Land cover changes and greenhouse gas emissions in two different soil covers in the Brazilian Caatinga

• Published in: The Science of the total environment Vol. 571; pp. 1048 - 1057
• Main Authors: Ribeiro, Kelly, Sousa-Neto, Eráclito Rodrigues de, Carvalho, João Andrade de, Sousa Lima, José Romualdo de, Menezes, Rômulo Simões Cezar, Duarte-Neto, Paulo José, da Silva Guerra, Glauce, Ometto, Jean Pierre Henry Baulbaud
• Format: Journal Article
• Language: English
• Published: Netherlands Elsevier B.V 15.11.2016
• Subjects: Caatinga; Greenhouse gases (GHG); Land use/cover changes; Pasture; Brazil, Pernambuco; Greenhouse gases (GHG); Land use/cover changes; Caatinga; Pasture
• ISSN: 0048-9697; 1879-1026
• DOI: 10.1016/j.scitotenv.2016.07.095

The Caatinga biome covers an area of 844,453km2 and has enormous endemic biodiversity, with unique characteristics that make it an exclusive Brazilian biome. It falls within the earth's tropical zone and is one of the several important ecoregions of Brazil. This biome undergoes natural lengthy periods of drought that cause losses in crop and livestock productivity, having a severe impact on the population. Due to the vulnerability of this ecosystem to climate change, livestock has emerged as the main livelihood of the rural population, being the precursor of the replacement of native vegetation by grazing areas. This study aimed to measure GHG emissions from two different soil covers: native forest (Caatinga) and pasture in the municipality of São João, Pernambuco State, in the years 2013 and 2014. GHG measurements were taken by using static chamber techniques in both soil covers. According to a previous search, so far, this is the first study measuring GHG emissions using the static chamber in the Caatinga biome. N2O emissions ranged from −1.0 to 4.2mgm−2d−1 and −1.22 to 3.4mgm−2d−1 in the pasture and Caatinga, respectively, and they did not significantly differ from each other. Emissions were significantly higher during dry seasons. Carbon dioxide ranged from −1.1 to 14.1 and 1.2 to 15.8gm−2d−1 in the pasture and Caatinga, respectively. CO2 emissions were higher in the Caatinga in 2013, and they were significantly influenced by soil temperature, showing an inverse relation. Methane emission ranged from 6.6 to 6.8 and −6.0 to 4.8mgm−2d−1 in the pasture and Caatinga, respectively, and was significantly higher only in the Caatinga in the rainy season of 2014. Soil gas fluxes seemed to be influenced by climatic and edaphic conditions as well as by soil cover in the Caatinga biome. [Display omitted] •Land use/cover changes have altered biogeochemical cycles in the Caatinga.•Nitrous oxide and carbon dioxide emissions were significantly higher than methane.•Gaseous emissions correlated with soil temperature and moisture•There was no difference between emissions measured in native vegetation and pasture treatments.