Hostname: page-component-cd9895bd7-dzt6s Total loading time: 0 Render date: 2024-12-27T10:19:55.457Z Has data issue: false hasContentIssue false

Using the term utricle

Published online by Cambridge University Press:  20 May 2016

Andrew M. Torres
Affiliation:
Department of Botany and The Kansas Geological Survey, University of Kansas, Lawrence 66045
D. L. Baars
Affiliation:
Department of Botany and The Kansas Geological Survey, University of Kansas, Lawrence 66045

Extract

Certain groups of living Chlorophyta (green algae) have thalli made up of long, tubular cells with many nuclei and many plastids (Tappan, 1980; Bold and Wynne, 1985). The only cross walls in these coenocytes are those that isolate the gamete-producing structures. As the coenocytes approach the edges of the thallus, they branch, generally dichotomously, one or more times and eventually terminate in clavate or bulbous segments called utricles (Latin for small bag or bottle). Thus, the utricles are the termini of coenocytes that occur along the surface of the thallus and interface with the environment. Utricles have been figured in many descriptions and illustrations of such calcified genera as Halimeda (Wray, 1977) and such noncalcareous genera as Codium (Bold and Wynne, 1985). Because of the easily recognized distinction between the parts of the coenocytes, the thallus in cross section consists of a cortex occupied by the utricles and their contiguous segments and a medulla occupied by the long tubular portions of the cell (Figure 1).

Type
Paleontological Notes
Copyright
Copyright © The Paleontological Society 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Baars, D. L. 1968. Nature of calcification in codiacean algae. American Association of Petroleum Geologists Bulletin, 52:518.Google Scholar
Bold, H. C., and Wynne, A. J. 1985. Introduction to the Algae. 2nd edition. Prentice-Hall, Englewood Cliffs, New Jersey, 720 p.Google Scholar
Borowitzka, M. A., and Larkum, A. W. D. 1976. Calcification in the green alga Halimeda. Journal of Experimental Botany, 27:879893.Google Scholar
Hillis-Colinvaux, L. 1980. Ecology and taxonomy of Halimeda: primary producers of coral reefs. Journal for the Advancement of Marine Biology, 17:1327.Google Scholar
Kirkland, B. L., Moore, C. H. Jr., and Dickson, J. A. D. 1991. Aragonitic Pennsylvanian phylloid algae from New Mexico: the missing link. American Association of Petroleum Geologists Bulletin, 75:610.Google Scholar
Mankiewicz, C. M. 1988. Occurrence and paleoecologic significance of Halimeda in late Miocene reefs, southeastern Spain. Coral Reefs, 6:271279.Google Scholar
Scoffin, T. P. 1987. An Introduction to Carbonate Sediments and Rocks. Chapman and Hall, New York, 274 p.Google Scholar
Tappan, H. 1980. The Paleobiology of Plant Protists. W. H. Freeman and Company, San Francisco, 1,028 p.Google Scholar
Wilbur, K. M., Colinvaux, L. H., and Watabe, N. 1969. Electron microscope study of calcification in the alga Halimeda (order Siphonales). Phycologia, 8:2735.Google Scholar
Wray, J. L. 1977. Calcareous Algae. Elsevier, New York, 185 p.Google Scholar