Seasonal changes in the chemical and physical characteristics of Calanus finmarchicus and Oikopleura vanhoeffeni fecal pellets

Fecal pellets from Oikopleura vanhoeffeni and Calanus finmarchicus were analyzed in the spring, summer, fall and winter to determine if there were changes in their physical (size, phytoplankton content & density) or chemical (particulate organic carbon & particulate silicate) characteristics...

Full description

Bibliographic Details
Main Author: Urban, Juanita
Format: Thesis
Language:English
Published: Memorial University of Newfoundland 1992
Subjects:
Online Access:https://research.library.mun.ca/4187/
https://research.library.mun.ca/4187/1/Urban_Juanita.pdf
https://research.library.mun.ca/4187/3/Urban_Juanita.pdf
Description
Summary:Fecal pellets from Oikopleura vanhoeffeni and Calanus finmarchicus were analyzed in the spring, summer, fall and winter to determine if there were changes in their physical (size, phytoplankton content & density) or chemical (particulate organic carbon & particulate silicate) characteristics. Changes in phytoplankton content due to seasonal succession were observed in both feces types which resulted from a change from a diatom based food chain in the spring to one based on the microbial loop in the fall. Changing phytoplankton content also resulted in seasonal changes in the dynamic density of the fecal pellets, due to the differential compactness of the component particles. Changes in the dynamic density resulted in changes in the potential of both fecal pellet types to exit the upper mixed layer and contribute to vertical nutrient and particle flux. -- Current literature equations used for predicting the settling velocity of fecal pellets gave correct trends for my data but overestimated the actual rates by 2-100 times. Empirical settling velocity equations were developed for the two fecal types based on their physical characteristics. The resulting equations for both C. finmarchicus and 0. vanhoeffeni were modified Stokes equations. For O. vanhoeffeni, the settling velocity (Ws) can be expressed as: -- [special characters omitted] -- and for C. finmarchicus as: -- [special characters omitted] -- where μ is the viscosity of the water, ps is the density of the fecal pellet, p is the density of the water, g is gravity (981 cm s⁻¹, Dn is the diameter of an equivalent sphere, and L and D are the length and diameter of the fecal pellet. Using these equations, seasonal settling velocities were calculated for the copepod fecal pellets. Fall C. finmarchicus fecal pellets had the fastest settling velocities (25-95 m day⁻¹), indicating that these feces have a greater potential in contributing to the nutrient flux than do spring feces (7-35 m day⁻¹). The higher measured sinking velocities for 0. vanhoeffeni fecal ...