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From the Cover: Starch grain evidence for the preceramic dispersals of maize and root crops into tropical dry and humid forests of Panama

机译:从封面开始:淀粉粒证据表明玉米和块根作物在陶瓷的前期扩散到巴拿马的热带干燥和潮湿森林中

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摘要

The Central American isthmus was a major dispersal route for plant taxa originally brought under cultivation in the domestication centers of southern Mexico and northern South America. Recently developed methodologies in the archaeological and biological sciences are providing increasing amounts of data regarding the timing and nature of these dispersals and the associated transition to food production in various regions. One of these methodologies, starch grain analysis, recovers identifiable microfossils of economic plants directly off the stone tools used to process them. We report on new starch grain evidence from Panama demonstrating the early spread of three important New World cultigens: maize (Zea mays), manioc (Manihot esculenta), and arrowroot (Maranta arundinacea). Maize starch recovered from stone tools at a site located in the Pacific lowlands of central Panama confirms previous archaeobotanical evidence for the use of maize there by 7800–7000 cal BP. Starch evidence from preceramic sites in the less seasonal, humid premontane forests of Chiriquí province, western Panama, shows that maize and root crops were present by 7400–5600 cal BP, several millennia earlier than previously documented. Several local starchy resources, including Zamia and Dioscorea spp., were also used. The data from both regions suggest that crop dispersals took place via diffusion or exchange of plant germplasm rather than movement of human populations practicing agriculture.
机译:中美洲地峡是最初在墨西哥南部和南美北部的驯化中心种植的植物类群的主要传播途径。考古和生物科学领域最近开发的方法论正在提供越来越多的数据,这些数据涉及这些扩散的时间和性质以及各个地区向食品生产的相关过渡。这些方法之一是淀粉颗粒分析,可直接从用于加工经济植物的石器中回收可识别的经济植物微化石。我们从巴拿马报道了新的淀粉粒证据,证明了三个重要的新世界品种的早期传播:玉米(Zea mays),木薯粉(Manihot esculenta)和葛粉(Maranta arundinacea)。在巴拿马中部太平洋低地的一个工地上,从石器中回收的玉米淀粉证实了先前的考古学证据表明,到7800–7000 cal BP,那里的玉米使用量很高。巴拿马西部奇里基省(CiriquíProvince)季节性较差,湿润的山前森林的陶瓷前体部位的淀粉证据表明,到7400-5600 cal BP时,玉米和块根作物存在,比先前记录的早了几千年。还使用了一些本地淀粉资源,包括Zamia和Dioscorea spp.。来自这两个地区的数据表明,农作物的扩散是通过植物种质的扩散或交换而不是通过从事农业活动的人口的流动来实现的。

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