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土壤真菌菌丝具有出人意料的灵活化学计量 C:N 和 C:P 比。

Soil fungal mycelia have unexpectedly flexible stoichiometric C:N and C:P ratios.

机构信息

Institute of Biology, Freie Universität Berlin, Altensteinstr. 6, Berlin, 14195, Germany.

Berlin-Brandenburg Institute of Advanced Biodiversity Research (BBIB), Berlin, 14195, Germany.

出版信息

Ecol Lett. 2021 Feb;24(2):208-218. doi: 10.1111/ele.13632. Epub 2020 Nov 9.

Abstract

Soil ecological stoichiometry provides powerful theories to integrate the complex interplay of element cycling and microbial communities into biogeochemical models. One essential assumption is that microbes maintain stable C:N:P (carbon:nitrogen:phosphorus) ratios independent of resource supply, although such homeostatic regulations have rarely been assessed in individual microorganisms. Here, we report an unexpected high flexibility in C:N and C:P values of saprobic fungi along nutrient supply gradients, overall ranging between 7-126 and 20-1488, respectively, questioning microbial homeostasis. Fungal N:P varied comparatively less due to simultaneous reductions in mycelial N and P contents. As a mechanism, internal recycling processes during mycelial growth and an overall reduced N and P uptake appear more relevant than element storage. The relationships among fungal stoichiometry and growth disappeared in more complex media. These findings affect our interpretation of stoichiometric imbalances among microbes and soils and are highly relevant for developing microbial soil organic carbon and nitrogen models.

摘要

土壤生态化学计量学为整合元素循环和微生物群落的复杂相互作用提供了强大的理论基础,将其纳入生物地球化学模型中。一个基本假设是,微生物在资源供应方面保持稳定的 C:N:P(碳:氮:磷)比率,尽管这种体内平衡调节在单个微生物中很少被评估。在这里,我们报告了沿养分供应梯度的腐生真菌的 C:N 和 C:P 值具有出人意料的高灵活性,分别在 7-126 和 20-1488 之间变化,这对微生物的体内平衡提出了质疑。由于菌丝体 N 和 P 含量同时减少,真菌 N:P 的变化相对较小。作为一种机制,菌丝体生长过程中的内部再循环过程以及整体减少的 N 和 P 吸收似乎比元素储存更为重要。在更复杂的培养基中,真菌化学计量与生长之间的关系消失了。这些发现影响了我们对微生物和土壤之间化学计量失衡的解释,对开发微生物土壤有机碳和氮模型具有重要意义。

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