High-resolution terrestrial carbon isotope and planktic foraminiferal records of the Upper Cenomanian to the Lower Campanian in the Northwest Pacific

Takashima, Reishi; Nishi, Hiroshi; Yamanaka, Toshiro; Hayashi, Keitaro; Waseda, Amane; Obuse, Akiko; Tomosugi, Takashige; Deguchi, Naoki; Mochizuki, Sunao

doi:10.1016/j.epsl.2009.11.058

Cited by 60 publications

(63 citation statements)

References 45 publications

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“…The Hydrogen Index (HI) is the ra- Haboro R. Haboro R. The study areas. The northern rectangle is the Haboro area, the southern area is the Obira area, the middle rectangle with dashed line (a) is the Kotanbetsu area studied by Takashima et al (2010), and the southern rectangle with dashed line (b) is the area studied by Uramoto et al (2007Uramoto et al ( , 2009). (C) Geological map of the Haboro area.…”

Section: Methodsmentioning

confidence: 99%

“…In the present study, higherresolution δ 13 C data are reported, and the analysis spans the Coniacian through to the lower Campanian. The need for a chronostratigraphic revision of the Japanese inoceramid zonation was indicated by Takashima et al (2010) in their high-resolution δ 13 C stratigraphy for the Upper Cenomanian through to Lower Campanian of the Kotanbetsu area of Hokkaido. However, Takashima et al (2010) reported the δ 13 C data from a single area and the only fossil records used were those of the inoceramids reported by Wani and Hirano (2000) from the same section.…”

Section: Introductionmentioning

confidence: 99%

“…The need for a chronostratigraphic revision of the Japanese inoceramid zonation was indicated by Takashima et al (2010) in their high-resolution δ 13 C stratigraphy for the Upper Cenomanian through to Lower Campanian of the Kotanbetsu area of Hokkaido. However, Takashima et al (2010) reported the δ 13 C data from a single area and the only fossil records used were those of the inoceramids reported by Wani and Hirano (2000) from the same section. In the present study, on the other hand, the δ 13 C analyses were performed on material from sections with rich macrofossil and microfossil records in two different areas of Hokkaido.…”

Section: Introductionmentioning

confidence: 99%

“…Temporal fluctuations in the carbon isotope ratios (δ 13 C) of marine carbonates are a reliable tool for regional and international correlations (e.g., Jenkyns et al 1994;Erbacher et al 1996;Voigt and Hilbrecht 1997;Stoll and Schrag 2000;Voigt 2000;Jarvis et al 2002Jarvis et al , 2006Voigt et al 2010). In Japan, δ 13 C stratigraphic studies on terrestrial organic matter have been undertaken for the Yezo Group (Hasegawa 1992;Hasegawa and Saito 1993;Hasegawa 1997;Hirano and Fukuju 1997;Hasegawa and Hatsugai 2000;Ando et al 2002Ando et al , 2003Hasegawa et al 2003;Ando and Kakegawa 2007;Uramoto et al 2007Uramoto et al , 2009Takashima et al 2010). Hasegawa (1997) discussed the resemblance between the δ 13 C curves for marine carbonates and those for terrestrial organic matter, and concluded that the δ 13 C stratigraphy of terrestrial organic matter provides a reliable tool for correlation with the marine carbonates.…”

Section: Introductionmentioning

confidence: 99%

“…In the present study, on the other hand, the δ 13 C analyses were performed on material from sections with rich macrofossil and microfossil records in two different areas of Hokkaido. The high-resolution δ 13 C stratigraphy from the upper Turonian to the lower Campanian of the studied succession was then compared with the δ 13 C fluctuations reported by Voigt and Hilbrecht (1997), Hasegawa et al (2003), Jarvis et al (2006), Takashima et al (2010), and Voigt et al (2010).…”

Section: Introductionmentioning

confidence: 99%

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A revised inoceramid biozonation for the Upper Cretaceous based on high-resolution carbon isotope stratigraphy in northwestern Hokkaido, Japan

Hayakawa¹,

Hirano²

2013

Acta Geologica Polonica

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ABSTRACT:Hayakawa, T., Hirano, H. 2013. A revised inoceramid biozonation for the Upper Cretaceous based on high-resolution carbon isotope stratigraphy in northwestern Hokkaido, Japan. Acta Geologica Polonica, 63 (2), 239-263. Warszawa.Biostratigraphic correlations of inoceramid bivalves between the North Pacific and Euramerican provinces have been difficult because the inoceramid biostratigraphy of the Japanese strata has been based on endemic species of the northwest Pacific. In this study, carbon stable isotope fluctuations of terrestrial organic matter are assembled for the Upper Cretaceous Yezo Group in the Haboro and Obira areas, Hokkaido, Japan, in order to revise the chronology of the inoceramid biozonation in Japan. The carbon isotope curves are correlated with those of marine carbonates in English and German sections with the aid of age-diagnostic taxa. According to the correlations of the carbon isotope curves, 11 isotope events are recognised in the sections studied. As a result of these correlations, the chronology of the inoceramid biozones of the Northwest Pacific has been considerably revised. The revised inoceramid biozones suggest that the timing of the origination and extinction of the inoceramids in the North Pacific biotic province is different from the stage/substage boundaries defined by inoceramids, as used in Europe and North America.

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Section: Methodsmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

See 3 more Smart Citations

A revised inoceramid biozonation for the Upper Cretaceous based on high-resolution carbon isotope stratigraphy in northwestern Hokkaido, Japan

Hayakawa¹,

Hirano²

2013

Acta Geologica Polonica

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Testing geological proxies for deep‐time tidal model simulations

Guo,

Fitzgerald,

Hewitt

et al. 2023

The Depositional Record

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Tides are a key driver of a range of Earth system processes, and we now have the capacity to simulate tidal dynamics on a range of temporal and spatial scales. Deep‐time tidal model simulations have been used to provide insight into past ocean circulation patterns, evolution of life and the developments of the Earth‐Moon system's orbital configuration. However, these tidal model simulations are relatively poorly constrained and validated because of a lack of readily available proxies. The feasibility of using two types of proxy is explored here; (1) sedimentary deposits which can directly estimate palaeotidal ranges, and (2) black shale, to constrain three palaeotidal model simulations for different time slices. Specifically, three palaeotidal range proxies were used for the early Devonian (400 Ma), three palaeotidal range proxies and five black shales for the lower Jurassic (185 Ma), and eight black shales for the early Cretaceous (95 Ma). Both tidal proxies confirm the tidal model results in most locations. The model results for 400 Ma and 185 Ma matched 2/3 of the palaeotidal range proxies for each of these periods. The locations of black shale were compared with tidal front locations predicted by the model outputs based on the Simpson–Hunter parameter and the model results from 95 to 185 Ma agree with the black shale proxies in 10/13 of the locations. In the cases where there is a disagreement, the model resolution is probably too low to fully resolve the details of the coastal topography, or—in one case—the palaeobathymetry is incorrect. Consequently, it is argued that it is worth expanding this type of work, and that such data can be used to validate both models and reconstructions.

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Intercontinental correlation of organic carbon and carbonate stable isotope records: evidence of climate and sea‐level change during the Turonian (Cretaceous)

Jarvis

Trabucho‐Alexandre

Gröcke

et al. 2015

The Depositional Record

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Carbon (d 13 C org , d 13 C carb ) and oxygen (d 18 O carb ) isotope records are presented for an expanded Upper Cretaceous (Turonian-Coniacian) hemipelagic succession cored in the central Bohemian Cretaceous Basin, Czech Republic. Geophysical logs, biostratigraphy and stable carbon isotope chemostratigraphy provide a high-resolution stratigraphic framework. The d 13 C carb and d 13 C org profiles are compared, and the time series correlated with published coeval marine and non-marine isotope records from Europe, North America and Japan. All previously named Turonian carbon isotope events are identified and correlated at high-resolution between multiple sections, in different facies, basins and continents. The viability of using both carbonate and organic matter carbon isotope chemostratigraphy for improved stratigraphic resolution, for placing stage boundaries, and for intercontinental correlation is demonstrated, but anchoring the time series using biostratigraphic data is essential. An Early to Middle Turonian thermal maximum followed by a synchronous episode of stepped cooling throughout Europe during the Middle to Late Turonian is evidenced by bulk carbonate and brachiopod shell d18 O carb data, and regional changes in the distribution and composition of macrofaunal assemblages. The Late Turonian Cool Phase in Europe was coincident with a period of long-term sea-level fall, with significant water-mass reorganization occurring during the mid-Late Turonian maximum lowstand. Falling D 13 C (d 13 C carb -d 13 C org ) trends coincident with two major cooling pulses, point to pCO 2 drawdown accompanying cooling, but the use of paired carbon isotopes as a high-resolution pCO 2 proxy is compromised in the low-carbonate sediments of the Bohemian Basin study section by diagenetic overprinting of the d 13 C carb record. Carbon isotope chemostratigraphy is confirmed as a powerful tool for testing and refining intercontinental and marine to terrestrial correlations.

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High-resolution terrestrial carbon isotope and planktic foraminiferal records of the Upper Cenomanian to the Lower Campanian in the Northwest Pacific

Cited by 60 publications

References 45 publications

A revised inoceramid biozonation for the Upper Cretaceous based on high-resolution carbon isotope stratigraphy in northwestern Hokkaido, Japan

A revised inoceramid biozonation for the Upper Cretaceous based on high-resolution carbon isotope stratigraphy in northwestern Hokkaido, Japan

Testing geological proxies for deep‐time tidal model simulations

Intercontinental correlation of organic carbon and carbonate stable isotope records: evidence of climate and sea‐level change during the Turonian (Cretaceous)

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