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 investigation, is still an open question. While not as intense as the "lessepsian" movement, the process may be scientific interest and may therefore warrant increased levels of monitoring. By 2100 the overall level of the Mediterranean could rise between as a result of the effects of climate change. This could have adverse effects on populations across the Mediterranean: Coastal ecosystems also appear to be threatened by sea level rise, especially enclosed seas such as the Baltic, the Mediterranean and the Black Sea. These seas have only small and primarily east-west movement corridors, which may restrict northward displacement of organisms in