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Reduviasporonites

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Journal Article
Journal: Palynology
Published: 01 January 2002
Palynology (2002) 26 (1): 35–58.
...C.B. FOSTER; M.H. STEPHENSON; C. MARSHALL; G.A. LOGAN; P.F. GREENWOOD Abstract Geochemical analyses of specimens of Reduviasporonites suggests that it is most likely of algal, rather than fungal origin. As probable alga, Reduviasporonites is unlikely to be integral to the process of mass extinction...
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Journal Article
Journal: Palynology
Published: 01 October 1999
Palynology (1999) 23 (1): 37–41.
...William C. Elsik Abstract The fungal form-genus Reduviasporonites includes the range of morphology found in type and other material from Oklahoma and numerous well-preserved specimens from Italy and elsewhere. Chordecystia Foster 1979 and Tympanicysta Balme 1980 are both junior synonyms...
Journal Article
Journal: Palynology
Published: 01 October 1999
Palynology (1999) 23 (1): 43–53.
...Gordon D. Wood; William C. Elsik Abstract Specimens of the fungus Reduviasporonites stoschianus (Balme 1980) Elsik 1999 were recovered from the Copacabana Formation of Peru. Biostratigraphic data from smaller foraminifera, fusulinids and associated calcareous microfossils indicate that occurrences...
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A: Pyrolysis gas chromatography–mass spectrometry (GC-MS) total ion chromatogram (TIC) data for Reduviasporonites:A—dibenzofuran; B—methyldibenzofuran; asterisk—contaminant. Numbers are n-alkene/n-alkane carbon numbers. B: Summed ion chromatograms (m/z 55+57) from pyrolysis GC-MS data for Reduviasporonites.
Published: 01 October 2009
Figure 2. A: Pyrolysis gas chromatography–mass spectrometry (GC-MS) total ion chromatogram (TIC) data for Reduviasporonites :A—dibenzofuran; B—methyldibenzofuran; asterisk—contaminant. Numbers are n- alkene/ n- alkane carbon numbers. B: Summed ion chromatograms (m/z 55+57) from pyrolysis GC
Image
(a) spinose acritarch, Q55/4, MPA 62263; (b) Reduviasporonites chalastus, D48, MPA 62263; (c) Pretricolpipollenites bharadwaji, E51, MPA 62263. (d and e) Pretricolpipollenites bharadwaji, H60/4, 62263; (f and g) Pretricolpipollenites bharadwaji, P68, 62263; (h) Taeniaesporites spp. D48/2, MPA 62263; (i) Taeniaesporites spp., W58/1, 62263; (j) Taeniaesporites spp., W58/1, MPA 62263; (k) Laevigatosporites sp. Q48, MPA 62263.
Published: 01 July 2013
Plate 16: (a) spinose acritarch , Q55/4, MPA 62263; (b) Reduviasporonites chalastus , D48, MPA 62263; (c) Pretricolpipollenites bharadwaji , E51, MPA 62263. (d and e) Pretricolpipollenites bharadwaji , H60/4, 62263; (f and g) Pretricolpipollenites bharadwaji , P68, 62263; (h
Image
Filaments of Reduviasporonites stoschianus (Balme) Elsik, dominantly barrel-shaped Permian-Triassic palynomorphs that have been assigned both fungal and algal origin. Scale bar represents 40 μm.
Published: 01 October 2009
Figure 1. Filaments of Reduviasporonites stoschianus (Balme) Elsik, dominantly barrel-shaped Permian-Triassic palynomorphs that have been assigned both fungal and algal origin. Scale bar represents 40 μm.
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See Fig. 5 caption for explanation. (A)–(C)?Reduviasporonites sp. (all × 540; Glenrothes Borehole). (A) J35, MPA 50641, MPK13322; (B) H32/4, MPA 50641, MPK 13323; (C) M17/3, MPA 50641, MPK 13324. (D)–(I) ?Algal palynomorph sp. 3 (all Blairmulloch Farm Borehole). (D) (× 540) K44/3,83.75, MPK 13325; (E) (× 540) L28, 83.75, MPK 13326; (F) (× 540) H51/4,83.75, MPK 13327; (G) (× 840, detail of (F) H51/4, 83.75, MPK 13327; (H) (× 540) H50/4, 83.75, MPK 13329; (I) (× 540) J34/2, 83.75, MPK 13330.
Published: 01 November 2004
Fig. 8. See Fig. 5 caption for explanation. (A)–(C) ?Reduviasporonites sp. (all × 540; Glenrothes Borehole). (A) J35, MPA 50641, MPK13322; (B) H32/4, MPA 50641, MPK 13323; (C) M17/3, MPA 50641, MPK 13324. (D)–(I) ?Algal palynomorph sp. 3 (all Blairmulloch Farm Borehole). (D) (× 540
Journal Article
Journal: Geology
Published: 01 October 2009
Geology (2009) 37 (10): 875–878.
...Figure 2. A: Pyrolysis gas chromatography–mass spectrometry (GC-MS) total ion chromatogram (TIC) data for Reduviasporonites :A—dibenzofuran; B—methyldibenzofuran; asterisk—contaminant. Numbers are n- alkene/ n- alkane carbon numbers. B: Summed ion chromatograms (m/z 55+57) from pyrolysis GC...
FIGURES
Image
Phytoplankton from the latest Permian of South China. Each scale bar is 10 μm. All figure images were taken using the transmitted light microscope. 1–11, 18–23: Reduviasporonites chalastus; 12–17: Reduviasporonites catenulatus. The section/sample numbers for all specimens are as follows. 1–6, 11, 14, 23: Shangsi section/TS28-17; 12–13: Xiakou section/XK254-1; 16–17: Zhongzhai section/ZZ19-3; 7–10, 15, 18–22: Shangsi section/TS28-18.
Published: 01 December 2013
Plate 4 Phytoplankton from the latest Permian of South China. Each scale bar is 10 μ m. All figure images were taken using the transmitted light microscope. 1–11, 18–23: Reduviasporonites chalastus ; 12–17: Reduviasporonites catenulatus . The section/sample numbers for all specimens
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The name of each taxon is followed by the England Finder code and slide number. Slides are held at the Institut für Geologie und Paläontologie, Heisenbergstr. 2 48149, Münster University, Münster, Germany. 1, Pretricolpipollenites bharadwajii, E31, DR3; 2, Pretricolpipollenites bharadwajii, H60/4, 62263; 3, Pretricolpipollenites bharadwajii, E51, 62263; 4, Pretricolpipollenites bharadwajii, P68, 62263; 5, Reduviasporonites chalastus, O18, DG3; 6, Reduviasporonites chalastus, T33/2, DG3; 7, Protohaploxypinus uttingii, T30/2, UW2; 8, Protohaploxypinus uttingii, K9, UW2; 9, Protohaploxypinus uttingii, H6, UW2; 10, Protohaploxypinus uttingii, D20/2, UW1; 11, Protohaploxypinus uttingii, M16/2, UW1; 12, Thymospora-Torispora complex, C57/3, 62258, 13, Thymospora-Torispora complex, C57/3, 62258; 14, Thymospora-Torispora complex, C41/2, 62258 (distal view); 15, Thymospora-Torispora complex, C41/2, 62258 (proximal view); 16, Thymospora-Torispora complex, D62/3, 62258; 17, Thymospora-Torispora complex, D62/3, 62258.
Published: 14 October 2024
bharadwajii , H60/4, 62263; 3, Pretricolpipollenites bharadwajii , E51, 62263; 4, Pretricolpipollenites bharadwajii , P68, 62263; 5, Reduviasporonites chalastus , O18, DG3; 6, Reduviasporonites chalastus , T33/2, DG3; 7, Protohaploxypinus uttingii , T30/2, UW2; 8, Protohaploxypinus uttingii , K9, UW2; 9
Journal Article
Journal: Geology
Published: 01 September 2011
Geology (2011) 39 (9): 883–886.
...Henk Visscher; Mark A. Sephton; Cindy V. Looy Abstract Throughout the world, latest Permian records of organic-walled microfossils are characterized by the common presence of remains of filamentous organisms, usually referred to the palynomorph genus Reduviasporonites . Although generally regarded...
FIGURES
Journal Article
Journal: Palynology
Published: 01 March 2015
Palynology (2015) 39 (1): 1–18.
... the poorest assemblages of the studied Permian–Triassic interval. Reduviasporonites occurs only sporadically throughout the Amb succession. * Corresponding author. Email: [email protected] , [email protected] © 2015 American Association of Stratigraphic Palynologists 2015 Plate...
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Journal Article
Journal: Palynology
Published: 01 December 2013
Palynology (2013) 37 (2): 325–344.
...Plate 4 Phytoplankton from the latest Permian of South China. Each scale bar is 10 μ m. All figure images were taken using the transmitted light microscope. 1–11, 18–23: Reduviasporonites chalastus ; 12–17: Reduviasporonites catenulatus . The section/sample numbers for all specimens...
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Journal Article
Published: 01 July 2013
Journal of Micropalaeontology (2013) 32 (2): 183–195.
..., Striadiporites and Reduviasporonites , suggests the temporary existence of shallow, pond- or lake-like aquatic habitats, possibly related to tectonic activity. * (e-mail: [email protected] ) 5 2 2013 24 4 2013 © The Micropalaeontological Society 2013 Most of the investigated...
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Journal Article
Journal: Palynology
Published: 01 January 2008
Palynology (2008) 32 (1): 39–61.
... spores and three of microthyriaceous thyriothecia, comprising 45 species are recorded. The fungal assemblage is characterized by species of toruloid spores in chains, and cylindrical spores belonging to Dicellaesporites , Diporicellaesporites , Pluricellaesporites , Reduviasporonites...
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Journal Article
Published: 01 November 2004
Proceedings of the Yorkshire Geological Society (2004) 55 (2): 145–158.
...Fig. 8. See Fig. 5 caption for explanation. (A)–(C) ?Reduviasporonites sp. (all × 540; Glenrothes Borehole). (A) J35, MPA 50641, MPK13322; (B) H32/4, MPA 50641, MPK 13323; (C) M17/3, MPA 50641, MPK 13324. (D)–(I) ?Algal palynomorph sp. 3 (all Blairmulloch Farm Borehole). (D) (× 540...
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Image
Representative palynomorphs of OSPZ6. Magnifications as noted for each specimen. (1) Reduviasporonites chalastus, C38, DILM-1, 7827.9 (x820). (2) Reduviasporonites chalastus, D31/1, DILM-1, 7827.9 (x730). (3) Playfordiaspora cancellosa, K37, V-619, 2187 (x450). (4) Thymospora opaqua, M30/4, V-619, 2155.6 (x1,000). (5) Camptotriletes warchianus, N24, WATK-1, 13466.1 (x560). (6) Pyramidosporites cyathodes, L31/4, DILM-1, 7838.8 (x480). (7) Lueckisporites virkkiae, F46, V-619, 2187 (x1,150). (8) Protohaploxypinus microcorpus, H38/3, V-619, 2187 (x350). (9) Triplexisporites cf. playfordii, L41, 2154, V-619 (x770). (10) Protohaploxypinus uttingii, D34, HWTH-6, 6224.4 (x1,000). (11) Protohaploxypinus uttingii, N29/3, HWTH-6, 6224.4 (x1,000). (12) Peroaletes khuffensis, C27/3, V-619, 2194.8 (x850). (13) ?Florinites balmei, G56/1, HRDH-51, 12601.8 (x850). (14) Lueckisporites virkkiae, D22 V-619, 2194.8 (x1,000). (15) Pyramidosporites cyathodes, H34, V-619, 2173.5 (x480).
Published: 01 July 2003
Plate 6: Representative palynomorphs of OSPZ6. Magnifications as noted for each specimen. (1) Reduviasporonites chalastus, C38, DILM-1, 7827.9 (x820). (2) Reduviasporonites chalastus, D31/1, DILM-1, 7827.9 (x730). (3) Playfordiaspora cancellosa, K37, V-619, 2187 (x450). (4) Thymospora
Journal Article
Published: 01 November 2008
Proceedings of the Yorkshire Geological Society (2008) 57 (2): 123–130.
... the ‘Magnesian Limestone’ or higher beds. Foster et al. (2002 ) included material from the Hilton Plant Beds in their study of Reduviasporonites chalastus, which they concluded is algal rather than fungal in origin (see section 2.2.2). Palynology preparations from 31 levels in the Hilton Borehole...
FIGURES
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 2006
GeoArabia (2006) 11 (3): 173–178.
.... A. However ?Florinites balmei , is common at two levels and Indotriradites sp. E and Reduviasporonites sp. B also occur indicating a close correlation with the “Khuff transition section” in Barik-36. Barik-36 is an extensively cored section through the middle and upper Gharif members...
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Journal Article
Journal: Palynology
Published: 16 January 2023
Palynology (2023) 47 (1): 2097329.
... inwardly is a diagnostic feature of Portalites Hemmer & Nygreen. Reduviasporonites chalastus (Foster) Elsik 1999 Plate 3 , figures 8–12 Remarks. An abundance of Reduviasporonites ( =Tympanicystia = Chordecystia ), an environment-dependent taxon, cannot be used...
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