Swaveda

The Barley of Kunal: What Early Harappan Stratigraphy and Micro-Botanical Remains Reveal About Pre-Indus Agriculture

A detailed look at stratified layers at Kunal in Haryana challenges the idea of a sudden agricultural shift, showing localized transitions that predate the regional integration of the Indus Valley.

Rohan Bhattacharya for SwavedaSeptember 28, 2026

Photo: Dev Jadiya, CC BY-SA 4.0, via Wikimedia Commons (https://commons.wikimedia.org/wiki/File%3AUdayagiri_and_Khandagiri_Caves_2024_8.jpg)
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The search for the origins of the Indus Valley Civilization often focuses on the dramatic transition from village to city. In the standard timeline, the early phases of sites in the Ghaggar-Hakra basin are treated as simple precursors to the urban planning of Harappa and Mohenjo-daro. However, a closer look at the micro-stratigraphy—the analysis of very thin, sequential layers of soil and debris—at Kunal in the Fatehabad district of Haryana tells a different story. The evidence from this small settlement shows that sophisticated agricultural strategies were already well-developed long before the first baked-brick cities appeared.

Excavations conducted by the Haryana State Department of Archaeology and Museums, alongside the Archaeological Survey of India (ASI), have revealed a continuous sequence of occupation. The site is particularly famous for its early phase, often classified as Pre-Harappan or Regional Hakra Ware culture. Rather than a primitive camp, the stratigraphy of Kunal reveals a highly organized sequence of pit dwellings, semi-subterranean houses, and above-ground mud-brick structures. It is within these micro-stratified layers, particularly the successive floors of the earliest pits, that archaeologists recovered charred botanical remains. These remains challenge the idea that complex farming was a late development.

The Stratigraphy of the Kunal Pits

The earliest occupation at Kunal, termed Period I-A, consists of round pits dug into the natural soil. These pits are not uniform. They show clear evidence of plastering with organic-rich clay, a technique used to keep the interiors dry and structurally sound. Inside these pits, researchers found mud-brick hearths. In reports published in Puratattva (the journal of the Indian Archaeological Society), excavators noted that the ash and charcoal layers within these hearths were not single-use deposits. Instead, they consist of multiple thin, micro-stratified lenses of burnt material, fine windblown dust, and plastered floors.

This sequence indicates long-term, seasonal reuse of the same cooking and processing installations. For the field archaeologist, these thin layers are crucial. They show that the settlement was occupied continuously over generations, rather than being a temporary site.

In subsequent occupational levels (Period I-B), the pit dwellings were lined with molded mud-bricks. By Period II, the pits were filled in, and the inhabitants constructed rectangular, above-ground mud-brick houses on the leveled surface. By tracking this sequence, archaeologists can link specific changes in crop use directly to the evolving architectural layout of the site.

Micro-Botanical Remains and the Barley Signature

The primary evidence for Pre-Harappan agricultural practices at Kunal comes from flotation samples, a laboratory technique where soil is mixed with water to float light carbonized organic material to the surface for recovery. Archaeobotanists K. S. Saraswat and Anil K. Pokharia published their comprehensive findings in a landmark 2003 paper in the journal Pragdhara per Pragdhara.

Their analysis of the charred material from the earliest pit levels identified a massive abundance of six-row barley (Hordeum vulgare), along with wheat, field pea (Pisum arvense), lentil (Lens culinaris), and grass pea (Lathyrus sativus). Interestingly, the barley found at Kunal was highly developed. It was not a wild ancestor, but a fully domesticated variety. The sheer volume of charred barley grains in the early hearth residues indicates that barley was the dietary staple of the community.

This early crop package is significant because of its ecological specificity. Six-row barley is highly drought-tolerant and can cope with salinity. In the dry, seasonal environment of Pre-Harappan Haryana, growing winter (rabi, crops harvested in spring) crops like barley and lentils required careful management of soil moisture. The presence of weed seeds commonly associated with cultivated fields further confirms that these crops were grown locally in managed plots, rather than being traded from elsewhere.

⚖ Scholarly Debate: Chronology and Dating Disputes of the Ghaggar Plain

Establishing the absolute chronology of Kunal has been a subject of intense debate in Indian archaeology, often played out in the pages of Man and Environment (the journal of the Indian Society for Prehistoric and Quaternary Studies).

Traditionally, scholars have placed the Early Harappan phase in Haryana within a framework of roughly 3300–2600 BCE. However, radiocarbon (C-14) dates obtained from charcoal and charred seeds in the deepest pit-dwelling levels of Kunal have yielded much older ages. Some of these determinations push the occupational timeline back to 5700–6000 BCE.

This massive divergence has split archaeological consensus into two distinct chronological frameworks:

  • The High Chronology (5700–5000 BCE): Proponents of this timeline argue that the radiocarbon dates from the deepest stratified layers of Kunal are accurate. If correct, this framework means that the agricultural and semi-sedentary lifestyle in the Ghaggar-Hakra basin began several millennia earlier than previously believed. It would position the regional Hakra phase as contemporary with, or even older than, the early occupational layers at Mehrgarh in Baluchistan.

  • The Low/Standard Chronology (3300–2600 BCE): Skeptics of the extreme early dates argue that these determinations are anomalous. Critics pointing to the "old wood effect"—where inner rings of long-lived trees yield radiocarbon dates centuries older than the context of their use—suggest the charcoal samples have skewed the results. They argue that the material culture at Kunal, such as the pottery types and metal artifacts, aligns typologically with a late fourth-millennium BCE horizon. They maintain that a sudden push of over two thousand years requires much broader stratigraphic verification across the region.

Even when applying the more conservative low chronology, the early levels of Kunal place the developed barley-processing culture several centuries before the urban transition of the Mature Harappan phase. This timeline refutes the old theory that complex double-cropping—growing both winter (rabi) and summer (kharif, crops harvested in autumn) crops—was a sudden innovation triggered by the administrative demands of the larger Indus cities. Instead, evidence shows that the agricultural transition was gradual and highly localized.

Local Adaptations Predating the Indus Integration

What the stratigraphy of Kunal ultimately shows is that the agricultural foundations of the region were built on slow, localized adaptations to the semi-arid environment. Before the administrative integration of the Mature Harappan period, the early inhabitants of Kunal were already selecting crop varieties that suited their specific micro-climate.

The transition from pit dwellings to mud-brick homes matches a steady, uninterrupted reliance on winter crops like barley. Rather than an agricultural revolution imposed from above, the complex farming systems of the Indus Valley Civilisation were simply the regional integration of strategies that had already been refined for generations in villages like Kunal.

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