{"title":"华东浙江沿海平原全新世断裂与新石器时代人类适应性研究","authors":"","doi":"10.1016/j.catena.2024.108340","DOIUrl":null,"url":null,"abstract":"<div><p>The Quaternary transgression had a significant impact on environmental changes and ancient human activities in eastern China. However, due to the lack of reliable core records, the history of the transgression and its impact on human activities along the eastern coast of Zhejiang Province remains unclear. Here, multi-proxy indicators including lithology, AMS<sup>14</sup>C dating, grain size, total organic carbon (TOC), total nitrogen (TN), elemental geochemistry, and microfossils in a new core (QTZ1) from the Wenzhou Coastal Plain (WCP) are employed to reconstruct sedimentary evolution, which experienced four phases as follows: (1) The terrestrial environment dominated by delta facies (before 11,700 cal a BP); (2) The marine-terrestrial transitional environment dominated by littoral facies (11,700–9,400 cal a BP); (3) The marine environment dominated by shallow marine facies (9,400–6,200 cal a BP), including the Holocene transgression maximum occurred during 8,400–7,400 cal a BP; (4) The marine-terrestrial transitional environment marked by littoral facies (after 6,200 cal a BP). A comparative analysis on the Holocene transgression intensity, as reconstructed by Sr/Ba in the WCP, and archaeological sites in the Ningshao Plain indicates that the ancestors gradually migrated to the eastern low-elevation plains and developed Neolithic rice cultivation after the transgression maximum. Our results sheds light on the correlation between the Holocene transgression, sedimentary evolution, and ancient human activities in Zhejiang Coastal Plain, providing valuable insights into Quaternary environmental changes and human adaptations in the eastern China.</p></div>","PeriodicalId":9801,"journal":{"name":"Catena","volume":null,"pages":null},"PeriodicalIF":5.4000,"publicationDate":"2024-08-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Holocene transgression and Neolithic human adaptations in the Zhejiang coastal Plain, East China\",\"authors\":\"\",\"doi\":\"10.1016/j.catena.2024.108340\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>The Quaternary transgression had a significant impact on environmental changes and ancient human activities in eastern China. However, due to the lack of reliable core records, the history of the transgression and its impact on human activities along the eastern coast of Zhejiang Province remains unclear. Here, multi-proxy indicators including lithology, AMS<sup>14</sup>C dating, grain size, total organic carbon (TOC), total nitrogen (TN), elemental geochemistry, and microfossils in a new core (QTZ1) from the Wenzhou Coastal Plain (WCP) are employed to reconstruct sedimentary evolution, which experienced four phases as follows: (1) The terrestrial environment dominated by delta facies (before 11,700 cal a BP); (2) The marine-terrestrial transitional environment dominated by littoral facies (11,700–9,400 cal a BP); (3) The marine environment dominated by shallow marine facies (9,400–6,200 cal a BP), including the Holocene transgression maximum occurred during 8,400–7,400 cal a BP; (4) The marine-terrestrial transitional environment marked by littoral facies (after 6,200 cal a BP). A comparative analysis on the Holocene transgression intensity, as reconstructed by Sr/Ba in the WCP, and archaeological sites in the Ningshao Plain indicates that the ancestors gradually migrated to the eastern low-elevation plains and developed Neolithic rice cultivation after the transgression maximum. Our results sheds light on the correlation between the Holocene transgression, sedimentary evolution, and ancient human activities in Zhejiang Coastal Plain, providing valuable insights into Quaternary environmental changes and human adaptations in the eastern China.</p></div>\",\"PeriodicalId\":9801,\"journal\":{\"name\":\"Catena\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":5.4000,\"publicationDate\":\"2024-08-29\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Catena\",\"FirstCategoryId\":\"97\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S034181622400537X\",\"RegionNum\":1,\"RegionCategory\":\"农林科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Catena","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S034181622400537X","RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
Holocene transgression and Neolithic human adaptations in the Zhejiang coastal Plain, East China
The Quaternary transgression had a significant impact on environmental changes and ancient human activities in eastern China. However, due to the lack of reliable core records, the history of the transgression and its impact on human activities along the eastern coast of Zhejiang Province remains unclear. Here, multi-proxy indicators including lithology, AMS14C dating, grain size, total organic carbon (TOC), total nitrogen (TN), elemental geochemistry, and microfossils in a new core (QTZ1) from the Wenzhou Coastal Plain (WCP) are employed to reconstruct sedimentary evolution, which experienced four phases as follows: (1) The terrestrial environment dominated by delta facies (before 11,700 cal a BP); (2) The marine-terrestrial transitional environment dominated by littoral facies (11,700–9,400 cal a BP); (3) The marine environment dominated by shallow marine facies (9,400–6,200 cal a BP), including the Holocene transgression maximum occurred during 8,400–7,400 cal a BP; (4) The marine-terrestrial transitional environment marked by littoral facies (after 6,200 cal a BP). A comparative analysis on the Holocene transgression intensity, as reconstructed by Sr/Ba in the WCP, and archaeological sites in the Ningshao Plain indicates that the ancestors gradually migrated to the eastern low-elevation plains and developed Neolithic rice cultivation after the transgression maximum. Our results sheds light on the correlation between the Holocene transgression, sedimentary evolution, and ancient human activities in Zhejiang Coastal Plain, providing valuable insights into Quaternary environmental changes and human adaptations in the eastern China.
期刊介绍:
Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment.
Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.