ペルミア 熱帯 低地 の 植物 の 進化 の 隠し 台所
Patrick Blomenkemper1, Hans Kerp1, Abdalla Abu Hamad2
1Palaeobotany Research Group, Institute of Geology and Palaeontology, University of Münster, Münster, Germany.
まとめ
ヨルダンで発見された化石は 古代の熱帯植物の起源を示しています これらの発見は,最も古い針葉樹一族を含む主要な種子植物系統の初期の進化に光を当てています.
科学分野:
- 古植物学
- 進化生物学
- 地質史
背景:
- 緯度生物多様性グラデーションは,地球の地質史に根ざした進化的起源を持っています.
- 海洋化石の記録は 低緯度地域が多くの動物集団の 息地であることを示しています
- 陸上の化石記録は特に 乾燥した環境から 革新を促すものは稀です
研究 の 目的:
- 熱帯の生息地における現代の植物群の初期の進化的起源を調査する.
- ペルミア紀の赤道低地からの地上の化石記録を 調べるため
主な方法:
- ヨルダンのペルミア期鉱床からの混合植物化石の分析
- 初期の種植物の系統と その進化的意義の特定
主要な成果:
- ペルミア紀の赤道低地における 3つの主要な種子植物の初期の記録の発見
- 生存中のコニファー族の最も古い代表者の特定
- 乱れやすい熱帯の生息地での初期の植物群の進化の証拠
結論:
- ペルミアの赤道低地では 陸上の生物の進化の歴史について 重要な洞察が得られます
- この発見は,生物多様性の緯度グラデントの深い根源を理解するのに役立ちます.
- 発見された化石は,メソゾイク時代に支配的な植物群の起源を垣間見ることができます.
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