Quo vadis, Tommotian? › Research Explorer

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Quo vadis, Tommotian? / Grazhdankin, Dmitriy V.; Marusin, Vasiliy V.; Izokh, Olga P. et al.

In: Geological Magazine, Vol. 157, No. 1, 0016756819001286, 01.01.2020, p. 22-34.

Research output: Contribution to journal › Article › peer-review

Harvard

Grazhdankin, DV , Marusin, VV , Izokh, OP, Karlova, GA, Kochnev, BB, Markov, GE, Nagovitsin, KE, Sarsembaev, Z, Peek, S, Cui, H & Kaufman, AJ 2020, 'Quo vadis, Tommotian?', Geological Magazine, vol. 157, no. 1, 0016756819001286, pp. 22-34. https://doi.org/10.1017/S0016756819001286

APA

Grazhdankin, D. V., Marusin, V. V., Izokh, O. P., Karlova, G. A., Kochnev, B. B., Markov, G. E., Nagovitsin, K. E., Sarsembaev, Z., Peek, S., Cui, H., & Kaufman, A. J. (2020). Quo vadis, Tommotian? Geological Magazine, 157(1), 22-34. [0016756819001286]. https://doi.org/10.1017/S0016756819001286

Vancouver

Grazhdankin DV , Marusin VV , Izokh OP, Karlova GA, Kochnev BB, Markov GE et al. Quo vadis, Tommotian? Geological Magazine. 2020 Jan 1;157(1):22-34. 0016756819001286. doi: 10.1017/S0016756819001286

Author

Grazhdankin, Dmitriy V. ; Marusin, Vasiliy V. ; Izokh, Olga P. et al. / Quo vadis, Tommotian?. In: Geological Magazine. 2020 ; Vol. 157, No. 1. pp. 22-34.

BibTeX

@article{76f1d5b2e9c54281a690d9cfd128c643,

title = "Quo vadis, Tommotian?",

abstract = "The concept of the Tommotian Regional Stage of the Siberian Platform has been closely linked to the idea of the 'Cambrian Explosion' of animals and protists when the entire Earth system shifted rapidly into Phanerozoic mode. We conducted a multidisciplinary study of an informal 'synstratotype' of the lower Tommotian boundary in the upper Mattaia Formation, Kessyusa Group in the Olenek Uplift, NE of the Siberian Platform. The Mattaia Formation characterizes an upper shoreface to inner-shelf depositional setting and provides important faunal ties and correlation with carbonate-dominated and aliminosiliciclastic open-shelf areas. A section of the upper Mattaia Formation at Boroulakh, Olenek River is suggested here as a model for the Global Boundary Stratotype Section and Point for the base of the Cambrian Stage 2. This level contains the lowermost occurrence of the cosmopolitan fossil helcionelloid mollusc Aldanella attleborensis. Section global markers near the base of the stage include a positive excursion of δ13C values reaching +5.4‰, a U-Pb zircon date of 529.7 ± 0.3 Ma, massive appearance of diverse small skeletal fossils (including Watsonella crosbyi), a sudden increase in diversity and abundance of trace fossils, as well as a conspicuous increase in depth and intensity of bioturbation. Coincidently, it is this level that has always been regarded as the lower Tommotian boundary on the Olenek Uplift.",

keywords = "biostratigraphy, Cambrian Stage 2, chemostratigraphy, Olenek Uplift, Siberian Platform, PRECAMBRIAN-CAMBRIAN BOUNDARY, OLENEK UPLIFT, NORTHEASTERN-SIBERIAN-PLATFORM, STAGE, INTERNATIONAL-COMMISSION, RADIATION, CARBON-ISOTOPE STRATIGRAPHY, CHRONOSTRATIGRAPHY, BIOSTRATIGRAPHICAL CONSTRAINTS, RIVER SECTION",

author = "Grazhdankin, {Dmitriy V.} and Marusin, {Vasiliy V.} and Izokh, {Olga P.} and Karlova, {Galina A.} and Kochnev, {Boris B.} and Markov, {Georgiy E.} and Nagovitsin, {Konstantin E.} and Zhiger Sarsembaev and Sara Peek and Huan Cui and Kaufman, {Alan J.}",

year = "2020",

month = jan,

day = "1",

doi = "10.1017/S0016756819001286",

language = "English",

volume = "157",

pages = "22--34",

journal = "Geological Magazine",

issn = "0016-7568",

publisher = "Cambridge University Press",

number = "1",

}

RIS

TY - JOUR

T1 - Quo vadis, Tommotian?

AU - Grazhdankin, Dmitriy V.

AU - Marusin, Vasiliy V.

AU - Izokh, Olga P.

AU - Karlova, Galina A.

AU - Kochnev, Boris B.

AU - Markov, Georgiy E.

AU - Nagovitsin, Konstantin E.

AU - Sarsembaev, Zhiger

AU - Peek, Sara

AU - Cui, Huan

AU - Kaufman, Alan J.

PY - 2020/1/1

Y1 - 2020/1/1

N2 - The concept of the Tommotian Regional Stage of the Siberian Platform has been closely linked to the idea of the 'Cambrian Explosion' of animals and protists when the entire Earth system shifted rapidly into Phanerozoic mode. We conducted a multidisciplinary study of an informal 'synstratotype' of the lower Tommotian boundary in the upper Mattaia Formation, Kessyusa Group in the Olenek Uplift, NE of the Siberian Platform. The Mattaia Formation characterizes an upper shoreface to inner-shelf depositional setting and provides important faunal ties and correlation with carbonate-dominated and aliminosiliciclastic open-shelf areas. A section of the upper Mattaia Formation at Boroulakh, Olenek River is suggested here as a model for the Global Boundary Stratotype Section and Point for the base of the Cambrian Stage 2. This level contains the lowermost occurrence of the cosmopolitan fossil helcionelloid mollusc Aldanella attleborensis. Section global markers near the base of the stage include a positive excursion of δ13C values reaching +5.4‰, a U-Pb zircon date of 529.7 ± 0.3 Ma, massive appearance of diverse small skeletal fossils (including Watsonella crosbyi), a sudden increase in diversity and abundance of trace fossils, as well as a conspicuous increase in depth and intensity of bioturbation. Coincidently, it is this level that has always been regarded as the lower Tommotian boundary on the Olenek Uplift.

AB - The concept of the Tommotian Regional Stage of the Siberian Platform has been closely linked to the idea of the 'Cambrian Explosion' of animals and protists when the entire Earth system shifted rapidly into Phanerozoic mode. We conducted a multidisciplinary study of an informal 'synstratotype' of the lower Tommotian boundary in the upper Mattaia Formation, Kessyusa Group in the Olenek Uplift, NE of the Siberian Platform. The Mattaia Formation characterizes an upper shoreface to inner-shelf depositional setting and provides important faunal ties and correlation with carbonate-dominated and aliminosiliciclastic open-shelf areas. A section of the upper Mattaia Formation at Boroulakh, Olenek River is suggested here as a model for the Global Boundary Stratotype Section and Point for the base of the Cambrian Stage 2. This level contains the lowermost occurrence of the cosmopolitan fossil helcionelloid mollusc Aldanella attleborensis. Section global markers near the base of the stage include a positive excursion of δ13C values reaching +5.4‰, a U-Pb zircon date of 529.7 ± 0.3 Ma, massive appearance of diverse small skeletal fossils (including Watsonella crosbyi), a sudden increase in diversity and abundance of trace fossils, as well as a conspicuous increase in depth and intensity of bioturbation. Coincidently, it is this level that has always been regarded as the lower Tommotian boundary on the Olenek Uplift.

KW - biostratigraphy

KW - Cambrian Stage 2

KW - chemostratigraphy

KW - Olenek Uplift

KW - Siberian Platform

KW - PRECAMBRIAN-CAMBRIAN BOUNDARY

KW - OLENEK UPLIFT

KW - NORTHEASTERN-SIBERIAN-PLATFORM

KW - STAGE

KW - INTERNATIONAL-COMMISSION

KW - RADIATION

KW - CARBON-ISOTOPE STRATIGRAPHY

KW - CHRONOSTRATIGRAPHY

KW - BIOSTRATIGRAPHICAL CONSTRAINTS

KW - RIVER SECTION

UR - http://www.scopus.com/inward/record.url?scp=85078045251&partnerID=8YFLogxK

U2 - 10.1017/S0016756819001286

DO - 10.1017/S0016756819001286

M3 - Article

AN - SCOPUS:85078045251

VL - 157

SP - 22

EP - 34

JO - Geological Magazine

JF - Geological Magazine

SN - 0016-7568

IS - 1

M1 - 0016756819001286

ER -

ID: 23208790