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Dob's Linn

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Journal Article
Published: 01 November 2011
Proceedings of the Yorkshire Geological Society (2011) 58 (4): 311–317.
...Lucy A. Muir SUMMARY A specimen of Glyptograptus from the Silurian of Dob's Linn is described that possessed a bifurcating virgula, with a biserial stipe along each virgula. The colony lived for some considerable time with this morphology, showing that at least some graptoloids could survive...
FIGURES
Journal Article
Published: 01 April 2006
Scottish Journal of Geology (2006) 42 (1): 59–64.
...Claire L. Pannell; Euan N. K. Clarkson; Jan Zalasiewicz Synopsis A 1.89-m section excavated from the Stimulograptus sedgwickii Biozone (Silurian: Llandovery, Aeronian) at Dob’s Linn, Southern Uplands, Scotland, representing some 0.2 Ma of deposition, shows pronounced, quantitatively established...
FIGURES
Journal Article
Published: 01 April 2004
Scottish Journal of Geology (2007) 40 (1): 43–48.
...Richard A. Batchelor; Jane Evans Synopsis New Sr and Nd isotope and rare earth element data obtained from primary apatite microphenocysts indicate that the Dob’s Linn metabentonites originated from a mildly depleted mantle source, probably generated in a continental margin or back-arc basin...
FIGURES | View All (6)
Journal Article
Published: 01 August 1997
Journal of the Geological Society (1997) 154 (4): 709–718.
...C. J. UNDERWOOD; S. F. CROWLEY; J. D. MARSHALL; P. J. BRENCHLEY Abstract Since its designation as the Global Stratotype Section and Point (GSSP) for the base of the Silurian System, the choice of Dob's Linn, Southern Scotland, has received criticism due to the difficulties of relating its well...
Journal Article
Published: 01 March 1983
Journal of Paleontology (1983) 57 (2): 391–400.
...S. Henry Williams; Martin G. Lockley Abstract Hitherto undescribed inarticulate brachiopods associated with Lapworth's famous Late Ordovician graptolitic shale succession at Dob's Linn, Scotland, are shown to belong to a single highly distinctive species group best accommodated as the genotype...
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Aeronian-Telychian K-bentonite bed succession along <b>Linn</b> Branch, <b>Dob’s</b> <b>Linn</b>...
Published: 01 January 2016
Figure 14 Aeronian-Telychian K-bentonite bed succession along Linn Branch, Dob’s Linn, 16 km northeast of Moffat, southern Scotland. Dotted ornament marks greywackes. Note the very large number (49) of individual ash beds (after Bergström et al. 1998b ).
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Maps (A—Great Britain; B—section location) and photograph (C) of <b>Dob’s</b> <b>Linn</b>...
in > Geology
Published: 18 May 2020
Figure 2. Maps (A—Great Britain; B—section location) and photograph (C) of Dob’s Linn (Scotland, UK; 55°25′46.484″N, 3°16′17.605″W, North American Datum of 1983). View is to the southeast. Sample bags in C are 20 cm long.
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Geochemical data from <b>Dob’s</b> <b>Linn</b> (Scotland, UK). (A) Organic δ 13 C (δ 13 C...
in > Geology
Published: 18 May 2020
Figure 3. Geochemical data from Dob’s Linn (Scotland, UK). (A) Organic δ 13 C (δ 13 C org ). (B) Mo and Mo/Al. (C) U and U/Al. (D) Mn. (E) Hg. (F) Hg normalized to total organic carbon (TOC) and total Al. (G) Enrichment factors (EFs) of Zn, Ba, Ni, and P. “ashes” marks level at which numerous
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The stratigraphy of the Moffat Shale Group at <b>Dob’s</b> <b>Linn</b> showing the distri...
Published: 05 October 2014
Fig. 3. The stratigraphy of the Moffat Shale Group at Dob’s Linn showing the distribution and abundance of metabentonites (after Merriman & Roberts 1990 ; Tucker et al . 1990 ).
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Carbon isotope records and graptolite biozonation from <b>Dob&#x27;s</b> <b>Linn</b>, Scotland...
Published: 01 July 2011
Figure 3. Carbon isotope records and graptolite biozonation from Dob's Linn, Scotland (Silurian global stratotype section and point [GSSP]; Underwood et al., 1997 ), Wangjiawan Riverside (180 m from Hirnantian GSSP; Chen et al., 2006 ), and Laframboise Point, Anticosti Island (current study
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Location of sections, <b>Dob&#x27;s</b> <b>Linn</b> (adapted from  Toghill 1968 ).
Published: 01 April 2006
Fig. 1. Location of sections, Dob's Linn (adapted from Toghill 1968 ).
Journal Article
Published: 01 July 1987
Canadian Journal of Earth Sciences (1987) 24 (7): 1450–1464.
... the Ordovician Anceps bands C and D of the Ordovician–Silurian boundary stratotype at Dob's Linn, Scotland. The interval of Fauna 13 and the Gamachian Stage may correspond to Anceps Band E and the C .? extraordinarius Band (and contiguous strata) at Dob's Linn. The base of the G . ensifer Zone and the higher...
Journal Article
Journal: Geology
Published: 18 May 2020
Geology (2020) 48 (8): 777–781.
...Figure 2. Maps (A—Great Britain; B—section location) and photograph (C) of Dob’s Linn (Scotland, UK; 55°25′46.484″N, 3°16′17.605″W, North American Datum of 1983). View is to the southeast. Sample bags in C are 20 cm long. ...
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Journal Article
Journal: GSA Bulletin
Published: 01 January 2011
GSA Bulletin (2011) 123 (1-2): 186–205.
... at the Global Boundary Stratotype Section and Points (GSSPs) for the base of the Hirnantian and Silurian in south-central China and at Dob's Linn in Scotland. The known stratigraphic range of chitinozoans, a group of organic microfossils known for their high biostratigraphic resolution and minimal facies...
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Journal Article
Published: 01 June 2003
Scottish Journal of Geology (2003) 39 (1): 89–96.
... to cyphus in its common usage, i.e. in the interpretation of Elles & Wood, largely based upon Lapworth’s material from Dob’s Linn, Scotland. The monograptid praematurus, a mid-Rhuddanian taxon, was originally described as a variety, and evolutionary precursor, of Coronograptus cyphus. However...
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Journal Article
Published: 01 June 2003
Scottish Journal of Geology (2003) 39 (1): 17–28.
... in the Moffat Shale Group (Birkhill Shale Formation) at the western end of the Ettrick Valley and at Dob’s Linn, and is also known from a mudstone interbed in turbidite sandstones to the north of the Megget Dam. Its associates include Torquigraptus magnificus (Přibyl & Münch), recorded for the first time...
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Journal Article
Published: 01 November 2000
Geological Magazine (2000) 137 (6): 623–650.
... with that of other parts of the world such as Dob’s Linn in Scotland, Spain and Portugal, Thuringia–Saxonia–Bavaria, Bohemia, Poland, Kazakhstan, Kolyma, Malaya Peninsula, Yukon, Canadian Arctic Islands, Nevada, Argentina, Niger and Victoria, Australia. The Hirnantian Substage, which has been proposed by us recently...
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Journal Article
Published: 01 December 1997
Journal of the Geological Society (1997) 154 (6): 929–934.
...HOWARD A. ARMSTRONG; ANGELA L. COE Abstract Sedimentological analysis of the Ordovician-Silurian international boundary stratotype section at Dob's Linn, Scotland shows systematic changes in muddy turbidite microfacies which are interpreted in terms of a four phase glaciation. This comprised: (1...
Series: Geological Society, London, Geology of Series, Geological Society, London, Geology of Series
Published: 01 January 2008
DOI: 10.1144/CEV1P.2
EISBN: 9781862393929
... Belt. Previous structural units, within the Polish section of the EEC (after Ryka 1998 ). Massifs: Dob, Dobrzyn. Maz, Mazowsze, Pom, Pomorze. Metamorphic complexes: Cie, Ciechanow; Ks, Kaszuby, MC, Mazury Complex with rapakivi-like granitoids and anorthosite massifs (Suwa?ki & Ketrzyn); Pod...
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Typical graptolites at the Ordovician-Silurian boundary of northwestern Eur...
Published: 01 July 2009
, Eisteddfa, Wales - Gurig; 2: Specimen GB 48bis a 1 , Birkhill Shales, Dob’s Linn; 3: Specimen TCH 102 a 6 , Želkovice Formation, Belec; 4: Specimen SAR 2 e 26 , Genna Muxerru Formation, Monte Cortghiana Becciu; 5: Specimen GB 51 f 1 , Birkhill Shales, Dob’s Linn; 6: Specimen GB 51 h 2 , Birkhill Shales