Red Sea goby and nape and there are 24–28 scales in lateral line. It grows to a maximum length of . The Red Sea goby was formerly endemic to the northern Red Sea but have invaded the Mediterranean Sea by Lessepsian migration through the Suez Canal, and is common in the Lake Bardawil and has been found off Israel and Lebanon. The species was described by Paul Chabanaud in 1933 from type specimens collected in Lake Timsah on the Suez Canal. The Red Sea goby can be found on sandy substrates in inshore, shallow waters where it feeds on harpacticoid copepods and nematodes,
Mediterranean Sea crisis, before being refilled by the Zanclean flood about 5.3 million years ago. It covers an approximate area of 2.5 million km (965,000 sq mi), but its connection to the Atlantic (the Strait of Gibraltar) is only wide. The Strait of Gibraltar is a narrow strait that connects the Atlantic Ocean to the Mediterranean Sea and separates Gibraltar and Spain in Europe from Morocco in Africa. In oceanography, it is sometimes called the "Eurafrican Mediterranean Sea" or the "European Mediterranean Sea" to distinguish it from mediterranean seas elsewhere. The Mediterranean Sea has an average depth of and the deepest recorded