The geographical distribution of animals, with a study of the relations ...

The geographical distribution of animals, with a study of the relations ... The geographical distribution of animals, with a study of the relations ...

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200 ZOOLOGICAL GEOGRAPHY. [part in.mountainous, and much of their surface considerably elevated.Further east we have all European Turkey and Greece, amountain region with a comparatively small extent of levelplain. Id Asia the whole country, from Smyrna throughArmenia and Persia to the further borders of ,Affghanistan, is avast mountainous plateau, almost all above 2000, and extensivedistricts above 5000 feet in elevation. The only large tract oflow-land is the valley of the Euphrates. There is also somelow-land south of the Caucasus, and in Syria the valley of theJordan. In North Africa the valley of the Nile and the coastplains of Tripoli and Algiers are almost the only exceptions tothe more or less mountainous and plateau-like character of thecountry. Much of this extensive area is now bare and arid,and often even of a desert character ; a fact no doubt due, ingreat part, to the destruction of aboriginal forests. This lossis rendered permanent by the absence of irrigation, and, it isalso thought, by the abundance of camels and goats, animalswhich are exceedingly injurious to woody vegetation, and areable to keep down the natural growth of forests. Mr. Marshwhose valuable work Man and Nature gives much informationon this subject) believes that even large portions of the Africanand Asiatic deserts would become covered with woods, and theclimate thereby greatly improved, were they protected fromthese destructive domestic animals, which are probably notindigenous to the country. Spain, in proportion to its extent,is very barren ;Italy and European Turkey are more woody andluxuriant ; but it is perhaps in Asia Minor, on the range of theTaurus, along the shores of the Black Sea, and to the south ofthe Caucasus range, that this sub-region attains its maximum ofluxuriance in vegetation and in animal life. From the Caspianeastward extends a region of arid plains and barren deserts,diversified by a few more fertile valleys, in which the characteristicflora and fauna of this portion of the Palsearctic regionabounds. Further east we come to the forests of the HindooKoosh, which probably form the limit of the sub-region.Beyond these we enter on the Siberian sub-region to the north,and on the outlying portion of the Oriental region on the south.

chai\ x.] THE PAL^IARCTIC REGION. 201In addition to the territories now indicated as forming partof the Mediterranean sub-region, we must add the group ofCanary Islands off the west coast of Africa which seem to bean extension of the Atlas mountains, and the oceanic groups ofMadeira and the Azores ; the latter about 1,000 miles from thecontinent of Europe, yet still unmistakably allied to it both intheir vegetable and animal productions. The peculiarities of thefaunas of these islands will be subsequently referred to.It seems at first sight very extraordinary, that so large andwide a sea as the Mediterranean should not separate distinctfaimas, and this is the more remarkable when we find how verydeep the Mediterranean is, and therefore how ancient we maywell suppose it to be. Its eastern portion reaches a depth of2,100 fathoms or 12,600 feet, while its western basin is about1,600 fathoms or 9,600 feet in greatest depth, and a considerablearea of both basins is more than 1,000 fathoms deep. But afurther examination shows, that a comparatively shallow sea orsubmerged bank incloses Malta and Sicily, and that on theopposite coast a similar bank stretches out from the coast ofTripolileaving a narrow channel the greatest depth of which is240 fathoms. Here therefore is a broad plateau, which anelevation of about 1,500 feetof land connecting Italy with Africa ;would alsowould convert into a wide extentwhile the same elevationconnect Morocco with Spain, leaving two extensivelakes to represent what is now the Mediterranean Sea, and affordingfree communication for laud animals between Europe andNorth Africa. That such a state of things existed at a comparativelyrecent period, is almost certain ; not only because aconsiderable number of identical species of mammalia inhabit theopposite shores of the Mediterranean, but also because numerousremains of three species of elephants have been found in cavesin Malta,—now a small rocky island in which it would be impossiblefor such animals to live even if they could reach it.Remains of hippopotami are also found atGibraltar, and manyother animals of African types in Greece ; all indicating meansof communication between South Europe and North Africa whichno longer exist. (See Chapter VI. pp. 113—115.)Vol. I.—15

chai\ x.] THE PAL^IARCTIC REGION. 201In addition to <strong>the</strong> territories now indicated as forming part<strong>of</strong> <strong>the</strong> Mediterranean sub-region, we must add <strong>the</strong> group <strong>of</strong>Canary Islands <strong>of</strong>f <strong>the</strong> west coast <strong>of</strong> Africa which seem to bean extension <strong>of</strong> <strong>the</strong> Atlas mountains, and <strong>the</strong> oceanic groups <strong>of</strong>Madeira and <strong>the</strong> Azores ; <strong>the</strong> latter about 1,000 miles from <strong>the</strong>continent <strong>of</strong> Europe, yet still unmistakably allied to it both in<strong>the</strong>ir vegetable and animal productions. <strong>The</strong> peculiarities <strong>of</strong> <strong>the</strong>faunas <strong>of</strong> <strong>the</strong>se islands will be subsequently referred to.It seems at first sight very extraordinary, that so large andwide a sea as <strong>the</strong> Mediterranean should not separate distinctfaimas, and this is <strong>the</strong> more remarkable when we find how verydeep <strong>the</strong> Mediterranean is, and <strong>the</strong>refore how ancient we maywell suppose it to be. Its eastern portion reaches a depth <strong>of</strong>2,100 fathoms or 12,600 feet, while its western basin is about1,600 fathoms or 9,600 feet in greatest depth, and a considerablearea <strong>of</strong> both basins is more than 1,000 fathoms deep. But afur<strong>the</strong>r examination shows, that a comparatively shallow sea orsubmerged bank incloses Malta and Sicily, and that on <strong>the</strong>opposite coast a similar bank stretches out from <strong>the</strong> coast <strong>of</strong>Tripolileaving a narrow channel <strong>the</strong> greatest depth <strong>of</strong> which is240 fathoms. Here <strong>the</strong>refore is a broad plateau, which anelevation <strong>of</strong> about 1,500 feet<strong>of</strong> land connecting Italy <strong>with</strong> Africa ;would alsowould convert into a wide extentwhile <strong>the</strong> same elevationconnect Morocco <strong>with</strong> Spain, leaving two extensivelakes to represent what is now <strong>the</strong> Mediterranean Sea, and affordingfree communication for laud <strong>animals</strong> between Europe andNorth Africa. That such a state <strong>of</strong> things existed at a comparativelyrecent period, is almost certain ; not only because aconsiderable number <strong>of</strong> identical species <strong>of</strong> mammalia inhabit <strong>the</strong>opposite shores <strong>of</strong> <strong>the</strong> Mediterranean, but also because numerousremains <strong>of</strong> three species <strong>of</strong> elephants have been found in cavesin Malta,—now a small rocky island in which it would be impossiblefor such <strong>animals</strong> to live even if <strong>the</strong>y could reach it.Remains <strong>of</strong> hippopotami are also found atGibraltar, and manyo<strong>the</strong>r <strong>animals</strong> <strong>of</strong> African types in Greece ; all indicating means<strong>of</strong> communication between South Europe and North Africa whichno longer exist. (See Chapter VI. pp. 113—115.)Vol. I.—15

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