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  2. Paleopedology - Wikipedia

    en.wikipedia.org/wiki/Paleopedology

    Remains of former soils can either be found under deposited sediment in unglaciated areas or in extremely steep cliffs where the old soil can be seen below the younger present-day soil. In cases where volcanoes have been active, some soil fossils occur under the volcanic ash .

  3. Paleopedological record - Wikipedia

    en.wikipedia.org/wiki/Paleopedological_record

    Soil fossils are usually classified by USDA soil taxonomy.With the exception of some exceedingly old soils which have a clayey, grey-green horizon that is quite unlike any present soil and clearly formed in the absence of O 2, most fossil soils can be classified into one of the twelve orders recognised by this system.

  4. Paleosol - Wikipedia

    en.wikipedia.org/wiki/Paleosol

    In soil science the definition differs slightly: paleosols are soils formed long ago that have no relationship in their chemical and physical characteristics to the present-day climate or vegetation. Such soils are found within extremely old continental cratons, or in small scattered locations in outliers of other ancient rock domains.

  5. List of fossil sites - Wikipedia

    en.wikipedia.org/wiki/List_of_fossil_sites

    This list of fossil sites is a worldwide list of localities known well for the presence of fossils. Some entries in this list are notable for a single, unique find, while others are notable for the large number of fossils found there.

  6. Fossil - Wikipedia

    en.wikipedia.org/wiki/Fossil

    Fossil collecting (sometimes, in a non-scientific sense, fossil hunting) is the collection of fossils for scientific study, hobby, or profit. Fossil collecting, as practiced by amateurs, is the predecessor of modern paleontology and many still collect fossils and study fossils as amateurs.

  7. Calico Early Man Site - Wikipedia

    en.wikipedia.org/wiki/Calico_Early_Man_Site

    Material recovered from nested Pleistocene alluvial deposits stratigraphically beneath a 100,000-year-old soil profile: a 'rock ring' (not a fire hearth) dated to 135,000 years by thermoluminescence (TL), about 200,000 years by uranium-series analysis, and about 197,000+/- 20,000 years by surface beryllium-10 (10 Be) dating.

  8. Yorktown Formation - Wikipedia

    en.wikipedia.org/wiki/Yorktown_Formation

    Hazel (1971) revised the age of the Yorktown from Miocene to Late Miocene to Early Pliocene using ostracod biostratigraphy. [5] The age was revised by Gibson (1983) to extend into the Middle Pliocene based on foraminifera. [6]

  9. Petrified wood - Wikipedia

    en.wikipedia.org/wiki/Petrified_wood

    India – protected geological sites known for petrified wood are the National Fossil Wood Park, Tiruvakkarai (20-million-year-old fossils), and the Akal Wood Fossil Park (180-million-year-old fossils). Petrified wood has also been discovered in Dholavira in Kutch, Gujarat, dating back to 187–176 million years. [24]

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