Sirius Passet
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Sirius Passet is a Cambrian Lagerstätte in Peary Land, Greenland. The Sirius Passet Lagerstätte was named after the Sirius sledge patrol that operates in North Greenland. It comprises six places in Nansen Land, on the east shore of J.P. Koch Fjord in the far north of Greenland. It was discovered in 1984 by A. Higgins of the Geological Survey of Greenland. A preliminary account was published by Simon Conway Morris and others in 1987 and expeditions led by J. S. Peel and Conway Morris have returned to the site several times between 1989 and the present. A field collection of perhaps 10,000 fossil specimens has been amassed. It is a part of the Buen Formation.
Age
The fauna is inevitably compared to that of the Burgess Shale, although it is probably ten to fifteen million years older – million years ago vs. million years ago) – and more closely contemporaneous with the fauna of the Maotianshan shales from Chengjiang, which are dated to million years ago.
Preservation
The preservation of the Sirius Passet is traditionally considered to represent silicification associated with a death mask, recalling the 'Ediacara-type' preservation of the Precambrian Ediacara biota. A 2022 study suggested that the original preservation mode was phosphatisation that was later altered by low-grade metamorphism with a peak temperature of 409 ± 50 °C (768 ± 90 °F) during the Devonian Ellesmerian orogeny, which resulted in widespread mineral replacement.
Geochemical analysis indicates that the fossils lived close to the boundary of an oxygen minimum zone, possibly being preserved in oxygen-starved periods.
IUGS geological heritage site
In respect of the importance of the exceptionally preserved fossils in our understanding of the event, the 'Cambrian Explosion in Sirius Passet' was included by the International Union of Geological Sciences (IUGS) in its assemblage of 100 'geological heritage sites' around the world in a listing published in October 2022. The organisation defines an 'IUGS Geological Heritage Site' as 'a key place with geological elements and/or processes of international scientific relevance, used as a reference, and/or with a substantial contribution to the development of geological sciences through history.'
Fauna
Although the fauna has not yet been fully described, it is known to consist of a moderate number of arthropods and sponges, and rare representatives of other groups. It has yielded the problematic taxon Halkieria, and the Panarthropods Kerygmachela and Pambdelurion, all of which have played prominent roles in discussions about the origins of the modern animal phyla.
Taxa from the Sirius Passet fauna
After
Arthropods
| Arthropods | |||
|---|---|---|---|
| Genus | Species | Notes | Images |
| Aaveqaspis | A. inesoni | An arthropod of uncertain affinities | |
| Arthroaspis | A. bergstroemi | A member of Artiopoda | |
| Buenaspis | B. forteyi | A nektaspid artiopod | |
| Buenellus | B. higginsi | A trilobite | |
| Campanamuta | C. mantoni | An artiopod | |
| Kleptothule | K. rasmusseni | A trilobite | |
| Molaria | M. steini | An artiopod | |
| Sidneyia? | Indeterminate | A vicissicaudatan artiopod, later authors have stated that the assignment to the genus is equivocal. | Life restoration of Sidneyia inexpectans from the Burgess Shale to which the Sirius Passet form has been considered closely related |
| Thulaspis | T. tholops | A basal artiopodan closely related to Squamacula. | |
| Siriocaris | S. trollae | A possible member of Lamellipedia | |
| Isoxys | I. volucris, I. sp | An Isoxyid arthropod | |
| Kiisortoqia | K. soperi | A basal arthropod with large frontal appendages | |
| Kerygmachela | K. kierkegaardi | A "gilled lobopodian" closely related to arthropods | |
| Pambdelurion | P. whittingtoni | A "gilled lobopodian" closely related to arthropods | |
| Tamisiocaris | T. borealis | A filter feeding radiodont | |
| Amplectobeluidae | Indeterminate | Predatory radiodont | |
| Pauloterminus | P. spinodorsalis | A shrimp-like arthropod, possibly a member of Hymenocarina |
Other animals
| Non-arthropod animals | |||
|---|---|---|---|
| Genus | Species | Notes | Images |
| Ooedigera | O. peeli | A vetulicolian, another indeterminate vetulicolian is also present | |
| Chordata | Indeterminate | Vertebrate-like chordate | |
| Hadranax | H. augustus | A lobopodian | |
| Halkieria | H. evangelista | A basal mollusc | |
| Xystoscolex | X. boreogyrus | A palaeoscolecid worm | |
| Chalazoscolex | C. pharkus | A palaeoscolecid worm | |
| Timorebestia | T. koprii | A giant stem-group chaetognath | |
| Nektognathus | N. evasmithae | A small nectocaridid, related to chaetognatha | |
| Chaetognatha | Indeterminate | Small-sized form | |
| Pygocirrus | P. butyricampum | An annelid worm | |
| Phragmochaeta | P. canicularis | A polychaete worm | |
| Singuuriqia | S. simony | A priapulid worm | |
| Sirilorica | S. carlsbergi, S. pustulosa | a stem-group Loricifera or a scalidophoran | |
| Hyolithus | H. cf. tenuis | A hyolith | |
| Trapezovitus | Indeterminate | ||
| Orthothecida | |||
| Hyolithida | |||
| Archaeocyatha | Indeterminate | A sponge | |
| Choia | C. cf. carteri | A sponge | |
| Constellatispongia | C. canismajorii | A sponge | |
| Crassicoactum | C. cucumis | A sponge | |
| Demospongiae | Indeterminate | A sponge | |
| Fieldospongia | F. bellineata | A sponge | |
| Hamptonia | H. limatula | A sponge | |
| Lenica | L. cf. unica L. hindei, L. perverse | A sponge | |
| Saetaspongia | S. cf. densa S. procera | A sponge | |
| Salactiniella | S. cf. plumata | A sponge | |
| Stephanella? | Indeterminate | A sponge |
See also
Further reading
- Martin, M.W.; Grazhdankin, D.V.; Bowring, S.A.; Evans, D.A.D.; Fedonkin, M.A.; Kirschvink, J.L. (2000). "Age of Neoproterozoic Bilaterian Body and Trace Fossils, White Sea, Russia: Implications for Metazoan Evolution". Science. 288 (5467): 841–845. Bibcode:. doi:. PMID .
- Harper, D. A. T.; Hammarlund, E. U.; Topper, T. P.; Nielsen, A. T.; Rasmussen, J. A.; Park, T.-Y. S.; Smith, M. P. (2019). . Journal of the Geological Society. 176 (6): 1023–1037. Bibcode:. doi:. S2CID .