South Pacific Gyre

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The Southern Pacific Gyre is part of the Earth's system of rotating ocean currents, bounded by the

chemical sludge, and other debris known as the South Pacific garbage patch.[4]

Sediment flux and accumulation

The South Pacific Gyre.

Earth's

biogenic and eolian deposition cause sediments to accumulate on the ocean floor very slowly. In the center of the South Pacific Gyre, the sedimentation rate is 0.1 to 1 m (0.3 to 3.3 ft) per million years. The sediment thickness (from basement basalts to the seafloor) ranges from 1 to 70m, with thinner sediments occurring closer to the center of the Gyre. The low flux of particles to the South Pacific Gyre causes the water there to be the clearest seawater in the world.[2]

Subseafloor biosphere

Beneath the seafloor, the

subseafloor biosphere previously studied.[2]

The South Pacific Gyre subseafloor community is also unusual because it contains oxygen throughout the entire sediment column. In other subseafloor biospheres, microbial respiration will break down organic material and consume all the oxygen near the seafloor leaving the deeper portions of the sediment column anoxic. However, in the South Pacific Gyre the low levels of organic material, the low rates of respiration, and the thin sediments allow the porewater to be oxygenated throughout the entire sediment column.[5] In July 2020, marine biologists reported that aerobic microorganisms (mainly), in "quasi-suspended animation", were found in organically poor sediments, up to 101.5 million years old, 250 feet below the seafloor of the region and could be the longest-living life forms ever found.[6][7]

Radiolytic H2: a benthic energy source

Benthic microbes in organic-poor sediments in oligotrophic oceanic regions, such as the South Pacific Gyre, are hypothesized to metabolize radiolytic hydrogen (H2) as a primary energy source.[8][2][9]

The oceanic regions within the South Pacific Gyre (SPG), and other subtropical gyres, are characterized by low primary productivity in the surface ocean; i.e. they are oligotrophic. The center of the SPG is the furthest oceanic province from a continent and contains the clearest ocean water on Earth[2] with ≥ 0.14 mg chlorophyll per m3.[2] Carbon exported to the underlying deep ocean sediments via the biological pump is limited in the SPG, resulting in sedimentation rates that are orders of magnitude lower than in productive zones, e.g. continental margins.[2]

Typically, deep-ocean benthic microbial life utilizes the organic carbon exported from surface waters. In oligotrophic regions where sediments are poor in organic material, subsurface benthic life exploits other primary energy sources, such as molecular hydrogen (H2).[10][8][2][9]

Radiolysis of interstitial water

Radioactive decay of naturally occurring uranium (238U and 235U), thorium (232Th), and potassium (40K) in seafloor sediments collectively bombard the interstitial water with α, β, and γ radiation. The irradiation ionizes and breaks apart water molecules, eventually yielding H2. The products of this reaction are aqueous electrons (e−aq), hydrogen radicals (H·), protons (H+), and hydroxyl radicals (OH·).[9] The radicals are highly reactive, therefore short-lived, and recombine to produce hydrogen peroxide (H2O2), and molecular hydrogen (H2).[10]

The amount of radiolytic H2 production in seafloor sediments is dependent on the quantities of radioactive isotopes present, sediment porosity, and grain size. These criteria indicate that certain sediment types, such as abyssal clays and siliceous oozes, may have higher radiolytic H2 production relative to other seafloor strata.[9] Also, radiolytic H2 production has been measured in seawater intrusions into subseafloor basement basalts.[10]

Microbial activity

The microbes best suited to utilize radiolytic H2 are the knallgas bacteria,

knallgas reaction:[11]

H2 (aq) + 0.5O2 (aq)  H2O (l)[12]

In the surface layer of sediment cores from oligotrophic regions of the SPG, O2 is the primary electron acceptor used in microbial metabolisms. The O2 concentrations decline slightly in surface sediment (initial few decimeters) and are unchanged to depth. Meanwhile, nitrate concentrations slightly increase downward or remain constant in sediment column at approximately the same concentrations as the deep water above the seafloor. Measured negative fluxes of O2 in the surface layer demonstrate that a relatively low abundance of aerobic microbes that are oxidizing the minimally deposited organic matter from the ocean above. Extremely low cell counts corroborate that microbes exist in small quantities in these surface sediments. In contrast, a sediment cores outside of the SPG show rapid elimination of O2 and nitrate at 1 meter below sea floor (mbsf) and 2.5 mbsf, respectively. This is evidence of much higher microbial activity, both aerobic and anaerobic.[9][2]

The production of radiolytic H2 (electron donor) is stoichiometrically balanced with production of 0.5 O2 (electron acceptor), therefore a measurable flux in O2 is not expected in the substrate if both radiolysis of water and knallgas bacteria co-occur.[9][2] So, despite the known occurrence of radiolytic H2 production, molecular hydrogen is below the detectable limit in the SPG cores, leading to the hypothesis that H2 is the primary energy source in low-organic seafloor sediments below the surface layer.[9][2][8]

Water color

Satellite data images show that some areas in the gyre are greener than the surrounding clear blue water, which is frequently interpreted as areas with higher concentrations of living phytoplankton. However, the assumption that greener ocean water always contains more phytoplankton is not always true. Even though the South Pacific Gyre contains these patches of green water, it has very little organism growth. Instead, some studies hypothesize that these green patches are a result of the accumulated waste of marine life. The optical properties of the South Pacific Gyre remain largely unexplored.[13]

Garbage patch

This section is an excerpt from South Pacific garbage patch.[edit]
The South Pacific Gyre can be seen in the lack of oceanic currents off the west coast of South America. Map of ocean currents circa 1943
This photo demonstrates the dispersal of plastic fragments of various sizes
Visualization of the flow pattern of ocean pollutants
The South Pacific garbage patch is an area of ocean with increased levels of marine debris and plastic particle pollution, within the ocean's pelagic zone. This area is in the South Pacific Gyre, which itself spans from waters east of Australia to the South American continent, as far north as the Equator, and south until reaching the Antarctic Circumpolar Current.[14] The degradation of plastics in the ocean also leads to a rise in the level of toxics in the area.[15] The garbage patch was confirmed in mid-2017, and has been compared to the Great Pacific garbage patch's state in 2007, making the former ten years younger. The South Pacific garbage patch is not visible on satellites, and is not a landmass. Most particles are smaller than a grain of rice.[16] A researcher said: "This cloud of microplastics extends both vertically and horizontally. It's more like smog than a patch".[16]

References

  1. ^ "Anybody home? Little response in Pacific gyre". NBC News. Associated Press. 22 June 2009. Retrieved 3 January 2021.
  2. ^
    PMID 19561304
    .
  3. ^ Inc, Pelmorex Weather Networks (27 July 2020). "What lives in the Pacific's 'ocean desert'". The Weather Network. Retrieved 31 December 2022. {{cite web}}: |last= has generic name (help)
  4. ^ Montgomery, Hailey (28 July 2017). "South Pacific Ocean Gyre Holds Massive Garbage Patch". Pelmorex Weather Networks. The Weather Network. Archived from the original on 28 November 2020. Retrieved 14 August 2017.
  5. ^ Fischer, J.P., et al. "Oxygen Penetration deep into the sediment of the South Pacific Gyre" Biogeoscience (Aug. 2009): 1467(6).
  6. ^ Wu, Katherine J. (28 July 2020). "These Microbes May Have Survived 100 Million Years Beneath the Seafloor – Rescued from their cold, cramped and nutrient-poor homes, the bacteria awoke in the lab and grew". The New York Times. Retrieved 31 July 2020.
  7. PMID 32724059
    .
  8. ^ a b c Sauvage, J; et al. (2013). "Radiolysis and life in deep subseafloor sediment of the South Pacific Gyre". Goldschmidt 2013 Conference Abstracts: 2140.
  9. ^
    PMID 18163872
    .
  10. ^
    PMID 26870029
    .
  11. ^ Singleton P, Sainsbury D (2001). "Hydrogen-oxidizing bacteria (the 'hydrogen bacteria'; knallgas bacteria)". Dictionary of Microbiology and Molecular Biology. 3rd ed.
  12. PMID 11250035
    .
  13. S2CID 128518190
    .
  14. ^ "South Pacific Gyre – Correntes Oceânicas" – via Google Sites.
  15. ^ Barry, Carolyn (20 August 2009). "Plastic Breaks Down in Ocean, After All And Fast". National Geographic Society. Archived from the original on August 26, 2009.
  16. ^ a b Nield, David (25 July 2017). "There's Another Huge Plastic Garbage Patch in The Pacific Ocean". Sciencealert.com. ScienceAlert.

Further reading

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