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The Hakobuchi Formation is a geological formation in Hokkaido, Japan. It is the uppermost unit of the Yezo Group, being early Maastrichtian in age. It consists of bioturbated glauconitic sandstones, siltstones and conglomerates with coaly mudstone and minor tuffite. It was deposited in a continental shelf setting. It is noted for its fossil content with the invertebrates mainly consisting of bivalves and ammonites. With vertebrates including the mosasaurs Mosasaurus hobetsuensis and Phosphorosaurus ponpetelegans. As well the sea turtle Mesodermochelys and the hadrosaurid dinosaur Kamuysaurus.

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  • Hakobuchi Formation (en)
  • 函淵層 (ja)
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  • The Hakobuchi Formation is a geological formation in Hokkaido, Japan. It is the uppermost unit of the Yezo Group, being early Maastrichtian in age. It consists of bioturbated glauconitic sandstones, siltstones and conglomerates with coaly mudstone and minor tuffite. It was deposited in a continental shelf setting. It is noted for its fossil content with the invertebrates mainly consisting of bivalves and ammonites. With vertebrates including the mosasaurs Mosasaurus hobetsuensis and Phosphorosaurus ponpetelegans. As well the sea turtle Mesodermochelys and the hadrosaurid dinosaur Kamuysaurus. (en)
  • 函淵層(はこぶちそう)は、日本の北海道の地層。蝦夷層群の最上部の累層であり、下部カンパニアン階 - 暁新統に相当する。を受けた海緑石質砂岩、シルト岩、炭質泥岩と少量の層灰岩からなる礫岩で主に構成される。当該の層は大陸棚に堆積した。主に二枚貝類とアンモナイトからなる無脊椎動物の化石が産出することが特筆されるほか、脊椎動物ではモササウルス科のモササウルス・ホベツエンシスやフォスフォロサウルス・ポンペテレガンスが産出している。この他にはウミガメのメソダーモケリス、ハドロサウルス科の恐竜であるカムイサウルスがある。 (ja)
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  • Hakobuchi Formation (en)
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  • Maastrichtian (en)
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  • The Hakobuchi Formation is a geological formation in Hokkaido, Japan. It is the uppermost unit of the Yezo Group, being early Maastrichtian in age. It consists of bioturbated glauconitic sandstones, siltstones and conglomerates with coaly mudstone and minor tuffite. It was deposited in a continental shelf setting. It is noted for its fossil content with the invertebrates mainly consisting of bivalves and ammonites. With vertebrates including the mosasaurs Mosasaurus hobetsuensis and Phosphorosaurus ponpetelegans. As well the sea turtle Mesodermochelys and the hadrosaurid dinosaur Kamuysaurus. (en)
  • 函淵層(はこぶちそう)は、日本の北海道の地層。蝦夷層群の最上部の累層であり、下部カンパニアン階 - 暁新統に相当する。を受けた海緑石質砂岩、シルト岩、炭質泥岩と少量の層灰岩からなる礫岩で主に構成される。当該の層は大陸棚に堆積した。主に二枚貝類とアンモナイトからなる無脊椎動物の化石が産出することが特筆されるほか、脊椎動物ではモササウルス科のモササウルス・ホベツエンシスやフォスフォロサウルス・ポンペテレガンスが産出している。この他にはウミガメのメソダーモケリス、ハドロサウルス科の恐竜であるカムイサウルスがある。 (ja)
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