Pokharia Anil K, Agnihotri Rajesh, Sharma Shalini, Bajpai Sunil, Nath Jitendra, Kumaran R N, Negi Bipin Chandra
Birbal Sahni Institute of Palaeosciences, Lucknow, Uttar Pradesh, India.
Archaeological Survey of India, Vadodara, Gujarat, India.
PLoS One. 2017 Oct 6;12(10):e0185684. doi: 10.1371/journal.pone.0185684. eCollection 2017.
Archaeological sites hold important clues to complex climate-human relationships of the past. Human settlements in the peripheral zone of Indus culture (Gujarat, western India) are of considerable importance in the assessment of past monsoon-human-subsistence-culture relationships and their survival thresholds against climatic stress exerted by abrupt changes. During the mature phase of Harappan culture between ~4,600-3,900yrsBP, the ~4,100±100yrsBP time slice is widely recognized as one of the major, abrupt arid-events imprinted innumerous well-dated palaeo records. However, the veracity of this dry event has not been established from any archaeological site representing the Indus (Harappan) culture, and issues concerning timing, changes in subsistence pattern, and the likely causes of eventual abandonment (collapse) continue to be debated. Here we show a significant change in crop-pattern (from barley-wheat based agriculture to 'drought-resistant' millet-based crops) at ~4,200 yrs BP, based on abundant macrobotanical remains and C isotopes of soil organic matter (δ13CSOM) in an archaeological site at Khirsara, in the Gujarat state of western India. The crop-change appears to be intentional and was likely used as an adaptation measure in response to deteriorated monsoonal conditions. The ceramic and architectural remains of the site indicate that habitation survived and continued after the ~4,200yrsBP dry climatic phase, but with declined economic prosperity. Switching to millet-based crops initially helped inhabitants to avoid immediate collapse due to climatic stresses, but continued aridity and altered cropping pattern led to a decline in prosperity levels of inhabitants and eventual abandonment of the site at the end of the mature Harappan phase.
考古遗址为过去复杂的气候与人类关系提供了重要线索。印度河文化周边地区(古吉拉特邦,印度西部)的人类定居点对于评估过去季风、人类、生存与文化之间的关系以及它们在应对突然变化所带来的气候压力时的生存阈值具有相当重要的意义。在公元前约4600 - 3900年的哈拉帕文化成熟阶段,公元前约4100±100年的时间切片被广泛认为是众多年代测定良好的古记录中所记录的主要突发干旱事件之一。然而,这一干旱事件的真实性尚未在任何代表印度河(哈拉帕)文化的考古遗址中得到证实,关于其时间、生存模式的变化以及最终废弃(崩溃)的可能原因等问题仍在争论之中。在此,我们基于印度西部古吉拉特邦希尔萨拉一处考古遗址丰富的大植物遗存和土壤有机质的碳同位素(δ13CSOM),展示了公元前约4200年作物模式的显著变化(从以大麦 - 小麦为主的农业转变为以“抗旱”小米为主的作物)。作物变化似乎是有意为之,很可能是作为对季风条件恶化的一种适应措施。该遗址的陶瓷和建筑遗迹表明,在公元前约4200年的干旱气候阶段之后,居住地得以存续并延续,但经济繁荣程度有所下降。最初转向以小米为主的作物帮助居民避免了因气候压力而立即崩溃,但持续的干旱和作物模式的改变导致居民繁荣水平下降,最终在哈拉帕文化成熟阶段末期该遗址被废弃。