No rock could be a biochemical.
Biochemical sedimentary rocks form from sediment derived by biological processes. A type of sedimentary rock primarily comprising deposits resulting.
Chalk is a biochemical sedimentary rock, formed mainly from the calcareous remains of microscopic marine organisms like plankton. It is primarily composed of calcium carbonate and is often found in extensive deposits in areas that were once covered by ancient seas.
Shale is a type of sedimentary rock that is formed from the compaction and cementation of clay or mud particles. It is not considered a biochemical rock because it is primarily composed of physical and chemical processes, rather than being formed from the accumulation of organic materials like limestone or coal.
No, a conglomerate is not a biochemical. A conglomerate is a geological term referring to a rock made up of different kinds of minerals and rock fragments. Biochemicals, on the other hand, are chemicals produced by living organisms.
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.
Enzymes
A lipid
organic/biochemical sedimentary rocks are formed of once-living organisms
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.
Lipids Lipids
No, the rock cycle is not part of the biochemical cycle. The rock cycle describes the process through which rocks change and transform over time due to various geological forces, whereas the biochemical cycle involves the movement and transformation of matter like carbon, nitrogen, and phosphorus through living organisms, the atmosphere, and the Earth's crust.
Chalk and coal are examples of a kind of sedimentary rock called biochemical sedimentary rock. Biochemical sedimentary rocks form from the accumulation and lithification of organic remains, such as shells and plant material.