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dc.contributor.authorBicharanloo, Bahareh
dc.contributor.authorBagheri Shirvan, Milad
dc.contributor.authorCavagnaro, Timothy R.
dc.contributor.authorKeitel, Claudia
dc.contributor.authorDijkstra, Feike A.
dc.date.accessioned2024-02-25T22:03:41Z
dc.date.available2024-02-25T22:03:41Z
dc.date.issued2022en_AU
dc.identifier.urihttps://hdl.handle.net/2123/32251
dc.description.abstractGrassland plants allocate photosynthetically fixed carbon (C) belowground to root biomass and rhizodeposition, but also to support arbuscular mycorrhizal fungi (AMF). These C allocation pathways could increase nutrient scavenging, but also mining of nutrients through enhanced organic matter decomposition. While important for grassland ecosystem functioning, methodological constraints have limited our ability to measure these processes under field conditions. We used 13CO2 and 15N pulse labelling methods to examine belowground C allocation to root biomass production, rhizodeposition and AMF colonisation during peak plant growth in a grassland field experiment after three years of N fertilisation (0 and 40 kg N ha−1 year−1) and defoliation frequency treatments (“low” and “high”, with 3–4 and 6–8 simulated grazing events per year, mimicking moderate and intense grazing, respectively). Moreover, we quantified the consequences for plant nitrogen (N) uptake and decomposition of soil organic C (SOC). Nitrogen fertilisation increased rhizodeposition and AMF colonisation (by 63 % and 54 %), but reduced root biomass (by 25 %). With high defoliation frequency, AMF colonisation increased (by 60 %), but both root biomass and rhizodeposition declined (by 35 % and 58 %). Plant N uptake was highest without N fertilisation and low defoliation frequency, and positively related to root biomass and the number of root tips. Therefore, when N supply is low and the capacity to produce C through photosynthesis is high, belowground C allocation to root production and associated root tips was important to scavenge for N in the soil. In contrast, the strong positive relationship between the rate of rhizodeposition and SOC decomposition, suggests that rhizodeposition may help plants to mine for nutrients locked in SOC. Taken together, the results of this study suggest that belowground C allocation pathways affected by N fertilisation and defoliation frequency affect plant N scavenging and mining with important consequences for longterm grassland C dynamics.en_AU
dc.language.isoenen_AU
dc.publisherElsevieren_AU
dc.relation.ispartofScience of the Total Environmenten_AU
dc.rightsCopyright All Rights Reserveden_AU
dc.subjectMicrobial miningen_AU
dc.subjectMycorrhizaen_AU
dc.subjectNutrient cyclingen_AU
dc.subjectPulse labellingen_AU
dc.subjectRespirationen_AU
dc.subjectRhizodepositionen_AU
dc.titleNitrogen addition and defoliation alter belowground carbon allocation with consequences for plant nitrogen uptake and soil organic carbon decomposition.en_AU
dc.typeArticleen_AU
dc.subject.asrc410604en_AU
dc.subject.asrc410203en_AU
dc.identifier.doi10.1016/j.scitotenv.2022.157430
dc.type.pubtypeAuthor accepted manuscripten_AU
dc.relation.arcDP190102262
usyd.facultySeS faculties schools::Faculty of Science::School of Life and Environmental Sciencesen_AU
usyd.citation.volume846en_AU
usyd.citation.spage157430en_AU
workflow.metadata.onlyNoen_AU


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