首页> 外文期刊>Geomorphology >Holocene geomorphological evolution and the Neolithic occupation in South Hangzhou Bay, China
【24h】

Holocene geomorphological evolution and the Neolithic occupation in South Hangzhou Bay, China

机译:全新世地貌演化与中国杭州湾南部新石器时代职业

获取原文
获取原文并翻译 | 示例
           

摘要

Well-known for its intensive land-sea interactions and the brilliant Neolithic Cultures, the South Hangzhou Bay (SHB) of eastern China has been the focus of early agricultural rise in adaptation to coastal environmental change. In this study, geological records from sediment cores were integrated with archaeological findings in SHB to establish the linkage between coastal geomorphological processes and Neolithic occupation since the Holocene. It showed that the Holocene geomorphological evolution of SHB was inherited from the south wing of the Late Pleistocene Qiantang incised valley. During ca.10,000-7600 cal yr BP, the paleo-incised valley was inundated and infilled by marine transgressive deposits, forming an estuary. Then coastal progradation started and gradually formed the periphery of SHB. Noticeably, freshwater wetlands firstly occurred at the apex of SHB, enabling foragers to settle down and fostering the Kuahuqiao Culture and rice exploitation (7800-7400 cal yr BP). In the semi-closed Yaojiang Valley (YJV), east of SHB, alluvial plain developed after 7800-7600 cal yr BP with coastal progradation, providing a habitat to favor the early arrivals and later became the centre of the Hemudu Culture (7000-5000 cal yr BP). Meanwhile, the Neolithic sites sporadically occurred off the YJV due to the existing inundation. The coastal progradation slowed down ca.5000-2500 cal yr BP, in association with decreased sedimentation rates. In the last 2500 years, the Shaoxing Plain and the Cixi Plain of SHB showed rapid progradation resulting from increasing sediment input and intensive reclamation. The diverse geomorphological processes of SHB were modulated by the combination of Holocene sea-level changes, sediment input and the inherited local topography. The Neolithic migrations were in phase with landscape transformations and gradual formation of coastal plain since the Mid-Holocene, facilitating the Neolithic subsistence transition from hunting-gathering to rice farming and fostering the brilliant Neolithic cultural sequence in SHB. (c) 2021 Elsevier B.V. All rights reserved.
机译:以其密集的陆海互动和辉煌的新石器时代文化而闻名,中国东部南杭州湾(SHB)一直是早期农业崛起适应沿海环境变革的重点。在本研究中,沉积物核心的地质记录与SHB的考古发现集成,以建立自全新世以来沿海地貌过程和新石器时代占用之间的联系。结果表明,SHB的全新世地貌演变是从晚熟的南翼的南翼切开谷的南部。在CA.10,000-7600 CAL YR BP期间,古成立的谷被淹没并被海洋海洋近灾沉积物浸入,形成河口。然后沿海寄生开始并逐渐形成了SHB的周边。明显的是,淡水湿地首先发生在SHB的顶点,使迫使制者安定下来并培养Kuahuqiao培养和水稻剥削(7800-7400 CAL YR BP)。在半封闭的雅江谷(YJV),SHB东部,冲积平原后7800-7600 CAL YR BP开发,沿海寄生,提供栖息地,以利于早期抵达,后来成为六祖文化的中心(7000-5000 CAL YR BP)。同时,由于现有的淹没,新石器时代的网站偶尔出现在YJV上。沿海途径减缓了CA.5000-2500 CAL YR BP,与降低沉降率下降。在过去的2500年里,Shaoxing Plain和SHB的CIXI平原显示出沉积物投入和密集填海的增加产生的快速促成。通过全新世海平变化,沉积物输入和遗传局部地形的组合调节SHB的各种地貌过程。新石器时代的迁移与自全新世以来沿海平原沿海平原的横向变换和逐步形成,促进了新石器时代的生存从狩猎聚集到稻米种植和培育SHB中的辉煌新石器时代文化序列。 (c)2021 elestvier b.v.保留所有权利。

著录项

  • 来源
    《Geomorphology》 |2021年第15期|107827.1-107827.14|共14页
  • 作者单位

    East China Normal Univ State Key Lab Estuarine & Coastal Res Shanghai 200241 Peoples R China;

    East China Normal Univ State Key Lab Estuarine & Coastal Res Shanghai 200241 Peoples R China;

    East China Normal Univ State Key Lab Estuarine & Coastal Res Shanghai 200241 Peoples R China;

    East China Normal Univ State Key Lab Estuarine & Coastal Res Shanghai 200241 Peoples R China;

    East China Normal Univ State Key Lab Estuarine & Coastal Res Shanghai 200241 Peoples R China;

    East China Normal Univ Sch Geog Sci Shanghai 200241 Peoples R China;

    East China Normal Univ State Key Lab Estuarine & Coastal Res Shanghai 200241 Peoples R China;

    East China Normal Univ State Key Lab Estuarine & Coastal Res Shanghai 200241 Peoples R China;

    East China Normal Univ State Key Lab Estuarine & Coastal Res Shanghai 200241 Peoples R China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Shoreline migration; Sea-level; Neolithic; Eastern China Coast; Human adaptation;

    机译:海岸线迁移;海平面;新石器时代;中国东部海岸;人类适应;

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号