ケノゾイク全体で海洋プランクトンダイアトムの多様性の動態
Daniel L Rabosky1, Ulf Sorhannus
1Department of Ecology and Evolutionary Biology, Cornell University, Ithaca, New York 14853, USA. DLR32@cornell.edu
Nature
|January 9, 2009
まとめ
海洋の生産性にとって極めて重要な海洋ダイアトムは,エオセン・オリゴセンの境界で多様性のピークに達した. それ以来,その多様性は減少し,草原の拡大と競争に関する以前の仮説に異議を唱えました.
科学分野:
- マリン・パレオントロジー (海洋古生物学)
- 海洋学 海洋学 海洋学
- 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
背景:
- ダイアトムは海洋の主要植物プランクトンであり,海洋の一次生産性と炭素循環に不可欠です.
- ダイアトムの進化を理解することは,過去の大気中のCO2レベルと気候を理解する鍵です.
- 以前の仮説では,草原の拡大と植物プランクトンの競争がダイアトムの多様化を促したと示唆されていた.
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