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Archive 005 · Death005-003

K-Pg Boundary Layer

The K-Pg boundary is a thin layer of rock enriched in iridium, a metal rare in Earth's crust but common in asteroids. It records the impact that formed the Chicxulub crater and triggered a mass extinction about 66 million years ago, wiping out all non-bird dinosaurs and about three quarters of species on Earth.

The Human Archives artwork

Where the Boundary Was Found

Follow the documented locations

01 / Context

A Global Layer of Fallout

K–Pg boundary sections around the world can preserve an iridium anomaly and other impact indicators, including shocked minerals and spherules. The deposits vary by location; they are not one uniformly thin band with every marker present.

Together with the Chicxulub crater, the global evidence records a large asteroid impact about 66 million years ago. The boundary is not the whole catastrophe pressed into one line. It is a set of local sediments through which a global event can be correlated.

02 / Context

The Day After the Sky Fell

The layer is quiet rock, but impact models and deposits point to blast, seismic and ocean effects near the crater, ejecta travelling far beyond it, and atmospheric disruption that darkened and cooled the planet. Effects differed with distance and environment.

For living organisms, there was no single cinematic 'day after' shared everywhere. Food webs failed across months and years. Their world did not turn into ours; many lineages ended, others survived, and later evolution remained contingent.

03 / Context

From Catastrophe to Continuity

Birds were already a living dinosaur lineage before the impact; some survived while every non-avian dinosaur lineage disappeared. Mammals also predated the boundary and diversified afterward alongside many other survivors.

The extinction changed ecological opportunity, but it did not happen in order to make humans possible. Our existence depends on countless prior contingencies; 'prerequisite' becomes misleading when it turns dependence into destiny.

04 / Interpretation

Reflections on the Boundary

At some outcrops, a person can span the K–Pg boundary with a fingertip. Yet 'below' and 'above' do not mean that dinosaurs, ammonites, mammals, birds, and flowering plants line up neatly against every hand specimen. Preservation has gaps, sedimentation rates differ, and several surviving groups crossed the line.

The thinness is still startling. A brief interval can separate fossil assemblages whose difference took generations of death and survival to unfold. The layer is not the largest possible violence made flat; it is one material trace through which that planetary change becomes measurable.

Artifact Profile

Artifact ID
005-003
Discipline
geological
Medium
rock
Collection terms
mass-extinction · asteroid-impact · dinosaurs · iridium-layer · chicxulub

About the visual

Visual type
The Human Archives artwork
Authored caption
A thin boundary interval in layered rock, associated with ejecta from the Chicxulub impact and a global extinction in which non-avian dinosaurs disappeared while birds survived.

Sources and provenance

  1. Cretaceous–Paleogene boundary overview
  2. International Commission on Stratigraphy — Global Boundary Stratotype Sections and Points
  3. NASA Earth Observatory — Chicxulub impact evidence
  4. Alvarez et al. (1980), Science: Extraterrestrial Cause for the Cretaceous–Tertiary Extinction
  5. Smithsonian National Museum of Natural History: Extinction Over Time
  6. Alvarez et al. (1980), Science
Presentation version
734c7067b7d773bd
Recorded review
2026-08-30

Revision and release records are shown where available. This page does not imply every historical edit has a review record.

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