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Lingularia

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Journal Article
Journal: Paleobiology
Published: 28 April 2016
Paleobiology (2016) 42 (3): 380–393.
.... During the Early Triassic recovery interval, disaster taxa proliferated and numerically dominated many marine benthic invertebrate assemblages. These disaster taxa include the bivalve genera Claraia , Unionites , Eumorphotis , and Promyalina , and the inarticulate brachiopod Lingularia . The exact nature...
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Published: 01 December 2010
Table 1. Taphonomic census results for Lingularia selwyni and lingulide-constructed trace fossils.
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Brachiopods from the Shuizhutang Formation. (1) Lingularia sp., a ventral valve, LN191001. (2–9, 26, 27) Fusichonetes soochowensis (Chao, 1928): (2–6, 9) external molds of dorsal valves: (2) LN221803, (3) LN223301, (4) LN223402, (5) LN223601, (6) LN216601, (9) LN221701; (7, 8, 26, 27) internal molds of ventral valves: (7) LN001801, (8) LN221301, (26) LN001401, (27) LN001701. (10–14) F. quadrata (Zhan in Hou et al., 1979): (10–12, 14) external molds of dorsal valves: (10) LN188903, (11) LN222301, (12) LN222703, (14) LN223703; (13) an internal mold of a ventral valve, LN222802. (15–17) F. flatus (Shen and Archbold, 2002), external molds of dorsal valves: (15) LN002603, (16) LN221102, (17) LN222003. (18–21) Neochonetes (Huangichonetes) substrophomenoides: (18–20) internal molds of ventral valves: (18) LN001201, (19) LN002403, (20) LN216503; (21) dorsal interior, LN220503. (22–25) N. (Sommeriella) strophomenoides Waagen, 1884: (22–24) internal molds of ventral valves: (22) LN003403, (23) LN218003, (24) LN219901; (25) an internal mold of a dorsal valve, LN220303. Scale bars = 3 mm.
Published: 01 January 2023
Figure 6. Brachiopods from the Shuizhutang Formation. ( 1 ) Lingularia sp., a ventral valve, LN191001. ( 2–9, 26, 27 ) Fusichonetes soochowensis (Chao, 1928 ): ( 2–6, 9 ) external molds of dorsal valves: ( 2 ) LN221803, ( 3 ) LN223301, ( 4 ) LN223402, ( 5 ) LN223601, ( 6 ) LN216601, ( 9
Journal Article
Published: 12 August 2021
Proceedings of the Yorkshire Geological Society (2021) 63 (4): pygs2020-015.
...) in a borehole in Oxfordshire in 1975. Burrows ( Lingulichnus ) attributed to this organism were reported from the Tarporley Siltstone in Cheshire in 1981. These records are evidence of marine influence in the depositional environments of those formations. Fig. 4. cf. Lingularia sp., Stonish Hill...
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cf. Lingularia sp., Stonish Hill, Eakring. (OUMNH G.151; ex. Reading 6992). Rose and Kent (1955, text-fig. 1; drawn by Miss E.R. Turlington), reproduced by courtesy of Cambridge University Press.
Published: 12 August 2021
Fig. 3. cf. Lingularia sp., Stonish Hill, Eakring. (OUMNH G.151; ex. Reading 6992). Rose and Kent (1955 , text-fig. 1; drawn by Miss E.R. Turlington), reproduced by courtesy of Cambridge University Press.
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cf. Lingularia sp., Stonish Hill, Eakring. OUMNH G.153 (bedding surface, counterpart of G.154; valve surface convex). © Oxford University Museum of Natural History. Image P995402, photographer Simon Harris (BGS/UKRI).
Published: 12 August 2021
Fig. 4. cf. Lingularia sp., Stonish Hill, Eakring. OUMNH G.153 (bedding surface, counterpart of G.154; valve surface convex). © Oxford University Museum of Natural History. Image P995402, photographer Simon Harris (BGS/UKRI).
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cf. Lingularia sp., Stonish Hill, Eakring. OUMNH G.154 (bedding surface, counterpart of G.153; valve surface concave). © Oxford University Museum of Natural History. Image P995403, photographer Simon Harris (BGS/UKRI).
Published: 12 August 2021
Fig. 5. cf. Lingularia sp., Stonish Hill, Eakring. OUMNH G.154 (bedding surface, counterpart of G.153; valve surface concave). © Oxford University Museum of Natural History. Image P995403, photographer Simon Harris (BGS/UKRI).
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Group of cf. Lingularia sp. (on a bedding surface). Stonish Hill, Eakring. OUMNH G.155. © Oxford University Museum of Natural History. Image P995404, photographer Simon Harris (BGS/UKRI).
Published: 12 August 2021
Fig. 6. Group of cf. Lingularia sp. (on a bedding surface). Stonish Hill, Eakring. OUMNH G.155. © Oxford University Museum of Natural History. Image P995404, photographer Simon Harris (BGS/UKRI).
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Group of cf. Lingularia sp. (on a bedding surface). Stonish Hill, Eakring. OUMNH G.156. © Oxford University Museum of Natural History. Image P995405, photographer Simon Harris (BGS/UKRI).
Published: 12 August 2021
Fig. 7. Group of cf. Lingularia sp. (on a bedding surface). Stonish Hill, Eakring. OUMNH G.156. © Oxford University Museum of Natural History. Image P995405, photographer Simon Harris (BGS/UKRI).
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cf. Lingularia sp. (on a bedding surface). Stonish Hill, Eakring. UKBGS RM 3970. Image P995406, photographer Simon Harris (BGS/UKRI). British Geological Survey ©UKRI. All rights Reserved.
Published: 12 August 2021
Fig. 8. cf. Lingularia sp. (on a bedding surface). Stonish Hill, Eakring. UKBGS RM 3970. Image P995406, photographer Simon Harris (BGS/UKRI). British Geological Survey ©UKRI. All rights Reserved.
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cf. Lingularia sp. (side view of the sample, upper surface at the top). Stonish Hill, Eakring. CAMSM G.422. © Sedgwick Museum, University of Cambridge. Image P 995400, photographer Simon Harris (BGS/UKRI).
Published: 12 August 2021
Fig. 9. cf. Lingularia sp. (side view of the sample, upper surface at the top). Stonish Hill, Eakring. CAMSM G.422. © Sedgwick Museum, University of Cambridge. Image P 995400, photographer Simon Harris (BGS/UKRI).
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Figure 1
Published: 28 April 2016
Figure 1 Images of the five genera of Early Triassic disaster genera as summarized by Benton ( 2003 ). (A) Unionites cf. canalensis , (B) Promyalina cf. putiatinensis , (C) Lingularia borealis , (D) Eumorphotis cf. virginensis , and (E) Claraia aurita . Scale
Journal Article
Journal: PALAIOS
Published: 01 December 2010
PALAIOS (2010) 25 (12): 807–817.
...Table 1. Taphonomic census results for Lingularia selwyni and lingulide-constructed trace fossils. ...
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Journal Article
Journal: PALAIOS
Published: 01 January 2007
PALAIOS (2007) 22 (1): 74–97.
...-Triassic extinction event is summarized. Western Canada is an ideal location to assess lingulide distribution patterns as upper Paleozoic and lower Mesozoic strata are extensively exposed, and lingulides (cf. Lingularia Biernat and Emig) and the trace fossil Lingulichnus Hakes are both common...
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Relative Shapley additive explanations (SHAP) value attributes showing how the different ecological variables for five example genera—A, Ishigaum, B, Coelocladiella, C, Lingularia, D, Costatumulus, and E, Crurithyris—change in the model prediction for the extinction interval. The x-axis is the model output value. The base value is the prediction if no ecological variables are considered, that is, the average predicted probability. Model output value is the prediction considering the ecological variables for the investigated genus, with positive values indicating extinction and negative values indicating survival. Features that push the prediction higher (to the right), that is, more likely to go extinct, are shown in burgundy, and the opposite is shown in blue. The categorical values for the functional traits are given in Table 1 for each feature.
Published: 01 August 2022
Figure 6. Relative Shapley additive explanations (SHAP) value attributes showing how the different ecological variables for five example genera—A, Ishigaum , B, Coelocladiella , C, Lingularia , D, Costatumulus , and E, Crurithyris —change in the model prediction for the extinction interval
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Fossil invertebrates from polished slabs of the Servino Formation. A) Coelostylina werfensis, Acquaseria Member, CD-12. B) Polygrina sp., Ca'San Marco Member, MR-01. C, D) Gastropod sp. A, Gastropod Oolite Member, CD-07. E) cf. Allocosmia sp., Myophoria Beds Member, CD-25. F) Natiria costata, Myophoria Beds Member, CD-43. G) Microconchus sp., Gastropod Oolite Member, CD-08. H) Holocrinus, Myophoria Beds Member, CD-42. I) Ophiuroidea, Acquaseria Member, CD-16. J) Neoschizodus spp., Myophoria Beds Member, CD-39. K) Bivalve sp. A, Gastropod Oolite Member, CD-10. L) Austrotindaria spp., Myophoria Beds Member, CD-43. M) cf. Bakevellia spp., Ca'San Marco Member, CD-01. N) Costatoria costata, Myophoria Beds Member, CD-39. O) cf. Eumorphotis spp., Gastropod Oolite Member, CD-11. P) cf. Scythentolium sp., Myophoria Beds Member, MR-03. Q) Lingularia spp., Gastropod Oolite Member, CD-05.
Published: 12 June 2018
Beds Member, MR-03. Q ) Lingularia spp., Gastropod Oolite Member, CD-05.
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Figure 4. Outcrop and trace fossil photographs, Brown Hill. A) Brown Hill, 467–473 m. Lingulides (Lingularia selwyni) and the trace fossil Lingulichnus are common from 467.4 to 470 m. B) Close-up of silty shale with very fine-grained sandstone interbeds. Beds BNHL467.5 and BNHL 467.9 are labeled. Hammer 33 cm long. C) Bedding plane with L. verticalis and an in situ lingulide, from Bed BNHL467.5. All three L. verticalis exhibit the classic eye-shaped cross-sectional outline of Lingulichnus. The dark dots in the centre of each trace fossil are interpreted as pedicle traces. The in situ lingulide (black line at upper right) shows a disturbed sand halo around it indicating that the specimen is preserved within its burrow. D) Three in situ lingulides on a bedding plane. Like the specimen in view C, these specimens are surrounded by disturbed sediment haloes indicating that they are preserved within their burrows. E) Bedding plane showing the bi-symmetrical outline that is characteristic of Lingulichnus. This specimen is the top of a J-shaped Lingulichnus hamatus through the portion where the burrow had become vertical. F) Bedding plane of three specimens of Lingulichnus verticalis and the type specimen of L. hamatus (GSC-C-431346).
Published: 01 December 2010
Figure 4. Outcrop and trace fossil photographs, Brown Hill. A) Brown Hill, 467–473 m. Lingulides ( Lingularia selwyni ) and the trace fossil Lingulichnus are common from 467.4 to 470 m. B) Close-up of silty shale with very fine-grained sandstone interbeds. Beds BNHL467.5 and BNHL 467.9
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Photographs of the type core of the Calais Sandstone Member, Anten Coquina Member and Pocketknife Member of the Montney Formation. A. Basal contact of the Calais Member, 5741.8’, well 102/07-20-70-24W5M. B. Cross-stratified sandstone in the Calais Member, 5735’, well 102/07-20-70-24W5M. C. Basal contact of the Anten Coquina Member, 1847.5 m, well 102/10-36-67-24W5M. Note the sharp contact of bioclastic grainstone (biocl.) incising into laminated siltstone (silt). D. Cross-stratified bioclastic grainstone, Anten Coquina Member, 1842 m, well 102/10-36-67-24W5M. E. Lingulide brachiopod (Lingularia cf. L. selwyni), 2450 m, well 01-16-76-13W6M F. Ammonoid from the Lower Montney Member. a-005-C/94-G-10, 1871.6 m. G. Ammonoid cf. Ophiceras sp., from the Lower Montney Member, a-005-C/94-G-10, 1867.8 m. H. Pectinid bivalves (cf. Claraia sp.) from the Pocketknife Member, well b-050-H, and pectinids from the Lower Montney Member, 94-B-16, 2075 m. I. Claraia sp. from the Pocketknife Member, a-018-D/94-A-13, 2175.67 m. Photographs F–I from Sanders (2016).
Published: 01 March 2018
brachiopod ( Lingularia cf. L. selwyni ), 2450 m, well 01-16-76-13W6M F. Ammonoid from the Lower Montney Member. a-005-C/94-G-10, 1871.6 m. G. Ammonoid cf. Ophiceras sp., from the Lower Montney Member, a-005-C/94-G-10, 1867.8 m. H. Pectinid bivalves (cf. Claraia sp.) from the Pocketknife Member, well b
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Published: 01 January 2023
Table 1. List of species with only illustrations in the text. Species name  Illustration  Species name  Illustration  Lingularia sp. Fig. 6.1 Alatorthotetina derbyiformis Fig. 14.13 , 14.14 Fusichonetes quadrata Fig. 6.10 – 6.14 Orthothetina frechi Fig
Journal Article
Published: 01 September 2009
Journal of the Geological Society (2009) 166 (5): 859–872.
... ) auritus (Schlotheim); 29, Oxytoma inequivalve (J. Sowerby); 30, Bositra buchi (Roemer); 31, Liostrea hisingeri (Nilsson); 32, Dacryomya ovum (Sowerby). Brachiopods: 33, Lingularia longovicensis (Terquem); 34, Lobothyris punctata (J. Sowerby); 35, Tetrarhynchia tetrahedra (Sowerby...
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