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editThe benthic boundary layer (BBL) is the layer of water directly above the sediment at the bottom of a body of water (river, lake, or sea, etc.)[1]. Through specific sedimentation, certain organisms are able to live in this deep layer of water. The BBL is generated by the friction of the water moving over the surface of the substrate, which decrease the water current significantly in this layer[2]. The thickness of this zone is determined by many factors, including the Coriolis force. The benthic organisms and processes in this boundary layer echo the water column above them[2]. The BBL serves as a transitional zone between the water column and the sediment layer by regulating biogeochemical processes and the flux of nutrients and organic materials[2] . This zone also serves as the main layer of resistance for the shift of of mass, heat, and nutrients from the sediment to the water, or vice versa[1]. It is this area of interaction between the two environments that is important in many species' reproductive strategies, particularly larvae dispersal. The benthic boundary layer also contains nutrients that are important for fisheries, wide arrays of microscopic life, varieties of suspended materials, and sharp energy gradients. It is also the sink for many anthropogenic substances released into the environment as the substances commonly sink to the bottom of the water column[2].
Life in the Deep Sea Benthic Boundary Layer
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The BBL represents a few tens of meters of the water column directly above the sea floor and constitutes an important zone of biological activity in the ocean. While the supply of POM, or marine snow, is relatively limited and inhibits species abundance, it sustains a complex yet understudied microbial loop that can maintain both meiofaunal and macrofaunal populations. In the microbial loop, non-moving benthic organism living in the benthic boundary layer supply nutrients to the loop by releasing unused particles for use by microbial communities[2]. Studies have determined that microbial activities were up to a factor of 7.5 higher in the BBL than in adjacent waters[3].
Organisms that live in the benthic boundary layer are known as being benthopelagic[4]. All organisms living predominantly in the benthic boundary layer must acquire their food from falling particles in the water column[2]. Bacterial growth and consumption of falling organic detritus is hindered by the hydrostatic pressure of water and increase in depth[5]. This allows for changeable and consumable matter to reach the ocean flood and be consumed by benthic organsims. The quality and quantity of nutrients reaching the sea floor play a major role in the development of benthic communities[2]. These organisms ultimately play a vital role in the remineralization of matter and aid in breaking down POM that may eventually become permanent sediment.
Presently, it is known that deep-BBL bacterial populations are able to support protozoan bacterivores such as foraminifera and various metazoan zooplankton, which in turn can support larger organisms. Meiofauna and macrofauna found in the deep-BBL include: copepods, annelids, nematodes, bivalves, ostracods, isopods, amphipods, arthropods and gastropods. The current number of species living in the benthic boundary layer is widely unknown. However, it is theorized that up to 10,000,000 species are living in the BBL[6].
Sedimentation in the Benthic Boundary Layer
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The BBL plays a vital role in the cycling of matter and is commonly referred to as the “endpoint” or "sink" for sediment material, which fuels high metabolic rates for microbial populations[4]. The particles from the pelagic ecosystem sink to the BBL where they will be used by organisms[2]. Studies have estimated that particles from the photic zone sink at a rate of approximately 100 meters per day[7]. Up to 10% of sediment from the photic zone is able to sink all the way down to the benthic boundary layer[4]. However, the total amount of mass that falls to the BBL is impacted by total pelagic production and seasonal variability[7]. After passing through the BBL, this degraded material is either returned to the water column or mobilized into the sediment, where it may eventually become immobilized due to currents or sediment force. Re-suspension or upward fluxes of particles can occur due to environmental disturbances such as wind, currents, tide fluctuations, and benthic storms[4]. With growing concern over the ultimate fate of matter in the ocean, knowledge of the complex biological processes in the deep sea BBL (deep-BBL) and how they affect future sedimentation and remineralization rates is valuable to the scientific community.
At sea depths of 1800m or greater, the BBL is noted as having a near homogeneous temperature and salinity with periodic fluxes of detritus or particulate organic matter (POM). POM is strongly linked to seasonal variations in surface productivity and hydrodynamic conditions. The amount of POM that sinks into the water is directly correlated with production in the photic zone of the water column. The homogeneous temperatures and salinity, as well as the lack of current in this layer, are due to the friction between the water and the sediment below it[2]. Excluding hydrothermal vents, much of the deep sea benthos is allochthonous, with the importance of bacteria for substrate conversion being paramount.
Future Directions
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This zone is of interest to biologist, geologists, sedimentologists, oceanographers, physicists, and engineers, as well as many other scientific disciplines. As the effects of anthropogenic activities begin taking an even greater toll on marine processes, long-term studies are essential in determining the health and stability of the deep-BBL[6]. Current climate variation and warming could also play a major role in changes in the the BBL by decimating living species present there and could prompt long-term studies in future scientific communities. Currently, several groups are employing cabled observatories (ALOHA Cabled Observatory, Monterey Accelerated Research System, NEPTUNE, VENUS, and Liquid Jungle Lab (LJL) Panama- PLUTO) to work towards developing these much needed time-series. Cabled underwater networks provide continuous power to cabled instruments to allow for long-term studies[6]. The cables also provide a way for data to be reviewed in real-time from the shore. Time-lapse cameras, sediment traps, bottom-transecting vehicles, baited traps, acoustic arrays, slaved cameras, and autonomous underwater vehicles (AUVs) are also being used to gather more information about the organisms and processes in the benthic boundary layer[6]. Using these research techniques, scientists may begin to find new ways to conserve BBL communities and gather new data about species.
References
edit- ^ a b Svensson, Urban; Rahm, Lars (15 June, 1988). "Modeling the Near-Bottom Region of the Benthic Boundary Layer". Journal of Geophysical Research. 93 (C6): 6909–6915.
{{cite journal}}: Check date values in:|date=(help) - ^ a b c d e f g h i Gili, Josep-Maria; Vendrell-Simón, Begoña; Arntz, Wolf; Sabater, Francesc; Ros, Joandomènec (2020-12-11). "The benthos: the ocean's last boundary?". Scientia Marina. 84 (4): 463–475. doi:10.3989/scimar.05091.24A. ISSN 1886-8134.
- ^ Ritzrau, Will (1996-12-01). "Microbial activity in the benthic boundary layer: Small-scale distribution and its relationship to the hydrodynamic regime". Journal of Sea Research. 36 (3): 171–180. doi:10.1016/S1385-1101(96)90787-X. ISSN 1385-1101.
- ^ a b c d Angel, M. V.; Boxshall, G. A. (1990). "Life in the Benthic Boundary Layer: Connections to the Mid-Water and Sea Floor [and Discussion]". Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences. 331 (1616): 15–28. ISSN 0080-4614.
- ^ de Jesus Mendes, Pedro A.; Maier, Irene; Thomsen, Laurenz (2007-11). "Effect of physical variables on particle critical erosion shear stress: Hydrostatic pressure, slope and changes in water density". Estuarine, Coastal and Shelf Science. 75 (3): 317–326. doi:10.1016/j.ecss.2007.04.035.
{{cite journal}}: Check date values in:|date=(help) - ^ a b c d Sherman, Alana D.; Smith, K.L. (2009-09). "Deep-sea benthic boundary layer communities and food supply: A long-term monitoring strategy". Deep Sea Research Part II: Topical Studies in Oceanography. 56 (19–20): 1754–1762. doi:10.1016/j.dsr2.2009.05.020.
{{cite journal}}: Check date values in:|date=(help) - ^ a b Baldwin, R.J.; Glatts, R.C.; Smtih Jr., K.L. (2 October 1997). "Particulate matter fluxes into the benthic boundary layer at a long time-series station in the abyssal NE Pacific: composition and fluxes". Deep-Sea Research II. 45: 643–665.