Earth Before Humans

Imagine sea ice near the equator, glaciers grinding across continents, and sunlight reflected back into space by a planet turning white. During the Cryogenian Period, Earth entered at least two extraordinary glacial intervals. The evidence is strong that ice reached very low latitudes. Inside this episode: - Ice At An Unlikely Latitude - A Climate Feedback With Its Foot On The Accelerator - Two Long Freezes, Not One Frozen Afternoon - How A White Planet Could Thaw Sources include peer-reviewed

Pangaea did not appear when continents slid together like tidy puzzle pieces, and it did not break when one crack split the planet. It was assembled through a long sequence of collisions and dismantled through a long sequence of rifts. The supercontinent is a story of moving plates, vanished oceans, mountain belts, and climates transformed by geography. Inside this episode: - Reading Continents As Moving Pieces - Assembly By Closing Oceans - One Ocean, Enormous Distances - The Stress Of Staying

About two hundred fifty-two million years ago, ecosystems collapsed in oceans and on land with a severity unmatched by any later mass extinction. The event is called the Great Dying, but the name can hide its most important feature. This was not one instant of disappearance.Inside this episode: - Recognizing A Biological Boundary - A Volcanic Province Of Continental Scale - Warming Multiplies Problems - Oceans Losing Breath Sources include peer-reviewed Earth-science research, official

A forest seems like scenery until it does not exist. Before trees, riverbanks lacked deep root networks, soils were thinner, and tall canopies did not divide sunlight into layers. During the Devonian Period, plants assembled the first forests and began engineering continents in ways that reached from local streams to the global carbon cycle. Inside this episode: - Before A Forest - Gilboa And A Surprising Tree - Roots Become Geological Actors - Rivers With New Boundaries Sources include

Before shells, claws, and recognizable fish, ancient seafloors carried quilted bodies, branching fronds, disks, and tracks made by creatures that rarely resemble modern animals. The Ediacaran world is not a failed sketch of the Cambrian. It is its own interval of ecological experiments, known through fossils that preserve soft forms ordinary fossilization usually destroys. Inside this episode: - A World Recorded In Impressions - Shapes Without Easy Names - A Seafloor Covered By Living Mats - Clues

Sixty-six million years ago, an asteroid struck near the Yucatan and altered the course of life. Follow the evidence linking Chicxulub to the K-Pg extinction, the rapid collapse of a vast crater, the darkness and cooling that followed, and the ocean-drilling cores that record destruction and recovery.Inside this episode: - The iridium boundary and the search for an impact crater - How the Chicxulub peak ring formed - What happened during the first day - Darkness, cooling, food-web collapse, and

High in the Canadian Rockies, stone preserves an ocean community about 508 million years old. Explore how the Burgess Shale captured soft-bodied animals, what Charles Doolittle Walcott collected there, and why fossils such as Opabinia, Hallucigenia, and Anomalocaris transformed our picture of Cambrian life. Inside this episode: - The 1909 discovery in Yoho National Park - How rapid burial preserved soft anatomy - The unfamiliar animals of the Cambrian ocean - What the fossils reveal about food

For much of early Earth, the atmosphere contained almost no free oxygen. Follow the evidence for the Great Oxidation Event, when microbial photosynthesis and a changing balance of chemical sinks allowed oxygen to persist, reshaping rocks, climate, oceans, and the possibilities for later life. Inside this episode: - Earth before oxygen accumulated in the atmosphere - How oxygenic photosynthesis changed the planetary balance - Sulfur isotopes, red beds, iron formations, and other evidence - Why