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A meta‐analysis of climate change effects on forage quality in grasslands: specificities of mountain and M editerranean areas
Author(s) -
Dumont B.,
Andueza D.,
Niderkorn V.,
Lüscher A.,
Porqueddu C.,
PiconCochard C.
Publication year - 2015
Publication title -
grass and forage science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.716
H-Index - 56
eISSN - 1365-2494
pISSN - 0142-5242
DOI - 10.1111/gfs.12169
Subject(s) - forage , temperate climate , agronomy , climate change , environmental science , legume , biomass (ecology) , grassland , global warming , zoology , biology , ecology
Atmospheric carbon dioxide ( CO 2 ), global mean temperature and interannual variability in temperature and rainfall are expected to increase significantly by the end of the 21st century. To review the effects of these factors on forage quality, we carried out a meta‐analysis of climate manipulation experiments. The first notable result was a lack of effect of elevated CO 2 on structural carbohydrates and digestibility. Elevated CO 2 increased the total non‐structural carbohydrates of forage tissues by an average of 25% and decreased forage nitrogen ( N ) content by 8%. Increased legume abundance in multispecies swards can, however, maintain N concentration in the harvested biomass. There were no consistent effects of warming on contents of N , water‐soluble and structural carbohydrates, or on digestibility. We highlight the continuum in the effect of water availability, from drought to irrigation, with a curvilinear increase of forage N as water availability decreased. Digestibility increased, on average, by 7% with drought, but with strong experimental variations. The review places special emphasis on discussion of the specificities of mountain and M editerranean grasslands, the former being limited by low temperature, the latter by drought and heat. Elevated CO 2 decreased forage N content in mountain areas and in temperate plains alike. It increased N content by an average of 3% in M editerranean areas; this could be due to shifts in vegetation communities under elevated CO 2 or to a greater concentration of N in plant tissues under drought conditions. Further experiments are needed to investigate the effects of combined factors, including extreme climatic events.