まとめ
米国南西部の砂漠は,冬の降水量が減ったために8,000年前に森から砂漠へと変化した. この気候変動は,氷河の融解が気象パターンに影響したため,世界的な傾向に遅れをとった.
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
- 四季地質学 四季地質学
- エコロジー エコロジー エコロジー
背景:
- パックラットミッドンは,貴重な古生態学的記録を提供します.
- 米国南西部の砂漠は,四季期の終わりに重大な気候変動を経験した.
研究 の 目的:
- アメリカの南西部の砂漠で,過去の森のコミュニティを再建する.
- 植物のシフトのタイミングと原因を特定する.
主な方法:
- 29のパックラットミッドンの放射性炭素年代測定.
- 過去の植生を推論するために,ミッドン内の化石植物物質の分析.
主要な成果:
- 森林地帯のコミュニティは,南西の砂漠で1万年未満前に文書化されました.
- 砂漠や草原への同期的な移行は,およそ8,000年前にチワフアン,ソノラン,モハベの砂漠で起こった.
- 推論された原因: アレウト低地と冬の嵐の軌跡が北に移動し,降水量が減少した.
結論:
- 南西部の非梅雨気候への移行は,北半球と比較して遅かった.
- 大陸の氷河の融解は,大気循環パターンに影響を与え,南西部の気候に影響を与えた.
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