Wiki User
∙ 13y agoTrue
Wiki User
∙ 13y agoYes, a specialized rock that is a remnant of a dead organism is considered a fossil. Fossils are the preserved remains or traces of ancient organisms, providing valuable insights into the history of life on Earth.
A trace of a long dead organism could be a fossilized imprint, track, or remains left behind in sedimentary rock. These traces provide valuable information about the organism's existence, behavior, and environment in the past. Scientists study these traces to learn more about ancient life on Earth.
An organism considered dead can no longer perform life functions and does not respond to stimuli. In contrast, a living organism actively maintains homeostasis and responds to its environment to sustain life processes. The concept of an organism being "dead and alive" simultaneously does not align with biological definitions.
A body fossil would be in the form, or part of, the organism that has fossilized. A trace fossil indicates evidences other than a fossilized body part, that indicates the existence of an organism, such as burrows, trails, eggs, nests, and fecal matter.
B. The organism must be buried in sediment soon after it dies.C - the organism must go through a process of petrificationNeededMoist sediment or soilorganism trapped, dieslack of anything disturbing that areamoistness ; warmth ; heat to break down additional layeringpressure from more layers on toplengthy amount of time (millions of years)
A black dwarf does not burn anything. A black dwarf is the cooled remnant of a dead star.
not really fossil is made from dead organism
A dead organism decomposes in a rainforest
fossil
yes but only where dead organism
a fossil
yes but only where dead organism
Gasoline, coal, or fossil fuels
Pyritisation is when iron pyrite replaces hard remains of a dead organism.
Dead organism are compressed by dirt
To turn a dead organism into fossil fuel, three main factors are needed: 1) organic material from the dead organism, such as plants or animals, 2) high pressure from layers of sediment accumulating over time, and 3) high temperatures, typically from the Earth's heat and pressure from the overlying sediment. Over millions of years, these conditions transform the organic material into fossil fuels like coal, oil, or natural gas.
The best way to identify fossils is to get a book or website that shows pictures of different types. Most fossils are formed by petrification, where part of the dead organism has slowly changed into rock. However, you might also find a fossil cast, where rock has formed around a dead organism and left a mold; it can either be a hollow space, or more rock may have filled in the shape of the organism. There are even fossil footprints and fossil poo!
A trace of a long dead organism could be a fossilized imprint, track, or remains left behind in sedimentary rock. These traces provide valuable information about the organism's existence, behavior, and environment in the past. Scientists study these traces to learn more about ancient life on Earth.