Record Details

Osmotic and ionic regulation in the earthworm Lumbricus terrestris

ScholarsArchive at Oregon State University

Field Value
Title Osmotic and ionic regulation in the earthworm Lumbricus terrestris
Names Dietz, Thomas Howard (creator)
Alvarado, R. H. (advisor)
Date Issued 1969-05-01 (iso8601)
Note Graduation date: 1969
Abstract Earthworms are capable of osmotic and ionic regulation while
living in a dilute balanced salt solution. When transferred from soil
to pond-water (PW) their body weight increases by 15 percent due to
a net uptake of water.
This results in an initial dilution of the
coelomic fluid (CF).
Subsequently, Na and Cl are accumulated in net
amounts returning the CF ionic concentration to the same level as
when the animals were in soil (75 mM Na/1, 47 mM Cl/1).
Water is taken up across the skin.
Although worms in PW do
drink, the amount is minimal.
In a steady state, the rate of water
uptake and loss must be equal.
Water is voided as a hypo-osmotic
urine from the nephridia.
The clearance of Inulin and Dextran from
the CF is about 75 μl/10 g-hr.
Since some water is probably reabsorbed from the nephridia, this gives a maximum estimate of
urine excretion. Worms living in PW use their gastro-intestinal tract as an auxiliary excretory organ.
Fluid excreted from the rectum is hypo-osmotic and hypo-ionic to the CF.
It is hypothesized
that fluid entering the esophagous, at the level of the calciferous
gland, is an ultrafiltrate of the blood.
Chloride is reabsorbed from
the esophageal fluid in exchange for HCO₃ ions.
The esophageal
fluid enters the crop.
Fluid in the crop is similar in composition to
the CF except that the Cl concentration is lower (2 mM/l). As the
fluid passes down the intestine Na is reabsorbed in exchange for
NH₄, resulting in the formation of a dilute rectal fluid.
Earthworms living in a dilute aquatic environment accumulate
Na and Cl against an elecrochemical gradient by active transport
across the skin. Sodium and Cl are transported independently.
To
maintain electrical neutrality, Na is probably exchanged for NH₄ or
H ions and Cl exchanged for HCO₃.
Kinetic analysis of the Na
transport system for PW acclimated worms indicates a V[subscript m] of 1.1 μeq Na/10 g-hr and a K[subscript s] of 1.6 mM Na/1.
These values suggest
the epithelium is less permeable to Na than in most fresh-water
animals.
The ion transport systems are delicately regulated. A dilution of the CF increases the rate of active transport of both Na and
Cl. Sodium efflux is unchanged but the Cl efflux is reduced.
The
mechanism of regulation is unknown; however, neuroendocrine
mediation has been implicated. It is concluded that earthworms can adapt to an aquatic environment. However, they do possess some characteristics which
distinguish them from truely fresh-water animals.
The use of the
gastro-intestinal tract for producing a dilute fluid excreta is unique.
The relative low skin permeability to Na results in a Na transport
rate much lower in magnitude than fresh-water organisms of comparable size.
Genre Thesis/Dissertation
Topic Earthworms
Identifier http://hdl.handle.net/1957/46528

© Western Waters Digital Library - GWLA member projects - Designed by the J. Willard Marriott Library - Hosted by Oregon State University Libraries and Press