Abstract
Archaeomonads are chrysophyte cysts abundant in Weddell Sea sea ice, but they form in the water column in reponse to conditions that occur in areas where no sea ice is present. The association between archaeomonads and sea ice depends on a particular sequence of oceanographic conditions, beginning with lateral advection followed by vertical harvesting on rising ice crystals. Comparing fossil and modern distributions suggests archaeomonads underwent an ecological transition or expansion in the Early Tertiary Period, from sediment underlying anoxic waters to sediments underlying sea ice.
Original language | English |
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Pages (from-to) | 289-298 |
Number of pages | 10 |
Journal | BioSystems |
Volume | 19 |
Issue number | 4 |
DOIs | |
Publication status | Published - 1986 |
Externally published | Yes |
Bibliographical note
Funding Information:We thank C. Barnes, L. LaPorte, J. PearseA, . Sater,a ndan anonymourse viewer for helpful commentos n the manuscriptT. . Foster generouslyp rovidedship time and access to physical data. D. Buckry, D. Garrison,K . Buck, S. Ackley,a ndH. Tappan provided valuable discussion.L . Margulis gave much appreciateedn couragemenant d stimulation.T his work was supportedb y NSF grants DPP 7514936,D PP 78-07797, DPP 80-20616.
Keywords
- Archaeomonad
- Chrysophyte cyst
- Paleoecology
- Sea ice
- Weddell Sea