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Record #107369:
- #107369
Main publication details
MARC recordTrace fossils from the Lower Cambrian Bastion Formation of North-East Greenland / Ron K. Pickerill, John S. Peel.
| Title: | Trace fossils from the Lower Cambrian Bastion Formation of North-East Greenland / Ron K. Pickerill, John S. Peel. |
| Author(s): | Pickerill, Ron K. Peel, John S. |
| Date: | 1990. |
| In: | Grønlands Geologiske Undersøgelse. Rapport. (1990.), Vol. 147 (1990) |
| Abstract: | Describes new trace fossil collections from siliciclastic shallow marine shelf deposits, with taxonomic re-assessment of previously reported material. Entire assemblage comprises 19 ichnogenera, 25 ichnospecies, and two vernacular ichnotaxa. Stratigraphic range of Rusophycus latus Webby is formally extended from Lower Ordovician to Lower Cambrian. Comparison with similar sequences suggests that sub-trilobitic Lower Bastion Formation is late Tommotian to early Atdabanian in age, possibly entirely Atdabanian. |
| Notes: | Grønlands Geologiske Undersøgelse. Rapport. Vol. 147 :5-43 (1990). |
| Keywords: | 551.7 -- Stratigraphy. 551.732 -- Cambrian. 551.733.1 -- Ordovician. 56 -- Palaeontology. B -- Geology and soil sciences. (*38) -- Greenland. (*381.4) -- Kong Christian den Xs Land. |
| SPRI record no.: | 107369 |
LDR 01455naa#a2200000#a#4500 001 SPRI-107369 005 20240419023454.0 007 ta 008 240419s1990####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-107369 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aPickerill, Ron K. 245 10 ‡aTrace fossils from the Lower Cambrian Bastion Formation of North-East Greenland /‡cRon K. Pickerill, John S. Peel. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1990. 300 ## ‡ap. 5-43 :‡bill., table, maps. 500 ## ‡aGrønlands Geologiske Undersøgelse. Rapport. Vol. 147 :5-43 (1990). 520 3# ‡aDescribes new trace fossil collections from siliciclastic shallow marine shelf deposits, with taxonomic re-assessment of previously reported material. Entire assemblage comprises 19 ichnogenera, 25 ichnospecies, and two vernacular ichnotaxa. Stratigraphic range of Rusophycus latus Webby is formally extended from Lower Ordovician to Lower Cambrian. Comparison with similar sequences suggests that sub-trilobitic Lower Bastion Formation is late Tommotian to early Atdabanian in age, possibly entirely Atdabanian. 650 07 ‡a551.7 -- Stratigraphy.‡2udc 650 07 ‡a551.732 -- Cambrian.‡2udc 650 07 ‡a551.733.1 -- Ordovician.‡2udc 650 07 ‡a56 -- Palaeontology.‡2udc 650 07 ‡aB -- Geology and soil sciences.‡2local 651 #7 ‡a(*38) -- Greenland.‡2udc 651 #7 ‡a(*381.4) -- Kong Christian den Xs Land.‡2udc 700 1# ‡aPeel, John S. 773 0# ‡7nnas ‡tGrønlands Geologiske Undersøgelse. Rapport. ‡gVol. 147 (1990) ‡wSPRI-39401 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240419