The Triassic–Jurassic extinction cleared ecological space for dinosaurs to become the dominant land animals of the Jurassic.
Subject: Evolution.
About 201 million years ago, massive volcanic eruptions disrupted climate and oceans as Pangea began to split. Many competitors vanished. Dinosaurs did not just survive the crisis; they inherited the world it left behind.
The Ordovician–Silurian extinction shows how climate change can reshape evolution by collapsing old ecosystems and opening space for new life.
Subject: Evolution.
About 444 million years ago, global cooling locked water in ice, sea levels fell, and shallow marine habitats vanished. Most life still lived in the oceans, so the damage was enormous. Yet after the collapse, life reorganized. Evolution did not stop; it changed direction.
The Permian-Triassic extinction was not just the end of many species. It was a planetary reset that destroyed the old synapsid-dominated world and opened the door for the archosaur line that would later give rise to dinosaurs.
Subject: Evolution.
In Earth history, two great extinctions stand out. The P-T event 252 million years ago caused by global warming, and the K-Pg even 66 million years ago caused by a meteor. The dinosaur world did not appear because its ancestors were “better.” It emerged because of the Great Dying.
Prokaryotes are nucleus-free cells that include both bacteria and archaea — the two lineages that split shortly after LUCA.
Subject: Evolution.
“Prokaryote” is a structural description, not a single evolutionary branch. After LUCA, life divided into bacteria and archaea, and these prokaryotic lineages dominated Earth for billions of years before complex eukaryotic life emerged.
The Cenozoic era starts with the K–Pg extinction 66 million years ago. That event marks the sudden end of the reign of dinosaurs and the rise of mammals and birds.
Subject: Evolution.
The Cenozoic Era begins with catastrophe, but its story is really one of opportunity. When the K–Pg extinction struck 66 million years ago, it ended the age of non-avian dinosaurs and shattered ecosystems across the planet. Yet from that loss, mammals diversified into forms large and small, birds spread into skies and habitats once shared with pterosaurs, and flowering plants and grasslands reshaped the land.
About 3 billion years ago, bacteria started experimenting with photosynthesis.
Subject: Bacteria Evolution.
By 3 billion years ago, bacteria were experimenting with photosynthesis. The complex water-splitting photosynthesis we see today likely only evolved once and is known as oxygenic. A simpler version called anoxygenic was beta-tested by many different bacteria first.
About 1.3 billion years ago, following the “Great Oxidation Event,” the bacterial world fractured into specialized lineages, creating the foundational “Ecological Cast” that still runs our planet and our bodies today.
Subject: Bacteria Evolution.
By 1.3 billion years ago, as Earth’s chemistry shifted, Bacteria split into major phyla like the hardy, spore-forming Firmicutes, the chemical-producing Actinobacteria, and the fiber-digesting Bacteroidota. This massive diversification filled every niche from deep-sea vents to the first soils, establishing the complex microbial networks that would eventually allow complex life to survive.
Shortly after LUCA, about 3.7 billion years ago, the first bacteria emerged.
Subject: Evolution.
About 3.7 billion years ago, but for sure after LUCA, the first bacteria emerged. While LUCA had the basic machinery to be alive, “True Bacteria” evolved specific structural and chemical “trademarks” that set them apart from LUCA and their cousins, the Archaea: peptidoglycan cell wall and ester-linked lipids.
The Mesozoic era starts with the end-Permian mass extinction 252 million years ago. Dinosaurs ruled over all, including us. It ends the reign of dinosaurs with the K–Pg extinction 66 million years ago.
Subject: Evolution.
The Mesozoic era starts with the end-Permian mass extinction 252 million years ago ending the reign of our synapsid ancestors. Within it, it includes the end-Triassic extinction 201 million years ago and the Toarcian environmental crisis 183 million years ago. The Mesozoic era ends the reign of dinosaurs with the K–Pg extinction 66 million years ago.
About 2 billion years ago, bacteria are added to cells and that group leads to eukaryotes. You are a walking chimera ecosystem made of an Archaea host and trillions of Bacterial power-plants.
Subject: Evolution.
By 2.4 billion years ago, bacteria are added to cells and within the archaea group and eukaryotes emerge. You are a walking ecosystem. A Chimera, a hybrid creature made of an Archaea host and trillions of Bacterial power-plants. Without that theft 2 billion years ago for the massive energy boost needed for muscle and brains, life would likely still be just a thin layer of slime on the ocean floor.