Biol. Bull. Sign up for etocs!
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Biol Bull 135: 563-573. (December 1968)
© 1968 Marine Biological Laboratory
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by RUSSELL-HUNTER, W. D.
Right arrow Articles by APLEY, M. L.
Right arrow Search for Related Content
PubMed
Right arrow Articles by RUSSELL-HUNTER, W. D.
Right arrow Articles by APLEY, M. L.

PEDAL EXPANSION IN THE NATICID SNAILS. II. LABELLING EXPERIMENTS USING INULIN

W. D. RUSSELL-HUNTER 1 and MARTYN L. APLEY 2

1 Department of Zoology, Syracuse University, Syracuse, New York 13210
2 Department of Invertebrate Zoology, Marine Biological Laboratory, Woods Hole, Massachusetts 02543

1. Inulin-labelled sea water has been used in an investigation of the pedal water-sinus system, and other water spaces, in Polinices duplicatus. Analyses were by a photometric measurement of the reaction of inulin hydrolysate with resorcinol.

2. Of the sea water uptake during expansion: about 90% enters the pedal water-sinus system, about 5-7% is water which rapidly circulates through the mantle-cavity, and about 2% is superficial water on the snail's shell and expanded surfaces.

3. When the snail is in the contracted state a residual volume of sea water is retained in the pedal water-sinus system, and this can amount to 12.8% of the volume of the pedal system in the expanded snail.

4. There is no exchange between the water-sinus system and the blood at any time and, in the fully expanded snail, little or no exchange between the system and the environmental sea water. Labelling showed that 49-71% of the pedal sea water could remain unexchanged after 72 hours.

5. The surprisingly "stagnant" nature of the sea water in the pedal water-sinuses is discussed. Physiological consequences are probably slight, though, under certain ecological conditions, the large static water content is responsible for an unusual condition of temporary hyperthermia. A hypothesis, that little energy is expended by a Polinices in remaining fully expanded, is coupled with evidence of traumatic change in behavior resulting from sustained contraction. It seems likely that the features of water spaces and exchange rates demonstrated in Polinices duplicatus would be similar in any large naticid.




This article has been cited by other articles:


Home page
PALAIOSHome page
Post-Miocene Shift in Stereotypic Naticid Predation on Confamilial Prey from the Mid-Atlantic Shelf: Coevolution with Dangerous Prey
Palaios, October 1, 2000; 15(5): 414 - 429.





HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 1968 by the Marine Biological Laboratory.