Unique location of hydrothermal biota in the Lower Cambrian sedimentary-volcanogenic complex of the Kyzyl–Tashtyg ore field (Eastern Tuva)
Study of Early Cambrian sedimentary-volcanogenic complexes hosting the Kyzyl–Tashtyg pyrite deposit in Eastern Tuva has revealed cyanobacteria and algae that existed in zones of ore-forming hydrothermal systems similar in characteristics to present-day “black smokers” at ocean bottoms. Along with ar...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Terleev, A.A. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2014transfer abstract |
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| Umfang: |
8 |
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| Übergeordnetes Werk: |
Enthalten in: D-lactic acidosis mediated neuronal encephalopathy in acute lymphoblastic leukemia patient: An under diagnosis - Mendu, Damodara Rao ELSEVIER, 2015, New York, NY |
|---|---|
| Übergeordnetes Werk: |
volume:55 ; year:2014 ; number:1 ; pages:54-61 ; extent:8 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.rgg.2013.12.004 |
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ELV034168087 |
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| 520 | |a Study of Early Cambrian sedimentary-volcanogenic complexes hosting the Kyzyl–Tashtyg pyrite deposit in Eastern Tuva has revealed cyanobacteria and algae that existed in zones of ore-forming hydrothermal systems similar in characteristics to present-day “black smokers” at ocean bottoms. Along with archaeocyaths and Cyanophyta from the host sedimentary rocks and microfossils from basalt amygdules, various cyanobacteria, monocyatheans, and sponge spicules have been found in ferrosiliceous deposits and metasedimentary rocks. Scanning electron microscopic, mineralogical, and thermobarogeochemical studies helped to reconstruct their hydrothermal environment. | ||
| 520 | |a Study of Early Cambrian sedimentary-volcanogenic complexes hosting the Kyzyl–Tashtyg pyrite deposit in Eastern Tuva has revealed cyanobacteria and algae that existed in zones of ore-forming hydrothermal systems similar in characteristics to present-day “black smokers” at ocean bottoms. Along with archaeocyaths and Cyanophyta from the host sedimentary rocks and microfossils from basalt amygdules, various cyanobacteria, monocyatheans, and sponge spicules have been found in ferrosiliceous deposits and metasedimentary rocks. Scanning electron microscopic, mineralogical, and thermobarogeochemical studies helped to reconstruct their hydrothermal environment. | ||
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10.1016/j.rgg.2013.12.004 doi GBVA2014018000025.pica (DE-627)ELV034168087 (ELSEVIER)S1068-7971(13)00240-X DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 610 VZ 660 VZ 660 VZ 58.10 bkl Terleev, A.A. verfasserin aut Unique location of hydrothermal biota in the Lower Cambrian sedimentary-volcanogenic complex of the Kyzyl–Tashtyg ore field (Eastern Tuva) 2014transfer abstract 8 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Study of Early Cambrian sedimentary-volcanogenic complexes hosting the Kyzyl–Tashtyg pyrite deposit in Eastern Tuva has revealed cyanobacteria and algae that existed in zones of ore-forming hydrothermal systems similar in characteristics to present-day “black smokers” at ocean bottoms. Along with archaeocyaths and Cyanophyta from the host sedimentary rocks and microfossils from basalt amygdules, various cyanobacteria, monocyatheans, and sponge spicules have been found in ferrosiliceous deposits and metasedimentary rocks. Scanning electron microscopic, mineralogical, and thermobarogeochemical studies helped to reconstruct their hydrothermal environment. Study of Early Cambrian sedimentary-volcanogenic complexes hosting the Kyzyl–Tashtyg pyrite deposit in Eastern Tuva has revealed cyanobacteria and algae that existed in zones of ore-forming hydrothermal systems similar in characteristics to present-day “black smokers” at ocean bottoms. Along with archaeocyaths and Cyanophyta from the host sedimentary rocks and microfossils from basalt amygdules, various cyanobacteria, monocyatheans, and sponge spicules have been found in ferrosiliceous deposits and metasedimentary rocks. Scanning electron microscopic, mineralogical, and thermobarogeochemical studies helped to reconstruct their hydrothermal environment. Simonov, V.A. oth Kanygin, A.V. oth Tokarev, D.A. oth Stupakov, S.I. oth Kotlyarov, A.V. oth Enthalten in Elsevier Mendu, Damodara Rao ELSEVIER D-lactic acidosis mediated neuronal encephalopathy in acute lymphoblastic leukemia patient: An under diagnosis 2015 New York, NY (DE-627)ELV018845363 volume:55 year:2014 number:1 pages:54-61 extent:8 https://doi.org/10.1016/j.rgg.2013.12.004 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_40 58.10 Verfahrenstechnik: Allgemeines VZ AR 55 2014 1 54-61 8 045F 550 |
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10.1016/j.rgg.2013.12.004 doi GBVA2014018000025.pica (DE-627)ELV034168087 (ELSEVIER)S1068-7971(13)00240-X DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 610 VZ 660 VZ 660 VZ 58.10 bkl Terleev, A.A. verfasserin aut Unique location of hydrothermal biota in the Lower Cambrian sedimentary-volcanogenic complex of the Kyzyl–Tashtyg ore field (Eastern Tuva) 2014transfer abstract 8 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Study of Early Cambrian sedimentary-volcanogenic complexes hosting the Kyzyl–Tashtyg pyrite deposit in Eastern Tuva has revealed cyanobacteria and algae that existed in zones of ore-forming hydrothermal systems similar in characteristics to present-day “black smokers” at ocean bottoms. Along with archaeocyaths and Cyanophyta from the host sedimentary rocks and microfossils from basalt amygdules, various cyanobacteria, monocyatheans, and sponge spicules have been found in ferrosiliceous deposits and metasedimentary rocks. Scanning electron microscopic, mineralogical, and thermobarogeochemical studies helped to reconstruct their hydrothermal environment. Study of Early Cambrian sedimentary-volcanogenic complexes hosting the Kyzyl–Tashtyg pyrite deposit in Eastern Tuva has revealed cyanobacteria and algae that existed in zones of ore-forming hydrothermal systems similar in characteristics to present-day “black smokers” at ocean bottoms. Along with archaeocyaths and Cyanophyta from the host sedimentary rocks and microfossils from basalt amygdules, various cyanobacteria, monocyatheans, and sponge spicules have been found in ferrosiliceous deposits and metasedimentary rocks. Scanning electron microscopic, mineralogical, and thermobarogeochemical studies helped to reconstruct their hydrothermal environment. Simonov, V.A. oth Kanygin, A.V. oth Tokarev, D.A. oth Stupakov, S.I. oth Kotlyarov, A.V. oth Enthalten in Elsevier Mendu, Damodara Rao ELSEVIER D-lactic acidosis mediated neuronal encephalopathy in acute lymphoblastic leukemia patient: An under diagnosis 2015 New York, NY (DE-627)ELV018845363 volume:55 year:2014 number:1 pages:54-61 extent:8 https://doi.org/10.1016/j.rgg.2013.12.004 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_40 58.10 Verfahrenstechnik: Allgemeines VZ AR 55 2014 1 54-61 8 045F 550 |
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10.1016/j.rgg.2013.12.004 doi GBVA2014018000025.pica (DE-627)ELV034168087 (ELSEVIER)S1068-7971(13)00240-X DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 610 VZ 660 VZ 660 VZ 58.10 bkl Terleev, A.A. verfasserin aut Unique location of hydrothermal biota in the Lower Cambrian sedimentary-volcanogenic complex of the Kyzyl–Tashtyg ore field (Eastern Tuva) 2014transfer abstract 8 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Study of Early Cambrian sedimentary-volcanogenic complexes hosting the Kyzyl–Tashtyg pyrite deposit in Eastern Tuva has revealed cyanobacteria and algae that existed in zones of ore-forming hydrothermal systems similar in characteristics to present-day “black smokers” at ocean bottoms. Along with archaeocyaths and Cyanophyta from the host sedimentary rocks and microfossils from basalt amygdules, various cyanobacteria, monocyatheans, and sponge spicules have been found in ferrosiliceous deposits and metasedimentary rocks. Scanning electron microscopic, mineralogical, and thermobarogeochemical studies helped to reconstruct their hydrothermal environment. Study of Early Cambrian sedimentary-volcanogenic complexes hosting the Kyzyl–Tashtyg pyrite deposit in Eastern Tuva has revealed cyanobacteria and algae that existed in zones of ore-forming hydrothermal systems similar in characteristics to present-day “black smokers” at ocean bottoms. Along with archaeocyaths and Cyanophyta from the host sedimentary rocks and microfossils from basalt amygdules, various cyanobacteria, monocyatheans, and sponge spicules have been found in ferrosiliceous deposits and metasedimentary rocks. Scanning electron microscopic, mineralogical, and thermobarogeochemical studies helped to reconstruct their hydrothermal environment. Simonov, V.A. oth Kanygin, A.V. oth Tokarev, D.A. oth Stupakov, S.I. oth Kotlyarov, A.V. oth Enthalten in Elsevier Mendu, Damodara Rao ELSEVIER D-lactic acidosis mediated neuronal encephalopathy in acute lymphoblastic leukemia patient: An under diagnosis 2015 New York, NY (DE-627)ELV018845363 volume:55 year:2014 number:1 pages:54-61 extent:8 https://doi.org/10.1016/j.rgg.2013.12.004 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_40 58.10 Verfahrenstechnik: Allgemeines VZ AR 55 2014 1 54-61 8 045F 550 |
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10.1016/j.rgg.2013.12.004 doi GBVA2014018000025.pica (DE-627)ELV034168087 (ELSEVIER)S1068-7971(13)00240-X DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 610 VZ 660 VZ 660 VZ 58.10 bkl Terleev, A.A. verfasserin aut Unique location of hydrothermal biota in the Lower Cambrian sedimentary-volcanogenic complex of the Kyzyl–Tashtyg ore field (Eastern Tuva) 2014transfer abstract 8 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Study of Early Cambrian sedimentary-volcanogenic complexes hosting the Kyzyl–Tashtyg pyrite deposit in Eastern Tuva has revealed cyanobacteria and algae that existed in zones of ore-forming hydrothermal systems similar in characteristics to present-day “black smokers” at ocean bottoms. Along with archaeocyaths and Cyanophyta from the host sedimentary rocks and microfossils from basalt amygdules, various cyanobacteria, monocyatheans, and sponge spicules have been found in ferrosiliceous deposits and metasedimentary rocks. Scanning electron microscopic, mineralogical, and thermobarogeochemical studies helped to reconstruct their hydrothermal environment. Study of Early Cambrian sedimentary-volcanogenic complexes hosting the Kyzyl–Tashtyg pyrite deposit in Eastern Tuva has revealed cyanobacteria and algae that existed in zones of ore-forming hydrothermal systems similar in characteristics to present-day “black smokers” at ocean bottoms. Along with archaeocyaths and Cyanophyta from the host sedimentary rocks and microfossils from basalt amygdules, various cyanobacteria, monocyatheans, and sponge spicules have been found in ferrosiliceous deposits and metasedimentary rocks. Scanning electron microscopic, mineralogical, and thermobarogeochemical studies helped to reconstruct their hydrothermal environment. Simonov, V.A. oth Kanygin, A.V. oth Tokarev, D.A. oth Stupakov, S.I. oth Kotlyarov, A.V. oth Enthalten in Elsevier Mendu, Damodara Rao ELSEVIER D-lactic acidosis mediated neuronal encephalopathy in acute lymphoblastic leukemia patient: An under diagnosis 2015 New York, NY (DE-627)ELV018845363 volume:55 year:2014 number:1 pages:54-61 extent:8 https://doi.org/10.1016/j.rgg.2013.12.004 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_40 58.10 Verfahrenstechnik: Allgemeines VZ AR 55 2014 1 54-61 8 045F 550 |
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D-lactic acidosis mediated neuronal encephalopathy in acute lymphoblastic leukemia patient: An under diagnosis |
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Unique location of hydrothermal biota in the Lower Cambrian sedimentary-volcanogenic complex of the Kyzyl–Tashtyg ore field (Eastern Tuva) |
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Unique location of hydrothermal biota in the Lower Cambrian sedimentary-volcanogenic complex of the Kyzyl–Tashtyg ore field (Eastern Tuva) |
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Terleev, A.A. |
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D-lactic acidosis mediated neuronal encephalopathy in acute lymphoblastic leukemia patient: An under diagnosis |
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D-lactic acidosis mediated neuronal encephalopathy in acute lymphoblastic leukemia patient: An under diagnosis |
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unique location of hydrothermal biota in the lower cambrian sedimentary-volcanogenic complex of the kyzyl–tashtyg ore field (eastern tuva) |
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Unique location of hydrothermal biota in the Lower Cambrian sedimentary-volcanogenic complex of the Kyzyl–Tashtyg ore field (Eastern Tuva) |
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Study of Early Cambrian sedimentary-volcanogenic complexes hosting the Kyzyl–Tashtyg pyrite deposit in Eastern Tuva has revealed cyanobacteria and algae that existed in zones of ore-forming hydrothermal systems similar in characteristics to present-day “black smokers” at ocean bottoms. Along with archaeocyaths and Cyanophyta from the host sedimentary rocks and microfossils from basalt amygdules, various cyanobacteria, monocyatheans, and sponge spicules have been found in ferrosiliceous deposits and metasedimentary rocks. Scanning electron microscopic, mineralogical, and thermobarogeochemical studies helped to reconstruct their hydrothermal environment. |
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Study of Early Cambrian sedimentary-volcanogenic complexes hosting the Kyzyl–Tashtyg pyrite deposit in Eastern Tuva has revealed cyanobacteria and algae that existed in zones of ore-forming hydrothermal systems similar in characteristics to present-day “black smokers” at ocean bottoms. Along with archaeocyaths and Cyanophyta from the host sedimentary rocks and microfossils from basalt amygdules, various cyanobacteria, monocyatheans, and sponge spicules have been found in ferrosiliceous deposits and metasedimentary rocks. Scanning electron microscopic, mineralogical, and thermobarogeochemical studies helped to reconstruct their hydrothermal environment. |
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Study of Early Cambrian sedimentary-volcanogenic complexes hosting the Kyzyl–Tashtyg pyrite deposit in Eastern Tuva has revealed cyanobacteria and algae that existed in zones of ore-forming hydrothermal systems similar in characteristics to present-day “black smokers” at ocean bottoms. Along with archaeocyaths and Cyanophyta from the host sedimentary rocks and microfossils from basalt amygdules, various cyanobacteria, monocyatheans, and sponge spicules have been found in ferrosiliceous deposits and metasedimentary rocks. Scanning electron microscopic, mineralogical, and thermobarogeochemical studies helped to reconstruct their hydrothermal environment. |
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Unique location of hydrothermal biota in the Lower Cambrian sedimentary-volcanogenic complex of the Kyzyl–Tashtyg ore field (Eastern Tuva) |
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