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  1. en.wikipedia.org › wiki › ArcheanArchean - Wikipedia

    The Archean Eon (IPA: / ɑːr ˈ k iː ə n / ar-KEE-ən, also spelled Archaean or Archæan), in older sources sometimes called the Archaeozoic, is the second of the four geologic eons of Earth's history, preceded by the Hadean Eon and followed by the Proterozoic.

  2. en.wikipedia.org › wiki › EoarcheanEoarchean - Wikipedia

    The Eoarchean (IPA: / ˌiːoʊ.ɑːrˈkiːən / EE-oh-ar-KEE-ən; also spelled Eoarchaean) is the first era of the Archean Eon of the geologic record. It spans 431 million years, from the end of the Hadean Eon 4031 Mya to the start of the Paleoarchean Era 3600 Mya.

  3. Archaik (ang. Archean, od gr. arche ‛na przedzie’), archeozoik (z gr. dzoe ‛życie’), azoik (z gr. ‛bez życia’) w sensie geochronologicznym: drugi najstarszy eon w dziejach Ziemi po hadeiku, trwający ok. półtora miliarda lat (od 4,0 do 2,5 mld lat temu). Archaik dzieli się na cztery ery: eoarchaik, paleoarchaik, mezoarchaik i neoarchaik.

  4. 15 paź 2024 · Archean Eon, interval lasting from about 4.0 billion to 2.5 billion years ago, the first formal division of Precambrian time. Fossil evidence of the earliest primitive life-forms appears in rocks about 3.5–3.7 billion years old; other evidence suggests that life may have emerged before 3.95 billion years ago.

  5. The Archean eon, which preceded the Proterozoic eon, spanned about 1.5 billion years and is subdivided into four eras: the Neoarchean (2.8 to 2.5 billion years ago), Mesoarchean (3.2 to 2.8 billion years ago), Paleoarchean (3.6 to 3.2 billion years ago), and Eoarchean (4 to 3.6 billion years ago).*

  6. 11 kwi 2024 · Life most likely started during the late Hadean or early Archean Eons. The earliest evidence of life are chemical signatures, microscopic filaments, and microbial mats. Carbon found in 4.1 billion year old zircon grains have a chemical signature suggesting an organic origin.

  7. Archean Eon, or Archaean Eon or Archeozoic Eon, Older of the two divisions of Precambrian time. The Archean begins with the formation of the Earth’s crust 4 billion years ago and extends to 2.5 billion years ago, up to the start of the Proterozoic Eon, the second division of the Precambrian Period.

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