkey, and Ukraine:
- St. Thomas Island – Bulgaria
- St. Anastasia Island – Bulgaria
- St. Cyricus Island – Bulgaria
- St. Ivan Island – Bulgaria
- St. Peter Island – Bulgaria
- Sacalinu Mare Island – Romania
- Sacalinu Mic Island – Romania
- Misura / Novaya Zemliya – Romania and Ukraine
- Utrish Island
- Krupinin Island
- Sudiuk Island
- Kefken Island
- Oreke Island
- Giresun Island
- Dzharylgach Island – Ukraine
- Zmiinyi (Snake) Island – Ukraine
Mediterranean connection during the Holocene
The Black Sea is connected to the World Ocean by a chain of two shallow straits, the Dardanelles and the Bosporus. The Dardanelles is 55 m (180 ft) deep and the Bosporus is as shallow as 36 m (118 ft). By comparison, at the height of the last ice age, sea levels were more than 100 m (330 ft) lower than they are now.
There is also evidence that water levels in the Black Sea were considerably lower at some point during the post-glacial period. Some researchers theorize that the Black Sea had been a landlocked freshwater lake (at least in upper layers) during the last glaciation and for some time after.
In the aftermath of the last glacial period, water levels in the Black Sea and the Aegean Sea rose independently until they were high enough to exchange water. The exact timeline of this development is still subject to debate. One possibility is that the Black Sea filled first, with excess freshwater flowing over the Bosporus sill and eventually into the Mediterranean Sea. There are also catastrophic scenarios, such as the "Black Sea deluge theory" put forward by William Ryan, Walter Pitman and Petko Dimitrov.
The Black Sea deluge is a hypothesized catastrophic rise in the level of the Black Sea circa 5600 BC due to waters from the Mediterranean Sea breaching a sill in the Bosporus Strait. The hypothesis was headlined when The New York Times published it in December 1996, shortly before it was published in an academic journal. While it is agreed that the sequence of events described did occur, there is debate over the suddenness, dating, and magnitude of the events. Relevant to the hypothesis is that its description has led some to connect this catastrophe with prehistoric flood myths.
The Black Sea was a busy waterway on the crossroads of the ancient world: the Balkans to the west, the Eurasian steppes to the north, the Caucasus and Central Asia to the east, Asia Minor and Mesopotamia to the south, and Greece to the south-west.
The oldest processed gold in the world was found in Varna, Bulgaria, and Greek mythology portrays the Argonauts as sailing on the Black Sea. The land at the eastern end of the Black Sea, Colchis, (now Georgia), marked for the Greeks the edge of the known world.
The steppes to the north of the Black Sea have been suggested as the original homeland (Urheimat) of the speakers of the Proto-Indo-European language, (PIE) the progenitor of the Indo-European language family, by some scholars such as Marija Gimbutas; others move the homeland further east towards the Caspian Sea, yet others to Anatolia.
Greek presence in the Black Sea began at least as early as the 9th century BC with colonization the Black Sea's southern coast. By 500 BC, permanent Greek communities existed all around the Black Sea and a lucrative trade network connected the entirety of the Black Sea to the wider Mediterranean. While Greek colonies generally maintained very close cultural ties to their founding polis, Greek colonies in the Black Sea began to develop their own Black Sea Greek culture, know today as Pontic. The coastal community of Black Sea Greeks remained a prominent part of the Greek World for centuries.
The Black Sea became a virtual Ottoman Navy lake within five years of Genoa losing the Crimean Peninsula in 1479, after which the only Western merchant vessels to sail its waters were those of Venice's old rival Ragusa. This restriction was challenged by the Russian Navy from 1783 until the relaxation of export controls in 1789 because of the French Revolution.
Ancient trade routes in the region are currently[when?] being extensively studied by scientists, as the Black Sea was sailed by Hittites, Carians, Colchians, Thracians, Greeks, Persians, Cimmerians, Scythians, Romans, Byzantines, Goths, Huns, Avars, Slavs, Varangians, Crusaders, Venetians, Genoese, Georgians, Tatars and Ottomans.
Perhaps the most promising areas in deepwater archaeology are the quest for submerged prehistoric settlements in the continental shelf and for ancient shipwrecks in the anoxic zone, which are expected to be exceptionally well preserved due to the absence of oxygen. This concentration of historical powers, combined with the preservative qualities of the deep anoxic waters of the Black Sea, has attracted increased interest from marine archaeologists who have begun to discover a large number of ancient ships and organic remains in a high state of preservation.
Commercial and civic use
According to NATO, the Black sea is a strategic corridor that provides smuggling channels for moving legal and illegal goods including drugs, radioactive materials, and counterfeit goods that can be used to finance terrorism.
Ports and ferry terminals
Merchant fleet and traffic
According to the International Transport Workers' Federation 2013 study, there were around 2,400 commercial vessels operating in the Black Sea.
Anchovy: the Turkish commercial fishing fleet catches around 300,000 tons per year on average, and fishery carried out mainly in winter and the highest portion of the stock is caught between November and December.
Since the 1980s, the Soviet Union started offshore drilling for petroleum in the sea's western portion (adjoining Ukraine's coast). Independent Ukraine continued and intensified that effort within its exclusive economic zone, inviting major international oil companies for exploration. Discovery of the new, massive oilfields in the area stimulated an influx of foreign investments. It also provoked a short-term peaceful territorial dispute with Romania which was resolved in 2011 by an international court redefining the exclusive economic zones between the two countries.
Holiday resorts and spas
In the years following the end of the Cold War, the popularity of the Black Sea as a tourist destination steadily increased. Tourism at Black Sea resorts became one of the region's growth industries. The following is a list of notable Black Sea resort towns:
- 2 Mai (Romania)
- Agigea (Romania)
- Ahtopol (Bulgaria)
- Amasra (Turkey)
- Anaklia (Georgia)
- Anapa (Russia)
- Albena (Bulgaria)
- Alupka (Crimea, Ukraine/Russia (disputed))
- Alushta (Crimea, Ukraine/Russia (disputed))
- Balchik (Bulgaria)
- Batumi (Georgia)
- Burgas (Bulgaria)
- Byala (Bulgaria)
- Cap Aurora (Romania)
- Chakvi (Georgia)
- Constantine and Helena (Bulgaria)
- Constanța (Romania)
- Corbu (Romania)
- Costineşti (Romania)
- Eforie (Romania)
- Emona (Bulgaria)
- Eupatoria (Crimea, Ukraine/Russia (disputed))
- Foros (Crimea, Ukraine/Russia (disputed))
- Feodosiya (Crimea, Ukraine/Russia (disputed))
- Giresun (Turkey)
- Gagra (Abkhazia, Georgia[a])
- Gelendzhik (Russia)
- Golden Sands (Bulgaria)
- Gonio (Georgia)
- Gurzuf (Crimea, Ukraine/Russia (disputed))
- Hopa (Artvin, Turkey)
- Istanbul (Turkey)
- Jupiter (Romania)
- Kamchia (Bulgaria)
- Kavarna (Bulgaria)
- Kiten (Bulgaria)
- Kobuleti (Georgia)
- Koktebel (Crimea, Ukraine/Russia (disputed))
- Lozenetz (Bulgaria)
- Mamaia (Romania)
- Mangalia (Romania)
- Năvodari (Romania)
- Neptun (Romania)
- Nesebar (Bulgaria)
- Novorossiysk (Russia)
- Ordu (Turkey)
- Obzor (Bulgaria)
- Odessa (Ukraine)
- Olimp (Romania)
- Pitsunda (Abkhazia, Georgia[a])
- Pomorie (Bulgaria)
- Primorsko (Bulgaria)
- Rize (Turkey)
- Rusalka (Bulgaria)
- Samsun (Turkey)
- Saturn (Romania)
- Sinop (Turkey)
- Sochi (Russia)
- Sozopol (Bulgaria)
- Sudak (Crimea, Ukraine/Russia (disputed))
- Skadovsk (Ukraine)
- Sulina (Romania)
- Sunny Beach (Bulgaria)
- Şile (Turkey)
- Sveti Vlas (Bulgaria)
- Trabzon (Turkey)
- Tsikhisdziri (Georgia)
- Tuapse (Russia)
- Ureki (Georgia)
- Vama Veche (Romania)
- Varna (Bulgaria)
- Venus (Romania)
- Yalta (Crimea, Ukraine/Russia (disputed))
- Zonguldak (Turkey)
Modern military use
International and military use of the Straits
The 1936 Montreux Convention provides for free passage of civilian ships between the international waters of the Black and the Mediterranean Seas. However, a single country (Turkey) has complete control over the straits connecting the two seas. Military ships are separate categories from civilian ships and they can only pass through the straits if the ship is belonging to a Black Seapower. Other military ships have the right to pass through the straits if they are not in a war against Turkey and they can stay in the Black Sea basin for a limited time. The 1982 amendments to the Montreux Convention allow Turkey to close the Straits at its discretion in both wartime and peacetime.
The 1936 Montreux Convention governs the passage of vessels between the Black, the Mediterranean and Aegean Seas and the presence of military vessels belonging to non-littoral states in the Black Sea waters.
- 1927 Crimean earthquakes
- Ancient Black Sea shipwrecks
- Anoxic event
- Bulgarian Black Sea Coast
- Caucasian Riviera
- Internationalization of the Danube River
- Karadeniz Technical University
- Kuma–Manych Depression
- Mount Akhun
- Romanian Black Sea resorts
- UNEP/GRID-Arendal Maps and Graphics Library (2001). "Socio-economic indicators for the countries of the Black Sea basin". Archived from the original on February 10, 2011. Retrieved December 11, 2010.CS1 maint: uses authors parameter (link)
- "Black Sea Geography, Oceanography, Ecology, History" Living Black Sea
- Surface Area—"Black Sea Geography". University of Delaware College of Marine Studies. 2003. Retrieved April 3, 2014.
- Maximum Depth—"Europa – Gateway of the European Union Website". Environment and Enlargement – The Black Sea: Facts and Figures. Archived from the original on November 14, 2008.
- Murray, J. W.; Jannasch, H. W.; Honjo, S; Anderson, R. F.; Reeburgh, W. S.; Top, Z.; Friederich, G. E.; Codispoti, L. A.; Izdar, E. (March 30, 1989). "Unexpected changes in the oxic/anoxic interface in the Black Sea". Nature. 338 (6214): 411–413. Bibcode:1989Natur.338..411M. doi:10.1038/338411a0.
- World and Its Peoples. Marshall Cavendish. July 21, 2010. p. 1444. ISBN 9780761479024 – via Internet Archive.
black sea 1175 km east west.
- Gray, Richard (August 1, 2010). "Undersea river discovered flowing on sea bed". The Daily Telegraph. Retrieved August 2, 2010.
- "Limits of Oceans and Seas, 3rd edition" (PDF). International Hydrographic Organization. 1953. Retrieved February 7, 2010.
- "Turkish Statistical Institute". Rapor.tuik.gov.tr. Archived from the original on August 25, 2012. Retrieved January 14, 2014.
- "Turkish Statistical Institute". Rapor.tuik.gov.tr. Archived from the original on January 16, 2014. Retrieved January 14, 2014.
- "Cât a crescut populația în principalele zone metropolitane ale țării în ultimele două decenii". www.analizeeconomice.ro.
- "Turkish Statistical Institute". Rapor.tuik.gov.tr. Archived from the original on January 16, 2014. Retrieved January 14, 2014.
- "Turkish Statistical Institute". Rapor.tuik.gov.tr. Archived from the original on March 19, 2013. Retrieved January 14, 2014.
- "Batumi City Hall website". Retrieved August 10, 2017.
- Özhan Öztürk (2005). Karadeniz Ansiklopedik Sözlük. İstanbul: Heyamola Yayınları. pp. 617–620. Archived from the original on October 15, 2012.
- Schmitt 1989, pp. 310–313.
- Peterson, Joseph H. "Greater Bundahishn". www.avesta.org. Retrieved July 1, 2017.
- Gibbon, Edward (1993) . The History of the Decline and Fall of the Roman Empire. Everyman's Library. ISBN 0-679-42308-7.
- Simmons, M. D.; Tari, G. C.; Okay, A. I., eds. (2018). Petroleum Geology of the Black Sea. The Geological Society of London. p. 2. ISBN 9781786203588.CS1 maint: ref=harv (link)
- McKenzie, DP (1970). "Plate tectonics of the Mediterranean region". Nature. 226 (5242): 239–43. Bibcode:1970Natur.226..239M. doi:10.1038/226239a0. PMID 16057188.
- McClusky, S.; S. Balassanian; et al. (2000). "Global Positioning System constraints on plate kinematics and dynamics in the eastern Mediterranean and Caucasus" (PDF). Journal of Geophysical Research. 105 (B3): 5695–5719. Bibcode:2000JGR...105.5695M. doi:10.1029/1999JB900351.
- Shillington, Donna J.; White, Nicky; Minshull, Timothy A.; Edwards, Glyn R.H.; Jones, Stephen M.; Edwards, Rosemary A.; Scott, Caroline L. (2008). "Cenozoic evolution of the eastern Black Sea: A test of depth-dependent stretching models" (PDF). Earth and Planetary Science Letters. 265 (3–4): 360–378. Bibcode:2008E&PSL.265..360S. doi:10.1016/j.epsl.2007.10.033.
- Simmons, Tari & Okay 2018, p. 11.
- Nikishin, A (2003). "The Black Sea basin: tectonic history and Neogene–Quaternary rapid subsidence modelling". Sedimentary Geology. 156 (1–4): 149–168. Bibcode:2003SedG..156..149N. doi:10.1016/S0037-0738(02)00286-5.
- Barale, Vittorio; Gade, Martin (2008). Remote Sensing of the European Seas. p. 17. ISBN 978-1-4020-6771-6.
- Prothero, G.W. (1920). Anatolia. London: H.M. Stationery Office.
- "Agriculture in the Black Sea Region". Bs-agro.com. Archived from the original on October 31, 2013. Retrieved January 14, 2014.
- Simmons, Tari & Okay 2018, p. 10-12.
- Descriptive Physical Oceanography. Talley, Pickard, Emery, Swift.
- "Meromictic". Merriam-webster.com. Retrieved January 14, 2014.
- "Exploring Ancient Mysteries: A Black Sea Journey". Ceoe.udel.edu. Retrieved January 14, 2014.
- Gregg, M. C., and E. O¨ zsoy (2002), Flow, water mass changes, and hydraulics in the Bosporus, J. Geophys. Res., 107(C3), 3016, doi:10.1029/2000JC000485
- "Black Sea Commission, State of Environment Report 2001-2006/7, Chap. 1B".
- "Black Sea Commission, State of Environment Report 2001-2006/7, Chap. 1A".
- Korotaev, G. (2003). "Seasonal, interannual, and mesoscale variability of the Black Sea upper layer circulation derived from altimeter data". Journal of Geophysical Research. 108 (C4): 3122. Bibcode:2003JGRC..108.3122K. doi:10.1029/2002JC001508.
- Black Sea Becomes Turquoise Archived October 28, 2008, at the Wayback Machine earthobservatory.nasa.gov. Retrieved December 2, 2006.
- Schuiling, Roelof Dirk; Cathcart, Richard B.; Badescu, Viorel; Isvoranu, Dragos; Pelinovsky, Efim (2006). "Asteroid impact in the Black Sea. Death by drowning or asphyxiation?". Natural Hazards. 40 (2): 327–338. doi:10.1007/s11069-006-0017-7.
- "Asteroid impact in the Black Sea: tsunami and toxic gas emission" (PDF). www.cosis.net.
- Oguz, T.; H. W. Ducklow; et al. (1999). "A physical-biochemical model of plankton productivity and nitrogen cycling in the Black Sea" (PDF). Deep-Sea Research Part I. 46 (4): 597–636. Bibcode:1999DSRI...46..597O. doi:10.1016/S0967-0637(98)00074-0. Archived from the original (PDF) on April 26, 2012.
- Oguz, T. & A. Merico (2006). "Factors controlling the summer Emiliania huxleyi bloom in the Black Sea: A modeling study" (PDF). Journal of Marine Systems. 59 (3–4): 173–188. Bibcode:2006JMS....59..173O. doi:10.1016/j.jmarsys.2005.08.002. Archived from the original (PDF) on April 26, 2012.
- Friedrich, J.; C. Dinkel; et al. (2002). "Benthic Nutrient Cycling and Diagenetic Pathways in the North-western Black Sea" (PDF). Estuarine, Coastal and Shelf Science. 54 (3): 369–383. Bibcode:2002ECSS...54..369F. doi:10.1006/ecss.2000.0653. Archived from the original (PDF) on October 4, 2011.
- Mechanisms impeding the natural Mediterranization process of Black Sea fauna (pdf). Retrieved on September 6, 2017
- Selifonova P.J.. 2011. Ships’ ballast as a Primary Factor for‘Mediterranization’of Pelagic Copepod Fauna (Copepoda) in the Northeastern Black Sea (pdf). Retrieved on September 6, 2017
- Eker, E.; L. Georgieva; et al. (1999). "Phytoplankton distribution in the western and eastern Black Sea in spring and autumn 1995" (PDF). ICES Journal of Marine Science. 56: 15–22. doi:10.1006/jmsc.1999.0604. Archived from the original (PDF) on April 26, 2012.
- Eker-Develi, E (2003). "Distribution of phytoplankton in the southern Black Sea in summer 1996, spring and autumn 1998". Journal of Marine Systems. 39 (3–4): 203–211. Bibcode:2003JMS....39..203E. doi:10.1016/S0924-7963(03)00031-9.
- Krakhmalny, A. F. (1994). "Dinophyta of the Black Sea (Brief history of investigations and species diversity)." Algologiya 4: 99–107.
- Gomez, F. & L. Briceno (2004). "An annotated checklist of dinoflagellates in the Black Sea" (PDF). Hydrobiologia. 517 (1): 43–59. doi:10.1023/B:HYDR.0000027336.05452.07.
- Uysal, Z (2006). "Vertical distribution of marine cyanobacteria Synechococcus spp. in the Black, Marmara, Aegean, and eastern Mediterranean seas". Deep-Sea Research Part II. 53 (17–19): 1976–1987. Bibcode:2006DSRII..53.1976U. doi:10.1016/j.dsr2.2006.03.016.
- "Delphinus delphis ssp. ponticus (Black Sea Common Dolphin, Common Dolphin, Short-beaked Common Dolphin)". IUCN Red List of Threatened Species.old-form url
- "Tursiops truncatus ssp. ponticus (Black Sea Bottlenose Dolphin, Common Bottlenose Dolphin)". IUCN Red List of Threatened Species.old-form url
- "Phocoena phocoena ssp. relicta (Black Sea Harbour Porpoise, Harbour Porpoise)". IUCN Red List of Threatened Species.old-form url
- First stranding record of a Risso's Dolphin (Grampus griseus) in the Marmara Sea, Turkey Archived October 20, 2017, at the Wayback Machine (pdf). Retrieved on September 6, 2017
- Goldman E.. 2017. Crimean bridge construction boosts dolphin population in Kerch Strait. The Russia Beyond the Headlines. Retrieved on March 10, 2017
- Reznikova E.. 2017. Крымские стройки убивают все живое на дне моря. Примечания. Новости Севастополя и Крыма. Retrieved on September 29, 2017
- Karamanlidis, A.; Dendrinos, P. (2015). "Monachus monachus". IUCN Red List of Threatened Species. 2015: e.T13653A45227543. doi:10.2305/IUCN.UK.2015-4.RLTS.T13653A45227543.en.
- Grinevetsky, Sergei R.; Zonn, Igor S.; Zhiltsov, Sergei S.; Kosarev, Aleksey N.; Kostianoy, Andrey G. (September 30, 2014). The Black Sea Encyclopedia. ISBN 9783642552274.
- Emek Inanmaz, Özgür; Değirmenci, Özgür; Gücü, Ali Cemal (2014). "A new sighting of the Mediterranean Monk Seal,Monachus monachus(Hermann, 1779), in the Marmara Sea (Turkey)". Zoology in the Middle East. 60 (3): 278–280. doi:10.1080/09397140.2014.944438.
- Frantzis A., Alexiadou P., Paximadis G., Politi E., Gannier A., Corsini-Foka M. (2003). "Current knowledge of the cetacean fauna of the Greek Seas" (PDF). Journal of Cetacean Research and Management. 5 (3): 219–232. Retrieved April 21, 2016.CS1 maint: uses authors parameter (link)
- Anderson R.. 1992. Black Sea Whale Aided By Activists. Chicago Tribune. Retrieved on April 21. 2016
- Gladilina, E.V.; Kovtun, Oleg; Kondakov, Andrey; Syomik, A.M.; Pronin, K.K.; Gol'din, Pavel (January 1, 2013). "Grey seal Halichoerus grypus in the Black Sea: The first case of long-term survival of an exotic pinniped". Marine Biodiversity Records. 6. doi:10.1017/S1755267213000018 – via ResearchGate.
- Kabasakal, Hakan (2014). "The status of the great white shark (Carcharodon carcharias) in Turkey's waters" (PDF). Marine Biodiversity Records. 7. doi:10.1017/S1755267214000980.
- Cuma. 2009. Çanakkale’de 10 metrelik köpekbalığı!. Retrieved on September 4, 2017
- Humborg, Christoph; Ittekkot, Venugopalan; Cociasu, Adriana; Bodungen, Bodo v. (1997). "Effect of Danube River dam on Black Sea biogeochemistry and ecosystem structure". Nature. 386 (6623): 385–388. Bibcode:1997Natur.386..385H. doi:10.1038/386385a0.
- Sburlea, A.; L. Boicenco; et al. (2006). "Aspects of eutrophication as a chemical pollution with implications on marine biota at the Romanian Black Sea shore". Chemicals as Intentional and Accidental Global Environmental Threats. NATO Security through Science Series: 357–360. doi:10.1007/978-1-4020-5098-5_28. ISBN 978-1-4020-5096-1.
- Gregoire, M.; C. Raick; et al. (2008). "Numerical modeling of the central Black Sea ecosystem functioning during the eutrophication phase". Progress in Oceanography. 76 (3): 286–333. Bibcode:2008PrOce..76..286G. doi:10.1016/j.pocean.2008.01.002.
- Colin Woodard (February 11, 2001). Ocean's end: travels through endangered seas. Basic Books. pp. 1–28. ISBN 978-0-465-01571-9. Retrieved August 1, 2011.
- Lancelot, C (2002). "Modelling the Danube-influenced North-western Continental Shelf of the Black Sea. II: Ecosystem Response to Changes in Nutrient Delivery by the Danube River after its Damming in 1972" (PDF). Estuarine, Coastal and Shelf Science. 54 (3): 473–499. Bibcode:2002ECSS...54..473L. doi:10.1006/ecss.2000.0659.
- Woodard, Colin, "The Black Sea's Cautionary Tale," Congressional Quarterly Global Researcher, October 2007, pp. 244–245
- Canadian Institute of Ukrainian Studies (1988). "Kyivan Rus'". Encyclopedia of Ukraine. Retrieved March 29, 2016.
- Geptner, V. G., Sludskij, A. A. (1972). Mlekopitajuščie Sovetskogo Soiuza. Vysšaia Škola, Moskva. (In Russian; English translation: Heptner, V.G., Sludskii, A. A., Komarov, A., Komorov, N.; Hoffmann, R. S. (1992). Mammals of the Soviet Union. Vol III: Carnivores (Feloidea). Smithsonian Institution and the National Science Foundation, Washington DC).
- Hurrell, J. W. (1995). "Decadal Trends in the North Atlantic Oscillation: Regional Temperatures and Precipitation". Science. 269 (5224): 676–679. Bibcode:1995Sci...269..676H. doi:10.1126/science.269.5224.676. PMID 17758812.
- Lamy, F., Arz, H. W., Bond, G. C., Barh, A. and Pätzold, J. (2006). "Multicentennial-scale hydrological changes in the Black Sea and northern Red Sea during the Holocene and the Arctic/North Atlantic Oscillation" (PDF). Paleoceanography. 21 (1): n/a. Bibcode:2006PalOc..21.1008L. doi:10.1029/2005PA001184. Archived from the original (PDF) on April 15, 2012.CS1 maint: uses authors parameter (link)
- Türkeş, Murat (1996). "Spatial and temporal analysis of annual rainfall variations in Turkey". International Journal of Climatology. 16 (9): 1057–1076. Bibcode:1996IJCli..16.1057T. doi:10.1002/(SICI)1097-0088(199609)16:9<1057::AID-JOC75>3.3.CO;2-4.
- Cullen, H. M.; A. Kaplan; et al. (2002). "Impact of the North Atlantic Oscillation on Middle Eastern climate and streamflow" (PDF). Climatic Change. 55 (3): 315–338. doi:10.1023/A:1020518305517.
- Ozsoy, E. & U. Unluata (1997). "Oceanography of the Black Sea: A review of some recent results". Earth-Science Reviews. 42 (4): 231–272. Bibcode:1997ESRv...42..231O. doi:10.1016/S0012-8252(97)81859-4.
- Brody, L. R., Nestor, M.J.R. (1980). Regional Forecasting Aids for the Mediterranean Basin. Handbook for Forecasters in the Mediterranean, Naval Research Laboratory. Part 2.
- Wilford, John Noble (December 17, 1996). "Geologists Link Black Sea Deluge To Farming's Rise". The New York Times. Retrieved June 17, 2013.
- William Ryan & Walter Pitman (1998). Noah's Flood: The New Scientific Discoveries About the Event That Changed History. New York: Simon & Schuster Paperbacks. ISBN 0-684-85920-3.
- King, Charles (March 18, 2004). "Pontus Euxinus 700BC–AD500". The Black Sea. Oxford University Press. ISBN 978-0-19-924161-3.
- David Nicolle (1989). The Venetian Empire 1200–1670. Osprey Publishing. p. 17. ISBN 978-0-85045-899-2.
- Bruce McGowan. Economic Life in Ottoman Europe: Taxation, Trade and the Struggle for Land, 1600–1800, Studies in Modern Capitalism. p. 134. ISBN 978-0-521-13536-8.
- "Black Sea Security". NATO Advanced Research Workshop. NATO. 2010. Retrieved December 31, 2010.
- "Черное море признано одним из самых неблагоприятных мест для моряков". International Transport Workers' Federation. BlackSeaNews. May 27, 2013. Retrieved September 20, 2013.
- Turkish Black Sea Acoustic Surveys: Winter distribution of anchovy along the Turkish coast Serdar SAKINAN. Middle East Technical University – Institute of Marine Sciences
- "Bulgarian Sea Resorts". Retrieved February 2, 2007.
- Postcard from the Silk Road - Batumi...(http://www.znadwiliiwilno.lt/wp-content/uploads/2020/04/Znad-Wilii-57m.pdf
- "Montreaux and The Bosporus Problem" (in Turkish).
- "Montreaux Convention and Turkey (pdf)" (PDF). Archived from the original (PDF) on March 19, 2013.
- Press, Associated (December 4, 2018). "Ukraine's ports partially unblocked by Russia, says Kiev" – via www.theguardian.com.
- Ghervas, Stella (2017). "The Black Sea". In Armitage, D.; Bashford, S. (eds.). Oceanic Histories. Cambridge: Cambridge University Press. pp. 234–266. doi:10.1017/9781108399722.010. ISBN 978-1-1083-9972-2.
- Stella Ghervas, "Odessa et les confins de l'Europe: un éclairage historique", in Stella Ghervas et François Rosset (ed), Lieux d'Europe. Mythes et limites (Paris: Editions de la Maison des sciences de l'homme, 2008), pp. 107–124. ISBN 978-2-7351-1182-4
- Charles King, The Black Sea: A History, 2004, ISBN 0-19-924161-9
- William Ryan and Walter Pitman, Noah's Flood, 1999, ISBN 0-684-85920-3
- Neal Ascherson, Black Sea (Vintage 1996), ISBN 0-09-959371-8
- Schmitt, Rüdiger (1989). "BLACK SEA". Black Sea – Encyclopaedia Iranica. Encyclopaedia Iranica, Vol. IV, Fasc. 3. pp. 310–313.CS1 maint: ref=harv (link)
- Rüdiger Schmitt, "Considerations on the Name of the Black Sea", in: Hellas und der griechische Osten (Saarbrücken 1996), pp. 219–224
- West, Stephanie (2003). 'The Most Marvellous of All Seas': the Greek Encounter with the Euxine. 50. Greece & Rome. pp. 151–167.
- Petko Dimitrov; Dimitar Dimitrov (2004). The Black Sea, the Flood and the Ancient Myths. Varna. p. 91. ISBN 978-954-579-335-6.
- Dimitrov, D. 2010. Geology and Non-traditional resources of the Black Sea. LAP Lambert Academic Publishing. ISBN 978-3-8383-8639-3. 244p.
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