Chlorosis Egyptian

Chlorosis egyptica, or “Dolian soil,” is one of the oldest marine aquatic organisms. This is a typical seashore plant with characteristic features. It grows on sandy or small shell rocks at a speed of 4-6 cm per year and up to 20-30 cm per season. Distributed in the eastern part of the Mediterranean, as well as in the western part of the Black Sea, starting from Turkey (Sea of ​​Marmara), and in the Atlantic Ocean near France. Known from Egypt, the Levant, the Kerch Strait and is widespread in Ukraine. Traces of it are allowed in the south of Russia. In Ukraine, its most characteristic are the brackish soils of the Crimean coast, in Russia - the Novorossiysk region, the coast of the North Caucasus. It is often observed on the shores and islands of the Black, Azov, and Caspian seas, but is more often found in saline bays, lagoons, and shallow reservoirs near Ilya. In the northern part of the development area it reaches the mouth of the Danube. Like many other marine plants, in the Black Sea basin it begins its development from a very early age. From seed to the appearance of twigs from the water, sea grass forms in 9-12 months, sometimes faster. Temperatures above 5 °C are required for mass development. The population of the colony is formed even faster. On the Black Sea coast, its habitat is one of the most numerous green seaweeds in the world. It is distributed throughout the Black Sea basin. The lowest water quality is observed in the northwestern part and in narrow, sparse areas of the central part. The maximum development of the sea is noted in the Odessa Bay, where conditions for plant growth are very good. If we compare marine and Egyptian chlorosis with its marine relatives the cockerel and scallop, then one cannot help but pay attention to their specific external differences. So, representatives of the genus enteromorphidae differ from seaweed and scallops in the absence of ridges on the leaves. This species belongs