Paratype: | 96.8G.960 |
Locality: | Henllan Brook, Llanelwedd, Powys |
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Rock Unit: | Llanfawr Mudstone Formation |
Geological Age: | Llandeilian Stage (Ordovician Period) (458.4 – 460.5 Ma B.P.) |
Resources: | {None available} |
Paratype: | 96.8G.961 |
Locality: | Henllan Brook, Llanelwedd, Powys |
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Rock Unit: | Llanfawr Mudstone Formation |
Geological Age: | Llandeilian Stage (Ordovician Period) (458.4 – 460.5 Ma B.P.) |
Resources: | {None available} |
Paratype: | 96.8G.962 |
Locality: | Treffgarne, Haverfordwest, Pembrokeshire |
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Rock Unit: | Unknown |
Geological Age: | Arenig Series (Ordovician Period) (465.5 – 477.7 Ma B.P.) |
Resources: | {None available} |
Paratype: | 96.8G.963 |
Locality: | Treffgarne, Haverfordwest, Pembrokeshire |
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Rock Unit: | Unknown |
Geological Age: | Arenig Series (Ordovician Period) (465.5 – 477.7 Ma B.P.) |
Resources: | {None available} |
Lectotype: | A 10284 |
Locality: | Keisley, Westmorland, England |
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Rock Unit: | Keisley Limestone |
Geological Age: | Ashgill Series (Ordovician Period) (443.8 – 449 Ma B.P.) |
Resources: |
Lectotype: | A 10294 |
Locality: | Pusgill, Dufton, Westmorland, England |
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Rock Unit: | Corona Bed |
Geological Age: | Longvillian Substage (Ordovician Period) (452.75 – 454 Ma B.P.) |
Resources: |
Syntype: | A 10295 |
Locality: | Pusgill, Dufton, Westmorland, England |
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Rock Unit: | Corona Bed |
Geological Age: | Longvillian Substage (Ordovician Period) (452.75 – 454 Ma B.P.) |
Resources: |
Syntype: | A 10296 |
Locality: | Melmerby (cutting on Alston Road), Cumberland, England |
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Rock Unit: | Dufton Shale |
Geological Age: | Caradoc Series (Ordovician Period) (449 – 458.4 Ma B.P.) |
Resources: |
Syntype: | A 10297 |
Locality: | Melmerby (cutting on Alston Road), Cumberland, England |
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Rock Unit: | Dufton Shale |
Geological Age: | Caradoc Series (Ordovician Period) (449 – 458.4 Ma B.P.) |
Resources: |
Syntype: | A 10298 |
Locality: | Melmerby (cutting on Alston Road), Cumberland, England |
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Rock Unit: | Dufton Shale |
Geological Age: | Caradoc Series (Ordovician Period) (449 – 458.4 Ma B.P.) |
Resources: |