No one knows for sure. Some people believe that an asteroid earlier in time hit Earth and caused massive climate change that killed off reptiles, but spared dinosaurs. Others believe that it was simply climate change.
The Devonian Period occurred approximately 419-359 million years ago and is known as the "Age of Fishes" due to the diversification of fish species. It was also a time of significant plant evolution, with the first forests appearing. The period ended with a mass extinction event that affected marine life.
The period after the Devonian Period (416 to 359.2Ma) is the Carboniferous Period (359.2 to 299Ma).
The Phacops rana, a species of trilobite, became extinct during the end-Devonian mass extinction, which was likely caused by a combination of climate change, volcanic activity, and a drop in sea levels. These environmental changes likely disrupted the trilobite's habitats and food sources, leading to their extinction.
Devonian, Carboniferous and Permian Periods
Which mass extinction? There have been five such events. The first one, the Ordovician-Silurian extinction event occurred before the Devonian. The Late Devonian event occurred during the Devonian. All other mass extinctions occurred after the Devonian.
superstorm
They are the end-Ordovician extinction, end-Devonian extinction, end-Permian extinction, the Triassic extinction, end-Cretaceous extinction.
The primary hypothesis is that they were led to extinction by hunting by humans.
There were five major extinction events in the past. They are called the Cretaceous-Tertiary (or K-T) extinction event, the late Devonian mass extinction, the Permian mass extinction, the Ordovician-Silurian mass extinction and the Triassic-Jurassic mass extinction event.
Evidence leads most paleontologists to believe the Devonian mass extinction event to be caused by global cooling, triggered by a glaciation event on Godwana. A less-proven theory states the extinction could have also been caused by meteoric impact.Background Info:After the Ordovician mass extinction event around 440 - 450 million years ago, surviving groups of species continued to diversify evolutionarily into what became the Silurian and Devonian periods.The Devonian period spanned from 408-360 million years ago, in which came the first sharks, bony fish, and ammonoids (a type of predatory mollusk) in the ocean, as well as terrestrial amphibians, insects, and true land plants.
I have never known it to be called anything but "The Devonian", but one might speculate it could be called "The First Flowering", as the Devonian was when there was the first massive increase in sea creatures, as well as the first heavy vegetation on the surface of earth. The Devonian ended with a mass extinction event that is still not understood. There is some discussion of the "Alamo Impact Event" being connected with it, but most scientists believe that was too small, and too far before the mass extinction (3.5 million years) to have been the cause.
Dinosaur?
No one knows for sure. Some people believe that an asteroid earlier in time hit Earth and caused massive climate change that killed off reptiles, but spared dinosaurs. Others believe that it was simply climate change.
The Philippine eagle is not extinct, but it is critically endangered. A common hypothesis is that it is the destruction of habitat that is threatening this bird.
The Devonian Period occurred approximately 419-359 million years ago and is known as the "Age of Fishes" due to the diversification of fish species. It was also a time of significant plant evolution, with the first forests appearing. The period ended with a mass extinction event that affected marine life.
Placoderms appeared in the fossil register during the Silurian period, and all placoderms (including the nightmarish Dunkleosteus terrelli) went extinct on the Late Devonian extinction.On the Carboniferous period there were already no placoderm fishes in the oceans.This Paleozoic era extinction(s) is not yet fully understood.However, the extinction of many marine life families in the Devonian/Carboniferous mass extinction, during the Frasnian/Famennian stages and specially the Kellwasser event, was due to the widespread oceanic anoxia.Few other reliable paleontologic data is known.