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Dunlop, Jason A., Anderson, Lyall I., Braddy, Simon J. (1998) A new chasmataspid (Chelicerata: Chasmataspida) from the Lower Devonian of the Midland Valley of Scotland. Transactions of the Royal Society of Edinburgh: Earth Sciences, 89 (3) 161-165 doi:10.1017/s0263593300007100

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Reference TypeJournal (article/letter/editorial)
TitleA new chasmataspid (Chelicerata: Chasmataspida) from the Lower Devonian of the Midland Valley of Scotland
JournalTransactions of the Royal Society of Edinburgh: Earth Sciences
AuthorsDunlop, Jason A.Author
Anderson, Lyall I.Author
Braddy, Simon J.Author
Year1998Volume89
Issue3
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0263593300007100Search in ResearchGate
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Mindat Ref. ID494541Long-form Identifiermindat:1:5:494541:7
GUID0
Full ReferenceDunlop, Jason A., Anderson, Lyall I., Braddy, Simon J. (1998) A new chasmataspid (Chelicerata: Chasmataspida) from the Lower Devonian of the Midland Valley of Scotland. Transactions of the Royal Society of Edinburgh: Earth Sciences, 89 (3) 161-165 doi:10.1017/s0263593300007100
Plain TextDunlop, Jason A., Anderson, Lyall I., Braddy, Simon J. (1998) A new chasmataspid (Chelicerata: Chasmataspida) from the Lower Devonian of the Midland Valley of Scotland. Transactions of the Royal Society of Edinburgh: Earth Sciences, 89 (3) 161-165 doi:10.1017/s0263593300007100
In(1998) Transactions of the Royal Society of Edinburgh: Earth Sciences Vol. 89 (3) Cambridge University Press (CUP)
Abstract/NotesAbstractA new chasmataspid (Chelicerata, Chasmataspida) is described as Forfarella mitchelli gen. et sp. nov. from the Lower Devonian of Scotland. This species is problematic in that it was catalogued under the name Forfarella mitchelli Waterston (no date), but was never formally described. Furthermore, its type locality is uncertain. Chasmataspids are a poorly known taxon within Chelicerata which appear to be closely related to eurypterids. F. mitchelli is only the fourth chasmataspid species to be described. Though poorly preserved, it shows affinities with other Devonian chasmataspids and supports the hypothesis that this group may have been more geographically widespread in the Devonian than has previously been recognised.


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