日本地球惑星科学連合2014年大会

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セッション記号 M (領域外・複数領域) » M-IS ジョイント

[M-IS34_2PM2] 全球環境変動解明の鍵: 南大洋・南極氷床

2014年5月2日(金) 16:15 〜 17:00 414 (4F)

コンビーナ:*野木 義史(国立極地研究所)、大島 慶一郎(北海道大学北海道大学低温科学研究所)、池原 実(高知大学海洋コア総合研究センター)、座長:大島 慶一郎(北海道大学低温科学研究所)、田村 岳史(国立極地研究所)

16:45 〜 17:00

[MIS34-10] 南極地質掘削「ANDRILL Coulman High Project」の紹介と日本の貢献

*菅沼 悠介1池原 実2須藤 斎3野木 義史1 (1.国立極地研究所、2.高知大学海洋コア研究センター、3.名古屋大学)

The Coulman High Project (CHP) proposes to recover two, high-quality, continuous drill-cores by drilling into Paleogene to lowest Miocene strata beneath the Ross Ice Shelf on the Coulman High in the Ross Embayment, Antarctica. The overarching objective is to establish a history of Cenozoic climate, tectonic and glacial changes in an ice-proximal setting to determine the sensitivity of Antarctica's ice sheets to a range of climatic and tectonic forcings. The sedimentary archives to be recovered in these two ~800-m drill holes will offer a window into the range of environments, ecosystems and tectonic events in the Ross Sea region as it stepped from the warm, high-CO2 Greenhouse world of the Eocene into the lower-CO2 and highly variable Icehouse climate of the Oligocene and early Miocene. Antarctica was the keystone in this global climate transition and hosted the growth of ice sheets that started major cryosphere influence on global systems. The sensitivity of the climate system to elevated levels of greenhouse gases, the strength of polar amplification, and the behavior of the AIS in a world warmer than today remain fundamental questions to be addressed by CHP's integrated data-climate modeling studies. These seek to reduce the large uncertainties in predictions of future ice-sheet dynamics and sea level, in part by testing models with ancient scenarios under conditions warmer than today. To improve predictions of long-term future climate and sea level, it is imperative to obtain geological records of past polar climates and ice sheets from time intervals when atmospheric CO2 was two to four times higher than present levels. Modern observations and instrumental records provide details regarding current and short-term change, but high-fidelity climate records that span previous periods characterized by higher-than-present CO2 are only available from the Earth's geological records.The Japanese ANDRILL consortium has decided to join the CHP. In this talk, we will introduce the scientific backgrounds, logistics, and schedule of this drilling project.