Bacterial, fungal, and algal microfossils in the Lower Proterozoic Baikal region of Siberia (Udokan and Sayany Mountains)
Abstract Microfossils from metamorphized Lower Proterozoic deposits of the Udokan Mountains (Naminga Formation) and Sayany Region (Daldarma Formation) are investigated in preparations and petrographic thin sections. They include leucoxenized and ferruginous threads varying in size (50–500 μm) and th...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Stanevich, A. M. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2013 |
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| Schlagwörter: |
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| Anmerkung: |
© Pleiades Publishing, Ltd. 2013 |
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| Übergeordnetes Werk: |
Enthalten in: Paleontological journal - Moscow : MAIK Nauka/Interperiodica Publ., 1996, 47(2013), 9 vom: 28. Nov., Seite 977-983 |
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| Übergeordnetes Werk: |
volume:47 ; year:2013 ; number:9 ; day:28 ; month:11 ; pages:977-983 |
| Links: |
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| DOI / URN: |
10.1134/S0031030113090207 |
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| Katalog-ID: |
SPR020163673 |
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| 100 | 1 | |a Stanevich, A. M. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Bacterial, fungal, and algal microfossils in the Lower Proterozoic Baikal region of Siberia (Udokan and Sayany Mountains) |
| 264 | 1 | |c 2013 | |
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| 520 | |a Abstract Microfossils from metamorphized Lower Proterozoic deposits of the Udokan Mountains (Naminga Formation) and Sayany Region (Daldarma Formation) are investigated in preparations and petrographic thin sections. They include leucoxenized and ferruginous threads varying in size (50–500 μm) and thread accumulations, which are compared to cyanobacteria. Mineralized thalli probably belong to algae. Small, rounded forms from carbonaceous beds are treated as iron and chemolithotrophic bacteria of stagnant zones of paleobasins. Round or pear-shaped nontransparent forms with projections or several fused forms are described from preparations and identified as fungal microfossils. Similar forms have been recorded in the Lower Proterozoic of Karelia. | ||
| 650 | 4 | |a Bacteria |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a fungi |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a algae |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a microfossils |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Lower Proterozoic |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Siberia |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Baikal Region |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Udokan |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Sayany |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Postnikov, A. A. |4 aut | |
| 700 | 1 | |a Kornilova, T. A. |4 aut | |
| 700 | 1 | |a Terleev, A. A. |4 aut | |
| 700 | 1 | |a Popov, N. V. |4 aut | |
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10.1134/S0031030113090207 doi (DE-627)SPR020163673 (SPR)S0031030113090207-e DE-627 ger DE-627 rakwb eng Stanevich, A. M. verfasserin aut Bacterial, fungal, and algal microfossils in the Lower Proterozoic Baikal region of Siberia (Udokan and Sayany Mountains) 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2013 Abstract Microfossils from metamorphized Lower Proterozoic deposits of the Udokan Mountains (Naminga Formation) and Sayany Region (Daldarma Formation) are investigated in preparations and petrographic thin sections. They include leucoxenized and ferruginous threads varying in size (50–500 μm) and thread accumulations, which are compared to cyanobacteria. Mineralized thalli probably belong to algae. Small, rounded forms from carbonaceous beds are treated as iron and chemolithotrophic bacteria of stagnant zones of paleobasins. Round or pear-shaped nontransparent forms with projections or several fused forms are described from preparations and identified as fungal microfossils. Similar forms have been recorded in the Lower Proterozoic of Karelia. Bacteria (dpeaa)DE-He213 fungi (dpeaa)DE-He213 algae (dpeaa)DE-He213 microfossils (dpeaa)DE-He213 Lower Proterozoic (dpeaa)DE-He213 Siberia (dpeaa)DE-He213 Baikal Region (dpeaa)DE-He213 Udokan (dpeaa)DE-He213 Sayany (dpeaa)DE-He213 Postnikov, A. A. aut Kornilova, T. A. aut Terleev, A. A. aut Popov, N. V. aut Enthalten in Paleontological journal Moscow : MAIK Nauka/Interperiodica Publ., 1996 47(2013), 9 vom: 28. Nov., Seite 977-983 (DE-627)342321196 (DE-600)2071703-9 1555-6174 nnns volume:47 year:2013 number:9 day:28 month:11 pages:977-983 https://dx.doi.org/10.1134/S0031030113090207 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 47 2013 9 28 11 977-983 |
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10.1134/S0031030113090207 doi (DE-627)SPR020163673 (SPR)S0031030113090207-e DE-627 ger DE-627 rakwb eng Stanevich, A. M. verfasserin aut Bacterial, fungal, and algal microfossils in the Lower Proterozoic Baikal region of Siberia (Udokan and Sayany Mountains) 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2013 Abstract Microfossils from metamorphized Lower Proterozoic deposits of the Udokan Mountains (Naminga Formation) and Sayany Region (Daldarma Formation) are investigated in preparations and petrographic thin sections. They include leucoxenized and ferruginous threads varying in size (50–500 μm) and thread accumulations, which are compared to cyanobacteria. Mineralized thalli probably belong to algae. Small, rounded forms from carbonaceous beds are treated as iron and chemolithotrophic bacteria of stagnant zones of paleobasins. Round or pear-shaped nontransparent forms with projections or several fused forms are described from preparations and identified as fungal microfossils. Similar forms have been recorded in the Lower Proterozoic of Karelia. Bacteria (dpeaa)DE-He213 fungi (dpeaa)DE-He213 algae (dpeaa)DE-He213 microfossils (dpeaa)DE-He213 Lower Proterozoic (dpeaa)DE-He213 Siberia (dpeaa)DE-He213 Baikal Region (dpeaa)DE-He213 Udokan (dpeaa)DE-He213 Sayany (dpeaa)DE-He213 Postnikov, A. A. aut Kornilova, T. A. aut Terleev, A. A. aut Popov, N. V. aut Enthalten in Paleontological journal Moscow : MAIK Nauka/Interperiodica Publ., 1996 47(2013), 9 vom: 28. Nov., Seite 977-983 (DE-627)342321196 (DE-600)2071703-9 1555-6174 nnns volume:47 year:2013 number:9 day:28 month:11 pages:977-983 https://dx.doi.org/10.1134/S0031030113090207 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 47 2013 9 28 11 977-983 |
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10.1134/S0031030113090207 doi (DE-627)SPR020163673 (SPR)S0031030113090207-e DE-627 ger DE-627 rakwb eng Stanevich, A. M. verfasserin aut Bacterial, fungal, and algal microfossils in the Lower Proterozoic Baikal region of Siberia (Udokan and Sayany Mountains) 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2013 Abstract Microfossils from metamorphized Lower Proterozoic deposits of the Udokan Mountains (Naminga Formation) and Sayany Region (Daldarma Formation) are investigated in preparations and petrographic thin sections. They include leucoxenized and ferruginous threads varying in size (50–500 μm) and thread accumulations, which are compared to cyanobacteria. Mineralized thalli probably belong to algae. Small, rounded forms from carbonaceous beds are treated as iron and chemolithotrophic bacteria of stagnant zones of paleobasins. Round or pear-shaped nontransparent forms with projections or several fused forms are described from preparations and identified as fungal microfossils. Similar forms have been recorded in the Lower Proterozoic of Karelia. Bacteria (dpeaa)DE-He213 fungi (dpeaa)DE-He213 algae (dpeaa)DE-He213 microfossils (dpeaa)DE-He213 Lower Proterozoic (dpeaa)DE-He213 Siberia (dpeaa)DE-He213 Baikal Region (dpeaa)DE-He213 Udokan (dpeaa)DE-He213 Sayany (dpeaa)DE-He213 Postnikov, A. A. aut Kornilova, T. A. aut Terleev, A. A. aut Popov, N. V. aut Enthalten in Paleontological journal Moscow : MAIK Nauka/Interperiodica Publ., 1996 47(2013), 9 vom: 28. Nov., Seite 977-983 (DE-627)342321196 (DE-600)2071703-9 1555-6174 nnns volume:47 year:2013 number:9 day:28 month:11 pages:977-983 https://dx.doi.org/10.1134/S0031030113090207 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 47 2013 9 28 11 977-983 |
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10.1134/S0031030113090207 doi (DE-627)SPR020163673 (SPR)S0031030113090207-e DE-627 ger DE-627 rakwb eng Stanevich, A. M. verfasserin aut Bacterial, fungal, and algal microfossils in the Lower Proterozoic Baikal region of Siberia (Udokan and Sayany Mountains) 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2013 Abstract Microfossils from metamorphized Lower Proterozoic deposits of the Udokan Mountains (Naminga Formation) and Sayany Region (Daldarma Formation) are investigated in preparations and petrographic thin sections. They include leucoxenized and ferruginous threads varying in size (50–500 μm) and thread accumulations, which are compared to cyanobacteria. Mineralized thalli probably belong to algae. Small, rounded forms from carbonaceous beds are treated as iron and chemolithotrophic bacteria of stagnant zones of paleobasins. Round or pear-shaped nontransparent forms with projections or several fused forms are described from preparations and identified as fungal microfossils. Similar forms have been recorded in the Lower Proterozoic of Karelia. Bacteria (dpeaa)DE-He213 fungi (dpeaa)DE-He213 algae (dpeaa)DE-He213 microfossils (dpeaa)DE-He213 Lower Proterozoic (dpeaa)DE-He213 Siberia (dpeaa)DE-He213 Baikal Region (dpeaa)DE-He213 Udokan (dpeaa)DE-He213 Sayany (dpeaa)DE-He213 Postnikov, A. A. aut Kornilova, T. A. aut Terleev, A. A. aut Popov, N. V. aut Enthalten in Paleontological journal Moscow : MAIK Nauka/Interperiodica Publ., 1996 47(2013), 9 vom: 28. Nov., Seite 977-983 (DE-627)342321196 (DE-600)2071703-9 1555-6174 nnns volume:47 year:2013 number:9 day:28 month:11 pages:977-983 https://dx.doi.org/10.1134/S0031030113090207 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 47 2013 9 28 11 977-983 |
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10.1134/S0031030113090207 doi (DE-627)SPR020163673 (SPR)S0031030113090207-e DE-627 ger DE-627 rakwb eng Stanevich, A. M. verfasserin aut Bacterial, fungal, and algal microfossils in the Lower Proterozoic Baikal region of Siberia (Udokan and Sayany Mountains) 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2013 Abstract Microfossils from metamorphized Lower Proterozoic deposits of the Udokan Mountains (Naminga Formation) and Sayany Region (Daldarma Formation) are investigated in preparations and petrographic thin sections. They include leucoxenized and ferruginous threads varying in size (50–500 μm) and thread accumulations, which are compared to cyanobacteria. Mineralized thalli probably belong to algae. Small, rounded forms from carbonaceous beds are treated as iron and chemolithotrophic bacteria of stagnant zones of paleobasins. Round or pear-shaped nontransparent forms with projections or several fused forms are described from preparations and identified as fungal microfossils. Similar forms have been recorded in the Lower Proterozoic of Karelia. Bacteria (dpeaa)DE-He213 fungi (dpeaa)DE-He213 algae (dpeaa)DE-He213 microfossils (dpeaa)DE-He213 Lower Proterozoic (dpeaa)DE-He213 Siberia (dpeaa)DE-He213 Baikal Region (dpeaa)DE-He213 Udokan (dpeaa)DE-He213 Sayany (dpeaa)DE-He213 Postnikov, A. A. aut Kornilova, T. A. aut Terleev, A. A. aut Popov, N. V. aut Enthalten in Paleontological journal Moscow : MAIK Nauka/Interperiodica Publ., 1996 47(2013), 9 vom: 28. Nov., Seite 977-983 (DE-627)342321196 (DE-600)2071703-9 1555-6174 nnns volume:47 year:2013 number:9 day:28 month:11 pages:977-983 https://dx.doi.org/10.1134/S0031030113090207 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 47 2013 9 28 11 977-983 |
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Bacteria fungi algae microfossils Lower Proterozoic Siberia Baikal Region Udokan Sayany |
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Stanevich, A. M. @@aut@@ Postnikov, A. A. @@aut@@ Kornilova, T. A. @@aut@@ Terleev, A. A. @@aut@@ Popov, N. V. @@aut@@ |
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| author |
Stanevich, A. M. |
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Stanevich, A. M. misc Bacteria misc fungi misc algae misc microfossils misc Lower Proterozoic misc Siberia misc Baikal Region misc Udokan misc Sayany Bacterial, fungal, and algal microfossils in the Lower Proterozoic Baikal region of Siberia (Udokan and Sayany Mountains) |
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Bacterial, fungal, and algal microfossils in the Lower Proterozoic Baikal region of Siberia (Udokan and Sayany Mountains) Bacteria (dpeaa)DE-He213 fungi (dpeaa)DE-He213 algae (dpeaa)DE-He213 microfossils (dpeaa)DE-He213 Lower Proterozoic (dpeaa)DE-He213 Siberia (dpeaa)DE-He213 Baikal Region (dpeaa)DE-He213 Udokan (dpeaa)DE-He213 Sayany (dpeaa)DE-He213 |
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misc Bacteria misc fungi misc algae misc microfossils misc Lower Proterozoic misc Siberia misc Baikal Region misc Udokan misc Sayany |
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misc Bacteria misc fungi misc algae misc microfossils misc Lower Proterozoic misc Siberia misc Baikal Region misc Udokan misc Sayany |
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misc Bacteria misc fungi misc algae misc microfossils misc Lower Proterozoic misc Siberia misc Baikal Region misc Udokan misc Sayany |
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Bacterial, fungal, and algal microfossils in the Lower Proterozoic Baikal region of Siberia (Udokan and Sayany Mountains) |
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(DE-627)SPR020163673 (SPR)S0031030113090207-e |
| title_full |
Bacterial, fungal, and algal microfossils in the Lower Proterozoic Baikal region of Siberia (Udokan and Sayany Mountains) |
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Stanevich, A. M. |
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Stanevich, A. M. Postnikov, A. A. Kornilova, T. A. Terleev, A. A. Popov, N. V. |
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47 |
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Stanevich, A. M. |
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10.1134/S0031030113090207 |
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bacterial, fungal, and algal microfossils in the lower proterozoic baikal region of siberia (udokan and sayany mountains) |
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Bacterial, fungal, and algal microfossils in the Lower Proterozoic Baikal region of Siberia (Udokan and Sayany Mountains) |
| abstract |
Abstract Microfossils from metamorphized Lower Proterozoic deposits of the Udokan Mountains (Naminga Formation) and Sayany Region (Daldarma Formation) are investigated in preparations and petrographic thin sections. They include leucoxenized and ferruginous threads varying in size (50–500 μm) and thread accumulations, which are compared to cyanobacteria. Mineralized thalli probably belong to algae. Small, rounded forms from carbonaceous beds are treated as iron and chemolithotrophic bacteria of stagnant zones of paleobasins. Round or pear-shaped nontransparent forms with projections or several fused forms are described from preparations and identified as fungal microfossils. Similar forms have been recorded in the Lower Proterozoic of Karelia. © Pleiades Publishing, Ltd. 2013 |
| abstractGer |
Abstract Microfossils from metamorphized Lower Proterozoic deposits of the Udokan Mountains (Naminga Formation) and Sayany Region (Daldarma Formation) are investigated in preparations and petrographic thin sections. They include leucoxenized and ferruginous threads varying in size (50–500 μm) and thread accumulations, which are compared to cyanobacteria. Mineralized thalli probably belong to algae. Small, rounded forms from carbonaceous beds are treated as iron and chemolithotrophic bacteria of stagnant zones of paleobasins. Round or pear-shaped nontransparent forms with projections or several fused forms are described from preparations and identified as fungal microfossils. Similar forms have been recorded in the Lower Proterozoic of Karelia. © Pleiades Publishing, Ltd. 2013 |
| abstract_unstemmed |
Abstract Microfossils from metamorphized Lower Proterozoic deposits of the Udokan Mountains (Naminga Formation) and Sayany Region (Daldarma Formation) are investigated in preparations and petrographic thin sections. They include leucoxenized and ferruginous threads varying in size (50–500 μm) and thread accumulations, which are compared to cyanobacteria. Mineralized thalli probably belong to algae. Small, rounded forms from carbonaceous beds are treated as iron and chemolithotrophic bacteria of stagnant zones of paleobasins. Round or pear-shaped nontransparent forms with projections or several fused forms are described from preparations and identified as fungal microfossils. Similar forms have been recorded in the Lower Proterozoic of Karelia. © Pleiades Publishing, Ltd. 2013 |
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9 |
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Bacterial, fungal, and algal microfossils in the Lower Proterozoic Baikal region of Siberia (Udokan and Sayany Mountains) |
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https://dx.doi.org/10.1134/S0031030113090207 |
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Postnikov, A. A. Kornilova, T. A. Terleev, A. A. Popov, N. V. |
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Postnikov, A. A. Kornilova, T. A. Terleev, A. A. Popov, N. V. |
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| doi_str |
10.1134/S0031030113090207 |
| up_date |
2024-07-03T14:17:49.272Z |
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| score |
7.4011583 |