Erniettomorph
| Erniettomorph Temporal range:
| |
|---|---|
| Swartpuntia, an erniettomorph | |
| Scientific classification | |
| Kingdom: | Animalia |
| Phylum: | †Petalonamae |
| Class: | †Erniettomorpha Pflug, 1972 |
| Genera | |
The Erniettomorphs are a form of Ediacaran fossil consisting of rows of airbed-like tubes arranged along a midline with a glide symmetry, vaguely resembling plant leaves in shape. Representative genera include Ernietta, Phyllozoon, Pteridinium, Swartpuntia, and Tulaneia.[1][2] Undisputed Erniettomorphs were Ediacaran, but the genera Erytholus, Rutgersella, and Protonympha, who have by some been included in this group but are by no means clear members, are found through to the Late Devonian. Their affinity is uncertain; they probably form a clade and are most likely a sister group to the rangeomorphs, which bear a similar (though fractal) construction. Placements within the metazoan crown-group have been rebutted, and it is most likely that these peculiar organisms lie in the stem group to the animals.[1] There is no evidence that they possessed a mouth or gut.[1] Because they may have been found in water which was too deep to permit photosynthesis – and in some cases, lived half-buried in sediment, it is speculated that they fed by osmosis from the sea water.[3] Such a lifestyle requires a very high surface area to volume ratio – higher than is observed in fossils. However, this paradox can be resolved if much of the volume of the organisms was not metabolically active. Many Pteridinium fossils are found completely filled with sand; if this sand were present within the organism while it was alive, this would reduce its metabolically active volume enough to make osmotic feeding viable.[3]
See also
- Rangeomorpha, a probable sister clade
- Proarticulata, sharing similar 'glide symmetry'
- Ediacara biota, for an overview of the bizarre late Ediacaran organisms
- List of Ediacaran genera
References
- ^ a b c Xiao, S.; LaFlamme, M. (2009). "On the eve of animal radiation: phylogeny, ecology and evolution of the Ediacara biota". Trends in Ecology & Evolution. 24 (1): 31–40. doi:10.1016/j.tree.2008.07.015. PMID 18952316.
- ^ Runnegar, Bruce; Horodyski, Robert J.; Gehling, James G.; Jensen, Sören; Bengtson, Stefan; Peterson, Kevin J.; Saltzman, Matthew R.; Vendrasco, Michael J. (November 2024). "Tulaneia amabilia n. gen. n. sp.: a new erniettomorph from the Wood Canyon Formation, Nevada and the age of the Ediacaran–Cambrian transition in the Great Basin". Journal of Paleontology. 98 (6): 929–951. doi:10.1017/jpa.2024.45.
- ^ a b Laflamme, M.; Xiao, S.; Kowalewski, M. (2009). "Osmotrophy in modular Ediacara organisms". Proceedings of the National Academy of Sciences. 106 (34): 14438–14443. Bibcode:2009PNAS..10614438L. doi:10.1073/pnas.0904836106. PMC 2732876. PMID 19706530.
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