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1 окаменелые остатки организмов
Oil: body fossilsУниверсальный русско-английский словарь > окаменелые остатки организмов
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Body plan — A body plan, or bauplan, is essentially the blueprint for the way the body of an organism is laid out. An organism s symmetry,cite web | title = Up and down...or around and around? Body Symmetry in Animals | work = The Diversity of Living… … Wikipedia
Annelid — Temporal range: Early Ordovician–Recent[1] … Wikipedia
Dinosaur — For other uses, see Dinosaur (disambiguation). Dinosaurs Temporal range: Late Triassic–Late Cretaceous, 231.4–65.5 Ma … Wikipedia
Paleontology — Palaeontology redirects here. For the scientific journal, see Palaeontology (journal). Paleontology studies the entire history of life on Earth. Paleontology (pronounced /ˌpælɪɒnˈtɒlədʒi/; British: palaeontology; from Greek: παλαιός… … Wikipedia
Trace fossil — Chirotherium footprints in a Triassic sandstone … Wikipedia
Cambrian explosion — The Cambrian explosion or Cambrian radiation was the seemingly rapid appearance of most major groups of complex animals around Ma|530, as evidenced by the fossil record. [http://www.ucmp.berkeley.edu/cambrian/camb.html The Cambrian Period] ]… … Wikipedia
Australopithecus — /aw stray loh pith i keuhs, peuh thee keuhs, aw streuh /, n. an extinct genus of small brained,large toothed bipedal hominids that lived in Africa between one and four million years ago. Cf. australopithecine. [ < NL (1905), equiv. to austral(is) … Universalium
Temnospondyli — Temnospondyls Temporal range: Early Carboniferous Early Cretaceous, 330–120 Ma Possible descendant taxon Lissamphibia survives to present … Wikipedia
Ediacara biota — The Ediacara (IPAEng|ˌiːdɪˈækərə, formerly Vendian) biota are ancient lifeforms of the Ediacaran Period, which represent the earliest known complex multicellular organisms. They appeared soon after the Earth thawed from the Cryogenian period s… … Wikipedia
Odontogriphus — Temporal range: Burgess Shale … Wikipedia
Cambrian Period — Oldest time division of the Paleozoic Era. During the Cambrian, 543–490 million years ago, there were widespread seas and several scattered landmasses. The largest continent was Gondwana. The average climate was probably warmer than today, with… … Universalium