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Proaulopora

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Micrographs of Acuasiphonoria–Proaulopora association from coral reef (A–E from TZ822, O3l; F–I from TZ24, O3l; J–L from TZ241, O3l). Abbreviations as in Figure 5 and: Proa. = Proaulopora; Apop. = Apophoretella. A, B) Proaulopora attached on unidentified organism, 12-66-15. C) Gomphosiphon intergrowth with coral, 12-66-35. D) Acuasiphonoria framework, 5850.33 m. E) Bija as reef framework builder, with Apophoretella intergrowth, 12-66-32. F) Proaulopora as dweller with coral Tetradium, 14-35-34. G) Proaulopora attached on surface of coral Amsassia, 16-35-15. H) Proaulopora intergrowth with coral, 17-43-9. I) Acuasiphonoria as framework, 16-35-8. J) Proaulopora intergrowth with coral Tetradium, 4-36-27. K) Proaulopora attached on surface of coral Amsassia, 10-52-5. L) Unidentified organism, 13-45-18. M) Girvanella as dweller in reef, 10-52-10.
Published: 01 July 2017
Fig . 13. Micrographs of Acuasiphonoria – Proaulopora association from coral reef (A–E from TZ822, O 3 l; F–I from TZ24, O 3 l; J–L from TZ241, O 3 l). Abbreviations as in Figure 5 and: Proa. = Proaulopora ; Apop. = Apophoretella . A , B ) Proaulopora attached on unidentified organism
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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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Fossil genera of Proaulopora and Phacelophyton and their probable present-day analogues, Dichothrix and Calothrix (rivulariaceans cyanobacteria), based on morphology. (1) Pictures of Proaulopora ordosia n. sp. from Ordos Basin (this study); (2) pictures of Proaulopora rarissina from Tarim Basin (Liu et al., 2016b); (3) synthesized pictures of Phacelophyton yushanensis from both Tarim Basin (longitudinal sections, Liu et al., 2016b) and Ordos Basin (cross sections, this paper); arrows indicate the swirl-like appearance of sheath and the position of dichotomous branching in the cross section.
Published: 01 January 2021
Figure 8. Fossil genera of Proaulopora and Phacelophyton and their probable present-day analogues, Dichothrix and Calothrix (rivulariaceans cyanobacteria), based on morphology. ( 1 ) Pictures of Proaulopora ordosia n. sp. from Ordos Basin (this study); ( 2 ) pictures of Proaulopora
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Micrographs of Hedstroemia–Cayeuxia from lagoonal deposits and Girvanella–Proaulopora association from tidal flat deposits. Abbreviations as in previous captions (Figs. 5, 13) and: Heds. = Hedstroemia; Zono. = Zonotrichities. A–E) Hedstroemia–Cayeuxia association from lagoon: micritic limestone containing Hedstroemia, TZ72-12-84-10, O3l (A); micritic limestone containing Cayeuxia, M5-19-40-29, O3l (B); micritic limestone containing Ortonella, TZ83-3-50-23, O3l (C); micritic limestone containing Zonotrichities, O3l (D); micritic limestone containing Hedstroemia, TZ161, 4439.6 m, O3l (E). F) Micritic limestone containing Garwoodia, from 4475.63 m of TZ43, O3l. G) Micritic limestone, containing Hedstroemia, TZ23-9-47-36, O3l. H) Zonotrichites associated with Tetradium, O3l, from 4696.56 m of well TZ7. I–M) Proaulopora–Girvanella association from tidal flat: Girvanella occurrence in micritic limestone with fenestral structure, TK1-26-15-8, O2y (I, J); Proaulopora occurrence in micritic limestone with fenestral structure, TK1-22-19-17, O2y (K); Girvanella occurrence in micritic limestone with fenestral structure, TZ161-23-50-25, O3l (L); Proaulopora occurrence in micritic limestone with fenestral structure, TZ451-6-42-13, O3l (M).
Published: 01 July 2017
Fig . 16. Micrographs of Hedstroemia – Cayeuxia from lagoonal deposits and Girvanella – Proaulopora association from tidal flat deposits. Abbreviations as in previous captions ( Figs. 5 , 13 ) and: Heds. = Hedstroemia ; Zono. = Zonotrichities . A – E ) Hedstroemia – Cayeuxia association
Journal Article
Published: 01 January 2021
Journal of Paleontology (2021) 95 (1): 1–23.
...Figure 8. Fossil genera of Proaulopora and Phacelophyton and their probable present-day analogues, Dichothrix and Calothrix (rivulariaceans cyanobacteria), based on morphology. ( 1 ) Pictures of Proaulopora ordosia n. sp. from Ordos Basin (this study); ( 2 ) pictures of Proaulopora...
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First thumbnail for: Diversity and systematics of Middle-Late Ordovicia...
Second thumbnail for: Diversity and systematics of Middle-Late Ordovicia...
Third thumbnail for: Diversity and systematics of Middle-Late Ordovicia...
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(1–3) Proaulopora ordosia n. sp., O3p. (1) Sample No. HSHB-2-2, cross sections; arrows indicate the cross sections where two tubes are included in one tubular sheath; (2, 3) sample No. HSH-5-C, cross section and longitudinal sections; the arrows in (2) indicate the external collars extending from the outer surface; the arrows in (3) point to the non-disjunctionally dichotomous branching. (4–8) Phacelophyton yushanensis; (4) O2k, sample No. Na1-3917.51, cross section and longitudinal sections; arrow indicates the position of dichotomous branching; (5) O2k, sample No. Na1-3918.03, cross sections; arrow points to the swirl-like appearance of the sheath in the cross section; (6) O2k, sample No. Na1-3918.22, cross section and longitudinal sections; (7, 8) O3p, sample No. TQPBD-7, (7) longitudinal section, (8) most are cross sections, the arrow points to a longitudinal section.
Published: 01 January 2021
Figure 7. ( 1–3 ) Proaulopora ordosia n. sp., O 3p . ( 1 ) Sample No. HSHB-2-2, cross sections; arrows indicate the cross sections where two tubes are included in one tubular sheath; ( 2, 3 ) sample No. HSH-5-C, cross section and longitudinal sections; the arrows in ( 2 ) indicate the external
Journal Article
Journal: PALAIOS
Published: 01 July 2017
PALAIOS (2017) 32 (7): 462–489.
...Fig . 13. Micrographs of Acuasiphonoria – Proaulopora association from coral reef (A–E from TZ822, O 3 l; F–I from TZ24, O 3 l; J–L from TZ241, O 3 l). Abbreviations as in Figure 5 and: Proa. = Proaulopora ; Apop. = Apophoretella . A , B ) Proaulopora attached on unidentified organism...
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First thumbnail for: PALEOENVIRONMENTAL DISTRIBUTION OF ORDOVICIAN CALC...
Second thumbnail for: PALEOENVIRONMENTAL DISTRIBUTION OF ORDOVICIAN CALC...
Third thumbnail for: PALEOENVIRONMENTAL DISTRIBUTION OF ORDOVICIAN CALC...
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 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...
Second thumbnail for: UPPER VENDIAN-LOWER CAMBRIAN BIOSTRATIGRAPHY OF TH...
Third thumbnail for: UPPER VENDIAN-LOWER CAMBRIAN BIOSTRATIGRAPHY OF TH...
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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
Figure 3. 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 , O 3p , sample No. HSHB-2-2; ( 2 ) reef limestone containing the stromatoporid Clathrodictyon , O
Journal Article
Published: 01 April 2002
Russ. Geol. Geophys. (2002) 43 (4): 334–342.
... 2002 UIGGM, SIBERIAN BRANCH OF THE RAS 2002 UIGGM, SIBERIAN BRANCH OF THE RAS Layer 9. Gray and pinkish-gray organogenic limestone abundant in organic detritus. Trilobites Olenoides sp., Kootenia sp.; calcibionts Tubophyllum victori , Proaulopora glabra ; hyolithellminths Hyolithellus...
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First thumbnail for: BIOSTRATIGRAPHY OF THE UPPER VENDIAN, LOWER AND MI...
Second thumbnail for: BIOSTRATIGRAPHY OF THE UPPER VENDIAN, LOWER AND MI...
Third thumbnail for: BIOSTRATIGRAPHY OF THE UPPER VENDIAN, LOWER AND MI...
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 May 1998
Russ. Geol. Geophys. (1998) 39 (5): 575–580.
... in the late Mesozoic [ 10 ]. To draw this conclusion, we had to argue against a number of concepts that more typical representatives of calcibionts such as Epiphyton Born., Razumovskia Vologd., Chabakovia Vologd., Batenevia Korde, and others belong to red algae, whereas Proaulopora Vologd. belongs...
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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...
Third thumbnail for: SOME PECULIARITIES OF THE EVOLUTION OF THE CALCARE...
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Levels of the appearance of principally new morphological types of microfossils in the Riphean [16]. Forms: 1 – Quatematiphycus Yaksch., 2 – Glomophycus Yaksch, 3 – Orculiphycus Yaksch., 4 – Corynophycus Yaksch., 5 – Polybessurus Schopf., 6 – Ulophyton Tim. et Herm., 7 – Proaulopora Vologd., 8 – Archaeoclada Herm., 9 – Trachyhystrichosphaera membranacea Pjat. 10 – Palaeovaucheria clavata Herm., 11 – Bailicania memorabilae Trestsh., 12 – Micrhystridium Deflandre, 13 – Fistularia Yaksch., 14 – Baltishaeridium varium Volkova, 15 – Catenuata Yaksch.
Published: 01 December 1997
Herm., 7 – Proaulopora Vologd., 8 – Archaeoclada Herm., 9 – Trachyhystrichosphaera membranacea Pjat. 10 – Palaeovaucheria clavata Herm., 11 – Bailicania memorabilae Trestsh., 12 – Micrhystridium Deflandre, 13 – Fistularia Yaksch., 14 – Baltishaeridium varium Volkova, 15
Journal Article
Published: 01 December 1997
Russ. Geol. Geophys. (1997) 38 (12): 1912–1920.
... Herm., 7 – Proaulopora Vologd., 8 – Archaeoclada Herm., 9 – Trachyhystrichosphaera membranacea Pjat. 10 – Palaeovaucheria clavata Herm., 11 – Bailicania memorabilae Trestsh., 12 – Micrhystridium Deflandre, 13 – Fistularia Yaksch., 14 – Baltishaeridium varium Volkova, 15...
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First thumbnail for: STAGES OF THE EVOLUTION OF MICROFOSSILS AND PHYTOL...
Second thumbnail for: STAGES OF THE EVOLUTION OF MICROFOSSILS AND PHYTOL...
Third thumbnail for: STAGES OF THE EVOLUTION OF MICROFOSSILS AND PHYTOL...
Journal Article
Published: 01 March 1997
Russ. Geol. Geophys. (1997) 38 (3): 648–660.
... Ulzutui paleontological beds have been described from the Oktyabr’sky and Ulzutui areas [ 8 ]. In other areas remains are scarce. Also, Leptosocyathus sp., Erismacoscinus * incurvatus (Vol.), E. comucopiae (Born.), Epiphyton sp., Proaulopora sp. were found in the Oktyabr’sky area...
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First thumbnail for: STRATIGRAPHY OF CAMBRIAN DEPOSITS IN THE OZERNY OR...
Second thumbnail for: STRATIGRAPHY OF CAMBRIAN DEPOSITS IN THE OZERNY OR...
Third thumbnail for: STRATIGRAPHY OF CAMBRIAN DEPOSITS IN THE OZERNY OR...
Journal Article
Published: 01 October 2012
Russ. Geol. Geophys. (2012) 53 (10): 972–981.
... polymorphus Masl., Renalcis granosus Vologd., Proaulopora glabra Krasnop., and Gemma sp., Subtifloria sp., as well as stratiform stromatolites Irregularia sp., Stratifera sp. and columnar stromatolites Collumna-collenia sp . Examination of thin sections revealed small shelly fossils...
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First thumbnail for: Cambrian section in the east of the West Siberian ...
Second thumbnail for: Cambrian section in the east of the West Siberian ...
Third thumbnail for: Cambrian section in the east of the West Siberian ...
Journal Article
Published: 01 March 2004
Russ. Geol. Geophys. (2004) 45 (3): 295–309.
... some authors [ 32 , 33 ], attributing the clastic limestones of the upper Belka Formation (152 m) to the Ust’-Kundat Formation (Member A). We share this opinion. Organic remains in the upper Belka Formation are represented by calcareous algae of the genera Korilophyton Voron., Proaulopora Vologd...
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First thumbnail for: NEOPROTEROZOIC STRATIGRAPHY OF THE ALTAI-SAYAN FOL...
Second thumbnail for: NEOPROTEROZOIC STRATIGRAPHY OF THE ALTAI-SAYAN FOL...
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...
Third thumbnail for: REEF FRAMEWORKS ON THE SIBERIAN PLATFORM THROUGH T...
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Published: 01 January 2021
, Cayeuxia , Bija , Apophoretella , Ortonella , Zonotrichites , Bevocastira , Proaulopora , Phacelophyton , Gomphosiphon Renalcis , Izhella , Epiphyton , Wetheredella , Rothpletzella , Garwoodia reef, open platform, lagoon, tidal flat lower Katian, Darriwilian Riding and Fan, 2001 ; Wang