Trends in the abundance of picophytoplankton due to changes in boundary currents and by marine heat waves in Australian coastal waters from IMOS National Reference Stations
- Published
- Accepted
- Subject Areas
- Ecology, Marine Biology, Microbiology, Biological Oceanography
- Keywords
- picophytoplankton, Prochlorococcus, Synechococcus, IMOS National Reference Stations, Marine heat wave, Leeuwin Current, East Australian Current
- Copyright
- © 2018 THOMSON et al.
- Licence
- This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, reproduction and adaptation in any medium and for any purpose provided that it is properly attributed. For attribution, the original author(s), title, publication source (PeerJ Preprints) and either DOI or URL of the article must be cited.
- Cite this article
- 2018. Trends in the abundance of picophytoplankton due to changes in boundary currents and by marine heat waves in Australian coastal waters from IMOS National Reference Stations. PeerJ Preprints 6:e26677v1 https://doi.org/10.7287/peerj.preprints.26677v1
Abstract
The picophytoplankton, Prochlorococcus and Synechococcus, are small photosynthetic cells (< 3µm diameter) important in the world’s tropical oceans. With a large surface area to volume ratio these cells are very responsive to their environment, and their distribution and abundance make them good indicators of variability in our coastal oceans. To understand change in Australian waters, we used flow cytometry to analyse monthly samples of picophytoplankton (2009 – 2017) from 2 Integrated Marine Observing System (IMOS) National Reference Stations (NRS) in southern Australia. We found clear seasonal patterns in abundance from Rottnest Island (Western Australia) and Maria Island (Tasmania) due to seasonality in flows of the Leeuwin and East Australian Currents. However, our data also shows that the abundance of the tropical picophytoplankton in southern Australian waters is increasing due to strengthening boundary currents and more intense eddies on the east coast and through the effects of marine heat waves on the west coast. This is significant as it points to fundamental changes in the size and community composition of phytoplankton at the base of the marine food chain. Our data also highlight how sustained ocean biodiversity observations help us understand our changing oceans.
Author Comment
This is a preprint submission to PeerJ Preprints of an abstract accepted for the World Conference on Marine Biodiversity 2018