初期の陸上の植物によって強制された岩岩の進化
William J McMahon1, Neil S Davies2
1Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK.
まとめ
陸上の植物は 泥の量を劇的に増やしました この研究は,植生が進化した後,泥岩の割合が急増し,地球の歴史と気候に影響を与えたことを示しています.
科学分野:
- 地理科学
- 古生物学
- 堆積物学
背景:
- 泥岩は地球の歴史の重要なアーカイブであり 海の化学と気候に影響を与えます
- 泥岩の形成を理解することは 過去の環境を再現するための鍵です
研究 の 目的:
- 陸上の植物の進化と陸上に残された泥の割合との関連を調査する.
- 地球の歴史を通して 泥岩の堆積の変化を 定量化するために
主な方法:
- 古代から炭鉱期にわたる704の流層構造からの層図データ分析.
- 陸上の植物の進化前と後の堆積物における泥岩の比率の比較
主要な成果:
- 陸上植物が進化した後に,陸上に残された泥の割合が大きく増加した.
- この泥岩の波はオルドヴィキウス・シルウリアン時代に始まった.
- 植生後のアルルービウムには,平均して,植生前のアルルービウムよりも1.4倍の大きさの泥岩が含まれています.
結論:
- 植物の進化は,大陸からの泥の生産と沈殿物の流れを根本的に変えました.
- この泥岩の堆積の変化は 海洋化学と気候の規制に 長期的な影響を及ぼしました
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