Terminology Note:
Different people use terms related to different kinds of hydrothermal vents at the bottom of the ocean.
There are at least two classes of these vents, driven by different energy sources with outflows with different chemical properties.
These different sites have different credibilities as possible sources of living system origins (
locations where origin of life seems feasible).
Vents with flows driven by contact of sea water with very hot rock or magma. I have seen these called
geothermal vents (geological heat source) or
hydrothermal vents.
These have:
- high temperature outflows
- usually high velocity flows
- high levels of dissolved metals (resulting in "black smokers" when the precipitate).
Possible problems for origin of life events:
- The high temperatures are considered by some to make organic chemical significantly less stable (break down rapidly).
- The high flow rates would be more likely to blow organics materials away, reducing their concentration which makes possible biochemical interactions much less likely. These would be needed to build up the biochemical complexity for life processes.
Vents driven by
serpentinization of seawater reactions with the kind of rock (mafic or ultramafic) created at the seafloor, where the spreading occurs. These vents were first predicted by Michael Russell in 1993, and first found in 2000. (He also hypothesized them as a potential origin of life site.) The rock recently brought into contact with the ocean, gets oxidized and hydrated, by reacting with seawater, to form serpentinite or related kinds of rocks.
I have seen these called
hydrothermal vents and
alkaline hydrothermal vents (which is longer but clearly distinct from the other group).
Going forward, I will try to use "alkaline hydrothermal vent" due to clarity, but not what I've done before.
The outflow from these vents is different chemically:
- less hot, high pH (alkaline)
- dissolved CO2 (could be used to make organic molecules) and H2
- lesser amounts of dissolved metals (Fe, Ni, ...)
- Contact of the vent water with seawater creates "white smokers" due to carbonate precipitation, but can be greyish depending on metal content.
The slow flows that get divided up into smaller and smaller passages, allow many small outflow passages with gradual mixing of vent and sea water. Ultimately it can become a very slow flow through a lot of small passages (somewhat like a sponge filter if you know aquarium technology).
Potentially many different little crevices making many little opportunistic laboratories for different combinations of undirected organic syntheses.
Differences between seawater and the ocean have a difference in proton concentration (H
+ or pH) are what the some consider to be the driving force for chemistry at the origin of life. A proton gradient parallels the cell's use of a proton gradient across a membrane by its energy generation mechanisms. By this, I mean all eukaryotic, bacterial and archeal cells.
This is a feature conserved in all life. Viruses are not cells, don't make their own energy, and don't have these features. However, they require cells that do, in order to reproduce.
The hot water vents are usually located where ocean spreading is occurring and the hottest rock/lava material is exposed. They dissolve minerals in the hot water, which when it contacts the cooler ocean water will start to precipitate, creating the outflow towers. As the ocean floor spreads and local areas move away from the heat source, old vents will stop and new ones will form where the sea floor is now opening up.
The alkaline hydrothermal vents are located further from the actual site of ocean floor spreading.
They are found in older rocks that are not so hot, but have had time to react with the seawater. The reaction releases some heat but they don't get nearly as hot as the geothermal vents. Perhaps because of this they have (generally) slower outflow speeds.
Alkaline hydrothermal vents can be very large and last for thousands of years, providing the opportunity for many different random experiments in biochemistry.
In both cases (vent types), the dissolved metals can precipitate out, in small crystals that are related to enzymatic reaction centers in biological enzymes today. The reaction promoting properties of these kinds of Fe/Ni containing molecules are important components of many different origin of life scenarios. Scenarios that have been proposed to have occurred at several different sites.