38 relations: Albumares, Algae, Anfesta stankovskii, Animal, Bituminous limestone, Burgess Shale type preservation, Charnia, Charniodiscus, Ctenophora, Cyclomedusa, Dickinsonia, Doushantuo Formation, Echinoderm, Ediacaran, Ediacaran biota, Ediacaran type preservation, Ediacaria, Foraminifera, Fossil, Fossil embryo, Fractofusus misrai, Hiemalora, Incertae sedis, Kimberella, List of Ediacaran genera, Microbial mat, Palaeopascichnus, Parvancorina, Pteridinium, Rangea, Russia, Taphonomy, Tawuia, Trace fossil, Tribrachidium, Ural Mountains, White Sea, Yorgia.
Albumares brunsae is a tri-radially symmetrical fossil animal that lived in the late Ediacaran (Vendian) seafloor.
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Algae (or; singular alga) is an informal term for a large, diverse group of eukaryotes that are not necessarily closely related and are thus polyphyletic.
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Anfesta stankovskii is a tri-radially symmetrical fossil animal that lived in the late Ediacaran (Vendian) seafloor.
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Animals are multicellular, eukaryotic organisms of the kingdom Animalia (also called Metazoa).
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Bituminous limestone is limestone impregnated and sometimes deeply colored with bituminous matter derived from the decomposition of animal and plant remains entombed within the mass or in its vicinity.
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The Burgess Shale of British Columbia is famous for its exceptional preservation of mid-Cambrian organisms.
Charnia is the genus name given to a frond-like Ediacaran lifeform with segmented, leaf-like ridges branching alternately to the right and left from a zig-zag medial suture (thus exhibiting glide reflection, or opposite isometry).
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Charniodiscus is an Ediacaran fossil that in life was probably a stationary filter feeder that lived anchored to a sandy sea bed.
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Ctenophora (singular ctenophore, or; from the Greek κτείς kteis 'comb' and φέρω pherō 'carry'; commonly known as comb jellies) is a phylum of animals that live in marine waters worldwide.
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Cyclomedusa is a circular fossil of the Ediacaran biota; it has a circular bump in the middle and as many as five circular growth ridges around it.
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Dickinsonia is an iconic fossil of the Ediacaran biota.
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The Doushantuo Formation is a Lagerstätte in Guizhou Province, China that is notable for being one of the oldest beds to contain minutely preserved microfossils, phosphatic fossils that are so characteristic they have given their name to "Doushantuo type preservation".
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Echinoderm is the common name given to any member of the Phylum Echinodermata (from Ancient Greek, ἐχῖνος, echinos – "hedgehog" and δέρμα, derma – "skin") of marine animals.
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The Ediacaran Period, named after the Ediacara Hills of South Australia, is the last geological period of the Neoproterozoic Era and of the Proterozoic Eon, immediately preceding the Cambrian Period, the first period of the Paleozoic Era and of the Phanerozoic Eon.
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The Ediacaran (formerly Vendian) biota consisted of enigmatic tubular and frond-shaped, mostly sessile organisms that lived during the Ediacaran Period (ca. 635–542 Ma).
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Ediacaran type preservation relates to the dominant preservational mode in the Ediacaran period, where Ediacaran organisms were preserved as casts on the surface of microbial mats.
Ediacaria is a fossil genus dating to the Ediacaran Period of the Neoproterozoic Era.
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Foraminifera (Latin meaning hole bearers, informally called "forams") are members of a phylum or class of amoeboid protists characterized by streaming granular ectoplasm that among other things is used for catching food, and commonly by an external shell or "test" made of various materials and constructed in diverse forms.
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Fossils (from Classical Latin fossilis; literally, "obtained by digging") are the preserved remains or traces of animals, plants, and other organisms from the remote past.
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Fossil embryos are the preserved remains of organisms that have yet to hatch or be born.
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Fractofusus misrai is an Ediacaran fossil discovered in 1967 by S.B. Misra at Mistaken Point, Newfoundland and Labrador, Canada, which has since become the Mistaken Point Ecological Reserve.
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Hiemalora is a fossil of the Ediacaran biota, reaching around 3 cm in diameter, which superficially resembles a sea anemone.
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Incertae sedis (Latin for "of uncertain placement") is a term used for a taxonomic group where its broader relationships are unknown or undefined.
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Kimberella is a monospecific genus of bilaterian known only from rocks of the Ediacaran period.
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This is a list of all described Ediacaran genera, including the Ediacaran biota.
A microbial mat is a multi-layered sheet of microorganisms, mainly bacteria and archaea.
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Palaeopascichnus is a genus of Ediacaran organism comprising a series of lobes; it is plausibly a protozoan, but probably unrelated to the classical 'Ediacaran biota'.
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Parvancorina is a genus of shield-shaped bilaterally symmetrical fossil animal that lived in the late Ediacaran seafloor.
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Pteridinium is an erniettomorph found in a number of Precambrian deposits worldwide.
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Rangea is a frond-like Ediacaran fossil with six-fold radial symmetry.
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Russia (Ru-Россия.ogg), also officially known as the Russian Federation (a), is a country in northern Eurasia.
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Taphonomy is the study of decaying organisms over time and how they may become fossilized.
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Tawuia is a millimetric disc-shaped macrofossil from the Neoproterozoic.
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Trace fossils, also called ichnofossils (sg.; ιχνος ikhnos "trace, track"), are geological records of biological activity.
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Tribrachidium heraldicum is a tri-radially symmetrical fossil animal that lived in the late Ediacaran (Vendian) seas.
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The Ural Mountains (p; Урал тауҙары), or simply the Urals, are a mountain range that runs approximately from north to south through western Russia, from the coast of the Arctic Ocean to the Ural River and northwestern Kazakhstan.
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The White Sea (Белое море, Beloye more; Karelian and Vienanmeri, lit. Dvina Sea; Сэрако ямʼ, Serako yam) is a southern inlet of the Barents Sea located on the northwest coast of Russia.
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Yorgia waggoneri is a discoid Ediacaran, resembling a transition between the organisms Dickinsonia and Spriggina.
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