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初始极端干旱和降水长期变化对温带草原植物生物量分配的影响

The Effects of an Initial Extreme Drought and Chronic Change in Precipitation on Plant Biomass Allocation in a Temperate Grassland.

作者信息

Vörös Amira Fatime, Mojzes Andrea, Cseresnyés Imre, Kalapos Tibor, Kertész Miklós, Könnyű Balázs, Ónodi Gábor, Kröel-Dulay György

机构信息

HUN-REN Centre for Ecological Research Institute of Ecology and Botany Vácrátót Hungary.

Doctoral School of Biology Institute of Biology, ELTE Eötvös Loránd University Budapest Hungary.

出版信息

Ecol Evol. 2025 Sep 10;15(9):e71625. doi: 10.1002/ece3.71625. eCollection 2025 Sep.

Abstract

Drying climate may strongly affect plant productivity and standing biomass and, thus, ecosystem carbon cycling. Whilst drought effects on grassland aboveground plant biomass (AGB) have been widely studied and are generally negative, reports on belowground plant biomass (BGB) are much fewer, and results are more variable. In a full factorial experiment in a temperate grassland, we studied the legacy effect of an initial extreme drought, conducted in 2014, and the effect of four levels of chronic precipitation change: water addition, ambient precipitation, moderate drought and severe drought between 2015 and 2018, on AGB, BGB and BGB/AGB in 2019. AGB was negatively affected by chronic drought and also by extreme drought within each level of chronic precipitation change except severe drought. Total BGB was not influenced by extreme drought but was negatively impacted by chronic severe drought. Responses were the strongest in the shallow soil layer (0-10 cm), where both extreme and chronic droughts decreased belowground biomass, and weak in the deep soil layer (10-20 cm). BGB/AGB was not altered by extreme drought but increased in chronic drought plots because the decrease of AGB was much greater than the decrease in BGB. Our results indicate that the legacy of previous extreme drought and chronic change in precipitation are both important in shaping biomass pools and allocation in grasslands, sometimes with interactive effects.

摘要

干旱气候可能会强烈影响植物生产力和现存生物量,进而影响生态系统的碳循环。虽然干旱对草原地上植物生物量(AGB)的影响已得到广泛研究,且总体呈负面影响,但关于地下植物生物量(BGB)的报道要少得多,且结果的变异性更大。在温带草原进行的一项全因子实验中,我们研究了2014年进行的初始极端干旱的遗留效应,以及2015年至2018年期间四种慢性降水变化水平(增水、自然降水、中度干旱和重度干旱)对2019年AGB、BGB和BGB/AGB的影响。除重度干旱外,在每个慢性降水变化水平内,AGB均受到慢性干旱以及极端干旱的负面影响。总BGB不受极端干旱影响,但受到慢性重度干旱的负面影响。在浅层土壤层(0 - 10厘米)中响应最为强烈,极端干旱和慢性干旱均降低了地下生物量,而在深层土壤层(10 - 20厘米)中影响较弱。BGB/AGB不受极端干旱影响,但在慢性干旱地块中增加,因为AGB的减少幅度远大于BGB的减少幅度。我们的结果表明,先前极端干旱的遗留效应和降水的慢性变化在塑造草原生物量库和分配方面都很重要,有时还会产生交互作用。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d196/12422408/02f7a74ce6ae/ECE3-15-e71625-g004.jpg

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