Fossils

Igneous rocks form directly from a melt, hence there are no fossils contained within them.

Metamorphic rocks are pre-existing rocks (sedimentary, igneous, or even metamorphic rocks themselves) which have undergone significantly increased pressures and/or temperatures. Any structure(s) or fossils which may have been present tend to be destroyed, reworked, or have their character diminished. Additionally, the presence or absence of water can often cause a wide variation in the mineral assemblages.

Scientists can learn about extinction by studying fossils because fossils provide physical evidence of organisms that lived in the past, including those that have gone extinct. By examining the distribution and characteristics of these fossils, scientists can piece together the timing and causes of extinction events. Additionally, studying fossils can reveal patterns of extinction across different species and ecosystems, helping scientists understand the impact of environmental changes on biodiversity.

Fossils can form anywhere that conditions are conducive to preservation, such as in sedimentary rocks, tar pits, or ice. However, the likelihood of fossil formation varies depending on the environment and the organisms present.

A preserved fossil is an organism or Animal that has been PERFECTLY PRESERVED for lots of years, or however old it may be. For example, a wooly mammoth frozen in the ice for millions of years would be known as a preserved fossil.
There are 2 different types of fossil preservation- preservation with alteration and without. With alteration also has different types. The type of organism you are looking for depends on the how it was preserved.

Gideon Mantell is famous for his discovery of Iguanodon. He also gave it its name, which means, "iguana tooth."

fossils are preserved animals or plants. but index fossils are fossils have wide distribution,many of them,evolves rapidly, and very easy to recognize.

Ammonites are index fossils.

The fossils were made only in a certain short time period.

99% of all organism who lived once are now extinct, so a list would be more than extensive!

Dinosaurs are the big fossils. Mammal fossils are big too. Human and proto-human fossils may be the biggest things in fossils ever.

There is no definitive answer to who discovered the last fossil on earth, as new fossils are still being discovered regularly by paleontologists around the world. Fossil discoveries are ongoing and driven by scientific research and exploration.

Yes, fossils are real. Fossils are the preserved remains or impressions of plants, animals, and other organisms that lived in the distant past. They provide valuable information about Earth's history and the evolution of life.

Body fossils are made out of remains of plants and animals that have been preserved in rock or sediment. The original material of the organism is often replaced by minerals, creating a cast or replica of the organism's original structure. Hard parts of the organism, such as bones, shells, or teeth, are commonly preserved as body fossils.

The relative age of a fossil that can be determined by comparing it to an index fossil is called biostratigraphic dating. This method relies on the known age range of the index fossil to estimate the relative age of the fossil being studied.

When the animal dies its skeleton settles on the sea floor and is buried by sediment. that thickens and begins to turn to stone. The skeleton dissolves and a mold is formed. Minerals crystallize inside the mold and the cast is formed.

Fossil fuels are formed by natural resources such as dead organisms by decomposition (aerobic or mostly anaerobic). Fossil fuels have high percentages of carbon. It includes coal petrol diesel natural gas etc. It ranges from volatile materials like petrol to nonvolatile materials like coal.

Superposition is the methodology of younger sediments being deposited over older rocks. Paleontologists can determine the evolution or extinction of a species by looking at what fossils are either present or absent in a particular sedimentary layer.

The plant or animal must be encased in a substance that prevents destruction or erosion. Ice, tar, or layers of mud or clay can isolate the remains from sunlight, air, and consumption by other lifeforms. Over time, a mineralized form or a rock cast will result in a fossil or fossil imprint.

The earliest vertebrate fossil is believed to be Haikouichthys, a primitive fish that lived around 530 million years ago during the Cambrian period. Its discovery in China provided important insights into the early evolution of vertebrates.

Carbon dating is used to determine the approximate age of organic materials, such as bones or textiles, up to around 50,000 years old. By measuring the amount of a radioactive form of carbon in a sample and comparing it to the levels in the atmosphere when the organism was alive, scientists can estimate its age. This method is commonly used in archaeology, paleontology, and geology to date ancient artifacts and fossils.

When two continental plates collide, one has to give and the other rises over the first. It there are fossils in this material, it can be pushed to the highest peaks of mountains. Evidence of this is found in the grand canyon where fossils of ocean creatures anr found many thousands of feet above sea level.

The soft-bodied nature of early animals and their small size are two characteristics that explain the scarcity of animal fossils older than the Cambrian Period. Soft-bodied organisms are less likely to fossilize than hard-bodied ones, and small organisms are harder to preserve in the fossil record.

Fossils can change due to a variety of reasons such as erosion, pressure, and chemical reactions. Over time, the original organic material may be replaced by minerals, leading to changes in composition. Factors like temperature and moisture levels in the environment can also contribute to fossil alteration.

Coal forms from plant material that undergoes slow decomposition under high pressure and heat over millions of years. Human fossils are unlikely to be preserved in coal because humans are relatively recent in geological time and are less likely to have been present in the environments where coal formed. Additionally, human remains are usually buried in circumstances that do not lead to coal formation.

Greek learning was preserved through the efforts of scholars in places like Alexandria, Byzantium, and the Islamic world, who translated and copied Greek works. The Byzantine Empire also played a key role in preserving Greek texts. Additionally, the Renaissance in Europe sparked renewed interest in Greek learning and led to the rediscovery of many ancient Greek works.

A hardened and preserved footprint is an example of a fossilized trace fossil. Trace fossils are marks or imprints left behind by ancient organisms, providing insights into their behaviors and interactions with their environment.

No, fossils are typically found in sedimentary rocks, not igneous rocks. Sedimentary rocks form from the accumulation and compaction of sediments, which can preserve fossils, while igneous rocks form from the cooling and solidification of molten rock, where fossils are usually destroyed.