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基于特征的丛枝菌根真菌群落组装决定了土壤碳的形成和保持。

Trait-based assembly of arbuscular mycorrhizal fungal communities determines soil carbon formation and retention.

机构信息

Department of Natural Resource Sciences, McGill University, 21111 Lakeshore Road, Ste-Anne-de-Bellevue, QC, H9X 3V9, Canada.

Department of Biology, Algoma University, 1520 Queen St. East, Sault Ste. Marie, ON, P6A 2G4, Canada.

出版信息

New Phytol. 2023 Jul;239(1):311-324. doi: 10.1111/nph.18914. Epub 2023 May 10.

Abstract

Fungi are crucial for soil organic carbon (SOC) formation, especially for the more persistent mineral-associated organic C (MAOC) pool. Yet, evidence for this often overlooks arbuscular mycorrhizal fungi (AMF) communities and how their composition and traits impact SOC accumulation. We grew sudangrass with AMF communities representing different traits conserved at the family level: competitors, from the Gigasporaceae family; ruderals, from the Glomeraceae family; or both families combined. We labeled sudangrass with C-CO to assess AMF contributions to SOC, impacts on SOC priming, and fungal biomass persistence in MAOC. Single-family AMF communities decreased total SOC by 13.8%, likely due to fungal priming. Despite net SOC losses, all AMF communities contributed fungal C to soil but only the Glomeraceae community initially contributed to MAOC. After a month of decomposition, both the Glomeraceae and mixed-family communities contributed to MAOC formation. Plant phosphorus uptake, but not hyphal chemistry, was positively related to AMF soil C and MAOC accumulation. Arbuscular mycorrhizal fungi contribution to MAOC is dependent on the specific traits of the AMF community and related to phosphorus uptake. These findings provide insight into how variations in AMF community composition and traits, and thus processes like environmental filtering of AMF, may impact SOC accumulation.

摘要

真菌对于土壤有机碳(SOC)的形成至关重要,尤其是对于更持久的矿物结合有机碳(MAOC)库。然而,这方面的证据往往忽略了丛枝菌根真菌(AMF)群落,以及它们的组成和特征如何影响 SOC 的积累。我们用代表不同家族水平上保守特征的 AMF 群落来种植苏丹草:来自巨孢囊科的竞争者,来自球囊霉科的粗糙种,或两者结合。我们用 C-CO 标记苏丹草,以评估 AMF 对 SOC 的贡献、对 SOC 激发的影响,以及 MAOC 中真菌生物量的持久性。单一的 AMF 群落减少了 13.8%的总 SOC,这可能是由于真菌激发。尽管净 SOC 损失,所有 AMF 群落都将真菌 C 贡献给土壤,但只有球囊霉科群落最初贡献于 MAOC。在一个月的分解后,球囊霉科和混合家族群落都有助于 MAOC 的形成。植物磷吸收,而不是菌丝化学性质,与 AMF 土壤 C 和 MAOC 积累呈正相关。AMF 对 MAOC 的贡献取决于 AMF 群落的特定特征,与磷吸收有关。这些发现提供了深入了解 AMF 群落组成和特征的变化,以及像 AMF 的环境过滤这样的过程,如何影响 SOC 的积累。

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