Research output: Contribution to journal › Article › peer-review
Magneto- and carbon-isotope stratigraphy of the Lower-Middle Bathonian in the Sokur section (Saratov, Central Russia) : implications for global correlation. / Dzyuba, O. S.; Yu Guzhikov, A.; Manikin, A. G. et al.
In: Russian Geology and Geophysics, Vol. 58, No. 2, 01.02.2017, p. 206-224.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - Magneto- and carbon-isotope stratigraphy of the Lower-Middle Bathonian in the Sokur section (Saratov, Central Russia)
T2 - implications for global correlation
AU - Dzyuba, O. S.
AU - Yu Guzhikov, A.
AU - Manikin, A. G.
AU - Shurygin, B. N.
AU - Grishchenko, V. A.
AU - Kosenko, I. N.
AU - Surinskii, A. M.
AU - Seltzer, V. B.
AU - Urman, O. S.
PY - 2017/2/1
Y1 - 2017/2/1
N2 - The discovery of Tethyan and Boreal fossils in Bathonian deposits of the Sokur section in the vicinity of Saratov (Central Russia) reopened the possibility of direct correlation of the Bathonian sections in different paleobiogeographic provinces, which require further integrated studies involving both paleontological (based on different groups of fauna) and physicochemical (paleomagnetic and isotope-geochemical) methods. Stable carbon isotope data for belemnite (Cylindroteuthididae) rostra from the Sokur section show that the Subboreal Oraniceras besnosovi Zone and Boreal Arcticoceras harlandi Subzone are correlated with the Zigzag Zone of the standard scale, whereas the Boreal A. ishmae Subzone can be correlated completely or, even partly, with the Tenuiplicatus Zone. We identified equivalents of chrons of the geomagnetic polarity time scale (GPTS): e-Bath N, m-Bath R, and lt-Bath N, corresponding to the Lower-Middle Bathonian and, possibly, lowermost Upper Bathonian.
AB - The discovery of Tethyan and Boreal fossils in Bathonian deposits of the Sokur section in the vicinity of Saratov (Central Russia) reopened the possibility of direct correlation of the Bathonian sections in different paleobiogeographic provinces, which require further integrated studies involving both paleontological (based on different groups of fauna) and physicochemical (paleomagnetic and isotope-geochemical) methods. Stable carbon isotope data for belemnite (Cylindroteuthididae) rostra from the Sokur section show that the Subboreal Oraniceras besnosovi Zone and Boreal Arcticoceras harlandi Subzone are correlated with the Zigzag Zone of the standard scale, whereas the Boreal A. ishmae Subzone can be correlated completely or, even partly, with the Tenuiplicatus Zone. We identified equivalents of chrons of the geomagnetic polarity time scale (GPTS): e-Bath N, m-Bath R, and lt-Bath N, corresponding to the Lower-Middle Bathonian and, possibly, lowermost Upper Bathonian.
KW - Bathonian
KW - Boreal-Tethyan correlation
KW - chemostratigraphy
KW - magnetostratigraphy
KW - paleotemperature
KW - Russian Plate
KW - BELEMNITE ROSTRA
KW - NORTHERN SPAIN
KW - SIGNALS
KW - PALEOENVIRONMENTAL IMPLICATIONS
KW - SEDIMENTARY SETTINGS
KW - BAJOCIAN
KW - STABLE-ISOTOPE
KW - BASIN
KW - MAGNETOSTRATIGRAPHY
KW - FOSSILS
KW - Boreal Tethyan correlation
UR - http://www.scopus.com/inward/record.url?scp=85013020883&partnerID=8YFLogxK
U2 - 10.1016/j.rgg.2016.01.022
DO - 10.1016/j.rgg.2016.01.022
M3 - Article
AN - SCOPUS:85013020883
VL - 58
SP - 206
EP - 224
JO - Russian Geology and Geophysics
JF - Russian Geology and Geophysics
SN - 1068-7971
IS - 2
ER -
ID: 9640430