Gibralter has a tremendous flow of water through it from the Atlantic. but the obstacle is that the circulation of the North Atlantic brings mostly water from t

Gibralter has a tremendous flow of water through it from the Atlantic. but the obstacle is that the circulation of the North Atlantic brings mostly water from the North to feed that flow. The Suez Canal is a sea level canal, though, and feeds water from Indian Ocean via the Red Sea. The flow of water there is directly from Africa but not that far south, but there are mangroves in East Africa and in South Asia so that's not a deal breaker. Also, there is the matter of ship bilges being emptied, though I've no idea the current status of that type of transport of flora and fauna. here's an article I found about dispersal of floating seeds. apparently there are some obstacles due to them sinking mumble mumble salinity: https://insideclimatenews.org/news/19072022/mangrove-seeds-ocean-salinity-density/ https://insideclimatenews.org/news/19072022/mangrove-seeds-o... Most mangrove propagules don’t travel far. They drop straight under their parent tree or get trapped in the tangled roots of the surrounding mangrove forest and take root a few feet or miles away. But long distance dispersal across oceans and seas is still important, said Van der Stocken. If mangroves need to expand their range because of unsuitable environmental conditions from climate change or weather events, as in Texas, being able to spread their genetic material long distances on ocean currents becomes important, he said. Across the globe in the Atlantic and Eastern Pacific mangrove populations, including those along the Gulf of Mexico, reduced water density was less apparent in the study models. However, the model found these regions might develop saltier water than the Western Pacific. Even if propagules travel the same distance, increased salinity might affect their survival, which will have implications for the dispersal dynamics of mangroves in those regions.