4.6 Article

Phytoplankton Sources and Sinks of Dimethylsulphoniopropionate (DMSP) in Temperate Coastal Waters of Australia

Journal

MICROORGANISMS
Volume 10, Issue 8, Pages -

Publisher

MDPI
DOI: 10.3390/microorganisms10081539

Keywords

sulfur cycling; DMSP uptake; Trichodesmium; diatoms; size fractions; phytoplankton; east Australia

Categories

Funding

  1. Australian Research Council [DP140101045]
  2. School of Life Sciences and Climate Change Cluster, University of Technology Sydney

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This study tracked and analyzed the uptake and distribution of DMSP in a natural marine microbial community collected from the eastern coastline of Australia. The results revealed active uptake of DMSP in all size fractions of the community, with the largest fraction forming the major DMSP sink. Evidence for DMSP catabolism was observed in all size fractions, indicating loss from the system. Based on taxonomic diversity, the sources of DMSP were likely dinoflagellates, Phaeocystis sp., and Trichodesmium sp., while the sinks for DMSP were diatoms and picoeucaryotes in this temperate community.
The ecologically important organic sulfur compound, dimethylsulfoniopropionate (DMSP), is ubiquitous in marine environments. Produced by some species of phytoplankton and bacteria, it plays a key role in cellular responses to environmental change. Recently, uptake of DMSP by non-DMSP-producing phytoplankton species has been demonstrated, highlighting knowledge gaps concerning DMSP distribution through the marine microbial food web. In this study, we traced the uptake and distribution of DMSP through a natural marine microbial community collected from off the eastern coastline Australia. We found a diverse phytoplankton community representing six major taxonomic groups and conducted DMSP-enrichment experiments both on the whole community, and the community separated into large (>= 8.0 mu m), medium (3.0-8.0 mu m), and small (0.2-3.0 mu m) size fractions. Our results revealed active uptake of DMSP in all three size fractions of the community, with the largest fraction (>8 mu m) forming the major DMSP sink, where enrichment resulted in an increase of DMSPp by 144%. We observed evidence for DMSP catabolism in all size fractions with DMSP enrichment, highlighting loss from the system via MeSH or DMS production. Based on taxonomic diversity, we postulate the sources of DMSP were the dinoflagellates, Phaeocystis sp., and Trichodesmium sp., which were present in a relatively high abundance, and the sinks for DMSP were the diatoms and picoeucaryotes in this temperate community. These findings corroborate the role of hitherto disregarded phytoplankton taxa as potentially important players in the cycling of DMSP in coastal waters of Australia and emphasize the need to better understand the fate of accumulated DMSP and its significance in cellular metabolism of non-DMSP producers.

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