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Cardinia

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Image
Macrofauna from the initial extinction phase. A) Slab (NHMW 2012/0158/0001) with numerous Cardinia hybrida, some with preserved periostracum, 6.5 cm above base of Tiefengraben Member at Kammerköhralm locality. B) Cardinia hybrida (NHMW 2012/0159/0001) 6.5 cm above base of Tiefengraben Member at Restentalgraben locality. C) Agerchlamys textoria (NHMW 2012/0160/0001) 18 cm above base of Tiefengraben Member at Eiberg locality. D) Slab (NHMW 2012/0158/0002) showing four individuals of Meleagrinella sp. 1 cm above base of Tiefengraben Member at Kammerköhralm locality. E) Pseudolima cf. hettangiensis (NHMW 2012/0158/0003) 7.0 cm above base of Tiefengraben Member at Kammerköhralm locality. NHMW  =  Naturhistorisches Museum, Vienna. Scale bar  =  1 cm.
Published: 01 September 2012
FIGURE 4— Macrofauna from the initial extinction phase. A) Slab (NHMW 2012/0158/0001) with numerous Cardinia hybrida, some with preserved periostracum, 6.5 cm above base of Tiefengraben Member at Kammerköhralm locality. B) Cardinia hybrida (NHMW 2012/0159/0001) 6.5 cm above base of Tiefengraben
Journal Article
Published: 17 June 2020
Proceedings of the Yorkshire Geological Society (2020) 63 (2): 77–87.
... are reasonably common along with a diverse benthos that includes abundant bivalves (e.g. Gryphaea, Cardinia, Luciniola, Plagiostoma and Oxytoma ) and rarer serpulids, gastropods, foraminifera and solitary corals. In the upper part of the section thicker-shelled taxa are commonly bored by cirripedes and bryozoans...
FIGURES
First thumbnail for: The Hettangian–Sinemurian (Lower Jurassic) strata ...
Second thumbnail for: The Hettangian–Sinemurian (Lower Jurassic) strata ...
Third thumbnail for: The Hettangian–Sinemurian (Lower Jurassic) strata ...
Journal Article
Published: 01 January 1977
Canadian Journal of Earth Sciences (1977) 14 (1): 89–101.
... .) johnstoni includes Prosogyrotrigonia (?) sp. cf. P . inouyei (Yehara), Cardinia sp. cf. C . hybrida (J. Sowerby), C . sp. aff. C . concinna (J. Sowerby), Pleuromya (?) sp., Meleagrinella (?) sp., Oxytoma ( Oxytoma ) sp., and Parallelodon (?) sp. The bivalves closely resemble approximately coeval forms...
Image
Figure 3. Molluscs from silicified fauna, showing fine preservation of shell features; scale bars represent 1 cm. Note beekitized patches on shell in A and C. A: Gryphaea arcuata, dorsal view. B: Pholadomya glabra, right valve. C: Cardinia listeri, left valve. D: Allocosmia
Published: 01 March 2003
Figure 3. Molluscs from silicified fauna, showing fine preservation of shell features; scale bars represent 1 cm. Note beekitized patches on shell in A and C. A: Gryphaea arcuata , dorsal view. B: Pholadomya glabra , right valve. C: Cardinia listeri , left valve. D: Allocosmia
Journal Article
Journal: PALAIOS
Published: 01 September 2012
PALAIOS (2012) 27 (9): 607–616.
...FIGURE 4— Macrofauna from the initial extinction phase. A) Slab (NHMW 2012/0158/0001) with numerous Cardinia hybrida, some with preserved periostracum, 6.5 cm above base of Tiefengraben Member at Kammerköhralm locality. B) Cardinia hybrida (NHMW 2012/0159/0001) 6.5 cm above base of Tiefengraben...
FIGURES
First thumbnail for: MACROFAUNAL RESPONSE TO THE END-TRIASSIC MASS EXTI...
Second thumbnail for: MACROFAUNAL RESPONSE TO THE END-TRIASSIC MASS EXTI...
Third thumbnail for: MACROFAUNAL RESPONSE TO THE END-TRIASSIC MASS EXTI...
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Published: 01 April 2016
Table 1.— Paleoecology of the Triassic–Jurassic interval in the Gabbs Valley Range, Mineral County, NV, USA. *Bivalve genera identified in the upper Ferguson Hill Formation from present work include cf. Trigonia, Weyla , cf. Plagiostoma , cf. Astarte, Pinna , Modiolus, cf. Cardinia , cf
Journal Article
Published: 01 September 2007
Russ. Geol. Geophys. (2007) 48 (9): 721–736.
...), Janaija praelonga (Kipar.), Cardinioides fidus Kur., and Falcimytilus nasai Kob. et Ichik.; 7 m — bivalves Cardinioides fidus Kur. and Meleagrinella polaris (Kittl) and gastropods Worthenia sp.; 12 m — ammonoids Arctophyllites taimyrensis (Popow), bivalves Cardinia sp. juv., brachiopods...
FIGURES
First thumbnail for: Detailed biostratigraphy of Triassic deposits in t...
Second thumbnail for: Detailed biostratigraphy of Triassic deposits in t...
Third thumbnail for: Detailed biostratigraphy of Triassic deposits in t...
Journal Article
Published: 01 October 1997
Russ. Geol. Geophys. (1997) 38 (10): 1691–1706.
... Zittelihalobia ex gr. talajaensis (Polub.), Cardinia sp. indet.; brachiopods Sinuplicorhynchia kegalensis Dagys, ? PennospiriJerina sp.; ostracodes; 2–6.5 m – coleoids “Atractites” sp.; anaptychi; bivalves Zittelihalobia ex gr. zhilnensis (Polub.), Meleagrinella ex gr. polaris (Kittl...
FIGURES
First thumbnail for: ZONATION OF THE TRlASSIC DEPOSITS OF THE OMULEVKA ...
Second thumbnail for: ZONATION OF THE TRlASSIC DEPOSITS OF THE OMULEVKA ...
Journal Article
Journal: PALAIOS
Published: 01 September 2009
PALAIOS (2009) 24 (9): 568–577.
... by representatives of the Family Cardiniidae, but a few specimens of Modiolus and Taeniodon , as well as unionoid bivalves, were also identified ( Pieńkowski, 2004 ). All the egg capsules, however, are preserved only on shell surfaces of Cardinia . Invertebrate eggs are not common in the fossil record due...
FIGURES
First thumbnail for: Gastropod egg capsules preserved on bivalve shells...
Second thumbnail for: Gastropod egg capsules preserved on bivalve shells...
Third thumbnail for: Gastropod egg capsules preserved on bivalve shells...
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Biogeographical range of mollusks and brachiopods in the Carnian. Boreal taxa: Striatosirenites, Neosireniles, Arctosireniles, ArctophyUites, Janopecten, Ochotochlamys, Dentospiriferina, Pennospiriferina, Aulacothyroides, Viligella. Tethyan taxa: Discotropites, Anatropiles, Gonionotites, Yuvaviles, Projuvavites, Costatoria, Maorilrigonia, Cassianella, Pteria. Cosmopolitan taxa: Sirenites, Proarcestes, Zittelihalobia, Oxytoma, Cardinia, Chlamys, Neoschizodus, Unioniles, Costispirijerina, Zeilleria. Symbols: circles indicate ammonites, triangles indicate bivalves, squares are based on brachiopods, asterisks indicate Koryak pure tethyan assemblage of ammonites. Dark bars indicate boreal taxa, light bars indicate tethyan taxa, combined colors indicate cosmopolitan taxa. Ammonite-based boundary between tethyan and boreal realms is indicated with a solid line, bivalve-based with a broken line. The biogeographical ecotone is hatched.
Published: 01 November 1996
, Anatropiles , Gonionotites , Yuvaviles , Projuvavites , Costatoria , Maorilrigonia , Cassianella , Pteria . Cosmopolitan taxa: Sirenites , Proarcestes , Zittelihalobia , Oxytoma , Cardinia , Chlamys , Neoschizodus , Unioniles , Costispirijerina , Zeilleria . Symbols: circles indicate
Image
Examples of fossils collected from Redcar; specimens housed in Whitby Museum. (A) Red 1, Schlothemia sp. (WHITM: 2020/1.1); (B) Red 21, Arnioceras sp. encrusted by Liostrea irregularis (Münster) (WHITM 2020/1.2); (C) Red 17, Pleurotomaria cognata (Chapuis and Dewalque) (WHITM: 2020/1.3); (D) Red 2 photomicrograph of microgastropod in thin section; (E) Red 12 Isocrinus psilonoti (Quenstedt), partially articulated specimen with cirri, photographed in situ; (F–I) Red 15, Cardinia listeri (J. Sowerby) featuring a range of cirripede borings (WHITM: 2020/1.4–8); (J) cross-section through part of C. listeri shell; (I) showing potential Simonizapfes; (K) detail of C. listeri shell (I) with possible bryozoan borings; (L) C. listeri with growth defect, dashed line projects normal shell outline. Examples A–C have been whitened using ammonium chloride, scale bars 1 cm unless otherwise stated.
Published: 17 June 2020
) (WHITM: 2020/1.3); ( D ) Red 2 photomicrograph of microgastropod in thin section; ( E ) Red 12 Isocrinus psilonoti (Quenstedt), partially articulated specimen with cirri, photographed in situ; ( F – I ) Red 15, Cardinia listeri (J. Sowerby) featuring a range of cirripede borings (WHITM: 2020/1.4–8
Journal Article
Published: 01 August 2013
Russ. Geol. Geophys. (2013) 54 (8): 792–807.
... Sobolev); bivalves Zittelihalobia zhilnensis (Polubotko), Cardinia borealis Kiparisova, C. sibirica Voronetz, Cardinioides fidus Kur., Janopecten subpolaris (Polubotko), Ochotochlamys aff. korkodonensis (Polubotko), Pleuromya forsbergi (Boehm); brachiopods Sakawairhynchia olenekensis...
FIGURES
First thumbnail for: Triassic stratigraphy of the Eastern Laptev Sea co...
Second thumbnail for: Triassic stratigraphy of the Eastern Laptev Sea co...
Third thumbnail for: Triassic stratigraphy of the Eastern Laptev Sea co...
Journal Article
Published: 01 May 1990
Journal of the Geological Society (1990) 147 (3): 421–424.
... Cardinia hybrida, Pseudoli- mea hettangiensis, Antiquilima succincta and Chlamys tex- toria first occur in the basal few centimetres of the Grenz- mergel (Golebiowski & Braunstein 1988). The Eiberg (Tirol) section reveals that here is an almost complete turnover in the low diversity coccolith flora within...
Journal Article
Published: 01 November 2008
Proceedings of the Yorkshire Geological Society (2008) 57 (2): 107–112.
.... Dis­articulated bivalves occur throughout the ironstone, including large numbers of mostly worn G. arcuata, together with small pectinids and Cardinia sp. In the summer of 2006 a further excavation was docu­mented approximately 200–300 m to the southeast, between SE 88421431 and 8822 1452 ( Figs 2 , 3...
FIGURES
First thumbnail for: Gryphaea beds (upper Scunthorpe Mudstone Formation...
Second thumbnail for: Gryphaea beds (upper Scunthorpe Mudstone Formation...
Third thumbnail for: Gryphaea beds (upper Scunthorpe Mudstone Formation...
Journal Article
Journal: Paleobiology
Published: 01 August 2022
Paleobiology (2022) 48 (3): 420–445.
.... 3 . As, Astarte sp.; Ca, Camptonectes sp.; CR, Cardinia regularis ; Cas, Cassianella sp.; CV, Chlamys valoniensis ; Da, Dacryomya sp. GO, Gervillella ornata ; GrO, Gryphaea obliquata .; GH, Grammatodon hettangiensis ; IC, Isocyprina concentricum ; IE, Isocyprina ewaldi ; LB, Liostrea...
FIGURES
First thumbnail for: Bivalve body-size distribution through the Late Tr...
Second thumbnail for: Bivalve body-size distribution through the Late Tr...
Third thumbnail for: Bivalve body-size distribution through the Late Tr...
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Published: 24 September 2018
, 1915 ) − X   Lucinidae indet. X X   Mesomiltha ? sp. − X   Cardinia andium (Giebel in Burmeister and Giebel, 1861 ) X −   Neocrassina aureliae (Feruglio, 1934 ) X X   Isocyprina ancatruzi (Leanza, 1942 ) X X   Pleuromya sp. X X   Ceratomya sp. X
Journal Article
Published: 01 April 1991
Journal of the Geological Society (1991) 148 (2): 420–422.
... a significant Triassic ancestry. Cardinia hybrida is regarded by Hodges as a junior synonym of C. listeri (Sowerby) and does not occur at a lower stratigraphical position than the Angulata Zone of the Hettangian; stratigraphically earlier records of this species probably belong to C. ovalis (Stutchbury) which...
Journal Article
Journal: Geology
Published: 01 March 2003
Geology (2003) 31 (3): 211–214.
...Figure 3. Molluscs from silicified fauna, showing fine preservation of shell features; scale bars represent 1 cm. Note beekitized patches on shell in A and C. A: Gryphaea arcuata , dorsal view. B: Pholadomya glabra , right valve. C: Cardinia listeri , left valve. D: Allocosmia ...
FIGURES
First thumbnail for: Missing molluscs: Field testing taphonomic loss in...
Second thumbnail for: Missing molluscs: Field testing taphonomic loss in...
Third thumbnail for: Missing molluscs: Field testing taphonomic loss in...
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Body size and survivorship in bivalves during the Late Triassic mass extinction event and Hettangian recovery. A, The coefficient of variation for each extinction category through time. Thicker lines represent the mean value of the coefficient of variation, while the thinner lines represent the 95% confidence intervals estimated by bootstrapping. B, The residual values of log2 body size for each extinction category (survivors, victims, and postextinction colonizers). Each point represents the residual value of a single species within each stratigraphic unit. Zero on the y-axis represents the grand mean size estimated from all species. Dashed line is the 95% confidence intervals, estimated by bootstrapping. Black arrows indicate a reduction in size during the extinction horizon (shaded gray). Key to stratigraphic units as in Fig. 3. As, Astarte sp.; Ca, Camptonectes sp.; CR, Cardinia regularis; Cas, Cassianella sp.; CV, Chlamys valoniensis; Da, Dacryomya sp. GO, Gervillella ornata; GrO, Gryphaea obliquata.; GH, Grammatodon hettangiensis; IC, Isocyprina concentricum; IE, Isocyprina ewaldi; LB, Liostrea bristovi; LH, Liostrea hisingeri; MCa, Mactromya cardioides; Me, Mesomiltha sp.; MH, Modiolus hillanus; MM, Modiolus minimus; MS, Modiolus sodburiensis; Msp, Modiolus sp.; MV, Modiolus ventricosus; MY, Myoconcha psilonoti; MC, Mytilus cloacinus; OF, Oxytoma fallax; PE, Palaeoneilo elliptica; PN, Palaeonucula navis; Pe, Permophorus elongatus; Ph, Pholadomya sp.; PA, Placunopsis alpina; PG, Plagiostoma giganteum; PP, Plagiostoma punctatum; Pl, Pleuromya sp.; PR, Protocardia rhaetica; PD, Pseudolimea duplicata; Pt, ?Pteromya sp.; PCr, Pteromya crowcombeia; PL, Pteromya langportensis; RC, Rhaetavicula contorta; RB, Rollieria bronni; RT, Ryderia texturata. C, Phylogenetic correlogram for body size in Triassic–Jurassic bivalve species from the study sites. Moran's I coefficients are calculated from the mean sizes of the 37 species recorded in this study. Although the figure shows the phylogenetic gradient that would be expected if closely related species were more similar in size than distantly related species, the Moran's I coefficients are not significant at any taxonomic level (p > 0.05; see Supplementary Table 4). D, Phylogenetic effect on body-size selectivity. The plot shows the relationship between the average size of each species and its ordinal body size. The dashed line represents a linear regression fit to the data set; extinction selectivity against large body size would be indicated if the victim species were grouped above the regression line, while selection against small size would be indicated if victims grouped below the regression line.
Published: 01 August 2022
, Cardinia regularis ; Cas, Cassianella sp.; CV, Chlamys valoniensis ; Da, Dacryomya sp. GO, Gervillella ornata ; GrO, Gryphaea obliquata .; GH, Grammatodon hettangiensis ; IC, Isocyprina concentricum ; IE, Isocyprina ewaldi ; LB, Liostrea bristovi ; LH, Liostrea hisingeri ; MCa, Mactromya
Image
Correlation of Tr–J boundary sections at Astartekløft and St Audrie’s Bay and a comparison of the stratigraphic ranges of macrofossil leaves and marine bivalves at these two localities. Correlation is based on sporomorph assemblage zones and the first appearance of the pollen morphospecies Cerebropollenites thiergartii (Kuerschner et al. 2007). Carbon isotope data and stratigraphic schemes at Astartekløft and St Audrie’s Bay are from Hesselbo et al. (2002). Position of ‘Precursor’ carbon isotope excursion is from Ruhl & Kürschner (2011). Sporomorph zones at St Audrie’s Bay are from Orbell (1973) and Bonis et al. (2010b). Abbreviations of stratigraphic units at St Audrie’s Bay: PPB, ‘Pre-planorbis beds’; Lil. Fm., Lilstock Formation; CM, Cotham Member; LM, Langport Member. Central Atlantic Magmatic Province volcanic rocks: L. U., Lower Unit; I. U., Intermediate Unit. Correlation line ‘A’ indicates the first appearance of C. thiergartii (first appearance of C. thiergartii at St Audrie’s Bay (18.50 m) from Bonis et al. (2010b)). Correlation line ‘B’ connects the top of Sporomorph Assemblage Zone A2 at Astartekløft to the top of the Rhaetipollis Zone at St Audrie’s Bay (Orbell 1973; SAB 1 & 2 of Bonis et al. 2010b). Macrofossil leaves at Astartekløft from McElwain et al. (2007) and Mander et al. (2010): 1, Hausmannia; 2, Baiera; 3, Lepidopteris; 4, Podozamites; 5, Dictyophyllum; 6, Equisetites; 7, Pterophyllum; 8, Anomozamites; 9, Czekanowskia; 10, Nilssonia; 11, Ginkgo; 12, Elatocladus; 13, Pseudoctenis; 14, Stachyotaxus; 15, Cladophlebis; 16, Clathropteris; 17, Rhinipteris; 18, Ptilozamites; 19, Doratophyllum; 20, Taeniopteris; 21, Sphenobaiera; 22, Anthrophyopsis; 23, Ctenis; 24, Macrotaeniopteris; 25, Marattia; 26, Pagiophyllum; 27, Phlebopteris; 28, Sagenopteris; 29, Thaumatopteris. Marine bivalves at St Audrie’s Bay from Mander et al. (2008): 1, Permophorus elongatus; 2, Pteromya crowcombia; 3, Tutcheria cloacina; 4, Rhaetavicula contorta; 5, Ryderia sp.; 6, Chlamys valoniensis; 7, Modiolus sp.; 8, Modiolus hillanus; 9, Modiolus sodburiensis; 10, Modiolus minimus; 11, Placunopsis alpina; 12, Gervillella ornata; 13, Dacryomya sp.; 14, Protocardia rhaetica; 15, Isocyprina sp.; 16, Isocyprina concentricum; 17, Isocyprina ewaldi; 18, Cassianella sp.; 19, Plagiostoma giganteum; 20, Plagiostoma punctuatum; 21, Cardinia regularis; 22, Lyriomyophoria postera; 23, Liostrea sp.; 24, Liostrea hisingeri; 25, Pleuromya sp.; 26, Oxytoma fallax; 27, Pseudomytiloides dubius; 28, Rollieria bronni; 29, Palaeonucula navis.
Published: 01 January 2013
, Isocyprina ewaldi ; 18, Cassianella sp.; 19, Plagiostoma giganteum ; 20, Plagiostoma punctuatum ; 21, Cardinia regularis ; 22, Lyriomyophoria postera ; 23, Liostrea sp.; 24, Liostrea hisingeri ; 25, Pleuromya sp.; 26, Oxytoma fallax ; 27, Pseudomytiloides dubius ; 28, Rollieria bronni ; 29