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Restoration of the Late Cretaceous duck-billed dinosaur Eotrachodon †Eotrachodon – type locality for genus †Eotrachodon orientalis – type locality for species †Epitonium †Epitonium sillimani †Eulima †Eulima gracilistylis †Eulima monmouthensis †Euspira †Eutrephoceras †Exogyra †Exogyra costata †Exogyra ponderosa ...
Sea turtle fossils are also commonly found in the Cretaceous rocks of Alabama and in 2018, a new species of Peritresius was named based on Alabama fossils. [11] Areas of Alabama not covered by seawater were home to subtropical forests. [1] Armored and duckbilled dinosaurs, like Lophorhothon [12] and Eotrachodon, [13] inhabited the state, as did ...
This is an accepted version of this page This is the latest accepted revision, reviewed on 3 March 2025. This is a dynamic list and may never be able to satisfy particular standards for completeness. You can help by adding missing items with reliable sources. The Last Judgment by painter Hans Memling. In Christian belief, the Last Judgement is an apocalyptic event where God makes a final ...
By Will Dunham. WASHINGTON (Reuters) - Dinosaurs long dominated Earth's land ecosystems with a multitude of forms including plant-eating giants like Argentinosaurus, meat-eating brutes like ...
While the dinosaurs met their end around 66 million years ago in a catastrophic way, their extinction may have been crucial to the development of the human race.
Scientists have identified a new giant horned dinosaur species that roamed across modern-day North Africa about 95 million years ago, despite its fossilised remains being destroyed during the ...
This list of the Paleozoic life of Alabama contains the various prehistoric life-forms whose fossilized remains have been reported from within the US state of Alabama and are between 538.8 and 252.17 million years of age.
The Wetumpka impact crater is the only confirmed impact crater in Alabama, United States.It is located east of downtown Wetumpka in Elmore County.The crater is 4.7 miles (7.6 km) in diameter, and its age is estimated to be about 85 million years (late Cretaceous), [1] based on fossils found in the youngest disturbed deposits, which belong to the Mooreville Chalk Formation.