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Neolagarograptus tenuis

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The lectotype of  <span class="search-highlight">Neolagarograptus</span> <span class="search-highlight">tenuis</span>  ( Portlock, 1843 ), BGS GSM 7800...
Published: 01 November 2011
Fig. 4 The lectotype of Neolagarograptus tenuis ( Portlock, 1843 ), BGS GSM 7800, from the Limehill stream section, Pomeroy, Ireland (left); and sketch of lectotype slab (right) with measurements of width and 2TRD of graptolites suggesting relative extension parallel to the lectotype
Journal Article
Published: 01 November 2011
Proceedings of the Yorkshire Geological Society (2011) 58 (4): 351–356.
...Fig. 4 The lectotype of Neolagarograptus tenuis ( Portlock, 1843 ), BGS GSM 7800, from the Limehill stream section, Pomeroy, Ireland (left); and sketch of lectotype slab (right) with measurements of width and 2TRD of graptolites suggesting relative extension parallel to the lectotype...
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Journal Article
Published: 01 April 2006
Scottish Journal of Geology (2006) 42 (1): 59–64.
... patterns of graptolite abundance and diversity. The most striking signature comprises several marked peaks in abundance of the distinctive taxon Neolagarograptus tenuis (Portlock) within this interval. Such ‘bloom events’, if recognized further afield, may provide very fine-scale stratigraphic resolution...
FIGURES
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( A–D ) Camera lucida drawings of the type specimens of  Monograptus rheido...
Published: 01 November 2011
originally attributed to rheidolensis on slab BGS GSM 95257 from Nant Fuches-wen, and probably referable to Neolagarograptus tenuis . All from the Jones collection, × 10; scale bar = 2 mm.
Image
Monograptid graptolites from the convolutus Biozone of the Qusaiba Member (...
Published: 01 October 2007
). (4g): 204.9 ft, NHM QQ 206(1). (4h–4k) Neolagarograptus tenuis material for comparison with Neolagarograptus rickardsi. (4h): BGS JZ666, slender near-proximal fragment from Cwmystwyth, central Wales, SN 7668 7295. (4i): BGS NID 2100 poorly preserved topotype proximal end, Limehill Stream Section
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Aeronian and Telychian (middle and upper Llandovery) graptolites from the A...
Published: 01 March 2003
) Pristiograptus artus (Bouček)?; 341–80; 961.06 m. (o) Torquigraptus arcuatus (Bouček); 341–81; 961.45 m. (p) Streptograptus tenuis Loydell; 341–82; 963.34 m. (q) Petalolithus sp.; 341–83; 969.23 m. (r) Neolagarograptus tenuis (Portlock); 341–84; 969.66 m. (s, t) Streptograptus johnsonae Loydell
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 2007
GeoArabia (2007) 12 (4): 15–36.
...). (4g): 204.9 ft, NHM QQ 206(1). (4h–4k) Neolagarograptus tenuis material for comparison with Neolagarograptus rickardsi. (4h): BGS JZ666, slender near-proximal fragment from Cwmystwyth, central Wales, SN 7668 7295. (4i): BGS NID 2100 poorly preserved topotype proximal end, Limehill Stream Section...
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Stratigraphy and graptolite biozones of the early Silurian levels referred ...
Published: 01 November 2011
Fig. 2 Stratigraphy and graptolite biozones of the early Silurian levels referred to in the text, showing the ranges of Huttagraptus acinaces (the senior synonym of M. rheidolensis ), Neolagarograptus rickardsi and N. tenuis ; after Zalasiewicz et al . 2007 , 2009 .
Journal Article
Published: 01 November 2011
Proceedings of the Yorkshire Geological Society (2011) 58 (4): 208–210.
... species Monograptus rheidolensis , which has been attributed to different, contrasting taxa, and show that it includes two different species, one being mis-localized and likely attributable to Neolagarograptus tenuis , a species that remains distinctive even though its type material is shown...
Journal Article
Published: 01 June 2012
Geological Magazine (2012) 149 (6): 1089–1106.
... in the Radotín tunnel section, whereas Neolagarograptus tenuis (Portlock) is common at Hýskov. Normalograptus scalaris (Hisinger), Pseudorthograptus insectiformis (Nicholson), Pristiograptus regularis (Törnquist), Campograptus lobiferus (McCoy), Torquigraptus...
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Journal Article
Published: 01 March 2003
Geological Magazine (2003) 140 (2): 205–229.
...) Pristiograptus artus (Bouček)?; 341–80; 961.06 m. (o) Torquigraptus arcuatus (Bouček); 341–81; 961.45 m. (p) Streptograptus tenuis Loydell; 341–82; 963.34 m. (q) Petalolithus sp.; 341–83; 969.23 m. (r) Neolagarograptus tenuis (Portlock); 341–84; 969.66 m. (s, t) Streptograptus johnsonae Loydell...
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Journal Article
Published: 01 June 2003
Scottish Journal of Geology (2003) 39 (1): 17–28.
... the sedgwickii or halli Biozone, the horizon at this locality could be either. The graptolites associated with T. linterni sp. nov. identify the sedgwickii and halli biozones of the uppermost Aeronian (see Fig. 2 ). Torquigraptus linterni has not been found together with Neolagarograptus...
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Journal Article
Published: 01 June 2003
Scottish Journal of Geology (2003) 39 (1): 71–85.
... Republic is also C. lobiferus. At Hyskov the accompanying fauna includes S. sedgwickii, Neolagarograptus tenuis (Portlock) and Torquigraptus magnificus (Pribyl & Munch; for which, see Williams et al. 2003 ), collectively indicating the lower part of the sedgwickii Biozone (see Štorch 2001...
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Journal Article
Published: 09 September 2009
Geological Magazine (2009) 146 (6): 785–850.
... fauna, and distinguished an upper and lower subdivision within the biozone. The base is defined by the appearance of Stimulograptus sedgwickii , which appears together with Neolagarograptus tenuis (Hutt, 1974 –1975). Suggestions of a slightly earlier origin for St. sedgwickii (Rickards, 1976...
Journal Article
Published: 29 October 2012
Geological Magazine (2013) 150 (2): 300–332.
... Jones ( 1925 ) and Cocks et al . ( 1984 ), is that sedgwickii Biozone assemblages first appear in the Ydw Member of the Wormwood Formation (see Section 3.a and Fig. 17 ). The FAD of Neolagarograptus tenuis [9g] and, in its upper part, the LAD of Raphidograptus...
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