A compositional turnover zone of biogeographical magnitude within lowland Amazonia

2016 ◽  
Vol 43 (12) ◽  
pp. 2400-2411 ◽  
Author(s):  
Hanna Tuomisto ◽  
Gabriel M. Moulatlet ◽  
Henrik Balslev ◽  
Thaise Emilio ◽  
Fernando O. G. Figueiredo ◽  
...  
Keyword(s):  
2018 ◽  
Vol 15 (1) ◽  
pp. 279-295 ◽  
Author(s):  
Corina Buendía ◽  
Axel Kleidon ◽  
Stefano Manzoni ◽  
Björn Reu ◽  
Amilcare Porporato

Abstract. Phosphorus (P) availability decreases with soil age and potentially limits the productivity of ecosystems growing on old and weathered soils. Despite growing on ancient soils, ecosystems of lowland Amazonia are highly productive and are among the most biodiverse on Earth. P eroded and weathered in the Andes is transported by the rivers and deposited in floodplains of the lowland Amazon basin creating hotspots of P fertility. We hypothesize that animals feeding on vegetation and detritus in these hotspots may redistribute P to P-depleted areas, thus contributing to dissipate the P gradient across the landscape. Using a mathematical model, we show that animal-driven spatial redistribution of P from rivers to land and from seasonally flooded to terra firme (upland) ecosystems may sustain the P cycle of Amazonian lowlands. Our results show how P imported to land by terrestrial piscivores in combination with spatial redistribution of herbivores and detritivores can significantly enhance the P content in terra firme ecosystems, thereby highlighting the importance of food webs for the biogeochemical cycling of Amazonia.


Biotropica ◽  
2018 ◽  
Vol 50 (5) ◽  
pp. 758-767 ◽  
Author(s):  
Pablo Pérez Chaves ◽  
Kalle Ruokolainen ◽  
Hanna Tuomisto

2009 ◽  
Vol 142 (10) ◽  
pp. 2131-2139 ◽  
Author(s):  
Ivan Castro-Arellano ◽  
Steven J. Presley ◽  
Michael R. Willig ◽  
Joseph M. Wunderle ◽  
Luiz N. Saldanha

2007 ◽  
Vol 138 (1-2) ◽  
pp. 269-285 ◽  
Author(s):  
Ivan Castro-Arellano ◽  
Steven J. Presley ◽  
Luis Nelio Saldanha ◽  
Michael R. Willig ◽  
Joseph M. Wunderle

1984 ◽  
Vol 21 (3) ◽  
pp. 369-375 ◽  
Author(s):  
Kenneth E. Campbell ◽  
David Frailey

A thick blanket of Holocene alluvium lies over southwestern lowland Amazonia, and may possibly occur throughout much of the Amazon Basin. These deposits resulted from massive, seasonal flooding from about 11,000 to about 5000 yr B.P. that was followed by two cycles of erosion and deposition. Interpretations based on these geologic data suggest that southwestern lowland Amazonia is ecologically an “island” in a state of supersaturated disequilibrium as a result of colonization from Pleistocene refugia on its perimeter, and that habitats of highest diversity may be the most recent in origin. Conservation efforts and studies of Amazonian biogeography, soils, and paleoethnography should be reevaluated in light of the geologic data.


PLoS ONE ◽  
2010 ◽  
Vol 5 (12) ◽  
pp. e15822 ◽  
Author(s):  
Elsa Youngsteadt ◽  
Patricia Guerra Bustios ◽  
Coby Schal

The Holocene ◽  
2000 ◽  
Vol 10 (5) ◽  
pp. 543-553 ◽  
Author(s):  
Mark B. Bush ◽  
Michael C. Miller ◽  
Paulo E. De Oliveira ◽  
Paul A. Colinvaux

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