Transparent exopolymer particles (TEPs: Polysaccharides
enriched in deoxy sugars and galactose) form an important constituent of particulate
organic carbon (POC) in the ocean. Phytoplankton (predominantly diatoms) are thought
to be a major source of TEPs, as well as some benthic organisms (Heinonen et
al., 2007) and macroalgae detritus (Thornton, 2004). TEPs are thought to be
phytoplankton orientated, although in the Mediterranean littoral zone TEP
concentrations remain relatively high despite the low levels of planktonic primary
production, this suggests a non-planktonic source. Seagrass beds are important
sources of DOC in marine systems and therefore could provide the precursors
needed for TEP formation. The authors of this study investigate the role of
seagrass in TEP production by comparing two sites in the oligotrophic NW Mediterranean
Sea; one characterised by high levels of seagrass (Posidonia oceanica) leaf litter retention and the other site
rapidly flushed by open-sea water.
Sea surface water samples were collected fortnightly from
both sites. A total of 76 samples were taken from the open-water site (Faro Cap
Ses Salines) between January 2012 and March 2015, while 45 samples were taken
from the accumulation site (Es Caragol beach) from the August 2012 to September
2014. TEP concentrations were determined following the colorimetric method (of
Passow and Alldredge, 1995b) where by TEP is stained with alcian blue and
counted.
TEP concentrations ranged
from 4.6 to 90.6 μg XG Eq L−1 in Faro
Cap Ses Salines and from 26.8 to 1878.4 μg XG Eq L−1 in Es Caragol, with significantly
higher mean TEP concentrations recorded at Es Caragol. Seasonal fluctuations
were observed; at Faro Cap Ses Salines the highest concentrations of TEP were
recorded in February, June and July which likely coincides with the
phytoplankton bloom at that time. In Es Caragol fluctuations of TEP were erratic
with no clear seasonal patterns and remained consistently higher than the other
site. In the lab, the relationship between leaf-litter and TEP was quantified
and used to support the correlation between leaf litter and TEP shown by field results e.g. water in the presence of leaf litter (in the
lab) yielded TEP concentrations of 1551 μg XG Eq L−1 after 264h, which is similar to the maximum concentrations
recorded in nature at the accumulation site (Es Caragol).
By showing a >10-fold difference
in TEP concentrations between the two sites, this study provides the first
evidence that seagrass leaf litter is a source of TEP. These findings have
bio-geochemical implications and provide a new pathway to be considered with
regard to fluxes of DOM and POM in the marine environment. The Authors estimate that P. oceanica releases 76 Gg C as TEPs
annually to the Mediterranean Sea, however this is based on values from one meadow
in autumn and highlights the need for further study if an accurate value for
seagrass contribution is to be described. Using lab data to support field
recordings strengthened this study and I feel this method could be replicated in
temperate waters to aid in better understanding of the local and relative
importance of seagrass TEP production.
Reference
of this study:
Iuculano, F., Duarte, C.M., Marbà, N. and Agustí, S., 2017. Seagrass as
major source of transparent exopolymer particles in the oligotrophic
Mediterranean coast. Biogeosciences, 14(22), p.5069.
Additional references:
Heinonen, K.B., Ward, J.E. and Holohan, B.A., 2007. Production of
transparent exopolymer particles (TEP) by benthic suspension feeders in coastal
systems. Journal of
Experimental Marine Biology and Ecology, 341(2), pp.184-195.
Passow, U. and Alldredge, A.L., 1995. A dye‐binding assay for the spectrophotometric
measurement of transparent exopolymer particles (TEP). Limnology and Oceanography, 40(7), pp.1326-1335.
Hi Ellen,
ReplyDeleteVery interesting paper! I would have never thought of seagrass being a source of TEP!
What are your thoughts on increasing temperatures and other changing environmental factors? Does seagrass have tolerances to factors such as high UV? And if so do you think its sufficient?
Just curious.
Thanks,
Ankitha
Hi Ankitha,
DeleteUnfortunately and rather shockingly, it is predicted that under a low emissions scenario, seagrass meows of Posidonia oceanica will become regionally extinct in the western Mediterranean Sea by 2049 (+-10yrs). This is primarily due to seagrasses low tolerance to increasing regional temperatures (This species responds to 3◦ C warming with a 3 fold increase in mortality rate). To give some perspective on Mediterranean warming, between 2002-2010 the western Mediterranean increased by 1.05 ± 0.37 ◦ C (Jordà et al., 2012). The consequences of this on TEP production obviously remain to be seen, but in response to your question on seagrass tolerance alone, things do not look promising for the future of seagrass in the Mediterranean Sea. It could therefore be speculated that we will observe in a decrease in TEP production in the Mediterranean Sea, however nature often has ways of surprising us.
I hope this helped,
Ellen
For more information on Seagrass (Posidonia oceanica) the Mediterranean, I recommend this publication in nature:
Jordà, G., Marbà, N. and Duarte, C.M., 2012. Mediterranean seagrass vulnerable to regional climate warming. Nature Climate Change, 2(11), pp.821-824.
Hi Ellen,
ReplyDeleteI’ve had a read of this paper, after your recommendation, and think that it is a very interesting study!
It seems slightly strange to me that the authors chose two sites which both had seagrass present. It could have been interesting to see the difference in TEP levels between a site with rapidly flushed open-sea water, a site with an accumulation of leaf litter and finally a site with no seagrass presence. This would then allow a comparison between the seagrass production of TEP and the ‘background’ levels of TEP.
Another interesting point that the authors made was that both P. oceanica and phytoplankton are nutrient limited in the Mediterranean Sea – which enhances the release of TEP precursors. They don’t fully explain why this happens (apart from being due to Carbon over-flow during these conditions), so I would be really interested in hearing your thoughts on this!
Thanks,
Megan.
Hi Megan,
DeleteI must admit, I had similar thoughts as they appear to almost contradict them selves in saying that the open water site is still in close proximity to the meadows and further study without seagrass would be interesting.
With regards to the TEP increase due to "carbon over flow" what I understood was as follows:
"Carbon overflow" occurs when the organism continues to photosynthesis in a nutrient limiting environment. This is because the organic carbon (OC) produced from photosynthesis cannot be used by the organism for growth (due to limited nutrient uptake) so the surplus of OC molecules persist in the environment and increase the pool of precursor materials for TEP formation.
Hope this helps, thanks for the comment,
Ellen