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Subtifloria

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Micrographs of Girvanella–Proaulopora, Girvanella–Subtifloria Proaulopora–Bija association from open platform and bank. Abbreviations as in Figure 5 and: Subt. = Subtifloria; brac. = brachiopod. A–C) Girvanella–Proaulopora association: packstone, containing Girvanella masses, echinoderms, and brachiopods, LG36-9-132-9, O1-2y (A); containing Proaulopora, LG36-10-128-3, O1-2y (B); and grainstone with Proaulopora, ZG16-1-94-21, O1-2y (C). D–I) Girvanella–Subtifloria association: bioclastic packstone and grainstone, Girvanella, Subtifloria and echinoderms intergrowing, YM1-Y-25, O2y (D); bioclastic packstone and grainstone with Girvanella, echinoderms, TK1-10-24-24, O2y (E); bioclastic packstone and grainstone with Subtifloria and echinoderms, TK1-12-16-15, O2y (F); bioclastic packstone and grainstone with Girvanella, Subtifloria, and Proaulopora, GC4-2-52-4, O2y (G); bioclastic packstone and grainstone with Subtifloria, HA902-3-71-5, O2y (H); and bioclastic packstone with Girvanella, Subtifloria and echinoderms, YM2-43, O2y (I). J–O) Proaulopora–Bija association: bioclastic grainstone containing Bija, TZ24-16-35-11, O3l (J); packstone containing Bija, LN621-2-52-22 (K); bioclastic grainstone and packstone with Proaulopora, JF127-14-58-9, O3l (L); bioclastic grainstone and packstone containing Proaulopora, from 5853.37 m of LN63, O3l (M); bioclastic grainstone and packstone containing Bija, LN621-2-52-22, O3l (N); packstone containing Bija, JF127-13-20-12, O3l (O).
Published: 01 July 2017
Fig . 14. Micrographs of Girvanella – Proaulopora , Girvanella – Subtifloria Proaulopora – Bija association from open platform and bank. Abbreviations as in Figure 5 and: Subt. = Subtifloria ; brac. = brachiopod. A – C ) Girvanella – Proaulopora association: packstone, containing
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Figure12—Subtifloria sp. size measurements.
Published: 01 July 2010
Figure 12 — Subtifloria sp. size measurements.
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Figure9—Calcified Cyanobacteria. All scale bars  =  100 µm. 1, Bevocastria (thin-section D2jp-12-1), Givetian, Dushan section; 2, Girvanella (thin-section D3l24), Frasnian, Dushan section; 3, Girvanella (thin-section D3w114-3), Famennian, Dushan section; 4, Girvanella (thin-section D2m-44-3), Givetian, Liujing section; 5, Girvanella (thin-section D3w40a), Famennian, Yangdi section; 6, Hedstroemia (thin-section D3gl-1-a), Frasnian, Shenwan section; 7, Subtifloria (thin-section D3w39-5), Frasnian, Yangdi section; 8, Subtifloria (thin-section D3lj5), Frasnian, Yangdi section.
Published: 01 July 2010
-section D 2 m-44-3), Givetian, Liujing section; 5 , Girvanella (thin-section D 3 w40a), Famennian, Yangdi section; 6 , Hedstroemia (thin-section D 3 gl-1-a), Frasnian, Shenwan section; 7 , Subtifloria (thin-section D 3 w39-5), Frasnian, Yangdi section; 8 , Subtifloria (thin-section D 3 lj5
Journal Article
Published: 01 January 2021
Journal of Paleontology (2021) 95 (1): 1–23.
... ordosia n. sp. Girvanella , Subtifloria , Acuasiphonoria , Xianella , and Oscillatoriaceae gen. indet. are assigned to Osillatoriales of cyanobacteria; Ortonella , Hedstroemia , Cayeuxia , Zonotrichites , Proaulopora , and Phacelophyton are assigned to Nostocales of cyanobacteria; and Garwoodia , Renalcis...
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First thumbnail for: Diversity and systematics of Middle-Late Ordovicia...
Second thumbnail for: Diversity and systematics of Middle-Late Ordovicia...
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Journal Article
Journal: PALAIOS
Published: 01 July 2017
PALAIOS (2017) 32 (7): 462–489.
...Fig . 14. Micrographs of Girvanella – Proaulopora , Girvanella – Subtifloria Proaulopora – Bija association from open platform and bank. Abbreviations as in Figure 5 and: Subt. = Subtifloria ; brac. = brachiopod. A – C ) Girvanella – Proaulopora association: packstone, containing...
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First thumbnail for: PALEOENVIRONMENTAL DISTRIBUTION OF ORDOVICIAN CALC...
Second thumbnail for: PALEOENVIRONMENTAL DISTRIBUTION OF ORDOVICIAN CALC...
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Journal Article
Published: 01 July 2010
Journal of Paleontology (2010) 84 (4): 569–587.
...Figure 12 — Subtifloria sp. size measurements. ...
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First thumbnail for: MID-LATE DEVONIAN CALCIFIED MARINE ALGAE AND CYANO...
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Journal Article
Published: 01 April 2004
Russ. Geol. Geophys. (2004) 45 (4): 485–491.
... Altai). There are two successive algal complexes: lower — with Korilophyton , Gemma , Razumovskia , Girvanella , Proaulopora , and Renalcis ; upper — the same, supplemented with abundant species of the genus Epiphyton and with the genera Batinevia , Tubophyllum , and Subtifloria . These complexes...
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First thumbnail for: CALCAREOUS ALGAE AND LOWER BOUNDARY OF CAMBRIAN IN...
Journal Article
Published: 01 May 1984
Geological Magazine (1984) 121 (3): 205–210.
..., in the Aldanocyathus sunnaginicus Zone of the earliest Tommotian, Angulocellularia, Bajanophyton, Batenevia, Botomaella, Girvanella, Hedstroemia, Korilophyton, Proaulopora, Subtifloria, and Tarthinia appear. Immediately above this, in the Dokidocyathus regularis Zone of the middle Tommotian, Chabakovia appears...
Journal Article
Published: 01 April 2002
Russ. Geol. Geophys. (2002) 43 (4): 334–342.
...-covered intervals and containing only scarce remains of the calcimicrobes Tubophyllum victori and Subtifloria delicata . Section 3, to the contrary, is rich in faunal remains and is better exposed ( Figs. 2 and 3 ). Fig. 2. Schematic geological profile of Section 3. 1 — calcibionts; 2...
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First thumbnail for: BIOSTRATIGRAPHY OF THE UPPER VENDIAN, LOWER AND MI...
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Figs. 1, 2, 4, 6 — Renalcis sp.; Fine carbonate-mineralized sheath covers rounded colonies. In case of sheath damage there are dark cavities once occupied by cells and later in filled with secondary calcite. 1 — ×66; 2 — ×220; 4 — ×40; 6 — ×86; sample 8363, Kiya R., right bank, Usa Formation, Atdabanian Stage, Lower CambrialL Figs. 3, 5 — Girvanella sp., interlaced carbonate-mineralized tubes (filaments), their cross section show hollows infilled with dark calcite in places where formerly there were trichomes of algae, 3 — ×66; 5 — ×200; sample IS 452/958, Igarka region, right bank or the Yenisei R., near town of Igarka, Sukharikha Formation, Tommotian Stage, Lower CambriaI Figs. 7–9 — Subtifloria sp., carbonate-mineralized filaments after dissolutiolL 7. 8 — ×66, 9 — ×32, sample 2155, East Sayan, Sarkhoi R., Khuzhirtai Formation, Atdabanian Stage, Lower CambrialL Fig. 10 — Subtifloria sp.; carbonate-mineralized filaments after solution; x200. Sample 4335, Gorny A1tai, Uimen’ River basin, Ust’-Seman Formation, Toyonian Stage, Lower Cambrian. Figs. 11–14 — Proautopora sp.; carbonate-mineralized filaments after solution; the sheaths of some filaments show joints or collars; 11 — ×100; 12, 14 — ×180; 13 — ×130; sample 4335, Gorny A1tal, River Ulmen’ basin, Ust’-Seman Formation, Toyonian Stage, Lower Cambrian.
Published: 01 May 1998
or the Yenisei R., near town of Igarka, Sukharikha Formation, Tommotian Stage, Lower CambriaI Figs. 7–9 — Subtifloria sp., carbonate-mineralized filaments after dissolutiolL 7. 8 — ×66, 9 — ×32, sample 2155, East Sayan, Sarkhoi R., Khuzhirtai Formation, Atdabanian Stage, Lower CambrialL Fig. 10 — Subtifloria
Journal Article
Published: 01 August 1997
Russ. Geol. Geophys. (1997) 38 (8): 1385–1397.
... meters of the Sukharikha Formation (without the uppermost 1.5–2.0 meters) contain an assemblage of calcareous algae Hedstroemia sp., Renalcis polymorphus Masl., Proaulopora glabra Krasn., Subtifloria gracila Luch., constituting bioherms. Numerous trace fossils in cup-shaped burrows...
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First thumbnail for: UPPER VENDIAN-LOWER CAMBRIAN BIOSTRATIGRAPHY OF TH...
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(1) Girvanella problematica, O3b, sample No. JJSBGS-2-C, oblique longitudinal sections. (2, 3) Girvanella kasakiensis, O2k; (2) sample No. ZZS-Z-2, oblique longitudinal sections; (3) sample No. Na1-3917.51m, oblique longitudinal sections. (4, 5) Subtifloria delicata, O2k; (4) sample No. ZZS-K-3, longitudinal sections, (5) sample No. ZZS-Z-5, longitudinal sections. (6, 7) Acuasiphonoria ordovica, from O3p, sample No TQPQ-4-1, longitudinal and cross sections.
Published: 01 January 2021
Figure 4. ( 1 ) Girvanella problematica , O 3b , sample No. JJSBGS-2-C, oblique longitudinal sections. ( 2, 3 ) Girvanella kasakiensis , O 2k ; ( 2 ) sample No. ZZS-Z-2, oblique longitudinal sections; ( 3 ) sample No. Na1-3917.51m, oblique longitudinal sections. ( 4, 5 ) Subtifloria delicata
Journal Article
Published: 01 October 2013
Jour. Geol. Soc. India (2013) 82 (4): 339–350.
... salinity condition ( Sinha et al. 2005 ). Pyrite is an indicator of poorly oxygenated low energy environment rich in organic matter ( Miller and Heller, 1994 ). Brachiopod and echinoids are frequent biotic frequency with Solenopora filiformis, Dasyporella silurica, Nuia sibirica , and ?Subtifloria algae...
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First thumbnail for: Calcareous Algal Association from the Lower Paleoz...
Second thumbnail for: Calcareous Algal Association from the Lower Paleoz...
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Journal Article
Published: 27 January 2016
Canadian Journal of Earth Sciences (2016) 53 (7): 702–711.
... resolved at the species level. Calcimicrobes (14 taxa) encompass taxa considered to represent calcified cyanobacteria ( Girvanella kasakiensis , G . problematica , Subtifloria delicata , Garwoodia gregaria , Bija sibirica , Ortonella tenuissima , Hedstroemia halimedoidea , Figs. 3A–3H ) and taxa...
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First thumbnail for: Taphocoenoses and diversification patterns of calc...
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Journal Article
Published: 01 May 1998
Russ. Geol. Geophys. (1998) 39 (5): 575–580.
... or the Yenisei R., near town of Igarka, Sukharikha Formation, Tommotian Stage, Lower CambriaI Figs. 7–9 — Subtifloria sp., carbonate-mineralized filaments after dissolutiolL 7. 8 — ×66, 9 — ×32, sample 2155, East Sayan, Sarkhoi R., Khuzhirtai Formation, Atdabanian Stage, Lower CambrialL Fig. 10 — Subtifloria...
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First thumbnail for: SOME PECULIARITIES OF THE EVOLUTION OF THE CALCARE...
Second thumbnail for: SOME PECULIARITIES OF THE EVOLUTION OF THE CALCARE...
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Published: 01 January 2021
, Rothpletzella (misidentified as Sphaerocodium ), Garwoodia reef, lagoon late Katian Bian and Zhou, 1990 ; Fang et al., 1993 ; Chen, 1996 ; Kwon et al., 2012 ; Li et al., 2015 Tarim Tarim Basin, Northwest China Girvanella , Subtifloria , Razumovskia , Acuasiphonoria , Hedstromemia
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(1) Rhabdoporella pachyderma Rothplez, 1913, Axial Section, SR-30, Late Ordovician to Early Silurian, Bar=100 μm. (2) Girvanella problematica Nicholson & Etheridge, 1878, Ordovician to Carboniferous, LS, SR-16 (Arenaceous mudstone), Bar = 20 μm. (3 and 5) ?Subtifloria sp; 3. LS, SR-50 (Grainstone), Early Cambrian-Devonian, Bar = 400 μm 5. LS, SR-10 (Wackestone bioclast), Sumna-Rimkhim section, Shiala Formation, Bar = 100 μm. (4) Nuia sibirica Maslov, 1954, TS, SR-17 (Wackestone bioclast), Early Cambrian to Devonian, Bar = 120 μm. (6) Solenopora filiformis (Nicholson) Rothpletz, 1913, TS, SR-8 (Wackestone bioclast), Silurian, Bar = 300 μm. (7 and 8) Apidium indicumReed, 1912. 7 (Tangential Section), Caradoc, SR-30, Bar=300 μm. 8. (Tangential Section), SR-30, Bar=350 μm. All the figures are from the Shiala Formation of Sumna-Rimkhim section.
Published: 01 October 2013
Plate 2. ( 1 ) Rhabdoporella pachyderma   Rothplez, 1913 , Axial Section, SR-30, Late Ordovician to Early Silurian, Bar=100 μm. ( 2 ) Girvanella problematica   Nicholson & Etheridge, 1878 , Ordovician to Carboniferous, LS, SR-16 (Arenaceous mudstone), Bar = 20 μm. ( 3 and 5 ) ?Subtifloria
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Sedimentary facies types of strata from outcrops and wells involved. (1–4) Reef facies; (1) reef limestone containing the coral Lichenaria and calcified cyanobacteria Proaulopora, O3p, sample No. HSHB-2-2; (2) reef limestone containing the stromatoporid Clathrodictyon, O3b, sample No. LJPA-1; (3) reef limestone containing the calcareous green alga Vermiporella, O3b, sample No. LJP6 (2)-12; (4) reef limestone formed by the red alga Solenopora, O3b, sample No. LJPBGS-1 (d). (5, 6) Open platform; (5) packstone, containing many bioclastics, such as echinoderms, possible alga Halysis, and many calcified cyanobacteria Phacelophyton, O2K, Na1-3918.03m; (6) packstone, containing many bioclastics, such as trilobite, echinoderms, and calcified cyanobacteria Subtifloria, O2K, ZZS-K-3, scale bar = 1 mm. (7, 8) Lagoonal facies; micritic limestone, containing some coral Tetradium and calcified cyanobacteria Zonotrichites, O3p, sample No. XT1-7-33-25. (9) Tidal flat facies; micritic limestone, containing calcified cyanobacteria Proaulopora and Ortonella, O3b, samle No. DZ-2.
Published: 01 January 2021
, such as echinoderms, possible alga Halysis , and many calcified cyanobacteria Phacelophyton , O 2K , Na1-3918.03m; ( 6 ) packstone, containing many bioclastics, such as trilobite, echinoderms, and calcified cyanobacteria Subtifloria , O 2K , ZZS-K-3, scale bar = 1 mm. ( 7, 8 ) Lagoonal facies; micritic limestone
Journal Article
Published: 01 March 1997
Russ. Geol. Geophys. (1997) 38 (3): 661–668.
... microphytoliths Nubecularites punctatus Reitl., N. catagraphus Reitl., calcareous algae Renalcis sp., Girvanella sp., Subtifloria delicata Masl., and radiolarians Paleocenosphaera parva Nazarov ( Fig. 3 , No. 5, thin section T5021/191), widespread in the Lower Cambrian. The member gradually gives...
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First thumbnail for: FINDINGS OF FORAMINIFERS IN “ANCIENT” DEPOSITS OF ...
Second thumbnail for: FINDINGS OF FORAMINIFERS IN “ANCIENT” DEPOSITS OF ...
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Journal Article
Published: 01 December 1999
Russ. Geol. Geophys. (1999) 40 (12): 1753–1762.
..., Girvanella, Hedstroemia, Proaulopora, and Subtifloria. The roof of the Sukharikha Formation, dated as Early Tommotian, consists of up to 1.5 m wide flat biscuit-like Renalcis algal bioherms [ 23 ]. In the western Anabar region, Vendian bioherms form the upper section of the uppermost Vendian Manykai...
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First thumbnail for: REEF FRAMEWORKS ON THE SIBERIAN PLATFORM THROUGH T...
Second thumbnail for: REEF FRAMEWORKS ON THE SIBERIAN PLATFORM THROUGH T...
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