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THE MEDITERRANEAN SEA
The Med was called "Mare Nostrum," or "Our Sea" when it was a Roman lake. The Med is the cradle of numerous major civilizations and empires. Like the Minoans, or the Seleucids, both of whom some of you have heard of maybe. This is where some of the best history is. Please, allow me to educate you a bit on the Med:
The Mediterranean Basin covers portions of three continents:
Europe,
Africa, and
Asia. It is distinct from the
drainage basin, which extends much further south and north due to major rivers ending in the Mediterranean Sea, such as the
Nile and
Rhône. Conversely, the Mediterranean Basin includes regions not in the drainage basin.
[1]
It has a varied and contrasting topography. The Mediterranean Region offers an ever-changing landscape of high mountains, rocky shores, impenetrable scrub, semi-arid steppes, coastal wetlands, sandy beaches and a myriad islands of various shapes and sizes dotted amidst the clear blue sea. Contrary to the classic sandy beach images portrayed in most tourist brochures, the Mediterranean is surprisingly hilly. Mountains can be seen from almost anywhere.
[2]
By definition, the Mediterranean Basin extends from
Macaronesia in the west, to the
Levant in the east, although some places may or may not be included depending on the view, as is the case with Macaronesia: some definitions only include
Madeira and the
Canary Islands[3] while others include the whole Macaronesia (with the
Azores and
Cape Verde).
[4]
In Western Asia, it covers the western and southern portions of the peninsula of Anatolia, as far as
Iraq,
[5] but excluding the temperate-climate mountains of central Turkey. It includes the Mediterranean
Levant at the eastern end of the Mediterranean, bounded on the east and south by the
Syrian and
Negev deserts.
The northern portion of the
Maghreb region of northwestern Africa has a Mediterranean climate, separated from the
Sahara Desert, which extends across
North Africa, by the
Atlas Mountains. In the eastern Mediterranean the Sahara extends to the southern shore of the Mediterranean, with the exception of the northern fringe of the peninsula of
Cyrenaica in
Libya, which has a dry Mediterranean climate.
Europe lies to the north of the Mediterranean. The European portion of the Mediterranean Basin loosely corresponds to
Southern Europe. The three large Southern European peninsulas, the
Iberian Peninsula,
Italian Peninsula, and the
Balkan Peninsula, extend into and comprise much of the Mediterranean-climate zone. A system of folded mountains, including the
Pyrenees dividing
Spain from
France, the
Alps dividing
Italy from
Central Europe, the
Dinaric Alps along the eastern
Adriatic, and the
Balkan and
Rila-
Rhodope mountains of the Balkan Peninsula divide the Mediterranean from the temperate climate regions of
Western,
Northwestern or
Northern Europe,
Central Europe, and
Eastern Europe.
Geology and paleoclimatology[edit]
The Mediterranean Basin was shaped by the ancient collision of the northward-moving African–Arabian continent with the stable Eurasian continent. As Africa–Arabia moved north, it closed the former
Tethys Sea, which formerly separated Eurasia from the ancient super continent of
Gondwana, of which Africa was part. At about the same time, 170 mya in the
Jurassic period, a small Neotethys ocean basin formed shortly before the Tethys Sea was closed at the eastern end. The collision pushed up a vast system of mountains, extending from the
Pyrenees in Spain to the
Zagros Mountains in
Iran. This episode of mountain building, known as the
Alpine orogeny, occurred mostly during the
Oligocene (34 to 23 million years ago (
mya)) and
Miocene (23 to 5.3 mya) epochs. The Neotethys became larger during these collisions and associated folding and subduction.
About 6 mya during the late Miocene, the Mediterranean was closed at its western end by drifting Africa, which caused the entire sea to evaporate. There followed several (debated) episodes of sea drawdown and re-flooding known as the
Messinian Salinity Crisis, which ended when the Atlantic last re-flooded the basin at the end of the Miocene.
[6] Recent research has suggested that a desiccation-flooding cycle may have repeated several times
[7][8] during the last 630,000 years of the Miocene epoch, which could explain several events of large amounts of salt deposition. Recent studies, however, show that repeated desiccation and re-flooding is unlikely from a
geodynamic point of view.
[9][10]
The end of the Miocene also marked a change in the Mediterranean Basin's climate. Fossil evidence shows that the Mediterranean Basin had a relatively humid subtropical climate with summer rainfall during the Miocene, which supported
laurel forests. The shift to a Mediterranean climate occurred within the last 3.2–2.8 million years, during the
Pliocene epoch, as summer rainfall decreased. The subtropical laurel forests retreated, although they persisted on the islands of
Macaronesia off the Atlantic coast of Iberia and North Africa, and 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.
Flora and fauna[edit]
See also:
Category:Environment of the Mediterranean
Phytogeographically, the Mediterranean Basin together with the nearby Atlantic coast, the
Mediterranean woodlands and forests and
Mediterranean dry woodlands and steppe of
North Africa, the
Black Sea coast of northeastern
Anatolia, the southern coast of
Crimea between
Sevastopol and
Feodosiya and the Black Sea coast between
Anapa and
Tuapse in
Russia forms the
Mediterranean Floristic Region, which belongs to the Tethyan Subkingdom of the
Boreal Kingdom and is enclosed between the
Circumboreal,
Irano-Turanian,
Saharo-Arabian and
Macaronesian floristic regions.
The Mediterranean Region was first proposed by German botanist
August Grisebach in the late 19th century.
The
monotypic Drosophyllaceae, recently segregated from
Droseraceae, is the only plant family
endemic to the region. Among the endemic plant genera are:[
dubious – discuss]
The genera
Aubrieta,
Sesamoides,
Cynara,
Dracunculus,
Arisarum and
Biarum are nearly endemic. Among the endemic species prominent in the Mediterranean vegetation are the
Aleppo pine,
stone pine,
Mediterranean cypress,
bay laurel,
Oriental sweetgum,
holm oak,
kermes oak,
strawberry tree,
Greek strawberry tree,
mastic,
terebinth,
common myrtle,
oleander,
Acanthus mollis and
Vitex agnus-castus. Moreover, many plant
taxa are shared with one of the four neighboring floristic regions only. According to different versions of
Armen Takhtajan's delineation, the Mediterranean Region is further subdivided into seven to nine
floristic provinces: Southwestern Mediterranean (or Southern Moroccan and Southwestern Mediterranean), Ibero-Balearian (or Iberian and Balearian), Liguro-Tyrrhenian, Adriatic,
East Mediterranean, South Mediterranean and Crimeo-Novorossiysk.
[11]
The Mediterranean Basin is the largest of the world's five
Mediterranean forests, woodlands, and scrub regions. It is home to a number of plant communities, which vary with rainfall, elevation, latitude, and soils.
- Scrublands occur in the driest areas, especially areas near the seacoast where wind and salt spray are frequent. Low, soft-leaved scrublands around the Mediterranean are known as garrigar in Catalan, garrigue in French, phrygana in Greek, tomillares in Spanish, and batha in Hebrew.
- Shrublands are dense thickets of evergreen sclerophyll shrubs and small trees, and are the most common plant community around the Mediterranean. Mediterranean shrublands are known as màquia in Catalan, macchia in Italian, maquis in French, and "matorral" in Spanish. In some places shrublands are the mature vegetation type, and in other places the result of degradation of former forest or woodland by logging or overgrazing, or disturbance by major fires.
- Savannas and grasslands occur around the Mediterranean, usually dominated by annual grasses.
- Woodlands are usually dominated by oak and pine, mixed with other sclerophyll and coniferous trees.
- Forests are distinct from woodlands in having a closed canopy, and occur in the areas of highest rainfall and in riparian zones along rivers and streams where they receive summer water. Mediterranean forests are generally composed of evergreen trees, predominantly oak and pine. At higher elevations Mediterranean forests transition to mixed broadleaf and tall conifer forests similar to temperate zone forests.
The Mediterranean Basin is home to considerable
biodiversity, including 22,500
endemic vascular plant species.
Conservation International designates the region as a
biodiversity hotspot, because of its rich biodiversity and its threatened status. The Mediterranean Basin has an area of 2,085,292 km2, of which only 98,009 km2 remains undisturbed.
Endangered
mammals of the Mediterranean Basin include the
Mediterranean monk seal, the
Barbary macaque, and the
Iberian lynx.
Ecoregions[edit]
The WWF identifies 22
Mediterranean forests, woodlands, and scrub ecoregions in the Mediterranean Basin, most of which featuring
sclerophyll plant species:
- Aegean and Western Turkey sclerophyllous and mixed forests (Greece, Turkey, North Macedonia, Bulgaria)
- Anatolian conifer and deciduous mixed forests (Turkey)
- Canary Islands dry woodlands and forests (Spain)
- Corsican montane broadleaf and mixed forests (France)
- Crete Mediterranean forests (Greece)
- Cyprus Mediterranean forests (Cyprus)
- Eastern Mediterranean conifer–sclerophyllous–broadleaf forests (Lebanon, Iraq, Israel, Jordan, Palestine, Syria, Turkey)
- Iberian conifer forests (Spain)
- Iberian sclerophyllous and semi-deciduous forests (Portugal, Spain)
- Illyrian deciduous forests (Albania, Bosnia and Herzegovina, Croatia, Greece, Italy, Montenegro, Slovenia)
- Italian sclerophyllous and semi-deciduous forests (France, Italy, San Marino)
- Mediterranean acacia–argania dry woodlands (Western Sahara, Morocco, Canary Islands (Spain))
- Mediterranean dry woodlands and steppe (Algeria, Egypt, Libya, Morocco, Tunisia)
- Mediterranean woodlands and forests (Algeria, Morocco, Tunisia)
- Northeastern Spain and Southern France Mediterranean forests (France, Monaco, Spain)
- Northwest Iberian montane forests (Portugal, Spain)
- Pindus Mountains mixed forests (Albania, Greece, North Macedonia)
- South Apennine mixed montane forests (Italy)
- Southeastern Iberian shrubs and woodlands (Spain)
- Southern Anatolian montane conifer and deciduous forests (Lebanon, Israel, Jordan, Syria, Turkey)
- Southwest Iberian Mediterranean sclerophyllous and mixed forests (Portugal, Spain)
- Tyrrhenian–Adriatic sclerophyllous and mixed forests (Croatia, France, Italy, Malta)
Map of the Mediterranean Basin's ecoregions.
1201: Aegean and Western Turkey sclerophyllous and mixed forests.
1202: Anatolian conifer and deciduous mixed forests.
1203: Canary Islands dry woodlands and forests.
1204: Corsican montane broadleaf and mixed forests.
1205: Crete Mediterranean forests.
1206: Cyprus Mediterranean forests.
1207: Eastern Mediterranean conifer-sclerophyllous-broadleaf forests.
1208: Iberian conifer forests.
1209: Iberian sclerophyllous and semi-deciduous forests.
1210: Illyrian deciduous forests.
1211: Italian sclerophyllous and semi-deciduous forests.
1212: Mediterranean acacia-argania dry woodlands and succulent thickets.
1213: Mediterranean dry woodlands and steppe.
1214: Mediterranean woodlands and forests.
1215: Northeastern Spain and Southern France Mediterranean forests.
1216: Northwest Iberian montane forests.
1217: Pindus Mountains mixed forests.
1218: South Apeninne mixed montane forests.
1219: Southeastern Iberian shrubs and woodlands.
1220: Southern Anatolian montane conifer and deciduous forests.
1221: Southwest Iberian Mediterranean sclerophyllous and mixed forests.
1222: Tyrrhenian-Adriatic sclerophyllous and mixed forests
.
History[edit]
Main article:
History of the Mediterranean region
Neanderthals inhabited western Asia and the non-glaciated portions of Europe starting about 230,000 years ago. Modern humans
moved into western Asia from Africa less than 100,000 years ago. Modern humans, known as
Cro-Magnons, moved into Europe approximately 50–40,000 years ago.
The most recent glacial period, the
Wisconsin glaciation, reached its
maximum extent approximately 21,000 years ago, and ended approximately 12,000 years ago. A warm period, known as the
Holocene climatic optimum, followed the ice age.
Food crops, including
wheat,
chickpeas, and
olives, along with
sheep and
goats, were
domesticated in the eastern Mediterranean in the
9th millennium BCE, which allowed for the
establishment of agricultural settlements. Near Eastern crops spread to southeastern Europe in the
7th millennium BCE.
Poppy and
oats were domesticated in Europe from the 6th to the 3rd millennium BCE. Agricultural settlements spread around the Mediterranean Basin.
Megaliths were constructed in Europe from 4500 – 1500 BCE.
A strengthening of the summer
monsoon 9000–7000 years ago increased rainfall across the
Sahara, which became a
grassland, with lakes, rivers, and wetlands. After a period of climatic instability, the Sahara settled into a desert state by the
4th millennium BCE.
Agriculture[edit]
Further information:
Mediterranean cuisine
Wheat is the dominant grain grown around the Mediterranean Basin.
Pulses and
vegetables are also grown. The characteristic tree crop is the
olive.
Figs are another important fruit tree, and
citrus, especially
lemons, are grown where irrigation is present.
Grapes are an important
vine crop, grown for fruit and to make
wine.
Rice and summer vegetables are grown in irrigated areas.
See also[edit]
Wikimedia Commons has media related to
Mediterranean.
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