Flood pulse dynamics affects exploitation of both aquatic and terrestrial prey by Amazonian floodplain settlements

2016 ◽  
Vol 201 ◽  
pp. 129-136 ◽  
Author(s):  
Whaldener Endo ◽  
Carlos A. Peres ◽  
Torbjørn Haugaasen
Keyword(s):  
Water ◽  
2021 ◽  
Vol 13 (21) ◽  
pp. 3034
Author(s):  
Dirk Thielen ◽  
Paolo Ramoni-Perazzi ◽  
Mary L. Puche ◽  
Marco Márquez ◽  
José Isrrael Quintero ◽  
...  

The Pantanal is the largest wetland of the world and one of the most important biodiversity hotspots in South America. An unprecedented ongoing megadrought is severely affecting its ecological functioning, flood pulse dynamics, and fire regime. Regarding this problematic, the present study generates reliable information about the following key issues: 1—Evolution and dynamics, 2—Origin and determinants, and 3—Forecast based on identified determinants and current trends. Results show that the evolution of the megadrought has been differentiable in both, space and time. As for its origin and determinants, Climate Change was ratified as one of the most important threats to the Pantanal, and to vast areas of South America, since a strong correlation was identified between megadrought’s dynamics and the occurrence of intense marine heatwaves at Northern Hemisphere oceanic waters, and more specifically, at the Northeast Pacific. Results also show that the megadrought is expected to continue at both the Pantanal and the surrounding Highlands, at least until December 2023. Thus, an intensification of fires risk, extending now to areas historically flooded or perhumid should be expected, concomitantly to a very negative impact on non-fire-resistant vegetation cover, as well as ecosystem functioning and biodiversity, perhaps even worse than those from 2020, widely covered by the international media.


2016 ◽  
Vol 44 (2) ◽  
pp. 293-304 ◽  
Author(s):  
Rafael Hernandez Guzman ◽  
Arturo Ruiz Luna ◽  
Cesar A. Berlanga Robles ◽  
Jesus T. Ponce Palafox

Wetlands ◽  
2018 ◽  
Vol 38 (5) ◽  
pp. 975-991 ◽  
Author(s):  
Gisele Catian ◽  
Danilo Muniz da Silva ◽  
Yzel Rondon Súarez ◽  
Edna Scremin-Dias

2020 ◽  
Vol 25 (1) ◽  
pp. 69-75 ◽  
Author(s):  
Christopher P. Bonvillain ◽  
Quenton C. Fontenot

Abstract Anthropogenic modifications to river-floodplain systems can decouple floodplains from mainstem inputs, alter flood pulse dynamics, and disrupt population dynamics and trophic web stability of aquatic biota. The Atchafalaya River Basin (ARB) receives an annual flood pulse from the Mississippi River that contributes to high crayfish abundance. Conversely, reduced crayfish abundance in the Barataria Basin (BB) is attributed to the system no longer receiving an annual flood pulse from the Mississippi River. Therefore, the purpose of this research was to determine if the absence of an annual flood pulse and reduced crayfish abundance influenced the diets of carnivorous fishes by examining stomach contents of fishes from both basins. Stomach contents were grouped as crayfish, fish, non-crayfish invertebrate, and herpetological. Although the percent occurrence of crayfish in fish stomachs differed between floodplain inundation and low-water periods in the ARB, crayfish were still the major diet constituent of ARB fishes during both periods. Non-crayfish invertebrate was the major diet constituent in BB fishes, with crayfish ranking as the second fewest diet constituent present. Our results demonstrate how flood pulse dynamics influence crayfish, and ultimately trophic webs, in large river-floodplain systems.


Ecology ◽  
2000 ◽  
Vol 81 (10) ◽  
pp. 2730-2741 ◽  
Author(s):  
Arthur C. Benke ◽  
Indrajeet Chaubey ◽  
G. Milton Ward ◽  
E. Lloyd Dunn

2012 ◽  
Vol 78 (2) ◽  
pp. 285-294 ◽  
Author(s):  
Michael M. McGlue ◽  
Aguinaldo Silva ◽  
Hiran Zani ◽  
Fabrício A. Corradini ◽  
Mauro Parolin ◽  
...  

AbstractThe Pantanal is the world's largest tropical wetland and a biodiversity hotspot, yet its response to Quaternary environmental change is unclear. To address this problem, sediment cores from shallow lakes connected to the Upper Paraguay River (PR) were analyzed and radiocarbon dated to track changes in sedimentary environments. Stratal relations, detrital particle size, multiple biogeochemical indicators, and sponge spicules suggest fluctuating lake-level lowstand conditions between ~ 11,000 and 5300 cal yr BP, punctuated by sporadic and in some cases erosive flood flows. A hiatus has been recorded from ~ 5300 to 2600 cal yr BP, spurred by confinement of the PR within its channel during an episode of profound regional drought. Sustained PR flooding caused a transgression after ~ 2600 cal yr BP, with lake-level highstand conditions appearing during the Little Ice Age. Holocene PR flood pulse dynamics are best explained by variability in effective precipitation, likely driven by insolation and tropical sea-surface temperature gradients. Our results provide novel support for hypotheses on: (1) stratigraphic discontinuity of floodplain sedimentary archives; (2) late Holocene methane flux from Southern Hemisphere wetlands; and (3) pre-colonial indigenous ceramics traditions in western Brazil.


2021 ◽  
Author(s):  
Aifang Chen ◽  
Junguo Liu ◽  
Matti Kummu ◽  
Olli Varis ◽  
Qiuhong Tang ◽  
...  

2013 ◽  
Vol 30 (4) ◽  
pp. 1077 ◽  
Author(s):  
Alexander O. Korotkevich ◽  
Kathryn E. Rasmussen ◽  
Gregor Kovačič ◽  
Victor Roytburd ◽  
Andrei I. Maimistov ◽  
...  

2014 ◽  
Vol 40 (2) ◽  
pp. 455-462 ◽  
Author(s):  
Elizabeth C. Minor ◽  
Brandy Forsman ◽  
Stephanie J. Guildford

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