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


     


Biol Bull 110: 320-333. (June 1956)
© 1956 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 Google Scholar
Google Scholar
Right arrow Articles by OKAZAKI, K.
Right arrow Search for Related Content
PubMed
Right arrow Articles by OKAZAKI, K.

SKELETON FORMATION OF SEA URCHIN LARVAE. I. EFFECT OF CA CONCENTRATION OF THE MEDIUM

KAYO OKAZAKI 1

1 Department of Biology, Tokyo Metropolitan University, Setagaya-ku, Tokyo and Misaki Marine Biological Station, Misaki, Miura-City, Japan

1. The threshold Ca concentration for the growth of the larval skeleton is lower than that which permits the normal development of sea urchin larvae.

2. The time of the beginning of skeleton formation is retarded by a decrease in Ca concentration from the normal level, while an increased Ca concentration has little effect in this respect.

3. Modification of the Ca concentration of the medium influences the form of the skeleton of sea urchin larvae.

a). In larvae transferred to very dilute calcium before the time of skeleton formation, a mass of unorganized skeletal substance develops.

b). In larvae put into very concentrated calcium from a similarly early stage, several tri-radiate spicules are formed in each larva, but these fail to make a typical skeleton.

c). If the transfer is deferred till the tri-radiate spicules are formed, new skeletal development in the experimental media is continued on the old spicules, and a pluteus skeleton which is similar to the typical one results, though it is much stunted in Ca-low, and slender in Ca-high media.

d). The proportion of the thickness to the length of the skeleton is inversely proportional to the Ca concentration. This is true regardless of the stage of transfer.

e). The elongation of the skeletal rods is inhibited at the extremes of the Ca-series, particularly on the dilute side.

f). The apparent increase in skeletal length is rather better in 0.6 or 0.8 Ca than in high-calcium, except that the contrary situation holds for a short time after transfer.

4. The ectoderm of the presumptive arm may differentiate without any skeleton. However, such differentiated ectoderm finally falls off from the body or disappears unless the supporting skeleton develops.

5. It is suggested that an organic matrix may be formed before deposition of the mineral components of the skeleton; that this matrix is deformed by changes in the calcium concentration; and that such deformation, in turn, influences the rate of growth and the form of the skeleton.







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 1956 by the Marine Biological Laboratory.