PT  - JOURNAL ARTICLE
AU  - Sara Manafzadeh
AU  - Yannick M. Staedler
AU  - Hamid Moazzeni
AU  - David Masson
AU  - Jürg Schönenberger
AU  - Elena Conti
TI  - Response of oriental xerophytes to the occidental industrial revolution
AID  - 10.1101/173013
DP  - 2017 Jan 01
TA  - bioRxiv
PG  - 173013
4099  - http://biorxiv.org/content/early/2017/08/06/173013.short
4100  - http://biorxiv.org/content/early/2017/08/06/173013.full
AB  - Since the Industrial Revolution, human activities have contributed substantially to climate change, by adding CO2 to the atmosphere, especially since the mid-20th century (the “Great Acceleration”). Climatic change does not have the same impact on different regions of the Earth, neither in the recorded past, nor in models of the future. Therefore, to anticipate on these changes, we need to understand and be able to predict the possible responses of the different regional vegetations of the world to these changes, and most significantly to increased drought conditions. The aim of this study is to understand the response of the xerophytes of the immense oriental Irano-Turanian bioregion to post-industrial global warming and to compare it with the response of the xerophytes of the neighbouring occidental Mediterranean bioregion. We measured stomata index and stomata density from 83 herbarium sheets (coll. 1821-2014) from species of the non-succulent xerophyte, Haplophyllum. We tested for differences before and after the “Great Acceleration” in both bioregions. SI decreased in the occidental species (significant only for abaxial leaf side), whereas SI significantly increased in the oriental species (both sides). We suggest that changes in both occidental and oriental species are linked to atmospheric CO2 due to the different constraints that act on their growth. In light-limited occidental species, atmospheric CO2 caused the stomata index decrease, whereas in the predominantly water-limited oriental species, increased drought stress and temperature (climatic change) caused stomata index increase. In conclusion, we propose that whereas atmospheric CO2 directly caused a decrease in stomata index in occidental xerophytes, it indirectly caused an increase in stomata index in oriental xerophytes via climate change (increase in aridity, drought stress, and temperature). This study highlights the considerable potential of research based on historical herbarium collections to answer ecological questions, especially regarding climatic change.