Carbon Dating How Old Is The Earth

To find out, we need to peek into the carbon dating process that specialists use to arrive at tens of thousands of years. What role might the Genesis Flood have played in the amount of carbon? The Flood would have buried large amounts of carbon from living organisms
(plant and animal) to form today’s fossil fuels (coal, oil, etc.).

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Carbon-Dating Ancient Pottery Just Got Easier

Since the discovery of carbon dating, it has revolutionized our understanding of our planet. For example, we can finally put a date on prehistoric life forms and rock strata. Using the principle of faunal succession, if an unidentified fossil is found in the same rock layer as an index fossil, the two species must have existed during the same period of time (Figure 4). If the same index fossil is found in different areas, the strata in each area were likely deposited at the same time. Thus, the principle of faunal succession makes it possible to determine the relative age of unknown fossils and correlate fossil sites across large discontinuous areas. A fossil can be studied to determine what kind of organism it represents, how the organism lived, and how it was preserved.

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About Nine Planets

The importance of Carbon years after its discovery is difficult to understate. While the isotope would fundamentally change entire scientific fields and our understanding of the past, its creators didn’t fare quite as well. Tracking this ratio has been critical in unraveling mysteries in the fields of anthropology, archaeology, and paleontology, among countless others. But Kamen and Ruben’s discovery didn’t go mainstream until 1946, when Willard Frank Libby, a professor of chemistry at the University of Chicago, conceived of a way to use carbon-14 to date organic matter.

In 1946, Libby proposed this groundbreaking idea in the journal Physical Review. The “chronostratigraphic unit” is the name assigned to the layer of rock. The age given in million years (Ma) is an assumption based on the belief in evolution (not science). The carbon years before present (YBP) have not been corrected with the assumptions above and don’t conflict with a 6,000 year old earth. Any percentage modern carbon (pMC) above 0.01 support the biblical age of the earth and is proof that fossils and rock layers are not millions of years old.

There was a sudden injection of carbon 14 in the 1950s and 1960s during the atomic bomb tests, and these tests can help us understand the effects of sudden changes to carbon 14/12 levels. The nuclear testing caused the carbon 14 values to skyrocket in the atmosphere while the carbon 12 remained the same; carbon-14 levels doubled from the pre-atomic-testing values (Reference 1). Carbon 14 has a half-life of 5730 years and had it not been for the dry land and the oceans, it would have taken 10s of thousands of years to recover to the pre-atomic-testing levels, but, surprisingly, it recovered quickly, in just a few decades. Equilibrium was reached quickly due to the carbon-14 absorption in the land and sea.

“Today, we’re releasing carbon quickly in huge amounts and it is having a big impact on global climate.” Paradoxically, UC’s Algeo said, these refuges of life likely helped to warm the planet, ending the Marinoan ice age. The algae in the water released carbon dioxide into the atmosphere over time, gradually thawing the glaciers.

In other words, the Rhenium decays over 1 billion times faster under such conditions. Thus, any age estimates based on Rhenium-Osmium decay may be vastly inflated. However, age is not a substance that can be measured by scientific equipment. The tools of science allow us to measure mass, volume, pressure, force, weight, and composition…  but not age.

Table from book

The carbon isotope ratio in the ancient skies was the same as it is today. The number of protons in the nucleus of an atom determines the element. For example, all carbon atoms have 6 protons, all atoms of nitrogen have 7 protons, and all oxygen atoms have 8 protons. The number of neutrons in the nucleus can vary in any given type of atom.