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What's A Fossil?

What's A Fossil?

The modern use of the word ‘fossil’ refers to the physical proof of former life from a period of time prior to recorded human history. This prehistoric evidence includes the fossilised remains of dwelling organisms, impressions and moulds of their physical type, and marks/traces created in the sediment by their activities. There isn't any universally agreed age at which the evidence might be termed fossilised, nonetheless it’s broadly understood to encompass anything more than a couple of thousand years. Such a definition includes our prehistoric human ancestry and the ice age fauna (e.g. mammoths) as well as more ancient fossil teams such as the dinosaurs, ammonites and trilobites.

The earliest reported fossil discoveries date from 3.5 billion years ago, however it wasn’t until approximately 600 million years ago that complex multi-mobile life began to enter the fossil report, and for the purposes of fossil hunting nearly all of effort is directed towards fossils of this age and younger.

Fossils occur commonly around the globe although just a small proportion of life makes it into the fossil record. Most dwelling organisms merely decay with out hint after dying as pure processes recycle their soft tissues and even hard components corresponding to bone and shell. Thus, the abundance of fossils in the geological document reflects the frequency of favourable situations the place preservation is feasible, the immense number of organisms that have lived, and the huge size of time over which the rocks have accumulated.



How do fossils type?
The time period ‘fossilisation’ refers to a wide range of typically advanced processes that enable the preservation of organic remains within the geological record. It often consists of the next circumstances: rapid and everlasting burial/entombment – defending the specimen from environmental or biological disturbance; oxygen deprivation – limiting the extent of decay and likewise organic activity/scavenging; continued sediment accumulation as opposed to an eroding surface – ensuring the organism remains buried in the long-time period; and the absence of excessive heating or compression which might otherwise destroy it.

Fossil evidence is typically preserved within sediments deposited beneath water, partly because the situations outlined above happen more frequently in these environments, and in addition because the majority of the Earth’s surface is covered by water (70%+). Even fossils derived from land, together with dinosaur bones and organisms preserved within amber (fossilised tree resin) were finally preserved in sediments deposited beneath water i.e. in wetlands, lakes, rivers, estuaries or swept out to sea.

Fossilisation also can happen on land, albeit to a far lesser extent, and includes (for instance) specimens that have undergone mummification in the sterile environment of a cave or desert. Nevertheless in reality these examples are only a delay to decomposition somewhat than an enduring mode of fossilisation and specimens require everlasting storage in a local weather managed environment with a purpose to restrict its affects.

In the following example a fish is used to illustrate the phases related to fossilisation within off-shore marine sediments. This is just one summarised example, in reality there are dependless situations that create the conditions vital for fossilisation in marine sediments.

Death
Having reached adulthood and returned to its beginning place to spawn, this explicit fish reaches the tip of its life and dies. Soon after death the body of the fish turns into water-logged and sinks to the seafloor (note that very often the gases produced throughout decomposition cause the carcass to float back to the surface, so the ultimate resting place could also be far away). More typically than not the carcass could be pulled apart and scattered by scavenging crustaceans and different fish, nonetheless on this occasion the absence of any massive scavengers leaves the fish comparatively undisturbed.