Global synchroneity of a positive carbon isotope excursion at the Cenomanian/Turonian boundary: Validation by calcareous microfossil biostratigraphy of the Yezo Group, Hokkaido, Japan

• Published in: Island Arc
• Main Authors: Hasegawa, Takashi, Saito, Tsunemasa
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 1993
• Subjects: Planktonic foraminifera
• Online Access: http://dx.doi.org/10.1111/j.1440-1738.1993.tb00085.x; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1440-1738.1993.tb00085.x; https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1440-1738.1993.tb00085.x

Abstract Isotopic analyses of organic carbon from the mid‐Cretaceous sequence in Hokkaido, Japan, revealed a 2‰ positive excursion of δ 13 C values at the biostratigraphically defined Cenomanian/Turonian (C/T) boundary recognized in the Yezo Group. The planktonic foraminiferal Whiteinella archaeocretacea Zone, which is known to bracket the Cenomanian/Turonian boundary elsewhere in the world, was recognized in the Oyubari area of central Hokkaido based on the distribution of commonly occurring planktonic foraminifera. In the Tappu area of northwestern Hokkaido, where diagnostic planktonic foraminifera are rare but calcareous nannoplankton occur commonly, the interval coeval with the W. archaeocretacea Zone can also be established by recognizing the conjoined last appearance levels of Corollithion kennedyi and Axopodorhabdus albianus , both calcareous nannoplankton species. Carbon isotope profiles exhibit a similar pattern with comparable peaks and troughs occurring in the same stratigraphic position in the sequences. A prominent, positive 2‰ shift of δ 13 C values, here called ‘δ 13 C spike’ occurs in the middle of the W. archaeocretacea Zone in the Oyubari area and just above the conjoined last appearances of the two above‐mentioned nannoplankton taxa in the Tappu area. The Cenomanian/Turonian boundary can be drawn just above the peak position of the spike in both sections. The Rock Eval analyses and biomarker analyses of organic carbon indicate that organic carbon subjected to our isotope analyses is of terrestrial origin. Therefore, the observed 2%o shift should reflect changes in the isotopic composition of the atmospheric CO 2 . A unique layer composed predominantly of sand‐grain sized spumellarian Radiolaria is present immediately above the δ 13 C spike both in the Oyubari and Tappu areas, suggesting an increasing availability of both nutrients and silica in surface waters.