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- 6cb96c3b-1a1c-4d26-a894-2638d5cd05d1 definition "The Pliocene, 5.3 to 2.6 million years ago, was a time of global cooling after the warmer Miocene. The cooling and drying of the global environment may have contributed to the enormous spread of grasslands and savannas during this time. The change in vegetation undoubtedly was a major factor in the rise of long-legged grazers who came to live in these areas. Additionally, the Panamanian land-bridge between North and South America appeared during the Pliocene, allowing migrations of plants and animals into new habitats. Of even greater impact was the accumulation of ice at the poles, which would lead to the extinction of most species living there, as well as the advance of glaciers and ice ages of the Late Pliocene and the following Pleistocene." @default.
- 6cb96c3b-1a1c-4d26-a894-2638d5cd05d1 id "1648582" @default.
- 6cb96c3b-1a1c-4d26-a894-2638d5cd05d1 path_id a9f88ca9-5d19-45fa-8fbb-3c6ff5f1f190 @default.
- 6cb96c3b-1a1c-4d26-a894-2638d5cd05d1 path_id af145656-986a-4969-bb77-6e5b2cff1ede @default.
- 6cb96c3b-1a1c-4d26-a894-2638d5cd05d1 path_id db5be985-d8dc-4063-abff-4cbd8eb39653 @default.
- 6cb96c3b-1a1c-4d26-a894-2638d5cd05d1 path_id e5a3aed9-de46-4903-a999-f9f8bcdf1cd7 @default.
- 6cb96c3b-1a1c-4d26-a894-2638d5cd05d1 path_label "CENOZOIC" @default.
- 6cb96c3b-1a1c-4d26-a894-2638d5cd05d1 path_label "Chronostratigraphic Units" @default.
- 6cb96c3b-1a1c-4d26-a894-2638d5cd05d1 path_label "NEOGENE" @default.
- 6cb96c3b-1a1c-4d26-a894-2638d5cd05d1 path_label "PHANEROZOIC" @default.
- 6cb96c3b-1a1c-4d26-a894-2638d5cd05d1 prefLabel "PLIOCENE" @default.
- 6cb96c3b-1a1c-4d26-a894-2638d5cd05d1 reference "International Commission on Stratigraphy (http://www.stratigraphy.org/)" @default.
- 6cb96c3b-1a1c-4d26-a894-2638d5cd05d1 tag "Chronostratigraphic Units" @default.