Nature Climate Change · 2024
Díaz-Martínez, P., Maestre, F. T., Moreno-Jiménez, E., Delgado-Baquerizo, M., Eldridge, D. J., Saiz, H., Gross, N., Le Bagousse-Pinguet, Y., Gozalo, B., Ochoa, V. +117
, Guirado, E., García-Gómez, M., Valencia, E., Asensio, S., Berdugo, M., Martínez-Valderrama, J., Mendoza, B. J., García-Gil, J. C., Zaccone, C., Panettieri, M., García-Palacios, P., Fan, W., Benavente-Ferraces, I., Rey, A., Eisenhauer, N., Cesarz, S., Abedi, M., Ahumada, R. J., Alcántara, J. M., Amghar, F., Aramayo, V., Arroyo, A. I., Bahalkeh, K., Ben Salem, F., Blaum, N., Boldgiv, B., Bowker, M. A., Bran, D., Branquinho, C., Bu, C., Cáceres, Y., Canessa, R., Castillo-Monroy, A. P., Castro, I., Castro-Quezada, P., Chibani, R., Conceição, A. A., Currier, C. M., Darrouzet-Nardi, A., Deák, B., Dickman, C. R., Donoso, D. A., Dougill, A. J., Durán, J., Ejtehadi, H., Espinosa, C., Fajardo, A., Farzam, M., Ferrante, D., Fraser, L. H., Gaitán, J. J., Gusman Montalván, E., Hernández-Hernández, R. M., von Hessberg, A., Hölzel, N., Huber-Sannwald, E., Hughes, F. M., Jadán-Maza, O., Geissler, K., Jentsch, A., Ju, M., Kaseke, K. F., Kindermann, L., Koopman, J. E., Le Roux, P. C., Liancourt, P., Linstädter, A., Liu, J., Louw, M. A., Maggs-Kölling, G., Makhalanyane, T. P., Issa, O. M., Marais, E., Margerie, P., Mazaneda, A. J., McClaran, M. P., Messeder, J. V. S., Mora, J. P., Moreno, G., Munson, S. M., Nunes, A., Oliva, G., Oñatibia, G. R., Osborne, B., Peter, G., Pueyo, Y., Quiroga, R. E., Reed, S. C., Reyes, V. M., Rodríguez, A., Ruppert, J. C., Sala, O., Salah, A., Sebei, J., Sloan, M., Solongo, S., Stavi, I., Stephens, C. R. A., Teixido, A. L., Thomas, A. D., Throop, H. L., Tielbörger, K., Travers, S., Val, J., Valko, O., van den Brink, L., Velbert, F., Wamiti, W., Wang, D., Wang, L., Wardle, G. M., Yahdjian, L., Zaady, E., Zeberio, J. M., Zhang, Y., Zhou, X., Plaza, C.
Vulnerability of mineral-associated soil organic carbon to c…
No abstract in the library.
What changed what, as the paper reports it. Grouped by the measured property.
with mean annual temperaturesignificant · 0–7.5 cm · January 2016–September 2019, dry-season sampling · global drylands · Spatial climate association, not imposed warming or measured temporal change. Figure2e separate POC model MAT coefficient95%CI below zero; canopy interaction buffers the decline. Pooled3.2%/°C and pooled p-value not assigned to this fraction.
“**further observed that as mean annual temperature increased, POC and MAOC contents** 249 **decreased, but to a lesser extent, beneath vegetation.”
with mean annual precipitationsignificant · 0–7.5 cm · January 2016–September 2019, dry-season sampling · global drylands · Spatial climate association. Figure2e separate POC model MAP coefficient95%CI above zero; similar precipitation response beneath canopy and in open soil. No pooled6.6%/100mm or pooled P=0.039 assigned.
“**further observed that as mean annual temperature increased, POC and MAOC contents** 249 **decreased, but to a lesser extent, beneath vegetation. Conversely, as mean annual precipitation** 250 **increased, both contents increased in a similar manner in open areas and in areas under the**”
perennial vegetation vs. open areas not covered by perennial vegetationsignificant · 0–7.5 cm · January 2016–September 2019, dry-season sampling · global drylands · Observed vegetation/open microsites in same plots; not a randomized vegetation treatment. Figure2e POC cover contrast95%CI above zero. Positive MAT×cover interaction indicates buffering of the negative temperature association.
“Both POC and MAOC contents were higher in soil beneath perennial vegetation (Fig. 2).”
with mean annual temperaturesignificant · 0–7.5 cm · January 2016–September 2019, dry-season sampling · global drylands · Spatial climate association. Figure2e separate MAOC model MAT coefficient95%CI below zero; vegetation buffers negative slope. No pooled percentage or p-value assigned.
“**further observed that as mean annual temperature increased, POC and MAOC contents** 249 **decreased, but to a lesser extent, beneath vegetation.”
| Depth | Texture | Clay | pH | Organic C | Bulk density |
|---|---|---|---|---|---|
| 0–7.5 cm | – | – | – | – | – |
Li et al. · 2021 · Soil and Tillage Research
4 shared concepts
12 findings1 site
Ebabu et al. · 2022 · International Soil and Water Conservation Research
3 shared concepts
19 findings1 site
Sünnemann et al. · 2023 · Communications Earth & Environment
3 shared concepts
9 findings2 sites
Keller et al. · 2021 · Global Change Biology
4 shared concepts
14 findings9 sites
Franzluebbers, Reberg Horton & Creamer · 2020 · Soil Science Society of America Journal
3 shared concepts
19 findings1 site
with mean annual precipitationsignificant · 0–7.5 cm · January 2016–September 2019, dry-season sampling · global drylands · Spatial climate association. Figure2e separate MAOC model MAP coefficient95%CI above zero; similar response beneath canopy and in open soil. No pooled percentage/p-value assigned.
“**further observed that as mean annual temperature increased, POC and MAOC contents** 249 **decreased, but to a lesser extent, beneath vegetation. Conversely, as mean annual precipitation** 250 **increased, both contents increased in a similar manner in open areas and in areas under the**”
perennial vegetation vs. open areas not covered by perennial vegetationsignificant · 0–7.5 cm · January 2016–September 2019, dry-season sampling · global drylands · Observed vegetation/open microsites in same plots. Figure2e MAOC cover contrast95%CI above zero. Positive MAT×cover interaction indicates buffering of negative temperature association; no causality inferred.
“Both POC and MAOC contents were higher in soil beneath perennial vegetation (Fig. 2).”
