February 27, 2017
Measuring the pulse of the ocean
Posted by Lauren Lipuma
This is the latest in a series of dispatches from scientists and education officers aboard the Schmidt Ocean Institute’s R/V Falkor. Read more posts here, and track the Falkor’s progress here.
Act 1: Blowin’ in the wind
At the unholy hour of 0400, I find myself on the aft deck of the world-class research vessel Falkor, bubbling with excitement stemming from a unique combination of four shots of espresso, generally being a morning person, and, most importantly, preparing to test an experimental device that I have put my blood, sweat, and tears into. As I bear-hug my newly collected bucket full of seawater on the rocking transit back to the wet lab, I take a moment to silently congratulate myself on the superb display of stamina and posture; it appears that my sea legs have finally decided to make an appearance. The sun will be coming up soon. It’s a Bob Dylan kind of day. Time to turn up the music and get to work.
Act 2: There ain’t no party like a plankton party
In addition to being an eclectic lab DJ, one of my roles as a scientist aboard this righteously amazing research vessel is to investigate the rates of biological activity among microscopic communities within the ocean. The invitees to this epic microbial festival include bacteria, viruses, zooplankton, larval fish, and phytoplankton (algae). The photosynthetic members of this microscopic plankton community (PHYTO-plankton) are the base of a complex ocean food web, and have a large cascading ecological impact on the abundance and diversity of fisheries that we depend on. In addition, phytoplankton play a significant role in the global cycling of carbon, as well as the production of oxygen we breathe. Just like the plants in your garden, phytoplankton utilize carbon dioxide and micronutrients in the seawater – along with various light harvesting pigments which capture sunlight at different wavelengths – to create new cell bodies.
A byproduct of this magnificent life-giving process of photosynthesis is the production of oxygen, which we measure with great precision as a proxy for the amount of carbon that has been fixed into organic matter. The remaining (non-photosynthetic) members of this microbial party are not particularly polite dinner guests and have a tendency to exploit the kindness of our fearless photosynthetic community by eating the food that the phytoplankton have dutifully prepared, namely themselves (phytoplankton bodies) along with their subsequent secretion of dissolved organic matter (zooplankton are quite the sloppy eaters). We measure this microscopic massacre in the form of oxygen consumption, because, like us, these microbial heterotrophs need oxygen and organic matter that phytoplankton produce in order to live. Collectively, the ocean acts as one breathing organism as this process plays out, silently taking in copious amounts of carbon dioxide from the atmosphere and giving us oxygen that we breathe. This balance (or lack thereof) of carbon/oxygen uptake versus production lends us insight into the overall health or metabolic status of an ecosystem, in a way similar to taking the pulse of your body.
Act 3: Some telescopic insights into microscopic processes
One of the more confounding elements of studying oceanography is dealing with the fact that many measurements only tell us something about one very specific time and place in a very large and dynamic ocean. So, in addition to these experiments, we are monitoring the “color” of the ocean with continuous underway measurements of the reflectance of sunlight from the water. As sunlight hits the ocean, phytoplankton are capturing some of this light for photosynthesis, and they imperceptibly change the color of the water as light scatters back from the sea. Out in this near-barren desert of photosynthetic activity, we use a very precise radiometric measurement of over 100 wavelengths across the ultraviolet/visible spectrum to detect these subtle changes. As a NASA scientist, my other research life consists of using data from ocean-observing satellites that monitor changes in the color of the ocean over the entire globe every day. By understanding more about the link between biological activity that I’m measuring in the lab, the types of phytoplankton in the water, and how this changes the color of the ocean, we can refine how we monitor these processes from space, and thus increase our understanding of carbon cycle dynamics on a global scale. Just to re-iterate, we are literally monitoring the activity of microscopic organisms that are too small to see with the naked eye with a telescope orbiting our planet at over 15,000 mph to study climate scale processes. I think that’s pretty neat.
Act 4: Some microscopic insights into life, the universe, and everything
It’s been a long day, so I am going to wind down, grab my guitar, and serenade the sunset. They say if you sing to plants, they grow better, so there is some scientific merit to this ritual, mind you. Incidentally, our artist-at-sea, Kirsten, has inspired me through one of her onboard art + science seminars to try and take a more careful and purposeful look at the world around me. I will temporarily suspend the thought of Rayleigh scattering and radiative transfer equations as I watch the sun’s rays extend across the horizon. For now, I’ll just listen and observe.
— This post originally appeared on the Schmidt Ocean Institute blog.