Dob's Linn: Difference between revisions
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{{Infobox valley |
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'''Dob's Linn''' is a small steep valley in [[Dumfries and Galloway]], just north of the A708 road between [[Moffat]] and [[Selkirk, Scottish Borders|Selkirk]], in [[Scotland]]. It is part of the [[Grey Mare's Tail, Moffat Hills|Grey Mare's Tail Nature Reserve]] which is owned by the [[National Trust for Scotland]].<ref>[https://www.nts.org.uk/visit/places/grey-mares-tail National Trust for Scotland: Grey Mare's Tail Nature Reserve]</ref> According to tradition, Dob's Linn is named for a [[covenanter]], Halbert Dobson, who took refuge there from Government troops during [[The Killing Time]] in the late 17th century.<ref>{{cite book | first = James | last = Hogg | title = The works of the Ettrick shepherd | editor-first = Thomas | editor-last = Thomson | date = 1869 | author-link = James Hogg | publisher = Blackie and Son | place = London | page = [https://archive.org/details/worksofettricksh02hogg/page/77 77] | url = https://archive.org/details/worksofettricksh02hogg}}</ref> |
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| ⚫ | Dob's Linn is important in geology as the location of the [[Global Boundary Stratotype Section and Point]] (GSSP)<ref>{{cite web|url=http://www.stratigraphy.org/ordsil.htm |title=GSSP for the Ordovician-Silurian Boundary |last=Ogg |first=James |accessdate=2006-07-01 |archiveurl=https://web.archive.org/web/20060618104006/http://www.stratigraphy.org/ordsil.htm |archivedate=2006-06-18 |url-status=dead }}</ref> which marks the boundary between the [[Ordovician]] and [[Silurian]] periods, and marks the base of the [[Llandovery epoch]], on the [[geologic time scale]]. Dob's Linn was ratified as the GSSP by the [[International Union of Geological Sciences]] in 1984.<ref>{{cite web|url=http://www.scottishgeology.com/outandabout/classic_sites/locations/dobs_linn.html |title=Dob's Linn |work=Scottish Geology |publisher=[[Hunterian Museum and Art Gallery|Hunterian Museum]] |accessdate=2006-07-01 |url-status=dead |archiveurl=https://archive.today/20110518035418/http://www.scottishgeology.com/outandabout/classic_sites/locations/dobs_linn.html |archivedate=2011-05-18 }}</ref> |
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| ⚫ | The boundary is defined as the [[First appearance datum|first appearance]] of [[graptolite]]s ''Parakidograptus acuminatus'' and ''Akidograptus ascensu'' 1.6 m above the base of the Birkhill Shale Formation. The [[shale]] section also contains [[chitinozoa]] and [[conodont]]s, but neither are well preserved. Dob's Linn has been criticized for the difficulty in relating its graptolite [[biostratigraphy|biostratigraphic]] sequence with shallow water sequences elsewhere, although the stratotype also appears to correspond with a [[carbon-13]] isotope excursion in the latest Ordovician which can be identified worldwide.<ref>{{cite journal | last = Underwood | first = C J |author2=S F Crowley|author3=J D Marshall|author4=P J Brenchley |date=July 1997 | title = High-resolution carbon isotope stratigraphy of the basal Silurian Stratotype (Dob's Linn, Scotland) and its global correlation | journal = Journal of the Geological Society | doi = 10.1144/gsjgs.154.4.0709 | volume = 154 | pages = 709 | issue = 4}}</ref> |
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| ⚫ | The boundary is defined as the [[First appearance datum|first appearance]] of [[graptolite]]s ''Parakidograptus acuminatus'' and ''Akidograptus ascensu'' 1.6 m above the base of the Birkhill Shale Formation. The [[shale]] section also contains [[chitinozoa]] and [[conodont]]s, but neither are well preserved. Dob's Linn has been criticized for the difficulty in relating its graptolite [[biostratigraphy|biostratigraphic]] sequence with shallow water sequences elsewhere, although the stratotype also appears to correspond with a [[carbon-13]] isotope excursion in the latest Ordovician which can be identified worldwide.<ref>{{cite journal | last = Underwood | first = C J |author2=S F Crowley|author3=J D Marshall|author4=P J Brenchley |date=July 1997 | title = High-resolution carbon isotope stratigraphy of the basal Silurian Stratotype (Dob's Linn, Scotland) and its global correlation | journal = Journal of the Geological Society | doi = 10.1144/gsjgs.154.4.0709 | volume = 154 | pages = 709 | issue = 4| citeseerx = 10.1.1.502.6989 }}</ref> |
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| ⚫ | The area was first studied by [[Charles Lapworth]] in the late 19th century. His work established fossil [[graptolite]]s as a method of understanding [[stratigraphy|stratigraphic]] sequences<ref>{{cite journal | first = Charles | last = Lapworth | title = The Moffat Series | journal = Quarterly Journal of the Geological Society | date = 1878 | volume = 34 | pages = |
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| ⚫ | The area was first studied by [[Charles Lapworth]] in the late 19th century. His work established fossil [[graptolite]]s as a method of understanding [[stratigraphy|stratigraphic]] sequences.<ref>{{cite journal | first = Charles | last = Lapworth | title = The Moffat Series | journal = Quarterly Journal of the Geological Society | date = 1878 | volume = 34 | issue = 1–4 | pages = 240–346 | url = https://archive.org/details/LapworthMoffatSeries1878QuJouGeolSocVol34Page240| doi = 10.1144/GSL.JGS.1878.034.01-04.23 }}</ref> A more recent description of the area, enumerating the zones established by Lapworth, is given in the British Regional Geology Monograph.<ref>{{cite book| first = J. | last = Pringle | title = British regional Geology: The South of Scotland | edition = 2 | place = London | publisher = Her Majesty's Stationery Office (HMSO) | date = 1948 | pages = [https://archive.org/details/SouthOfScotlandBritishRegionalGeologyImages/page/n45 34]–46 | url = https://archive.org/details/SouthOfScotlandBritishRegionalGeologyImages}}</ref> Before Lapworth's work, it was thought that the Silurian rocks of the Southern Uplands formed a single sequence, that would have to be about 6000m in thickness. By his identification of particular graptolite species in different zones of the Dob's Linn exposure, Lapworth was able to demonstrate that the Uplands consist of a much thinner layer, consistent with Silurian deposits elsewhere, that had been repeatedly folded and faulted, with multiple repetitions of the same strata, often upside down.<ref>{{cite book | last = Oldroyd | first = David R | title = The Highlands Controversy | publisher = The University of Chicago Press | date =1990 | location = Chicago | isbn = 978-0-226-62635-2 | pages = 217–265}}</ref> The understanding that sequences of sedimentary rocks could be inverted played an important part in the later resolution of the [[Highlands controversy of Northwest Scotland|Highlands Controversy]] in which Lapworth was also involved. |
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== References == |
== References == |
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{{reflist}} |
{{reflist}} |
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== External links == |
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* {{cite web | first1 = E.N.K. | last1 = Clarkson | first2 = C.M. | last2 = Taylor | title = Dob's Linn, Moffat - an excursion |accessdate = 28 Jan 2019 | url = http://earthwise.bgs.ac.uk/index.php/Dob%27s_Linn,_Moffat_-_an_excursion | work = from: Scottish Borders geology: an excursion guide | publisher = Scottish Academic Press | date = 1992}} |
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== Gallery == |
== Gallery == |
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| File:Climacograptus wilsoni Graptolite Fossils from Dob's Linn Scotland.jpg |
| File:Climacograptus wilsoni Graptolite Fossils from Dob's Linn Scotland.jpg |
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|''Climacograptus wilsoni'' graptolite fossils on black shale (26 x 25 millimetres) of middle Ordovician age (Soudleyan Stage, ~mid-Caradocian) from the main cliff at |
|''Climacograptus wilsoni'' graptolite fossils on black shale (26 x 25 millimetres) of middle Ordovician age (Soudleyan Stage, ~mid-Caradocian) from the main cliff at Dob's Linn (about 36.1-43.1 metres below the Ordovician-Silurian boundary GSSP |
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| File:Quarterlyjourna341878geol 0417 Lapworth Plate XII.jpg |
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| Lapworth's original map of the exposure at Dob's Linn |
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[[Category:Paleozoic Scotland]] |
[[Category:Paleozoic Scotland]] |
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[[Category:History of Dumfries and Galloway]] |
[[Category:History of Dumfries and Galloway]] |
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{{Scotland-hist-stub}} |
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Latest revision as of 10:25, 8 April 2022
| Dob's Linn | |
|---|---|
 Looking down Dob's Linn Gorge from the top | |
  Dob's Linn | |
| Floor elevation | 300 m (980 ft) |
| Geography | |
| Country | Scotland |
| District | Dumfries and Galloway |
| Coordinates | 55°25′47″N 3°16′11″W / 55.4297°N 3.2697°W |
Dob's Linn is a small steep valley in Dumfries and Galloway, just north of the A708 road between Moffat and Selkirk, in Scotland. It is part of the Grey Mare's Tail Nature Reserve which is owned by the National Trust for Scotland.[1] According to tradition, Dob's Linn is named for a covenanter, Halbert Dobson, who took refuge there from Government troops during The Killing Time in the late 17th century.[2]
Dob's Linn is important in geology as the location of the Global Boundary Stratotype Section and Point (GSSP)[3] which marks the boundary between the Ordovician and Silurian periods, and marks the base of the Llandovery epoch, on the geologic time scale. Dob's Linn was ratified as the GSSP by the International Union of Geological Sciences in 1984.[4]
The boundary is defined as the first appearance of graptolites Parakidograptus acuminatus and Akidograptus ascensu 1.6 m above the base of the Birkhill Shale Formation. The shale section also contains chitinozoa and conodonts, but neither are well preserved. Dob's Linn has been criticized for the difficulty in relating its graptolite biostratigraphic sequence with shallow water sequences elsewhere, although the stratotype also appears to correspond with a carbon-13 isotope excursion in the latest Ordovician which can be identified worldwide.[5]
The area was first studied by Charles Lapworth in the late 19th century. His work established fossil graptolites as a method of understanding stratigraphic sequences.[6] A more recent description of the area, enumerating the zones established by Lapworth, is given in the British Regional Geology Monograph.[7] Before Lapworth's work, it was thought that the Silurian rocks of the Southern Uplands formed a single sequence, that would have to be about 6000m in thickness. By his identification of particular graptolite species in different zones of the Dob's Linn exposure, Lapworth was able to demonstrate that the Uplands consist of a much thinner layer, consistent with Silurian deposits elsewhere, that had been repeatedly folded and faulted, with multiple repetitions of the same strata, often upside down.[8] The understanding that sequences of sedimentary rocks could be inverted played an important part in the later resolution of the Highlands Controversy in which Lapworth was also involved.
References[edit]
- ^ National Trust for Scotland: Grey Mare's Tail Nature Reserve
- ^ Hogg, James (1869). Thomson, Thomas (ed.). The works of the Ettrick shepherd. London: Blackie and Son. p. 77.
- ^ Ogg, James. "GSSP for the Ordovician-Silurian Boundary". Archived from the original on 18 June 2006. Retrieved 1 July 2006.
- ^ "Dob's Linn". Scottish Geology. Hunterian Museum. Archived from the original on 18 May 2011. Retrieved 1 July 2006.
- ^ Underwood, C J; S F Crowley; J D Marshall; P J Brenchley (July 1997). "High-resolution carbon isotope stratigraphy of the basal Silurian Stratotype (Dob's Linn, Scotland) and its global correlation". Journal of the Geological Society. 154 (4): 709. CiteSeerX 10.1.1.502.6989. doi:10.1144/gsjgs.154.4.0709.
- ^ Lapworth, Charles (1878). "The Moffat Series". Quarterly Journal of the Geological Society. 34 (1–4): 240–346. doi:10.1144/GSL.JGS.1878.034.01-04.23.
- ^ Pringle, J. (1948). British regional Geology: The South of Scotland (2 ed.). London: Her Majesty's Stationery Office (HMSO). pp. 34–46.
- ^ Oldroyd, David R (1990). The Highlands Controversy. Chicago: The University of Chicago Press. pp. 217–265. ISBN 978-0-226-62635-2.
External links[edit]
- Clarkson, E.N.K.; Taylor, C.M. (1992). "Dob's Linn, Moffat - an excursion". from: Scottish Borders geology: an excursion guide. Scottish Academic Press. Retrieved 28 January 2019.
Gallery[edit]
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Folds in the Rock Strata high up in the Dob's Linn Gorge -
Plan of the typical locality of Dobb's Linn (sic) (after Lapworth) -
Climacograptus wilsoni graptolite fossils on black shale (26 x 25 millimetres) of middle Ordovician age (Soudleyan Stage, ~mid-Caradocian) from the main cliff at Dob's Linn (about 36.1-43.1 metres below the Ordovician-Silurian boundary GSSP -
Lapworth's original map of the exposure at Dob's Linn
55°25′47″N 3°16′11″W / 55.42972°N 3.26972°W
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