Chasmataspidida
Chasmataspidids, sometime referred to as chasmataspids, are a group of extinct chelicerate arthropods that form the order Chasmataspidida. Chasmataspidids are probably related to horseshoe crabs (Xiphosura) and/or sea scorpions (Eurypterida), while more recent studies suggest that they form a clade (Dekatriata) with Eurypterida and Arachnida. Chasmataspidids are known sporadically in the fossil record through to the mid-Devonian, with possible evidence suggesting that they were also present during the late Cambrian. Chasmataspidids are most easily recognised by having an opisthosoma divided into a wide forepart (preabdomen) and a narrow hind part (postabdomen) each comprising 4 and 9 segments respectively. There is some debate about whether they form a natural group.

James C. Lamsdell, Gerald O. Gunderson and Ronald C. Meyer · 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
- DekatriataPBDB
- Motility
- actively mobilePBDB, for Arthropoda
Time the record covers
At least 83 million years on record.
The record covers at least 477.1 Mya to 393.47 Mya. No occurrence read is dated outside 486.85 Mya to 382.31 Mya.
21 occurrences of Chasmataspidida on record, most of them in the Devonian. 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
21 occurrences- Ordovician19%
- Silurian14%
- Devonian67%
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
13 formations
- Zub Formation4
- Zub or Kureika Formation2
- Big Hill Formation · Richmond Group2
- Sundvollen Formation1
- Blackford Formation1
- Siegen Formation1
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The named rock units Chasmataspidida has been recovered from, largest first. Drawn where the rock is now, not where it formed. 3 occurrences have no formation on record, which is common for older literature.
Chasmataspidida and its relatives
DevonianWhere Chasmataspidida and its relatives were recorded in the Devonian.
Found in the same rock
134 taxa- Heteroaspis stoermeri3 sites
- Borchgrevinkium taimyrensis2 sites
- Diploaspis casteri2 sites
- Dvulikiaspis menneri2 sites
- Parahughmilleria hefteri2 sites
- Pterygotus2 sites
- Skrytyaspis andersoni2 sites
- Xiphosurida2 sites
- Acanthacanthus ornatus1 site
- Acanthopora transitans1 site
- Acanthospina irregulare1 site
- Achanarraspis reedi1 site
- Acritolepis urvantsevi1 site
- Acritolepis ushakovi1 site
- Actinoceras1 site
- Adelophthalmus sievertsi1 site
- Alkenia mirabilis1 site
- Alkenopterus brevitelson1 site
- Angaraspis urvantzevi1 site
- Animalia1 site
- Apiculatisporis1 site
- Archaeobatophora typa1 site
- Archaeomartus levis1 site
- Archaeometa1 site
The Paleobiology Database records 16 sites for Chasmataspidida, 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
13 references- A diverse chasmataspidid (Arthropoda: Chelicerata) fauna from the Early Devonian (Lochkovian) of Siberia8
- Arthropods from the Lower Devonian (Lower Emsian) of Alken an der Mosel, Germany. Part 2. Xiphosura2
- A common arthropod from the Late Ordovician Big Hill Lagerstätte (Michigan) reveals an unexpected ecological diversity within Chasmataspidida1
- The first diploaspidid (Chelicerata: Chasmataspidida) from North America (Silurian, Bertie Group, New York State) is the oldest species of Diploaspis1
- A new Lagerstätte from the Late Ordovician Big Hill Formation, Upper Peninsula, Michigan1
- The Fezouata fossils of Morocco; an extraordinary record of marine life in the Early Ordovician1
- Chelicerate arthropods, including the oldest phalangiotarbid arachnid, from the Early Devonian (Siegenian) of the Rhenish Massif, Germany1
- The first Silurian chasmataspid, Loganamaraspis dunlopi gen. et sp. nov. (Chelicerata: Chasmataspidida) from Lesmahagow, Scotland, and its implications for eurypterid phylogeny1
- Arthropods from the Lower Devonian Severnaya Zemlya Formation of October Revolution Island (Russia)1
- A Middle Devonian chasmataspid arthropod from Achanarras Quarry, Caithness, Scotland1
- Silurian communities of the Oslo Region, Norway1
- A new chasmataspid (Chelicerata: Chasmataspida) from the Lower Devonian of the Midland Valley of Scotland1
Each of the 21 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. 1 further reference is not listed. 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 Chasmataspidida
- Source
- Wikipedia/Commons
- Credit
- James C. Lamsdell, Gerald O. Gunderson and Ronald C. Meyer
- Licence
- CC BY-SA 4.0
- Commercial use
- the licence allows it
No 3D scan of Chasmataspidida was found in MorphoSource and Sketchfab.
Smithsonian Open Access was not reached for this taxon, so this list is what the others held rather than everything there is.
The description on this site
- 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 itDekatriata through timeFormations of the DevonianThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Caster and Brooks 1956)