Energy & Green Tech

Scientists enhance recyclability of waste plastic

Plastics are incredible materials with properties invaluable to the functioning of our modern world. They are strong, flexible, versatile, long-lasting and inexpensive. In particular, high-density polyethylene (HDPE) is ubiquitous ...

Energy & Green Tech

New Zealand's green hydrogen edge

Aotearoa New Zealand is likely to have a competitive advantage when it comes to generating clean, green hydrogen and this edge should help the country reduce its future reliance on fossil fuels, says a leading sustainable ...

Energy & Green Tech

Sun, wind aplenty, Spain vies to lead EU in green hydrogen

With an abundance of sun and wind, Spain is positioning itself as Europe's future leader in green hydrogen production to clean up heavy industries. But some energy sector experts express caution over ramping up an industry ...

Energy & Green Tech

Cow manure fuels French tractors

A French farmer steps away from his barn and fills up a tractor with fuel made from the manure of his cows, an attempt to put their climate-damaging methane to good use.

Energy & Green Tech

Q&A: Offshore wind power's last mile

Offshore wind power has the potential to provide all the electrical power needed by the Northeast with thousands of extremely large wind turbines located offshore. But one of the biggest hurdles to creating that reality is ...

Software

ExaSMR simulation toolkit advances nuclear reactor design

Alternatives to carbon-producing energy sources are becoming ever more imperative as climate change shows its effects on the Earth and in our daily lives. Although fossil fuels still generate much of the electricity in the ...

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Fossil

Fossils (from Latin fossus, literally "having been dug up") are the preserved remains or traces of animals, plants, and other organisms from the remote past. The totality of fossils, both discovered and undiscovered, and their placement in fossiliferous (fossil-containing) rock formations and sedimentary layers (strata) is known as the fossil record. The study of fossils across geological time, how they were formed, and the evolutionary relationships between taxa (phylogeny) are some of the most important functions of the science of paleontology. Such a preserved specimen is called a "fossil" if it is older than some minimum age, most often the arbitrary date of 10,000 years ago. Hence, fossils range in age from the youngest at the start of the Holocene Epoch to the oldest from the Archaean Eon several billion years old. The observations that certain fossils were associated with certain rock strata led early geologists to recognize a geological timescale in the 19th century. The development of radiometric dating techniques in the early 20th century allowed geologists to determine the numerical or "absolute" age of the various strata and thereby the included fossils.

Like extant organisms, fossils vary in size from microscopic, such as single bacterial cells only one micrometer in diameter, to gigantic, such as dinosaurs and trees many meters long and weighing many tons. A fossil normally preserves only a portion of the deceased organism, usually that portion that was partially mineralized during life, such as the bones and teeth of vertebrates, or the chitinous exoskeletons of invertebrates. Preservation of soft tissues is rare in the fossil record. Fossils may also consist of the marks left behind by the organism while it was alive, such as the footprint or feces (coprolites) of a reptile. These types of fossil are called trace fossils (or ichnofossils), as opposed to body fossils. Finally, past life leaves some markers that cannot be seen but can be detected in the form of biochemical signals; these are known as chemofossils or biomarkers.

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