System (period) Series Stage (age) Lower boundary, Ma
Ordovician Lower Tremadocian 485.4±1.9
Cambrian Furongian Stage 10 ~489.5
Jiangshanian Golden spike~494
Paibian Golden spike~497
Miaolingian Guzhangian Golden spike~500.5
Drumian Golden spike~504.5
Wuliuan Golden spike~509
Series 2 Stage 4 ~514
Stage 3 ~521
Terreneuvian Stage 2 ~529
Fortunian Golden spike538.8±0.2
Ediacaran older
Subdivisions and "golden spikes" according to IUGS as of September 2023[1]
The cambrian sea by zdenek burian 1951

The Cambrian is the first geological period (system in stratigraphy) of the Paleozoic era and the Phanerozoic eon, lasting from 538.8 ± 0.2 to 485.4 ± 1.9 million years ago (mya) and is succeeded by the Ordovician. Its subdivisions, and indeed its base, are somewhat in flux. The period was established by Adam Sedgwick, who named it after Cambria, the Latin name for Wales, where Britain's Cambrian rocks are best exposed.

Cambrian Period Trilobites

The Cambrian is unique in its unusually high proportion of lagerstätten. These are sites of exceptional preservation, where 'soft' parts of organisms are preserved as well as their more resistant shells. This means that our understanding of the Cambrian biology surpasses that of some later periods. The Cambrian period marked a profound change in life on Earth; prior to the Cambrian, living organisms on the whole were small, unicellular and simple. Complex, multicellular organisms gradually became more common in the millions of years immediately preceding the Cambrian, but it was not until this period that mineralised – hence readily fossilised – organisms became common.

The rapid diversification of lifeforms in the Cambrian, known as the Cambrian explosion, produced the first representatives of many modern phyla, representing the evolutionary stems of modern groups of species, such as the arthropods. While diverse life forms prospered in the oceans, the land was comparatively barren – with nothing more complex than a microbial soil crust and a few forms that apparently emerged to browse on the microbial materials. Most of the continents were probably dry and rocky due to a lack of vegetation. Shallow seas flanked the margins of several continents created during the breakup of the supercontinent Pannotia.


An undersea Cambrian landscape.

The seas were relatively warm, and polar ice was absent for much of the period. The United States Federal Geographic Data Committee uses a "barred capital C" character similar to the capital letter Ukrainian Ye ‹Є› to represent the Cambrian Period. The proper Unicode character is U+A792 Ꞓ latin capital letter c with bar.


The Cambrian is especially noted for having bizarre animals compared to today. Good examples are Hallucigenia, Anomalocaris, Wiwaxia, Marrella and Opabinia. This is the result of the Cambrian Explosion, where many body plans appeared at once.