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An investigation on plant species diversity in Colchic Province (Turkey)

An investigation on plant species diversity in Colchic Province (Turkey)

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Figure 1. East Black Sea and its locati<strong>on</strong> <strong>in</strong> <strong>Turkey</strong> (by Google Earth).<br />

<strong>Colchic</strong> Prov<strong>in</strong>ce, located <strong>on</strong> the eastern part of the River<br />

Melet <strong>in</strong> Eastern Black Sea regi<strong>on</strong> because of develop<strong>in</strong>g<br />

tourism sector <strong>in</strong> the regi<strong>on</strong>; hydroelectric projects,<br />

highway c<strong>on</strong>structi<strong>on</strong>, agricultural activities and the<br />

transhumance traditi<strong>on</strong>. The data obta<strong>in</strong>ed from the<br />

research area are thought to make a c<strong>on</strong>tributi<strong>on</strong> to the<br />

understand<strong>in</strong>g of the regi<strong>on</strong>al flora.<br />

General descripti<strong>on</strong> of the research area<br />

The research area starts from Ordu City and from the<br />

River Melet, which flows <strong>in</strong>to the Black Sea, and extends<br />

to Georgia, and to the prov<strong>in</strong>cial borders of Ardahan and<br />

Erzurum. The Black Sea is situated <strong>in</strong> the north of the<br />

research area and Tokat, Sivas, Erz<strong>in</strong>can, Bayburt and<br />

Erzurum Cities are located <strong>in</strong> the south. The area is<br />

located between 36°41’25’’ and 42°42’ 35’’ eastern<br />

meridians and between 39°50’23’’ and 41°31’28’’<br />

northern parallels (Figure 1).<br />

Deveci 821<br />

With<strong>in</strong> the regi<strong>on</strong>, great soil groups such as grey-brown<br />

podzolic soil, red-yellow podzolic, brown forest, n<strong>on</strong>calcareous<br />

brown soil, brown, high mounta<strong>in</strong>-meadow,<br />

alluvial and colluvial soils are widespread. Alluvial soils<br />

c<strong>on</strong>stitute 1.4% of the regi<strong>on</strong>al surface area, while<br />

Colluvial soils c<strong>on</strong>stitute 0.6%. The majority of the soils<br />

c<strong>on</strong>sist of great soil groups such as red-yellow podzolic,<br />

grey-brown podzolic, n<strong>on</strong>-calcareous brown forest, brown<br />

forest and high mounta<strong>in</strong>-meadow soils (KHGM, 2011).<br />

The surface area of the regi<strong>on</strong> is 3.62 milli<strong>on</strong> ha,<br />

represent<strong>in</strong>g 4.64% of that of <strong>Turkey</strong>. The land suitable<br />

for tillage farm<strong>in</strong>g <strong>in</strong> the regi<strong>on</strong> c<strong>on</strong>stitute 1.18% of the<br />

lands suitable for tillage farm<strong>in</strong>g throughout <strong>Turkey</strong>, and<br />

11.02% of the lands unsuitable for tillage farm<strong>in</strong>g. The<br />

high proporti<strong>on</strong> of VII class land <strong>in</strong>dicates that the regi<strong>on</strong><br />

generally has rugged terra<strong>in</strong>s. While I to IV class land<br />

represents 8.3% of the surface area of the regi<strong>on</strong>, that of<br />

VI and VII class lands is 86.1% and that of VIII class<br />

lands is 5.6%. The regi<strong>on</strong> is comprised of land unsuitable<br />

for tillage farm<strong>in</strong>g because of the general structure it has.

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