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过剩碳驱动分配和植物-土壤相互作用。

Surplus Carbon Drives Allocation and Plant-Soil Interactions.

机构信息

Department of Forest and Conservation Sciences, University of British Columbia, 2424 Main Mall, Vancouver, BC, Canada V6T1Z4.

Department of Forest and Conservation Sciences, University of British Columbia, 2424 Main Mall, Vancouver, BC, Canada V6T1Z4.

出版信息

Trends Ecol Evol. 2020 Dec;35(12):1110-1118. doi: 10.1016/j.tree.2020.08.007. Epub 2020 Sep 11.

Abstract

Plant growth is usually constrained by the availability of nutrients, water, or temperature, rather than photosynthetic carbon (C) fixation. Under these conditions leaf growth is curtailed more than C fixation, and the surplus photosynthates are exported from the leaf. In plants limited by nitrogen (N) or phosphorus (P), photosynthates are converted into sugars and secondary metabolites. Some surplus C is translocated to roots and released as root exudates or transferred to root-associated microorganisms. Surplus C is also produced under low moisture availability, low temperature, and high atmospheric CO concentrations, with similar below-ground effects. Many interactions among above- and below-ground ecosystem components can be parsimoniously explained by the production, distribution, and release of surplus C under conditions that limit plant growth.

摘要

植物的生长通常受到养分、水或温度的限制,而不是光合作用碳(C)固定的限制。在这些条件下,叶片生长比 C 固定受到更大的限制,多余的光合产物从叶片中输出。在受到氮(N)或磷(P)限制的植物中,光合产物被转化为糖和次生代谢物。一些多余的 C 被转运到根部,并以根分泌物的形式释放出来,或者转移到与根相关的微生物中。在水分供应不足、低温和高大气 CO 浓度下也会产生多余的 C,其对地下的影响类似。在限制植物生长的条件下,通过对多余 C 的产生、分配和释放,可以简洁地解释地上和地下生态系统成分之间的许多相互作用。

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