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The lower boundary of the Cambrian was originally held to represent the first appearance of complex life, represented by trilobites.
The recognition of small shelly fossils before the first trilobites, and Ediacara biota substantially earlier, led to calls for a more precisely defined base to the Cambrian period.
Although diverse life forms prospered in the oceans, the land is thought to have been comparatively barren—with nothing more complex than a microbial soil crust 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.
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The base of the Cambrian lies atop a complex assemblage of trace fossils known as the Treptichnus pedum assemblage.
The use of Treptichnus pedum, a reference ichnofossil to mark the lower boundary of the Cambrian, is difficult as the occurrence of very similar trace fossils belonging to the Treptichnids group are found well below the T.
For years, she's been fielding rumors that she's dated well-known artists that she's worked with.
sedimentary deposits, sites of exceptional preservation where "soft" parts of organisms are preserved as well as their more resistant shells.
As a result, our understanding of the Cambrian biology surpasses that of some later periods.
The rapid diversification of lifeforms in the Cambrian, known as the Cambrian explosion, produced the first representatives of all modern animal phyla.
Phylogenetic analysis has supported the view that during the Cambrian radiation, metazoa (animals) evolved monophyletically from a single common ancestor: flagellated colonial protists similar to modern choanoflagellates.
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The seas were relatively warm, and polar ice was absent for much of the period.