| 英文摘要 |
Kuo-yeh A is a representative site of the early Neolithic Period in Penghu Islands. Based on the study of pottery sherds excavated in 1984, there are two types of pottery identified by the characteristics of rim form, fabric, and decoration. The result of thin-section petrographic analysis reveals that these two types of pottery are different in paste and corresponding provenances respectively. Type I, the majority in the assemblage, consists mainly of reddish-brown quartz-tempered jars with an everted short rim. Some are decorated in red paint. A few basalt-related components in the paste demonstrate its local relationship in basaltic rocks that dominate in the islands. However, the considerable granite-related components imply that the clay is sourced from the outcrops of unconsolidated Miocene granite-derived clastic sedimentary stratum. As the shell-tempered pottery mentioned in Lin et al. (2022), this quartz-tempered pottery is another type of local product in prehistoric Penghu. The examples of Type II, the orange fine-paste pottery, are relatively few in number and consist mainly of jars with an everted thick or beveled rim. This pottery type is marked by the common occurrence of incised parallel lines on rims, but no colored paint has been observed. The few coarse sandstone grains in the paste suggest that the pottery was made in southwestern Taiwan and then imported to here. Additionally, a single grayish-brown sandstone-tempered rim of a jar decorated with tooth-imprints on the lip is also considered product imported from southwestern Taiwan. Based on these records, we suggest that the Early Neolithic population in Penghu and southwestern Taiwan tapped into local resources to manufacture pottery objects of distinct forms and styles. A large number of pottery and basaltic tools made in Penghu were sent to southwestern Taiwan in that period while a few pottery vessels produced in Taiwan were transported to Penghu. These exchanges, though unequal in volume, evidence bilateral transportation of objects between the two regions during the early Neolithic period. |