benthic boundary layer

The benthic boundary layer (BBL) represents a few tens of meters of the water column directly above the sea floor{{cite journal |first=Joan E. |last=Cartes |year=1998 |url=http://decapoda.nhm.org/pdfs/29449/29449.pdf |title=Dynamics of the bathyal Benthic Boundary Layer in the northwestern Mediterranean: depth and temporal variations in macrofaunal–megafaunal communities and their possible connections within deep-sea trophic webs |journal=Progress in Oceanography |volume=41 | issue=1 |pages=111–139| doi=10.1016/S0079-6611(98)00018-4 | bibcode=1998PrOce..41..111C }} and constitutes an important zone of biological activity in the ocean.{{Cite book|doi=10.1007/978-94-011-2452-2_1|chapter=Bacterial Standing Stock and Consumption of Organic Carbon in the Benthic Boundary Layer of the Abyssal North Atlantic|title=Deep-Sea Food Chains and the Global Carbon Cycle|pages=1–10|year=1992|last1=Lochte|first1=K.|isbn=978-94-010-5082-1}} It plays a vital role in the cycling of matter, and has been called the “endpoint” for sedimenting material, which fuels high metabolic rates for microbial populations.{{Cite journal|doi=10.1016/S0079-6611(03)00034-X|title=Microbial activities at the benthic boundary layer in the Aegean Sea|journal=Progress in Oceanography|volume=57|issue=2|pages=219|year=2003|last1=Bianchi|first1=A|last2=Tholosan|first2=O|last3=Garcin|first3=J|last4=Polychronaki|first4=T|last5=Tselepides|first5=A|last6=Buscail|first6=R|last7=Duineveld|first7=G|bibcode=2003PrOce..57..219B}}

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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. While the supply of POM (particulate organic matter), 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. In a study by Will Ritzrau (1996), it was determined that microbial activities were up to a factor of 7.5 higher in the BBL than in adjacent waters.{{Cite journal |last1=Ritzrau |first1=Will |year=1996 |title=Microbial activity in the benthic boundary layer: Small-scale distribution and its relationship to the hydrodynamic regime |journal=Journal of Sea Research |volume=36 |issue=3–4 |pages=171–180 |bibcode=1996JSR....36..171R |doi=10.1016/S1385-1101(96)90787-X}} While this study was completed between 100-400m depth, it could have implications for the deep-BBL.

Organisms that live in the benthic boundary layer are known as being benthopelagic.{{Cite journal |last1=Angel |first1=M. V. |last2=Boxshall |first2=G. A. |date=1990 |title=Life in the Benthic Boundary Layer: Connections to the Mid-Water and Sea Floor [and Discussion] |url=https://www.jstor.org/stable/53650 |journal=Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences |volume=331 |issue=1616 |pages=15–28 |doi=10.1098/rsta.1990.0053 |jstor=53650 |s2cid=123179301 |issn=0080-4614|url-access=subscription }} All organisms living predominantly in the benthic boundary layer must acquire their food from falling particles in the water column. Bacterial growth and consumption of falling organic detritus is hindered by the hydrostatic pressure of water and increase in depth.{{Cite journal |last1=de Jesus Mendes |first1=Pedro A. |last2=Maier |first2=Irene |last3=Thomsen |first3=Laurenz |date=November 2007 |title=Effect of physical variables on particle critical erosion shear stress: Hydrostatic pressure, slope and changes in water density |url=https://linkinghub.elsevier.com/retrieve/pii/S0272771407001989 |journal=Estuarine, Coastal and Shelf Science |language=en |volume=75 |issue=3 |pages=317–326 |doi=10.1016/j.ecss.2007.04.035|bibcode=2007ECSS...75..317D |url-access=subscription }} This allows for changeable and consumable matter to reach the ocean flood and be consumed by benthic organisms. The quality and quantity of nutrients reaching the sea floor play a major role in the development of benthic communities. These organisms ultimately play a vital role in the remineralization of matter and aid in breaking down POM that may eventually become permanent sediment. Excluding hydrothermal vents, much of the deep sea benthos is allochthonous,{{Cite journal|doi=10.1016/S0967-0645(99)00064-8|title=Deep-sea macrofaunal assemblages within the Benthic Boundary Layer of the Cap-Ferret Canyon (Bay of Biscay, NE Atlantic)|journal=Deep Sea Research Part II: Topical Studies in Oceanography|volume=46|issue=10|pages=2309–2329|year=1999|last1=Sorbe|first1=Jean Claude|bibcode=1999DSRII..46.2309S}} and the importance of bacteria for substrate conversion is paramount.

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{{cite journal |last1=Poremba |first1=K. |last2=Hoppe |first2=H.-G. |year=1995 |url=https://www.int-res.com/articles/meps/118/m118p237.pdf |title=Partial variation of benthic microbial production and hydrolytic enzymatic activity down the continental slope of the Celtic Sea |journal=Marine Ecology Progress Series |volume=118 |pages=237–245|doi=10.3354/meps118237 |bibcode=1995MEPS..118..237P }}{{cite journal|doi=10.1111/j.1574-6941.2000.tb00731.x|pmid=10967208|title=Bacteria in the cold deep-sea benthic boundary layer and sedimentâwater interface of the NE Atlantic|journal=FEMS Microbiology Ecology|volume=33|issue=2|pages=89–99|year=2000|last1=Turley|first1=Carol|doi-access=free}}

Presently, it is known that deep-BBL bacterial populations are able to support protozoan bacterivores like foraminifera and some metazoan zooplankton,{{cite book|url=https://books.google.com/books?id=sdkVngEACAAJ|page=161|title=Marine Microbiology|isbn=978-1-85996-288-6|last1=Munn|first1=Colin B|year=2004}} which in turn can support larger organisms.{{cite journal |last1=Guidi-Guilvard |first1=L. D. |last2=Thistle |first2=D. |last3=Khripounoff |first3=A. |last4=Gasparini |first4=S. |year=2009 |url=http://archimer.ifremer.fr/doc/2009/publication-7416.pdf |title=Dynamics of benthic copepods and other meiofauna in the benthic boundary layer of the deep NW Mediterranean Sea |journal=Marine Ecology Progress Series |volume=396 |pages=181–195|doi=10.3354/meps08408 |bibcode=2009MEPS..396..181G }} Meiofauna and macrofauna found in the deep-BBL include: copepods, annelids, nematodes, bivalves, ostracods, isopods, amphipods, arthropods and gastropods, to name a few.{{cite journal|doi=10.1016/S0967-0645(99)00064-8|title=Deep-sea macrofaunal assemblages within the Benthic Boundary Layer of the Cap-Ferret Canyon (Bay of Biscay, NE Atlantic)|journal=Deep Sea Research Part II: Topical Studies in Oceanography|volume=46|issue=10|pages=2309–2329|year=1999|last1=Sorbe|first1=Jean Claude|bibcode=1999DSRII..46.2309S}}{{Cite journal |last1=Sherman |first1=Alana D. |last2=Smith |first2=K.L. |year=2009 |title=Deep-sea benthic boundary layer communities and food supply: A long-term monitoring strategy |journal=Deep Sea Research Part II: Topical Studies in Oceanography |volume=56 |issue=19–20 |pages=1754 |bibcode=2009DSRII..56.1754S |doi=10.1016/j.dsr2.2009.05.020}} 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.{{Cite journal |last1=Sherman |first1=Alana D. |last2=Smith |first2=K.L. |date=September 2009 |title=Deep-sea benthic boundary layer communities and food supply: A long-term monitoring strategy |url=https://linkinghub.elsevier.com/retrieve/pii/S0967064509001854 |journal=Deep Sea Research Part II: Topical Studies in Oceanography |language=en |volume=56 |issue=19–20 |pages=1754–1762 |doi=10.1016/j.dsr2.2009.05.020|bibcode=2009DSRII..56.1754S |url-access=subscription }} These organisms ultimately play a vital role in the remineralization of matter and aid in breaking down POM that may eventually become permanent sediment.

The benthic boundary layer (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. The particles from the pelagic ecosystem sink to the BBL where they will be used by organisms. Studies have estimated that particles from the photic zone sink at a rate of approximately 100 meters per day.{{Cite journal |last1=Baldwin |first1=R.J. |last2=Glatts |first2=R.C. |last3=Smtih Jr. |first3=K.L. |date=2 October 1997 |title=Particulate matter fluxes into the benthic boundary layer at a long time-series station in the abyssal NE Pacific: composition and fluxes |url=https://www.sciencedirect.com/science/article/pii/S0967064597000970 |journal=Deep Sea Research Part II: Topical Studies in Oceanography |volume=45 |pages=643–665|doi=10.1016/S0967-0645(97)00097-0 |url-access=subscription }} Up to 10% of sediment from the photic zone is able to sink all the way down to the benthic boundary layer. However, the total amount of mass that falls to the BBL is impacted by total pelagic production and seasonal variability. 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. 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.

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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.

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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. Current climate variation and warming could also play a major role in changes in 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. 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. Using these research techniques, scientists may begin to find new ways to conserve BBL communities and gather new data about species.

{{Reflist}}

• The Benthic Boundary Layer, Transport Processes and Biogeochemistry. Edited by Bernard P. Boudreau and Bo Barker Jørgensen . February 2001, Oxford University Press.

Category:Oceanography

Category:Limnology