Friday, 21 October 2016

The Cold Zone – The Hydrothermal Vents Overlooked Cousin.

The Cold Zone – The Hydrothermal Vents Overlooked Cousin

Oases of life...


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.

4 comments:

  1. Hi Stefan,

    Thanks 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

    ReplyDelete
    Replies
    1. Hi Johanna,

      I'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

      Delete
  2. Hi Stefan,

    Sorry for not making it clearer, I meant geologically.

    Thanks,
    Johanna

    ReplyDelete
  3. Hi there Johanna,

    Sorry 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

    ReplyDelete

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