Sidneyia
Sidneyia is an extinct marine arthropod known from fossils found from the Early to the Mid Cambrian of China and the Mid Cambrian Burgess Shale of British Columbia, Canada. It is thought to have been a durophagous (crushing) predator that used its spine-covered leg bases (gnathobases) to feed on hard-bodied animals like trilobites and brachiopods, as well as possibly soft bodied animals. It was historically placed in the group "Xenopoda" alongside Emeraldella. It is now placed within the clade Vicissicaudata along with aglaspidids, chelonellids, as well as Emeraldella, among others. Vicissicaudata forms part of the broader group Artiopoda, which includes trilobites.

Qohelet12 · CC BY-SA 4.0 · via Wikipedia/Commons. May be a photograph of a specimen, or an artist’s reconstruction — an interpretation of a skeleton, since colour and soft tissue are almost never preserved.
On record
Recorded, not inferred- Sits inside
- VicissicaudataPBDB
- Diet
- carnivorePBDB
- Life habit
- nektobenthicPBDB
- Motility
- actively mobilePBDB
Time the record covers
At least 3.2 million years on record.
The record covers at least 509.7 Mya to 506.5 Mya. No occurrence read is dated outside 515.3 Mya to 497 Mya.
33 occurrences of Sidneyia on record, most of them in the Cambrian. Bar height is expected occurrences, not a count: each fossil is spread across the span it is dated to, so a tall narrow bar means tight dating and a low wide one means loose.
When
33 occurrences- Cambrian100%
These are dates about fossils, not the animal: the record can only begin after it arose and end before it died out, so either end may reach further. Shares are expected occurrences: a fossil dated to a span is counted partly in each period it straddles. More on what this infers.
Found in
7 formations
- Burgess Shale Formation · Chancellor Group25
- Kinzers Formation2
- Stephen Formation2
- Lower Wheeler Shale Formation1
- Langston Formation1
- Mantou Formation1
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The named rock units Sidneyia has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Sidneyia and its relatives
CambrianWhere Sidneyia and its relatives were recorded in the Cambrian.
Found in the same rock
312 taxa- Liangshanella23 sites
- Diraphora22 sites
- Ehmaniella burgessensis22 sites
- Hazelia22 sites
- Marrella splendens22 sites
- Selkirkia columbia22 sites
- Wiwaxia corrugata22 sites
- Burgessia21 sites
- Morania21 sites
- Ottoia prolifica21 sites
- Pentagnostus praecurrens21 sites
- Waptia fieldensis21 sites
- Yohoia21 sites
- Canadaspis perfecta20 sites
- Haplophrentis carinatus20 sites
- Naraoia compacta20 sites
- Scenella amii20 sites
- Laggania19 sites
- Micromitra19 sites
- Pollingeria grandis19 sites
- Hurdia18 sites
- Lingulella17 sites
- Trilobita17 sites
- Tubullela sp.17 sites
The Paleobiology Database records 31 sites for Sidneyia, and this reads all of them. The number is how many of those sites it was catalogued from too. The 24 sharing the most are listed.
This is not a list of everything alive at the time. It is only what has come out of the same ground as this animal and been written down.
Entered from
11 references- Paleoecology of the Greater Phyllopod Bed community, Burgess Shale22
- Lower Cambrian Olenellus zone of the Appalachians2
- A Cambrian soft-bodied biota after the first Phanerozoic mass extinction1
- Occurrence of the hurdiid radiodont Cambroraster in the middle Cambrian (Wuliuan) Mantou Formation of North China1
- Paleocommunity analysis of the Burgess Shale Tulip Beds, Mount Stephen, British Columbia: Comparison with the Walcott Quarry and implications for community variation in the Burgess Shale1
- A new phyllopod bed-like assemblage from the Burgess Shale of the Canadian Rockies1
- A new Burgess Shale–type assemblage from the “thin” Stephen Formation of the southern Canadian Rockies1
- Palaeontology and depositional environments of ancient brine seeps in the Middle Cambrian Burgess Shale at The Monarch, British Columbia, Canada1
- Middle Cambrian arthropods from Utah1
- The Burgess Shale and associated Cambrian formations west of the Fossil Gully Fault Zone on Mount Stephen, British Columbia1
- Exceptionally preserved nontrilobite arthropods and Anomalocaris from the Middle Cambrian of Utah1
Each of the 33 occurrences read was entered from one of these publications, ordered by how many each accounts for. This is not a search for papers mentioning the name. Entries link to doi.org where the Paleobiology Database holds an identifier, and to its own record where it does not. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.
Media and terms
Media content1
Picture of Sidneyia
- Source
- Wikipedia/Commons
- Credit
- Qohelet12
- Licence
- CC BY-SA 4.0
- Commercial use
- the licence allows it
No 3D scan was found. Smithsonian Open Access, MorphoSource and Sketchfab were all searched.
The description on this site
- Source
- Wikipedia, “Sidneyia”
- Licence
- CC BY-SA 4.0
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itVicissicaudata through timeFormations of the CambrianThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Walcott 1911