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Articles by Yolima Carrillo
Faster-and-tighter nitrogen cycle supports mature forest productivity under elevated CO 2
Abstract INTRODUCTION RESULTS AND DISCUSSION MATERIALS AND METHODS Acknowledgments Supplementary Materials REFERENCES Information & Authors Metrics & Citations View Options References Figures Tables Media Share Abstract Rising atmospheric carbon dioxide (CO2) concentration could enhance forest carbon (C) uptake, but nitrogen (N) is thought to progressively constrain this effect. Yet, significant biomass gains were demonstrated in a mature oak forest after 6 years of Free Air CO2 Enrichment.
Enhanced below-ground functioning is associated with higher plant resistance against drought: Implications for ecosystem functions
1 INTRODUCTION Water is a major determinant of ecosystem functioning. Alterations in water availability such as those derived from extended dry periods (i.e. drought), structures plant and soil microbial communities as well as their interactions (Pugnaire et al., 2019; Van Dyke et al., 2022). However, we lack understanding on how above-ground plant traits link to soil microbial communities and the functions they perform in response to drought.
Nutrient‐Rich Mineral‐Associated Organic Matter Limits Carbon Storage Under Elevated Carbon Dioxide in a Low Phosphorus Eucalyptus Woodland Soil
Conflicts of Interest The authors declare no conflicts of interest. Supporting Information Filename Description gcb70585-sup-0001-AppendixS1.pdfPDF document, 1 MB Appendix S1: gcb70585-sup-0001-AppendixS1.pdf. References , , , and . 2018. “An Investigation of the Distribution of Phosphorus Between Free and Mineral-Associated Soil Organic Matter, Using Density Fractionation.” Plant and Soil 427: 139–148. , , , , , and . 2020.
Grazing‐N addition interactions drive soil carbon priming and balance via bacterial assimilation in a meadow steppe
Figure S1. (a) Geographic location of the study site (marked as red star). (b) Block design layout in situ. (c) Field treatment design. (d) Field treatment design. Figure S2. Effects of N addition on plant characteristics under grazed and ungrazed conditions. Figure S3. Effects of N addition on soil pH, total N, and dissolved inorganic N under grazed and ungrazed conditions. Figure S4.
Prolonged drought legacies influence the performance of foliar herbivores on legumes through shifts in plant-soil biotic interactions
INTRODUCTION Projected changes in climate include increased warming and more variable rainfall, which are likely to contribute to more severe and prolonged droughts (IPCC, 2022). There is increasing evidence that changes in rainfall, including drought, can modify plant–soil biotic and plant–herbivore interactions, which could have longer term effects on ecosystem dynamics (Crawford & Hawkes, 2020; Meisner et al., 2018).
Microbial competition for phosphorus limits the CO2 response of a mature forest - Nature
Abstract The capacity for terrestrial ecosystems to sequester additional carbon (C) with rising CO2 concentrations depends on soil nutrient availability1,2. Previous evidence suggested that mature forests growing on phosphorus (P)-deprived soils had limited capacity to sequester extra biomass under elevated CO2 (refs. 3,4,5,6), but uncertainty about ecosystem P cycling and its CO2 response represents a crucial bottleneck for mechanistic prediction of the land C sink under climate change7.
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