Until the late 1950s, the Precambrian was not believed to have hosted multicellular organisms. However, with radiometric dating techniques, it has been found that fossils initially found in the Ediacara Hills in Southern Australia date back to the late Precambrian. These fossils are body impressions of organisms shaped like disks, fronds and some with ribbon patterns that were most likely tentacles.
These are the earliest multicellular organisms in Earth's history, despite the fact that unicellularity had been around for a long time before that. The requirements for multicellularity were embedded in the genes of some of these cells, specifically choanoflagellates. These are thought to be the precursors for all animals. They are highly related to sponges (Porifera), which are the simplest multicellular animals.
In order to understand the transition to multicellularity during the Precambrian, it is important to look at the requirements for multicellularity—both biological and environmental.
Precambrian
The Precambrian dates from the beginning of Earth's formation (4.6 billion years ago) to the beginning of the Cambrian Period, 539 million years ago. The Precambrian consists of the Hadean, Archaean and Proterozoic eons. Specifically, this article examines the Ediacaran, when the first multicellular bodies are believed to have arisen, as well as what caused the rise of multicellularity. This time period arose after the Snowball Earth of the mid Neoproterozoic. The "Snowball Earth" was a period of worldwide glaciation, which is believed to have served as a population bottleneck for the subsequent evolution of multicellular organisms.
Precambrian bodies
The Earth formed around 4.6 billion years ago, with unicellular life emerging somewhat later after the cessation of the Late Heavy Bombardment, a period of intense asteroid impacts possibly caused by migration of the gas giant planets to their current orbits, however multicellularity and bodies are a relatively recent event in Earth's history. Bodies first started appearing towards the end of the Precambrian Era, during the Ediacaran period. The fossils of the Ediacaran period were first found in Southern Australia in the Ediacara Hills, hence the name. However these fossils were initially thought to be part of the Cambrian and it wasn't until the late 1950s when Martin Glaessner identified the fossils as actually being from the Precambrian era. The fossils that were found date to about 600 million years ago and are found in a variety of morphologies.
Fossils of the Ediacaran
For more information, see Ediacaran biota.
The fossils found that date back to the Precambrian lack distinct structures since there were no skeletal forms during this period. Skeletons did not arise until the Cambrian Period when oxygen levels increased. This is because skeletons require collagen, which uses Vitamin C as a cofactor, which requires oxygen. For more information on the rise of oxygen see the section on oxygen. The majority of fossils from this Era come from either Mistaken Point on the East Coast of Canada or the Ediacara Hills in Southern Australia.
Most of the fossils are found as impressions of soft-bodied organisms in the shape of disks, ribbons or fronds. There are also trace fossils that provide evidence that some of these Precambrian organisms were most-likely worm-like creatures that were locomotive. Most of these fossils lack any recognizable heads, mouths or digestive organs, and are thought to have fed via absorptive mechanisms and symbiotic relationships with chemoautotrophs (Chemotroph), photoautotrophs (Phototroph) or osmoautotrophs. The ribbon-like fossils resemble tentacled organisms, and are thought to have fed by capturing prey. The frondose fossils resemble sea pens and other cnidarians. The trace fossils suggest that there were annelid type creatures, and the disk fossils resemble sponges. Despite these similarities, much of the identification is speculation since the fossils do not show very distinct structures. Other fossils do not resemble any known lineages.