4.6 Article

The emission of volatile halocarbons by seaweeds and their response towards environmental changes

Journal

JOURNAL OF APPLIED PHYCOLOGY
Volume 32, Issue 2, Pages 1377-1394

Publisher

SPRINGER
DOI: 10.1007/s10811-019-02026-x

Keywords

Halocarbons; Bromoform; Air-Sea gas exchange; Climate change; Environmental change; Seaweed

Funding

  1. Phase II Higher Institution Centre of Excellence (HICoE) Fund
  2. Ministry of Education Malaysia [IOES-2014F]
  3. University of Malaya Top 100 Research University Grant [TU001D-2018]
  4. University of Malaya Postgraduate Research Funds, PPP [PG300-2016A]
  5. NERC [NE/J016047/1] Funding Source: UKRI

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Volatile halocarbons can deplete the protective stratospheric ozone layer contributing to global climate change and may even affect local climate through aerosol production. These compounds are produced through anthropogenic and biogenic processes. Biogenic halocarbons may be produced as defence compounds, anti-oxidants or by-products of metabolic processes. These compounds include very short-lived halocarbons (VSLH), e.g. bromoform (CHBr3), dibromomethane (CH2Br2), methyl iodide (CH3I), diiodomethane (CH2I2). Efforts to quantify the biogenic sources of these compounds, especially those of marine origin, e.g. seaweeds, phytoplankton and seagrass meadows, are often complicated by inherent biological variability as well as spatial and temporal changes in emissions. The contribution of the coastal region and the oceans to the stratospheric load of halocarbons has been widely debated. This highlights the need to understand the factors affecting the release of these compounds from marine sources for which data for modelling purposes are generally lacking. Seaweeds are important sources of biogenic halocarbons subjected to changing environmental conditions. Huge uncertainties in the prediction of current and future global halocarbon pool exist due to the lack of spatial and temporal data input from coastal and oceanic sources. Therefore, investigating the effect of changing environmental conditions on the emission of VSLH by the seaweeds could help towards better estimations of halocarbon emissions. This is especially important in light of global changes in both climate and the environment, the expansion of seaweed cultivation industry and the interactions between halocarbon emission and their environment. In this paper, we review current knowledge of seaweed halocarbon emissions, how environmental factors affect these emissions and identify gaps in understanding. Our aim is to direct much needed research to improve understanding of the contribution of marine biogenic sources of halocarbons and their impact on the environment.

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