The Cold Zone – The Hydrothermal
Vents Overlooked Cousin
Oases of life...
Despite
the first paper based on cold seeps being published a couple of decades ago;
cold seeps are often overlooked and within the high-arctic regions are poorly
explored. Along the coast of Svalbard there
are a collection of cold seeps with many having been previously studied for the
biogeochemical properties. However until this time
no studies have explored the associated benthic community and its relation to the
methane seeps.
The Study Itself
Åström et al., 2016
described the cold seep-associated
communities and habitats located on the shelf of western Svalbard and the western Barents
Sea. Samples took place throughout June and July
2014 and May 2015, quantifying
both the benthic communities and the sedimentary characteristics of 10 stations
across three sites. Benthic fauna was quantified via; total abundance and
biomass. While sediment properties included; Sediment grain size, total organic carbon (TOC), porosity, Density and Sediment Pigment concentrations.
The analysis of the results revealed the large localized
impact that cold seeps have on the abundance and diversity of the benthic
communities. The areas around the seeps are home to high levels of biomass
however lacked diversity. Comprised of only a handful of taxa, the species present
were adapted to the harsh environment often living as part of a symbiotic
relationship, using the reduced chemicals as an energy source.
The studied cold Seeps were overwhelmed by Polycheates with the
most abundant family being the Siboglinids, a tubeworm that thrives in reduced
environments where reduced chemicals are present. Adult Siboglinids lack a
mouth and digestive system and rely on symbiosis with chemoautotroph symbionts
for their energetic requirements. This high abundance of chemosynthetic fauna
indicates that in regions lacking photosynthtically derived organic matter
chemosynthesis is an advantageous life strategy provides the organism a competitive
advantage.
What is the future for cold seeps?
These kinds of studies could provide a basis to help us
explore and understand the delicate balance between biological, hydrographic and
geological characteristics and how they impact benthic communities. The investigation
of how ocean warming could influence these unique environments is an area that
is becoming increasingly relevant and important all the time, yet lacks the
studies to full understand the interaction. However the area is being
progressed by a number of published researchers studying the destabilization of
solid gas hydrates. These solid hydrates require an environment with high
pressure and low temperature to form but due to ocean warming the limited environments
that meet this requirements are diminishing; resulting in increase of methane
emissions from dissociating hydrates. Future studies should focus on
understanding the interactions and adaptations of benthic communities’ as well
as the development of models to hopefully predict how such a large change could
influence the benthic communities.
Citations:
EKL Åström, ML Carroll, WG Ambrose, J Carroll. Arctic cold seeps in marine methane hydrate environments: impacts on shelf macrobenthic community structure offshore Svalbard. Marine Ecology Progress Series, 2016; 552: 1 DOI: 10.3354/meps11773
Extra Reading
Hung, Chia-Wei et al. “Benthic Fluxes of Dissolved Organic Carbon from Gas Hydrate Sediments in the Northern South China Sea.” Scientific Reports 6 (2016): 29597. PMC. Web. 21 Oct. 2016.
Hi Stefan,
ReplyDeleteThanks for your review, this seems like a very interesting are of study. Do you know how stable cold seeps are, compared to hydrothermal vents?
Thanks,
Johanna
Hi Johanna,
DeleteI'm unsure of what you mean by stable, do you mean geologically as in how long they are often active for and if they fluctuate in output or biologically?
Sorry about this,
Stefan
Hi Stefan,
ReplyDeleteSorry for not making it clearer, I meant geologically.
Thanks,
Johanna
Hi there Johanna,
ReplyDeleteSorry about the very slow reply. Your question was very interesting so I did a bit of extra research on it and found some pretty interesting things.
Firstly cold seeps are generally a lot more stable than their hotter cousin the hydrothermal vent as unlike the vents they consist of a fissure and a reservoir of solid methane hydrates within the sediment. This means that the cold seeps cease their activities as soon as the methane in the sediment is exhausted. Studies that have looked at cold seep communities have reported evidence of mussel and clam communities persisting in the same sites for 500-4,000 years.
Although nowhere near as destructive as other underwater geological activities such as volcanoes, there is a chance of a catastrophic event where an entire layer of shallow hydrate could break free of the bottom and greatly affect local communities.
In summary, Cold seeps are active for a far longer stretch of time often lasting thousands of years and are generally less volatile than other underwater geological events.
Thanks, if you have any more questions feel free to ask.
Stefan