Fossils have layer upon layer of hardened tissue. Therefore they are quite rough in texture where the insides are more malleable. Depending on what the fossil is of some fossils give off a sour aroma. Most of the time animal fossils deteriate at a faster rate than fossils of humans or shells. Fossils are a unique study and I you study them further.
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Well, the tracks are examples of trace fossils. Trace fossils are not fossils in the traditional sense. Instead, they are fossils of something other than the animal or plant's form, like a animal track or burrow, that tells us an animal has been there.
Invertebrate paleontologists study fossils of animals without backbones, like mollusks and arthropods. Vertebrate paleontologists focus on fossils of animals with backbones, such as dinosaurs, mammals, and fish. Micropaleontologists study microscopic fossils like pollen, foraminifera, and diatoms to understand past environments and climates.
Ah, those are called fossils, my friend! Fossils are like little time capsules that give us a peek into the past, showing us what plants and animals looked like long ago. It's amazing how nature preserves these treasures for us to discover and learn from.
Fossils, which are the preserved remains or imprints of plants and animals from the past, are the most common traces of past life found in Earth's crust. Other traces include trace fossils like footprints, burrows, or coprolites (fossilized feces), as well as microfossils like pollen grains or microscopic shells. Additionally, chemical signatures in rocks or minerals can also provide clues about past life on Earth.
Fossils have layer upon layer of hardened tissue. Therefore they are quite rough in texture where the insides are more malleable. Depending on what the fossil is of some fossils give off a sour aroma. Most of the time animal fossils deteriate at a faster rate than fossils of humans or shells. Fossils are a unique study and I you study them further.
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this is an incoherent question that cannot possibly be answered
No. Fossils are chemicals like stone that have replaced organisms after they die.
Two kinds of fossils are body fossils, which preserve the actual remains or impressions of an ancient organism, and trace fossils, which are indirect evidence of an organism's activity, such as footprints or burrows.
In simplest terms, fossils show what living things were like long ago.
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Cast fossils: Formed when minerals fill a mold left by a decayed organism. Mold fossils: Created when an organism's remains leave an impression in sediment that hardens into rock. Petrified fossils: Organic material replaced by minerals over time, forming a rock-like replica. Trace fossils: Evidence of an organism's activity (e.g., footprints or burrows) preserved in sedimentary rock. Carbon fossils: Organisms preserved in carbon-rich environments, like coal or oil deposits. Preserved fossils: Organisms remain intact or partially intact due to exceptional preservation conditions.
if a person had fossils he/she would have to be dead... like your grand grand parents pushing up daises
When something be on side of the road like a dinousar and the fossils.
If you're referring to the remains of prehistoric organisms, they don't eat anything. They're dead. If you're referring to antiquated or stubbornly unchanging people, they eat whatever they feel like.
molds and casts, trace fossils, petrified wood, and carbon filmThe four types of fossils are mold fossils, cast fossils, true-form fossils, and trace fossils. Mold fossils are impressions from when the plant or animal first decomposed. Cast fossils are plant or animal remains. True-form fossils are remaining body parts from an animal. Trace fossils are marks that have been left by animal, such as footprints.