Abstract

Abstract. We report here production rates of isoprene and monoterpene compounds (α-pinene, β-pinene, camphene and d-limonene) from six phytoplankton monocultures as a function of irradiance and temperature. Irradiance experiments were carried out for diatom strains (Thalassiosira weissflogii and Thalassiosira pseudonana), prymnesiophyte strains (Pleurochrysis carterae), dinoflagellate strains (Karenia brevis and Prorocentrum minimum), and cryptophyte strains (Rhodomonas salina), while temperature experiments were carried out for diatom strains (Thalassiosira weissflogii and Thalassiosira pseudonana). Phytoplankton species, incubated in a climate-controlled room, were subject to variable light (90 to 900 μmol m−2 s−1) and temperature (18 to 30 °C) regimes. Compared to isoprene, monoterpene emissions were an order of magnitude lower at all light and temperature levels. Emission rates are normalized by cell count and Chlorophyll a (Chl a) content. Diatom strains were the largest emitters, with ~ 2 × 10−17 g(cell)−1h−1 (~ 35 μg (g Chl a)−1 h−1) for isoprene and ~ 5 × 10−19 g (cell)−1 h−1 (~ 1 μg (g Chl a)−1) h−1) for α-pinene. The contribution to the total monoterpene production was ~ 70% from α-pinene, ~ 20% for d-limonene, and < 10% for camphene and β-pinene. Phytoplankton species showed a rapid increase in production rates at low irradiance (< 150 μmol m−2 s−1) and a gradual increase at high (> 250 μmol m−2 s−1) irradiance. Measurements revealed different patterns for time-averaged emissions rates over two successive days. On the first day, most of the species showed a distinct increase in production rates within the first 4 h while, on the second day, the emission rates were overall higher, but less variable. The data suggest that enhanced amounts of isoprene and monoterpenes are emitted from phytoplankton as a result of perturbations in environmental conditions that cause imbalance in chloroplasts and force primary producers to acclimate physiologically. This relationship could be a valuable tool for development of dynamic ecosystem modeling approaches for global marine isoprene and monoterpene emissions based on phytoplankton physiological responses to a changing environment.

Highlights

  • The age of global warming has brought about a heightened amount of attention to the interactions between life and the Earth’s climate

  • Since species response to stress can be related to changes in cellular chlorophyll content, we have chosen to use phytoplankton cell number as the base and Chlorophyll a (Chl a) concentration as a supplement to normalize isoprene and monoterpene emission rates for these experiments

  • Production of isoprene and monoterpenes in plants proceeds through a methylerythritol phosphate (MEP) metabolic pathway that is strongly tied to photosynthesis of primary producers through chlorophyll and carotenoid synthesis (Lichtenthaler, 2009)

Read more

Summary

Introduction

The age of global warming has brought about a heightened amount of attention to the interactions between life and the Earth’s climate. Global climate models with advanced treatment of manmade aerosols and pollutants and their interactions with clouds have been widely used for calculations from climate sensitivity to greenhouse gas emissions. A lesser-known uncertainty in climate predictions as a result of natural aerosols has only recently been explored (Meskhidze et al, 2011; Carslaw et al, 2013). As estimates of anthropogenic forcing are based on a pre-industrial atmosphere composed mainly of natural aerosols, the representation of natural aerosols in climate models strongly influences the predictions of current and future climate effects of anthropogenic aerosols (Hoose et al, 2009). Data analysis shows that up to 45 % of the variance of aerosol forcing arises from uncertainties in natural emissions of volcanic sulfur dioxide, marine dimethyl sulfide, biogenic volatile organic carbon (BVOC), biomass burning, and sea Published by Copernicus Publications on behalf of the European Geosciences Union

Results
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call