189 results on '"EZAKI, Yoichi"'
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2. Cambrian through Ordovician reef transitions in North and South China: Changes in reef construction and background geobiological environments
3. Cambrian Series 2 (Stage 4) calcimicrobial reefs in Shandong Province, North China: Calcimicrobial diversity and contribution to reef construction
4. Rare earth and yttrium elements (REY) patterns of mesostructures of Miaolingian (Cambrian) thrombolites at Jiulongshan, Shandong Province, China
5. Earliest known Cambrian calcimicrobial reefs occur in the Gobi-Altai, western Mongolia: Intriguing geobiological products immediately after the Ediacaran–Cambrian boundary
6. Late Ediacaran Boxonia-bearing stromatolites from the Gobi-Altay, western Mongolia
7. Paleoecological and Phylogenetic Implications of Asexual Reproduction in the Permian Scleractiniamorph Numidiaphyllum
8. MICROBIALITE DEVELOPMENT DURING THE PROTRACTED INHIBITION OF SKELETAL-DOMINATED REEFS IN THE ZHANGXIA FORMATION (CAMBRIAN SERIES 3) IN SHANDONG PROVINCE, NORTH CHINA
9. Earliest Triassic Microbialite Micro- to Megastructures in the Huaying Area of Sichuan Province, South China: Implications for the Nature of Oceanic Conditions after the End-Permian Extinction
10. Stromatolites near the Permian–Triassic boundary in Chongyang, Hubei Province, South China: A geobiological window into palaeo-oceanic fluctuations following the end-Permian extinction
11. Stacking patterns and growth models of multiscopic structures within Cambrian Series 3 thrombolites at the Jiulongshan section, Shandong Province, northern China
12. The Permian coral Numidiaphyllum: new insights into anthozoan phylogeny and Triassic scleractinian origins
13. Paleozoic Scleratinia: Progenitors or Extinct Experiments?
14. Three‐dimensional reconstruction of thein situmode of life of the Cambrian coralCambroctoconus: asexual reproduction and colony growth in immediate response to cryptic habitats
15. Full Coralla [Video] [Etc]
16. Microbialite With Coralla [SequentialSectionImageSeries] [Etc]
17. A Corallum (No 18) [Video] [Etc]
18. Three Coralla (Nos 8, 9, And 93) [Video] [Etc]
19. Three Coralla (Nos 8, 9, And 93) [Mesh] [Etc]
20. Full Coralla [Mesh] [Etc]
21. A Corallum (No 4) [Video] [Etc]
22. A Corallum (No 18) [Mesh] [Etc]
23. A Corallum (No 4) [Mesh] [Etc]
24. Lower Ordovician Stromatolites from the Anhui Province of South China: Construction and Geobiological Significance
25. The late early Cambrian microbial reefs immediately after the demise of archaeocyathan reefs, Hunan Province, South China
26. Three‐dimensional reconstruction of the in situ mode of life of the Cambrian coral Cambroctoconus: asexual reproduction and colony growth in immediate response to cryptic habitats.
27. ASEXUAL REPRODUCTION OF PLIOCENE SOLITARY SCLERACTINIAN CORAL TRUNCATOFLABELLUM: A MORPHOLOGICAL AND BIOMETRIC STUDY
28. EARLY ORDOVICIAN SHIFT IN REEF CONSTRUCTION FROM MICROBIAL TO METAZOAN REEFS
29. Geobiological Aspects of the Earliest Triassic Microbialites along the Southern Periphery of the Tropical Yangtze Platform: Initiation and Cessation of a Microbial Regime
30. Late Early Cambrian archaeocyath reefs in Hubei Province, South China: modes of construction during their period of demise
31. Early Ordovician reef construction in Anhui Province, South China: A geobiological transition from microbial- to metazoan-dominant reefs
32. First record of Heterocorallia (Hexaphyllia Stuckenberg 1904) from the Lower Carboniferous (Viséan) of west-central Sinai, Egypt
33. Microbial impacts on the genesis of Lower Devonian reefal limestones, eastern Australia
34. Lower Ordovician Stromatolites from the Anhui Province of South China: Construction and Geobiological Significance
35. Marked accumulation patterns characteristic of Lower Devonian stromatoporoid bindstone: Palaeoecological interactions between skeletal organisms and microbes
36. Microskeletal Structures Suggest Taxonomic Distinction between Subgenera of Azooxanthellate Scleractinian Flabellum
37. Cryptic growth strategies of the Cambrian coral Cambroctoconus : flexible modes of budding and growth in immediate response to available space
38. [Comment. Earliest Triassic Microbialite Micro-to Megastructures in the Huaying Area of Sichuan Province, South China: Implications for the Nature of Oceanic Conditions after the End-Permian Extinction (Ezaki et al., 2003)]: Reply
39. The fabrics and origins of peloids immediately after the end-Permian extinction, Guizhou Province, South China
40. Variations in the disappearance patterns of rugosan corals in Tethys and their implications for environments at the end of the Permian
41. Fluctuations in pelagic environments near the Permian–Triassic boundary in the Mino-Tamba Terrane, southwest Japan
42. Erratum to: Early Ordovician reefs in South China (Chenjiahe section, Hubei Province): deciphering the early evolution of skeletal-dominated reefs
43. First real-time observation of transverse division in azooxanthellate scleractinian corals
44. Evidence for decoupling of relative abundance and biodiversity of marine organisms in initial stage of GOBE: A preliminary study on lower ordovician shellbeds of South China
45. Modes of regeneration and adaptation to soft-bottom substrates of the free-living solitary scleractinianDeltocyathoides orientalis
46. First real-time observation of transverse division in azooxanthellate scleractinian corals
47. Permian and Triassic radiolarians from the western Guangxi area, China
48. Lithostratigraphy and microfacies of the Lower Carboniferous (Visean) Um Bogma Formation in Gabal Nukhul, west-central Sinai, Egypt
49. Burrowing hard corals occurring on the sea floor since 80 million years ago
50. Permian radiolarians from the Qinfang Terrane, South China, and its geological significance
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