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Updated: Jul 14, 2026

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The Preparation of Electrohydrodynamic Bridges from Polar Dielectric Liquids
Published on: September 30, 2014
チリ南部における最後の氷河期からホロセンの移行期である
K D Bennett1, S G Haberle, S H Lumley
1Quaternary Geology, Department of Earth Sciences, Uppsala University, Villavägen 16, S-752 36 Uppsala, Sweden. Keith.Bennett@geo.uu.se
まとめ
北大西洋におけるヤング・ドライアス冷却現象は,地球規模の現象ではなかった. チリ南部の新しい証拠は,この冷却は地域的であり,北大西洋地域のみに影響を与えたことを示しています.
科学分野:
- 古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは
- 四次科学とは四次科学である.
- 海洋学 海洋学とは
背景:
- 最後の氷河期の終焉により,北大西洋は著しく温暖化しました.
- この温暖化は,氷河活動が再開した時期であるヤング・ドライアス・クロノゾーン (YDC) によって中断された.
- YDCの冷却のグローバルまたは地域的な性質は,古気象学における重要な問題である.
研究 の 目的:
- ユング・ドライアスの冷却現象が世界的な現象であったか,北大西洋地域に限定されていたかを調査する.
- YDC中に南半球の古気候を再構築する.
主な方法:
- 年代,堆積物,古生態学的記録の分析.
- チリ南部の小湖から採取した堆積物分析.
主要な成果:
- チリ南部の堆積物記録は,若いドライアスのクロノゾーン中に冷却の証拠を示さない.
- これは,南太平洋の地表水域に重大な冷却が欠けていることを示しています.
結論:
- ユング・ドライアスの冷却現象は,地域的な現象であり,主に北大西洋に影響を与えた.
- この発見は,YDCに関するグローバルな説明に異議を唱え,北大西洋を中心としたメカニズムを支持している.
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