[1] Animals evidence is found as far as the Cryogenian period. 24-Isopropylcholestane (24-ipc) are foud in rocks form ~650 million years ago; only made by sponges and pelagophyte algae. Its likely origin is from sponges based on molecular clock estimates for the origin of 24-ipc production in both groups. Analyses of pelagophyte algae consistently recover a Phanerozoic origin, while analyses of sponges recover a Neoproterozoic origin, consistent with the appearance of 24-ipc in the fossil record.
First animals' body fossils appear in the Ediacaran, represented by forms like Charnia and Spriggina. It had long been doubted whether these fossils truly represented animals, but the discovery of the animal lipid cholesterol in fossils of Dickinsonia establishes their nature.[95] Animals are thought to have originated under low-oxygen conditions, suggesting that they were capable of living entirely by anaerobic respiration, but as they became specialised for aerobic metabolism they became fully dependent on oxygen in their environments.
[1] Many animal phyla first appear in the fossil record during the Cambrian explosion, starting about 539 million years ago, in beds such as the Burgess Shale. Extant phyla in these rocks cover molluscs, brachiopods, onychophorans, tardigrades, arthropods, echinoderms and hemichordates, along with numerous now-extinct forms such as the predatory Anomalocaris. The apparent suddenness of the event may however be an artefact of the fossil record, rather than showing that all these animals appeared simultaneously. That view is supported by the discovery of Auroralumina attenboroughii, the earliest known Ediacaran crown-group cnidarian (557–562 mya, some 20 million years before the Cambrian explosion) from Charnwood Forest, England. It is thought to be one of the earliest predators, catching small prey with its nematocysts as modern cnidarians do.
[1] Some palaeontologists suggest that animals lived much prior the Cambrian explosion. Early fossils that may be animals appear e.g. in the 665-million-year-old rocks of the Trezona Formation of South Australia, interpreted as maybe early sponges. Trace fossils like tracks and burrows found in the Tonian period (from 1 gya) may tell triploblastic worm-like animals' presence, as big (~5 mm wide) and complex as earthworms. But akin tracks are made by the giant single-celled protist Gromia sphaerica, so the Tonian trace fossils may not indicate early animal evolution.
Around the same time, layered microorganisms mats called stromatolites reduced in diversity, maybe due to grazing by newly evolved animals. Objects like sediment-filled tubes resembling trace fossils of wormlike animals' burrows were found in North America's 1.2 gya rocks, in 1.5 gya rocks in Australia and North America, and in 1.7 gya rocks in Australia. Their interpretation to have an animal origin is unsure, as they may be water-escape or other structures.