Hydrothermal fluids at spreading centers of Mid Oceanic Ridges originate due to circulation of sea water through hot volcanic rocks. Heated rocks and deeper magmas pull in the cold seawater, heat it and then pull out the hydrothermal fluid- the hot water.
The hydrothermal water laden with metals and many other elements returns back into the overlying oceans.
Circulating sea water through porous volcanic rocks not only cools the lithosphere but also contribute to the sea water chemistry, and formation of important mineral deposits of Co, Ni, Lanthanides and PGEs. Continental weathering also contributes to the seawater composition.
The hydrothermal energy and nutrients support complex ecosystems at Mid Oceanic Ridges. Microorganisms in the ecosystem also play important role in the precipitation of minerals.
In the year 2024, India having with two ocean probes, applied to International Sea Bed Authority under the UN Convention on the Law of the Sea (UNCLOS) to explore deep sea around Carlsberg Ridge in the north western limb of the Indian Ocean Ridge system, and Afanasy Nikitin Seamount in the Central Indian basin.
These missions can yield minerals and metals, associated with crusts and nodules, important in clean energy transition and other strategic importance.
Which of the following is mainly contributed to the sea water composition by volcanic activities?