A PRELIMINARY STUDY OF ICE CORE CHRONOLOGY AT DOME FUJI STATION, ANTARCTICA

A 112.59m-deep ice core was drilled at Dome Fuji Station by a JARE-34 party in 1993 when a pilot hole was prepared for a deep core drilling operation. A preliminary examination was made for ice core chronology by two signals : one electric conductivity peaks measured in the home laboratory and the o...

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Bibliographic Details
Main Authors: ワタナベ オキツグ, フジイ ヨシユキ, モトヤマ ヒデアキ, フルカワ テルオ, ショウジ ヒトシ, エノモト ヒロユキ, カメダ タカオ, ナリタ ヒデキ, ナルセ レンジ, ホンドウ タケオ, フジタ シュウジ, マエ シンジ, アズマ ノブヒコ, コバヤシ シュンイチ, ナカオ マサヨシ, アゲタ ユタカ, Okitsugu WATANABE, Yoshiyuki FUJII, Hideaki MOTOYAMA, Teruo FURUKAWA, Hitoshi SHOJI, Hiroyuki ENOMOTO, Takao KAMEDA, Hideki NARITA, Renji NARUSE, Takeo HONDOH, Shuji FUJITA, Shinji MAE, Nobuhiko AZUMA, Shun'ichi KOBAYASHI, Masayoshi NAKAWO, Yutaka AGETA
Format: Report
Language:English
Published: National Institute of Polar Research 1997
Subjects:
Byrd
Byrd Camp
Dome Fuji
Dome Fuji Station
Antarc*
Antarctica
ice core
Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3965
http://id.nii.ac.jp/1291/00003965/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3965&item_no=1&attribute_id=18&file_no=1
Description
Summary:A 112.59m-deep ice core was drilled at Dome Fuji Station by a JARE-34 party in 1993 when a pilot hole was prepared for a deep core drilling operation. A preliminary examination was made for ice core chronology by two signals : one electric conductivity peaks measured in the home laboratory and the other field observation results obtained by JARE-36 party on the deeper part of the core. The electric conductivity peak analyses suggest the same 5 volcanic eruptions, in 1464 AD, 1259 AD, 865 AD, 639 AD and 346 BC, reported for the ice core of Byrd Camp, Antarctica. Field observations for ECM and crystal size distributions suggest that the period 374m depth level corresponds to the end of Wisconsin ice period. The results suggest that accumulation rate at Dome Fuji Station is between 2.5 and 3.0cm of water equivalent/year, and the end of Wisconsin-Holocene Transition will be found between depths of 340 and 400m. The depth-age curves for the core at Dome Fuji Station are obtained from the surface (at present) to 400m (at 12000years BP).

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