Isthmus of Panama
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The Isthmus of Panama (sometimes known as the Isthmus of Darien), a narrow strip of land connecting the continents of North and South America. The Isthmas in crossed by the Panama Canal and forms the nation of Panamá.
Twenty million years ago ocean covered the area where Panama is today. There was a gap between the continents of North and South America through which the waters of the Atlantic and Pacific Oceans flowed freely. Beneath the surface, two plates of the Earth's crust were slowly colliding into one another, forcing the Pacific Plate to slide slowly under the Caribbean Plate. The pressure and heat caused by this collision led to the formation of underwater volcanoes, some of which grew tall enough to break the surface of the ocean and form islands as early as 15 million years ago. More and more volcanic islands filled in the area over the next several million years. Meanwhile, the movement of the two tectonic plates was also pushing up the sea floor, eventually forcing some areas above sea level.
Over time, massive amounts of sediment (sand, soil, and mud) were peeled away from North and South America by strong ocean currents and fed through the gaps between the newly forming islands. Little by little, over millions of years, the sediment deposits added to the islands until the gaps were completely filled. By about 3 million years ago, an isthmus had formed between North and South America. (An “isthmus” is a narrow strip of land, with water on either side, that connects two larger bodies of land.)
Scientists believe the formation of the Isthmus of Panama is one of the most important geologic events to happen on Earth in the last 60 million years. Even though it is only a tiny sliver of land, relative to the sizes of continents, the Isthmus of Panama had an enormous impact on Earth's climate and its environment. By shutting down the flow of water between the two oceans, the land bridge re-routed currents in both the Atlantic and Pacific Oceans. Atlantic currents were forced northward, and eventually settled into a new current pattern that we call the Gulf Stream today. With warm Caribbean waters flowing toward the northeast Atlantic, the climate of northwestern Europe grew warmer. (Winters there would be as much as 10 degrees C colder in winter without the transport of heat from the Gulf Stream.) The Atlantic, no longer mingling with the Pacific, also grew saltier. Each of these changes helped establish the global ocean circulation pattern we see today. In short, the Isthmus of Panama directly and indirectly influenced ocean and atmospheric circulation patterns, which regulated patterns of rainfall, which in turn sculpted landscapes.
The formation of the Isthmus of Panama also played a major role in biodiversity on our world. The bridge made it easier for animals and plants to migrate between the continents. For instance, in North America today, the opossum, armadillo, and porcupine all trace back to ancestors that came across the land bridge from South America. Likewise, the ancestors of bears, cats, dogs, horses, llamas, and raccoons all made the trek south across the isthmus.
The Isthmus includes nine ecoregions (See Ecoregions of Panama) has show here
Source: World Wildlife Fund
1. Mesoamerican Gulf-Caribbean mangroves (Bocas del Toro-San Bastimentos Island-San Blas mangroves)
2. Isthmian-Atlantic moist forests
3. Talamancan montane forests
4. Isthmian-Pacific moist forests
5. Southern Mesoamerican Pacific mangroves
6. Panamanian dry forests
7. South American Pacific mangroves
8. Eastern Panamanian montane forests
9. Chocó-Darién moist forests
The subtropical and tropical Mesoamerica Biodiversity Hotspot includes the northern two thirds of Panamá, from the border with Costa Rica to the Panama Canal. From the Panama Canal, the Tumbes-Chocó-Magdalena Biodiversity Hotspot extends south and east into the wet and moist forests of Panama's Darién Province. The hotspot includes a wide variety of habitats, ranging from mangroves, beaches, rocky shorelines, and coastal wilderness.