
Fossil of an ammonite
How can we be so sure of the age of the earth?
The age of the earth, according to the current scientific consensus is 4.54 billion years old (Dalrymple, 2001). One of beauties of this conclusion is that it is reached via various lines of evidence. Just like the proverb “all roads lead to Rome”, different methods of dating still conclude the earth is billions of years old.
But what are these methods?
There are many, but I’ll classify them into two groups– radiometric and non-radiometric methods.
Radiometric
Radiometric dating is dependant on the idea of radioactive decay. It measures how the current proportions different elements in rocks differ from their initial ratios. For instance, Uranium-235 decays into Lead-207 at a fixed and measurable rate. Over time, we expect to have less uranium and more lead, and thus we can use the relative proportions of the two elements to determine the age of the earth (Dalrymple, 2001). This is the most common method of dating the age of the earth. Other methods of radiometric dating using different elements (such as lead and argon) still date the age of the earth to be between 4.5 billion to 4.7 billion years old (Dalrymple, 2004).
Non-radiometric
Although non-radiometric methods can not be estimate the age of the earth as far back as radiometric methods (they only can provide an lower limit; there is no upper limit due to limtiations in such methods), they still show that the earth is very old indeed.
One non-radiometric method involves studying ice cores, or rather the variational in snow layers caused by the seasons. The differences in snow layers that appear during winter, spring, summer and fall allows us to date the age of ice formations. The differences include (i) increased bubbles and larger crystals of summer ice compared to winter ice, (ii) dust deposited during summer, (iii) nitric acid concentrations (measured via electrical conductivity), (iv) chemical containments and (v) relative amonts of heavy hydrogen (deuterium) and heavy oxygen (oxygen-18) in ice. Two ice cores drilled in 1990s in Greenland were dated to have been formed 123, 000 years ago (Andersen et al., 2004).
Another interesting method I would like to cover in this post involves studying calcium carbonate deposits in marine invertebrates. Similar to the banding patterns in trees (or ice cores as I earlier covered), it is possible to date fossils of clams and corals by looking at the carbon carbonate banding patterns. I’ll attempt to summarise how is it done.
Astronomical data has revealed that the speed of the Earth’s rotation is decreasing. This is due to friction of the moving tides on the earth’s surface (which are produced by the sun’s and moon’s gravitational field). This implies that the length of each day is getting longer since the formation of the earth-moon system. The average increased in day length is estimated to be .23 milliseconds per century. This means 1000 years ago, a day would be .23 seconds shorter than than a day now. If a direct estimate of day length is possible, we can use such information to date material.
And it turns out that we can obtain an estimate of day length from clam and corals fossils. Consider a clam living at the seashore. When the tide is in, the clam is open and respires aerobically. This incorporates calcium carbonate in the shells. When the tide is out, the clam shuts and respires anaerobically. This decalcifies the shells. Such differing patterns of deposition patterns allows us estimate the day length of the time fossiled organisms were alive.
As it turns out, some fossiled clams show a deposition patterns of a 21-hour day length , indicating that the fossils were about 465 million years old. What was more fascinating was that radiometric dating of the shells confirms this result (within a 99 percent accuracy) (Zhenyu et al., 2007).
Conclusion
So how old is the earth? Very old indeed.
References
Andersen, K.K. et al. (2004) High-resolution record of Northern Hemisphere climate extending into the last interglacial period. Nature 2004, 147-151
Dalrymple, G.B. (2001) “The age of the Earth in the twentieth century: a problem (mostly) solved”. Special Publications, Geological Society of London 190, 205–221
Dalrymple, G.B. (2004). Ancient Earth, Ancient Skies: The Age of the Earth and Its Cosmic Surroundings.
Stephenson, F.R. (2003). Historical Eclipses and Earth’s Rotation. Astronomy and Geophysics 44, 2.22-2.27.
Zhenyu, Z., Yaoqi, Z., Guosheng, J. (2007). The periodic growth increments of biological shells and the orbital parameters of Earth-Moon system. Environmental Geology 51, 1271–1277.