Human activities, early farming and natural environment in the north-western Kanto Plain (Central Japan) during the Final Jomon–Early Kofun period (990 cal BCE–330 cal CE) inferred from palynological and archaeobotanical records

Christian Leipe , Franziska Kobe , Anna Schubert , Eiko Endo , Maya Yasui , Hirotaka Koshitsuka , Michiko Ono , Pavel E. Tarasov , Mayke Wagner
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Abstract

The emergence, spread and intensification of agriculture, the impact of early agriculture on the natural environment and the possible role of climate on subsistence economies and population dynamics are important research questions in Japanese geoarchaeology. New directly dated archaeobotanical records of the Middle Yayoi (390–200 cal BCE, 1σ error) and Early Kofun (210–330 cal CE) periods from the Ikegami archaeological site and a 1300-year palynological record from the nearby Morinji Marsh help address these questions in the Kanto Plain of Central Japan. The pollen record suggests that management of chestnut and horse-chestnut by Final Jomon people in the study region declined around 750 cal BCE. The microcharcoal record indicates that human-induced fire activity decreased after 990 cal BCE and reached a minimum 500 years later, which coincides with the hemispheric-scale Iron Age Cold Epoch and late Bond event 2. Increasing use of fire from ca. 500 cal BCE is contemporaneous with the earliest evidence of millet-rice cultivation from south-western Kanto and the Central Highlands. This and pollen-based indicators of crop cultivation around Morinji Marsh ca. 200 cal BCE are consistent with the 14C-dated arrival of the first full-scale rice farmers at Ikegami. Their food economy still had a noticeable wild plant component (e.g. beans, walnut, horse-chestnut and acorn), however, the archaeobotanical assemblages from the Early Kofun period show a higher focus on rice cultivation and no evidence of a wild plant component. Variations in the charcoal concentrations and archaeobotanical data from the study region help postulate three phases of farming intensification related to cultural diffusion and/or migration. These phases, dated to ca. 500–300, 300–100 cal BCE and 100 cal BCE–250 cal CE, correspond to the pottery typologically defined late Early–early Middle Yayoi, middle–late Middle Yayoi and Late Yayoi periods, respectively.
从古生物学和考古植物学记录中推断的最后绳文-早期甲文时期(公元前 990 卡-公元前 330 卡)关东平原(日本中部)西北部的人类活动、早期农耕和自然环境
农业的出现、传播和强化,早期农业对自然环境的影响,以及气候对生计经济和人口动态可能产生的作用,是日本地质考古学的重要研究课题。池上考古遗址出土的弥生中期(公元前 390-200 年,误差为 1σ)和甲文早期(公元前 210-330 年)直接测定年代的考古植物学新记录,以及附近森路沼泽 1300 年的古植物学记录,有助于解决日本中部关东平原的这些问题。花粉记录表明,研究地区的最终绳文人对栗树和七叶树的管理在公元前 750 年左右有所减少。微炭记录表明,人类引起的火灾活动在公元前 990 千年后有所减少,并在 500 年后达到最低点,这与半球规模的铁器时代冷纪和晚期邦德事件 2 相吻合。约公元前 500 卡以后,人类越来越多地使用火,这与关东西南部和中央高地最早的黍稻种植证据同时出现。这与约公元前 200 卡的森吉沼泽附近作物栽培的花粉指标相吻合,与池上第一批全面种植水稻的农民的 14C 年代到来相吻合。他们的食物经济中仍有明显的野生植物成分(如豆类、核桃、马栗和橡子),但早期甲分时期的考古植物组合显示,他们更注重水稻种植,而没有野生植物成分的证据。研究地区木炭浓度和考古植物学数据的变化有助于推测与文化传播和/或迁移有关的三个农耕强化阶段。这些阶段的年代分别约为公元前 500-300 年、公元前 300-100 年和公元前 100-250 年,与陶器类型学上定义的弥生早期晚期、弥生中期晚期和弥生晚期相对应。
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