Within-plant isoprene oxidation confirmed by direct emissions of oxidation products methyl vinyl ketone and methacrolein


Autoria(s): Jardine, Kolby J.; Monson, Russell K.; Abrell, Leif; Saleska, Scott R.; Arneth, Almut; Jardine, Angela; Ishida, Francoise Yoko; Yanez Serrano, Ana Maria; Artaxo Netto, Paulo Eduardo; Karl, Thomas; Fares, Silvano; Goldstein, Allen; Loreto, Francesco; Huxman, Travis
Contribuinte(s)

UNIVERSIDADE DE SÃO PAULO

Data(s)

05/11/2013

05/11/2013

2012

Resumo

Isoprene is emitted from many terrestrial plants at high rates, accounting for an estimated 1/3 of annual global volatile organic compound emissions from all anthropogenic and biogenic sources combined. Through rapid photooxidation reactions in the atmosphere, isoprene is converted to a variety of oxidized hydrocarbons, providing higher order reactants for the production of organic nitrates and tropospheric ozone, reducing the availability of oxidants for the breakdown of radiatively active trace gases such as methane, and potentially producing hygroscopic particles that act as effective cloud condensation nuclei. However, the functional basis for plant production of isoprene remains elusive. It has been hypothesized that in the cell isoprene mitigates oxidative damage during the stress-induced accumulation of reactive oxygen species (ROS), but the products of isoprene-ROS reactions in plants have not been detected. Using pyruvate-2-13C leaf and branch feeding and individual branch and whole mesocosm flux studies, we present evidence that isoprene (i) is oxidized to methyl vinyl ketone and methacrolein (iox) in leaves and that iox/i emission ratios increase with temperature, possibly due to an increase in ROS production under high temperature and light stress. In a primary rainforest in Amazonia, we inferred significant in plant isoprene oxidation (despite the strong masking effect of simultaneous atmospheric oxidation), from its influence on the vertical distribution of iox uptake fluxes, which were shifted to low isoprene emitting regions of the canopy. These observations suggest that carbon investment in isoprene production is larger than that inferred from emissions alone and that models of tropospheric chemistry and biotachemistryclimate interactions should incorporate isoprene oxidation within both the biosphere and the atmosphere with potential implications for better understanding both the oxidizing power of the troposphere and forest response to climate change.

Philecology Foundation of Fort Worth, Texas

Philecology Foundation of Fort Worth, Texas

National Science Foundation through the AMAZON-PIRE [0730305]

National Science Foundation through the AMAZONPIRE

[CHE 0216226]

Identificador

GLOBAL CHANGE BIOLOGY, MALDEN, v. 18, n. 3, supl. 1, Part 6, pp. 973-984, MAR, 2012

1354-1013

http://www.producao.usp.br/handle/BDPI/41126

10.1111/j.1365-2486.2011.02610.x

http://dx.doi.org/10.1111/j.1365-2486.2011.02610.x

Idioma(s)

eng

Publicador

WILEY-BLACKWELL

MALDEN

Relação

GLOBAL CHANGE BIOLOGY

Direitos

closedAccess

Copyright WILEY-BLACKWELL

Palavras-Chave #AMAZON #BIOSPHERE-ATMOSPHERE INTERACTIONS #ISOPRENE OXIDATION #METHACROLEIN #METHYL VINYL KETONE #REACTIVE OXYGEN SPECIES #TEMPERATURE STRESS #THERMOTOLERANCE #VOLATILE ORGANIC-COMPOUNDS #TROPICAL RAIN-FOREST #ATMOSPHERIC CHEMISTRY #COMPOUND EMISSIONS #OZONE #LEAVES #OXYGEN #STRESS #METABOLISM #MECHANISM #BIODIVERSITY CONSERVATION #ECOLOGY #ENVIRONMENTAL SCIENCES
Tipo

article

original article

publishedVersion