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The Von Damm Hydrothermal Field is a field of
hydrothermal vent A hydrothermal vent is a fissure on the seabed from which geothermally heated water discharges. They are commonly found near volcanically active places, areas where tectonic plates are moving apart at mid-ocean ridges, ocean basins, and hotspot ...
s located just south of
Grand Cayman Grand Cayman is the largest of the three Cayman Islands and the location of the territory's capital, George Town. In relation to the other two Cayman Islands, it is approximately 75 miles (121 km) southwest of Little Cayman and 90 miles ( ...
in the
Caribbean The Caribbean (, ) ( es, El Caribe; french: la Caraïbe; ht, Karayib; nl, De Caraïben) is a region of the Americas that consists of the Caribbean Sea, its islands (some surrounded by the Caribbean Sea and some bordering both the Caribbean Se ...
, on the
Mid-Cayman Rise The Mid-Cayman Rise or Mid-Cayman Spreading Center is a relatively short (110 km long) divergent plate boundary in the middle of the Cayman Trough. It forms part of a dominantly transform boundary that is part of the southern margin to the N ...
in the
Cayman Trough __NOTOC__ The Cayman Trough (also known as the Cayman Trench, Bartlett Deep and Bartlett Trough) is a complex transform fault zone pull-apart basin which contains a small spreading ridge, the Mid-Cayman Rise, on the floor of the western Caribbe ...
. It is approximately south of the Beebe Vent Field. The vent field is named in commemoration of geochemical oceanographer Karen Von Damm, who died in 2008. Von Damm is situated a depth of approximately below sea level, situating it within the
Bathyal zone The bathypelagic zone or bathyal zone (from Greek βαθύς (bathýs), deep) is the part of the open ocean that extends from a depth of below the ocean surface. It lies between the mesopelagic above, and the abyssopelagic below. The bathypelagi ...
with the majority of other hydrothermal vent fields. The hydrothermal plume "Von Damm" was detected in 2010, with the site being visually confirmed later that year. Von Damm is of particular interest due to its location atop an ocean core complex associated with the Mid-Cayman spreading center. This exposes potential ultramafic rocks to seawater, hosting geochemical reactions unique to those of Beebe nearby and potentially similar to those of the Lost City Field. By some, Von Damm is considered a new class of hydrothermal system (deviating from black smoker and alkaline systems) and may be a common occurrence.


Geography

The Von Damm vent field is located centrally on the Mid-Cayman Rise between the Oriente and Swan Island transform faults. The ocean core complex, which the field resides on the eastern side of, is known as Mount Dent and is the most central of the three known on the spreading center. The other two being Mount Emms and Mount Hudson. Mount Dent rises from a depth of approximately to , an elevation change comparable to
Mount McArthur (British Columbia) Mount McArthur is a mountain located in Yoho National Park, British Columbia, Canada. It was named in 1886 by Otto Koltz after James J. McArthur, a land surveyor who mapped the Canadian Rockies for the Canadian Pacific Railway. Climate Based ...
or
Mount Tate , commonly referred to as Tateyama, is a mountain located in the southeastern area of Toyama Prefecture, Japan. It is one of the tallest mountains in the Hida Mountains at . It is one of Japan's along with Mount Fuji and Mount Haku. Tateyama ...
. The field itself is approximately west of the Mid-Cayman spreading center, where the crust is estimated to be 1-2 million years old. The field is composed of two main regions, north and south, on overlapping talc mounds linked by locations of diffuse flow. Talc mounds continue to the southeast, with the largest inactive mound located approximately east of the active vents. Due to the proximity to the Cayman Islands, the Von Damm field falls under British jurisdiction.


Vents

Vents plumes at the Von Damm vent field don't contain significant amounts of metals, so venting fluids lack the colors used to identify vents (black and white smokers). Most venting locations are covered in the shrimp ''Rimicaris hybisae'', however. This makes them easier to identify by looking for dense patches of shrimp and shimmering water.


Northern Summit

Vents at the northern end of the Von Damm Vent Field include the hottest observed in the entire vent field. The ''Spire'' has the hottest temperatures, between and and among the lowest observed pH values at around 5.5 to 6. These are less pronounced at nearby venting locations, such as ''White Castle'', ''Ginger Castle'', ''Arrow Loop'', and ''Hotter than Hole''.


Southern Mounds

Further southeast are vents associated with longer-lived venting and tend to be cooler in temperature. Vent locations such as ''Old Man Tree'', ''Shrimp Hole'', ''X-15'' and ''X18'' are all venting at temperatures below . ''Ravelin'' is perhaps the hottest at this side of the field, venting at up to .


Geochemistry

The Von Damm vent field consists of talc mounds, which have exposed
mafic A mafic mineral or rock is a silicate mineral or igneous rock rich in magnesium and iron. Most mafic minerals are dark in color, and common rock-forming mafic minerals include olivine, pyroxene, amphibole, and biotite. Common mafic rocks include ...
or
ultramafic Ultramafic rocks (also referred to as ultrabasic rocks, although the terms are not wholly equivalent) are igneous and meta-igneous rocks with a very low silica content (less than 45%), generally >18% MgO, high FeO, low potassium, and are composed ...
rocks such as
gabbro Gabbro () is a phaneritic (coarse-grained), mafic intrusive igneous rock formed from the slow cooling of magnesium-rich and iron-rich magma into a holocrystalline mass deep beneath the Earth's surface. Slow-cooling, coarse-grained gabbro is che ...
s or peridotites containing the mineral
olivine The mineral olivine () is a magnesium iron silicate with the chemical formula . It is a type of nesosilicate or orthosilicate. The primary component of the Earth's upper mantle, it is a common mineral in Earth's subsurface, but weathers quickl ...
. Chimney structures at the Von Damm field are of varying shapes and sizes, but tend to also consist of talc precipitates. Upon discovery, this mineralogy was unique to Von Damm, as other vent fields displayed chimneys of calcium carbonate or metal sulfides. Fluid chemistry at Von Damm has elevated concentrations of volatiles such as
hydrogen Hydrogen is the chemical element with the symbol H and atomic number 1. Hydrogen is the lightest element. At standard conditions hydrogen is a gas of diatomic molecules having the formula . It is colorless, odorless, tasteless, non-toxic, an ...
,
methane Methane ( , ) is a chemical compound with the chemical formula (one carbon atom bonded to four hydrogen atoms). It is a group-14 hydride, the simplest alkane, and the main constituent of natural gas. The relative abundance of methane on Eart ...
, and
hydrogen sulfide Hydrogen sulfide is a chemical compound with the formula . It is a colorless chalcogen-hydride gas, and is poisonous, corrosive, and flammable, with trace amounts in ambient atmosphere having a characteristic foul odor of rotten eggs. The unde ...
.
Formate Formate (IUPAC name: methanoate) is the conjugate base of formic acid. Formate is an anion () or its derivatives such as ester of formic acid. The salts and esters are generally colorless.Werner Reutemann and Heinz Kieczka "Formic Acid" in ''Ull ...
has also been detected in high concentrations relative to deep seawater, which may be thermodynamically favored when fluids are mixed with seawater.


Biology

The biology at the Von Damm vent field are similar to those found at the Beebe site to the north, though slightly more diverse. In addition to shrimp, squat lobsters, and anemones, Von Damm features extensive coverage of limpets over rocky faces, eelpout fish at venting areas, and
tube worm A tubeworm is any worm-like sessile invertebrate that anchors its tail to an underwater surface and secretes around its body a mineral tube, into which it can withdraw its entire body. Tubeworms are found among the following taxa: * Annelida, the ...
s similar to those observed in the Pacific. Tube worms have been detected in the vicinity of ''Shrimp Hole'', which exhibits chemical characteristics more aligned to that of a
methane seep A cold seep (sometimes called a cold vent) is an area of the ocean floor where hydrogen sulfide, methane and other hydrocarbon-rich fluid seepage occurs, often in the form of a brine pool. ''Cold'' does not mean that the temperature of the seep ...
. An abundance of mussel shells have been observed at the Von Damm field. As with other vent fields, it is possible for deepwater sharks or roaming fishes such as
grenadiers A grenadier ( , ; derived from the word ''grenade'') was originally a specialist soldier who threw hand grenades in battle. The distinct combat function of the grenadier was established in the mid-17th century, when grenadiers were recruited from ...
to appear around the field.


Microbiology

In fluids sampled at the Von Damm field, ''
Sulfurovum ''Sulfurovum'' is a genus within the ''Campylobacterota Campylobacterota are a phylum of bacteria. All species of this phylum are Gram-negative. The Campylobacterota consist of few known genera, mainly the curved to spirilloid ''Wolinella'' s ...
'' has been identified as a dominant bacteria and '' Methanothermacoccus'' have been identified as an abundant archaea. These organisms have been identified at both the Beebe and Von Damm sites of the Mid-Cayman Rise, though higher concentrations of reduced carbon species at Von Damm may be responsible for higher microbial diversity.


Similarities to other locations

Von Damm is a location which has much in common with other vents situated on ocean core complexes such as the Lost City field at the
Atlantis Massif The Atlantis Massif is a prominent undersea massif in the North Atlantic Ocean. It is a dome-shaped region approximately across and rising about from the sea floor. It is located at approximately 30°8′N latitude 42°8′W longitude; just eas ...
. However, Von Damm exhibits chimneys atop mounds consisting of talc. Geochemically, the field is somewhat of an intermediate between hot basalt and ultramafic systems with a more neutral pH. Tube worms are a staple to many venting fields in the Pacific but are rarely found in the Atlantic, which has sparked interest from biologists regarding potential migrations between oceans for a variety of factors.


Gallery

{{Gallery, mode=packed, height=100 , File:Map0033176781x800x800.jpg, A top-down bathymetry profile over Mount Dent from the 2011 RV Okeanos Explorer cruise. , File:Expl698368708x800x800.jpg, Eelpout, shrimp, and limpets consist of most of the macrobiology at sites of venting fluids , File:Expl693152562x800x800.jpg, A spire, covered in shrimp , File:Expl694913617x800x800.jpg, A close up of ''Rimicaris hybisae'' by a venting orifice , File:Expl691995543x800x800.jpg, A winding tube worm , File:Expl692295543x800x800.jpg, Close up of a tube worm extended for feeding , File:VonDamm Crustaceans.jpg, Squat lobsters and shrimp found at the Von Damm vent field , File:VonDamm Tubeworms.jpg, Tubeworms found at the Von Damm vent field in February 2020 , File:Expl690891507x800x800.jpg, A large venting site dubbed "Hotter Than Hole" , File:Expl275572745x800x800.jpg, ROV ''Little Hercules'' diving at the Von Damm field in 2011 , File:Expl275272745x800x800.jpg, ROV ''Serios'' diving as a part of the two-body system for ''Little Hercules''


References


External links


Von Damm in the Interridge Database


Hydrothermal vents Caribbean Sea