Digging into Jerusalem’s history
Developed in the 1940s, radiocarbon dating works by measuring radiocarbon (carbon-14, or 14C) in a given object. Radiocarbon is constantly being produced in the atmosphere and becomes part of the carbon cycle. These atoms are absorbed into the tissue of organic matter such as plants, animals and people – but when that living organism dies, it stops absorbing radiocarbon. The 14C undergoes radioactive decay, turning into nitrogen-14. Since radiocarbon has a known rate of decay, researchers can use the number of remaining 14C atoms to determine something’s age.
Going to the excavation sites in Jerusalem, Boaretto, with Dr. Johanna Regev, was able to carry out more than 100 radiocarbon measurements on organic material, mostly charred seeds.
“We have to be able not only to collect material like seeds, bones or charcoal from the site, but to identify the context, such as where the seeds were burnt,” Boaretto says. “We achieve this with the methods we have developed over the years, using analytical instruments that we have at Weizmann and also bring with us to the field. In this manner, we can go beyond the standard archaeological analysis of the site.”
After that, the researchers separated the original material from contaminants and carried out multiple radiocarbon measurements at Weizmann’s Dangoor Research Accelerator Mass Spectrometry (D-REAMS) Laboratory in order to get the highest level of accuracy and precision in dating.
“We have an understanding of how the site was formed, so when we collect seeds or mortar samples related to the site, we can be confident that these were there when the site was built, which means we can date the site itself from that,” she explains.
Overcoming the Hallstatt plateau was also made possible with the help of 100 calendar-dated tree rings obtained from well-known archives. Tree-ring dating, also known as dendrochronology, is built on the fact that a tree will grow a ring every year until its death. The more rings a tree has, the older it is. Combining this with the radiocarbon method, researchers were able to obtain a more precise and detailed determination of the radiocarbon concentration in the atmosphere during the period of interest, which also helped create an absolute chronology. This study was made possible by an experiment set up by Dr. Lior Regev at D-REAMS, Weizmann’s dedicated accelerator for research.
The existence of two historical events that occurred at well-established dates – the 586 BCE destruction of Jerusalem by the Babylonians, and the 8th century BCE earthquake and subsequent widespread reconstruction efforts – helped provide further insights into the radiocarbon behavior in the atmosphere. The researchers noticed differences between the radiocarbon in the material in the region compared to the measured concentration in European and American tree rings from the same time. These differences – when the radiocarbon data don’t match what we know they should be thanks to the tree rings – are known as “offsets,” and understanding them can be of fundamental importance for scientists studying the climate and atmosphere, as well as for archaeological chronologies.