Osmotrofia em organismos modulares da fauna Ediacara

Osmotrophy in modular Ediacara organisms

Marc Laflamme,1, Shuhai Xiao and Michał Kowalewski

+ Author Affiliations

Department of Geosciences, Virginia Polytechnic Institute and State University, Blacksburg, VA 24061

Abstract

The Ediacara biota include macroscopic, morphologically complex soft-bodied organisms that appear globally in the late Ediacaran Period (575–542 Ma). The physiology, feeding strategies, and functional morphology of the modular Ediacara organisms (rangeomorphs and erniettomorphs) remain debated but are critical for understanding their ecology and phylogeny. Their modular construction triggered numerous hypotheses concerning their likely feeding strategies, ranging from micro-to-macrophagus feeding to photoautotrophy to osmotrophy. Macrophagus feeding in rangeomorphs and erniettomorphs is inconsistent with their lack of oral openings, and photoautotrophy in rangeomorphs is contradicted by their habitats below the photic zone. Here, we combine theoretical models and empirical data to evaluate the feasibility of osmotrophy, which requires high surface area to volume (SA/V) ratios, as a primary feeding strategy of rangeomorphs and erniettomorphs. Although exclusively osmotrophic feeding in modern ecosystems is restricted to microscopic bacteria, this study suggests that (i) fractal branching of rangeomorph modules resulted in SA/V ratios comparable to those observed in modern osmotrophic bacteria, and (ii) rangeomorphs, and particularly erniettomorphs, could have achieved osmotrophic SA/V ratios similar to bacteria, provided their bodies included metabolically inert material. Thus, specific morphological adaptations observed in rangeomorphs and erniettomorphs may have represented strategies for overcoming physiological constraints that typically make osmotrophy prohibitive for macroscopic life forms. These results support the viability of osmotrophic feeding in rangeomorphs and erniettomorphs, help explain their taphonomic peculiarities, and point to the possible importance of earliest macroorganisms for cycling dissolved organic carbon that may have been present in abundance during Ediacaran times.

erniettomorphs rangeomorphs Fractofusus Pteridinium

Footnotes

1To whom correspondence should be sent at the present address: Department of Geology and Geophysics, Yale University, P.O. Box 208109, New Haven, CT 06520-8190. E-mail: marc.laflamme@yale.edu

Author contributions: M.L., S.X., and M.K. designed research; M.L. performed research; M.K. contributed new reagents/analytic tools; M.L., S.X., and M.K. analyzed data; and M.L., S.X., and M.K. wrote the paper.

Edited by James W. Valentine, University of California, Berkeley, CA, and approved July 7, 2009

The authors declare no conflict of interest.

This article is a PNAS Direct Submission.

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