Qingyuan County, Zhejiang, China is recognized as a source of mushrooms around the world and as Mushroom City in China. Because of a favorable ecological environment and abundant forest resources, mushroom farmers in Qingyuan have engaged in mushroom production for 800 years and continued to form unique mushroom production systems where people and nature live in a harmonious way, and a rich and colorful mushroom culture. The Qingyuan Mushroom Culture System was named the Nationally Important Agricultural Heritage systems of China in 2014. Based on analysis of the importance of agricultural heritage and the necessity and urgency of protection, here we examine the agricultural heritage of the Qingyuan mushroom culture system as a research case study and comprehensively describe its heritage values, including supply materials and production, ecosystem services, cultural inheritance and multi-function agricultural development. These results provide reference values for agricultural heritage protection and inheritance of edible fungi in China, agricultural sustainable development and extension of agricultural function. 相似文献
A region of low sea surface temperature (SST) extends southward in the central part of southern South China Sea during boreal winter, which is called the South China Sea cold tongue (SCS CT). The present study investigates the factors of interannual variation of SST in the SCS CT region and explores the individual and combined impacts of El Niño-Southern Oscillation (ENSO) and East Asian winter monsoon (EAWM) on the SCS CT intensity. During years with ENSO alone or with co-existing ENSO and anomalous EAWM, shortwave radiation and ocean horizontal advection play major roles in the interannual variation of the SCS CT intensity. Ocean advection contributes largely to the SST change in the region southeast of Vietnam. In strong CT years with anomalous EAWM alone, surface wind-related latent heat flux has a major role and shortwave radiation is secondary to the EAWM-induced change of the SCS CT intensity, whereas the role of ocean horizontal advection is relatively small. The above differences in the roles of ocean advection and latent heat flux are associated with the distribution of low level wind anomalies. In anomalous CT years with ENSO, low level anomalous cyclone/anticyclone-related wind speed change leads to latent heat flux anomalies with effects opposite to shortwave radiation. In strong CT years with anomalous EAWM alone, surface wind-related latent heat flux anomalies are large as anomalous winds are aligned with climatological winds.
