Past and present land use influences on tropical riparian zones: an isotopic assessment with implications for riparian forest width determination

被引:8
|
作者
Salemi, Luiz Felippe [1 ,5 ]
Machado Lins, Silvia Rafaela [1 ]
Ravagnani, Elizabethe de Campos [1 ]
Magioli, Marcelo [2 ]
Martinez, Melissa Gaste [1 ]
Guerra, Fernando [3 ]
Vidas, Natassia Bonini [1 ]
Fransozi, Aline [4 ]
de Barros Ferraz, Silvio Frosini [4 ]
Martinelli, Luiz Antonio [1 ]
机构
[1] Univ Sao Paulo, Ctr Energia Nucl Agr, Lab Ecol Isotop, Piracicaba, SP, Brazil
[2] Univ Sao Paulo, Lab Ecol Manejo & Conservacao Fauna Silvestre, Escola Super Agr Luiz de Queiroz, Ciencias Florestais, Av Padua Dias 11, BR-13418900 Piracicaba, SP, Brazil
[3] Univ Sao Paulo, Ctr Energia Nucl Agr, Lab Fertilidade Solo, BR-13418900 Piracicaba, SP, Brazil
[4] Univ Sao Paulo, Lab Hidrol Florestal, Ciencias Florestais, Escola Super Agr Luiz de Queiroz, Av Padua Dias 11, BR-13418900 Piracicaba, SP, Brazil
[5] Univ Brasilia, Div Ciencias Vida & Terra, Fac Planaltina, Brasilia, DF, Brazil
来源
BIOTA NEOTROPICA | 2016年 / 16卷 / 02期
基金
巴西圣保罗研究基金会;
关键词
Watershed; Soil degradation; Organic matter; Sediment; Carbon cycling; ORGANIC-MATTER DYNAMICS; SEDIMENT DEPOSITION; CARBON; BRAZIL; SOILS; VEGETATION; SUGARCANE; RATIO;
D O I
10.1590/1676-0611-BN-2015-0133
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
In this article, by using carbon stable isotopes, we assessed the past and present land use influences that riparian areas are subject within agricultural landscapes. Emphasis is given to the understanding of the effects of the 2012 Brazilian Forest Act on such areas. We selected five riparian areas within a highly C-4 dominated agricultural landscape. Three of them had 30 meters native riparian forest buffer (NRFB) and two of them had 8 meter and no NRFB. We used three 100 meter-transects located 5, 15 and 30 meters relative to stream channel to obtain soil samples (0 - 10 cm). All riparian areas presented soil carbon isotopic signatures that are not C-3 (native forests) irrespective of having or not 30 meters NRFB. Two cases presenting less than 30 meters NRFB had higher C-4 derived carbon contribution. All of the other three areas that followed the 30 meters NRFB presented, to some degree, C-4 derived carbon, which was attributed to C-4 organic matter deposition originated from cultivated areas and, in one case, to the persistence of former exotic grasses. With the 2012 Forest Act allowing narrower buffers (<30 meters), we expect C-4 contributions to soil organic matter to remain high in riparian areas and streams within agricultural landscapes dominated by C-4 plants where 30 meter NRFB is no longer required. Such contributions will likely continue to have detrimental effects on stream water quality and biota.
引用
收藏
页数:8
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