Evaporates do not have a biochemical origin. An evaporate is a mineral deposit that is left after a body of water evaporates.
Chemical sedimentary rocks
When seas or lakes evaporate, evaporites form which are sedimentary rocks that consist of minerals deposited from evaporating water. Common evaporite minerals include halite (rock salt), gypsum, and calcite.
Rocks formed by the evaporation of water are called evaporites. Examples of evaporites include rock salt, gypsum, and sylvite. These rocks form as a result of the precipitation of minerals as the water evaporates, leaving behind the dissolved materials.
The remaining minerals are called evaporites.
what are the biochemical tests for ascomycetes fungi?
Yes. Most limestone is biochemical.
Douglas W. Kirkland has written: 'Marine evaporites: origin, diagenesis, and geochemistry' -- subject(s): Addresses, essays, lectures, Evaporites 'The heliothermic lake' -- subject(s): Solar energy, Limnology
No. Evaporites are found in sedimentary rocks.
Alexander Ivanovich Oparin was a Soviet biochemist who, in 1924, put forward a coherent theory for the origin of life through gradually increasing sophistication of biochemical change in his book The Origin of Life.
Examples of biochemical sedimentary rocks include limestone, which forms from the accumulation of shells and coral fragments, and chert, which is formed from the silica-rich remains of marine organisms. Evaporites are sedimentary rocks that form from the precipitation of minerals from evaporating water bodies, such as rock salt (halite) and gypsum, which are common examples.
Evaporites are rocks that form by the precipitation of minerals from the evaporation of water. Common types of evaporites include rock salt (halite), gypsum, and anhydrite. These rocks typically form in arid environments where the rate of evaporation exceeds the rate of water inflow.
Vivian S. Hall has written: 'Salt, evaporites, and brines' -- subject(s): Bibliography, Evaporites, Saline waters, Salt
evaporites or precipatates
rock salt and rock gypsum
Chemical sedimentary rocks
Evaporites, which are sedimentary rocks formed by the evaporation of water in closed basins, can play a significant role in the formation and trapping of oil deposits. They often create impermeable seals that trap hydrocarbons generated from organic-rich source rocks beneath them. Additionally, the presence of evaporites can indicate specific depositional environments that are conducive to oil generation. Thus, the relationship is primarily one of structural and environmental influence, where evaporites help contain and preserve oil reservoirs.
While of biochemical origin, coal is not considered an igneous rock, but rather a sedimentary one, due to its process of formation wherein dead and decaying organic matter (such as animal and plant matter, typing being found in bogs or swamps) was compressed into rock form over a period of several hundred million years.