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Did Climate Change Cause the Demise of the Ancient Indus Valley Civilization?

The Indus civilization was the largest—but least known—of the first great urban cultures that also included Egypt and Mesopotamia. Named for one of their largest cities, the Harappans relied on river floods to fuel their agricultural surpluses. Today, numerous remains of the Harappan settlements are found in a vast desert region far from any flowing river.

Creation of the Harappan Culture

More than 4,000 years ago, the Harappan culture thrived in the Indus River Valley of what is now modern Pakistan and northwestern India, where they built sophisticated cities, invented sewage systems that predated ancient Rome's, and engaged in long-distance trade with settlements in Mesopotamia. Yet by 1800 BC this advanced culture had abandoned their cities, moving instead to smaller villages in the Himalayan foothills. A new study from the Woods Hole Oceanographic Institution (WHOI) has found evidence that climate change likely drove the Harappans to resettle far away from the floodplains of the Indus.

Sophisticated water reservoir, evidence for hydraulic sewage systems in the ancient Indus Valley Civilization.  (Rama's Arrow / CC-BY-SA 3.0)

Sophisticated water reservoir, evidence for hydraulic sewage systems in the ancient Indus Valley Civilization.  (Rama's Arrow / CC-BY-SA 3.0 )

A Shift in Weather Changed Everything

Beginning in roughly 2500 BC, a shift in temperatures and weather patterns over the Indus valley caused summer monsoon rains to gradually dry up, making agriculture difficult or impossible near Harappan cities, says Liviu Giosan, a geologist at WHOI and lead author on the paper that was published November 13, 2018, in the journal Climate of the Past .

"Although fickle summer monsoons made agriculture difficult along the Indus, up in the foothills, moisture and rain would come more regularly," Giosan says. "As winter storms from the Mediterranean hit the Himalayas, they created rain on the Pakistan side, and fed little streams there. Compared to the floods from monsoons that the Harappans were used to seeing in the Indus, it would have been relatively little water, but at least it would have been reliable."

Remains of the Harappan settlements. (Liviu Giosan et al/ CC BY SA 4.0)

Remains of the Harappan settlements. ( Liviu Giosan et al/ CC BY SA 4.0 )

Evidence for this shift in seasonal rainfall - and the Harappans switch from relying on Indus floods to rains near the Himalaya to water crops - is difficult to find in soil samples. That's why Giosan and his team focused on sediments from the ocean floor off Pakistan's coast. After taking core samples at several sites in the Arabian Sea, he and his group examined the shells of single-celled plankton called foraminifera (or "forams") that they found in the sediments, helping them understand which ones thrived in the summer, and which in winter.

The miliolid foraminiferan Quinqueloculina from the North Sea. (CC BY-SA 4.0)

The miliolid foraminiferan Quinqueloculina from the North Sea. ( CC BY-SA 4.0 )

Evidence Leads to Deeper Clues on Climate

Once he and the team identified the season based on the forams' fossil remains, they were able to then focus on deeper clues to the region's climate: paleo-DNA, fragments of ancient genetic material preserved in the sediments.

"The seafloor near the mouth of the Indus is a very low-oxygen environment, so whatever grows and dies in the water is very well preserved in the sediment," says Giosan. "You can basically get fragments of DNA of nearly anything that's lived there.”

During winter monsoons, he notes, strong winds bring nutrients from the deeper ocean to the surface, feeding a surge in plant and animal life. Likewise, weaker winds at other times of year provide fewer nutrients, causing slightly less productivity in the waters offshore.

"The value of this approach is that it gives you a picture of the past biodiversity that you'd miss by relying on skeletal remains or a fossil record. And because we can sequence billions of DNA molecules in parallel, it gives a very high-resolution picture of how the ecosystem changed over time," adds William Orsi, paleontologist and geobiologist at Ludwig Maximilian University of Munich, who collaborated with Giosan on the work.

Sure enough, based on evidence from the DNA, the pair found that winter monsoons seemed to become stronger - and summer monsoons weaker - towards the later years of the Harappan civilization, corresponding with the move from cities to villages.

Mohenjo-daro is an ancient Indus Valley Civilization city built around 2500 BC that was abandoned after 1900 BC. (suronin / Adobe)

Mohenjo-daro is an ancient Indus Valley Civilization city built around 2500 BC that was abandoned after 1900 BC. (suronin / Adobe)

End to an Urban Life - A Civilization on the Move

"We don't know whether Harappan caravans moved toward the foothills in a matter of months or this massive migration took place over centuries. What we do know is that when it concluded, their urban way of life ended," Giosan says.

The rains in the foothills seem to have been enough to hold the rural Harappans over for the next millennium, but even those would eventually dry up, contributing to their ultimate demise.

Early and Late Harappan Sites. (Liviu Giosan et al/ CC BY SA 4.0)

Early and Late Harappan Sites. ( Liviu Giosan et al/ CC BY SA 4.0 )

"We can't say that they disappeared entirely due to climate - at the same time, the Indo-Aryan culture was arriving in the region with Iron Age tools and horses and carts. But it's very likely that the winter monsoon played a role," Giosan says.

The big surprise of the research, Giosan notes, is how far-flung the roots of that climate change may have been. At the time, a "new ice age" was settling in, forcing colder air down from the Arctic into the Atlantic and northern Europe. That in turn pushed storms down into the Mediterranean, leading to an upswing in winter monsoons over the Indus valley.

What Lessons Can Be Learned from the Past?

"It's remarkable, and there's a powerful lesson for today," he notes. "If you look at Syria and Africa, the migration out of those areas has some roots in climate change. This is just the beginning - sea level rise due to climate change can lead to huge migrations from low lying regions like Bangladesh, or from hurricane-prone regions in the southern U.S. Back then, the Harappans could cope with change by moving, but today, you will run into all sorts of borders. Political and social convulsions can then follow."

Also collaborating on the study was Ann G. Dunlea, Samuel E. Munoz, Jeffrey. P. Donnelly, and Valier Galy of WHOI; William D. Orsi of Ludwig-Maximilians-Universität MuÌnchen; Marco Coolen and Cornelia Wuchter of Curtin University in Australia; Kaustubh Thirumalai of Brown University; Peter D. Clift of Louisiana State University; and Dorian Q. Fuller of University College, London.

The work was supported by the National Science Foundation's Division of Ocean Sciences and internal WHOI funds.

Top image: Indus Valley Source: RealityImages / Adobe

The article, originally titled ‘ Climate change likely caused migration, demise of ancient Indus Valley civilization’ was first published on Science Daily.

Source: Woods Hole Oceanographic Institution. "Climate change likely caused migration, demise of ancient Indus Valley civilization." ScienceDaily. ScienceDaily, 14 November 2018. www.sciencedaily.com/releases/2018/11/181114234855.htm

References

Liviu Giosan, William D. Orsi, Marco Coolen, Cornelia Wuchter, Ann G. Dunlea, Kaustubh Thirumalai, Samuel E. Munoz, Peter D. Clift, Jeffrey P. Donnelly, Valier Galy, Dorian Q. Fuller. Neoglacial climate anomalies and the Harappan metamorphosis . Climate of the Past , 2018; 14 (11): 1669 DOI: 10.5194/cp-14-1669-2018

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