Stratigraphy and sedimentary environment of the Lower Cretaceous system in the Katsuuragawa Basin, Southwest Japan:Comparison of the two Cretaceous subbelts in the Chichibu Belt

Matsukawa, Masaki; Eto, Fumiya

doi:10.5575/geosoc.93.491

Cited by 12 publications

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“…12. Stratigraphy of Lower Cretaceous sections in both outer and inner zones of southwest Japan and stratigraphical occurrence of nonmarine molluscan species and transgressiveeregressive phases (Matsukawa, 1983;Matsukawa and Eto, 1987;Kozai and Ishida, 2003;Matsukawa et al, 2003a).…”

Section: Evaluation Of Nonmarine Molluscan Assemblagesmentioning

confidence: 99%

The Cretaceous Tetori biota in Japan and its evolutionary significance for terrestrial ecosystems in Asia

Matsukawa

Itô

Nishida

et al. 2006

Cretaceous Research

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Section: Evaluation Of Nonmarine Molluscan Assemblagesmentioning

confidence: 99%

The Cretaceous Tetori biota in Japan and its evolutionary significance for terrestrial ecosystems in Asia

Matsukawa

Itô

Nishida

et al. 2006

Cretaceous Research

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“…Katsuura area, Shikoku.-Lower Cretaceous deposits, ranging from the Barremian to Albian stages, are exposed in the Katsuura area, Tokushima Prefecture, Shikoku. The strata trend in the E-W direction, forming a syncline, and are divided into the Tatsukawa, Hanoura, Hoji, and Fujikawa formations, in ascending stratigraphic order (see Nakai, 1968;Matsukawa and Eto, 1987). The former three formations consist of shallow-marine and brack ish-water strata, while the Fujikawa Formation is an offshore mudstone.…”

Section: Note On Stratigraphymentioning

confidence: 99%

The ammonoidDesmocerasin the Upper Albian (Lower Cretaceous) of Japan

Kawabe

Haggart

2003

J. Paleontol.

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The Upper Albian Desmoceras species of Japan are described, based on material from the Yezo Supergroup in Hokkaido, north Japan, and from the Fujikawa Formation in Shikoku, southwest Japan. Based on comparative analysis of morphologic variation and shell growth of relevant specimens, we assign the present material to two species: Desmoceras (Desmoceras) latidorsatum (Michelin, 1838) and Desmoceras (Pseudouhligella) poronaicum Yabe, 1904. Japanese examples of the latter species have been previously referred to “Desmoceras (Pseudouhligella) dawsoni,” a Canadian species present on Queen Charlotte Islands, British Columbia, but not represented in the Japanese Islands. Desmoceras (Pseudouhligella) poronaicum is also known from British Columbia.The subgenus Pseudouhligella presumably originated in the eastern Pacific during the Late Albian and subsequently migrated to the western Pacific during latest Albian to earliest Cenomanian time. Desmoceras (D.) latidorsatum is a Tethyan form; its presence in the Upper Albian of the North Pacific probably reflects a northward excursion of warm-water currents from the tropical region during Late Albian time.

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Oceanward shifting of the Hauterivian (Early Cretaceous) arc-trench system in East Asia

Takahashi

Matsukawa

2000

Geosci J

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Stratigraphy and sedimentary environment of the Lower Cretaceous system in the Katsuuragawa Basin, Southwest Japan:Comparison of the two Cretaceous subbelts in the Chichibu Belt

Cited by 12 publications

References 0 publications

The Cretaceous Tetori biota in Japan and its evolutionary significance for terrestrial ecosystems in Asia

The Cretaceous Tetori biota in Japan and its evolutionary significance for terrestrial ecosystems in Asia

The ammonoidDesmocerasin the Upper Albian (Lower Cretaceous) of Japan

Oceanward shifting of the Hauterivian (Early Cretaceous) arc-trench system in East Asia

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