The Plymouth Student Scientist
Document Type
Literature Review
Abstract
Phytoplankton is the main driver of ocean net primary production (Falkowski et al., 1998) and a dominant force behind biogeochemical cycling in the ocean. It is a component of one of the oldest and best described virus-host relationships (e.g. Suttle et al., 1990). Viruses have typically been viewed as pathogens of marine organisms but it has become clear that they also play a critical role in biogeochemical processes in marine systems, themselves falling into the category of dissolved organic matter (DOM) (Wilhelm & Suttle, 1999). Viruses play a large part in carbon (Middelboe & Lyck, 2002), sulphur (Hill et al., 1998) and iron cycling (Poorvin et al., 2004) in the world‟s oceans. Earth‟s climate has warmed by approximately 0.6°C during the last 100 years. The rate of warming has doubled in the second half of the century (Houghton, 2001). This rapid change has been attributed to the impact of anthropogenic activities on the atmosphere. Climate change is already affecting marine ecosystems and more extreme changes are predicted for the future (Walther et al., 2002). Whilst a number of studies have examined the effects of climate variables on phytoplankton, it is unclear how marine viruses are affected by these changes. This is important because of the close relationship between viruses and their phytoplankton host. This review will outline the nature of phytoplankton and marine viruses, with a virocentric bias. Relevant biogeochemical cycles and the impact of climate change are described and the possible effects of the altered environment on the phytoplankton-virus system are considered.
Publication Date
2009-12-01
Publication Title
The Plymouth Student Scientist
Volume
2
Issue
2
First Page
289
Last Page
302
ISSN
1754-2383
Deposit Date
May 2019
Creative Commons License
This work is licensed under a Creative Commons Attribution 4.0 International License.
Recommended Citation
Sorensen, George
(2009)
"The role of the virus-phytoplankton system in marine biogeochemical cycling: possible impacts of climate change,"
The Plymouth Student Scientist: Vol. 2:
Iss.
2, Article 7.
DOI: https://doi.org/10.24382/ehsh-p434
Available at:
https://pearl.plymouth.ac.uk/tpss/vol2/iss2/7