[en] A sample of carbonized fallen tree piece (Picea or Pinus; diameter 5 cm and length 15 cm) was discovered in a crop in the Noboribetsu pumice flow deposit, where fossil-rootless fumaroles had been found recently. It existed in the loam layer immediately above the Satsunai pumice bed covering the Noboribetsu formation and the fumaroles below it. Its ¹⁴C age was determined to be 11,330 +- 320 Y.B.P. Though the distribution and eruption source of Satsunai pumice bed are still unknown, the ¹⁴C age has significance as follows in the Quaternary chronology. (1) The Satsunai pumice bed is important as a pumice bed indicating the boundary between the pleistocene and the Recent epoch. (2) By means of the Satsunai pumice bed, the age of upper Noboribetsu formation is given. (3) As there is no high bench deposit on the Noboribetsu pumice flow deposit, the time gap may be small between the Satsunai pumice bed and the Noboribetsu formation below it. (J.P.N.)