为了更好地理解闽江下游的连江县黄岐屿遗址的环境背景和考古年代,在已有AMS14C年代学研究的基础上,选择黄岐屿遗址的T2剖面进行年代学样品采样,在室内运用中颗粒石英的单片再生剂量法进行光释光年代学研究。结果表明:黄岐屿遗址地层的...为了更好地理解闽江下游的连江县黄岐屿遗址的环境背景和考古年代,在已有AMS14C年代学研究的基础上,选择黄岐屿遗址的T2剖面进行年代学样品采样,在室内运用中颗粒石英的单片再生剂量法进行光释光年代学研究。结果表明:黄岐屿遗址地层的OSL埋藏年龄范围为8.5±0.5-4.4±0.2 ka,属于早-中全新世阶段的沉积/文化地层。其中2019118样品的年龄为4.4±0.2 ka,属于昙石山文化,与AMS14C年龄相当;2019117样品年龄为5.7±0.3 ka,可能存在年龄的高估;2019119样品的年龄为8.5±0.5 ka,受采样环境的影响,该地层的OSL埋藏年龄可能指示遗址底界的最大年龄。对比黄岐屿遗址所在的福州盆地地貌和环境演化过程以及区域史前人类活动发现,该遗址对应6 500-4 000 a B P的大暖期气候和相对高海面时期,该时期福州盆地发育了众多的同时期的史前遗存,区域内产生了繁荣的昙石山文化和昙石山下层文化。新石器时代末期4.2-4.0 ka气候突变的冷事件、4 000-3 000 a B P太平洋两岸热带-亚热带地区的气候环境的急剧变化以及北方吴越文化的侵入可能是造成该遗址缺失后续文化遗存的原因。展开更多
Located on the southeast coast of China,Fujian is an important junction for the spread and migration of agriculture and populations from mainland Asia to Taiwan and the Island Southeast Asia.Research on the emergence ...Located on the southeast coast of China,Fujian is an important junction for the spread and migration of agriculture and populations from mainland Asia to Taiwan and the Island Southeast Asia.Research on the emergence of agriculture and its relationship with the regional environmental context is key to understanding the evolution of ancient human-land interactions in the coastal zone of China.This paper presents a detailed microfossil analysis of the Dapingding site,which is located in the lower reaches of the Min River on the southeast coast of China.We found a large number of phytoliths produced in rice stems and leaves from the cultural layers of this site,dated to 7,500 cal.a BP.In addition,we found rice husk impressions and rice phytoliths in the pottery sherds of these cultural layers.Among these phytoliths,rice bulliform phytoliths with≥9 fish-scale patterns indicating the degree of rice domestication,accounted for 44%.This percentage is much higher than the established standard for wild rice bulliform phytoliths with fish-scale patterns,suggesting that rice cultivation had already occurred on the southeast coast of China approximately 7,500 years ago.Subsequently,the starting time of agricultural activity on the southeast coast of China was pushed from 5,000 to 7,500 years ago.Comparing the regional history of sea level and coastline changes in the early to mid-Holocene,we suggest that the emergence of early rice cultivation in Southeast China was associated with high sea levels in the midHolocene and the last transgression in the Fuzhou Basin.The’Fuzhou Bay’,formed by the retreating coastline and transgression driven by high sea levels,may have provided a sea channel for the southward movement of northern rice farmers.展开更多
文摘为了更好地理解闽江下游的连江县黄岐屿遗址的环境背景和考古年代,在已有AMS14C年代学研究的基础上,选择黄岐屿遗址的T2剖面进行年代学样品采样,在室内运用中颗粒石英的单片再生剂量法进行光释光年代学研究。结果表明:黄岐屿遗址地层的OSL埋藏年龄范围为8.5±0.5-4.4±0.2 ka,属于早-中全新世阶段的沉积/文化地层。其中2019118样品的年龄为4.4±0.2 ka,属于昙石山文化,与AMS14C年龄相当;2019117样品年龄为5.7±0.3 ka,可能存在年龄的高估;2019119样品的年龄为8.5±0.5 ka,受采样环境的影响,该地层的OSL埋藏年龄可能指示遗址底界的最大年龄。对比黄岐屿遗址所在的福州盆地地貌和环境演化过程以及区域史前人类活动发现,该遗址对应6 500-4 000 a B P的大暖期气候和相对高海面时期,该时期福州盆地发育了众多的同时期的史前遗存,区域内产生了繁荣的昙石山文化和昙石山下层文化。新石器时代末期4.2-4.0 ka气候突变的冷事件、4 000-3 000 a B P太平洋两岸热带-亚热带地区的气候环境的急剧变化以及北方吴越文化的侵入可能是造成该遗址缺失后续文化遗存的原因。
基金supported by the National Natural Science Foundation of China(Grant Nos.42077407,T2192954 and 41771241)the Social Science Foundation of Fujian Province(Grant No.FJ2019B013)the Innovation Research Team Fund of Fujian Normal University(Grant No.IRTL1705)。
文摘Located on the southeast coast of China,Fujian is an important junction for the spread and migration of agriculture and populations from mainland Asia to Taiwan and the Island Southeast Asia.Research on the emergence of agriculture and its relationship with the regional environmental context is key to understanding the evolution of ancient human-land interactions in the coastal zone of China.This paper presents a detailed microfossil analysis of the Dapingding site,which is located in the lower reaches of the Min River on the southeast coast of China.We found a large number of phytoliths produced in rice stems and leaves from the cultural layers of this site,dated to 7,500 cal.a BP.In addition,we found rice husk impressions and rice phytoliths in the pottery sherds of these cultural layers.Among these phytoliths,rice bulliform phytoliths with≥9 fish-scale patterns indicating the degree of rice domestication,accounted for 44%.This percentage is much higher than the established standard for wild rice bulliform phytoliths with fish-scale patterns,suggesting that rice cultivation had already occurred on the southeast coast of China approximately 7,500 years ago.Subsequently,the starting time of agricultural activity on the southeast coast of China was pushed from 5,000 to 7,500 years ago.Comparing the regional history of sea level and coastline changes in the early to mid-Holocene,we suggest that the emergence of early rice cultivation in Southeast China was associated with high sea levels in the midHolocene and the last transgression in the Fuzhou Basin.The’Fuzhou Bay’,formed by the retreating coastline and transgression driven by high sea levels,may have provided a sea channel for the southward movement of northern rice farmers.
