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相关概念视频

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Membrane-enclosed structures called vesicles transport proteins and lipids across the cell. The vesicles derive their cargo from the plasma membrane, Golgi, ER, or endosome. Coated vesicles are spherical, protein-coated carriers with a 50–100 nm diameter that mediate bidirectional transport between the ER and the Golgi. The distribution of proteins between the ER and Golgi complex is dynamic and is maintained by different coated vesicles. Their formation is driven by the assembly of...
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Enzymes are proteins made of amino acids. The functional group of each constituent amino acid catalyzes a wide variety of chemical reactions via ionic interactions or acid-base reactions. However, amino acids cannot catalyze oxidation-reduction and group transfer reactions and need to be aided by non-protein components called cofactors. Cofactors are also referred to as the chemical teeth of an enzyme.
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Cohesion is the attraction between molecules of the same type, such as water molecules. Water molecules have an overall neutral charge but are polar molecule. An oxygen atom in one water molecule has a partial negative charge that can bind to a hydrogen atom with a partial positive charge in a second water molecule, forming a hydrogen bond. Each water molecule can form up to four hydrogen bonds with other water molecules. Hydrogen bonds are responsible for water's cohesive nature.
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Cohesin protein complexes are a molecular glue that holds two sister chromatids together. They play an important role both in mitosis and meiosis. In mitosis, all cohesin complexes present on the chromosomes are removed before the start of the anaphase stage.
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公司 CO CO CO CO

Yue He1, Yongwen Liu2, Lingjie Lei1

  • 1Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing, China.

Global change biology
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概括

二氧化碳施肥显著促进了森林生物质在北半球生态系统中的碳储存. 自20世纪90年代以来,这一过程占了生物质增加的一半以上,其中森林占比较高.

关键词:
在二氧化碳受精过程中.二氧化碳丰富试验的实验.碳循环循环的过程动态的全球植被模型.新兴的约束是限制.

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科学领域:

  • 生态生态学 生态生态学
  • 气候科学 气候科学
  • 生物地质化学生物地质化学

背景情况:

  • 北半球的极热带生态系统 (NHee) 是一个重要的碳汇,但驱动因素是不确定的.
  • 二氧化碳 (CO2) 施肥是增加陆地碳吸收的推测驱动因素.

研究的目的:

  • 孤立和量化二氧化碳施肥在森林生物质碳储存中的历史作用.
  • 将模型估计与观测数据进行比较,以限制二氧化碳受精效应.

主要方法:

  • 综合了24次二氧化碳丰富实验的数据.
  • 使用了10个动态全球植被模型 (DGVM) 的集合.
  • 采用了新兴约束技术和基于观察的生物质数据集 (库存,卫星).

主要成果:

  • 总干事们低估了森林中的二氧化碳施肥效应,但在历史上过度估计了草原中的二氧化碳施肥效应.
  • 对森林生物质 (β森林模态) 的受约束CO2施肥效应为0.86 ± 0.28 kg C m−2 [100 ppm]−1.1.
  • 自20世纪90年代以来,二氧化碳施肥占森林生物质碳储量增加的5464%.

结论:

  • 近几十年来,二氧化碳施肥一直是森林生物质碳汇的主要驱动因素.
  • 精确量化二氧化碳施肥对于理解森林C循环至关重要.
  • 这些发现支持森林在气候变化缓解政策中的作用.