North Atlantic Current eastward and becomes much broader and more diffuse. It then splits into a colder northeastern branch and a warmer eastern branch. As the warmer branch turns southward, most of the subtropical component of the Gulf Stream is diverted southward, and as a consequence, the North Atlantic is mostly supplied by subpolar waters, including a contribution from the Labrador Current recirculated into the NAC at 45°N. West of Continental Europe, it splits into two major branches. One branch goes southeast, becoming the Canary Current as it passes northwest Africa and turns southwest. The other major branch continues north along the coast
Atlantic Europe parts of Scandinavia and the Baltic), resulting in similar landscapes with common endemic plant and animal species. From a strictly physical point of view most of the Atlantic European shoreline can be considered a single biogeographical region. Physical geographers label this biogeographical area as the "European Atlantic Domain", part of the Euro-Siberian botanic region. The Atlantic Bronze Age is a cultural complex of the Bronze Age period of approximately 1300–700 BC, that marked the economic and cultural exchange between the current territories of Portugal, Spain, France, Great Britain and Ireland. Via the Bell Beaker culture, Atlantic and Central Europe were