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Objective Background | Materials | Procedure | Discussion Background Couldn’t quite read that? Well, the point is that many things are too small for us to see, including much of the life and matter on this planet. We tend to be more familiar and comfortable with things when they are on a scale large enough that we can see them. As a result, most of us don’t usually think of how things happen on very small scales – but it’s important that we do because all living things are not only composed of molecules, they also rely on molecules for their energy to live (including us!). Let’s take an example of a person eating an apple. How does the energy from the apple actually get into their body and become energy they can use? You can watch them take bites, and know that they chew and swallow the pieces, and that those pieces provide them with energy. End of story, right? … not quite. Those bites of apple make their way to the stomach where digestive enzymes break down the pieces into smaller and smaller pieces, and eventually into molecules, that are absorbed into cells in our stomach and intestines and carried by our bloodstream. Ultimately, energy in living organisms is used or created at the molecular level. Organisms break down their food into molecules, and then use those molecules to create energy for respiration (the basic functions that keep us alive) or store it to build other molecules for growth. So, you can see (well, actually you can’t) that energy and matter are truly transferred at the molecular level for living things. What about the flow of energy and matter between organisms in the marine environment? We’re able to see large organisms feed and grow in the ocean, but are things that happen at the molecular level important in the ocean as well? Click on the link below to find out … It was only 30 years ago that scientists first began to understand that bacteria and other microbes play a big role in the cycling of matter and energy in the ocean. Without the microbial loop, a large portion of organic carbon on the planet would remain dissolved for thousands or millions of years before returning to the food web. Bacteria are a critical link not only for recycling dissolved organic matter, but also for converting organic carbon to inorganic carbon through metabolic processes such as respiration. In fact, most heterotrophs (organisms that consume other organisms for energy) create inorganic carbon in the form of CO2 through respiration, including humans. This CO2 can then be used by many autotrophs (organisms that convert inorganic molecules into energy) such as plants, algae and cyanobacteria to create energy that helps fuel life for much of the rest of the planet. For example, CO2 created by bacteria as they “feed” on DOM and respire can be used by phytoplankton to perform photosynthesis and create their own energy. All organisms rely on carbon-based molecules for at least part of their survival, growth and reproduction. In the next activity you’ll be asked to consider how matter and energy move through a marine food web by tracing the multiple pathways that can be taken by carbon as it transforms into different molecules. Good luck! Materials
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