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  2. Fossil history of flowering plants - Wikipedia

    en.wikipedia.org/wiki/Fossil_history_of...

    The fossil history of flowering plants records the development of flowers and other distinctive structures of the angiosperms, now the dominant group of plants on land.The history is controversial as flowering plants appear in great diversity in the Cretaceous, with scanty and debatable records before that, creating a puzzle for evolutionary biologists that Charles Darwin named an "abominable ...

  3. Gunflint chert - Wikipedia

    en.wikipedia.org/wiki/Gunflint_Chert

    The Gunflint Iron Formation is a banded iron formation, composed predominantly of dense chert and slate layers interbedded with ankerite carbonate layers. The chert layers can be subdivided into black layers (containing organic material and pyrite), red layers (containing hematite), and green layers (containing siderite). [5]

  4. Timeline of plant evolution - Wikipedia

    en.wikipedia.org/wiki/Timeline_of_plant_evolution

    This oxygen liberated by cyanobacteria then oxidized dissolved iron in the oceans, the iron precipitated out of the sea water, and fell to the ocean floor to form sedimentary layers of oxidized iron called Banded Iron Formations (BIFs). These BIFs are part of the geological record of evidence for the evolutionary history of plants by ...

  5. Piacenzian - Wikipedia

    en.wikipedia.org/wiki/Piacenzian

    The find was made by Ethiopian student Chalachew Seyoum at a site called Ledi-Geraru between the Mille and Awash rivers, in Afar Regional State (near [ 14 ] [ 15 ] Based on geological evidence from the Afar region, the individual would have lived just after a major climate shift , during which forests and waterways were rapidly replaced by arid ...

  6. Neogene - Wikipedia

    en.wikipedia.org/wiki/Neogene

    The Neogene (/ ˈ n iː. ə dʒ iː n / NEE-ə-jeen, [6] [7]) is a geologic period and system that spans 20.45 million years from the end of the Paleogene Period 23.04 million years ago to the beginning of the present Quaternary Period 2.58 million years ago.

  7. Evolutionary history of plants - Wikipedia

    en.wikipedia.org/wiki/Evolutionary_history_of_plants

    The establishment of a land-based flora increased the rate of accumulation of oxygen in the atmosphere, as the land plants produced oxygen as a waste product. When this concentration rose above 13%, around 0.45 billion years ago, [26] wildfires became possible, evident from charcoal in the fossil record. [27]

  8. Category:Neogene plants - Wikipedia

    en.wikipedia.org/wiki/Category:Neogene_plants

    Category: Neogene plants. 4 languages. ... Prehistoric plants of the Neogene Period, during the Middle Cenozoic Era Subcategories. This category has the following 2 ...

  9. Ediacaran biota - Wikipedia

    en.wikipedia.org/wiki/Ediacaran_biota

    On the early Earth, reactive elements, such as iron and uranium, existed in a reduced form that would react with any free oxygen produced by photosynthesising organisms. Oxygen would not be able to build up in the atmosphere until all the iron had rusted (producing banded iron formations), and all the other reactive elements had been oxidised.