Limestone is often a biochemical rock that contains fossils. It primarily forms from the accumulation of organic materials, such as the remains of marine organisms like corals and mollusks, which contribute to its composition. Over time, these materials can solidify into rock, preserving the fossils within. This characteristic makes limestone significant for studying past environmental conditions and the evolution of life.
Biochemical rock is characterized by the presence of organic materials or fossils that indicate biological activity in its formation. This type of rock often contains remains of plants and animals, such as shells or coral, and is typically formed through the accumulation of biological debris. Common examples include limestone, which can form from coral reefs or shell deposits, and coal, which originates from plant material. The organic origin distinguishes biochemical rocks from other sedimentary types.
The rough estimating of the age of a fossil or rock containing fossils is called relative dating, and is based on the position of the rock or fossil in undisturbed sedimentary strata which contains what are called 'index fossils', fossils that only appear in specific geologic time periods.
Sandstone is primarily a clastic sedimentary rock composed of sand-sized grains, usually derived from the weathering of pre-existing rocks. While it can contain biochemical components, such as fossils or grains formed from biological processes (like silica from diatoms), it is not classified as a biochemical rock. Instead, biochemical rocks are typically those formed from the accumulation of organic materials, such as limestone made from coral or shell fragments. Therefore, while sandstone may incorporate some biochemical elements, its primary classification is as a clastic rock.
fossils are fine in metamorphic rock
Limestone is often a biochemical rock that contains fossils. It primarily forms from the accumulation of organic materials, such as the remains of marine organisms like corals and mollusks, which contribute to its composition. Over time, these materials can solidify into rock, preserving the fossils within. This characteristic makes limestone significant for studying past environmental conditions and the evolution of life.
Limestone is a biochemical rock that can contain fossils. It is formed from the accumulation of calcite or aragonite shells or skeletal fragments of organisms such as corals, foraminifera, and mollusks. Over time, these remains can be compressed and preserved in the rock.
Paleontologists are looking for fossils in sedimentary rock.
The Adirondack rocks have been both severely folded and sheared by ductile deformation and shattered by brittle.
Index fossils are fossils of organisms that lived for a relatively short period of time but were widespread geographically. By identifying these index fossils in a particular layer of rock, scientists can determine the age of the rock and correlate it with other rock layers containing the same index fossils. This allows for the relative dating of rock layers based on the presence of specific index fossils.
Biochemical rock is characterized by the presence of organic materials or fossils that indicate biological activity in its formation. This type of rock often contains remains of plants and animals, such as shells or coral, and is typically formed through the accumulation of biological debris. Common examples include limestone, which can form from coral reefs or shell deposits, and coal, which originates from plant material. The organic origin distinguishes biochemical rocks from other sedimentary types.
fossils
sedimentary
They Often Contain fossils.
No rock could be a biochemical.
Quite often, fossils are contained within shale rock.
fossils