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The Mediterranean Sea
Sea
is a sea connected to the Atlantic Ocean, surrounded by the Mediterranean Basin
Mediterranean Basin
and almost completely enclosed by land: on the north by Southern Europe
Southern Europe
and Anatolia, on the south by North Africa
North Africa
and on the east by the Levant. Although the sea is sometimes considered a part of the Atlantic Ocean, it is usually identified as a separate body of water. Geological evidence indicates that around 5.9 million years ago, the Mediterranean was cut off from the Atlantic and was partly or completely desiccated over a period of some 600,000 years, the Messinian
Messinian
salinity crisis, before being refilled by the Zanclean flood
Zanclean flood
about 5.3 million years ago. It covers an approximate area of 2.5 million km2 (965,000 sq mi), but its connection to the Atlantic (the Strait
Strait
of Gibraltar) is only 14 km (8.7 mi) wide. The Strait of Gibraltar
Gibraltar
is a narrow strait that connects the Atlantic Ocean
Atlantic Ocean
to the Mediterranean Sea
Sea
and separates Gibraltar
Gibraltar
and Spain
Spain
in Europe
Europe
from Morocco
Morocco
in Africa. In oceanography, it is sometimes called the Eurafrican Mediterranean Sea
Sea
or the European Mediterranean Sea
Sea
to distinguish it from mediterranean seas elsewhere.[2][3] The Mediterranean Sea
Sea
has an average depth of 1,500 m (4,900 ft) and the deepest recorded point is 5,267 m (17,280 ft) in the Calypso Deep
Calypso Deep
in the Ionian Sea. The sea is bordered on the north by Europe, the east by Asia, and in the south by Africa. It is located between latitudes 30° and 46° N and longitudes 6° W and 36° E. Its west-east length, from the Strait
Strait
of Gibraltar to the Gulf of Iskenderun, on the southwestern coast of Turkey, is approximately 4,000 km (2,500 miles). The sea's average north-south length, from Croatia’s southern shore to Libya, is approximately 800 km (500 miles). The Mediterranean Sea, including the Sea
Sea
of Marmara (connected by the Dardanelles
Dardanelles
to the Aegean Sea), has a surface area of approximately 2,510,000 square km (970,000 square miles).[4] The sea was an important route for merchants and travellers of ancient times that allowed for trade and cultural exchange between emergent peoples of the region. The history of the Mediterranean region is crucial to understanding the origins and development of many modern societies. The countries with coastlines on the Mediterranean Sea
Sea
are Albania, Algeria, Bosnia and Herzegovina, Croatia, Cyprus, Egypt, France, Greece, Israel, Italy, Lebanon, Libya, Malta, Morocco, Monaco, Montenegro, Slovenia, Spain, Syria, Tunisia
Tunisia
and Turkey. In addition, the Gaza Strip
Gaza Strip
and the British Overseas Territories
British Overseas Territories
of Gibraltar
Gibraltar
and Akrotiri and Dhekelia
Akrotiri and Dhekelia
have coastlines on the sea.

Contents

1 Name 2 History

2.1 Ancient civilisations 2.2 Middle Ages
Middle Ages
and empires 2.3 21st century
21st century
and migrations

3 Geography

3.1 Extent 3.2 Oceanography 3.3 Coastal countries 3.4 Coastal cities 3.5 Subdivisions

3.5.1 Other seas 3.5.2 Other features

3.6 10 largest islands by area 3.7 Climate

3.7.1 Sea
Sea
temperature

4 Geology

4.1 Tectonics
Tectonics
and paleoenvironmental analysis

4.1.1 Messinian
Messinian
salinity crisis 4.1.2 Desiccation and exchanges of flora and fauna 4.1.3 Shift to a "Mediterranean climate"

5 Paleoclimate 6 Ecology and biota 7 Environmental history

7.1 Natural hazards 7.2 Biodiversity

7.2.1 Invasive species 7.2.2 Arrival of new tropical Atlantic species

7.3 Sea-level rise 7.4 Pollution 7.5 Shipping 7.6 Tourism 7.7 Overfishing 7.8 Aquaculture

8 Gallery 9 See also 10 Notes 11 References 12 External links

Name[edit]

With its highly indented coastline and large number of islands, Greece has the longest Mediterranean coastline.

The Ancient Greeks called the Mediterranean simply η θάλασσα 'the Sea' or sometimes η μεγάλη θάλασσα 'the Great Sea', η ημέτερα θάλασσα 'Our Sea', or η θάλασσα η καθ'εμάς 'the sea around us'. The Romans called it Mare Magnum 'Great Sea' or Mare Internum 'Internal Sea' and, starting with the Roman Empire, Mare Nostrum
Mare Nostrum
'Our Sea'. The term Mare Mediterrāneum appears later: Solinus apparently used it in the 3rd century, but the earliest extant witness to it is in the 6th century, in Isidore of Seville.[5][6] It means 'in the middle of land, inland' in Latin, a compound of medius 'middle', terra 'land, earth', and -āneus 'having the nature of'. The Latin word is a calque of Greek μεσόγαιος 'inland', from μέσος 'in the middle' and γήϊος 'of the earth' (from γῆ 'land, earth'). The original meaning may have been 'the sea in the middle of the earth' rather than 'the sea enclosed by land'.[7][8] The Carthaginians
Carthaginians
called it the " Syrian
Syrian
Sea". In ancient Syrian
Syrian
texts, Phoenician epics and in the Hebrew Bible, it was primarily known as the "Great Sea" (הַיָּם הַגָּדוֹל, HaYam HaGadol, Numbers 34:6,7; Joshua 1:4, 9:1, 15:47; Ezekiel 47:10,15,20), or simply "The Sea" ( 1 Kings
1 Kings
5:9; comp. 1 Macc.
1 Macc.
14:34, 15:11); however, it has also been called the "Hinder Sea" (הַיָּם הָאַחֲרוֹן), due to its location on the west coast of Greater Syria
Syria
or the Holy Land, and therefore behind a person facing the east, sometimes translated as "Western Sea", (Deut. 11:24; Joel 2:20). Another name was the " Sea
Sea
of the Philistines" (יָם פְּלִשְׁתִּים, Exod. 23:31), from the people inhabiting a large portion of its shores near the Israelites. In Modern Hebrew, it is called HaYam HaTikhon (הַיָּם הַתִּיכוֹן) 'the Middle Sea'.[9] In Modern Arabic, it is known as al-Baḥr [al-Abyaḍ] al-Mutawassiṭ (البحر [الأبيض] المتوسط) 'the [White] Middle Sea'. In Islamic and older Arabic literature, it was Baḥr al-Rūm(ī (بحر الروم or بحر الرومي ) 'the Sea of the Romans' or 'the Roman Sea'; at first, the name referred only to the Eastern Mediterranean, later to the whole Mediterranean. Other Arabic names were translarALABaḥr al-šām(ī) (يبحر الشرومام) 'the Sea
Sea
of Syria' and Baḥr al-Maghrib (بحرالمغرب) 'the Sea
Sea
of the West'.[10][6] In Turkish, it is the Akdeniz 'the White Sea'; in Ottoman, ﺁق دكيز though that sometimes only means the Aegean Sea.[11] The origin of thε name is not clear, as it is not known in earlier Greek, Byzantine, or Islamic sources. It may be to contrast with the Black Sea.[10][9][12] In Persian, the name was translated as Baḥr-i Safīd, which was also used in later Ottoman Turkish. It is probably the origin of the colloquial Greek Άσπρη Θάλασσα.[10] History[edit] Main article: History
History
of the Mediterranean region Ancient civilisations[edit]

Greek (red) and Phoenician (yellow) colonies in antiquity c. the 6th century BCE

The Roman Empire
Roman Empire
at its farthest extent in AD 117

Several ancient civilisations were located around the Mediterranean shores, and were greatly influenced by their proximity to the sea. It provided routes for trade, colonisation, and war, as well as food (from fishing and the gathering of other seafood) for numerous communities throughout the ages.[13] Due to the shared climate, geology, and access to the sea, cultures centered on the Mediterranean tended to have some extent of intertwined culture and history. Two of the most notable Mediterranean civilisations in classical antiquity were the Greek city states and the Phoenicians, both of which extensively colonised the coastlines of the Mediterranean. Later, when Augustus
Augustus
founded the Roman Empire, the Romans referred to the Mediterranean as Mare Nostrum
Mare Nostrum
("Our Sea"). For the next 400 years, the Roman Empire
Roman Empire
completely controlled the Mediterranean Sea
Sea
and virtually all its coastal regions from Gibraltar
Gibraltar
to the Levant. Darius I of Persia, who conquered Ancient Egypt, built a canal linking the Mediterranean to the Red Sea. Darius's canal was wide enough for two triremes to pass each other with oars extended, and required four days to traverse.[14] Middle Ages
Middle Ages
and empires[edit]

The Battle of Lepanto, 1571, ended in victory for the European Holy League against the Ottoman Turks.

The Western Roman Empire
Roman Empire
collapsed around AD 476. Temporarily the east was again dominant as Roman power lived on in the Byzantine Empire formed in the 4th century from the eastern half of the Roman Empire. Another power arose in the 7th century, and with it the religion of Islam, which soon swept across from the east; at its greatest extent, the Arab Empire controlled 75% of the Mediterranean region and left a lasting footprint on its eastern and southern shores. Europe
Europe
started to revive, however, as more organised and centralised states began to form in the later Middle Ages
Middle Ages
after the Renaissance of the 12th century.

The bombardment of Algiers
Algiers
by the Anglo-Dutch fleet in support of an ultimatum to release European slaves, August 1816

Ottoman power based in Anatolia
Anatolia
continued to grow, and in 1453 extinguished the Byzantine Empire
Byzantine Empire
with the Conquest of Constantinople. Ottomans gained control of much of the sea in the 16th century and maintained naval bases in southern France, Algeria
Algeria
and Tunisia. Barbarossa, the famous Ottoman captain is a symbol of this domination with the victory of the Battle of Preveza
Battle of Preveza
(1538). The Battle of Djerba (1560) marked the apex of Ottoman naval domination in the Mediterranean. As the naval prowess of the European powers increased, they confronted Ottoman expansion in the region when the Battle of Lepanto (1571) checked the power of the Ottoman Navy. This was the last naval battle to be fought primarily between galleys. The Barbary pirates
Barbary pirates
of North Africa
North Africa
preyed on Christian shipping and coastlines in the Western Mediterranean Sea.[15] According to Robert Davis, from the 16th to 19th centuries, pirates captured 1 million to 1.25 million Europeans as slaves.[16] The development of oceanic shipping began to affect the entire Mediterranean. Once, most trade between Western Europe
Europe
and the East had passed through the region, but after the 1490s the development of a sea route to the Indian Ocean
Indian Ocean
allowed the importation of Asian spices and other goods through the Atlantic ports of western Europe.[17][18][19] 21st century
21st century
and migrations[edit]

Satellite image of the Mediterranean Sea
Sea
at night

In 2013 the Maltese president described the Mediterranean sea as a "cemetery" due to the large amounts of migrants who drowned there after their boats capsized.[20] European Parliament president Martin Schulz said in 2014 that Europe's migration policy "turned the Mediterranean into a graveyard", referring to the number of drowned refugees in the region as a direct result of the policies.[21] An Azerbaijani official described the sea as "a burial ground ... where people die".[22] Following the 2013 Lampedusa migrant shipwreck, the Italian government decided to strengthen the national system for the patrolling of the Mediterranean Sea
Sea
by authorising "Operation Mare Nostrum", a military and humanitarian mission in order to rescue the migrants and arrest the traffickers of immigrants. In 2015, more than one million migrants crossed the Mediterranean Sea
Sea
into Europe.[23] Geography[edit]

A satellite image showing the Mediterranean Sea. The Strait
Strait
of Gibraltar
Gibraltar
can be seen in the bottom left (north-west) quarter of the image; to its left is the Iberian Peninsula
Iberian Peninsula
in Europe, and to its right, the Maghreb
Maghreb
in Africa.

The Dardanelles
Dardanelles
strait in Turkey. The north side is Europe
Europe
with the Gelibolu Peninsula
Gelibolu Peninsula
in the Thrace
Thrace
region; the south side is Anatolia
Anatolia
in Asia.

The Mediterranean Sea
Sea
is connected to the Atlantic Ocean
Atlantic Ocean
by the Strait of Gibraltar
Gibraltar
(known in Homer's writings as the "Pillars of Hercules") in the west and to the Sea
Sea
of Marmara and the Black Sea, by the Dardanelles
Dardanelles
and the Bosporus
Bosporus
respectively, in the east. The Sea
Sea
of Marmara (Dardanelles) is often considered a part of the Mediterranean Sea, whereas the Black Sea
Sea
is generally not. The 163 km (101 mi) long artificial Suez Canal
Suez Canal
in the southeast connects the Mediterranean Sea
Sea
to the Red Sea.[9] Large islands in the Mediterranean include Cyprus, Crete, Euboea, Rhodes, Lesbos, Chios, Kefalonia, Corfu, Limnos, Samos, Naxos and Andros
Andros
in the Eastern Mediterranean; Sicily, Cres, Krk, Brač, Hvar, Pag, Korčula
Korčula
and Malta
Malta
in the central Mediterranean; Sardinia, Corsica, and the Balearic Islands: Ibiza, Majorca, and Menorca
Menorca
in the Western Mediterranean. The typical Mediterranean climate
Mediterranean climate
has hot, humid, and dry summers and mild, rainy winters. Crops of the region include olives, grapes, oranges, tangerines, and cork. Extent[edit] The International Hydrographic Organization
International Hydrographic Organization
defines the limits of the Mediterranean Sea
Sea
as follows:[24] Stretching from the Strait
Strait
of Gibraltar
Gibraltar
in the west to the entrances to the Dardanelles
Dardanelles
and the Suez Canal
Suez Canal
in the east, the Mediterranean Sea
Sea
is bounded by the coasts of Europe, Africa
Africa
and Asia, and is divided into two deep basins:

Western Basin:

On the west: A line joining the extremities of Cape Trafalgar
Cape Trafalgar
(Spain) and Cape Spartel
Cape Spartel
(Africa). On the northeast: The west coast of Italy. In the Strait of Messina
Strait of Messina
a line joining the north extreme of Cape Paci (15°42'E) with Cape Peloro, the east extreme of the Island of Sicily. The north coast of Sicily. On the east: A line joining Cape Lilibeo the western point of Sicily (37°47′N 12°22′E / 37.783°N 12.367°E / 37.783; 12.367), through the Adventure Bank to Cape Bon
Cape Bon
(Tunisia).

Eastern Basin:

On the west: The northeastern and eastern limits of the Western Basin. On the northeast: A line joining Kum Kale (26°11'E) and Cape Helles, the western entrance to the Dardanelles. On the southeast: The entrance to the Suez Canal. On the east: The coasts of Syria
Syria
and Israel.

Oceanography[edit]

Predominant surface currents for June

Being nearly landlocked affects conditions in the Mediterranean Sea: for instance, tides are very limited as a result of the narrow connection with the Atlantic Ocean. The Mediterranean is characterised and immediately recognised by its deep blue colour. Evaporation
Evaporation
greatly exceeds precipitation and river runoff in the Mediterranean, a fact that is central to the water circulation within the basin.[25] Evaporation
Evaporation
is especially high in its eastern half, causing the water level to decrease and salinity to increase eastward.[26] The salinity at 5 m depth is 3.8%.[27] The pressure gradient pushes relatively cool, low-salinity water from the Atlantic across the basin; it warms and becomes saltier as it travels east, then sinks in the region of the Levant
Levant
and circulates westward, to spill over the Strait
Strait
of Gibraltar.[28] Thus, seawater flow is eastward in the Strait's surface waters, and westward below; once in the Atlantic, this chemically distinct Mediterranean Intermediate Water can persist thousands of kilometres away from its source.[29] The temperature of the water in the deepest part of the Mediterranean Sea
Sea
is 13.2 °C (55.8 °F).[27] Coastal countries[edit] For a more comprehensive list, see List of Mediterranean countries.

Map of the Mediterranean Sea

The following countries have a coastline on the Mediterranean Sea:

Northern shore (from west to east): Spain, France, Monaco, Italy, Slovenia, Croatia, Bosnia and Herzegovina, Montenegro, Albania, Greece and Turkey. Eastern shore (from north to south): Turkey, Syria, Lebanon, Israel. Southern shore (from west to east): Morocco, Algeria, Tunisia, Libya, Egypt. Island nations: Malta, Cyprus.

Several other territories also border the Mediterranean Sea
Sea
(from west to east): The British overseas territory
British overseas territory
of Gibraltar, the Spanish autonomous cities of Ceuta
Ceuta
and Melilla
Melilla
and nearby islands, the Sovereign Base Areas
Sovereign Base Areas
on Cyprus, and the Palestinian Gaza Strip.

Barcelona, the largest metropolitan area on the Mediterranean Sea
Sea
and also the headquarters of the Union for the Mediterranean

The Acropolis of Athens
Athens
with the Mediterranean Sea
Sea
in the background

The ancient port of Jaffa
Jaffa
(now part of Tel Aviv-Yafo) in Israel: according to the Bible, where Jonah
Jonah
set sail before being swallowed by a whale[30]

Alexandria, one of the largest cities on the Mediterranean

Catania, Sicily, with Mount Etna
Mount Etna
in the background

İzmir, the third metropolis of Turkey
Turkey
after Istanbul
Istanbul
and Ankara

Coastal cities[edit] For a more comprehensive list, see List of coastal settlements of the Mediterranean Sea. Major cities (municipalities) with populations larger than 200,000 people bordering the Mediterranean Sea
Sea
are:

Country Cities

Algeria Algiers, Annaba, Oran

Egypt Alexandria, Port Said

France Marseille, Nice

Greece Athens, Piraeus, Patras, Thessaloniki

Israel Ashdod, Haifa, Netanya, Rishon LeZion, Tel Aviv

Italy Bari, Catania, Genoa, Messina, Naples, Palermo, Rome, Taranto, Trieste, Venice

Lebanon Beirut, Tripoli

Libya Benghazi, Khoms, Misrata, Tripoli, Zawiya, Zliten

Morocco Tétouan, Tangier

Palestine Gaza City, Khan Yunis

Spain Alicante, Badalona, Barcelona, Cartagena, Málaga, Palma, Valencia.

Syria Latakia

Tunisia Sfax, Sousse, Tunis

Turkey Antalya, Adana, İzmir, Mersin

Subdivisions[edit]

Africa
Africa
(left, on horizon) and Europe
Europe
(right), as seen from Gibraltar

According to the International Hydrographic Organization
International Hydrographic Organization
(IHO), the Mediterranean Sea
Sea
is subdivided into a number of smaller waterbodies, each with their own designation (from west to east):[24]

the Strait
Strait
of Gibraltar; the Alboran Sea, between Spain
Spain
and Morocco; the Balearic Sea, between mainland Spain
Spain
and its Balearic Islands; the Ligurian Sea
Sea
between Corsica
Corsica
and Liguria
Liguria
(Italy); the Tyrrhenian Sea
Sea
enclosed by Sardinia, Italian peninsula
Italian peninsula
and Sicily; the Ionian Sea
Sea
between Italy, Albania
Albania
and Greece; the Adriatic Sea
Sea
between Italy, Slovenia, Croatia, Bosnia and Herzegovina, Montenegro
Montenegro
and Albania; the Aegean Sea
Sea
between Greece
Greece
and Turkey.

Other seas[edit]

Positano, Tyrrhenian Sea

Although not recognised by the IHO treaties, there are some other seas whose names have been in common use from the ancient times, or in the present:

the Sea
Sea
of Sardinia, between Sardinia
Sardinia
and Balearic Islands, as a part of the Balearic Sea the Sea
Sea
of Sicily
Sicily
between Sicily
Sicily
and Tunisia, the Libyan Sea
Sea
between Libya
Libya
and Crete, In the Aegean Sea,

the Thracian Sea
Sea
in its north, the Myrtoan Sea
Sea
between the Cyclades
Cyclades
and the Peloponnese, the Sea
Sea
of Crete
Crete
north of Crete, the Icarian Sea
Sea
between Kos
Kos
and Chios

the Cilician Sea
Sea
between Turkey
Turkey
and Cyprus the Levantine Sea
Sea
at the eastern end of the Mediterranean the Libyan Sea
Sea
the bay north of Libya

Many of these smaller seas feature in local myth and folklore and derive their names from these associations. Other features[edit]

View of the Saint George Bay, and snow-capped Mount Sannine
Mount Sannine
from the Corniche, Beirut

The Port of Marseille
Marseille
seen from L'Estaque

Sarandë, Albania
Albania
is situated on an open sea gulf of the Ionian sea
Ionian sea
in the central Mediterranean.

In addition to the seas, a number of gulfs and straits are also recognised:

the Saint George Bay
Saint George Bay
in Beirut, Lebanon the Ras Ibn Hani
Ras Ibn Hani
cape in Latakia, Syria the Ras al-Bassit
Ras al-Bassit
cape in northern Syria. the Minet el-Beida
Minet el-Beida
("White Harbour") bay near ancient Ugarit, Syria the Strait
Strait
of Gibraltar, connects the Atlantic Ocean
Atlantic Ocean
to the Mediterranean Sea
Sea
and separates Spain
Spain
from Morocco the Bay of Gibraltar, at the southern end of the Iberian Peninsula the Gulf of Corinth, an enclosed sea between the Ionian Sea
Sea
and the Corinth Canal the Pagasetic Gulf, the gulf of Volos, south of the Thermaic Gulf, formed by the Mount Pelion
Mount Pelion
peninsula the Saronic Gulf, the gulf of Athens, between the Corinth Canal
Corinth Canal
and the Mirtoan Sea the Thermaic Gulf, the gulf of Thessaloniki, located in the northern Greek region of Macedonia the Kvarner Gulf, Croatia the Gulf of Lion, south of France the Gulf of Valencia, east of Spain the Strait
Strait
of Messina, between Sicily
Sicily
and the toe of Italy the Gulf of Genoa, northwestern Italy the Gulf of Venice, northeastern Italy the Gulf of Trieste, northeastern Italy the Gulf of Taranto, southern Italy

The Paklinski Islands
Paklinski Islands
off the coast of Croatia; the Adriatic Sea contains over 1200 islands and islets

the Gulf of Salerno, southwestern Italy the Gulf of Gaeta, southwestern Italy the Gulf of Squillace, southern Italy the Strait
Strait
of Otranto, between Italy
Italy
and Albania the Gulf of Haifa, northern Israel the Gulf of Sidra, between Tripolitania
Tripolitania
(western Libya) and Cyrenaica (eastern Libya) the Strait
Strait
of Sicily, between Sicily
Sicily
and Tunisia the Corsica
Corsica
Channel, between Corsica
Corsica
and Italy the Strait
Strait
of Bonifacio, between Sardinia
Sardinia
and Corsica the Gulf of İskenderun, between İskenderun
İskenderun
and Adana
Adana
(Turkey) the Gulf of Antalya, between west and east shores of Antalya
Antalya
(Turkey) the Bay of Kotor, in south-western Montenegro
Montenegro
and south-eastern Croatia the Malta
Malta
Channel, between Sicily
Sicily
and Malta the Gozo
Gozo
Channel, between Malta
Malta
Island and Gozo

10 largest islands by area[edit]

The two biggest islands of the Mediterranean: Sicily
Sicily
and Sardinia (Italy)

Main article: List of islands in the Mediterranean

Country Island Area in km2 Population

Italy Sicily 25,460 5,048,995

Italy Sardinia 23,821 1,672,804

Cyprus Cyprus 9,251 1,088,503

France Corsica 8,680 299,209

Greece Crete 8,336 623,666

Greece Euboea 3,655 218.000

Spain Majorca 3,640 869,067

Greece Lesbos 1,632 90,643

Greece Rhodes 1,400 117,007

Greece Chios 842 51,936

Climate[edit]

Map of climate zones in the areas surrounding the Mediterranean Sea, according to the Köppen climate classification

Sea
Sea
temperature[edit]

Mean sea temperature (°C)

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year

Marseille[31] 13 13 13 14 16 18 21 22 21 18 16 14 16.6

Gibraltar[32] 16 15 16 16 17 20 22 22 22 20 18 17 18.4

Málaga[33] 16 15 15 16 17 20 22 23 22 20 18 16 18.3

Athens[34] 16 15 15 16 18 21 24 24 24 21 19 18 19.3

Barcelona[35] 13 13 13 14 17 20 23 25 23 20 17 15 17.8

Heraklion[36] 16 15 15 16 19 22 24 25 24 22 20 18 19.7

Venice[37] 11 10 11 13 18 22 25 26 23 20 16 14 17.4

Valencia[38] 14 13 14 15 17 21 24 26 24 21 18 15 18.5

Malta[39] 16 16 15 16 18 21 24 26 25 23 21 18 19.9

Alexandria[40] 18 17 17 18 20 23 25 26 26 25 22 20 21.4

Naples[41] 15 14 14 15 18 22 25 27 25 22 19 16 19.3

Larnaca[42] 18 17 17 18 20 24 26 27 27 25 22 19 21.7

Limassol[43] 18 17 17 18 20 24 26 27 27 25 22 19 21.7

Antalya 17 17 17 18 21 24 27 28 27 25 22 19 21.8

Tel Aviv[44] 18 17 17 18 21 24 26 28 27 26 23 20 22.1

Geology[edit]

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See also: Geology
Geology
and paleoclimatology of the Mediterranean Basin

A submarine karst spring, called vrulja, near Omiš; observed through several ripplings of an otherwise calm sea surface.

The geologic history of the Mediterranean Sea
Sea
is complex. Underlain by oceanic crust, the sea basin was once thought to be a tectonic remnant of the ancient Tethys Ocean; it is now known to be a structurally younger basin, called the Neotethys, which was first formed by the convergence of the African and Eurasian
Eurasian
plates during the Late Triassic
Triassic
and Early Jurassic. Because it is a near-landlocked body of water in a normally dry climate, the Mediterranean is subject to intensive evaporation and the precipitation of evaporites. The Messinian salinity crisis
Messinian salinity crisis
started about six million years ago (mya) when the Mediterranean became landlocked, and then essentially dried up. There are salt deposits accumulated on the bottom of the basin of more than a million cubic kilometres—in some places more than three kilometres thick.[45][46] Scientists estimate that the sea was last filled about 5.3 million years ago (mya) in less than two years by the Zanclean flood. Water poured in from the Atlantic Ocean
Atlantic Ocean
through a newly breached gateway now called the Strait
Strait
of Gibraltar
Gibraltar
at an estimated rate of about three orders of magnitude (one thousand times) larger than the current flow of the Amazon River.[47] The Mediterranean Sea
Sea
has an average depth of 1,500 m (4,900 ft) and the deepest recorded point is 5,267 m (17,280 ft) in the Calypso Deep
Calypso Deep
in the Ionian Sea. The coastline extends for 46,000 km (29,000 mi). A shallow submarine ridge (the Strait
Strait
of Sicily) between the island of Sicily
Sicily
and the coast of Tunisia
Tunisia
divides the sea in two main subregions: the Western Mediterranean, with an area of about 850 thousand km2 (330 thousand mi2); and the Eastern Mediterranean, of about 1.65 million km2 (640 thousand mi2). A characteristic of the coastal Mediterranean are submarine karst springs or vruljas, which discharge pressurised groundwater into the coastal seawater from below the surface; the discharge water is usually fresh, and sometimes may be thermal.[48][49] Tectonics
Tectonics
and paleoenvironmental analysis[edit]

Messinian salinity crisis
Messinian salinity crisis
before the Zanclean flood

Play media

Animation: Messinian
Messinian
salinity crisis

The Mediterranean basin and sea system was established by the ancient African-Arabian continent colliding with the Eurasian
Eurasian
continent. As Africa-Arabia drifted northward, it closed over the ancient Tethys Ocean
Ocean
which had earlier separated the two supercontinents Laurasia
Laurasia
and Gondwana. At about that time in the middle Jurassic
Jurassic
period a much smaller sea basin, dubbed the Neotethys, was formed shortly before the Tethys Ocean
Tethys Ocean
closed at its western (Arabian) end. The broad line of collisions pushed up a very long system of mountains from the Pyrenees in Spain
Spain
to the Zagros Mountains
Zagros Mountains
in Iran in an episode of mountain-building tectonics known as the Alpine orogeny. The Neotethys grew larger during the episodes of collisions (and associated foldings and subductions) that occurred during the Oligocene
Oligocene
and Miocene
Miocene
epochs (34 to 5.33 mya); see animation: Africa-Arabia colliding with Eurasia. Accordingly, the Mediterranean basin consists of several stretched tectonic plates in subduction which are the foundation of the Eastern part of the Mediterranean Sea. Various zones of subduction harbour and form the deepest and most majestic oceanic ridges, east of the Ionian Sea
Sea
and south of the Aegean. The Central Indian Ridge
Central Indian Ridge
runs East of the Mediterranean Sea
Sea
South-East across the in-between of Africa
Africa
and the Arabian Peninsula
Peninsula
into the Indian Ocean. Nevertheless, while man-made geopolitical turmoil and chaos have governed the coastlines of many various Mediterranean nations throughout the courses of ancient, modern, present and foreseeable history, the Plate tectonic status of nations bordering the Mediterranean Sea
Sea
will find sharing the same geological concerns and fate. Messinian
Messinian
salinity crisis[edit] During Mesozoic
Mesozoic
and Cenozoic
Cenozoic
times, as the northwest corner of Africa converged on Iberia, it lifted the Betic-Rif mountain belts across southern Iberia and northwest Africa. There the development of the intramontane Betic and Rif basins led to creating two roughly-parallel marine gateways between the Atlantic Ocean
Atlantic Ocean
and the Mediterranean Sea. Dubbed the Betic and Rifian corridors, they progressively closed during middle and late Miocene
Miocene
times; perhaps several times.[50] During late Miocene
Miocene
times the closure of the Betic Corridor
Betic Corridor
triggered the so-called " Messinian
Messinian
salinity crisis" (MSC), when the Mediterranean almost entirely dried out. The time of beginning of the MSC was recently estimated astronomically at 5.96 mya, and it persisted for some 630,000 years until about 5.3 mya;[51] see Animation: Messinian
Messinian
salinity crisis, at right. After the initial drawdown and re-flooding there followed more episodes—the total number is debated—of sea drawdowns and re-floodings for the duration of the MSC. It ended when the Atlantic Ocean
Ocean
last re-flooded the basin—creating the Strait
Strait
of Gibraltar
Gibraltar
and causing the Zanclean flood—at the end of the Miocene
Miocene
(5.33 mya). Some research has suggested that a desiccation-flooding-desiccation cycle may have repeated several times, which could explain several events of large amounts of salt deposition.[52][53] Recent studies, however, show that repeated desiccation and re-flooding is unlikely from a geodynamic point of view. [54][55] Desiccation and exchanges of flora and fauna[edit] The present-day Atlantic gateway, i.e. the Strait
Strait
of Gibraltar, originated in the early Pliocene
Pliocene
via the Zanclean Flood. As mentioned, two other gateways preceded Gibraltar: the Betic Corridor
Betic Corridor
across southern Spain
Spain
and the Rifian Corridor across northern Morocco. The former gateway closed about six (6) mya, causing the Messinian salinity crisis (MSC); the latter or possibly both gateways closed during the earlier Tortonian times, causing a " Tortonian salinity crisis" (from 11.6 to 7.2 mya), which occurred well before the MSC and lasted much longer. Both "crises" resulted in broad connections of the mainlands of Africa
Africa
and Europe, which thereby normalised migrations of flora and fauna—especially large mammals including primates—between the two continents. The Vallesian
Vallesian
crisis indicates a typical extinction and replacement of mammal species in Europe during Tortonian times following climatic upheaval and overland migrations of new species;[56] see Animation: Messinian
Messinian
salinity crisis (and mammal migrations), at right. The near-completely enclosed configuration of the Mediterranean basin has enabled the oceanic gateways to dominate seawater circulation and the environmental evolution of the sea and basin. Circulation patterns are also affected by several other factors—including climate, bathymetry, and water chemistry and temperature—which are interactive and can induce precipitation of evaporites. Deposits of evaporites accumulated earlier in the nearby Carpathian foredeep during the Middle Miocene, and the adjacent Red Sea
Sea
Basin (during the Late Miocene), and in the whole Mediterranean basin (during the MSC and the Messinian
Messinian
age). Diatomites are regularly found underneath the evaporite deposits, suggesting a connection between their geneses. Today, evaporation of surface seawater (output) is more than the supply (input) of fresh water by precipitation and coastal drainage systems, causing the salinity of the Mediterranean to be much higher than that of the Atlantic—so much so that the saltier Mediterranean waters sink below the waters incoming from the Atlantic, causing a two-layer flow across the Gibraltar
Gibraltar
strait: that is, an outflow submarine current of warm saline Mediterranean water, counterbalanced by an inflow surface current of less saline cold oceanic water from the Atlantic. Herman Sörgel's Atlantropa
Atlantropa
project proposal in the 1920s proposed a hydroelectric dam to be built across the Strait
Strait
of Gibraltar, using the inflow current to provide a large amount of hydroelectric energy. The underlying energy grid was as well intended to support a political union between Europe
Europe
and, at least, the Marghreb part of Africa
Africa
(compare Eurafrika for the later impact and Desertec
Desertec
for a later project with some parallels in the planned grid).[57] Shift to a "Mediterranean climate"[edit] The end of the Miocene
Miocene
also marked a change in the climate of the Mediterranean basin. Fossil evidence from that period reveals that the larger basin had a humid subtropical climate with rainfall in the summer supporting laurel forests. The shift to a "Mediterranean climate" occurred largely within the last three million years (the late Pliocene
Pliocene
epoch) as summer rainfall decreased. The subtropical laurel forests retreated; and even as they persisted on the islands of Macaronesia
Macaronesia
off the Atlantic coast of Iberia and North Africa, the present Mediterranean vegetation evolved, dominated by coniferous trees and sclerophyllous trees and shrubs with small, hard, waxy leaves that prevent moisture loss in the dry summers. Much of these forests and shrublands have been altered beyond recognition by thousands of years of human habitation. There are now very few relatively intact natural areas in what was once a heavily wooded region. Paleoclimate[edit] Because of its latitudinal position and its land-locked configuration, the Mediterranean is especially sensitive to astronomically induced climatic variations, which are well documented in its sedimentary record. Since the Mediterranean is involved in the deposition of eolian dust from the Sahara
Sahara
during dry periods, whereas riverine detrital input prevails during wet ones, the Mediterranean marine sapropel-bearing sequences provide high-resolution climatic information. These data have been employed in reconstructing astronomically calibrated time scales for the last 9 Ma of the Earth's history, helping to constrain the time of past geomagnetic reversals.[58] Furthermore, the exceptional accuracy of these paleoclimatic records has improved our knowledge of the Earth's orbital variations in the past. Ecology and biota[edit] As a result of the drying of the sea during the Messinian
Messinian
salinity crisis,[59] the marine biota of the Mediterranean are derived primarily from the Atlantic Ocean. The North Atlantic is considerably colder and more nutrient-rich than the Mediterranean, and the marine life of the Mediterranean has had to adapt to its differing conditions in the five million years since the basin was reflooded. The Alboran Sea
Sea
is a transition zone between the two seas, containing a mix of Mediterranean and Atlantic species. The Alboran Sea
Sea
has the largest population of bottlenose dolphins in the Western Mediterranean, is home to the last population of harbour porpoises in the Mediterranean, and is the most important feeding grounds for loggerhead sea turtles in Europe. The Alboran sea also hosts important commercial fisheries, including sardines and swordfish. The Mediterranean monk seals live in the Aegean Sea
Sea
in Greece. In 2003, the World Wildlife Fund
World Wildlife Fund
raised concerns about the widespread drift net fishing endangering populations of dolphins, turtles, and other marine animals such as the ogre cancer. See also: Specially Protected Areas of Mediterranean Importance Environmental history[edit]

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For 4,000 years, human activity has transformed most parts of Mediterranean Europe, and the "humanisation of the landscape" overlapped with the appearance of the present Mediterranean climate.[60] The image of a simplistic, environmental determinist notion of a Mediterranean Paradise on Earth
Earth
in antiquity, which was destroyed by later civilisations dates back to at least the 18th century and was for centuries fashionable in archaeological and historical circles. Based on a broad variety of methods, e.g. historical documents, analysis of trade relations, floodplain sediments, pollen, tree-ring and further archaeometric analyses and population studies, Alfred Thomas Grove and Oliver Rackham's work on "The Nature of Mediterranean Europe" challenges this common wisdom of a Mediterranean Europe
Europe
as a "Lost Eden", a formerly fertile and forested region, that had been progressively degraded and desertified by human mismanagement.[60] The belief stems more from the failure of the recent landscape to measure up to the imaginary past of the classics as idealised by artists, poets and scientists of the early modern Enlightenment.[60] The historical evolution of climate, vegetation and landscape in southern Europe
Europe
from prehistoric times to the present is much more complex and underwent various changes. For example, some of the deforestation had already taken place before the Roman age. While in the Roman age large enterprises as the Latifundiums took effective care of forests and agriculture, the largest depopulation effects came with the end of the empire. Some[who?] assume that the major deforestation took place in modern times — the later usage patterns were also quite different e.g. in southern and northern Italy. Also, the climate has usually been unstable and showing various ancient and modern "Little Ice Ages",[61] and plant cover accommodated to various extremes and became resilient with regard to various patterns of human activity.[60] Humanisation was therefore not the cause of climate change but followed it.[60] The wide ecological diversity typical of Mediterranean Europe
Europe
is predominantly based on human behavior, as it is and has been closely related human usage patterns.[60] The diversity range was enhanced by the widespread exchange and interaction of the longstanding and highly diverse local agriculture, intense transport and trade relations, and the interaction with settlements, pasture and other land use. The greatest human-induced changes, however, came after World War II, respectively in line with the '1950s-syndrome'[62] as rural populations throughout the region abandoned traditional subsistence economies. Grove and Rackham suggest that the locals left the traditional agricultural patterns towards taking a role as scenery-setting agents for the then much more important (tourism) travellers. This resulted in more monotonous, large-scale formations.[60] Among further current important threats to Mediterranean landscapes are overdevelopment of coastal areas, abandonment of mountains and, as mentioned, the loss of variety via the reduction of traditional agricultural occupations.[60] Natural hazards[edit]

Stromboli
Stromboli
volcano in Italy

The region has a variety of geological hazards which have closely interacted with human activity and land use patterns. Among others, in the eastern Mediterranean, the Thera eruption, dated to the 17th or 16th century BC, caused a large tsunami that some experts hypothesise devastated the Minoan civilisation on the nearby island of Crete, further leading some to believe that this may have been the catastrophe that inspired the Atlantis
Atlantis
legend.[63] Mount Vesuvius
Mount Vesuvius
is the only active volcano on the European mainland, while others as Mount Etna
Mount Etna
and Stromboli
Stromboli
are to be found on neighbouring islands. The region around Vesuvius including the Phlegraean Fields
Phlegraean Fields
Caldera west of Naples
Naples
are quite active[64] and constitute the most densely populated volcanic region in the world and eruptive event may occur within decades.[65] Vesuvius itself is regarded as quite dangerous due to a tendency towards explosive (Plinian) eruptions.[66] It is best known for its eruption in AD 79 that led to the burying and destruction of the Roman cities of Pompeii
Pompeii
and Herculaneum. The large experience of member states and regional authorities has led to exchange on the international level with cooperation of NGOs, states, regional and municipality authorities and private persons.[67] The Greek–Turkish earthquake diplomacy is a quite positive example of natural hazards leading to improved relations of traditional rivals in the region after earthquakes in İzmir
İzmir
and Athens
Athens
1999. The European Union Solidarity Fund (EUSF) was set up to respond to major natural disasters and express European solidarity to disaster-stricken regions within all of Europe.[68] The largest amount of fund requests in the EU is being directed to forest fires, followed by floodings and earthquakes. Forest fires are, whether man made or natural, an often recurring and dangerous hazard in the Mediterranean region.[67] Also, tsunamis are an often underestimated hazard in the region. For example, the 1908 Messina
Messina
earthquake and tsunami took more than 123,000 lives in Sicily
Sicily
and Calabria and is among the most deadly natural disasters in modern Europe. Biodiversity[edit] See also: List of fish of the Mediterranean Sea
Sea
and List of fish of the Black Sea Unlike the vast multidirectional Ocean
Ocean
currents in open Oceans within their respective Oceanic zones; biodiversity in the Mediterranean Sea is that of a stable one due to the subtle but strong locked nature of currents which affects favorably, even the smallest macroscopic type of Volcanic Life Form. The stable Marine ecosystem
Marine ecosystem
of the Mediterranean Sea
Sea
and sea temperature provides a nourishing environment for life in the deep sea to flourish while assuring a balanced Aquatic ecosystem
Aquatic ecosystem
excluded from any external deep oceanic factors. Invasive species[edit]

The reticulate whipray is one of the species that colonised the Eastern Mediterranean through the Suez Canal
Suez Canal
as part of the ongoing Lessepsian migration.

The opening of the Suez Canal
Suez Canal
in 1869 created the first salt-water passage between the Mediterranean and Red Sea. The Red Sea
Sea
is higher than the Eastern Mediterranean, so the canal serves as a tidal strait that pours Red Sea
Sea
water into the Mediterranean. The Bitter Lakes, which are hyper-saline natural lakes that form part of the canal, blocked the migration of Red Sea
Sea
species into the Mediterranean for many decades, but as the salinity of the lakes gradually equalised with that of the Red Sea, the barrier to migration was removed, and plants and animals from the Red Sea
Sea
have begun to colonise the Eastern Mediterranean. The Red Sea
Sea
is generally saltier and more nutrient-poor than the Atlantic, so the Red Sea
Sea
species have advantages over Atlantic species in the salty and nutrient-poor Eastern Mediterranean. Accordingly, Red Sea
Sea
species invade the Mediterranean biota, and not vice versa; this phenomenon is known as the Lessepsian migration (after Ferdinand de Lesseps, the French engineer) or Erythrean invasion. The construction of the Aswan High Dam
Aswan High Dam
across the Nile
Nile
River in the 1960s reduced the inflow of freshwater and nutrient-rich silt from the Nile
Nile
into the Eastern Mediterranean, making conditions there even more like the Red Sea
Sea
and worsening the impact of the invasive species. Invasive species
Invasive species
have become a major component of the Mediterranean ecosystem and have serious impacts on the Mediterranean ecology, endangering many local and endemic Mediterranean species. A first look at some groups of exotic species show that more than 70% of the non-indigenous decapods and about 63% of the exotic fishes occurring in the Mediterranean are of Indo Pacific origin,[69] introduced into the Mediterranean through the Suez Canal. This makes the Canal as the first pathway of arrival of "alien" species into the Mediterranean. The impacts of some lessepsian species have proven to be considerable mainly in the Levantine basin of the Mediterranean, where they are replacing native species and becoming a "familiar sight". According to the International Union for Conservation of Nature definition, as well as Convention on Biological Diversity
Convention on Biological Diversity
(CBD) and Ramsar Convention
Ramsar Convention
terminologies, they are alien species, as they are non-native (non-indigenous) to the Mediterranean Sea, and they are outside their normal area of distribution which is the Indo-Pacific region. When these species succeed in establishing populations in the Mediterranean Sea, compete with and begin to replace native species they are "Alien Invasive Species", as they are an agent of change and a threat to the native biodiversity. In the context of CBD, "introduction" refers to the movement by human agency, indirect or direct, of an alien species outside of its natural range (past or present). The Suez Canal, being an artificial (man made) canal, is a human agency. Lessepsian migrants are therefore "introduced" species (indirect, and unintentional). Whatever wording is chosen, they represent a threat to the native Mediterranean biodiversity, because they are non-indigenous to this sea. In recent years, the Egyptian government's announcement of its intentions to deepen and widen the canal have raised concerns from marine biologists, fearing that such an act will only worsen the invasion of Red Sea
Sea
species into the Mediterranean, facilitating the crossing of the canal for yet additional species.[70] Arrival of new tropical Atlantic species[edit] In recent decades, the arrival of exotic species from the tropical Atlantic has become a noticeable feature. Whether this reflects an expansion of the natural area of these species that now enter the Mediterranean through the Gibraltar
Gibraltar
strait, because of a warming trend of the water caused by global warming; or an extension of the maritime traffic; or is simply the result of a more intense scientific investigation, is still an open question. While not as intense as the "lessepsian" movement, the process may be scientific interest and may therefore warrant increased levels of monitoring.[citation needed] Sea-level rise[edit] By 2100 the overall level of the Mediterranean could rise between 3 to 61 cm (1.2 to 24.0 in) as a result of the effects of climate change.[71] This could have adverse effects on populations across the Mediterranean:

Rising sea levels will submerge parts of Malta. Rising sea levels will also mean rising salt water levels in Malta's groundwater supply and reduce the availability of drinking water.[72] A 30 cm (12 in) rise in sea level would flood 200 square kilometres (77 sq mi) of the Nile
Nile
Delta, displacing over 500,000 Egyptians.[73]

Coastal ecosystems also appear to be threatened by sea level rise, especially enclosed seas such as the Baltic, the Mediterranean and the Black Sea. These seas have only small and primarily east-west movement corridors, which may restrict northward displacement of organisms in these areas.[74] Sea
Sea
level rise for the next century (2100) could be between 30 cm (12 in) and 100 cm (39 in) and temperature shifts of a mere 0.05–0.1 °C in the deep sea are sufficient to induce significant changes in species richness and functional diversity.[75] Pollution[edit] Pollution in this region has been extremely high in recent years.[when?] The United Nations Environment Programme
United Nations Environment Programme
has estimated that 650,000,000 t (720,000,000 short tons) of sewage, 129,000 t (142,000 short tons) of mineral oil, 60,000 t (66,000 short tons) of mercury, 3,800 t (4,200 short tons) of lead and 36,000 t (40,000 short tons) of phosphates are dumped into the Mediterranean each year.[76] The Barcelona
Barcelona
Convention aims to 'reduce pollution in the Mediterranean Sea
Sea
and protect and improve the marine environment in the area, thereby contributing to its sustainable development.'[77] Many marine species have been almost wiped out because of the sea's pollution. One of them is the Mediterranean monk seal
Mediterranean monk seal
which is considered to be among the world's most endangered marine mammals.[78] The Mediterranean is also plagued by marine debris. A 1994 study of the seabed using trawl nets around the coasts of Spain, France
France
and Italy
Italy
reported a particularly high mean concentration of debris; an average of 1,935 items per km2. Plastic debris
Plastic debris
accounted for 76%, of which 94% was plastic bags.[79] Shipping[edit]

A cargo ship cruises towards the Strait
Strait
of Messina

Some of the world's busiest shipping routes are in the Mediterranean Sea. It is estimated that approximately 220,000 merchant vessels of more than 100 tonnes cross the Mediterranean Sea
Sea
each year—about one third of the world's total merchant shipping. These ships often carry hazardous cargo, which if lost would result in severe damage to the marine environment. The discharge of chemical tank washings and oily wastes also represent a significant source of marine pollution. The Mediterranean Sea constitutes 0.7% of the global water surface and yet receives 17% of global marine oil pollution. It is estimated that every year between 100,000 t (98,000 long tons) and 150,000 t (150,000 long tons) of crude oil are deliberately released into the sea from shipping activities. Approximately 370,000,000 t (360,000,000 long tons) of oil are transported annually in the Mediterranean Sea
Sea
(more than 20% of the world total), with around 250–300 oil tankers crossing the sea every day. Accidental oil spills happen frequently with an average of 10 spills per year. A major oil spill could occur at any time in any part of the Mediterranean.[75] Tourism[edit]

Antalya
Antalya
on the Turkish Riviera
Turkish Riviera
(Turquoise Coast) received more than 11 million international tourist arrivals in 2014.

The Mediterranean Sea
Sea
is arguably among the most culturally diverse block basin sea regions in the world, with a unique combination of pleasant climate, beautiful coastline, rich history and various cultures. The Mediterranean region is the most popular tourist destination in the world—attracting approximately one third of the world's international tourists.[citation needed] Tourism is one of the most important sources of income for many Mediterranean countries regardless of the man-made geopolitical conflicts that harbour coastal nations. In that regard, authorities around the Mediterranean have made it a point to extinguish rising man-made chaotic zones that would affect the economies, societies in neighboring coastal countries, let alone shipping routes. Naval and rescue components in the Mediterranean Sea
Sea
are considered one of the very best due to the quick intercooperation of various Naval Fleets within proximity of each other. Unlike the vast open Oceans, the closed nature of the Mediterranean Sea
Sea
provides a much more adaptable naval initiative among the coastal countries to provide effective naval and rescue missions, considered the safest and regardless of any man-made or natural disaster. Tourism also supports small communities in coastal areas and islands by providing alternative sources of income far from urban centers. However, tourism has also played major role in the degradation of the coastal and marine environment. Rapid development has been encouraged by Mediterranean governments to support the large numbers of tourists visiting the region each year. But this has caused serious disturbance to marine habitats such as erosion and pollution in many places along the Mediterranean coasts. Tourism often concentrates in areas of high natural wealth, causing a serious threat to the habitats of endangered Mediterranean species such as sea turtles and monk seals. Reductions in natural wealth may reduce incentives for tourists to visit.[75] See also: environmental impact of tourism Overfishing[edit] Main article: overfishing Fish stock levels in the Mediterranean Sea
Sea
are alarmingly low. The European Environment Agency says that more than 65% of all fish stocks in the region are outside safe biological limits and the United Nations Food and Agriculture Organisation, that some of the most important fisheries—such as albacore and bluefin tuna, hake, marlin, swordfish, red mullet and sea bream—are threatened.[date missing] There are clear indications that catch size and quality have declined, often dramatically, and in many areas larger and longer-lived species have disappeared entirely from commercial catches. Large open water fish like tuna have been a shared fisheries resource for thousands of years but the stocks are now dangerously low. In 1999, Greenpeace
Greenpeace
published a report revealing that the amount of bluefin tuna in the Mediterranean had decreased by over 80% in the previous 20 years and government scientists warn that without immediate action the stock will collapse. Aquaculture[edit]

Aquaculture
Aquaculture
in western Greece

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Aquaculture
Aquaculture
is expanding rapidly—often without proper environmental assessment—and currently accounts for 30% of the fish protein consumed worldwide. The industry claims that farmed seafood lessens the pressure on wild fish stocks, yet many of the farmed species are carnivorous, consuming up to five times their weight in wild fish. Mediterranean coastal areas are already over exposed to human influence, with pristine areas becoming ever scarcer. The aquaculture sector adds to this pressure, requiring areas of high water quality to set up farms. The installation of fish farms close to vulnerable and important habitats such as seagrass meadows is particularly concerning. Gallery[edit]

Beach of Hammamet, Tunisia

The beach of la Courtade in the Îles d'Hyères, France

Sardinia's south coast, Italy

Pretty Bay, Malta

Panoramic view of Piran, Slovenia

Panoramic view of Cavtat, Croatia

View of Neum, Bosnia and Herzegovina

A view of Sveti Stefan, Montenegro

Ksamil Islands, Albania

Navagio, Greece

Marmaris, Turquoise Coast, Turkey

Paphos, Cyprus

Burj Islam
Islam
Beach, Latakia, Syria

A view of Raouché
Raouché
off the coast of Beirut, Lebanon

A view of Haifa, Israel

Coast of Alexandria, view From Bibliotheca Alexandrina, Egypt

Old city of Ibiza
Ibiza
Town, Spain

Les Aiguades near Béjaïa, Algeria

El Jebha, a port town in Morocco

Europa Point, Gibraltar

Panoramic view of La Condamine, Monaco

Sunset at the Deir al-Balah
Deir al-Balah
beach, Gaza Strip

See also[edit]

Mediterranean portal

Babelmed, the site of the Mediterranean cultures Euro-Mediterranean Parliamentary Assembly Familial Mediterranean fever History
History
of the Mediterranean region Holy League (Mediterranean) List of islands in the Mediterranean List of Mediterranean countries Mediterranean Basin Mediterranean climate

Mediterranean diet Mediterranean forests, woodlands, and scrub Mediterranean Games Mediterranean race Mediterranean sea (oceanography) Piri Reis
Piri Reis
– Early cartographer of the Mediterranean Seto Inland Sea
Sea
– also known as the Japanese Mediterranean Sea Suez Canal Tyrrhenian Basin Union for the Mediterranean

Notes[edit]

References[edit]

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Climate: Monthly Weather Averages – Cyprus".  ^ Weather2Travel.com. " Tel Aviv
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salinity crisis" (PDF). Stratigraphy. 5 (3–4): 229.  ^ Garcia-Castellanos, D., Estrada, F., Jiménez-Munt, I., Gorini, C., Fernàndez, M., Vergés, J., De Vicente, R. (10 December 2009) Catastrophic flood of the Mediterranean after the Messinian
Messinian
salinity crisis, Nature 462, pp. 778–781, doi:10.1038/nature08555 ^ Elmer LaMoreaux, Philip (2001). "Geologic/Hydrogeologic Setting and Classification of Springs". Springs and Bottled Waters of the World: Ancient History, Source, Occurrence, Quality and Use. Springer. p. 57. ISBN 978-3-540-61841-6.  ^ Žumer, Jože (2004). "Odkritje podmorskih termalnih izvirov" [Discovery of submarine thermal springs] (PDF). Geografski obzornik (in Slovenian). Association of the Geographical Societies of Slovenia. 51 (2): 11–17. ISSN 0016-7274.  (in Slovene) ^ de la Vara, Alba; Topper, Robin P.M.; Meijer, Paul Th.; Kouwenhoven, Tanja J. (2015). "Water exchange through the Betic and Rifian corridors prior to the Messinian
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Salinity
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Crisis: A model study". Paleoceanography. 30 (5): 548–557. Bibcode:2015PalOc..30..548V. doi:10.1002/2014PA002719.  ^ Krijgsman, W.; Fortuinb, A. R.; Hilgenc, F. J.; Sierrod, F. J. (2001). " Astrochronology for the Messinian
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level variations during the Messinian
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Salinity
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Crisis : The Suez Rift Case". Geophysical Research Letters. 35 (2): L02401. Bibcode:2008GeoRL..35.2401G. doi:10.1029/2007gl032494.  ^ Govers, R. (2009). Choking the Mediterranean to dehydration: The Messinian salinity crisis
Messinian salinity crisis
Geology, 37 (2), 167–170 doi:10.1130/G25141A.1 Link Archived 10 January 2015 at the Wayback Machine. ^ Garcia-Castellanos, D., A. Villaseñor, 2011. Messinian
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salinity crisis regulated by competing tectonics and erosion at the Gibraltar Arc. Nature, 2011-12-15 pdf here Link ^ Agusti, J; Moya-Sola, S (1990). "Mammal extinctions in the Vallesian (Upper Miocene)". Lecture Notes in Earth
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Sciences. Lecture Notes in Earth
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Sciences. 30: 425–432. doi:10.1007/BFb0011163. ISBN 3-540-52605-6. ISSN 1613-2580.  (Abstract) ^ Politische Geographien Europas: Annäherungen an ein umstrittenes Konstrukt, Anke Strüver, LIT Verlag Münster, 2005, p.43 ^ FJ, Hilgen. Astronomical calibration of Gauss to Matuyama sapropels in the Mediterranean and implication for the Geomagnetic Polarity Time Scale, 104 (1991) 226–244 Earth
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(review) Brian M. Fagan, Journal of Interdisciplinary History, Volume 32, Number 3, Winter 2002, pp. 454–455 ^ Little Ice Ages: Ancient and Modern, Jean M. Grove, Taylor & Francis, 2004 ^ Christian Pfister (Hrsg.), Das 1950er Syndrom: Der Weg in die Konsumgesellschaft, Bern 1995 ^ The wave that destroyed Atlantis
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Southern Ocean

Amundsen Sea Bellingshausen Sea Cooperation Sea Cosmonauts Sea Davis Sea D'Urville Sea King Haakon VII Sea Lazarev Sea Mawson Sea Riiser-Larsen Sea Ross Sea Scotia Sea Somov Sea Weddell Sea

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