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  2. Permineralization - Wikipedia

    en.wikipedia.org/wiki/Permineralization

    (Pyrite is iron sulfide.) As organic matter decays it releases sulfide which reacts with dissolved iron in the surrounding waters. Pyrite replaces carbonate shell material due to an undersaturation of carbonate in the surrounding waters. Some plants become pyritized when they are in a clay terrain, but to a lesser extent than in a marine ...

  3. Pyrite - Wikipedia

    en.wikipedia.org/wiki/Pyrite

    Pyrite is used with flintstone and a form of tinder made of stringybark by the Kaurna people of South Australia, as a traditional method of starting fires. [17] Pyrite has been used since classical times to manufacture copperas (ferrous sulfate). Iron pyrite was heaped up and allowed to weather (an example of an early form of heap leaching ...

  4. Mineral evolution - Wikipedia

    en.wikipedia.org/wiki/Mineral_evolution

    Life has made dramatic changes in the environment. Most dramatic was the Great Oxygenation Event, about 2.4 billion years ago, in which photosynthetic organisms flooded the atmosphere with oxygen. Living organisms also catalyze reactions, creating minerals such as aragonite that are not in equilibrium with their surroundings.

  5. Paleoclimatology - Wikipedia

    en.wikipedia.org/wiki/Paleoclimatology

    An influence of life has to be taken into account rather soon in the history of the atmosphere because hints of early life forms have been dated to as early as 3.5 to 4.3 billion years ago. [21] The fact that it is not perfectly in line with the 30% lower solar radiance (compared to today) of the early Sun has been described as the " faint ...

  6. Annual vs. perennial plant evolution - Wikipedia

    en.wikipedia.org/wiki/Annual_vs._perennial_plant...

    Above the species level, plant lineages clearly vary in their tendency for annuality or perenniality (e.g., wheat vs. oaks). On a microevolutionary timescale, a single plant species may show different annual or perennial ecotypes (e.g., adapted to dry or tropical range), as in the case of the wild progenitor of rice (Oryza rufipogon).

  7. Raunkiær plant life-form - Wikipedia

    en.wikipedia.org/wiki/Raunkiær_plant_life-form

    Life forms: (1) Phanerophyte, (2; 3) Chamaephyte, (4) Hemicryptophyte, (5; 6) Geophyte, (7) Helophyte, (8; 9) Hydrophyte. Therophyte and epiphyte are not shown. The Raunkiær system is a system for categorizing plants using life-form categories, devised by Danish botanist Christen C. Raunkiær and later extended by various authors.

  8. Pressure oxidation - Wikipedia

    en.wikipedia.org/wiki/Pressure_oxidation

    An example of a mine utilizing this technology is the Pueblo Viejo mine in the Dominican Republic. At Pueblo Viejo, the process is performed by injecting high-purity oxygen into autoclaves operating at 230 degrees C and 40 bar of pressure. The resulting chemical reactions oxides the sulfide minerals the gold is trapped within. [3]

  9. Pyrophyte - Wikipedia

    en.wikipedia.org/wiki/Pyrophyte

    The passage of fire, by increasing temperature and releasing smoke, is necessary to raise seeds dormancy of pyrophile plants such as Cistus and Byblis an Australian passive carnivorous plant. Imperata cylindrica is a plant of Papua New Guinea. Even green, it ignites easily and causes fires on the hills.