パリノロジックおよびイリジウム異常は白期と三次期の境界,サスカチュワンの南中部にある
まとめ
クレータ紀と三次紀の境界のイベントは,イリジウムとフェルンの胞子スパイクによって特徴づけられた植物生活に重大な混乱を引き起こしました. 生き残った種が再編成され,事象以前の気候状態に急速に戻ったことを示しています.
科学分野:
- パレオントロジー・パレオントロジー
- 地質学 地質学 地質学
- パレオボタニーは古植物学です.
背景:
- クレータ紀-三次紀 (K-T) の境界線は,重要な絶滅の出来事を示しています.
- このイベントに対する地上の生態系の反応を理解することは極めて重要です.
研究 の 目的:
- サスカチュワン州中南部におけるK-T境界イベントが陸生植物に与える影響を調査する.
- K-T境界を越えた植物種の豊富さと多様性の変化を分析する.
主な方法:
- 化石の花粉と胞子集合体の分析.
- イリジウムの異常を特定する.
- アンジオスペルマ種の絶滅率の評価.
主要な成果:
- 偶発的なイリジウムとフェルネスポロの豊富さの異常は,K-T境界にある.
- クレタ紀のアンジオスペルム種の最大30%の局所的な絶滅.
- 生き残った種が優勢で,最古の三次元の植物の再編成.
結論:
- K-Tイベントは,陸上の植物コミュニティに重大な混乱を引き起こしました.
- 花の再編成は,イベント後の古気候条件の急速な回復を示唆しています.
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