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Transport and breakdown of fecal pellets: Biological and sedimentological consequences 1
Author(s) -
Taghon Gary L.,
Nowell Arthur R. M.,
Jumars Peter A.
Publication year - 1984
Publication title -
limnology and oceanography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.7
H-Index - 197
eISSN - 1939-5590
pISSN - 0024-3590
DOI - 10.4319/lo.1984.29.1.0064
Subject(s) - pellets , benthic zone , settling , pellet , sediment , feces , zoology , environmental science , biology , geology , hydrology (agriculture) , ecology , oceanography , geotechnical engineering , environmental engineering , paleontology
Fecal pellets of benthic animals are important in sediment transport processes, yet few quantitative data are available on their salient physical characteristics. We measured, directly and independently, the densities (specific gravities), sizes, and settling velocities of pellets produced by Amphicteis scaphobranchiata , a deposit‐feeding polychaete worm. Pellet density was measured by an isosmotic density gradient technique. Densities ranged from 1.086 to 1.282 g·cm ‒3 and settling velocities from 3.03 to 5.94 cm·s ‒1 . Pellets transported as bedload for variable distances; the oldest pellets tested (6 h after production) traveled a median distance of 3.1 m, while freshly egested pellets traveled 9.5 m before disintegrating. Worms would reingest disaggregated pellets, but feeding rates correlated positively with pellet age, consistent with previous findings that this species feeds at a faster rate on energetically more profitable sediment. These results suggest substantial interactions among benthic animals, fecal pellets, and sediment transport processes.