ネオプロテロゾーイク期のリン酸塩の巨大硫黄細菌の証拠
Jake V Bailey1, Samantha B Joye, Karen M Kalanetra
1Department of Earth Sciences, University of Southern California, Los Angeles, California 90089, USA. jvbailey@usc.edu
Nature
|December 22, 2006
まとめ
古代の動物の胚ではなく,巨大な硫黄細菌が,ネオプロテロゾーイクドウシャントウの微生物化石を説明するかもしれない. これらのバクテリアはまた,おそらくこれらの化石を保存するリン酸化を促進しました.
科学分野:
- パレオントロジー・パレオントロジー
- 微生物学 微生物学とは
- 地質化学 地質化学
背景:
- 最近の発見は,真空塩酸硫黄酸化細菌におけるインシット・フォスファティゼーションと還元性細胞分裂を強調しています.
- ネオプロテロゾイク期のドゥシャントゥオ群には,微生物化石が含まれており,その一部は,以前は初期のメタゾウ類の卵と胚として解釈されていた.
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