Geologists have classified the last 4,200 years as being a distinct age in the story of our planet.
They are calling it the Meghalayan Age, the onset of which was marked by a mega-drought that crushed a number of civilisations worldwide.
The International Chronostratigraphic Chart, the famous diagram depicting the timeline for Earth's history (seen on many classroom walls) will be updated.
Image copyright IUGS
Image caption A portion of an Indian stalagmite that defines the beginning of the Meghalayan Age
It should be said, however, there is disquiet in the scientific community at the way the change has been introduced. Some researchers feel there has been insufficient discussion on the matter since the Meghalayan was first raised as an idea in a scholarly paper seven years ago.
Geologists divide up the 4.6-billion-year existence of Earth into slices of time.
Each slice corresponds to significant happenings - such as the break-up of continents, dramatic shifts in climate, and even the emergence of particular types of animals and plant life.
We currently live in what is called the Holocene Epoch, which reflects everything that has happened over the past 11,700 years - since a dramatic warming kicked us out of the last ice age. But the Holocene itself can be subdivided, according to the International Commission on Stratigraphy (ICS).
It is the official keeper of geologic time and it proposed three stages be introduced to denote the epoch's upper, middle and lower phases.
These all record major climate events. The Meghalayan, the youngest stage, runs from 4,200 years ago to 1950. It began with a destructive drought, whose effects lasted two centuries, and severely disrupted civilisations in Egypt, Greece, Syria, Palestine, Mesopotamia, the Indus Valley, and the Yangtze River Valley.
It was likely triggered by shifts in ocean and atmospheric circulation.
The Meghalayan Age is unique among the many intervals of the geologic timescale in that its beginning coincides with a global cultural event produced by a global climatic event, says Stanley Finney, professor of geological sciences at Long Beach State University and Secretary-General of the International Union of Geological Sciences (IUGS), which ratified the ICS proposal.
The middle phase of the Holocene will be referred to as the Northgrippian, and runs from 8,300 years ago up to the start of the Meghalayan. The onset for this age was an abrupt cooling, attributed to vast volumes of freshwater from melting glaciers in Canada running into the North Atlantic and disrupting ocean currents.
The oldest phase of the Holocene - the exit from the ice age - will be known as the Greenlandian.
To win a classification, a slice of geological time generally has to reflect something whose effects were were global in extent, and be associated with a rock or sediment type that is clear and unambiguous.
For the famous boundary 66 million years ago that marks the switch in period from the Cretaceous to Tertiary, this "golden spike" is represented by traces in sediments of the element iridium. This was spread across the planet in the debris scattered by the asteroid that wiped out the dinosaurs.
For the Meghalayan, the spike is epitomised in specific chemical signatures, the finest example of which can be seen in the layers of stalagmites on the floors of caves in the northeastern Indian state of Meghalaya.
Already the decision to discriminate ages within the Holocene has drawn fire from some scientists who believe the move is premature. They question whether some of the climate shifts used as anchors for the new ages were truly global in their impact.
