Grasslands spread worldwide and modern ecosystems took shape. The Isthmus of Panama formed and hominin ancestors emerged in Africa.
Explore the Neogene Earth in 3D →African fossils around 7–6 million years old, including Sahelanthropus, lie near the early history of the human lineage. Evidence for upright walking coexists with traits suited to climbing, and interpretations of the earliest fossils remain debated. Human evolution was a branching process, not a single moment when a modern-style walker appeared.
Around 5.5 million years ago, the Caspian basin, once part of the Paratethys, became separated from the Black Sea basin. Falling water levels are studied as a factor in severing connections between the basins. This was one stage in the Caspian’s formation: later rises reconnected it with the Black Sea.
Restricted Atlantic exchange left enormous salt deposits in the Mediterranean between 5.97 and 5.33 million years ago. Marine conditions returned around 5.33 million years ago; Sicilian erosion features support a rapid refilling flood. How far water levels fell, and exactly how refilling unfolded, remain debated.
Islands and shallow seas changed gradually; the final land bridge formed about 2.8 million years ago, connecting continents and restricting exchange between oceans. Relatives of horses and camels spread south; ground sloths and glyptodonts spread north. Some animals crossed before the land bridge was complete. At a separate historical date, the Panama Canal opened in 1914. Locks raise and lower ships to cross a lake; this did not restore the ancient seaway.
Northern Hemisphere glaciation intensified around 2.7–2.6 million years ago, within a longer cooling trend. Changes in Earth’s orbit and tilt paced repeated cold and warm intervals, with feedbacks from ice, oceans and greenhouse gases. The cycles later grew longer, shifting from roughly 41,000 to 100,000 years.