Patrick Burn Formation: Difference between revisions
Content deleted Content added
Citation bot (talk | contribs) Add: newspaper, bibcode. | Use this bot. Report bugs. | Suggested by Wiiformii | Category:CS1 errors: extra text: volume | #UCB_Category 942/958 |
GreenC bot (talk | contribs) Move 1 url. Wayback Medic 2.5 per WP:URLREQ#fossilworks.org |
||
| Line 28: | Line 28: | ||
== Description == |
== Description == |
||
According to the [[British Geological Survey]], the primary lithology of the formation consists of "Alternating beds of grey [[feldspathic]], medium-grained [[Turbidite|turbiditic]] [[sandstone]] and grey [[siltstone]] with beds of grey [[Lamination (geology)|laminated]] siltstone and silty [[mudstone]]."<ref>{{Cite web |title=Patrick Burn Formation |url=https://webapps.bgs.ac.uk/lexicon/lexicon.cfm?pub=PKB |access-date=2023-09-02 |website=BGS Lexicon of Named Rock Units |publisher=British Geological Survey}}</ref> The Birk Knowes site contains fossils from non-marine or marginal marine environment.<ref>{{Cite journal |last1=Tetlie |first1=O. Erik |last2=Braddy |first2=Simon J. |date=2003 |title=The first Silurian chasmataspid, Loganamaraspis dunlopi gen. et sp. nov. (Chelicerata: Chasmataspidida) from Lesmahagow, Scotland, and its implications for eurypterid phylogeny |url=https://www.cambridge.org/core/journals/earth-and-environmental-science-transactions-of-royal-society-of-edinburgh/article/abs/first-silurian-chasmataspid-loganamaraspis-dunlopi-gen-et-sp-nov-chelicerata-chasmataspidida-from-lesmahagow-scotland-and-its-implications-for-eurypterid-phylogeny/F2355DC34D69BB2A800023B67F4A4581 |journal=Earth and Environmental Science Transactions of the Royal Society of Edinburgh |language=en |volume=94 |issue=3 |pages=227–234 |doi=10.1017/S0263593300000638 |s2cid=73596575 |issn=1473-7116}}</ref> In 2000, Birk Knowes was closed by the Scottish government agency Scottish Natural Heritage (now [[NatureScot]]), due to the theft of specimens from the site by amateur collectors during the preceding decades, who essentially exhausted the fossiliferous deposit. At least some of the fossils ended up in a museum in Berlin, who refused to return them.<ref>{{Cite web |last=Williams |first=Huw |date=2003 |title=Filched Fish Fossils |url=https://www.bbc.co.uk/radio4/today/reports/archive/science_nature/fossils.shtml |
According to the [[British Geological Survey]], the primary lithology of the formation consists of "Alternating beds of grey [[feldspathic]], medium-grained [[Turbidite|turbiditic]] [[sandstone]] and grey [[siltstone]] with beds of grey [[Lamination (geology)|laminated]] siltstone and silty [[mudstone]]."<ref>{{Cite web |title=Patrick Burn Formation |url=https://webapps.bgs.ac.uk/lexicon/lexicon.cfm?pub=PKB |access-date=2023-09-02 |website=BGS Lexicon of Named Rock Units |publisher=British Geological Survey}}</ref> The Birk Knowes site contains fossils from non-marine or marginal marine environment.<ref>{{Cite journal |last1=Tetlie |first1=O. Erik |last2=Braddy |first2=Simon J. |date=2003 |title=The first Silurian chasmataspid, Loganamaraspis dunlopi gen. et sp. nov. (Chelicerata: Chasmataspidida) from Lesmahagow, Scotland, and its implications for eurypterid phylogeny |url=https://www.cambridge.org/core/journals/earth-and-environmental-science-transactions-of-royal-society-of-edinburgh/article/abs/first-silurian-chasmataspid-loganamaraspis-dunlopi-gen-et-sp-nov-chelicerata-chasmataspidida-from-lesmahagow-scotland-and-its-implications-for-eurypterid-phylogeny/F2355DC34D69BB2A800023B67F4A4581 |journal=Earth and Environmental Science Transactions of the Royal Society of Edinburgh |language=en |volume=94 |issue=3 |pages=227–234 |doi=10.1017/S0263593300000638 |s2cid=73596575 |issn=1473-7116}}</ref> In 2000, Birk Knowes was closed by the Scottish government agency Scottish Natural Heritage (now [[NatureScot]]), due to the theft of specimens from the site by amateur collectors during the preceding decades, who essentially exhausted the fossiliferous deposit. At least some of the fossils ended up in a museum in Berlin, who refused to return them.<ref>{{Cite web |last=Williams |first=Huw |date=2003 |title=Filched Fish Fossils |url=https://www.bbc.co.uk/radio4/today/reports/archive/science_nature/fossils.shtml |access-date=2023-01-12 |website=BBC Radio 4 Today}}</ref><ref>{{Cite journal |last=Hose |first=Thomas A. |date=2012-04-01 |title=3G's for Modern Geotourism |url=https://doi.org/10.1007/s12371-011-0052-y |journal=Geoheritage |language=en |volume=4 |issue=1 |pages=7–24 |doi=10.1007/s12371-011-0052-y |bibcode=2012Geohe...4....7H |s2cid=144250723 |issn=1867-2485}}</ref><ref>{{Cite news |last=Langlands |first=Eva |date=2023-09-01 |title=Looters destroy Scotland's fossil heritage sites |newspaper=[[The Times]] |language=en |url=https://www.thetimes.co.uk/article/looters-destroy-scotlands-fossil-heritage-sites-69kgjzjwzlp |access-date=2023-09-01 |issn=0140-0460}}</ref><ref>University of Glasgow 23 May 2002 [https://www.dph.gla.ac.uk/news/archiveofnews/2002/may/headline_29743_en.html MOVE TO HALT FOSSIL THEFT AND DAMAGE IN SCOTLAND]</ref> |
||
== Paleobiota == |
== Paleobiota == |
||
| Line 98: | Line 98: | ||
==References== |
==References== |
||
* {{cite web|title= Fossilworks: Gateway to the Paleobiology Database|author= ((Various Contributors to the Paleobiology Database))|url= |
* {{cite web|title= Fossilworks: Gateway to the Paleobiology Database|author= ((Various Contributors to the Paleobiology Database))|url= https://www.fossilworks.org|access-date= 17 December 2021}} |
||
<references /> |
<references /> |
||
Latest revision as of 08:28, 18 November 2024
| Patrick Burn Formation | |
|---|---|
| Stratigraphic range: Upper | |
| Type | Formation |
| Unit of | Priesthill Group |
| Underlies | Castle Formation |
| Overlies | Ponesk Burn Formation (presumed, actual boundary is cut by a fault) |
| Thickness | 850 m |
| Lithology | |
| Primary | Sandstone, Siltstone, Mudstone |
| Location | |
| Region | Scotland |
| Country |  United Kingdom |
The Patrick Burn Formation is a Silurian aged geologic formation outcropping near Lesmahagow in Lanarkshire in the Scottish Lowlands. Fossils are known from the formation, including from the Birk Knowes locality.[1][2]
Description
[edit]According to the British Geological Survey, the primary lithology of the formation consists of "Alternating beds of grey feldspathic, medium-grained turbiditic sandstone and grey siltstone with beds of grey laminated siltstone and silty mudstone."[3] The Birk Knowes site contains fossils from non-marine or marginal marine environment.[4] In 2000, Birk Knowes was closed by the Scottish government agency Scottish Natural Heritage (now NatureScot), due to the theft of specimens from the site by amateur collectors during the preceding decades, who essentially exhausted the fossiliferous deposit. At least some of the fossils ended up in a museum in Berlin, who refused to return them.[5][6][7][8]
Paleobiota
[edit]Arthropods
[edit]| Arthropods | |||
|---|---|---|---|
| Species | Notes | Images | |
| Slimonia acuminata | A slimonid eurypterid. |  | |
| Erettopterus bilobus | A pterygotid eurypterid. |  | |
| ?Nanahughmilleria lanceolata | An adelophthalmid eurypterid. | ||
| ?Hardieopterus lanarkensis | A hardieopterid eurypterid. | ||
| Loganamaraspis dunlopi | A chasmataspidid. | ||
| Cyamocephalus loganensis | A synziphosurine. |  | |
| Pseudoniscus falcatus | A synziphosurine. | ||
| Ainiktozoon loganense | A thylacocephalan. |  | |
| Ceratiocaris papilio | A phyllocarid. |  | |
Chordates
[edit]| Chordates | |||
|---|---|---|---|
| Species | Notes | Images | |
| Loganellia scotica | A loganelliid thelodont. |  | |
| Jamoytius kerwoodi | An enigmatic chordate. |  | |
See also
[edit]
References
[edit]- Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database". Retrieved 17 December 2021.
- ^ D., Dineley; S., Metcalf (1999). Fossil Fishes of Great Britain. Geological Conservation Review Series. Vol. No. 16. Peterborough. ISBN 1-86107-470-0.
{{cite book}}:|volume=has extra text (help) - ^ Žigaitė, Živile; Goujet, Daniel (2012). "New observations on the squamation patterns of articulated specimens ofLoganellia scotica(Traquair, 1898) (Vertebrata: Thelodonti) from the Lower Silurian of Scotland". Geodiversitas. 34 (2): 253–270. doi:10.5252/g2012n2a1. ISSN 1280-9659. S2CID 73663549.
- ^ "Patrick Burn Formation". BGS Lexicon of Named Rock Units. British Geological Survey. Retrieved 2 September 2023.
- ^ Tetlie, O. Erik; Braddy, Simon J. (2003). "The first Silurian chasmataspid, Loganamaraspis dunlopi gen. et sp. nov. (Chelicerata: Chasmataspidida) from Lesmahagow, Scotland, and its implications for eurypterid phylogeny". Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 94 (3): 227–234. doi:10.1017/S0263593300000638. ISSN 1473-7116. S2CID 73596575.
- ^ Williams, Huw (2003). "Filched Fish Fossils". BBC Radio 4 Today. Retrieved 12 January 2023.
- ^ Hose, Thomas A. (1 April 2012). "3G's for Modern Geotourism". Geoheritage. 4 (1): 7–24. Bibcode:2012Geohe...4....7H. doi:10.1007/s12371-011-0052-y. ISSN 1867-2485. S2CID 144250723.
- ^ Langlands, Eva (1 September 2023). "Looters destroy Scotland's fossil heritage sites". The Times. ISSN 0140-0460. Retrieved 1 September 2023.
- ^ University of Glasgow 23 May 2002 MOVE TO HALT FOSSIL THEFT AND DAMAGE IN SCOTLAND
External links
[edit]
 | This article about a specific stratigraphic formation in the United Kingdom is a stub. You can help Wikipedia by expanding it. |
 | This article related to the Silurian period is a stub. You can help Wikipedia by expanding it. |
 | This Scotland-related article is a stub. You can help Wikipedia by expanding it. |