从3500万年前到现在的微生物地毯中的碳固定模型
L J Rothschild1, R L Mancinelli
1Solar System Exploration Branch, NASA-Ames Research Center, Moffett Field, California 94035, USA.
Nature
|June 21, 1990
概括
早期生活 早期生活
科学领域:
- 古生物学的古生物学
- 生态生态学 生态生态学
- 地质化学 地质化学
背景情况:
- 生物碳固定对全球碳循环和生态至关重要.
- 斯特罗马托石,化石微生物地毯,记录了从3.5亿年前开始的早期碳固定,并且在原生态时代非常丰富.
- 斯特罗马托石的丰度下降,可能是由于掠食,竞争或环境变化.
研究的目的:
- 研究大气中的二氧化碳 (CO2) 水平对古代微生物地毯中的生物碳固定率的影响.
- 探索碳限制在前坎布里亚时代 stromatolites 的衰退中的作用.
主要方法:
- 利用现代微生物地毯作为古代 stromatolites 的类似物.
- 在不同的大气二氧化碳度下比较碳固定率,模拟过去的条件.
主要成果:
- 在大气二氧化碳水平升高的情况下,碳固定率更高,这是早期地球的特征.
- 微生物碳固定在早期的前剑桥时期可能没有受到碳限制.
- 碳固定变得有限,因为在前剑桥纪末期,无机碳供应减少.
结论:
- 减少的二氧化碳可用性可能有助于 stromatolites 的减少.
- 大气二氧化碳水平的变化显著影响了早期的生物碳固定和微生物生态系统.
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