Biomarkers in the Molar Tooth (MT)-bearing limestones in the Jilin-Liaoning area of China
The origin of Molar Tooth(MT) carbonates has been argued for more than 100 years, which are a kind of Proterozoic carbonates especially composed of microsparite with ptygmatically folded and sheet-like structures. Biomarkers detected in the microcalcsparite from the Wanlong and Xingmincun formations...
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| Veröffentlicht in: | Acta geochimica 2004-10, Vol.23 (4), p.334-341 |
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| creator | Hongwei, Kuang Yanxia, Li Yantao, Zeng Xianghua, Meng Ming, Ge |
| description | The origin of Molar Tooth(MT) carbonates has been argued for more than 100 years, which are a kind of Proterozoic carbonates especially composed of microsparite with ptygmatically folded and sheet-like structures. Biomarkers detected in the microcalcsparite from the Wanlong and Xingmincun formations in the Jilin-Liaoning area showed there are abundant normal alkanes, isoprenoids, hopanes, steranes, alkylmethylcyclohexanes, and alkylcyclohexanes, indicating a diversity of biological source: long-chain isoprenoids, the major components of chlorophyll, such as C^sub 19^, C^sub 20^, a kind of major biomarkers synthesized early by isoprenoid monomers; hopanes a type of characteristic biomarkers from prokaryote, such as archaebacteria and cyanobacteria; sterane a biomarker for eukaryote; and two kinds of alkanes with C^sub 17^, C^sub 18^ as the main peaks representing aquatic bacteria and with C^sub 23^, C^sub 24^ as the main peaks representing fungi, respectively. Biomarker analysis showed that MT is the result of bacterial and algal activities, which is a kind of organisms between aerobic and anaerobic bacteria, reproducing well in normal or slightly saline sea water under weak oxidation-reduction conditions, resulting in rapid deposition of calcite as microsparite due to some mechanisms.[PUBLICATION ABSTRACT] |
| doi_str_mv | 10.1007/BF02871305 |
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Biomarkers detected in the microcalcsparite from the Wanlong and Xingmincun formations in the Jilin-Liaoning area showed there are abundant normal alkanes, isoprenoids, hopanes, steranes, alkylmethylcyclohexanes, and alkylcyclohexanes, indicating a diversity of biological source: long-chain isoprenoids, the major components of chlorophyll, such as C^sub 19^, C^sub 20^, a kind of major biomarkers synthesized early by isoprenoid monomers; hopanes a type of characteristic biomarkers from prokaryote, such as archaebacteria and cyanobacteria; sterane a biomarker for eukaryote; and two kinds of alkanes with C^sub 17^, C^sub 18^ as the main peaks representing aquatic bacteria and with C^sub 23^, C^sub 24^ as the main peaks representing fungi, respectively. Biomarker analysis showed that MT is the result of bacterial and algal activities, which is a kind of organisms between aerobic and anaerobic bacteria, reproducing well in normal or slightly saline sea water under weak oxidation-reduction conditions, resulting in rapid deposition of calcite as microsparite due to some mechanisms.[PUBLICATION ABSTRACT]</description><identifier>ISSN: 1000-9426</identifier><identifier>ISSN: 2096-0956</identifier><identifier>EISSN: 1993-0364</identifier><identifier>EISSN: 2365-7499</identifier><identifier>DOI: 10.1007/BF02871305</identifier><language>eng</language><publisher>Dordrecht: Springer Nature B.V</publisher><subject>Algae ; Alkanes ; Anaerobic bacteria ; Aquatic bacteria ; Archaea ; Archaebacteria ; Biodiversity ; Biomarkers ; Calcite ; Carbonates ; Chemical analysis ; Chlorophyll ; Chlorophylls ; Cyanobacteria ; Fungi ; Geochemistry ; Hopanes ; Monomers ; Oxidation ; Oxidation-reduction potential ; Precambrian ; Seawater ; Stone ; Studies ; Teeth ; Terpenes ; Water analysis</subject><ispartof>Acta geochimica, 2004-10, Vol.23 (4), p.334-341</ispartof><rights>Institute of Geochemistry, Chinese Academy of Sciences 2004</rights><rights>Institute of Geochemistry, Chinese Academy of Sciences 2004.</rights><rights>Copyright © Wanfang Data Co. 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Biomarkers detected in the microcalcsparite from the Wanlong and Xingmincun formations in the Jilin-Liaoning area showed there are abundant normal alkanes, isoprenoids, hopanes, steranes, alkylmethylcyclohexanes, and alkylcyclohexanes, indicating a diversity of biological source: long-chain isoprenoids, the major components of chlorophyll, such as C^sub 19^, C^sub 20^, a kind of major biomarkers synthesized early by isoprenoid monomers; hopanes a type of characteristic biomarkers from prokaryote, such as archaebacteria and cyanobacteria; sterane a biomarker for eukaryote; and two kinds of alkanes with C^sub 17^, C^sub 18^ as the main peaks representing aquatic bacteria and with C^sub 23^, C^sub 24^ as the main peaks representing fungi, respectively. Biomarker analysis showed that MT is the result of bacterial and algal activities, which is a kind of organisms between aerobic and anaerobic bacteria, reproducing well in normal or slightly saline sea water under weak oxidation-reduction conditions, resulting in rapid deposition of calcite as microsparite due to some mechanisms.[PUBLICATION ABSTRACT]</description><subject>Algae</subject><subject>Alkanes</subject><subject>Anaerobic bacteria</subject><subject>Aquatic bacteria</subject><subject>Archaea</subject><subject>Archaebacteria</subject><subject>Biodiversity</subject><subject>Biomarkers</subject><subject>Calcite</subject><subject>Carbonates</subject><subject>Chemical analysis</subject><subject>Chlorophyll</subject><subject>Chlorophylls</subject><subject>Cyanobacteria</subject><subject>Fungi</subject><subject>Geochemistry</subject><subject>Hopanes</subject><subject>Monomers</subject><subject>Oxidation</subject><subject>Oxidation-reduction potential</subject><subject>Precambrian</subject><subject>Seawater</subject><subject>Stone</subject><subject>Studies</subject><subject>Teeth</subject><subject>Terpenes</subject><subject>Water analysis</subject><issn>1000-9426</issn><issn>2096-0956</issn><issn>1993-0364</issn><issn>2365-7499</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2004</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp10c1OGzEQAOBVBVJD6KVPsIIDUGnbWf-ujyQqlCqol_TQk-XdHScOG5vYiaB9eoxSgYSE5jBz-DSjmSmKzzV8rQHkt8kVkEbWFPiHYlQrRSuggh3kGgAqxYj4WByltAIglEo5Kv5MXFibeIcxlc6X2yWWt2EwsZyHsF2W57fzi6pFE51flINbY9oGjy_0pxucr2bOBP8MTERTBltOl86b4-LQmiHhp_95XPy--j6f_qhmv65vppezyhAFomqhrbni2HFUlhIUSHmjBPJeUC7BSmis7SzpDGu5wqZnvLZtJxsjDCd9T8fFxb7vg_HW-IVehV30eaL-t-g3y0eNBIDlAJHt2d7ex7DZ5WX02qUOh8F4DLukJRPQSEHrLE_fyJe2RDZCMZAgszp5VwGTRCrJMvqyR10MKUW0-j66fPO_ugb9_DX9-jX6BD1Ehmw</recordid><startdate>20041001</startdate><enddate>20041001</enddate><creator>Hongwei, Kuang</creator><creator>Yanxia, Li</creator><creator>Yantao, Zeng</creator><creator>Xianghua, Meng</creator><creator>Ming, Ge</creator><general>Springer Nature B.V</general><general>Key Laboratory of Exploration Technologies for Oil and Gas Resources, Yangtze University, Ministry of Education, Jingzhou 434023, China%School of Resource and Information of the University of Petroleum, Beijing 102200, China%Institute of Sedimentary Basin of China University of Geosciences, Beijing 100083, China</general><general>School of Geophysics and Petroleum Resources of Yangtze University</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8BQ</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>D1I</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>JG9</scope><scope>KB.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>M2P</scope><scope>M7S</scope><scope>PCBAR</scope><scope>PDBOC</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>Q9U</scope><scope>M7N</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>20041001</creationdate><title>Biomarkers in the Molar Tooth (MT)-bearing limestones in the Jilin-Liaoning area of China</title><author>Hongwei, Kuang ; 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Biomarkers detected in the microcalcsparite from the Wanlong and Xingmincun formations in the Jilin-Liaoning area showed there are abundant normal alkanes, isoprenoids, hopanes, steranes, alkylmethylcyclohexanes, and alkylcyclohexanes, indicating a diversity of biological source: long-chain isoprenoids, the major components of chlorophyll, such as C^sub 19^, C^sub 20^, a kind of major biomarkers synthesized early by isoprenoid monomers; hopanes a type of characteristic biomarkers from prokaryote, such as archaebacteria and cyanobacteria; sterane a biomarker for eukaryote; and two kinds of alkanes with C^sub 17^, C^sub 18^ as the main peaks representing aquatic bacteria and with C^sub 23^, C^sub 24^ as the main peaks representing fungi, respectively. Biomarker analysis showed that MT is the result of bacterial and algal activities, which is a kind of organisms between aerobic and anaerobic bacteria, reproducing well in normal or slightly saline sea water under weak oxidation-reduction conditions, resulting in rapid deposition of calcite as microsparite due to some mechanisms.[PUBLICATION ABSTRACT]</abstract><cop>Dordrecht</cop><pub>Springer Nature B.V</pub><doi>10.1007/BF02871305</doi><tpages>8</tpages></addata></record> |
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| subjects | Algae Alkanes Anaerobic bacteria Aquatic bacteria Archaea Archaebacteria Biodiversity Biomarkers Calcite Carbonates Chemical analysis Chlorophyll Chlorophylls Cyanobacteria Fungi Geochemistry Hopanes Monomers Oxidation Oxidation-reduction potential Precambrian Seawater Stone Studies Teeth Terpenes Water analysis |
| title | Biomarkers in the Molar Tooth (MT)-bearing limestones in the Jilin-Liaoning area of China |
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