View source for The Meghalayan Age

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[[Category:India |M ]]
[[Category:History |M ]]

=The background=
[https://epaper.timesgroup.com/Olive/ODN/TimesOfIndia/shared/ShowArticle.aspx?doc=TOIDEL%2F2018%2F07%2F23&entity=Ar01010&sk=3FB347A4&mode=text  How Meghalaya gave its name to 4,200 yrs of Earth’s age, July 23, 2018: ''The Times of India'']

[[File: How Meghalaya gave its name to 4,200 yrs of Earth’s age.jpg| How Meghalaya gave its name to 4,200 yrs of Earth’s age <br/> From: [https://epaper.timesgroup.com/Olive/ODN/TimesOfIndia/shared/ShowArticle.aspx?doc=TOIDEL%2F2018%2F07%2F23&entity=Ar01010&sk=3FB347A4&mode=text  How Meghalaya gave its name to 4,200 yrs of Earth’s age, July 23, 2018: ''The Times of India'']|frame|500px]]

Stalagmites on the floors of the Krem Mawmluh caves in Meghalaya provide evidence of a distinct stage in the geologic classification of Earth’s age, so say researchers who have termed this most current timespan in the planet’s 4.6 bnyear-old history the ‘Meghalayan Age’. These slices of time chart key events in the story of evolution of our planet and the life forms that occupy it.

''' What is geologic time? ''' 

The time recorded by written history charting important events of human civilisation is miniscule as compared to the overall history of the planet that is known as geologic time. The enumeration by geologists, palaeontologists, and other Earth scientists of geologic time units is done by the study of rock layers and the fossil forms trapped in that. Scientists determine the time when they were formed to understand Earth at that time. Broadly, each geologic timespan is divided into different units based on the occurrence in their duration of unique plants and animals as well as major evolutionary or extinction events. The longest unit of this geologic time scale is known as eon. Earth’s total age is divided into three formal and one informal eon.

''' How are the eons further subdivided? '''

The eon, a very large span of time, is subdivided into eras that are further broken down into periods. The periods are divided into epochs that are further divided into ages. These divisions are done by studying the rocks formed during these periods and the fossil forms trapped therein. The Phanerozoic Eon is divided into the Palaeozoic (541m to 252m years ago), Mesozoic (252m to 66m years ago), and Cenozoic (66m years ago to the present) eras, which are divided into twelve periods.

''' What is The Meghalayan Age? ''' 

Based on the difference between the animal and plant forms originating in them, geologic periods are further divided into series (epoch) that are again divided into stage/ages. The Quaternary period is divided into two series (epochs) — Pleistocene and Holocene. The Holocene series that covers approximately 11,700 years in Earth’s history is coincident with the late Stone Age. The Holocene series is divided into three stages of which the Meghalayan Age is the last. It starts at 4,200 years ago when agricultural societies around the world experienced an abrupt and critical mega-drought that resulted in the collapse of civilisations and prompted human migrations in Egypt, Greece, Syria, Palestine, Mesopotamia, the Indus Valley, and the Yangtze River Valley.


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[https://www.bbc.com/news/science-environment-44868527  Jonathan Amos, July 18, 2018: ''BBC'']
[[File: The famous timeline will be updated to reflect the new stages or ages, as they are called.jpg| The famous timeline will be updated to reflect the new "stages", or "ages", as they are called <br/> From: [https://www.bbc.com/news/science-environment-44868527  Jonathan Amos, July 18, 2018: ''BBC''] |frame|500px]]

[[File: A portion of an Indian stalagmite that defines the beginning of the Meghalayan Age.jpg|A portion of an Indian stalagmite that defines the beginning of the Meghalayan Age <br/> From: [https://www.bbc.com/news/science-environment-44868527  Jonathan Amos, July 18, 2018: ''BBC'']|frame|500px]]

The official history of Earth has a new chapter - and we are in it.

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.

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 six 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 the present. 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 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 the Palaeogene, 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 a perturbation in the types, or isotopes, of oxygen atoms present in the layers of a stalagmite growing from the floor of Mawmluh Cave in the northeastern state of Meghalaya in India. This two-step change is a consequence of weakening monsoon conditions.

"The isotopic shift reflects a 20-30% decrease in monsoon rainfall," explained Prof Mike Walker of the University of Wales, UK, who led the international team of Holocene scientists that developed the division proposal.

"The two most prominent shifts occur at about 4,300 and about 4,100 years before present, so the mid-point between the two would be 4,200 years before present, and this is the age that we attribute to the [Meghalayan golden spike]," he told BBC News.

''' Further changes to come? ''' 

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.

They are also concerned that the divisions have been approved when there is still an active debate about assigning a new geologic slice of time to reflect specifically the influence of humans on the planet.
Tentatively referred to as the Anthropocene, its precise definition - its beginning point and the spike used to denote its initiation - is the subject of ongoing research.

Mark Maslin is professor of geography at University College London, UK, and a key figure in the Anthropocene discussion.

He told BBC News: “After the original paper and going through various committees, they've suddenly announced [the Meghalayan] and stuck it on the diagram. It's official, we're in a new age; who knew? We have lots of new definitions that perhaps now contradict the Anthropocene Working Group and go against what most scientists perceive to be the most important change on Earth in the last 10,000 years.”

But Prof Walker moved to clarify the situation: "To be frank, I see absolutely no conflict at all between the new subdivisions that we have here and a future designation of the Anthropocene.

"These subdivisions of the Holocene are based entirely on physical (climatic/ environmental) evidence whereas any designation of the Anthropocene as a new unit within the geological timescale would rest entirely on evidence for human impact."