The Last Glacial Maximum Microblades from Kashiwadai 1 in Hokkaido, Japan

Although microliths are regarded as small standardized tools for complex composite technology, it is still not fully understood whether this schematic understanding developed in Old World prehistory can apply to the Late Pleistocene microblades in northeastern Asia. Here, referring to the definition of the Old World microliths, we explore the morphometric traits of the Late Pleistocene microblades in northeast Asia through an examination of the laminar blank production technology from the Last Glacial Maximum (LGM) microblade assemblage recovered from the Kashiwadai 1 site in Hokkaido, northern Japan. Metric and nonmetric data obtained from numerous laminar blanks reveal that microblades are comparable to bladelets without backing, as defined in the Old World records. The core reduction sequence reconstructed from the refitted specimen reveals that microblades are produced from blade core gradually reduced by careful core preparations, best labeled as the integrated laminar technology conceptually related to post-LGM bifacial microblade core technologies.