Plant-soil feedback across spatiotemporal scales from immediate effects to legacy

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60077344%3A_____%2F24%3A00585869" target="_blank" >RIV/60077344:_____/24:00585869 - isvavai.cz</a>

Alternative codes found

RIV/00216208:11310/24:10477344

Result on the web

<a href="https://www.sciencedirect.com/science/article/pii/S0038071723003516?via%3Dihub" target="_blank" >https://www.sciencedirect.com/science/article/pii/S0038071723003516?via%3Dihub</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.soilbio.2023.109289" target="_blank" >10.1016/j.soilbio.2023.109289</a>

Result language

angličtina

Original language name

Plant-soil feedback across spatiotemporal scales from immediate effects to legacy

Original language description

Plants and soil biota are important ecosystem engineers interacting via plant-soil feedback on large gradient of temporal scales from immediate interactions to long term legacy, which also operate on various spatial scales. Here I emphasize three major pathways of plant-soil feedbacks: i) the biota pathway, when plants affect soil biota, such as plant symbionts or antagonists, which affect plants, ii) the soil pathway, when plants affect soil environment, which then feedbacks to plants and finally iii) the biota-soil pathway, when plants affect soil biota, which then affect soil environment, which then effect plants. Living plant roots are major driver for biota pathway, which is more important for immediate effect, while litter largely supports the biota-soil pathway important for legacy effects. Many processes that have immediate effects, produce also small but more persistent changes in soil. Legacy is produced by accumulation of this small changes over time. This is supported by soil ability to preserve and accumulate, these small changes. Legacy also alternate outcome of immediate interactions between plants, soil and soil biota. The soil property changes, caused by legacy, happen either as slow gradual changes, or relatively fast, abrupt shifting between two steady states. In both cases, soil changes can reach tipping points, altering functioning of whole plant soil system. Apart from plants, also soil conditions or soil biota can be manipulated either intentionally (e.g. by land uses change, various agriculture, forestry or ecosystem restoration practices), or non-intentionally (e.g. biological invasion), which trigger changes in plant-soil-soil biota interactions as described above and cause immediate and legacy effects. Examples, presented in this review, suggest that legacy effect is particularly important in soils in early stages of pedogenesis or during response to or recovery after disturbance. Review highlight necessity studying plant soil feedback on all relevant spatiotemporal scales.

Czech name

—

Czech description

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Type

J_imp - Article in a specialist periodical, which is included in the Web of Science database

CEP classification

—

OECD FORD branch

40104 - Soil science

Project

Result was created during the realization of more than one project. More information in the Projects tab.

Continuities

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Publication year

2024

Confidentiality

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Name of the periodical

Soil Biology and Biochemistry

ISSN

0038-0717

e-ISSN

1879-3428

Volume of the periodical

189

Issue of the periodical within the volume

February

Country of publishing house

GB - UNITED KINGDOM

Number of pages

13

Pages from-to

109289

UT code for WoS article

001147920500001

EID of the result in the Scopus database

2-s2.0-85181678350