Archaeological analysis of a section of ancient rice fields at Tianluoshan for diatoms, seeds and phytoliths has shown that the highest local sea level in eastern China during the Holocene appeared before 7.0 ka BP. Entering the Mid-Holocene, as seawater regressed, a vast wetland plain appeared in the coastal area, where farmers of the Neolithic Hemudu culture cultivated rice. However, there were still several sea-level fluctuations in the Mid-Holocene, of which the biggest were from 6.4 to 6.3 ka BP and from 4.6 to 2.1 ka BP. In addition, in the period dominated by wetland grass vegetation, 6.3 to 4.6 ka BP, smaller fluctuations apparently pushed the coastline back on to the land. Even though the sea-level rises associated with these shoreline transgressions did not have the intensity of the highest sea level period, there still would have been profound impacts on the lives and production activities of people living in the region. Archaeological evidence from ancient rice fields at Tianluoshan shows that larger sea-level rise events pushed seawater onto the land and inundated large areas of rice fields, whereas weaker sea-level rise events resulted in the intrusion of seawater along rivers, causing an increase in soil salinity and a decrease in rice yields. The impact of sea-level rise on rice cultivation caused changes in local diet. In regions where rice production fell, the prevalence of gathering and hunting rose. High sea levels in the early Holocene imply that the origin of rice cultivation in the eastern coastal plain is likely to have been in small nearby mountain basins. At the end of the last glacial period (dated from 18 to 15 ka BP), as continental ice sheets quickly ablated and global sea levels rose, the gradual transition to the Holocene (post glacial) epoch occurred with a series of climatic fluctuations. Significant sea-level rise happened in the early Holocene, although there are many opinions on the magnitude, process, and rate of sea-level rise [1]. Relatively rapid sea-level rise continued until 7.5 ka BP, after which there was a general falling trend in the rate of sea-level change; however, fluctuations continued [2]. Most coastal areas in China have records of transgressions caused by sea-level rise in the Holocene. However, there are some local differences in the recognition of peak transgressions and the process of regressions because of regional differences in geological structures, paleotopography and depositional patterns from rivers and ocean currents [3]. For example, in the lower regions of the Yangtze River, the peak of transgression appeared between 7.5 and 7.0 ka BP, during which time the vertices of the estuary advanced to the areas between Zhenjiang and Yangzhou. Since then, the rate of sea-level rise has decreased and the rate of river deposition has increased resulting in the infilling of the huge estuary with a great deal of sediments, and the development of a delta [4,5]. The improved ecology of the delta provided suitable environments for lush vegetation and a rich faun...