New results of U–Pb SHRIMP dating of zircons from upper Wuchiapingian (Upper Permian) deposits in northeastern Russia
The first results are presented for U-Pb SHRIMP-II dating of zircons from the upper part of the Khivachian regional horizon (stage) of the Regional Stratigraphic Scale (RSS) of the Permian in northeastern Russia. The obtained isotope age of 255 ± 2 Ma is close to that of the present boundary between...
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| Veröffentlicht in: | Doklady earth sciences 2017-11, Vol.477 (1), p.1348-1352 |
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| creator | Biakov, A. S. Goryachev, N. A. Vedernikov, I. L. Brynko, I. V. Tolmacheva, E. V. |
| description | The first results are presented for U-Pb SHRIMP-II dating of zircons from the upper part of the Khivachian regional horizon (stage) of the Regional Stratigraphic Scale (RSS) of the Permian in northeastern Russia. The obtained isotope age of 255 ± 2 Ma is close to that of the present boundary between the Wuchiapingian and Changhsingian stages of the Permian system in the International Stratigraphic Scale (254.1 Ma). Based on the distribution of bivalves—
Intomodesma
spp. and
Claraioides
aff.
primitivus
(Yin)—in the sections considered, their relations to the stratigraphic positions of the samples considered and dated formerly, and in view of the interregional correlation of recent δ
13
С
org
data for clayey rocks, one may assume with certainty that most of the regional zone of
Intomodesma costatum
corresponds to the upper part of the Wuchiapingian stage. Here, the Changhsingian stage in northeastern Asia complies only with the uppermost part of this zone within the
I. postevenicum
subzone and, partially, of
Otoceras
layers within the
Otoceras concavum
zone. |
| doi_str_mv | 10.1134/S1028334X17110186 |
| format | Article |
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Intomodesma
spp. and
Claraioides
aff.
primitivus
(Yin)—in the sections considered, their relations to the stratigraphic positions of the samples considered and dated formerly, and in view of the interregional correlation of recent δ
13
С
org
data for clayey rocks, one may assume with certainty that most of the regional zone of
Intomodesma costatum
corresponds to the upper part of the Wuchiapingian stage. Here, the Changhsingian stage in northeastern Asia complies only with the uppermost part of this zone within the
I. postevenicum
subzone and, partially, of
Otoceras
layers within the
Otoceras concavum
zone.</description><identifier>ISSN: 1028-334X</identifier><identifier>EISSN: 1531-8354</identifier><identifier>DOI: 10.1134/S1028334X17110186</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Boundary layer ; Earth and Environmental Science ; Earth Sciences ; Geochemistry ; Isotopes ; Lead ; Minerals ; Mollusks ; Permian ; Stratigraphy ; Zirconium</subject><ispartof>Doklady earth sciences, 2017-11, Vol.477 (1), p.1348-1352</ispartof><rights>Pleiades Publishing, Ltd. 2017</rights><rights>Copyright Springer Science & Business Media Nov 2017</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a339t-11b6ea6e4234a7646365f1b63abe66e0a93149806a728da7e245e33d013f5f693</citedby><cites>FETCH-LOGICAL-a339t-11b6ea6e4234a7646365f1b63abe66e0a93149806a728da7e245e33d013f5f693</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S1028334X17110186$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S1028334X17110186$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Biakov, A. S.</creatorcontrib><creatorcontrib>Goryachev, N. A.</creatorcontrib><creatorcontrib>Vedernikov, I. L.</creatorcontrib><creatorcontrib>Brynko, I. V.</creatorcontrib><creatorcontrib>Tolmacheva, E. V.</creatorcontrib><title>New results of U–Pb SHRIMP dating of zircons from upper Wuchiapingian (Upper Permian) deposits in northeastern Russia</title><title>Doklady earth sciences</title><addtitle>Dokl. Earth Sc</addtitle><description>The first results are presented for U-Pb SHRIMP-II dating of zircons from the upper part of the Khivachian regional horizon (stage) of the Regional Stratigraphic Scale (RSS) of the Permian in northeastern Russia. The obtained isotope age of 255 ± 2 Ma is close to that of the present boundary between the Wuchiapingian and Changhsingian stages of the Permian system in the International Stratigraphic Scale (254.1 Ma). Based on the distribution of bivalves—
Intomodesma
spp. and
Claraioides
aff.
primitivus
(Yin)—in the sections considered, their relations to the stratigraphic positions of the samples considered and dated formerly, and in view of the interregional correlation of recent δ
13
С
org
data for clayey rocks, one may assume with certainty that most of the regional zone of
Intomodesma costatum
corresponds to the upper part of the Wuchiapingian stage. Here, the Changhsingian stage in northeastern Asia complies only with the uppermost part of this zone within the
I. postevenicum
subzone and, partially, of
Otoceras
layers within the
Otoceras concavum
zone.</description><subject>Boundary layer</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geochemistry</subject><subject>Isotopes</subject><subject>Lead</subject><subject>Minerals</subject><subject>Mollusks</subject><subject>Permian</subject><subject>Stratigraphy</subject><subject>Zirconium</subject><issn>1028-334X</issn><issn>1531-8354</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp1UM1KAzEQDqJgrT6At4AXPaxmNtns7lFEbaFqaS16W9J2tk1pkzXZpejJd_ANfRJT60EQTzPz_Q18hBwDOwfg4mIILM44F8-QAjDI5A5pQcIhyngidsMe6GjD75MD7xeMCSGSvEXW97imDn2zrD21JR19vn_0x3TYGXTv-nSqam1mG_xNu4k1npbOrmhTVejoUzOZa1UFgVaGno6-wT66VTjP6BQr63UI1YYa6-o5Kl-jM3TQeK_VIdkr1dLj0c9sk9HN9eNVJ-o93HavLnuR4jyvI4CxRCVRxFyoVArJZVIGjKsxSolM5RxEnjGp0jibqhRjkSDnUwa8TEqZ8zY52eZWzr406OtiYRtnwssC8pTlkGQ8DSrYqibOeu-wLCqnV8q9FsCKTb_Fn36DJ956fNCaGbpfyf-avgASMn1T</recordid><startdate>20171101</startdate><enddate>20171101</enddate><creator>Biakov, A. 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S.</au><au>Goryachev, N. A.</au><au>Vedernikov, I. L.</au><au>Brynko, I. V.</au><au>Tolmacheva, E. V.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>New results of U–Pb SHRIMP dating of zircons from upper Wuchiapingian (Upper Permian) deposits in northeastern Russia</atitle><jtitle>Doklady earth sciences</jtitle><stitle>Dokl. Earth Sc</stitle><date>2017-11-01</date><risdate>2017</risdate><volume>477</volume><issue>1</issue><spage>1348</spage><epage>1352</epage><pages>1348-1352</pages><issn>1028-334X</issn><eissn>1531-8354</eissn><abstract>The first results are presented for U-Pb SHRIMP-II dating of zircons from the upper part of the Khivachian regional horizon (stage) of the Regional Stratigraphic Scale (RSS) of the Permian in northeastern Russia. The obtained isotope age of 255 ± 2 Ma is close to that of the present boundary between the Wuchiapingian and Changhsingian stages of the Permian system in the International Stratigraphic Scale (254.1 Ma). Based on the distribution of bivalves—
Intomodesma
spp. and
Claraioides
aff.
primitivus
(Yin)—in the sections considered, their relations to the stratigraphic positions of the samples considered and dated formerly, and in view of the interregional correlation of recent δ
13
С
org
data for clayey rocks, one may assume with certainty that most of the regional zone of
Intomodesma costatum
corresponds to the upper part of the Wuchiapingian stage. Here, the Changhsingian stage in northeastern Asia complies only with the uppermost part of this zone within the
I. postevenicum
subzone and, partially, of
Otoceras
layers within the
Otoceras concavum
zone.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S1028334X17110186</doi><tpages>5</tpages></addata></record> |
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| subjects | Boundary layer Earth and Environmental Science Earth Sciences Geochemistry Isotopes Lead Minerals Mollusks Permian Stratigraphy Zirconium |
| title | New results of U–Pb SHRIMP dating of zircons from upper Wuchiapingian (Upper Permian) deposits in northeastern Russia |
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