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The Cambrian Explosion was a rapid diversification of life that occurred approximately 541 to 520 million years ago, during which most major animal groups (phyla) first appeared in the fossil record. This event marks a pivotal moment in Earth's history, when complex multicellular organisms with hard shells, exoskeletons, and sophisticated body plans evolved, including early arthropods like trilobites. Famous fossil sites such as the Burgess Shale in Canada and Chengjiang in China provide exceptional evidence of this dramatic evolutionary radiation. More Less
1698
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The first discovered Cambrian fossils were trilobites, described by Edward Lhuyd, the curator of the Oxford Museum, in 1698. At the time, their evolutionary importance was not understood.
Image source: Cambrian explosion
1784 - 1856
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Although their evolutionary importance was not known, on the basis of their old age William Buckland realized that a dramatic step-change in the fossil record had occurred around the base of what we now call the Cambrian.
1835
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Nineteenth-century geologists such as Adam Sedgwick and Roderick Murchison used fossils for dating rock strata, specifically for establishing the Cambrian and Silurian periods.
1859
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By 1859, leading geologists including Roderick Murchison were convinced that what was then called the lowest Silurian stratum showed the origin of life on Earth, though others, including Charles Lyell, differed.
2004
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In 2004, the start of the Cambrian was dated to 542 million years ago, providing a firm chronological anchor for the beginning of the explosive diversification of animal life.
Image source: Cambrian
2012
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In 2012, the date of the start of the Cambrian was revised from 542 Ma to 541 million years ago based on improved radiometric dating methods.
2022
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In 2022, the start of the Cambrian was changed again, this time to 538.8 million years ago, further refining the timeline of the explosive appearance of animal phyla.
1859
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Charles Darwin in his 1859 book On the Origin of Species discussed the then inexplicable lack of earlier fossils as one of the main difficulties for his theory of descent with slow modification through natural selection.
Image source: On the Origin of Species
1989
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Stephen Jay Gould's popular 1989 account of this work, Wonderful Life, brought the matter into the public eye and raised questions about what the Cambrian explosion represented.
Image source: Wonderful Life (book)
1996
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Budd (1996) regarded tardigrades as also being a stem group relative to the arthropods, illustrating that stem groups are relative concepts: tardigrades form a crown group in their own right while sitting on the arthropod stem lineage.
Image source: Crown group
1948
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In 1948, Preston Cloud argued that a period of 'eruptive' evolution occurred in the Early Cambrian, an early scientific recognition of the rapid diversification of life at the start of the period.
1970 - 1979
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As recently as the 1970s, despite Cloud's earlier argument, no sign was seen of how the relatively modern-looking organisms of the Middle and Late Cambrian arose from earlier forms.
2014
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New research done in 2014 using boron isotope analysis found that ocean alkalinity was rising until the Early Cambrian, shedding light on the chemical conditions of the oceans during the rise of animal life.
2019
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In 2019, a 'stunning' find of lagerstätten, known as the Qingjiang biota, was reported from the Danshui river in Hubei province, China, adding remarkably preserved Cambrian fossils to the record.
Image source: Qingjiang biota
2026
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New research done in 2026 analysing the coprolite record found it likely that a constant increase of available fecal matter in aggregate form starting in the Cambrian provided important nutrients to animal life and increased nutrients in deeper waters.
Image source: Coprolite
2026
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Research done in 2026 analysing digestive tract evolution through the Ediacaran and Cambrian examined how changes in gut anatomy may have influenced nutrient processing and ecosystem dynamics during the rise of animals.
Image source: Ediacaran
2026
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Studies completed in 2026 investigated the potential effects of digestive tract evolution on the biologic pump through the Ediacaran and Cambrian, finding that aggregated fecal matter transported nutrients into deeper waters, fueling marine ecosystems.
Image source: Biological pump
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