From diatom opal-A δ18O to chert δ18O in deep sea sediments
δ18O signature of marine deep-sea cherts was previously used to reconstruct past ocean temperature and oceanic bottom water δ18O through the Cenozoic and Mesozoic periods. Oxygen isotopes in deep-sea cherts which were never exposed to meteoric water exhibit a wide range of values indicating that the...
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| Autor*in: |
Yanchilina, A.G. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2020transfer abstract |
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| Umfang: |
15 |
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| Übergeordnetes Werk: |
Enthalten in: 109 Discovery of Novel DNA Methylation Markers for the Detection of Colorectal Neoplasia: Selection by Methylome-Wide Analysis - Taylor, William R. ELSEVIER, 2014, journal of the Geochemical Society and the Meteoritical Society, New York, NY [u.a.] |
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| Übergeordnetes Werk: |
volume:268 ; year:2020 ; day:1 ; month:01 ; pages:368-382 ; extent:15 |
| Links: |
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| DOI / URN: |
10.1016/j.gca.2019.10.018 |
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ELV048684376 |
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| 520 | |a δ18O signature of marine deep-sea cherts was previously used to reconstruct past ocean temperature and oceanic bottom water δ18O through the Cenozoic and Mesozoic periods. Oxygen isotopes in deep-sea cherts which were never exposed to meteoric water exhibit a wide range of values indicating that the evolution and maturation of biogenic amorphous opal (opal-A) to opal-CT and microquartz chert is accompanied by isotopic changes. We measured δ18O of diatom opal-A, opal-CT, and microquartz chert in downcore profiles of sediment cores ODP 795 and 799 from the Sea of Japan. Diatom opal-A, opal-CT and microquartz chert were separated and purified from the bulk sediment. This was followed by XRD, SEM/EDS and XPS to identify and quantify the mineral phases, the qualitative elemental concentrations and the amounts of authigenic clays. | ||
| 520 | |a δ18O signature of marine deep-sea cherts was previously used to reconstruct past ocean temperature and oceanic bottom water δ18O through the Cenozoic and Mesozoic periods. Oxygen isotopes in deep-sea cherts which were never exposed to meteoric water exhibit a wide range of values indicating that the evolution and maturation of biogenic amorphous opal (opal-A) to opal-CT and microquartz chert is accompanied by isotopic changes. We measured δ18O of diatom opal-A, opal-CT, and microquartz chert in downcore profiles of sediment cores ODP 795 and 799 from the Sea of Japan. Diatom opal-A, opal-CT and microquartz chert were separated and purified from the bulk sediment. This was followed by XRD, SEM/EDS and XPS to identify and quantify the mineral phases, the qualitative elemental concentrations and the amounts of authigenic clays. | ||
| 650 | 7 | |a Silica diagenesis |2 Elsevier | |
| 650 | 7 | |a Deep sea sediments |2 Elsevier | |
| 650 | 7 | |a Oxygen isotopes |2 Elsevier | |
| 700 | 1 | |a Yam, R. |4 oth | |
| 700 | 1 | |a Kolodny, Y. |4 oth | |
| 700 | 1 | |a Shemesh, A. |4 oth | |
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10.1016/j.gca.2019.10.018 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001406.pica (DE-627)ELV048684376 (ELSEVIER)S0016-7037(19)30662-3 DE-627 ger DE-627 rakwb eng 610 VZ 570 VZ BIODIV DE-30 fid 35.70 bkl 42.12 bkl 42.15 bkl Yanchilina, A.G. verfasserin aut From diatom opal-A δ18O to chert δ18O in deep sea sediments 2020transfer abstract 15 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier δ18O signature of marine deep-sea cherts was previously used to reconstruct past ocean temperature and oceanic bottom water δ18O through the Cenozoic and Mesozoic periods. Oxygen isotopes in deep-sea cherts which were never exposed to meteoric water exhibit a wide range of values indicating that the evolution and maturation of biogenic amorphous opal (opal-A) to opal-CT and microquartz chert is accompanied by isotopic changes. We measured δ18O of diatom opal-A, opal-CT, and microquartz chert in downcore profiles of sediment cores ODP 795 and 799 from the Sea of Japan. Diatom opal-A, opal-CT and microquartz chert were separated and purified from the bulk sediment. This was followed by XRD, SEM/EDS and XPS to identify and quantify the mineral phases, the qualitative elemental concentrations and the amounts of authigenic clays. δ18O signature of marine deep-sea cherts was previously used to reconstruct past ocean temperature and oceanic bottom water δ18O through the Cenozoic and Mesozoic periods. Oxygen isotopes in deep-sea cherts which were never exposed to meteoric water exhibit a wide range of values indicating that the evolution and maturation of biogenic amorphous opal (opal-A) to opal-CT and microquartz chert is accompanied by isotopic changes. We measured δ18O of diatom opal-A, opal-CT, and microquartz chert in downcore profiles of sediment cores ODP 795 and 799 from the Sea of Japan. Diatom opal-A, opal-CT and microquartz chert were separated and purified from the bulk sediment. This was followed by XRD, SEM/EDS and XPS to identify and quantify the mineral phases, the qualitative elemental concentrations and the amounts of authigenic clays. Silica diagenesis Elsevier Deep sea sediments Elsevier Oxygen isotopes Elsevier Yam, R. oth Kolodny, Y. oth Shemesh, A. oth Enthalten in Elsevier Taylor, William R. ELSEVIER 109 Discovery of Novel DNA Methylation Markers for the Detection of Colorectal Neoplasia: Selection by Methylome-Wide Analysis 2014 journal of the Geochemical Society and the Meteoritical Society New York, NY [u.a.] (DE-627)ELV012653268 volume:268 year:2020 day:1 month:01 pages:368-382 extent:15 https://doi.org/10.1016/j.gca.2019.10.018 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-BIODIV SSG-OLC-PHA 35.70 Biochemie: Allgemeines VZ 42.12 Biophysik VZ 42.15 Zellbiologie VZ AR 268 2020 1 0101 368-382 15 |
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10.1016/j.gca.2019.10.018 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001406.pica (DE-627)ELV048684376 (ELSEVIER)S0016-7037(19)30662-3 DE-627 ger DE-627 rakwb eng 610 VZ 570 VZ BIODIV DE-30 fid 35.70 bkl 42.12 bkl 42.15 bkl Yanchilina, A.G. verfasserin aut From diatom opal-A δ18O to chert δ18O in deep sea sediments 2020transfer abstract 15 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier δ18O signature of marine deep-sea cherts was previously used to reconstruct past ocean temperature and oceanic bottom water δ18O through the Cenozoic and Mesozoic periods. Oxygen isotopes in deep-sea cherts which were never exposed to meteoric water exhibit a wide range of values indicating that the evolution and maturation of biogenic amorphous opal (opal-A) to opal-CT and microquartz chert is accompanied by isotopic changes. We measured δ18O of diatom opal-A, opal-CT, and microquartz chert in downcore profiles of sediment cores ODP 795 and 799 from the Sea of Japan. Diatom opal-A, opal-CT and microquartz chert were separated and purified from the bulk sediment. This was followed by XRD, SEM/EDS and XPS to identify and quantify the mineral phases, the qualitative elemental concentrations and the amounts of authigenic clays. δ18O signature of marine deep-sea cherts was previously used to reconstruct past ocean temperature and oceanic bottom water δ18O through the Cenozoic and Mesozoic periods. Oxygen isotopes in deep-sea cherts which were never exposed to meteoric water exhibit a wide range of values indicating that the evolution and maturation of biogenic amorphous opal (opal-A) to opal-CT and microquartz chert is accompanied by isotopic changes. We measured δ18O of diatom opal-A, opal-CT, and microquartz chert in downcore profiles of sediment cores ODP 795 and 799 from the Sea of Japan. Diatom opal-A, opal-CT and microquartz chert were separated and purified from the bulk sediment. This was followed by XRD, SEM/EDS and XPS to identify and quantify the mineral phases, the qualitative elemental concentrations and the amounts of authigenic clays. Silica diagenesis Elsevier Deep sea sediments Elsevier Oxygen isotopes Elsevier Yam, R. oth Kolodny, Y. oth Shemesh, A. oth Enthalten in Elsevier Taylor, William R. ELSEVIER 109 Discovery of Novel DNA Methylation Markers for the Detection of Colorectal Neoplasia: Selection by Methylome-Wide Analysis 2014 journal of the Geochemical Society and the Meteoritical Society New York, NY [u.a.] (DE-627)ELV012653268 volume:268 year:2020 day:1 month:01 pages:368-382 extent:15 https://doi.org/10.1016/j.gca.2019.10.018 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-BIODIV SSG-OLC-PHA 35.70 Biochemie: Allgemeines VZ 42.12 Biophysik VZ 42.15 Zellbiologie VZ AR 268 2020 1 0101 368-382 15 |
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10.1016/j.gca.2019.10.018 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001406.pica (DE-627)ELV048684376 (ELSEVIER)S0016-7037(19)30662-3 DE-627 ger DE-627 rakwb eng 610 VZ 570 VZ BIODIV DE-30 fid 35.70 bkl 42.12 bkl 42.15 bkl Yanchilina, A.G. verfasserin aut From diatom opal-A δ18O to chert δ18O in deep sea sediments 2020transfer abstract 15 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier δ18O signature of marine deep-sea cherts was previously used to reconstruct past ocean temperature and oceanic bottom water δ18O through the Cenozoic and Mesozoic periods. Oxygen isotopes in deep-sea cherts which were never exposed to meteoric water exhibit a wide range of values indicating that the evolution and maturation of biogenic amorphous opal (opal-A) to opal-CT and microquartz chert is accompanied by isotopic changes. We measured δ18O of diatom opal-A, opal-CT, and microquartz chert in downcore profiles of sediment cores ODP 795 and 799 from the Sea of Japan. Diatom opal-A, opal-CT and microquartz chert were separated and purified from the bulk sediment. This was followed by XRD, SEM/EDS and XPS to identify and quantify the mineral phases, the qualitative elemental concentrations and the amounts of authigenic clays. δ18O signature of marine deep-sea cherts was previously used to reconstruct past ocean temperature and oceanic bottom water δ18O through the Cenozoic and Mesozoic periods. Oxygen isotopes in deep-sea cherts which were never exposed to meteoric water exhibit a wide range of values indicating that the evolution and maturation of biogenic amorphous opal (opal-A) to opal-CT and microquartz chert is accompanied by isotopic changes. We measured δ18O of diatom opal-A, opal-CT, and microquartz chert in downcore profiles of sediment cores ODP 795 and 799 from the Sea of Japan. Diatom opal-A, opal-CT and microquartz chert were separated and purified from the bulk sediment. This was followed by XRD, SEM/EDS and XPS to identify and quantify the mineral phases, the qualitative elemental concentrations and the amounts of authigenic clays. Silica diagenesis Elsevier Deep sea sediments Elsevier Oxygen isotopes Elsevier Yam, R. oth Kolodny, Y. oth Shemesh, A. oth Enthalten in Elsevier Taylor, William R. ELSEVIER 109 Discovery of Novel DNA Methylation Markers for the Detection of Colorectal Neoplasia: Selection by Methylome-Wide Analysis 2014 journal of the Geochemical Society and the Meteoritical Society New York, NY [u.a.] (DE-627)ELV012653268 volume:268 year:2020 day:1 month:01 pages:368-382 extent:15 https://doi.org/10.1016/j.gca.2019.10.018 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-BIODIV SSG-OLC-PHA 35.70 Biochemie: Allgemeines VZ 42.12 Biophysik VZ 42.15 Zellbiologie VZ AR 268 2020 1 0101 368-382 15 |
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10.1016/j.gca.2019.10.018 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001406.pica (DE-627)ELV048684376 (ELSEVIER)S0016-7037(19)30662-3 DE-627 ger DE-627 rakwb eng 610 VZ 570 VZ BIODIV DE-30 fid 35.70 bkl 42.12 bkl 42.15 bkl Yanchilina, A.G. verfasserin aut From diatom opal-A δ18O to chert δ18O in deep sea sediments 2020transfer abstract 15 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier δ18O signature of marine deep-sea cherts was previously used to reconstruct past ocean temperature and oceanic bottom water δ18O through the Cenozoic and Mesozoic periods. Oxygen isotopes in deep-sea cherts which were never exposed to meteoric water exhibit a wide range of values indicating that the evolution and maturation of biogenic amorphous opal (opal-A) to opal-CT and microquartz chert is accompanied by isotopic changes. We measured δ18O of diatom opal-A, opal-CT, and microquartz chert in downcore profiles of sediment cores ODP 795 and 799 from the Sea of Japan. Diatom opal-A, opal-CT and microquartz chert were separated and purified from the bulk sediment. This was followed by XRD, SEM/EDS and XPS to identify and quantify the mineral phases, the qualitative elemental concentrations and the amounts of authigenic clays. δ18O signature of marine deep-sea cherts was previously used to reconstruct past ocean temperature and oceanic bottom water δ18O through the Cenozoic and Mesozoic periods. Oxygen isotopes in deep-sea cherts which were never exposed to meteoric water exhibit a wide range of values indicating that the evolution and maturation of biogenic amorphous opal (opal-A) to opal-CT and microquartz chert is accompanied by isotopic changes. We measured δ18O of diatom opal-A, opal-CT, and microquartz chert in downcore profiles of sediment cores ODP 795 and 799 from the Sea of Japan. Diatom opal-A, opal-CT and microquartz chert were separated and purified from the bulk sediment. This was followed by XRD, SEM/EDS and XPS to identify and quantify the mineral phases, the qualitative elemental concentrations and the amounts of authigenic clays. Silica diagenesis Elsevier Deep sea sediments Elsevier Oxygen isotopes Elsevier Yam, R. oth Kolodny, Y. oth Shemesh, A. oth Enthalten in Elsevier Taylor, William R. ELSEVIER 109 Discovery of Novel DNA Methylation Markers for the Detection of Colorectal Neoplasia: Selection by Methylome-Wide Analysis 2014 journal of the Geochemical Society and the Meteoritical Society New York, NY [u.a.] (DE-627)ELV012653268 volume:268 year:2020 day:1 month:01 pages:368-382 extent:15 https://doi.org/10.1016/j.gca.2019.10.018 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-BIODIV SSG-OLC-PHA 35.70 Biochemie: Allgemeines VZ 42.12 Biophysik VZ 42.15 Zellbiologie VZ AR 268 2020 1 0101 368-382 15 |
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10.1016/j.gca.2019.10.018 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001406.pica (DE-627)ELV048684376 (ELSEVIER)S0016-7037(19)30662-3 DE-627 ger DE-627 rakwb eng 610 VZ 570 VZ BIODIV DE-30 fid 35.70 bkl 42.12 bkl 42.15 bkl Yanchilina, A.G. verfasserin aut From diatom opal-A δ18O to chert δ18O in deep sea sediments 2020transfer abstract 15 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier δ18O signature of marine deep-sea cherts was previously used to reconstruct past ocean temperature and oceanic bottom water δ18O through the Cenozoic and Mesozoic periods. Oxygen isotopes in deep-sea cherts which were never exposed to meteoric water exhibit a wide range of values indicating that the evolution and maturation of biogenic amorphous opal (opal-A) to opal-CT and microquartz chert is accompanied by isotopic changes. We measured δ18O of diatom opal-A, opal-CT, and microquartz chert in downcore profiles of sediment cores ODP 795 and 799 from the Sea of Japan. Diatom opal-A, opal-CT and microquartz chert were separated and purified from the bulk sediment. This was followed by XRD, SEM/EDS and XPS to identify and quantify the mineral phases, the qualitative elemental concentrations and the amounts of authigenic clays. δ18O signature of marine deep-sea cherts was previously used to reconstruct past ocean temperature and oceanic bottom water δ18O through the Cenozoic and Mesozoic periods. Oxygen isotopes in deep-sea cherts which were never exposed to meteoric water exhibit a wide range of values indicating that the evolution and maturation of biogenic amorphous opal (opal-A) to opal-CT and microquartz chert is accompanied by isotopic changes. We measured δ18O of diatom opal-A, opal-CT, and microquartz chert in downcore profiles of sediment cores ODP 795 and 799 from the Sea of Japan. Diatom opal-A, opal-CT and microquartz chert were separated and purified from the bulk sediment. This was followed by XRD, SEM/EDS and XPS to identify and quantify the mineral phases, the qualitative elemental concentrations and the amounts of authigenic clays. Silica diagenesis Elsevier Deep sea sediments Elsevier Oxygen isotopes Elsevier Yam, R. oth Kolodny, Y. oth Shemesh, A. oth Enthalten in Elsevier Taylor, William R. ELSEVIER 109 Discovery of Novel DNA Methylation Markers for the Detection of Colorectal Neoplasia: Selection by Methylome-Wide Analysis 2014 journal of the Geochemical Society and the Meteoritical Society New York, NY [u.a.] (DE-627)ELV012653268 volume:268 year:2020 day:1 month:01 pages:368-382 extent:15 https://doi.org/10.1016/j.gca.2019.10.018 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-BIODIV SSG-OLC-PHA 35.70 Biochemie: Allgemeines VZ 42.12 Biophysik VZ 42.15 Zellbiologie VZ AR 268 2020 1 0101 368-382 15 |
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Enthalten in 109 Discovery of Novel DNA Methylation Markers for the Detection of Colorectal Neoplasia: Selection by Methylome-Wide Analysis New York, NY [u.a.] volume:268 year:2020 day:1 month:01 pages:368-382 extent:15 |
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Enthalten in 109 Discovery of Novel DNA Methylation Markers for the Detection of Colorectal Neoplasia: Selection by Methylome-Wide Analysis New York, NY [u.a.] volume:268 year:2020 day:1 month:01 pages:368-382 extent:15 |
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from diatom opal-a δ18o to chert δ18o in deep sea sediments |
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From diatom opal-A δ18O to chert δ18O in deep sea sediments |
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δ18O signature of marine deep-sea cherts was previously used to reconstruct past ocean temperature and oceanic bottom water δ18O through the Cenozoic and Mesozoic periods. Oxygen isotopes in deep-sea cherts which were never exposed to meteoric water exhibit a wide range of values indicating that the evolution and maturation of biogenic amorphous opal (opal-A) to opal-CT and microquartz chert is accompanied by isotopic changes. We measured δ18O of diatom opal-A, opal-CT, and microquartz chert in downcore profiles of sediment cores ODP 795 and 799 from the Sea of Japan. Diatom opal-A, opal-CT and microquartz chert were separated and purified from the bulk sediment. This was followed by XRD, SEM/EDS and XPS to identify and quantify the mineral phases, the qualitative elemental concentrations and the amounts of authigenic clays. |
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δ18O signature of marine deep-sea cherts was previously used to reconstruct past ocean temperature and oceanic bottom water δ18O through the Cenozoic and Mesozoic periods. Oxygen isotopes in deep-sea cherts which were never exposed to meteoric water exhibit a wide range of values indicating that the evolution and maturation of biogenic amorphous opal (opal-A) to opal-CT and microquartz chert is accompanied by isotopic changes. We measured δ18O of diatom opal-A, opal-CT, and microquartz chert in downcore profiles of sediment cores ODP 795 and 799 from the Sea of Japan. Diatom opal-A, opal-CT and microquartz chert were separated and purified from the bulk sediment. This was followed by XRD, SEM/EDS and XPS to identify and quantify the mineral phases, the qualitative elemental concentrations and the amounts of authigenic clays. |
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δ18O signature of marine deep-sea cherts was previously used to reconstruct past ocean temperature and oceanic bottom water δ18O through the Cenozoic and Mesozoic periods. Oxygen isotopes in deep-sea cherts which were never exposed to meteoric water exhibit a wide range of values indicating that the evolution and maturation of biogenic amorphous opal (opal-A) to opal-CT and microquartz chert is accompanied by isotopic changes. We measured δ18O of diatom opal-A, opal-CT, and microquartz chert in downcore profiles of sediment cores ODP 795 and 799 from the Sea of Japan. Diatom opal-A, opal-CT and microquartz chert were separated and purified from the bulk sediment. This was followed by XRD, SEM/EDS and XPS to identify and quantify the mineral phases, the qualitative elemental concentrations and the amounts of authigenic clays. |
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