Bedoukian   RussellIPM   RussellIPM   Piezoelectric Micro-Sprayer


Home
Animal Taxa
Plant Taxa
Semiochemicals
Floral Compounds
Semiochemical Detail
Semiochemicals & Taxa
Synthesis
Control
Invasive spp.
References

Abstract

Guide

Alphascents
Pherobio
InsectScience
E-Econex
Counterpart-Semiochemicals
Print
Email to a Friend
Kindly Donate for The Pherobase

« Previous AbstractTo court or not to court - a multimodal sensory decision in Drosophila males    Next AbstractSeparating direct and indirect effects of rising temperatures on biogenic volatile emissions in the Arctic »

Plant Cell Environ


Title:Plant volatiles in extreme terrestrial and marine environments
Author(s):Rinnan R; Steinke M; McGenity T; Loreto F;
Address:"Terrestrial Ecology Section, Department of Biology, University of Copenhagen, Copenhagen O, DK-2100, Denmark; Centre for Permafrost (CENPERM), University of Copenhagen, Copenhagen K, DK-1350, Denmark"
Journal Title:Plant Cell Environ
Year:2014
Volume:20140425
Issue:8
Page Number:1776 - 1789
DOI: 10.1111/pce.12320
ISSN/ISBN:1365-3040 (Electronic) 0140-7791 (Linking)
Abstract:"This review summarizes the current understanding on plant and algal volatile organic compound (VOC) production and emission in extreme environments, where temperature, water availability, salinity or other environmental factors pose stress on vegetation. Here, the extreme environments include terrestrial systems, such as arctic tundra, deserts, CO(2) springs and wetlands, and marine systems such as sea ice, tidal rock pools and hypersaline environments, with mangroves and salt marshes at the land-sea interface. The emission potentials at fixed temperature and light level or actual emission rates for phototrophs in extreme environments are frequently higher than for organisms from less stressful environments. For example, plants from the arctic tundra appear to have higher emission potentials for isoprenoids than temperate species, and hypersaline marine habitats contribute to global dimethyl sulphide (DMS) emissions in significant amounts. DMS emissions are more widespread than previously considered, for example, in salt marshes and some desert plants. The reason for widespread VOC, especially isoprenoid, emissions from different extreme environments deserves further attention, as these compounds may have important roles in stress resistance and adaptation to extremes. Climate warming is likely to significantly increase VOC emissions from extreme environments both by direct effects on VOC production and volatility, and indirectly by altering the composition of the vegetation"
Keywords:"Arctic Regions Butadienes/metabolism Climate Desert Climate *Environment Hemiterpenes/metabolism Light Monoterpenes/metabolism Pentanes/metabolism Plants/*metabolism Seawater Stress, Physiological Temperature Volatile Organic Compounds/*metabolism Arctic;"
Notes:"MedlineRinnan, Riikka Steinke, Michael McGenity, Terry Loreto, Francesco eng Research Support, Non-U.S. Gov't Review 2014/03/08 Plant Cell Environ. 2014 Aug; 37(8):1776-89. doi: 10.1111/pce.12320. Epub 2014 Apr 25"

 
Back to top
 
Citation: El-Sayed AM 2024. The Pherobase: Database of Pheromones and Semiochemicals. <http://www.pherobase.com>.
© 2003-2024 The Pherobase - Extensive Database of Pheromones and Semiochemicals. Ashraf M. El-Sayed.
Page created on 13-11-2024