@article{oai:nipr.repo.nii.ac.jp:00005339,
 author = {ササキ, ヒロシ and スズキ, ヒデカツ and タカヤマ, マコト and スズキ, コウジ and ハンダ, ノブヒコ and クドウ, サカエ and フクチ, ミツオ and SASAKI, Hiroshi and SUZUKI, Hidekatsu and TAKAYAMA, Makoto and SUZUKI, Koji and HANDA, Nobuhiko and KUDOH, Sakae and FUKUCHI, Mitsuo},
 journal = {Proceedings of the NIPR Symposium on Polar Biology},
 month = {Feb},
 note = {P(論文), Time-series sediment traps were deployed at depths of 537 m, 796 m, 1259 m, 1722 m and 2727 m at ice edge of the Antarctic Ocean (64°42'S, 139°58'E) from 26 December 1994 to 20 January 1995. During a short period from 7 to 9 January, a sporadic flux increase within a few days in terms of total dry weight of 774 mg m^<-2>d^<-1> at 537 m was observed. The mass of sinking particles forming the flux maximum sank down to the deepest trap (2727 m) within 7-11 days, indicating that about 5% of these particles were transported downward to the bottom with the sinking rate of 199-313 m d^<-1> (mean 243 m d^<-1>). The considerable particle loss rate (13% [100 m]^<-1>) below the mesopelagic layers in a short period suggests the occurrence of consumption processes induced by the sporadic supply of freshly produced particles from above.},
 pages = {50--55},
 title = {SPORADIC INCREASE OF PARTICLE SEDIMENTATION AT THE ICE EDGE OF THE ANTARCTIC OCEAN DURING THE AUSTRAL SUMMER 1994-1995 (18th Symposium on Polar Biology)},
 volume = {10},
 year = {1997}
}