Forest islands in an agricultural sea.

2014 ◽  
pp. 79-95 ◽  
Author(s):  
A. M. Klein ◽  
V. Boreux ◽  
J. Bauhus ◽  
M. J. Chappell ◽  
J. Fischer ◽  
...  
Keyword(s):  
Ecosphere ◽  
2021 ◽  
Vol 12 (5) ◽  
Author(s):  
Ana Filipa Palmeirim ◽  
Maíra Benchimol ◽  
Inara R. Leal ◽  
Carlos A. Peres

2017 ◽  
Vol 23 (12) ◽  
pp. 5383-5397 ◽  
Author(s):  
Amy K. Langston ◽  
David A. Kaplan ◽  
Francis E. Putz

2021 ◽  
Vol 9 (2) ◽  
pp. 283
Author(s):  
Amelie Baomalgré Bougma ◽  
Korodjouma Ouattara ◽  
Halidou Compaore ◽  
Hassan Bismarck Nacro ◽  
Caleb Melenya ◽  
...  

In the more mesic savanna areas of West Africa, many areas of relatively tall and dense vegetation with a species composition more characteristic of forest than savanna are often found around villages areas. These ‘forest islands’ may be the direct action of human activity. To better understand these patches with relatively luxuriant vegetation, our study focused on how they influence soil aggregation in comparison with nearby areas and natural savanna vegetation across a precipitation transect in West Africa for which mean annual precipitation at the study sites ranges from 0.80 to 1.27 m a-1. Soil samples were taken from 0 to 5 cm and 5 to 10 cm depths and aggregate groups with diameters: > 500 μm, 500-250 μm and 250-53 μm (viz. “macroaggregates”, “mesoaggregates” and “microaggregates”) determined using the wet sieving method. The results showed significantly higher proportion of stable meso and macroaggregates in forest islands and natural savanna compared to agricultural soils (p <0.05). On the other hand, although there was no effect of land-use type on microaggregates stability, there was a strong tendency for the microaggregate fraction across all land use types to increase with increasing precipitation. Soil organic carbon and iron oxides contents are the most important factors influencing aggregate stability in West African ecosystems. By increasing soil structural stability, forest islands contribute to soil erosion reduction and the control of land degradation.


Bothalia ◽  
1983 ◽  
Vol 14 (3/4) ◽  
pp. 579-585 ◽  
Author(s):  
G. Paradis

Southern Benin has a dry subequatoriai climate with a rainfall gradient from 850 mm in the west to 1 500 mm in the east, the geomorphology is varied and the vegetation has been subjected to strong human influence. There are numerous plant formations, namely: 1, forest islands which are probably relics of the primitive vegetation and include (a) dense semi-deciduous forests of several types, (b) swamp forests of two types, (c) periodically flooded forest of two types, (d) Lophira lanceolata  (Hutchinson Dalziel, 1954-72) woodlands and (e) mangrove swamps; 2, formations which are probably derived and include (a) thickets of several types, (b) tree savannas and shrub savannas, (c) grassy savannas and prairies varying according to soil characteristics and (d) halophytic grasslands; and 3, floating vegetation on fresh-water lakes.


2019 ◽  
Vol 5 (4) ◽  
pp. eaav5449 ◽  
Author(s):  
José M. Capriles ◽  
Umberto Lombardo ◽  
Blaine Maley ◽  
Carlos Zuna ◽  
Heinz Veit ◽  
...  

The Amazon witnessed the emergence of complex societies after 2500 years ago that altered tropical landscapes through intensive agriculture and managed aquatic systems. However, very little is known about the context and conditions that preceded these social and environmental transformations. Here, we demonstrate that forest islands in the Llanos de Moxos of southwestern Amazonia contain human burials and represent the earliest settlements in the region between 10,600 and 4000 years ago. These archaeological sites and their contents represent the earliest evidence of communities that experienced conditions conducive to engaging with food production such as environmental stability, resource disturbance, and increased territoriality in the Amazonian tropical lowlands.


2003 ◽  
Vol 19 (05) ◽  
pp. 509-524 ◽  
Author(s):  
Richard G. Davies ◽  
Luis M. Hernández ◽  
Paul Eggleton ◽  
Raphael K. Didham ◽  
Laura L. Fagan ◽  
...  

Insects ◽  
2020 ◽  
Vol 11 (5) ◽  
pp. 278 ◽  
Author(s):  
Vanessa Diniz e Silva ◽  
Marina Vale Beirão ◽  
Danon Clemes Cardoso

Ectothermic organisms, such as insects, are highly temperature dependent and are good models for studies that predict organisms’ responses to global climate change. Predicting how climate change may affect species distributions is a complicated task. However, it is possible to estimate species’ physiological constraints through maximum critical temperature, which may indicate if the species can tolerate new climates. Butterflies are useful organisms for studies of thermal tolerance. We tested if species have different thermal tolerances and if different habitats influence the thermal tolerance of the butterflies present in Brazil’s campo rupestre (open areas) and forest islands (shaded areas). A total of 394 fruit-feeding butterflies, comprising 45 species, were tested. The results separated the species into two statistically different groups: the resistant species with maximum critical temperature of 53.8 ± 7.4 °C, and the non-resistant species with maximum critical temperature of 48.2 ± 7.4 °C. The species of butterflies displayed differences in maximum critical temperature between the campo rupestre and forest islands that can be related to the two distinct habitats, but this did not correlate phylogenetically. Species from the forest islands were also divided into two groups, “resistant” and “non-resistant”, probably due to the heterogeneity of the habitat; the forest islands have a canopy, and in the understory, there are shaded and sunny areas. Species from forest islands, especially species that displayed lower thermal tolerance, may be more susceptible to global warming.


2009 ◽  
Vol 258 (2) ◽  
pp. 71-80 ◽  
Author(s):  
Rosa Maria Román-Cuesta ◽  
Marc Gracia ◽  
Javier Retana

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