The Cambrian explosion
node
The interval in which almost all animal body plans that exist today first appear in the fossil record, together with mineralised skeletons, complex burrowing, eyes and predation. The word "explosion" is doing two jobs and only one of them is safe. As a description of the fossil record it is accurate: the change from the Ediacaran to the Cambrian assemblages is abrupt and it is worldwide. As a description of evolutionary history it is contested, because molecular clocks place the divergences of the major animal lineages substantially earlier, in the Ediacaran or the Cryogenian, implying a long cryptic history of small, unskeletonised, rarely preserved animals. Several developments could each make an existing lineage suddenly visible without any new lineage arising: biomineralisation, an increase in body size, the onset of deep burrowing, and the appearance of predators driving the evolution of hard parts. The base of the Cambrian is defined at Fortune Head in Newfoundland and dated on recent ICS charts at 538.8 ± 0.2 Ma, revised down from the 541 Ma figure cited widely through the 2010s.
A node is not a place. Drawing it on a map would assert something about the world that no stored fact supports.
Read in · 1
Evidence · 2
Timeline
No dated observations are stored for this object. Atlas shows what was observed and when — it does not infer a history.
Connections · 7
- The end-Ordovician mass extinctionprecedes
- Fortune Head GSSP, Newfoundlandconcerns
- Burgess Shale, Yoho National Parkconcerns
- Chengjiang fossil site, Yunnanconcerns
- Anomalocarisconcerns
- Konservat-Lagerstätte (exceptional preservation)concerns
- Molecular clock datingconcerns
Assembled narrative · 1
Assembled from 60 blocks · 2 evidence · 31 related
- Story
- The interval in which almost all animal body plans that exist today first appear in the fossil record, together with mineralised skeletons, complex burrowing, eyes and predation. The word "explosion" is doing two jobs and only one of them is safe. As a description of the fossil record it is accurate: the change from the Ediacaran to the Cambrian assemblages is abrupt and it is worldwide. As a description of evolutionary history it is contested, because molecular clocks place the divergences of the major animal lineages substantially earlier, in the Ediacaran or the Cryogenian, implying a long cryptic history of small, unskeletonised, rarely preserved animals. Several developments could each make an existing lineage suddenly visible without any new lineage arising: biomineralisation, an increase in body size, the onset of deep burrowing, and the appearance of predators driving the evolution of hard parts. The base of the Cambrian is defined at Fortune Head in Newfoundland and dated on recent ICS charts at 538.8 ± 0.2 Ma, revised down from the 541 Ma figure cited widely through the 2010s.
- Knowledge
- Molecular clock dating
- Fortune Head GSSP, Newfoundland
- Konservat-Lagerstätte (exceptional preservation)
- Burgess Shale, Yoho National Park
- Anomalocaris
- Chengjiang fossil site, Yunnan
- The Cambrian explosion
- The end-Ordovician mass extinction
- Connections
- Molecular clock dating
- Ediacara Hills, Flinders Ranges
- Fortune Head GSSP, Newfoundland
- Konservat-Lagerstätte (exceptional preservation)
- Burgess Shale, Yoho National Park
- Anomalocaris
- Chengjiang fossil site, Yunnan
- The Great Oxidation Event
- The end-Ordovician mass extinction
- Fortune Head GSSP, Newfoundland
- Burgess Shale, Yoho National Park
- Chengjiang fossil site, Yunnan
- Anomalocaris
- Konservat-Lagerstätte (exceptional preservation)
- Molecular clock dating
- The Cambrian explosion
- Mass extinction
- The Late Devonian crisis
- International Commission on Stratigraphy
- The Cambrian explosion
- Global Boundary Stratotype Section and Point
- The Cambrian explosion
- The numerical age of the Cambrian base is revised to 538.8 Ma
- The Cambrian explosion
- Konservat-Lagerstätte (exceptional preservation)
- The Cambrian explosion
- Walcott locates the Burgess Shale beds
- The Cambridge re-description of the Burgess fauna begins
- The Cambrian explosion
- Konservat-Lagerstätte (exceptional preservation)
- The Cambrian explosion
- Hou Xianguang finds the Chengjiang fauna
- The Cambrian explosion
- The Cambrian explosion
- The Cambridge re-description of the Burgess fauna begins
- The Cambrian explosion
- Burgess Shale, Yoho National Park
- Chengjiang fossil site, Yunnan
- The Cambrian explosion
- Hou Xianguang finds the Chengjiang fauna
- The Cambrian explosion
- LUCA — the last universal common ancestor
- Radiometric dating
- The Cambrian explosion
- LUCA is dated to about 4.2 Ga by phylogenomic analysis
- Evidence
- Supports the stage and period boundary ages used throughout this pack, including the Cambrian base at 538.8 ± 0.2 Ma on recent editions against 541.0 ± 1.0 Ma on earlier ones. V55 verification basis: this session had no network access to any source — WebFetch was egress-blocked and the WebSearch budget was exhausted — so the cited work was not retrieved and its pagination was not re-checked. No chart edition was opened, so the boundary figures are quoted from standing knowledge of the chart rather than read from it, and the edition in which the Cambrian base changed is not identified.
- Supports the narrative of Walcott's discovery and classification, the Whittington–Briggs–Conway Morris re-description, and the reassembly of Anomalocaris from three separately named fossils. Gould's own thesis about disparity and contingency is a contested interpretation and is not asserted as fact in this pack. V55 verification basis: this session had no network access to any source — WebFetch was egress-blocked and the WebSearch budget was exhausted — so the cited work was not retrieved and its pagination was not re-checked.
Observed changes · 0
No public Signals are attached to this object. Signals show what changed and when it was observed — never a direction or a rank.
Actions
/atlas?object=EVENT_CAMBRIAN_EXPLOSION&experience=EVENT_CAMBRIAN_EXPLOSION