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在感染山药的胶孢炭疽菌中,降雨期间直接飞溅传播比间接传播和后续传播更为普遍。

Direct splash dispersal prevails over indirect and subsequent spread during rains in Colletotrichum gloeosporioides infecting yams.

作者信息

Penet Laurent, Guyader Sébastien, Pétro Dalila, Salles Michèle, Bussière François

机构信息

INRA, UR1321, ASTRO Agrosystèmes tropicaux, F-97170, Petit-Bourg (Guadeloupe), France.

出版信息

PLoS One. 2014 Dec 22;9(12):e115757. doi: 10.1371/journal.pone.0115757. eCollection 2014.

Abstract

Plant pathogens have evolved many dispersal mechanisms, using biotic or abiotic vectors or a combination of the two. Rain splash dispersal is known from a variety of fungi, and can be an efficient driver of crop epidemics, with infectious strains propagating rapidly among often genetically homogenous neighboring plants. Splashing is nevertheless a local dispersal process and spores taking the droplet ride seldom move farther than a few decimeters. In this study, we assessed rain splash dispersal of conidia of the yam anthracnose agent, Colletotrichum gloeosporioides, in an experimental setting using a rain simulator, with emphasis on the impact of soil contamination (i.e., effect of re-splashing events). Spores dispersed up to 50 cm from yam leaf inoculum sources, though with an exponential decrease with increasing distance. While few spores were dispersed via re-splash from spore-contaminated soil, the proportion deposited via this mechanism increased with increasing distance from the initial source. We found no soil contamination carryover from previous rains, suggesting that contamination via re-splashing from contaminated soils mainly occurred within single rains. We conclude that most dispersal occurs from direct splashing, with a weaker contribution of indirect dispersal via re-splash.

摘要

植物病原体已经进化出许多传播机制,利用生物或非生物载体,或两者结合。多种真菌都存在雨滴飞溅传播的情况,并且它可能是作物病害流行的一个有效驱动因素,感染性菌株在通常基因同质的相邻植物间迅速传播。然而,飞溅是一种局部传播过程,搭乘水滴的孢子很少能移动到超过几分米的距离。在本研究中,我们在实验环境中使用降雨模拟器评估了山药炭疽病菌(胶孢炭疽菌)分生孢子的雨滴飞溅传播情况,重点关注土壤污染的影响(即再次飞溅事件的影响)。孢子从山药叶片接种源传播的距离可达50厘米,不过随着距离增加呈指数下降。虽然很少有孢子通过受孢子污染土壤的再次飞溅传播,但通过这种机制沉积的比例随着与初始源距离的增加而增加。我们没有发现前次降雨遗留的土壤污染情况,这表明受污染土壤的再次飞溅造成的污染主要发生在单次降雨期间。我们得出结论,大多数传播是由直接飞溅引起的,通过再次飞溅的间接传播作用较弱。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7866/4274098/92d2fbb363c0/pone.0115757.g001.jpg

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