Fractofusus misrai
| Fractofusus misrai Temporal range:
| |
|---|---|
| |
| Fractofusus misrai fossil in Newfoundland. | |
| Scientific classification | |
| Kingdom: | |
| Phylum: | |
| Class: | |
| Genus: | Gehling and Narbonne, 2007
|
| Species: | F. misrai
|
| Binomial name | |
| Fractofusus misrai Gehling and Narbonne, 2007
| |
Fractofusus misrai is an Ediacaran fossil discovered in 1967 by S.B. Misra at Mistaken Point, Newfoundland and Labrador, Canada, which has since become the Mistaken Point Ecological Reserve.[1] It was named after Professor Misra in 2007.[2] It represents a frondose rangeomorph, and its overall body plan shows glide reflection symmetry, which is typical of the clade. It is one of two described species in the genus Fractofusus, the other being Fractofusus andersoni.[2]
Discovery
[edit]
In the summer of 1967, S.B. Misra, an Indian graduate student (1966–69) at Newfoundland's Memorial University discovered a rich assemblage of imprints of soft bodied organisms on the surface of large rock slabs, while mapping the Conception Group of Avalon Peninsula of Newfoundland near Cape Race, at a place called Mistaken Point.[3]
These unusual impressions of previously unknown soft-bodied sea animals on the surfaces of argillites (mudstone) included coelenterates and other metazoa of the Ediacarian period, 575 to 560 million years ago.[4] These fossils are records of some of the oldest known complex life forms that existed anywhere on Earth. Misra was the first to prepare and present a systematic geological map of the region, to classify and describe the rock sequence of the area and to work out the depositional history of the rocks.
The description of the fossil assemblage together with their mode of occurrence, the cause of sudden death, ecological conditions and chronological position form part of Misra's detailed thesis submitted for a degree of Master of Science. The discovery was reported in a 1968 letter to Nature.[5] Misra described the Mistaken Point fauna in detail in 1969, in a paper published in the Bulletin of the Geological Society of America.[6] He sorted the fossil assemblage into five groups, namely spindle-shaped, leaf-shaped, round lobate, dendrite like, and radiating. Each group was defined in terms of distribution and form, sub-categories and biological affinity.[3]
The geological environment of the fossil-bearing rocks and the ecology of the animals that lived and died in the Conception Sea were described by Misra in two of his subsequent papers published in the Bulletin of the Geological Society of America in 1971[7] and in the Journal of the Geological Society of India in 1981.[8] Mistaken Point Ecological Reserve is a 5.7-square kilometer area of the coast that protects the fossils.[4]
Reproductive strategy
[edit]The distribution pattern of Fractofusus suggests that it had an effective reproductive strategy. This appears to have consisted of sending out a waterborne propagule to a distant area, and then spreading rapidly from there, very likely asexually, just as plants today spread by stolons or runners.[9][10]
See also
[edit]References
[edit]- ^ "Rare honour for Indian geologist". South Asia. BBC News. 18 September 2007. Retrieved 10 July 2011.
- ^ a b Gehling, James G; Narbonne, Guy M (2007). "Spindle-shaped Ediacara fossils from the Mistaken Point assemblage, Avalon Zone, Newfoundland". Canadian Journal of Earth Sciences. 44 (3): 367–387. doi:10.1139/e07-003.
- ^ a b "Mistaken Point, Newfoundland". www.ucmp.berkeley.edu. Retrieved 2017-07-16.
- ^ a b "Mistaken Point Ecological Reserve". Newfoundland and Labrador, Dept. of Environment and Conservation.
- ^ Anderson, M. M.; Misra, S. B. (16 November 1968). "Fossils found in pre-Cambrian Conception Group of southeastern Newfoundland". Nature. 220 (5168): 680–681. doi:10.1038/220680a0.
- ^ Misra, S.B. (November 1969). "Late Precambrian(?) fossils from southeastern Newfoundland". Geological Society of America Bulletin. 80 (11): 2133–2140. doi:10.1130/0016-7606(1969)80[2133:LPFFSN]2.0.CO;2.
- ^ Misra, S.B. (April 1971). "Stratigraphy and Depositional History of Late Precambrian Coelenterate-Bearing Rocks, Southeastern Newfoundland". Geological Society of America Bulletin. 82 (4): 979–988. doi:10.1130/0016-7606(1971)82[979:SADHOL]2.0.CO;2.
- ^ Misra, S.B. (August 1981). "Depositional Environment of the Late Precambrian Fossil-Bearing rocks of Southeastern Newfoundland, Canada". Journal of Geological Society of India. 22 (8).
- ^ Mitchell, Emily G.; Kenchington, Charlotte G.; Liu, Alexander G.; Matthews, Jack J.; Butterfield, Nicholas J. (2015). "Reconstructing the reproductive mode of an Ediacaran macro-organism". Nature. 524 (7565): 343–346. doi:10.1038/nature14646. hdl:1983/93446a6e-8c30-4927-992b-1f7fea755961. PMID 26237408.
- ^ Collins, Sarah. "Earliest evidence of reproduction in a complex organism". University of Cambridge. Retrieved 3 August 2015.