Plaque bacteria, earliest forms of life
Plaque bacteria have been linked to fossils from meteorites that date back millions of years. Plaque bacteria are survivors that landed and were spread by water throughout the planet. They found permanent residence among the rich mineral resources found in calcareous rock. Among the present day rocks, plaque bacteria exist as reminants of previous life. Their spore form is no larger than a grain of dust. Out of the spore, evolves a living organism. The spore of plaque bacteria come from the remains of shelled creatures such as foraminifera. When foraminifera die, their body decomposes, leaving their shells as fossils. The decomposed body are left as granules that carry the potential life of plaque bacteria. The granules of foraminifera mix with water and minerals to form mineral deposits. Minerals have a high alkaline content that certain living creatures can not tolerate. Alkaline environments have a high concentration of negative ions or electrons. The negative ions in an alkaline environment threaten the survival of oxygen dependent organisms. When the original organisms descended on earth, the planet had no oxygen dependent organisms. Bacteria used carbon dioxide for energy. This energy process is called fermentation. Bacteria that utilized this process are called fermentation bacteria. Fermentation bacteria that create energy without oxygen are called anaerobes. Fermentation bacteria take in carbon dioxide and expel oxygen. The oxygen made the original bacteria sick. The sick bacteria mutated to use the oxygen to their benefit. This process evolved a new class of organisms that utilized oxygen to create energy. These organisms are called aerobes. Human cells are forms of life that descended from aerobes. Oxygen is a good receptor of chemical ions necessary for creating energy. Energy for aerobes is dependent on breathing chemical ions. In simple terms, oxygen keeps the cell breathing cycle alive. Without oxygen, aerobes die. Oxygen is a threat to fermentation bacteria. Not pure oxygen, but unstable oxygen. Oxygen that has free electrons. Stable oxygen is in the form of O2 or two molecules of oxygen. Forms of unstable oxygen are singlet oxygen O1 or triplet oxygen O3. Fermentation bacteria are triggered by unstable oxygen to change from a spore or granule to full size adult bacteria. The process of growth involves forming a cell wall and colonizing to protect themselves in the changing environment. Plaque bacteria, like all living organisms have unique characteristics for survival. Their cell wall consists of biominerals. Biominerals form armored shells that serve to protect the bacteria from chemical poisons such as unstable oxygen. There are many species that form shells as protection. Clams, mussels, snails, turtles, crabs, oysters, egg shells, armadillos, rhinocerous, foraminifera and other creatures both large and small, land dwelling and sea dwelling, all form biomineral shells to protect themselves in the environment. The smallest and earliest forms of these creatures are plaque bacteria.
Plaque bacteria are unique organisms
Bacteria begin as a spore form and grow by developing a cell wall and taking in fluids to balloon to their adult size. Plaque bacteria are different in that they grow by developing a cell wall of biominerals. Plaque bacteria attract minerals to their outer coating by becoming a magnet. Magnets have attracting forces due to being surrounded by an electromagnetic field. Plaque bacteria turn into magnets when their environment becomes pulsated by free electrons. The electrons become attracted to the biofilm outer coating of plaque bacteria. The biofilm becomes an oxidizing agent to attract reducing agents. Calcium belongs to the alkaline earth metals that are reducing agents. Calcium attaches to the outer coating, reverses its polarity and turns into a magnet to attract more calcium. The calcium piles up in layers on the surface of plaque bacteria. The process forms an apatite formation that is similar to tooth enamel and bone. When the cell wall of plaque bacteria is fully formed, the cell wall becomes a magnet to attract the cell wall of other plaque bacteria. The cells walls bond to become a pair. The pair attracts other pair to form a chain. Chained bacteria attract other chains to form a cluster. Clusters attract other bacteria to form a colony. The colony attracts more calcium to cover all the attached bacteria to form a shell. The shell forms a crystal that is called plaque. The formation of plaque continues to grow as long as there is calcium available and as long as there are free electrons pulsating in the environment. Lowering the pH, neutralizes the free electrons and stops plaque formation. Plaque bacteria have no control of their actions. They simply follow the laws of science. Unlike humans, bacteria do not have reasoning power and are completely at the mercy of the pH of their environment.
Cultured Plaque bacteria
Robert Folk and Olavi Kajander may have discovered the cause of plaque in humans. They were able to isolate the bacteria and culture them. Folk discovered the bacteria in limestone and other calcareous rock. Folk discovered that the bacteria needed special staining and a special media solution to grow. He called the bacteria nannobacteria. Nannobacteria need water, minerals and air to form plaque. Folk was able to link nannobacteria to the oxidation of metals. Folk used nannobacteria to form rust. Folk believes that nannobacteria use biominerals to protect themselves in a changing environment. Kajander was able to grow plaque bacteria to link them with human disease. Kajander called the bacteria nanobacteria sanguineum. Nanobacteria grow plaque under certain conditions. Kander found nanobacteria living in cow blood and human blood. The bacteria did not form plaque in blood because of blood inhibitors. He identified the inhibitors as osteocalcin, osteopontin and fetuin. Nanobacteria would form plaque only when the pH was above 7.4. Under a pH of 7.4, nanobacteria would grow, but not form plaque. Nanobacteria needed an increase in pH to 7.6 to grow plaque that resemble calcium deposits in human disease. Kajander found that nanobacteria sucked up all the calcium and phosphate in a special medium of pH 7.6 until there was none of the minerals left. The plaque formation consisted of a shell that covered the colonized nanobacteria. Kajander used powder fragments from human kidney stones to grow plaque. Kajander was not able to grow plaque without the presence of nanobacteria. Kajander concluded that nanobacteria are essential to form plaque in human diseases. Among the diseases is dental plaque and periodontal disease.
Plaque bacteria and human disease
Even before the discovery by Folk and Kajander, resistant bacteria have been associated with degenerative diseases in humans. Resistant bacteria live in blood, essential to the clotting of blood. Lack of resisant bacteria results in bleeding diseases. Resistant bacteria that mutate and grow results in thick blood diseases. Kajander found that nanobacteria first use fats to form their cell wall. When the fat becomes depleted, nanobacteria replace the fats with calcium deposits. In human heart disease, nanobacteria could be the cause of plaque formation. In atherosclerosis, plaque formation consists of fatty deposits in the coronary arteries. The fat is contributed to a high cholesterol intake by the heart patient. Nanobacteria could use the cholesterol to form fatty plaque. In the absence of cholesterol, nanobacteria replace the fat with calcium minerals. This process results in arteriosclerosis, calcium deposits in the coronary arteries. Both of these heart conditions result from thick blood. Thick blood is treated with blood thinners such as aspirin and other prescription medicines. Thick blood is associated with stimulants. Stimulants are associated with alkaloids of chemicals with high alkaline content. When the blood has an increase in pH, resistant bacteria mutate and grow to thicken blood. What increases the pH in blood are oxidants or better known as free radicals. Free radicals carry free electrons to pulsate electricity in blood. Thick blood occurs because of free radicals and a weak immune system. A strong immune system has blood inhibitors to prevent plaque formation. Thick blood may be the link to heart disease and periodontal disease.
Plaque bacteria are resistant bacteria
Plaque bacteria are resistant bacteria because they resist man's attempt to destroy bacteria. Man has introduced heat pasteurization, radiation, chemotherapy and vaccines to destroy bacteria. Plaque bacteria are able to resist all these methods. Plaque bacteria become vulnerable when there is no water, minerals and an increase in pH above 7.4. Critics may argue that plaque bacteria are fragments of cell walls of gram negative bacilli. Even if that be the case, plaque formation needs water, minerals, pH above 7.4 and fragments of gram negative bacteria. In either case, plaque formation can be reduced or prevented if any of the ingredients are missing. In the oral cavity, only the pH can be changed to prevent plaque.
Plaque formation is science in action
The new theory of plaque formation is only a theory but the theory is backed by science. Think of plaque bacteria as living particles that have mass and energy surrounding their bodies. Particles follow a certain behavior pattern that can be formulated by mathmatical equations. A(pH above 7.4) + B(Plaque bacteria) + C(minerals) + D(water) + E(Unstable oxygen) = Plaque. Any of missing ingredients and there is no plaque formation. Water in the oral cavity is in the form of saliva, blood and lymph fluid. Unstable oxygen comes from products introduced into the oral cavity. By controlling the pH of saliva and reducing unstable oxygen products, dental plaque and periodontal disease can be inhibited.
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