Department of Humanities, Culture and Socio-Ecological Dynamics Group (CaSEs), Universitat Pompeu Fabra, Barcelona, Spain.
Institució Catalana de Recerca i Estudis Avançats (ICREA), Barcelona, Spain.
PLoS One. 2022 Jul 11;17(7):e0268482. doi: 10.1371/journal.pone.0268482. eCollection 2022.
The emergence of Neolithic economies and their spread through Eurasia was one of the most crucial transitions of the Holocene, with different mechanisms of diffusion-demic, cultural-being proposed. While this phenomenon has been exhaustively studied in Europe, with repeated attempts to model the speed of Neolithic diffusion based on radiocarbon dates, much less attention has been devoted to the dispersal towards the East, and in particular to South Asia. The Neolithic in the latter region at least partly derived from southwest Asia, given the presence of "founder crops" such as wheat and barley. The process of their eastward diffusion, however, may have been significantly different to the westward dispersal, which was mainly due to demic diffusion, as local domesticates were already available and farming was already practiced in parts of South Asia. Here, we use radiocarbon dates specifically related to the spread of the southwest Asian Neolithic crops to model the speed of dispersal of this agricultural package towards South Asia. To assess potential geographical and environmental effects on the dispersal, we simulate different speeds depending on the biomes being crossed, employing a genetic algorithm to search for the values that most closely approach the radiocarbon dates. We find that the most important barrier to be crossed were the Zagros mountains, where the speed was lowest, possibly due to topography and climate. A large portion of the study area is dominated by deserts and shrublands, where the speed of advance, albeit closer to the range expected for demic diffusion, was lower than observed in Europe, which can also potentially be attributed to environmental constraints in the adaptation of the crops. Finally, a notable acceleration begins in the Indus valley, exceeding the range of demic diffusion in the tropical and subtropical environments east of the Indus. We propose that the latter is due to the rapid diffusion among populations already familiar with plant cultivation.
新石器时代经济的出现及其在欧亚大陆的传播是全新世最重要的转型之一,提出了扩散-疫病、文化-存在等不同的扩散机制。虽然这一现象在欧洲已经被深入研究,人们反复尝试根据放射性碳年代测定来模拟新石器时代扩散的速度,但对于向东方,特别是向南亚的扩散,关注较少。鉴于小麦和大麦等“创始作物”的存在,该地区的新石器时代文化至少部分源自西南亚。然而,它们向东扩散的过程可能与向西扩散有很大的不同,向西扩散主要是由于疫病扩散,因为当地已经有了家养动物,南亚部分地区已经在进行农业种植。在这里,我们使用与西南亚新石器时代作物传播有关的放射性碳年代来模拟这种农业包向南亚扩散的速度。为了评估对扩散的潜在地理和环境影响,我们根据所穿越的生物群落模拟不同的速度,采用遗传算法来寻找最接近放射性碳年代的数据值。我们发现,最重要的障碍是扎格罗斯山脉,那里的速度最低,可能是由于地形和气候的原因。研究区域的很大一部分被沙漠和灌木林所主导,尽管推进速度更接近疫病扩散的预期范围,但比欧洲观察到的速度要低,这也可能归因于适应作物的环境限制。最后,在印度河流域出现了显著的加速,超过了印度东部热带和亚热带环境中疫病扩散的范围。我们提出,后者是由于已经熟悉植物栽培的人群之间的快速扩散。