绰墩遗址新石器时期水稻田、古水稻土剖面、植硅体和炭化稻形态特征的研究
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

基金项目:

* 国家自然科学基金重点项目“水稻土可持续利用机理研究”(40171056)资助


MORPHOLOGICAL CHARACTERISTICS OF PADDY FIELDS, PADDY SOIL PROFILE, PHYTOLITH AND FOSSIL RICE GRAIN OF THE NEOLITHIC AGE IN YANGTZE RIVER DELTA
Author:
Affiliation:

Fund Project:

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
  • |
  • 文章评论
    摘要:

    绰墩遗址第六次发掘的300m2范围内出土22块古田块,通过对其田埂、灌排系统(水口、水沟、水井)等结构特征的观察研究,对古田块和水沟中出土的灌溉用具——陶罐和陶盆碎片的鉴定是属于马家滨文化时期的器物;从田块表土层中淘洗出大量的炭化稻粒,每克土壤中检测到有上万至十余万颗水稻植硅体,这些结果证明所发现的田块是马家滨时期的灌溉稻田。对出土的炭化稻粒和土壤有机质的14C定年结果表明其年龄分别为5907aBP和6280aBP,是新石器即晚马家滨文化时期的水稻文明。对在遗址挖掘的两个整段剖面(P-01和P-03)的研究发现,P-01剖面上42~103cm层位埋藏有马桥文化-商朝初期(3320aBP)和在103~200cm层位埋藏有马家滨时期(6280aBP)的两个古水稻土剖面,这一结果佐证了前人关于8000年来长江三角洲地区曾有过几次大的洪水泛滥而使人类耕作活动中断的气候变化事件的结论。然而距P-01仅15m的P-03整段剖面上仅出现了马桥-商朝初期的古水稻土剖面(40~100cm),未发现马家滨时期古水稻土剖面(100~200cm),说明当时的生产力非常低下,仅能利用低洼平坦的地方种稻,稍高一点的居住点附近的坡地就无法改成梯田种植水稻了。这两个埋藏的古水稻土剖面均已经发育了水稻土的明显特征。对出土炭化稻粒的形态学研究表明,外型多为椭圆形,长宽比的变异较大,稃面有方格凹陷结构、周边有稃毛,顶端残留有稻芒的基部,基部有护颖而没有小梗,"钝形"的双峰乳突、浅平的凹陷乳沟等均显示其为人工栽培的粳型水稻。结果与丁颖20世纪50年代在黄河流域发现的汉代的炭化稻粒的特征是吻合的,从而支持了关于"我国长江流域与黄河流域古代最早栽培的水稻都是粳稻品种"的论点。

    Abstract:

    During the 6th excavation of Chuodun site (E120°50'41",N 31°24'07"),22 pieces of prehistoric farming lands were discovered within 300 m2,Each field was surrounded with bands in between,and ditches or water pools (wells) constructed for irrigation,and some pots wearers (belong to Majiabang culture periods) for water transfer from ditch to field were found in these ditches or fields;more.000 fossil rice grains were screened out,and about 10 to 60 thousands rice phytolith (opal) per gram soil were detected in these ancient lands,all facts above are strong proof indicating these small piece of ancient lands were irrigated paddy fields for rice cultivation by ancient human beings settled in this site.The age of these paddy fields were about 5 907 a BP to 6 280 a BP determined by 14C analysis.It is in Neolithic period and in agreement with Majiabang culture period identified by archaeological method.The small size of each field which only 0.4 m2 to 16 m2 and various shape etc.morphological characteristics were reflect the very low production capacity at that time.A soil monolith (P-01) was studied and described,results indicated that there were two buried paddy soil profile piled together.One is prehistoric paddy profile with age of 6 280 a BP (Majiabang cultural period) in the layer of 103~200 cm depth and the other was ancient paddy profile with age of 3 320 a BP (about Maqiao cultural periods to Early Shang dynasty period) in the layer of 42~103 cm depth.It proved that there were several times of flooding or sea water invade resulting to break off agricultural civilization.Another monolith (P-03) only 15 m apart from the above monolith (P-01),but it was not found the prehistoric paddy profile in the layer of 103~200 cm depth indicating early human beings settled in Chuodun site during that periods had no capacity to use hill land for rice planting yet,because of P-03 monolith was located at the foot of Chuodun hills,they had no technology to level it to construct terrace for rice planting,while the same buried paddy profile in the layer of 40~103 cm aged as Maqiao cultural period to Early Shang dynasty period was there same as in P-01.Both buried paddy soils have developed most of the typical characteristics of modern paddy soils.

    参考文献
    相似文献
    引证文献
引用本文

曹志洪,杨林章,林先贵,胡正义,董元华,章钢娅,陆彦椿,尹睿,吴艳宏,丁金龙,郑云飞.绰墩遗址新石器时期水稻田、古水稻土剖面、植硅体和炭化稻形态特征的研究[J].土壤学报,2007,44(5):838-847. DOI:10.11766/trxb200610110510 Cao Zhihong, Yang Linzhang, Lin Xiangui, Hu Zhengyi, Dong Yuanhua, Zhang Gangya, Lu Yanchun, Yin Rui, Wu Yanhong, Ding Jinlong, Zheng Yunfei. MORPHOLOGICAL CHARACTERISTICS OF PADDY FIELDS, PADDY SOIL PROFILE, PHYTOLITH AND FOSSIL RICE GRAIN OF THE NEOLITHIC AGE IN YANGTZE RIVER DELTA[J]. Acta Pedologica Sinica,2007,44(5):838-847.

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史
  • 收稿日期:2006-10-11
  • 最后修改日期:2007-02-08
  • 录用日期:
  • 在线发布日期: 2013-02-25
  • 出版日期: