For Scientists

Pyrosomes

 

Pyrosomes are a colonial form of pelagic tunicate.  This means that (like salps, doliolids, and appendicularians) they are chordates but not vertebrates.  Pyrosomes are composed of individual zooids.  Each zooid is a gelatinous organism that pushes water through itself and catches prey on an internal filter.  However, in pyrosomes, the zooids are arranged together into a bag-like structure, with each zooid pumping water from the outside of the bag to the inside as they catch their prey.  Pyrosomes vary widely in size.  Although the individiual zooids are typically millimeter-sized, the colonial organism can range in size from a few inches to several meters in length.  The ecological role of pyrosomes is poorly understood for a couple of reasons.  First, they are quite patchy in the ocean, so they can be difficult for scientists to find when they intend to study them.  Second, they are fragile organisms and the large ones specifically are very difficult to capture without harming them.  By comparison with their better studied relatives (salps and doliolids), we believe that pyrosomes are efficient filter feeders on relatively small protists, and possibly even bacteria.  However, very few species of pyrosomes have been studied and we know little about their feeding selectivity.  Understanding these creatures is important, however, because anecdotal evidence suggests that they may be increasing in abundance in the world ocean.

In a study led by our colleague Dr. Moira Decima, we quantified the abundances of a species of large pyrosome (Pyrostremma spinosum) during a cruise in the Costa Rica Dome.  Although P. spinosum was only captured in a fraction of our net tows, it dominated the total biovolume of the zooplankton community, because each colony was massive, often containing thousands of zooids.  We measured colony volumes of up to 5.5 liters, although the actual colonies may have been substantially larger because we cannot rule out the possibility that these fragile organisms were broken apart by our nets.  For comparison, the entire rest of the plankton community captured in one of our net tows was typically less than 0.1 liters.  To investigate their ecological and biogeochemical impact, we used stable isotope analyses (carbon and nitrogen, below) and gut pigment analyses of the chlorophyll (indicative of feeding on algae) and phycoerythrin (indicative of feeding on the cyanobacterium Synechococcus) inside the zooids.  We found that P. spinosum had a substantial impact on the total phytoplankton community, but that it was likely not feeding efficiently on cyanobacteria.  We also discovered that (unlike the rest of the zooplankton community) it was primarily feeding beneath the mixed layer, where it may play an important role in consuming slowly-sinking particles and had similar isotopic composition as sinking particles collected using sediment traps.  To see the manuscript based on our study, click here.

 

 

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