Effects of long-term inter-annual rainfall variation on the dynamics of regenerative communities during the old-field succession of a neotropical dry forest

2018 ◽  
Vol 426 ◽  
pp. 91-100 ◽  
Author(s):  
Miguel Martínez-Ramos ◽  
Patricia Balvanera ◽  
Felipe Arreola Villa ◽  
Francisco Mora ◽  
José Manuel Maass ◽  
...  
2021 ◽  
Vol 482 ◽  
pp. 118810
Author(s):  
Miguel Martínez-Ramos ◽  
Felipe Barragán ◽  
Francisco Mora ◽  
Susana Maza-Villalobos ◽  
Luis F. Arreola-Villa ◽  
...  

2016 ◽  
Vol 19 (9) ◽  
pp. 1101-1109 ◽  
Author(s):  
Shao-peng Li ◽  
Marc W. Cadotte ◽  
Scott J. Meiners ◽  
Zhichao Pu ◽  
Tadashi Fukami ◽  
...  

2016 ◽  
Vol 65 ◽  
pp. 44-54 ◽  
Author(s):  
Sonja Knapp ◽  
Jutta Stadler ◽  
Alexander Harpke ◽  
Stefan Klotz

2017 ◽  
Vol 3 (1) ◽  
pp. 107-116 ◽  
Author(s):  
Gema Escribano-Avila ◽  
Laura Cervera ◽  
Leonardo Ordóñez-Delgado ◽  
Andrea Jara-Guerrero ◽  
Luis Amador ◽  
...  

2011 ◽  
Vol 262 (6) ◽  
pp. 916-930 ◽  
Author(s):  
Kurt P. McLaren ◽  
Mathieu Lévesque ◽  
Chait Sharma ◽  
Byron Wilson ◽  
Morag A. McDonald

Plant Ecology ◽  
2014 ◽  
Vol 215 (10) ◽  
pp. 1081-1097 ◽  
Author(s):  
Milena Niño ◽  
Kurt P. McLaren ◽  
Henrik Meilby ◽  
Mathieu Lévesque ◽  
Byron Wilson ◽  
...  

Agriculture ◽  
2021 ◽  
Vol 11 (3) ◽  
pp. 215
Author(s):  
Liudmila Tripolskaja ◽  
Asta Kazlauskaite-Jadzevice ◽  
Virgilijus Baliuckas ◽  
Almantas Razukas

Ex-arable land-use change is a global issue with significant implications for climate change and impact for phytocenosis productivity and soil quality. In temperate humid grassland, we examined the impact of climate variability and changes of soil properties on 23 years of grass productivity after conversion of ex-arable soil to abandoned land (AL), unfertilized, and fertilized managed grassland (MGunfert and MGfert, respectively). This study aimed to investigate the changes between phytocenosis dry matter (DM) yield and rainfall amount in May–June and changes of organic carbon (Corg) stocks in soil. It was found that from 1995 to 2019, rainfall in May–June tended to decrease. The more resistant to rainfall variation were plants recovered in AL. The average DM yield of MGfert was 3.0 times higher compared to that in the AL. The DM yields of AL and MG were also influenced by the long-term change of soil properties. Our results showed that Corg sequestration in AL was faster (0.455 Mg ha−1 year−1) than that in MGfert (0.321 Mg ha−1 year−1). These studies will be important in Arenosol for selecting the method for transforming low-productivity arable land into MG.


2009 ◽  
Vol 9 (5) ◽  
pp. 1579-1595 ◽  
Author(s):  
C. Galy-Lacaux ◽  
D. Laouali ◽  
L. Descroix ◽  
N. Gobron ◽  
C. Liousse

Abstract. Long-term precipitation chemistry have been recorded in the rural area of Banizoumbou (Niger), representative of a semi-arid savanna ecosystem. A total of 305 rainfall samples ~90% of the total annual rainfall) were collected from June 1994 to September 2005. From ionic chromatography, pH major inorganic and organic ions were detected. Rainwater chemistry is controlled by soil/dust emissions associated with terrigeneous elements represented by SO42−, Ca2+, Carbonates, K+ and Mg2+. It is found that calcium and carbonates represent ~40% of the total ionic charge. The second highest contribution is nitrogenous, with annual Volume Weighed Mean (VWM) for NO3− and NH4+ concentrations of 11.6 and 18.1 μeq.l−1, respectively. This is the signature of ammonia sources from animals and NOx emissions from savannas soil-particles rain-induced. The mean annual NH3 and NO2 air concentration are of 6 ppbv and 2.6 ppbv, respectively. The annual VWM precipitation concentration of sodium and chloride are both of 8.7 μeq.l−1 which reflects the marine signature of monsoonal and humid air masses. The median pH value is of 6.05. Acidity is neutralized by mineral dust, mainly carbonates, and/or dissolved gases such NH3. High level of organic acidity with 8μeq.l−1 and 5.2 μeq.l−1 of formate and acetate were also found. The analysis of monthly Black Carbon emissions and Fraction of Absorbed Photosynthetically Active Radiation (FAPAR) values show that both biogenic emission from vegetation and biomass burning could explain the rainfall organic acidity content. The interannual variability of the VWM concentrations around the mean (1994–2005) is between ±5% and ±30% and mainly due to variations of sources strength and rainfall spatio-temporal distribution. From 1994 to 2005, the total mean wet deposition flux in the Sahelian region is of 60.1 mmol.m−2.yr−1 ±25%. Finally, Banizoumbou measurements are compared to other long-term measurements of precipitation chemistry in the wet savanna of Lamto (Côte d'Ivoire) and in the forested zone of Zoétélé (Cameroon). The total chemical loading presents a maximum in the dry savanna and a minimum in the forest (from 143.7, 100.2 to 86.6 μeq.l−1), associated with the gradient of terrigeneous sources. The wet deposition fluxes present an opposite trend, with 60.0 mmol.m−2.yr−1 in Banizoumbou, 108.6 mmol.m−2.yr−1 in Lamto and 162.9 mmol.m−2.yr−1 in Zoétélé, controlled by rainfall gradient along the ecosystems transect.


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