2008
DOI: 10.1016/j.agrformet.2008.03.013
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Assessment and up-scaling of CO2 exchange by patches of the herbaceous vegetation mosaic in a Portuguese cork oak woodland

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Cited by 20 publications
(19 citation statements)
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“…Peak ANPP, occurring in May 2012, gave values of 241 and 235 g m −2 in the 3-and 6-weekly watering treatment, respectively. Previous single-year studies on peak ANPP of the herbaceous understorey vegetation in evergreen woodlands in Iberia report values of 195-250 g m −2 (Castro and Freitas, 2009;Hussain et al, 2009;Li et al, 2008). However, Vázquez- de-Aldana et al (2008) reported large interannual variations of ANPP over a 20-year period, values ranging from 50 to 419 g m −2 , with ANPP correlated with annual precipitation.…”
Section: Precipitation Variabilitymentioning
confidence: 88%
“…Peak ANPP, occurring in May 2012, gave values of 241 and 235 g m −2 in the 3-and 6-weekly watering treatment, respectively. Previous single-year studies on peak ANPP of the herbaceous understorey vegetation in evergreen woodlands in Iberia report values of 195-250 g m −2 (Castro and Freitas, 2009;Hussain et al, 2009;Li et al, 2008). However, Vázquez- de-Aldana et al (2008) reported large interannual variations of ANPP over a 20-year period, values ranging from 50 to 419 g m −2 , with ANPP correlated with annual precipitation.…”
Section: Precipitation Variabilitymentioning
confidence: 88%
“…Air temperature inside and outside the chambers was logged continuously during measurements, and temperature inside the chambers was maintained within 1 • C relative to ambient temperature using ice packs. For a more detailed description of the chamber design and functioning, see Li et al (2008). As the measurements of F NET and F R were closely associated in time, estimations of gross CO 2 uptake (F A ) were made by subtraction of F R from F NET (F A = F R − F NET ).…”
Section: Co 2 and Water Vapour Fluxesmentioning
confidence: 99%
“…This led to an increase in total soil N input as observed between March and May. Major input of soil organic matter in the open locations of the montado ecosystem comes from the herbaceous vegetation, which actively photosynthesises during spring (Pereira et al, 2007;Aires et al, 2008;Li et al, 2008). Development of the herbaceous biomass in spring, therefore, is likely to increase N mineralization through increased inputs of labile organic compounds and total organic and respirable carbon (Hook et al, 1991).…”
Section: à2mentioning
confidence: 99%
“…The herbaceous layer has a rich biological diversity and is considered as habitats to be preserved (Moreno et al, 2005a). Due to its extent, the herbaceous layer provides a larger photosynthetic surface compared to the trees and could play a significant role in carbon fixation and ecosystem productivity (Pereira et al, 2007;Aires et al, 2008;Li et al, 2008) as well as influence soil nutrient and water balance (Joffre, 1990;Moreno et al, 2007). Due to the semiarid nature of the montado, the life cycle of the herbaceous plant community is confined to spring when soil moisture and temperatures favor their growth and development (Otieno et al, 2006;Pereira et al, 2007).…”
Section: Introductionmentioning
confidence: 99%