We have been working all week around the clock to maximize the few days we have at Lost City. We will start updating the website with more blog posts, photos, and videos in the next several days. Here is a guest post by Cameron Henderson, undergraduate student working in Susan Lang’s lab at the University of South Carolina:
The spectacular underwater world of the ‘Lost City’ hydrothermal field is perched near the summit of a huge underwater mountain called the Atlantis Massif. Geologists were studying the Atlantis Massif long before Lost City was discovered because it is made up of rocks that originated from the Earth’s mantle, which have been carried to the seafloor along major faults and have a distinct chemistry compared to most rocks exposed on the seafloor. Mantle rocks contain large amounts of the mineral olivine (a Mg-Fe silicate), which reacts with seawater and forms hydrous Mg-silicate minerals called serpentine and magnetite, an iron oxide that is highly magnetic. This process – referred to as serpentinization – produces methane, hydrogen and heat, among other things. These rock reactions excite scientists because they represent possible fuels for life in the absence of sunlight, and they could be analogous to conditions early in Earth’s history or found on other planets.
The extreme conditions in the impressive white towers of the Lost City are determined by these chemical reactions occurring in the rocks of the Atlantis Massif. The towers, which can be 60 meters (200 feet) tall, are formed when warm alkaline waters from deep within the Atlantis Massif exit the seafloor and mix with seawater. Unlike almost all other hot springs on the seafloor, the chemistry and circulation of water venting from the Lost City chimneys are not driven by hot lava or by cooling of magma at depth. In other words, the Lost City is not volcanic. Instead, it is a geochemical reactor. The hydrothermal activity is driven by the chemical reactions between seawater and the mantle rocks of the Atlantis Massif, which are cooling down as they are exposed to seawater. These same reactions could be providing fuel and food for microbial life, making them intriguing subjects for studying the origins of life. Our studies of the water venting from the Lost City chimneys could provide clues about how the first biochemical pathways might have emerged from geochemical reactions in seafloor rocks on the ancient Earth.
Now that we are in the open sea, out of sight of land, and beyond range of easy communication with our friends and family, it seems like a good time to discuss why we are out here. Why are we spending a whole month away from our loved ones and normal lives? Why are we spending so much of our time (and public funds) in the middle of the ocean taking samples of the seafloor? My two-year old daughter is going to do a hundred little things for the first time while I’m out here on this ship getting very seasick – why would I do that?
The short answer is the thrill of discovery. This expedition is so exciting to us because of the very good chance that we might be able to see things that nobody in the history of the world has ever seen before. Like what? We don’t know! And that’s the exciting part. The Lost City was discovered in exactly this way: a group of scientists (many of whom are involved in our current expedition) in 2000 were pursuing their scientific interests by exploring the geology of the Atlantis Massif (the underwater mountain on which Lost City is perched) and accidentally discovered this amazing natural wonder that was directly related to those scientific interests and yet completely unexpected.