Last Day of the Dinosaurs 2010

Bill Mondy narrates a sweeping, globe-spanning account of life at the very end of the Cretaceous, where a cascade of dramatic events reshapes ecosystems across continents. The tale begins in the Pacific Northwest, during the Maastrichtian, where a Quetzalcoatlus suddenly spots an unguarded T. rex nest and sinks its beak into the vulnerable young. The father T. rex, drawn by a powerful olfactory cue, charges back to defend the nest, his acute sense of smell snapping him toward danger. The enormous winged predator’s flight becomes a liability in the forest, and a fierce confrontation results in the T. rex injuring the Quetzalcoatlus by biting its foot. The encounter continues as the Quetzalcoatlus pecks at the T. rex’s eye and finally manages to break free, escaping into the trees, though only one hatchling survives the brutal clash.

Across the plains, two adult T. rex units stumble upon a mating dispute between two Triceratops and decide to intervene. By coordinating their efforts, the tyrant kings bring down the defeated adversary and claim the carcass for themselves, illustrating a stark, carnivorous alliance born of need in a world where food is scarce and danger is constant.

Meanwhile, a herd of Alamosaurus surveys the Mexican plains in search of sustenance. A female lays a clutch of eggs as a distant catastrophe begins to unfold: a nearby asteroid impact erupts into the sky, sending heat-hazed air surging across the landscape while fiery debris rains down. The planet shudders with a magnitude 11 earthquake, and a colossal blast finishes the job on the dying herd. Still, not all life is extinguished—some eggs remain buried beneath the soil, quietly surviving the catastrophe until conditions may permit a new start.

In Mongolia, a herd of Charonosaurus holds a lifeline at a watering hole, where females guard their eggs. The tension intensifies when a Saurornithoides steals an egg, prompting a confrontation with the mother. A second Saurornithoides presses the chase, forcing the Charonosaurus to flee. The predators press the pursuit, and the mother is brought down in the ensuing struggle, underscoring the brutal cost of survival in these volatile times.

The asteroid’s ejecta cloud begins to form, and as it travels toward the Pacific Northwest, a remorseless earthquake rattles the region anew. A mated pair of Quetzalcoatlus attempt to lift off, but the debris shower rips holes in their wings, and their bid for escape fails. A pair of Triceratops manage to ascend into the mountains, only to be burned alive by the searing ejecta cloud as the world’s climate ignites and reddens.

The heat from the cloud ignites fires that race through forests, driving large dinosaurs—T. rex, a cluster of Triceratops, and an Ankylosaurus—into flight, while smaller creatures take shelter underground. The female Quetzalcoatlus glides away, a survivor who witnessed the fall of forests she once called home.

Forty-five minutes after impact, the ejecta cloud sweeps into Mongolia from the east, and temperatures spike by several degrees every second, eventually reaching 300 °F (150 °C). Three Charonosaurus and a pair of Saurornithoides seek shelter in a cave, hoping for a window of safety. After five hours, the heat subsides, and as the Saurornithoides emerge to feast on the corpse of a Charonosaurus, two surviving Charonosaurus return to the watering hole. The dramatic temperature shift also triggers a massive sandstorm. The Saurornithoides survive by using their prey as barriers, while the third Charonosaurus remains hidden in the cave. When the storm clears, the two surviving Charonosaurus head to water, only to be ambushed; one Saurornithoides attacks the Charonosaurus, and in a brutal scramble, the herbivore collapses, crushing its attacker and ending the fight. The remaining Saurornithoides copes with the loss by cannibalizing its companion.

Four days after the impact, food remains scarce across the planet. In the Pacific Northwest, four Triceratops move toward an island that seems untouched by the fires. A megatsunami rapidly recedes the sea, revealing a temporary bridge of land. Three Triceratops cross, while the last remaining female Quetzalcoatlus lands to drink and catch a stranded fish. Just as she finishes feeding, the 300-foot wave surges toward the shore, and the Quetzalcoatlus along with the three crossing Triceratops are drawn into the sea and drown.

Ten days in, the planet has thinned to a skeleton of its former life. In Mongolia, the Charonosaurus succumbs to hydrogen sulfide gas rising from the watering hole, and a Saurornithoides that moves in to scavenge the corpse is felled by the same toxic gas. The landscape remains a grey wasteland, and in the Pacific Northwest a final, grim trio—an Ankylosaurus, a Triceratops, and a T. rex—engage in a deadly confrontation that ends with their mutual demise, a stark reminder of the fragility of even the most formidable species.

Elsewhere, in Mexico, an Alamosaurus egg buried underground hatches, offering a faint glimmer of continuity. Yet the fragile lineage—crippled by inbreeding and disease—soon dwindles, leaving no stable population to endure.

The planet’s survivors include a vast array of life forms that sheltered underground or adapted to the new normal: insects and other arthropods, small reptiles, crocodilians, amphibians, fish, and birds that flew or swam away from the devastation. Mammals, equipped with adaptability and faster reproduction, retreated to burrows and proliferated, quietly preparing for the day life might be rebalanced. As the ejecta cloud finally clears and sunlight returns, plant life—especially ferns—begins a slow, steady resurgence. Over the ensuing 65 million years, mammals ascend to dominance, setting the stage for the eventual emergence of humans and the long arc of life that follows.