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The researchers published their work July 18 in Proceedings of the National Academy of Sciences. 'I hope our study will motivate future research efforts to target mapping off-axis areas along the global mid-ocean ridge crest to better quantify the extent of off-axis versus on-axis hydrothermal venting.' 'There is much still left to be discovered about deep-sea vents along the global mid-ocean ridge, both in terms of where they are located as well as their geological, geochemical and biological characteristics,' adds McDermott. 'The new vent field may seed recovering hydrothermal ecosystems after volcanic eruptions,' explains Santiago Herrera, a co-author who is a biological oceanographer and faculty member in Lehigh UniversityвЂ™s Department of Biological Sciences. The seawater in hydrothermal vents may reach temperatures of over 700 degrees Fahrenheit. Researchers have nine vents instrumented in the entire study area. 'The mapping work provides a detailed picture of the seafloor so that we can monitor and quantify changes that occur when the next volcanic eruption happens along this portion of the East Pacific Rise ridge axis,' says Jill McDermott, chemical oceanographer and faculty member in Lehigh University's Department of Earth and Environmental Sciences, in a statement. Those measurements are a way to track changes that the vents experience.

'I hope our study will motivate future research efforts to target mapping off-axis areas along the global mid-ocean ridge crest to better quantify the extent of off-axis versus on-axis hydrothermal venting.' Pictured:В The remotely operated vehicle (ROV) Jason samples 368вЊ black smoker fluids using titanium syringe-style samplers for analysis

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