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  2. Evolution of insects - Wikipedia

    en.wikipedia.org/wiki/Evolution_of_insects

    The first insects were landbound, but about 400 million years ago in the Devonian period one lineage of insects evolved flight, the first animals to do so. [1] The oldest insect fossil has been proposed to be Rhyniognatha hirsti, estimated to be 400 million years old, but the insect identity of the fossil has been contested. [3]

  3. Micropaleontology - Wikipedia

    en.wikipedia.org/wiki/Micropaleontology

    Fusulinid from the Plattsmouth Chert, Red Oak, Iowa ().Micropaleontology can be roughly divided into four areas of study on the basis of microfossil composition: (a) calcareous, as in coccoliths and foraminifera, (b) phosphatic, as in the study of some vertebrates, (c) siliceous, as in diatoms and radiolaria, or (d) organic, as in the pollen and spores studied in palynology.

  4. Palynology - Wikipedia

    en.wikipedia.org/wiki/Palynology

    Palynology is also used to date and understand the evolution of many kinds of plants and animals. In paleoclimatology, fossil palynomorphs are studied for their usefulness in understanding ancient Earth history in terms of reconstructing paleoenvironments and paleoclimates. [3] [4]

  5. Biofact (archaeology) - Wikipedia

    en.wikipedia.org/wiki/Biofact_(archaeology)

    Biofacts can include but are not limited to plants, seeds, pollen, animal bones, insects, fish bones and mollusks. [1] The study of biofacts, alongside other archaeological remains such as artifacts are a key element to understanding how past societies interacted with their surrounding environment and with each other.

  6. Molecular paleontology - Wikipedia

    en.wikipedia.org/wiki/Molecular_paleontology

    On the other hand, DNA extraction from insects can be done by grinding the sample, mixing it with buffer, and undergoing purification through glass fiber columns. [47] In the end, regardless of how the sample was isolated for these fossils, the DNA isolated must be able to undergo amplification. [4] [46] [47]

  7. Evidence of common descent - Wikipedia

    en.wikipedia.org/wiki/Evidence_of_common_descent

    Continental drift explains the current biogeography of the tree. Present day Glossopteris fossils are found in Permian strata in southeast South America, southeast Africa, all of Madagascar, northern India, all of Australia, all of New Zealand, and scattered on the southern and northern edges of Antarctica. During the Permian, these continents ...

  8. Millions of ancient fossils were discovered underneath a ...

    www.aol.com/news/millions-ancient-fossils-were...

    During construction, millions of fossils were found at a California high school, including megalodon teeth, extinct dolphins, and bird skulls.

  9. Lepidoptera fossil record - Wikipedia

    en.wikipedia.org/wiki/Lepidoptera_fossil_record

    The fossil record for Lepidoptera is lacking in comparison to other winged species, and tending not to be as common as some other insects in the habitats that are most conducive to fossilization, such as lakes and ponds, and their juvenile stage has only the head capsule as a hard part that might be preserved.

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