These factors suggest, given the increasingly arid savanna ecology of the Grea­ter Indus Valley after ca. 4000 B.C., that this continued preference f… - Jim G. Shaffer

Pollen cores from Rajasthan seem to indicate that by the mid-third milennium BC, climatic conditions of the Indus Valley area became increasingly arid. Data from the Deccan region also suggests a similar circumstance there by the end of the second millennium BC. Additionally, and more directly devastating for the Indus Valley region, in the early second millennium BC, there was the capture of the Ghaggar-Hakra (or Saraswati) river system (then a focal point of human occupation) by adjacent rivers, with subsequent diversion of these waters eastwards. At the same time, there was increasing tectonic activity in Sindh and elsewhere. Combined, these geological changes meant major changes in the hydrology patterns of the region. These natural geologic processes had significant consequences for the food producing cultural groups throughout the greater Indus Valley area. Archaeological surveys have documented a cultural response to these environmental changes creating a “crisis” circumstance...

We reemphasize our earlier views, namely that scholars engaged in South Asian studies must describe emerging South Asia data objectively rather than perpetuate interpretations, now more than two centuries old, without regard to the data archaeologists have worked so hard to reveal.

Although the use of cattle as important cultural wealth declined in the first millennium B.C., their religious status remained high, or intensified, providing an im portant cultural link between the protohistoric and Early Historic Periods