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Co-occurrence of entomopathogenic nematodes and earthworms enhances enduring biocontrol activity and microbial diversity in a naturalized plant-soil system

Author: Chelkha, Maryam,Blanco-Pérez, Rubén,Labarga, David,de Toro, María,Dueñas-Hernani, Jorge,Wickings, Kyle,Campos-Herrera, Raquel
Publisher: Elsevier
Year: 2025
DOI: http://dx.doi.org/10.13039/501100000780
Source: https://digital.csic.es/bitstream/10261/376134/1/Chelkha_BiologicalControl_2025_Co-occurrence.pdf
Pe spec i e
Co-occu ence o en omopa hogenic nema odes and ea hwo ms enhances
endu ing biocon ol ac i i y and mic obial di e si y in a na u alized
plan -soil sys em
Ma yam Chelkha
a,b
, Rub´
en Blanco-P´
e ez
c
, Da id Laba ga
b
, Ma ía de To o
d
,
Jo ge Due˜
nas-He nani
b
, Kyle Wickings
a
, Raquel Campos-He e a
b,*
a
Depa men o En omology, Co nell Uni e si y, Co nell Ag iTech, 15 Cas le C eek D i e, Gene a 14456, NY, USA
b
Depa men o Vi icul u e, Ins i u o de Ciencias de la Vid y del Vino (ICVV, CSIC-Gobie no de La Rioja-Uni e sidad de La Rioja), Finca La G aje a, Log o˜
no 26007,
Spain
c
Soils, Biosys ems, and Ag o o es y Ecology Depa men , Misi´
on Biol´
ogica de Galicia (BMG-CSIC), Pon e ed a 36143, Spain
d
Genomics &Bioin o ma ics Co e Facili y, Cen e o Biomedical Resea ch o La Rioja (CIBIR), Log o˜
no 26006, Spain
HIGHLIGHTS GRAPHICAL ABSTRACT
•En omopa hogenic nema odes (EPNs)
and ea hwo ms (EW) in e ac ion poo ly
s udied.
•Adding EPN +EWs o EPN +cu aneous
exc e a (CEx) can modula e plan -soil
bio a sys em.
•EPN i ulence was highe in EWs and
CEx soils han in con ol a e 30 days.
•Bac e ial alpha di e si y was highe in
EPN o EPN +EW/CEx soils a e 30
days.
•Time e ealed o modula e he EPN +
EW/CEx in e ac ions in plan -soil
sys ems.
ARTICLE INFO
Keywo ds:
Eisenia e ida
Mic obiome
High h oughpu sequencing
Solanum lycope sicum
S eine nema el iae
Sus ainable ag icul u e
ABSTRACT
Soil ecosys ems hos di e se mic oo ganisms and auna essen ial o e es ial p ocesses, wi h ea hwo ms (EWs)
and en omopa hogenic nema odes (EPNs) playing c ucial oles. EWs enhance soil heal h by imp o ing ae a ion,
po osi y, and nu ien cycling, while EPNs, such as S eine nema and He e o habdi is, manage pes s by killing
insec s. This s udy aimed o assess he impac o EWs and hei de i a i es (cu aneous exc e a, CEx), alone o
combined wi h EPNs, on soil–plan dynamics, hypo hesizing ha hei co-occu ence would al e soil p ope ies,
bac e ial communi ies, EPN i ulence, and plan pe o mance. Using oma o plan s and ield soil, he s udy
in es iga ed di e en ea men s: con ol, EW (Eisenia e ida), EPN (S eine nema el iae), CEx, and combina ions o
EPN-EW and EPN-CEx, a wo and ou weeks pos -applica ion. Assessmen s included plan g ow h, EPN
in ec i i y, soil p ope ies, and bac e ial p o iling ia 16S RNA gene sequencing. Resul s showed no signi ican
impac on plan g ow h. Howe e , EPN i ulence dec eased a e 30 days when applied alone bu was main-
ained o enhanced when combined wi h EW o CEx. Combined applica ions o EPNs and CEx educed Mg and Ca
* Co esponding au ho .
E-mail add ess: [email p o ec ed] (R. Campos-He e a).
Con en s lis s a ailable a ScienceDi ec
Biological Con ol
jou nal homepage: www.else ie .com/loca e/ybcon
h ps://doi.o g/10.1016/j.biocon ol.2024.105685
Recei ed 26 Oc obe 2024; Recei ed in e ised o m 19 Decembe 2024; Accep ed 23 Decembe 2024
Biological Con ol 200 (2025) 105685
A ailable online 26 Decembe 2024
1049-9644/© 2024 The Au ho (s). Published by Else ie Inc. This is an open access a icle unde he CC BY-NC license (
h p://c ea i ecommons.o g/licenses/by-
nc/4.0/ ).
con en s, while o ganic ma e inc eased in he EPN-EW ea men . Bac e ial communi y changes we e obse ed
30 days pos -inocula ion, wi h inc eased alpha di e si y in co-applica ions o EPNs and EWs. The co-applica ion
o EPNs and EWs esul ed in bene icial impac s on soil p ope ies, EPN i ulence, and bac e ial di e si y. Timing
pos -inocula ion was c ucial in assessing hese e ec s, only de ec ing hose changes a e 30 days, sugges ing he
need o u he ex ended esea ch o unde s and he du a ion o hese changes. This s udy highligh s he
in ica e in e ac ions be ween EWs, EPNs, and plan -soil sys ems, emphasizing hei po en ial impac on plan
g ow h, soil nu ien dynamics, and soil o ganisms, highligh ing he impo ance o iming in e alua ing hese
in e ac ions.
1. In oduc ion
Soil, a non- enewable esou ce, is home o a signi ican po ion o he
Ea h’s biodi e si y (Wall, 2012; Fe ei a e al., 2022). I s inhabi an s,
including a chaea, bac e ia, oomyce es, ungi, nema odes, mi es,
sp ing ails, ea hwo ms, snails, e eb a es, and mo e, in e ac o p o-
ide essen ial ecosys em unc ions (Wall, 2012; Delgado-Baque izo
e al., 2020). These unc ions include main aining soil s uc u e, egu-
la ing hyd ological p ocesses, and decomposing o ganic ma e , di ec ly
impac ing nu ien cycles (Wall, 2012; Delgado-Baque izo e al., 2020).
Fu he mo e, om an ag icul u al s andpoin , soil biodi e si y plays a
c ucial ole in p omo ing plan g ow h and aiding in pes and disease
con ol by p o iding mechanisms o egula e hei popula ions, among
o he unc ions (Ga bach e al., 2014; Bomma co e al., 2018; F´
elix e al.,
2018). The e o e, p ese ing soil biodi e si y is essen ial o ensu ing
ood secu i y in a apidly changing wo ld (El Muj a e al., 2019).
Nume ous soil o ganisms imp o e c op heal h and yields in a ying
ways, o example, by limi ing damage caused by pes s and diseases,
enhancing wa e a ailabili y o nu ien in ake (Bomma co e al., 2018;
F´
elix e al., 2018; El Muj a e al., 2019). Wo ldwide dis ibu ed ea h-
wo ms (EWs), o ins ance, imp o e soil s uc u e, acili a e o ganic
ma e decomposi ion, and gene a e o ganic compounds (in hei
exc e a) ha ac as plan g ow h enhance s (Muscolo e al., 1999;
Eisenhaue &Scheu, 2008; Wall, 2012; Kos e al., 2017). EWs can also
con ibu e o modula ing soil bio a and he unc ions hey p o ide
(Byzo e al., 2007; Hoe ne e al., 2018; Bui ydai ˙
e e al., 2023; Fe lian
e al., 2024). Fo example, hei mo emen can enhance he dis ibu ion
o o he bene icial soil o ganisms, such as en omopa hogenic ungi and
nema odes (Shapi o-Ilan and B own, 2013). EW eeding ac i i y has also
been ound o con ibu e o he educ ion o plan -pa asi ic nema ode
popula ions (Dash e al., 1980; Boye e al., 2013), and hence, EWs can
play an impo an ole in p o ec ing plan oo s om hei a ack and
con ibu ing o secu ing c op yields.
One c yp ic bu possibly equal impo an playe o EWs is he bac-
e ia associa ed wi h he gu and he sec e ion o cu aneous exc e a
(CEx). O e all, he EW gu hos s a species-speci ic mic obial communi y
in luenced by habi a and en i onmen al condi ions (Ai a and Domí-
nguez, 2011; G´
omez-B and´
on e al., 2012). Oxygen and nu ien le els
play c ucial oles in shaping bac e ial composi ion wi hin he gu
compa ed o adjacen soils, a o ing anae obic and acul a i e anae obic
bac e ia like P o eobac e ia, Fi micu es, Bac e oide es, and Ac ino-
bac e ia (Ho n e al., 2003; D ake and Ho n, 2007). Indeed, i was
desc ibed ha he bac e ial communi y in he EW cas di e s om he
su ounding soils (Samped o and Whalen, 2007; Ai a e al., 2015, Ai a
e al., 2016), and hence, hei long- e m p esence could d i e bac e ial
composi ion. In addi ion, EWs sec e e ce ain subs ances, such as he
CEx, h ough do sal po es, which can include u ine, coelomic luid, and
mucus, con aining e en immune cells like coelomocy es wi h de ense
unc ions (Homa e al., 2008; San ocki e al., 2016). Coelomic luid has
been desc ibed o exhibi an imic obial and p o eoly ic p ope ies,
po en ially a ec ing soil o ganisms upon con ac (Dales and Kalaç,
1992; Bilej e al., 1995; Kasschau e al., 2007). In his line, Pla ˇ
sin e al.
(2017) demons a ed ha coelomic luids om ce ain EW species
inhibi he g ow h o phy opa hogenic ungi. Con e sely, sp ing ails
such as He e omu us ni idus ac i ely seek CEx om ea hwo ms,
sugges ing i s signi icance in hei habi a (Salmon and Ponge, 2001).
Hence, all EW ac ions (mo ing and eeding) and hei a ea o in luence,
he d ilosphe e, can modula e soil bio a and hei unc ions.
Simila ly, en omopa hogenic nema odes (EPNs) a e also well-known
bene icial soil o ganisms (Lacey e al., 2015), widesp ead in na u al and
ag icul u al soils (S ua e al., 2015; Campos-He e a e al., 2019). EPNs
occu in soils as a esis ance s age named in ec i e ju enile (IJ), capable
o ac i ely loca ing, pene a ing, and eleasing symbio ic bac e ia
(Xeno habdus o S eine nema and Pho o habdus o He e o habdi is), in
he insec hemocoel (Dillman e al., 2012; S ock, 2015). Inside he in-
sec , bo h nema odes and bac e ia p oduce by-p oduc s esponsible o
killing he hos wi hin 2–3 days (Dowds and Pe e s, 2002) and ep oduce
wi hin he cada e , p o ec ed by he emission o speci ic ola iles and
signals o a oid sca enge and sap ophy ic ac i i y (Gulcu e al., 2012;
Blanco-P´
e ez e al., 2019). Once he ood is deple ed, and he signal o
o e c oding a e p esen , a new coho o IJs inco po a es some bac e ia
inside and eme ges om he cada e , sea ching o new hos s (S ock,
2015).
In he ag icul u al con ex , inocula ion o biological con ol agen s
(e.g., EPNs) and bio e ilize s (e.g., EWs) can con ibu e o bene icial
unc ions ha suppo inc eased p oduc i i y (Be endsen e al., 2012).
Howe e , unde s anding he complex mul i ophic in e ac ions among
bene icial soil o ganisms and hei su ounding en i onmen is chal-
lenging bu c ucial o ad ancing he sus ainabili y o ag icul u al p ac-
ices. Rega ding EWs and EPNs, limi ed s udies ha e ocused on he
s udy o hei in e ac ions in soils. S ill, i is known ha he co-
occu ence o bo h soil o ganisms can enhance he EPN dispe sal and
i s i ulence agains insec pes , e en i species-speci ic (Shapi o e al.,
1995; Shapi o-Ilan and B own, 2013; Chelkha e al., 2021). Some
nega i e impac s ha e also been ound. Fo example, Campos-He e a
e al. (2006) con i med he ansi o IJs h oughou he diges i e ac o
EWs bu wi h limi ed su i al, and Chelkha e al. (2020) epo ed
educed EPN i ulence and ep oduc i i y a e co-occu ing wi h EWs.
The CEx p oduced by EWs migh also be ele an since ad e se e ec s on
EPN i ulence ha e been epo ed o some species-speci ic in e ac ions
(Chelkha e al., 2020, 2021; Fa o e e al., 2020). Howe e , mos o hese
s udies in ol e labo a o y app oaches using au ocla ed subs a es and
sho ime- ames which may limi insigh s in o EW-EPN in e ac ions
(Shapi o e al., 1995; Campos-He e a e al., 2006; Shapi o-Ilan and
B own, 2013; Chelkha e al., 2020, Chelkha e al., 2021). This signi ican
gap migh be add essed by explo ing EW-EPN co-occu ence wi hin
mo e na u alized and complex sys ems, such as hose in ol ing na u al
soils wi h hei bio a and li ing plan oo s.
This s udy aimed o in es iga e he impac o he co-occu ence o
EWs o hei CEx wi h EPNs on (i) plan pe o mance, (ii) nema ode
i ulence, (iii) soil physical–chemical p ope ies, and (i ) soil mic o-
bio a. We hypo hesized signi ican changes in he measu emen s o hese
a iables bu hen apidly e e ed o he o iginal condi ions. Two pos -
exposu e in e als—15 and 30 days— o explo e he empo al dynamics
we e e alua ed. The expe imen s we e pe o med on oma o plan s, a
well-es ablished model o s udying physiological p ocesses and disease
impac s (Díaz-Pend´
on e al., 2010; Gilbe son &Ba uman, 2013). This
choice also holds signi ican po en ial o in eg a ing EPN applica ions
in o below- and abo eg ound In eg a ed Pes Managemen (IPM) s a-
egies (Ba alla-Ca e a e al., 2010; Ga cia-del-Pino e al., 2013, 2018;
M. Chelkha e al. Biological Con ol 200 (2025) 105685
2
Lahi i and O , 2018; Campos-He e a e al., 2021). In his s udy, we
used na u al (no p e- ea ed o au ocla ed) soil om comme cial oma o
plan a ions o illus a e he changes in plan g ow h, soil abio ic p op-
e ies, and mic obio a. We selec ed bac e ial soil communi y p o illing
since hey play a c ucial ole in soil mic ohabi a s, con ibu ing signi -
ican ly o biogeochemical cycles in ol ing ca bon, ni ogen, sul u , and
phospho us (Long e al., 2016) and in luencing nu ien abso p ion by
al e ing oo s uc u e o physiology (Vessey, 2003). O e all, using a
holis ic app oach wi h mesocosms, we expec o un a el he in e ac ions
be ween hese bene icial soil o ganisms (EWs and EPNs) while co-
applied o de e mine whe he i is possible o enhance hei posi i e
e ec s wi hou comp omising o he soil p ope ies o plan
de elopmen .
2. Ma e ials and me hods
2.1. Expe imen al ma e ials and p epa a ion p ocedu es
A Clay Loam ex u e soil om a comme cial oma o c op plan a ion
(Coope a i a El Raso, Calaho a, La Rioja, Spain, 42.3188 N 1.9581 W)
wi h no p io EPN applica ion was collec ed in 2020 a wo di e en
imes: Ap il 22nd and May 14 h. A each sampling ime, app oxima ely
40 kg o soil (0–20 cm dep h) was e ie ed om andom loca ions,
combined in coole s, and s o ed a 4 ◦C o 2–3 days be o e expe imen
p ocedu es. The soil was manually homogenized, emo ing la ge ock
agmen s (>2–5 cm). I s physical–chemical cha ac e is ics we e: 39 %
sand, 30 % sil , 31 % clay, 3.5 % o ganic ma e (OM), C/N a io o 9, pH
7.6, and elec ical conduc i i y (EC) o 1.01 S/cm (La G aje a Regional
Labo a o y, La Rioja). Plas ic po s (11x11x11 cm) we e illed wi h 700 g
o esh soil om he co esponding mixed soil da e and main ained in a
g ow h chambe (22 ◦C, 16L:8D pho ope iod, and 60 % Rela i e Hu-
midi y, RH) o wo weeks o allow any possible oma o plan s and any
weed o eme ge om he soil seed bank. All eme ging plan s we e
manually emo ed. A his ime (T0), 50 g o soil om each po was
sa ed a −80 ◦C o u he analysis o he soil bac e ial communi y (see
sec ion 2.4).
Two comme cial oma o seeds (Solanum lycope sicum—Solanales:
Solanaceae— a . Moneymake ) (La Tienda Fi o Ag ícola, S.L.,
Cas ell´
on, Spain) we e plan ed pe plo illed wi h he expe imen al soil
and main ained in he same chambe condi ions. Once oma o plan s
eme ged, only one was kep pe po ( emo ing any addi ional eme ging
plan s i necessa y). Be o e ini ia ing he expe imen , he plan s we e
allowed o g ow o ou weeks and wa e ed e e y 2–3 days wi h 50 ml
o ap wa e o each a ege a i e s age (when de eloping h ee ue
lea es).
S eine nema el iae (Rhabdi ida: S eine nema idae) RM-107 (ITS e-
gion, GenBank accession numbe MW480131) — he p edominan EPN
species in Eu ope (Hominick, 2002) and commonly ound in na u al
habi a s and c ops, also in La Rioja (Campos-He e a e al., 2007, 2008;
Blanco-P´
e ez e al., 2022)—was used in his s udy. Nema odes we e
cul u ed a he Ins i u e o G ape ine and Wine Sciences (ICVV,
Log o˜
no, Spain) using he las ins a o Galle ia mellonella (Lepidop e a:
Py alidae) and s o ed a 14 ◦C un il use, wi h IJs ha es ed wo weeks
be o e each expe imen (Blanco-P´
e ez e al., 2022).
The EW species Eisenia e ida (Haplo axida: Lumb icidae), a model
o ganism wi h widesp ead dis ibu ion in soils (Hend ix e al., 2008),
was used o his s udy. Adul s o simila size (0.3–0.5 g and leng h
5.0–5.5 cm) ob ained om a comme cial sou ce (“O Minhoca io”, Ped o
Jos´
e Lanza, Lisbon, Po ugal) we e kep in labo a o y condi ions a
22–24 ◦C in he da k. Be o e he s a o each expe imen , EW we e
s a ed o 24 h in au ocla ed mois ened soil o p e en c oss-
con amina ion wi h hei cas s (Chelkha e al., 2021). F esh CEx we e
ob ained by exposing EWs o a pe oleum e he -sa u a ed a mosphe e
(El Ha i e al., 2001). The CEx equi alen o same amoun o EWs in
each expe imen was eco e ed in dis illed wa e o ensu e o p o ide 2
ml pe expe imen al uni (see sec ion 2.2) and kep on ice. Fo each
expe imen , esh CEx and new EW shipmen we e used.
2.2. Expe imen al design and ea men applica ion
The expe imen was di ided in o wo g oups (A and B) in a g ow h
chambe , wi h ea men s andomly alloca ed o each g oup ollowing a
spli -plo design (Supplemen a y da a 1,Fig. S1). T ea men s (n =8)
included: (i) nega i e con ol (C), (ii) ea hwo m (EW), (iii) EW cu a-
neous exc e a (CEx), (i ) en omopa hogenic nema odes (EPN), ( ) EPN
+EW, and ( i) EPN +CEx. In ea men s wi h EWs, h ee indi iduals
we e added pe po . Fo he CEx ea men s, 2 ml (equi alen o he
exc e a o h ee EWs) was added pe po and e-inocula ed a e one
week. Fo EPN ea men s, 3000 IJs pe po (equi alen o 25 IJs/cm
2
)
we e applied (Shapi o-Ilan e al., 2002). All po s we e co e ed wi h a
ab ic ne o con ain he EWs. Plan and soil e alua ions we e conduc ed
a e wo and ou weeks (T1 and T2, espec i ely), wi h ou plan s pe
ea men ( wo in each block, A and B) (Fig. S1). Expe imen al g ow h
chambe condi ions we e 24 ◦C day, 18 ◦C nigh , unde a 16L:8D
pho ope iod, and 60 % RH. All he po s we e wa e ed e e y 2–3 days
wi h 50 ml o ap wa e o ensu e he same condi ions. The expe imen
was conduc ed wice wi h new ma e ial, esh soil ( om each o he
sampling imes), and o ganism applica ions.
2.3. Plan esponse, i ulence analysis, ea hwo m su i al, and soil
cha ac e iza oin p ocedu es
We assessed plan mac onu ien con en s o measu e he plan
esponse, ocusing on o al Ni ogen con en as an indica o o s ess and
po en ial nu i ional de iciencies. Using a non-des uc i e op ical
senso , Dualex™ o ce A, Scien i ic (Ac ylab, Spain), we measu ed
chlo ophyll (CLR) and la onol (FLV) con en indices (Ce o ica e al.,
2012). Measu emen s we e aken in duplica e on each plan ’s ou h and
i h lea es. Each plan was ca e ully emo ed om he po , and he soil
was gen ly sepa a ed om he oo s, mixed wi h he es o he bulk soil
o each po , and sa ed o subsequen analysis. The oo s we e washed,
and he plan s we e d ied a 40 ◦C o one week o ob ain hei d y
weigh .
Simul aneously, 50 g o mixed soil was collec ed om each po and
s o ed a −80 ◦C o bac e ial soil communi y analysis (see sec ion 2.4).
Addi ionally, 200 g o mixed soil om po s wi h EPN applica ions we e
placed in plas ic con aine s and bai ed wi h en G. mellonella la ae o
e alua e EPN i ulence (Blanco-P´
e ez e al., 2022). Con aine s we e
kep a 22 ◦C and 60 % RH in da kness o ou days. Dead la ae we e
ans e ed o Whi e aps (Whi e, 1927) o con i m nema ode-induced
mo ali y. Su i ing la ae we e held o an addi ional 24 h o assess
la e mo ali y. Cada e s we e obse ed e e y 3–4 days o ensu e IJ
eme gence om la ae. Also, a he end o he expe imen , su i al o
he ea hwo ms in he co esponding ea men s we e con i med.
Comp ehensi e soil analyses we e conduc ed only o he ou -week
pos -applica ion (T2). An aliquo o 200 g o he mixed soil om each po
was sie ed o 2 mm and analyzed sepa a ely o pH (Millennia and
Ma kewi z, 2004), OM % (Walkley and Black, 1934), mac o-nu ien s
(N, P, and K), and oligo-nu ien s (Mg, Ca, and Na) (Eu o ins Ag o-
ambien al SA, ESA25244849).
2.4. Me a axonomical bac e ial communi y analysis: Lib a y p epa a ion
Fo each o he wo ials, we independen ly e alua ed h ee soil
samples pe ea men (T0, T1, and T2; s o ed a −80 ◦C) o soil bac-
e ial communi y analyses. DNA p ocedu es we e conduc ed using he
Powe Soil DNA isola ion ki (MO BIO Labo a o ies, San Diego bio ech
co ido , Ca lsbad, CA, USA). Fi s , 0.25 g o each soil sample was placed
in a Powe Bead ube. Then, ollowing he ki p o ocol, solu ion C1 o his
ki was added, and he samples we e homogenized wice wi h a high-
speed homogenize (speed 6.0 m/sec, adap e : QuickP ep, ime 40sec,
Lis ing ma ix A, Fas P ep-24™, MP Biomedicals). A e ha , DNA
M. Chelkha e al. Biological Con ol 200 (2025) 105685
3
ex ac ion was pe o med as desc ibed in he ki and s o ed a −20 ◦C
un il hei p ocessing o he bac e ial soil communi y cha ac e iza ion.
Fu he DNA analysis we e pe o med a he Cen e o Biomedical
Resea ch o La Rioja (CIBIR, Log o˜
no, La Rioja, Spain). Ini ial DNA
in eg i y and quan i y we e assessed by Capilla y Gel Elec opho esis
(F agmen Analyze , Genomic DNA Ki , Agilen Technologies) and
luo ime y (Qubi 3.0, dsDNA HS Assay ki , The mo Fishe Scien i ic,
MA, USA), espec i ely. NGS lib a ies we e p epa ed om 12.5 ng o
DNA acco ding o he 16S Me agenomic Sequencing Lib a y P epa a ion
p o ocol (Illumina, n.d.). The p ime s used ampli ied he V3-V4 egion
o he 16S RNA gene: 16S Amplicon PCR Fo wa d P ime =5
′
TCG
TCGGCAGCAGCGTCAGATGTGTAT AAGAGAGACAGCCTACGGGNGGC
WGCAG, and 16S Amplicon PCR Re e se P ime =5
′
GTCTCGTGGG
CTCGGAGATGTGTGTATAAGAGACAGGACTACHVGGGTATCTAATCC.
The quali y o he lib a ies was assessed using F agmen Analyze
(dsDNA Reagen Ki , 35–5000 bp, Agilen Technologies). In addi ion,
he DNA concen a ion was p ecisely measu ed wi h a Qubi 3.0 luo-
ome e (dsDNA HS Assay ki , The mo Fishe Scien i ic, MA, USA). Li-
b a ies we e hen pooled equimola ly and sequenced on an Illumina
MiSeq pla o m employing a 300-cycle pai ed-end un. Fo quali y
assu ance, comme cial mock communi ies we e inco po a ed as in e nal
con ols in he inal sequencing un, including Con ol Gu (MSA-1006)
and Con ol Soil (MSA-3001) as mic obiome s anda ds, p ocessed
iden ically o he o he samples.
2.5. Bac e ial soil communi y analysis: Bioin o ma ic p ocedu es
Pos -analysis quali y assessmen was conduc ed using Fas QC
0.11.9 (Bab aham Ins i u e, 2023) and Mul iQC 1.9 (Ewels e al.,
2016). Subsequen ly, bioin o ma ic analysis was pe o med using he
Qiime2 2022.8 pipeline (Bolyen e al., 2019). The Illumina sequence
p o ided demul iplexed aw sequences, which we e hen impo ed in o
he Qiime2 pipeline and p ocessed using DADA2 (Nea ing e al., 2018;
P odan e al., 2020). This p ocess in ol ed se e al s eps: adap e and
p ime imming, noise il e ing, de eplica ion, pai ed- ead joining,
iden i ica ion o Amplicon Sequence Va ian s (ASVs) a 99 % sequencing
simila i y, and chime a emo al. Taxonomic assignmen was accom-
plished using he SILVA da abase ( e sion 132), p e- ained wi h he
V3-V4 ampli ica ion p ime s used du ing we -lab p ocessing a a 70 %
con idence le el wi h de aul pa ame e s. ASVs assigned o chlo oplas s
o A chaea we e excluded om u he analysis. Fea u e and axonomy
ables we e gene a ed in “biom”and “ s ” o ma s o subsequen
analysis. Sequence da a ( aw iles) ha e been uploaded o he GenBank
SRA da abase unde accession numbe s SAMN41943565-,
SAMN41943642 and he BioP ojec accession numbe is
PRJNA1126460.
2.6. S a is ical analysis
We employed linea mixed models (LMMs) and gene alized linea
mixed models (GLMMs) o assess he e ec o he ea men s (C, EW,
CEx, EPN, EPN +EW, and EPN +CEx), ime (T1 and T2), and hei
in e ac ion (all ixed ac o s) on EPN i ulence, plan esponse (plan d y
weigh , CLR and FLV indexes), soil p ope ies, bac e ial alpha biodi-
e si y indices (Chao1 and Shannon), and ASV de ec ions o speci ic
axa ela ed o biocon ol (Bacillus, Pseudomonas, and Xeno habdus). We
conduc ed goodness-o - i es s o de e mine he mos app op ia e dis-
ibu ion o he analyzed a iables (Table S1). We con olled o a i-
a ions wi hin ials by including his a iable as a andom ac o in each
model.
In he bac e ial soil communi y analysis, he acqui ed da a unde -
wen no maliza ion (To al Sum Scaling, TSS) and he es ima ion o
a e ac ion cu es, ela i e abundance, alpha-di e si y, and be a-
di e si y using Mic obiomeAnalys (Dha iwal e al., 2017; Chong
e al., 2020; Lu e al., 2023). We used he a e ac ion cu es o e alua e
sample quali y. Also, Chao1 ichness and Shannon di e si y (alpha-
di e si y) we e compu ed. The ela ionship be ween bac e ial commu-
ni ies was explo ed h ough B ay-Cu is me ics (be a-di e si y), ol-
lowed by Pe mu a ional Mul i a ia e Analysis o Va iance
(PERMANOVA) and isualiza ion using P incipal Coo dina e Analysis
(PCoA) plo s.
S a is ical analyses we e pe o med in R e sion 4.3.0 (R Co e Team,
2023). Goodness-o - i es s we e conduc ed using he i dis plus pack-
age in R (Deligne e-Mulle &Du ang, 2015). We an he GLM and
GLMM es s using he lme and glme unc ions, espec i ely, om he
lme4 package (Ba es e al., 2015). Pos -hoc analyses a P<0.05 signi -
icance le el we e pe o med using he es ima ed ma ginal means
(EMMeans) app oach wi h he emmeans unc ion (Len h, 2023). PER-
MANOVA was pe o med using he egan package. Di e si y indexes
we e ep esen ed in PCoAs and boxplo s a he ASV le el using he
ggplo 2 package.
3. Resul s
3.1. Plan esponse, i ulence analysis, ea hwo m su i al, and soil
cha ac e iza oin p ocedu es
No signi ican di e ences we e ound among ea men s o he plan
esponse pa ame e s e alua ed (plan d y weigh , CLR, and FLV indices)
bu o he de ec ion ime pos -applica ions (Supplemen a y da a 2,
Fig. S2 and Table S2). In con as , EPN i ulence dec eased signi ican ly
30 days pos -inocula ions when EPNs we e applied alone compa ed o
when hey we e applied in combina ion wi h EWs (Fig. 1). All ea h-
wo ms su i ed o he ea men s a e 30 days exposu e (da a no
shown). Rega ding soil p ope ies, we only ound signi ican di e ences
among ea men s o he pe cen age o o ganic ma e and Ca and Mg
con en s (Fig. 2 and Table 1;Supplemen a y da a 2,Fig. S3). Speci -
ically, OM% was signi ican ly highe o he combina ion o EPN +EW
han con ol and CEx ea men s (Fig. 2A), while Ca and Mg con en s
we e signi ican ly lowe o he combina ion o EPN +CEx compa ed o
con ol ea men s, and o Mg, also compa ed o CEx and EPN +CEx
ea men s (Fig. 2B,C).
3.2. Soil bac e ia communi y composi ion
A o al o 72 samples (36 om each independen ial) we e e alu-
a ed since all eached he quali y and quan i y s anda ds ollowed in he
CIBIR Genomics &Bioin o ma ics Co e Facili y. We ob ained
13,682,371 sequences a e he bioin o ma ics ea men o he aw
sequences (pai ed-end alignmen s, quali y e alua ions, including he
emo al o chime ic sequences and single ons). The minimum numbe
o sequences pe sample was 124,833, and he maximum was 233,177,
wi h a mean o 171,030 and a median o 170,130. We es ablished he
minimum numbe o sequences a 32,565, e aining 2,540,070 (55.9 %)
ea u es ac oss 76 samples a he speci ied sampling dep h. We iden i ied
19,174 dis inc bac e ial ASVs wi h assigned agmen s a ying
282–540 bp leng hs, a e aging 416 ±13 bp. The e was minimal a i-
abili y in he o al numbe o sequences among samples. The a e ac ion
cu es indica ed ha mos samples eached sa u a ion, making hem
op imal o u he analysis (Supplemen a y da a 2,Fig. S4). Finally, he
p esence o speci ic bac e ia axa in he gene a Bacillus, Pseudomonas,
and Xeno habdus was no a ec ed by any o he ea men s e alua ed,
no o he de ec ion ime pos -applica ions (Supplemen a y da a 2,
Fig. S5 and Table S3).
3.3. Soil bac e ial di e si y
We ound signi ican di e ences in alpha di e si y indices, Chao1
and Shannon, among ea men s and o hei in e ac ion wi h he
de ec ion ime pos -applica ions (Fig. 3 and Table 2). Speci ically, bo h
indices we e signi ican ly lowe o CEx applied alone han he con ol
15 days pos -inocula ions (Fig. 3). Simila pa e ns be ween indices we e
M. Chelkha e al. Biological Con ol 200 (2025) 105685
4
also obse ed 30 days pos -applica ions, wi h signi ican ly lowe alues
o con ol ea men s and no ably highe alues o EPNs combined
wi h EWs (Fig. 3). Fo he PCoAs based on he B ay-Cu is index,
al hough we ound simila signi icances o he in es iga ed ac o s as
o he alpha indices, no clea dis inc ions in clus e ing o ma ions o
bac e ial communi y composi ion we e obse ed among ea men s o
be ween T1 and T2 (Fig. 4).
4. Discussion
This s udy p o ided new insigh s in o how co-occu ing bene icial
soil o ganisms, such as EWs and EPNs, a ec nema ode i ulence and
abio ic and bio ic (mic obio a) soil cha ac e is ics wi hin a complex,
na u alized plan -soil sys em. Addi ionally, da a was collec ed a wo
in e als ollowing ea men exposu e —15 and 30 days— o ensu e a
comp ehensi e analysis. Ou indings e ealed ha , a e 30 days, EPN
ac i i y and mic obial di e si y we e enhanced when bo h bene icial
o ganisms co-occu compa ed o indi idual ea men s o no applica-
ions (con ol ea men ). These esul s sugges a po en ial long- e m
indi ec bene i o plan s, possibly media ed no only by bio ic
changes bu also by abio ic soil cha ac e is ics, such as he inc ease o
OM in he EW-EPN ea men . Howe e , in his ega d, no signi ican
di e ences we e obse ed in plan g ow h- ela ed me ics. Longe - e m
s udies as well as o he species combina ion o EW and EPN may be
necessa y o iden i y he possible speci ic d i e s p omo ing plan heal h
and c op p o ec ion a ec ed by he co-occu ence o EPNs and EWs o
hei CEx.
Di e se s udies examining he in e ac ion be ween EPNs and EWs,
including hei CEx, ha e shown con as ing esul s—posi i e, neu al,
o de imen al—depending on he species and expe imen al se up
(Campos-He e a e al., 2006; Shapi o-Ilan and B own, 2013; Chelkha
e al., 2020, 2021; Fa o e e al., 2020). Se e al s udies ha e employed
mic ocosms (e.g., Pe i dishes, ubes, 24-well pla es) wi h au ocla ed
subs a es and sho in e ac ion pe iods o ensu e con ac be ween o -
ganisms (Campos-He e a e al., 2006; Chelkha e al., 2020, Chelkha
e al., 2021). In con as , Fa o e e al. (2020) conduc ed a ield meso-
cosm expe imen wi hin wo c opping sys ems, e ealing ha EWs
enhanced EPN in ec ion a es, he eby boos ing hei biocon ol po en-
ial agains oo - eeding pes s. This inding aligns wi h ou obse a ions
o inc eased EPN i ulence when combined wi h EWs/CEx a e 30 days
Fig. 1. Nema ode i ulence assessed by insec la al mo ali y 15 and 30 days pos -applica ion o en omopa hogenic nema odes alone (EPN) o combined wi h
ea hwo ms (EPN +EW) o EW cu aneous exc e a (EPN +CEx). As e isks ep esen s a is ically signi ican di e ences o MIXED model es s a ** P<0.01 and * P
<0.05. Di e en le e s indica e s a is ically signi ican di e ences (P<0.05) o pai wise compa isons wi hin ea men s.
Fig. 2. Impac o he e alua ed ea men s on he soil p ope ies (A) pe cen age o o ganic ma e (OM) and nu ien con en s o (B) Ca and (C) Mg, measu ed 30 days
pos -applica ions. T ea men s: con ol (C), ea hwo m (EW), EW cu aneous exc e a (CEx), en omopa hogenic nema odes (EPN), and he combina ions EPN +EW and
EPN +CEx. Di e en le e s indica e s a is ically signi ican di e ences (P<0.05) o pai wise compa isons wi hin ea men s. S a is ical analysis de ails can be
ound in Table 1.
Table 1
Summa y o esul s om MIXED models es ing o he e ec s o he e alua ed
ea men s on soil p ope ies. As e isks ep esen s a is ically signi ican di -
e ences wi hin ea men s a ** P<0.01; n.s., no signi ican . Values a e
ep esen ed in Fig. 2 and Fig. S3.
T ea men s
Soil Va iables
χ
2
5
P
pH 3,55 n.s.
OM 15,90 **
N 2,07 n.s.
P 7,03 n.s.
K 1,02 n.s.
Ca 16.82 **
Mg 19,92 **
Na 6,61 n.s.
M. Chelkha e al. Biological Con ol 200 (2025) 105685
5

pos -exposu e. This posi i e in e ac ion migh be a ibu ed o EWs’
abili y o mix he soil, as Shapi o-Ilan and B own (2013) desc ibed.
Howe e , Fa o e e al. (2020) also epo ed ha EPNs a oided plan s
wa e ed wi h CEx, possibly due o ad e se e ec s on hei i ness
(Chelkha e al., 2020, Chelkha e al., 2021). Con e sely, we obse ed
high EPN i ulence main enance a e 30 days pos -exposu e o EWs o
hei CEx compa ed wi h he educ ion in he EPN-alone con ol in a
complex sys em, as Fa o e e al. (2020) designed. The na u al soil likely
bu e ed he nega i e impac on EPN i ulence in di ec exposu e ex-
pe imen s (Chelkha e al., 2020, 2021; Fa o e e al., 2020). Soil p op-
e ies like OM and clay con en can in e ac wi h o ganic compounds
(Lehmann and Klebe , 2015). A ecen s udy indica ed ha EW-CEx
comp ises p o eins, amino acids, ca bohyd a es, a y acids, poly-
saccha ides, alcohol, phenol, and es e o ganic subs ances (Huan e al.,
2023). All hese compounds in e ac wi h he soil ac ion and bio a
when pe o ming di e en unc ions (Tiedje e al., 1999; Kasschau e al.,
2007; Homa e al., 2008; Lehmann and Klebe , 2015; San ocki e al.,
2016), po en ially modi ying hei impac on EPNs. The e o e, di e -
ences in soil bio ic and abio ic composi ion migh explain he disc ep-
ancies be ween ou indings and hose o p e ious s udies (Chelkha
e al., 2020, 2021; Fa o e e al., 2020). Hence, addi ional s udies,
including di e en ypes o soil ( ex u e, o ganic ma e pe cen age,
e c.) de i ed om o he c ops wi h po en ially a ying soil bio a, a e
necessa y o ex end ou obse a ions o a mo e gene al applica ion.
Simila ly, EWs can signi ican ly al e o he soil bio a in di e se soil
biomes (e.g., d ilosphe e, hizosphe e, bulk soil) h ough hei mo e-
men and eeding ac i i ies (Ai a e al., 2015, 2016; Wang e al., 2017;
Hoe ne e al., 2018; Medina-Sauza e al., 2019, Medina-Sauza e al.,
2023). Howe e , al hough EW eeding can, o ins ance, dec ease bac-
e ial soil di e si y a e passing h ough hei gu , his e ec depends on
soil ype (Koubo ´
a e al., 2015). Ou esul s no ed a sligh dec ease in
bac e ial alpha di e si y in he EWs ea men s a e 15 days pos -
exposu e, bu i did no pe sis beyond 30 days. Fu he mo e, Ai a
e al. (2016) ound ha EWs can modula e he bac e ial composi ion o a
subs a e, sugges ing ha EWs selec and build hei cas mic obiome
om inges ed bac e ia. Time is a c i ical ac o in his p ocess, as seen in
e micompos ing sys ems whe e bac e ial di e si y ini ially inc eases
bu la e declines in ma u e e micompos s (Vi as e al., 2009). Spe-
ci ically, Gopal e al. (2017) obse ed an inc ease in alpha di e si y un il
he 75 h day, ollowed by a decline a e he 105 h day in ma u e e -
micompos . Ou indings a e consis en wi h hese obse a ions,
pa icula ly o he co-occu ence o EPNs and EWs, which exhibi ed
Fig. 3. Alpha di e si y indexes (A) Chao1 and (B) Shannon o bac e ial soil communi y analyses 15 and 30 days pos -applica ions. T ea men s: con ol (C),
ea hwo m (EW), EW cu aneous exc e a (CEx), en omopa hogenic nema odes (EPN), and he combina ions EPN +EW) and EPN +CEx. Di e en le e s indica e
s a is ically signi ican di e ences (P<0.05) o pai wise compa isons wi hin ea men s. S a is ical analysis de ails can be ound in Table 2.
Table 2
Summa y o esul s om MIXED models es ing o he e ec s o he e alua ed
ea men s on bac e ial alpha biodi e si y a 15 and 30 days pos -applica ion.
As e isks ep esen s a is ically signi ican di e ences wi hin ea men s a **
P<0.01 and *** P<0.001; n.s., no signi ican . Values a e ep esen ed in Fig. 3.
T ea men s (Tx) Time Tx * Time
Di e si y
index
χ
2
d P
χ
2
d P
χ
2
d P
Chao1 42.87 5 *** 0.42 1 n.
s.
29.26 5 ***
Shannon 17.71 5 ** >0.01 1 n.
s.
18.71 5 **
Fig. 4. P incipal componen analysis o he bac e ial be a di e si y displaying
g oups o associa ion by (A) ea men s: con ol (C), ea hwo m (EW), EW
cu aneous exc e a (CEx), en omopa hogenic nema odes (EPN), and he com-
bina ions EPN +EW) and EPN +CEx; and (B) ime (15 and 30 days pos -
applica ion). As e isks ep esen s a is ically signi ican di e ences a *** P
<0.001; n.s., no signi ican .
M. Chelkha e al. Biological Con ol 200 (2025) 105685
6
inc eased bac e ial alpha di e si y 30 days pos -applica ion. Howe e ,
we unde s and ha he leng h o he s udy was a limi a ion since 2 and 4
weeks seem o be oo sho o de ec hose in e ac ions. Hence,
ex ending he du a ion o ou s udy may ha e e ealed he poin a
which bac e ial di e si y begins o decline and, hus, a deepe unde -
s anding o he changes wi hin he soil-mic obio a-plan sys em.
While ou s udy sheds ligh on he impac o EPN applica ion on he
soil bac e ial communi y, he e is s ill much o be in es iga ed (de Na do
e al., 2006; Li e al., 2024), no ably o in e ac ions wi h o he soil
o ganisms such as EWs. We ound ha 15 days pos -EPN applica ion,
he e we e no signi ican changes in he soil bac e ial communi y. This
inding is consis en wi h Li e al. (2024) o bac e ial communi y, bu
also no ed changes in he ungal communi y associa ed wi h EPN
occu ence. Consequen ly, u u e esea ch should include ungal di-
e si y when examining he combined e ec s o EPNs and EWs/CEx o
p o ide a mo e comp ehensi e unde s anding o ecosys em dynamics.
Howe e , we obse ed inc eased bac e ial soil di e si y a e 30 days,
sugges ing ha hese changes equi e a longe ime ame. This e ec , in
any case, disag ees wi h de Na do e al. (2006), who epo ed no in-
c ease in soil mic obial biomass, espi a ion, o ni ogen pools 64 days
pos -applica ion o he EPN species S eine nema ca pocapsae. Besides
di e ences in soil ypes and EPN species in ol ed (S. ca pocapsae s.
S. el iae) o , o ins ance, he p esence o oma o oo s in ou sys em, he
disc epancies migh be a ibu ed o he indi ec measu emen me hods
used by de Na do e al. (2006) as opposed o he molecula app oach
based on HTS in ou s udy. No ably, we obse ed di e ences in he
bac e ial alpha di e si y be ween T0 (soil sampled be o e plan ing he
oma o seeds and applying any ea men and excluded om he analysis
o obse e ea men e ec s) and pos - ea men imes (T1 and T2).
Rega ding he a ge gene a o in e es in biocon ol —Pseudomonas,
Bacillus, and Xeno habdus (Lacey e al., 2015; Vicen e-Díez e al.,
2023)—we did no obse e di e ences among ea men s, e en hose
including EPNs hos ing he bac e ium Xeno habdus. I is impo an o
no e ha he soil bac e ia analysis was pe o med on 0.25 g o bulk soil
om each ea men . While his app oach was necessa y o ou s udy, i
could ha e educed he likelihood o aking a ep esen a i e sample o
EPN-associa ed bac e ia. Fu u e esea ch should conside la ge o mo e
ep esen a i e soil samples o unde s and be e he in e ac ions be-
ween EPNs, hei associa ed bac e ia, and he soil mic obial
communi y.
Besides p ese ing EPN i ulence and inc easing bac e ial alpha di-
e si y, he EPN-EW in e ac ions in ou s udy had minimal e ec s on
plan pa ame e s and only in speci ic ea men s o ce ain soil p op-
e ies. Since plan oo s abso b ni ogen and o he essen ial mac onu-
ien s suppo ing chlo ophyll p oduc ion and o he i al p ocesses
(Wall, 2012; Fa hi, 2022; Hussain Shah e al., 2024), we expec ed he
ea men s o a ec plan ai s. We employed he no el, non-des uc i e
Dualex™app oach o measu e plan g ow h and de elopmen o e
ime, speci ically a e 2 and 4 weeks. This sys em consis s o a p ecise
op ical echnique o assess ni ogen le els ha uses speci ic UV exci a-
ion beams o la onoids and chlo ophyll (T emblay e al., 2010, 2012;
O e beck e al., 2018). Cong uen wi h Becagli e al. (2021), we e-
po ed dec eased chlo ophyll le els o e ime, bu no signi ican ea -
men e ec s. Howe e , some s udies ound opposi e pa e ns, o
example, inc eased chlo ophyll le els o e ime when e alua ing he use
o e micompos as an o ganic e ilize (Jankauskien˙
e e al., 2022) o
speci ic bac e ia associa ed wi h EWs (Bane jee e al., 2019). This di -
e ence can be a ibu ed o he ex emely di e en condi ions be ween
soil unde ac i e e micompos ing ac ion (wi h a high densi y o EWs)
and na u al soil, as in es iga ed he ein. Con lic ing indings in his
espec highligh he dependence o EW-plan in e ac ions on mul iple
aspec s, such as soil ype, species in ol ed, and associa ed bio a. On he
o he hand, la onol con en s in lea es and o e all plan g ow h (e.g.,
d y weigh ) inc eased o e ime wi hou signi ican di e ences among
ea men s. Since Zhang e al. (2009) showed ha CEx signi ican ly
p omo es oma o seedling g ow h, he lack o di e ences in ou s udy
migh be due o a ia ions in oma o cul i a s, soil ype, and speci ic CEx
composi ions o di e se E. e ida popula ions. Fu he s udies, mainly in
long- e m esea ch, a e needed o iden i y he c i ical d i e s ela ed o
he e ec o EWs and hei de i a i es on plan g ow h. Rega ding EPN-
plan oo in e ac ions, p e ious s udies ha e shown ha plan oo a -
chi ec u e (De ma a e al., 2014) and chemical cues om oo -he bi o e
a acks (Rasmann e al., 2005; Tu lings e al., 2012) in luence EPN
occu ence and beha io . Ou s udy ound no e ec on chlo ophyll and
la onol con en s and plan g ow h a e one mon h o EPN exposu e.
Howe e , since only one s udy (Helms e al., 2019) has also di ec ly
explo ed he impac o EPNs on plan g ow h and de enses, mo e
esea ch is needed o unde s and EPN-plan in e ac ions in soils.
Ou s udy epo ed only signi ican a ia ion in plan nu ien
a ailabili y in speci ic pa ame e s, inc easing OM in he EPN-EW
ea men and dec easing Ca and Mg in he EPN-CEx ea men . These
esul s con as wi h he well-documen ed abili y o EWs o imp o e soil
e ili y and p o ide essen ial nu ien s such as N, K, and Ca (La elle
e al., 2016; Medina-Sauza e al., 2023). One plausible explana ion o
his disc epancy is ha he expe imen may equi e addi ional ime o
p oduce measu able changes in soil p ope ies ( an de Heijden e al.,
2008). As obse ed o he soil bac e ial communi y, signi ican di e -
ences among he ea men s became appa en only a e 30 days in ou
s udy. The e o e, we sugges conduc ing u he s udies wi h ex ended
obse a ion pe iods o 3–6 mon hs o comp ehensi ely assess he impac
o he e alua ed ea men s on soil p ope ies.
Achie ing he goals o sus ainable ag icul u e, as ou lined by he UN
and suppo ed by ini ia i es like he Eu opean G een Deal (Eu opean
Commission, 2020), equi es de eloping new bio ools o eplace
chemical e ilize s and pes icides. A comp ehensi e unde s anding o
he in e ac ions be ween bene icial o ganisms, soil, and c ops is essen-
ial o gaining public con idence and encou aging he adop ion o hese
bio echnologies. This s udy showed ha in e ac ions be ween bene icial
soil o ganisms, such as EPNs and EWs, a e complex, ime-dependen ,
and species-speci ic. Fu he esea ch is needed o ill knowledge gaps,
inco po a ing di e en augmen ed EWs and EPN species, soil ypes,
a ge soil o ganisms (bac e ia, ungi, mic oa h opods, nema odes,
e c.), c ops, and en i onmen s.
CRediT au ho ship con ibu ion s a emen
Ma yam Chelkha: W i ing –o iginal d a , Me hodology, In es i-
ga ion, Fo mal analysis, Concep ualiza ion. Rub´
en Blanco-P´
e ez:
W i ing – e iew &edi ing, In es iga ion, Fo mal analysis. Da id Lab-
a ga: W i ing – e iew &edi ing, Fo mal analysis. Ma ía de To o:
W i ing – e iew &edi ing, Fo mal analysis, Concep ualiza ion. Jo ge
Due˜
nas-He nani: W i ing – e iew &edi ing, Me hodology. Kyle
Wickings: W i ing – e iew &edi ing. Raquel Campos-He e a:
W i ing – e iew &edi ing, Supe ision, Funding acquisi ion, Fo mal
analysis, Concep ualiza ion.
Decla a ion o compe ing in e es
The au ho s decla e ha hey ha e no known compe ing inancial
in e es s o pe sonal ela ionships ha could ha e appea ed o in luence
he wo k epo ed in his pape .
Acknowledgmen s
We wan o hank he echnicians a Coope a i a El Raso om Cal-
aho a (La Rioja, Spain) o hei assis ance in loca ing a sui able ield
wi h oma oes o he expe imen . MC was suppo ed by Voca ional
T aining, Highe Educa ion and Scien i ic Resea ch, and he a el
assis ance associa ed wi h he g an CSIC I-COOP+2018 g an
(COOPA20231). RBP was inanced wi h a Juan de la Cie a con ac
JDC2022-048978-I unded by MCIN/AEI/ 10.13039/501100011033
and by “Eu opean Union Nex Gene a ionEU/PRTR”. DL was suppo ed
M. Chelkha e al. Biological Con ol 200 (2025) 105685
7
by an FPI-UR/CAR 2022 ellowship om he Uni e sidad de La Rioja
(Spain). JDH is suppo ed by he P og ama In es igo om he Go e n-
men o La Rioja and he “Eu opean Union Nex Gene a ionEU/PRTR.
This s udy was suppo ed by he CSIC I-COOP+2018 g an
(COOPA20231) and he Ins i u o de Es udios Riojanos g an (Resolu ion
N◦18/2020). This s udy o ms pa o he AGROALNEXT p og am and
was suppo ed by MCIN wi h unding om Eu opean Union Nex Ge-
ne a ionEU (PRTR-C17.I1).
Appendix A. Supplemen a y da a
Supplemen a y da a o his a icle can be ound online a h ps://doi.
o g/10.1016/j.biocon ol.2024.105685.
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