The fossils belong to Petrifaction type of preservation.
petrified fossils
An organism that kills and eats all or part of another organism is called a carnivore.
The vast majority of visible fossils are marine invertebrates, animals that live in the sea and have no backbone, mostly animals with a hard outer shell. This would include clams, coral, brachiopods, ammonites, and other animals familiar to us, as well as extinct animals like trilobites and crinoids. In some locations the deposits are dominated by fish fossils and more rarely insects.
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.
A petrified fossil is a fossil formed when organic material is replaced by minerals, turning it into stone. This process preserves the structure of the original organism but fills it with minerals, essentially creating a rock replica of the organism. Petrified fossils provide valuable information about ancient life forms and environments.
Mold fossils- an empty space is left when an organism is buried in sedimentary and it decays.Cast fossils- Minerals in rocks fill space left by a decayed organism.(replica)Trace fossils- Markings left by an animal. (footprints, trail, or burrow)Petrified fossils- Minerals penetrate and replace all or part of an organism.Imprint fossils
Mold fossils- an empty space is left when an organism is buried in sedimentary and it decays.Cast fossils- Minerals in rocks fill space left by a decayed organism.(replica)Trace fossils- Markings left by an animal. (footprints, trail, or burrow)Petrified fossils- Minerals penetrate and replace all or part of an organism.Imprint fossils
Permineralized fossil are formed when dissolved minerals precipitate from a solution in the space occupied by the organism's remains.
petrified fossils
An organism that kills and eats all or part of another organism is called a carnivore.
All are indicative of the size and shape and possible habitat of the original organism.
A fossil formed through the process of permineralization, where minerals gradually replace the organic materials in the organism's remains, creating a rock-like replica of the original organism. This process preserves the structure and sometimes even the cellular details of the organism.
The vast majority of visible fossils are marine invertebrates, animals that live in the sea and have no backbone, mostly animals with a hard outer shell. This would include clams, coral, brachiopods, ammonites, and other animals familiar to us, as well as extinct animals like trilobites and crinoids. In some locations the deposits are dominated by fish fossils and more rarely insects.
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.
A fossil is the preserved remains or traces of a once-living organism, while an imprint is a mark or indentation left behind by an organism on a surface. Fossils can include imprints, but not all imprints are considered fossils. Fossils provide more detailed information about the organism's structure and biology, while imprints are more surface-level.
All parts of plants have been fossilized.
All your cells are part of you, and you are an organism. Nerve cells are included.