•Origin of macro-biominerals
•Formed by proteins -Provide template
•Biominerals tend to: -Be finely crystalline (less crystalline than geominerals) -Have more organics -Be stronger than geominerals -Be easier to form than geominerals (aragonite vs. calcite)
biochemical cycles connect biological, geological, and chemical aspects of the biosphere.
biochemical cycles connect biological, geological, and chemical aspects of the biosphere.
This is an example of geological vertical intrusion.
Any of the national geological surveys, for example the British Geological Survey.
Biogeochemical cycles connect biological, geological, and chemical aspects of the biosphere.
"Geo" means "earth"; "logy" means "the study of". So geology is the science of studying the earth. Something that is geological would pertain to this science in some way; for example, a geological survey.
Biominerals, which are naturally occurring minerals produced by living organisms, can be used in various applications, including medicine, environmental remediation, and materials science. In medicine, they can aid in bone regeneration and delivery of drugs due to their biocompatibility. In environmental contexts, biominerals can help in the detoxification of pollutants and the recovery of valuable metals from waste. Additionally, their unique properties make them suitable for developing innovative materials with enhanced performance characteristics.
The cycles that connect biological, geological, and chemical aspects of organisms in a biosphere include the carbon cycle, nitrogen cycle, and water cycle. The carbon cycle involves the exchange of carbon among living organisms, the atmosphere, and geological formations, impacting climate and energy flows. The nitrogen cycle facilitates the transformation of nitrogen through different chemical forms, essential for life and influenced by geological processes. Lastly, the water cycle connects all life forms by regulating hydration and nutrient transport, while also interacting with geological features through erosion and sedimentation.
Geological time starts at the Big bang. For example, if a scientist says that a 1000years is not a long time in "geological time" they simply mean on a timescale a thousand years in nothing
yes there are. biological events would not have been able to occur if geological events didnt occur. for example, if there was no oxygen in the atmosphere (geological event) plants would not have been able to come to life (biological event).